- published: 18 Mar 2015
- views: 545
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"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening , changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere.
It is also good to take into consideration the effects of denudation . Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region of denudation . The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies.
Crustal thickening has an upward component of motion and often occurs when continental crust is thrust onto continental crust. Basically nappes from each plate collide and begin to stack one on top of the other; evidence of this process can be seen in preserved ophiolitic nappes , and in rocks with an inverted metamorphic gradient. The preserved inverted metamorphic gradient indicates that nappes were actually stacked on top of each other so quickly, that hot rocks did not have time to equilibrate before being thrust on top of cool rocks. The process of nappe stacking can only continue for so long, as gravity will eventually disallow further vertical growth .
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Tectonic+uplift, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
- published: 29 Sep 2015
- views: 748
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape
- published: 18 Jun 2013
- views: 2277
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic uplift. Powered by MaryTTS, Wiktionary
- published: 30 Apr 2015
- views: 235
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between x=-50 and +50 km) and a 1D stream power law erosion model. River erosion is proportional to slope and water discharge (constant precipitation rate over the entire profile). The dashed line marks the topography that would form in absence of erosion.
Note the steady states reached before 5 Myr (about 3 km max. topography) and at ~8 Myr (flat topography). Note also that at equilibrium, the model correctly predicts uplift rate=erosion rate at every location, and that in the end, total erosion = total uplift
Calculated under Linux with the program tAo by Garcia-Castellanos (2007, EPSL).
There is an explanation here:
http://retosterricolas.blogspot.com/2012/02/steady-state-topography-during.html
+info on the software:
https://sites.google.com/site/daniggcc/software/tao
- published: 15 Feb 2012
- views: 1153
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
- published: 24 Aug 2016
- views: 10
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created and subjected to powerful compression forces which results in uplift of parts of the wax structure.
- published: 21 Nov 2015
- views: 128
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main Great Himalayas to the south, inhabited by people of Indo-Aryan and Tibetan descent. It is one of the most
sparsely populated regions in Jammu and Kashmir.
The largest town in Ladakh is Leh. It is one of the few remaining abodes of Buddhism in South Asia, including the Chittagong Hill Tracts, Bhutan and Sri Lanka; a majority of Ladakhis are Tibetan Buddhists and the rest are mostly Shia Muslims.
(Source Wikipedia)
This footage is part of the professionally-shot broadcast stock footage archive of Wilderness Films India Ltd., the largest collection of imagery from South Asia. The Wilderness Films India collection comprises of thousands of hours of high quality broadcast imagery, mostly shot on HDCAM 1080i High Definition, HDV and XDCAM. Write to us for licensing this footage on a broadcast format, for use in your production! We are happy to be commissioned to film for you or else provide you with broadcast crewing and production solutions across South Asia. We pride ourselves in bringing the best of India and South Asia to the world... Reach us at wfi @ vsnl.com and admin@wildfilmsindia.com.
- published: 13 Feb 2013
- views: 724
Tectonic uplift
Tectonic uplift is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening (such as mountain building events), changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere.
It is also good to take into consideration the effects of denudation (processes that wear away the earth's surface). Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies.
This page contains text from Wikipedia, the Free Encyclopedia -
https://wn.com/Tectonic_uplift
This article is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License, which means that you can copy and modify it as long as the entire work (including additions) remains under this license.
This article is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License, which means that you can copy and modify it as long as the entire work (including additions) remains under this license.
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6:08Plate Tectonics and Uplift
Plate Tectonics and UpliftPlate Tectonics and Uplift
-
2:02Tectonic uplift - Video Learning - WizScience.com
Tectonic uplift - Video Learning - WizScience.comTectonic uplift - Video Learning - WizScience.com
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening , changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. It is also good to take into consideration the effects of denudation . Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region of denudation . The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies. Crustal thickening has an upward component of motion and often occurs when continental crust is thrust onto continental crust. Basically nappes from each plate collide and begin to stack one on top of the other; evidence of this process can be seen in preserved ophiolitic nappes , and in rocks with an inverted metamorphic gradient. The preserved inverted metamorphic gradient indicates that nappes were actually stacked on top of each other so quickly, that hot rocks did not have time to equilibrate before being thrust on top of cool rocks. The process of nappe stacking can only continue for so long, as gravity will eventually disallow further vertical growth . Wiz Science™ is "the" learning channel for children and all ages. SUBSCRIBE TODAY Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK. Background Music: "The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library. This video uses material/images from https://en.wikipedia.org/wiki/Tectonic+uplift, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms. -
6:20Fossils and tectonic uplift in Taranaki
Fossils and tectonic uplift in TaranakiFossils and tectonic uplift in Taranaki
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape -
2:57Mountain building: Uplift, erosion and exhumation
Mountain building: Uplift, erosion and exhumationMountain building: Uplift, erosion and exhumation
-
0:26Tectonic-uplift Meaning
Tectonic-uplift Meaning -
0:30Tectonic uplift Meaning
Tectonic uplift MeaningTectonic uplift Meaning
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic uplift. Powered by MaryTTS, Wiktionary -
0:41Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D modelSteady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between x=-50 and +50 km) and a 1D stream power law erosion model. River erosion is proportional to slope and water discharge (constant precipitation rate over the entire profile). The dashed line marks the topography that would form in absence of erosion. Note the steady states reached before 5 Myr (about 3 km max. topography) and at ~8 Myr (flat topography). Note also that at equilibrium, the model correctly predicts uplift rate=erosion rate at every location, and that in the end, total erosion = total uplift Calculated under Linux with the program tAo by Garcia-Castellanos (2007, EPSL). There is an explanation here: http://retosterricolas.blogspot.com/2012/02/steady-state-topography-during.html +info on the software: https://sites.google.com/site/daniggcc/software/tao -
0:55tectonic uplift final
tectonic uplift finaltectonic uplift final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require. -
2:41Wax Geology Uplift
Wax Geology UpliftWax Geology Uplift
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created and subjected to powerful compression forces which results in uplift of parts of the wax structure. -
1:10Signs of Himalayan uplift and tectonic plates in Ladakh
Signs of Himalayan uplift and tectonic plates in LadakhSigns of Himalayan uplift and tectonic plates in Ladakh
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main Great Himalayas to the south, inhabited by people of Indo-Aryan and Tibetan descent. It is one of the most sparsely populated regions in Jammu and Kashmir. The largest town in Ladakh is Leh. It is one of the few remaining abodes of Buddhism in South Asia, including the Chittagong Hill Tracts, Bhutan and Sri Lanka; a majority of Ladakhis are Tibetan Buddhists and the rest are mostly Shia Muslims. (Source Wikipedia) This footage is part of the professionally-shot broadcast stock footage archive of Wilderness Films India Ltd., the largest collection of imagery from South Asia. The Wilderness Films India collection comprises of thousands of hours of high quality broadcast imagery, mostly shot on HDCAM 1080i High Definition, HDV and XDCAM. Write to us for licensing this footage on a broadcast format, for use in your production! We are happy to be commissioned to film for you or else provide you with broadcast crewing and production solutions across South Asia. We pride ourselves in bringing the best of India and South Asia to the world... Reach us at wfi @ vsnl.com and admin@wildfilmsindia.com.
-
Plate Tectonics and Uplift
published: 18 Mar 2015 -
Tectonic uplift - Video Learning - WizScience.com
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening , changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere. It is also good to take into consideration the effects of denudation . Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region...
published: 29 Sep 2015 -
Fossils and tectonic uplift in Taranaki
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape
published: 18 Jun 2013 -
Mountain building: Uplift, erosion and exhumation
published: 06 Jun 2015 -
-
Tectonic uplift Meaning
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic uplift. Powered by MaryTTS, Wiktionary
published: 30 Apr 2015 -
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between x=-50 and +50 km) and a 1D stream power law erosion model. River erosion is proportional to slope and water discharge (constant precipitation rate over the entire profile). The dashed line marks the topography that would form in absence of erosion. Note the steady states reached before 5 Myr (about 3 km max. topography) and at ~8 Myr (flat topography). Note also that at equilibrium, the model correctly predicts uplift rate=erosion rate at every location, and that in the end, total erosion = total uplift Calculated under Linux with the program tAo by Garcia-Castellanos (2007, EPSL). There is an explanation here: http://retosterri...
published: 15 Feb 2012 -
tectonic uplift final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
published: 24 Aug 2016 -
Wax Geology Uplift
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created and subjected to powerful compression forces which results in uplift of parts of the wax structure.
published: 21 Nov 2015 -
Signs of Himalayan uplift and tectonic plates in Ladakh
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main Great Himalayas to the south, inhabited by people of Indo-Aryan and Tibetan descent. It is one of the most sparsely populated regions in Jammu and Kashmir. The largest town in Ladakh is Leh. It is one of the few remaining abodes of Buddhism in South Asia, including the Chittagong Hill Tracts, Bhutan and Sri Lanka; a majority of Ladakhis are Tibetan Buddhists and the rest are mostly Shia Muslims. (Source Wikipedia) This footage is part of the professionally-shot broadcast stock footage archive of Wilderness Films India Ltd., the largest collection of imagery from South Asia. The Wilderness Films India collection comprises of thous...
published: 13 Feb 2013
Plate Tectonics and Uplift
- Order: Reorder
- Duration: 6:08
- Updated: 18 Mar 2015
- views: 545
- published: 18 Mar 2015
- views: 545
Tectonic uplift - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:02
- Updated: 29 Sep 2015
- views: 748
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas ...
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening , changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere.
It is also good to take into consideration the effects of denudation . Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region of denudation . The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies.
Crustal thickening has an upward component of motion and often occurs when continental crust is thrust onto continental crust. Basically nappes from each plate collide and begin to stack one on top of the other; evidence of this process can be seen in preserved ophiolitic nappes , and in rocks with an inverted metamorphic gradient. The preserved inverted metamorphic gradient indicates that nappes were actually stacked on top of each other so quickly, that hot rocks did not have time to equilibrate before being thrust on top of cool rocks. The process of nappe stacking can only continue for so long, as gravity will eventually disallow further vertical growth .
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Tectonic+uplift, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
wn.com/Tectonic Uplift Video Learning Wizscience.Com
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface that is not attributable to an isostatic response to unloading. Whereas isostatic response is important, an increase in the mean elevation of a region can only occur in response to tectonic processes of crustal thickening , changes in the density distribution of the crust and underlying mantle, and flexural support due to the bending of rigid lithosphere.
It is also good to take into consideration the effects of denudation . Within the scope of this topic, uplift relates to denudation in that denudation brings buried rocks closer to the surface. This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting isostatic response in the region of denudation . The timing, magnitude, and rate of denudation can be estimated using pressure-temperature studies.
Crustal thickening has an upward component of motion and often occurs when continental crust is thrust onto continental crust. Basically nappes from each plate collide and begin to stack one on top of the other; evidence of this process can be seen in preserved ophiolitic nappes , and in rocks with an inverted metamorphic gradient. The preserved inverted metamorphic gradient indicates that nappes were actually stacked on top of each other so quickly, that hot rocks did not have time to equilibrate before being thrust on top of cool rocks. The process of nappe stacking can only continue for so long, as gravity will eventually disallow further vertical growth .
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Tectonic+uplift, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
- published: 29 Sep 2015
- views: 748
Fossils and tectonic uplift in Taranaki
- Order: Reorder
- Duration: 6:20
- Updated: 18 Jun 2013
- views: 2277
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape
wn.com/Fossils And Tectonic Uplift In Taranaki
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape
- published: 18 Jun 2013
- views: 2277
Mountain building: Uplift, erosion and exhumation
- Order: Reorder
- Duration: 2:57
- Updated: 06 Jun 2015
- views: 7235
- published: 06 Jun 2015
- views: 7235
Tectonic-uplift Meaning
- Order: Reorder
- Duration: 0:26
- Updated: 30 Apr 2015
- views: 46
Video shows what tectonic-uplift means. , noun.. Tectonic-uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic-uplift. Powered by...
Video shows what tectonic-uplift means. , noun.. Tectonic-uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic-uplift. Powered by MaryTTS, Wiktionary
wn.com/Tectonic Uplift Meaning
Tectonic uplift Meaning
- Order: Reorder
- Duration: 0:30
- Updated: 30 Apr 2015
- views: 235
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, def...
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic uplift. Powered by MaryTTS, Wiktionary
wn.com/Tectonic Uplift Meaning
Video shows what tectonic uplift means. The raising of a geographical area as a consequence of plate tectonics.. Tectonic uplift Meaning. How to pronounce, definition audio dictionary. How to say tectonic uplift. Powered by MaryTTS, Wiktionary
- published: 30 Apr 2015
- views: 235
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
- Order: Reorder
- Duration: 0:41
- Updated: 15 Feb 2012
- views: 1153
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between...
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between x=-50 and +50 km) and a 1D stream power law erosion model. River erosion is proportional to slope and water discharge (constant precipitation rate over the entire profile). The dashed line marks the topography that would form in absence of erosion.
Note the steady states reached before 5 Myr (about 3 km max. topography) and at ~8 Myr (flat topography). Note also that at equilibrium, the model correctly predicts uplift rate=erosion rate at every location, and that in the end, total erosion = total uplift
Calculated under Linux with the program tAo by Garcia-Castellanos (2007, EPSL).
There is an explanation here:
http://retosterricolas.blogspot.com/2012/02/steady-state-topography-during.html
+info on the software:
https://sites.google.com/site/daniggcc/software/tao
wn.com/Steady State Topography Tectonic Uplift River Erosion Leading To Equilibrium, 1D Model
Steady state topography development along a vertical cross section. Calculated assuming constant uplift rate at the center (1 mm/yr stopping at t=5 Myr, between x=-50 and +50 km) and a 1D stream power law erosion model. River erosion is proportional to slope and water discharge (constant precipitation rate over the entire profile). The dashed line marks the topography that would form in absence of erosion.
Note the steady states reached before 5 Myr (about 3 km max. topography) and at ~8 Myr (flat topography). Note also that at equilibrium, the model correctly predicts uplift rate=erosion rate at every location, and that in the end, total erosion = total uplift
Calculated under Linux with the program tAo by Garcia-Castellanos (2007, EPSL).
There is an explanation here:
http://retosterricolas.blogspot.com/2012/02/steady-state-topography-during.html
+info on the software:
https://sites.google.com/site/daniggcc/software/tao
- published: 15 Feb 2012
- views: 1153
tectonic uplift final
- Order: Reorder
- Duration: 0:55
- Updated: 24 Aug 2016
- views: 10
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free to...
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
wn.com/Tectonic Uplift Final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
- published: 24 Aug 2016
- views: 10
Wax Geology Uplift
- Order: Reorder
- Duration: 2:41
- Updated: 21 Nov 2015
- views: 128
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created a...
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created and subjected to powerful compression forces which results in uplift of parts of the wax structure.
wn.com/Wax Geology Uplift
How to demonstrate the way geologic forces create conditions where uplift or mountain building takes place. In this instance a wax model of strata is created and subjected to powerful compression forces which results in uplift of parts of the wax structure.
- published: 21 Nov 2015
- views: 128
Signs of Himalayan uplift and tectonic plates in Ladakh
- Order: Reorder
- Duration: 1:10
- Updated: 13 Feb 2013
- views: 724
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main ...
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main Great Himalayas to the south, inhabited by people of Indo-Aryan and Tibetan descent. It is one of the most
sparsely populated regions in Jammu and Kashmir.
The largest town in Ladakh is Leh. It is one of the few remaining abodes of Buddhism in South Asia, including the Chittagong Hill Tracts, Bhutan and Sri Lanka; a majority of Ladakhis are Tibetan Buddhists and the rest are mostly Shia Muslims.
(Source Wikipedia)
This footage is part of the professionally-shot broadcast stock footage archive of Wilderness Films India Ltd., the largest collection of imagery from South Asia. The Wilderness Films India collection comprises of thousands of hours of high quality broadcast imagery, mostly shot on HDCAM 1080i High Definition, HDV and XDCAM. Write to us for licensing this footage on a broadcast format, for use in your production! We are happy to be commissioned to film for you or else provide you with broadcast crewing and production solutions across South Asia. We pride ourselves in bringing the best of India and South Asia to the world... Reach us at wfi @ vsnl.com and admin@wildfilmsindia.com.
wn.com/Signs Of Himalayan Uplift And Tectonic Plates In Ladakh
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India. It lies between the Kunlun mountain range in the north and the main Great Himalayas to the south, inhabited by people of Indo-Aryan and Tibetan descent. It is one of the most
sparsely populated regions in Jammu and Kashmir.
The largest town in Ladakh is Leh. It is one of the few remaining abodes of Buddhism in South Asia, including the Chittagong Hill Tracts, Bhutan and Sri Lanka; a majority of Ladakhis are Tibetan Buddhists and the rest are mostly Shia Muslims.
(Source Wikipedia)
This footage is part of the professionally-shot broadcast stock footage archive of Wilderness Films India Ltd., the largest collection of imagery from South Asia. The Wilderness Films India collection comprises of thousands of hours of high quality broadcast imagery, mostly shot on HDCAM 1080i High Definition, HDV and XDCAM. Write to us for licensing this footage on a broadcast format, for use in your production! We are happy to be commissioned to film for you or else provide you with broadcast crewing and production solutions across South Asia. We pride ourselves in bringing the best of India and South Asia to the world... Reach us at wfi @ vsnl.com and admin@wildfilmsindia.com.
- published: 13 Feb 2013
- views: 724
-
Llano Uplift, Central Texas
Llano Uplift: Kingsland, Tx https://en.wikipedia.org/wiki/Greensand https://en.wikipedia.org/wiki/Llano_Uplift Lake Lyndon B. Johnson https://en.wikipedia.org/wiki/Lake_Lyndon_B._Johnson Don't Mess With Texas, Litter Facts http://www.dontmesswithtexas.org/about/litter-facts/ Please follow me on Twitter https://twitter.com/CaptLateNight Medium Rock by Audionautix is licensed under a Creative Commons Attribution license (https://creativecommons.org/licenses/by/4.0/) Artist: http://audionautix.com/
published: 21 Oct 2016 -
BPW up to the uplift
published: 09 Oct 2016 -
tectonic uplift final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
published: 24 Aug 2016 -
Modelled uplift history of the Eastern Australian Highlands through time
Modelled topography of the eastern Australian highlands since 150 million years ago. The model is based on a coupled plate tectonic-mantle convection model run on the Australian high performance computer Raijin (http://nci.org.au/systems-services/national-facility/peak-system/raijin/). The model shows that the time-dependent interaction of plate motion with mantle downwellings and upwellings accounts for the broad pattern of margin uplift phases. Initial dynamic uplift of 400-600 m from 120-80 Ma was driven by the eastward motion of eastern Australia’s margin away from the sinking eastern Gondwana slab, followed by tectonic quiescence to about 60 Ma in the south (Snowy Mountains). Renewed uplift of ~700 m in the Snowy Mountains is propelled by the gradual motion of the margin over the e...
published: 16 Mar 2016 -
-
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"Nuevos Aires" Uplifted by CUrITa Sheffield
Our first mixed dance style genre event. Thank you Las Iguanas in the West One Plaza, Sheffield, for hosting us. 11th of October 2015.
published: 14 Oct 2015 -
Erosion and tectonics - Video Learning - WizScience.com
The interaction between "erosion and tectonics" has been a topic of debate since the early 1990s. While the tectonic effects on surface processes such as erosion have long been recognized , the opposite has only recently been addressed. The primary questions surrounding this topic are what types of interactions exist between erosion and tectonics and what are the implications of these interactions. While this is still a matter of debate, one thing is clear, the Earth's landscape is a product of two factors: tectonics, which can create topography and maintain relief through surface and rock uplift, and climate, which mediates the erosional processes that wear away upland areas over time. The interaction of these processes can form, modify, or destroy geomorphic features on the Earth’s su...
published: 02 Sep 2015
Llano Uplift, Central Texas
- Order: Reorder
- Duration: 3:28
- Updated: 21 Oct 2016
- views: 30
Llano Uplift: Kingsland, Tx
https://en.wikipedia.org/wiki/Greensand
https://en.wikipedia.org/wiki/Llano_Uplift
Lake Lyndon B. Johnson
https://en.wikipedia.org/w...
Llano Uplift: Kingsland, Tx
https://en.wikipedia.org/wiki/Greensand
https://en.wikipedia.org/wiki/Llano_Uplift
Lake Lyndon B. Johnson
https://en.wikipedia.org/wiki/Lake_Lyndon_B._Johnson
Don't Mess With Texas, Litter Facts
http://www.dontmesswithtexas.org/about/litter-facts/
Please follow me on Twitter
https://twitter.com/CaptLateNight
Medium Rock by Audionautix is licensed under a Creative Commons Attribution license (https://creativecommons.org/licenses/by/4.0/)
Artist: http://audionautix.com/
wn.com/Llano Uplift, Central Texas
Llano Uplift: Kingsland, Tx
https://en.wikipedia.org/wiki/Greensand
https://en.wikipedia.org/wiki/Llano_Uplift
Lake Lyndon B. Johnson
https://en.wikipedia.org/wiki/Lake_Lyndon_B._Johnson
Don't Mess With Texas, Litter Facts
http://www.dontmesswithtexas.org/about/litter-facts/
Please follow me on Twitter
https://twitter.com/CaptLateNight
Medium Rock by Audionautix is licensed under a Creative Commons Attribution license (https://creativecommons.org/licenses/by/4.0/)
Artist: http://audionautix.com/
- published: 21 Oct 2016
- views: 30
BPW up to the uplift
- Order: Reorder
- Duration: 2:04
- Updated: 09 Oct 2016
- views: 15
- published: 09 Oct 2016
- views: 15
tectonic uplift final
- Order: Reorder
- Duration: 0:55
- Updated: 24 Aug 2016
- views: 1
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free to...
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
wn.com/Tectonic Uplift Final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create animated videos and animated presentations for free. PowToon is a free tool that allows you to develop cool animated clips and animated presentations for your website, office meeting, sales pitch, nonprofit fundraiser, product launch, video resume, or anything else you could use an animated explainer video. PowToon's animation templates help you create animated presentations and animated explainer videos from scratch. Anyone can produce awesome animations quickly with PowToon, without the cost or hassle other professional animation services require.
- published: 24 Aug 2016
- views: 1
Modelled uplift history of the Eastern Australian Highlands through time
- Order: Reorder
- Duration: 0:21
- Updated: 16 Mar 2016
- views: 253
Modelled topography of the eastern Australian highlands since 150 million years ago. The model is based on a coupled plate tectonic-mantle convection model ru...
Modelled topography of the eastern Australian highlands since 150 million years ago. The model is based on a coupled plate tectonic-mantle convection model run on the Australian high performance computer Raijin (http://nci.org.au/systems-services/national-facility/peak-system/raijin/). The model shows that the time-dependent interaction of plate motion with mantle downwellings and upwellings accounts for the broad pattern of margin uplift phases. Initial dynamic uplift of 400-600 m from 120-80 Ma was driven by the eastward motion of eastern Australia’s margin away from the sinking eastern Gondwana slab, followed by tectonic quiescence to about 60 Ma in the south (Snowy Mountains). Renewed uplift of ~700 m in the Snowy Mountains is propelled by the gradual motion of the margin over the edge of the large Pacific mantle upwelling. In contrast the northernmost portion of the highlands records continuous uplift from 120 Ma to present-day totalling about 800 m. The northern highlands experienced a continuous history of dynamic uplift, first due to the end of subduction to the east of Australia, then due to moving over a large passive mantle upwelling. In contrast, the southern highlands started interacting with the edge of the large Pacific mantle upwelling ~40-50 million years later, resulting in a two-phase uplift history. Our results are in agreement with published uplift models derived from river profiles and the Cretaceous sediment influx into the Ceduna sub-basin offshore southeast Australia, reflecting the fundamental link between dynamic uplift, fluvial erosion and depositional pulses in basins distal to passive margin highlands. Video Credit: Tristan Salles. Citation: Müller, R.D., Flament, N., Matthews, K.J., Williams, S.E., Gurnis, M., Formation of Australian continental margin highlands driven by plate–mantle interaction, Earth and Planetary Science Letters, 441, 60-70.
wn.com/Modelled Uplift History Of The Eastern Australian Highlands Through Time
Modelled topography of the eastern Australian highlands since 150 million years ago. The model is based on a coupled plate tectonic-mantle convection model run on the Australian high performance computer Raijin (http://nci.org.au/systems-services/national-facility/peak-system/raijin/). The model shows that the time-dependent interaction of plate motion with mantle downwellings and upwellings accounts for the broad pattern of margin uplift phases. Initial dynamic uplift of 400-600 m from 120-80 Ma was driven by the eastward motion of eastern Australia’s margin away from the sinking eastern Gondwana slab, followed by tectonic quiescence to about 60 Ma in the south (Snowy Mountains). Renewed uplift of ~700 m in the Snowy Mountains is propelled by the gradual motion of the margin over the edge of the large Pacific mantle upwelling. In contrast the northernmost portion of the highlands records continuous uplift from 120 Ma to present-day totalling about 800 m. The northern highlands experienced a continuous history of dynamic uplift, first due to the end of subduction to the east of Australia, then due to moving over a large passive mantle upwelling. In contrast, the southern highlands started interacting with the edge of the large Pacific mantle upwelling ~40-50 million years later, resulting in a two-phase uplift history. Our results are in agreement with published uplift models derived from river profiles and the Cretaceous sediment influx into the Ceduna sub-basin offshore southeast Australia, reflecting the fundamental link between dynamic uplift, fluvial erosion and depositional pulses in basins distal to passive margin highlands. Video Credit: Tristan Salles. Citation: Müller, R.D., Flament, N., Matthews, K.J., Williams, S.E., Gurnis, M., Formation of Australian continental margin highlands driven by plate–mantle interaction, Earth and Planetary Science Letters, 441, 60-70.
- published: 16 Mar 2016
- views: 253
Llano Uplift
- Order: Reorder
- Duration: 4:30
- Updated: 12 Dec 2015
- views: 98
This video is about Llano Uplift
This video is about Llano Uplift
wn.com/Llano Uplift
Tectonic Uplift and Climate Change Pdf
- Order: Reorder
- Duration: 0:26
- Updated: 25 Nov 2015
- views: 5
http://realbooknow.net/books
http://realbooknow.net/books
wn.com/Tectonic Uplift And Climate Change Pdf
"Nuevos Aires" Uplifted by CUrITa Sheffield
- Order: Reorder
- Duration: 0:41
- Updated: 14 Oct 2015
- views: 23
Our first mixed dance style genre event.
Thank you Las Iguanas in the West One Plaza, Sheffield, for hosting us.
11th of October 2015.
Our first mixed dance style genre event.
Thank you Las Iguanas in the West One Plaza, Sheffield, for hosting us.
11th of October 2015.
wn.com/Nuevos Aires Uplifted By Curita Sheffield
Our first mixed dance style genre event.
Thank you Las Iguanas in the West One Plaza, Sheffield, for hosting us.
11th of October 2015.
- published: 14 Oct 2015
- views: 23
Erosion and tectonics - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:37
- Updated: 02 Sep 2015
- views: 197
The interaction between "erosion and tectonics" has been a topic of debate since the early 1990s. While the tectonic effects on surface processes such as erosio...
The interaction between "erosion and tectonics" has been a topic of debate since the early 1990s. While the tectonic effects on surface processes such as erosion have long been recognized , the opposite has only recently been addressed. The primary questions surrounding this topic are what types of interactions exist between erosion and tectonics and what are the implications of these interactions. While this is still a matter of debate, one thing is clear, the Earth's landscape is a product of two factors: tectonics, which can create topography and maintain relief through surface and rock uplift, and climate, which mediates the erosional processes that wear away upland areas over time. The interaction of these processes can form, modify, or destroy geomorphic features on the Earth’s surface.
The term tectonics refers to the study of the Earth's surface structure and the ways in which it changes over time. Tectonic processes typically occur at plate boundaries which are one of three types: convergent boundaries, divergent boundaries, or transform boundaries. These processes form and modify the topography of the Earth's surface, effectively increasing relief through the mechanisms of isostatic uplift, crustal thickening, and deformation in the form of faulting and folding. Increased elevations, in relation to regional base levels, lead to steeper river channel gradients and an increase in orographically localized precipitation, ultimately resulting in drastically increased erosion rates. The topography, and general relief, of a given area determines the velocity at which surface runoff will flow, ultimately determining the potential erosive power of the runoff. Longer, steeper slopes are more prone to higher rates of erosion during periods of heavy rainfall than shorter, gradually sloping areas. Thus, large mountain ranges, and other areas of high relief, formed through tectonic uplift will have significantly higher rates of erosion. Additionally, tectonics can directly influence erosion rates on a short timescale, as is clear in the case of earthquakes, which can trigger landslides and weaken surrounding rock through seismic disturbances.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Erosion+and+tectonics, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
wn.com/Erosion And Tectonics Video Learning Wizscience.Com
The interaction between "erosion and tectonics" has been a topic of debate since the early 1990s. While the tectonic effects on surface processes such as erosion have long been recognized , the opposite has only recently been addressed. The primary questions surrounding this topic are what types of interactions exist between erosion and tectonics and what are the implications of these interactions. While this is still a matter of debate, one thing is clear, the Earth's landscape is a product of two factors: tectonics, which can create topography and maintain relief through surface and rock uplift, and climate, which mediates the erosional processes that wear away upland areas over time. The interaction of these processes can form, modify, or destroy geomorphic features on the Earth’s surface.
The term tectonics refers to the study of the Earth's surface structure and the ways in which it changes over time. Tectonic processes typically occur at plate boundaries which are one of three types: convergent boundaries, divergent boundaries, or transform boundaries. These processes form and modify the topography of the Earth's surface, effectively increasing relief through the mechanisms of isostatic uplift, crustal thickening, and deformation in the form of faulting and folding. Increased elevations, in relation to regional base levels, lead to steeper river channel gradients and an increase in orographically localized precipitation, ultimately resulting in drastically increased erosion rates. The topography, and general relief, of a given area determines the velocity at which surface runoff will flow, ultimately determining the potential erosive power of the runoff. Longer, steeper slopes are more prone to higher rates of erosion during periods of heavy rainfall than shorter, gradually sloping areas. Thus, large mountain ranges, and other areas of high relief, formed through tectonic uplift will have significantly higher rates of erosion. Additionally, tectonics can directly influence erosion rates on a short timescale, as is clear in the case of earthquakes, which can trigger landslides and weaken surrounding rock through seismic disturbances.
Wiz Science™ is "the" learning channel for children and all ages.
SUBSCRIBE TODAY
Disclaimer: This video is for your information only. The author or publisher does not guarantee the accuracy of the content presented in this video. USE AT YOUR OWN RISK.
Background Music:
"The Place Inside" by Silent Partner (royalty-free) from YouTube Audio Library.
This video uses material/images from https://en.wikipedia.org/wiki/Erosion+and+tectonics, which is released under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . This video is licensed under Creative Commons Attribution-Share-Alike License 3.0 http://creativecommons.org/licenses/by-sa/3.0/ . To reuse/adapt the content in your own work, you must comply with the license terms.
- published: 02 Sep 2015
- views: 197
-
What Every Adventist Scientist Should Know: Rates of Erosion and Uplift 3-29-2014 by Ariel Roth
We continue a series on What Every Adventist Scientist Should Know. This fifth week we review the data on rates of erosion of continents and uplift of mountains. 1. Scores of references from the geological literature will be found in Chapter 15: Some Geologic Questions About Geologic Time, in: Roth AA. 1998. ORIGINS: Linking Science and Scripture. Review and Herald Publishing. 2. For a broad discussion of the time issue see Chapter 5: So Little Time for Everything, in Roth AA. 2007. Science Discovers God. Autumn House, Review and Herald. 3. For a discussion designed for students see: DISCUSSION 9: The Great Time Questions, Part 3, Data Favoring a Recent Creation, on the author's webpage: SciencesAndScriptures.com For additional recordings on various topics regarding faith and science vi...
published: 30 Mar 2014 -
Peter Van der Beek (UJF, Grenoble) - Barcelona 2014 Topo-Europe - Tectonics, Himalayan topography
10th Topo-Europe workshop Interplay between surface, lithospheric, and mantle processes Barcelona, September 17-19, 2014 More info and material here: https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014 http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom Meeting Organizers: Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius Host institution: ICTJA-CSIC, Barcelona, Spain Venue: CosmoCaixa PROGRAM: Wednesday 17th Opening: 09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea). 09:30 Karin Sigloch (Oxford, UK) Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times. 10:00 Hitoshi Kawakatsu (ERI, Tokyo U.) Seismic i...
published: 16 Oct 2014 -
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-Europe - tectonic-erosion in the Himalayas
10th Topo-Europe workshop Interplay between surface, lithospheric, and mantle processes Barcelona, September 17-19, 2014 More info and material here: https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014 http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom Meeting Organizers: Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius Host institution: ICTJA-CSIC, Barcelona, Spain Venue: CosmoCaixa PROGRAM: Wednesday 17th Opening: 09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea). 09:30 Karin Sigloch (Oxford, UK) Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times. 10:00 Hitoshi Kawakatsu (ERI, Tokyo U.) Seismic i...
published: 16 Oct 2014 -
New Zealand : Great Walks
New Zealand : Great Walks New Zealand is an island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volc...
published: 21 Jan 2016 -
Geoff Batt - Ironing out the Kinks: Oligo-Miocene self-organisation of the
Dynamic geochronological constraint derived from fault-bounded slivers of high grade crystalline rocks in the footwall to New Zealand’s Alpine Fault system captures the early evolution of this plate-bounding structure during the late Oligocene and early Miocene. This record reveals a telling insight into the way structurally complex crustal fabrics respond to major change in tectonic forcing. Initial development of a transform plate boundary through the central South Island of New Zealand saw deformation dispersed across a broad domain of inherited fault systems and complex crustal architecture. Local transpressional kinematics imposed on non-optimally aligned structures during this period produced isolated domains of rapid uplift and corresponding orogenic-scale topography. Sequential aba...
published: 04 Nov 2015 -
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Topo-Europe - Tectonics & Mesopotamian foreland basin
10th Topo-Europe workshop Interplay between surface, lithospheric, and mantle processes Barcelona, September 17-19, 2014 More info and material here: https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014 http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom Meeting Organizers: Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius Host institution: ICTJA-CSIC, Barcelona, Spain Venue: CosmoCaixa PROGRAM: Wednesday 17th Opening: 09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea). 09:30 Karin Sigloch (Oxford, UK) Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times. 10:00 Hitoshi Kawakatsu (ERI, Tokyo U.) Seismic i...
published: 16 Oct 2014 -
This is New Zealand
The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington, while its most populous city...
published: 07 Aug 2016 -
NewZealand Wellington - سفر به نیوزیلند ولینگتون - (Day 4)
#Wellington (/ˈwɛlɪŋtən/) (Māori: Te Whanga-nui-a-Tara) is the #capital city and second most populous urban area of #New #Zealand, with 398,300 residents. It is located at the #south-#western tip of the #North #Island, between #Cook #Strait and the #Rimutaka #Range. #Wellington is the major population centre of the southern North Island and is the administrative centre of the Wellington Region, which also includes the #Kapiti #Coast and #Wairarapa. As the nation's centre of #government, the New Zealand #Parliament, #Supreme #Court and most of the civil service are all based in the city. The #Beehive is the common name for the #Executive #Wing of the New Zealand Parliament #Buildings, located at the corner of #Molesworth Street and #Lambton Quay, Wellington. It is so-called because of its ...
published: 04 Oct 2016 -
07 Laurent Jolivet - Barcelona 2014 Topo-Europe
10th Topo-Europe workshop Interplay between surface, lithospheric, and mantle processes Barcelona, September 17-19, 2014 More info and material here: https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014 http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom Meeting Organizers: Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius Host institution: ICTJA-CSIC, Barcelona, Spain Venue: CosmoCaixa PROGRAM: Wednesday 17th Opening: 09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea). 09:30 Karin Sigloch (Oxford, UK) Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times. 10:00 Hitoshi Kawakatsu (ERI, Tokyo U.) Seismic i...
published: 16 Oct 2014 -
06 Barbara Carrapa - Barcelona 2014 Topo-Europe
10th Topo-Europe workshop Interplay between surface, lithospheric, and mantle processes Barcelona, September 17-19, 2014 More info and material here: https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014 http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom Meeting Organizers: Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius Host institution: ICTJA-CSIC, Barcelona, Spain Venue: CosmoCaixa PROGRAM: Wednesday 17th Opening: 09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea). 09:30 Karin Sigloch (Oxford, UK) Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times. 10:00 Hitoshi Kawakatsu (ERI, Tokyo U.) Seismic i...
published: 16 Oct 2014
What Every Adventist Scientist Should Know: Rates of Erosion and Uplift 3-29-2014 by Ariel Roth
- Order: Reorder
- Duration: 67:17
- Updated: 30 Mar 2014
- views: 300
We continue a series on What Every Adventist Scientist Should Know. This fifth week we review the data on rates of erosion of continents and uplift of mountain...
We continue a series on What Every Adventist Scientist Should Know. This fifth week we review the data on rates of erosion of continents and uplift of mountains.
1. Scores of references from the geological literature will be found in Chapter 15: Some Geologic Questions About Geologic Time, in: Roth AA. 1998. ORIGINS: Linking Science and Scripture. Review and Herald Publishing.
2. For a broad discussion of the time issue see Chapter 5: So Little Time for Everything, in Roth AA. 2007. Science Discovers God. Autumn House, Review and Herald.
3. For a discussion designed for students see: DISCUSSION 9: The Great Time Questions, Part 3, Data Favoring a Recent Creation, on the author's webpage: SciencesAndScriptures.com
For additional recordings on various topics regarding faith and science visit: ItsAboutGod.tv/sls
wn.com/What Every Adventist Scientist Should Know Rates Of Erosion And Uplift 3 29 2014 By Ariel Roth
We continue a series on What Every Adventist Scientist Should Know. This fifth week we review the data on rates of erosion of continents and uplift of mountains.
1. Scores of references from the geological literature will be found in Chapter 15: Some Geologic Questions About Geologic Time, in: Roth AA. 1998. ORIGINS: Linking Science and Scripture. Review and Herald Publishing.
2. For a broad discussion of the time issue see Chapter 5: So Little Time for Everything, in Roth AA. 2007. Science Discovers God. Autumn House, Review and Herald.
3. For a discussion designed for students see: DISCUSSION 9: The Great Time Questions, Part 3, Data Favoring a Recent Creation, on the author's webpage: SciencesAndScriptures.com
For additional recordings on various topics regarding faith and science visit: ItsAboutGod.tv/sls
- published: 30 Mar 2014
- views: 300
Peter Van der Beek (UJF, Grenoble) - Barcelona 2014 Topo-Europe - Tectonics, Himalayan topography
- Order: Reorder
- Duration: 31:26
- Updated: 16 Oct 2014
- views: 581
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https:...
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
wn.com/Peter Van Der Beek (Ujf, Grenoble) Barcelona 2014 Topo Europe Tectonics, Himalayan Topography
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
- published: 16 Oct 2014
- views: 581
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-Europe - tectonic-erosion in the Himalayas
- Order: Reorder
- Duration: 33:56
- Updated: 16 Oct 2014
- views: 242
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https:...
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
wn.com/Yani Najman (Lancaster U.) Barcelona 2014 Topo Europe Tectonic Erosion In The Himalayas
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
- published: 16 Oct 2014
- views: 242
New Zealand : Great Walks
- Order: Reorder
- Duration: 22:22
- Updated: 21 Jan 2016
- views: 568
New Zealand : Great Walks
New Zealand is an island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses – that ...
New Zealand : Great Walks
New Zealand is an island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington, while its most populous city is Auckland.
Polynesians settled in the islands that were to become New Zealand somewhere between 1250 and 1300 CE, and developed a distinctive Māori culture. In 1642, Abel Tasman, a Dutch explorer, became the first European to sight New Zealand. In 1840, representatives of the British Crown and Māori Chiefs signed the Treaty of Waitangi, making New Zealand a British colony. Today, the majority of New Zealand's population of 4.5 million is of European descent; the indigenous Māori are the largest minority, followed by Asians and Pacific Islanders. Reflecting this, New Zealand's culture is mainly derived from Māori and early British settlers, with recent broadening arising from increased immigration. The official languages are English, Māori and New Zealand Sign Language, with English predominant.
Read more: https://en.wikipedia.org/wiki/New_Zealand
May you find this video informative and be thrilled to subscribe for more. Thanks for watching!
wn.com/New Zealand Great Walks
New Zealand : Great Walks
New Zealand is an island country in the southwestern Pacific Ocean. The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington, while its most populous city is Auckland.
Polynesians settled in the islands that were to become New Zealand somewhere between 1250 and 1300 CE, and developed a distinctive Māori culture. In 1642, Abel Tasman, a Dutch explorer, became the first European to sight New Zealand. In 1840, representatives of the British Crown and Māori Chiefs signed the Treaty of Waitangi, making New Zealand a British colony. Today, the majority of New Zealand's population of 4.5 million is of European descent; the indigenous Māori are the largest minority, followed by Asians and Pacific Islanders. Reflecting this, New Zealand's culture is mainly derived from Māori and early British settlers, with recent broadening arising from increased immigration. The official languages are English, Māori and New Zealand Sign Language, with English predominant.
Read more: https://en.wikipedia.org/wiki/New_Zealand
May you find this video informative and be thrilled to subscribe for more. Thanks for watching!
- published: 21 Jan 2016
- views: 568
Geoff Batt - Ironing out the Kinks: Oligo-Miocene self-organisation of the
- Order: Reorder
- Duration: 49:27
- Updated: 04 Nov 2015
- views: 35
Dynamic geochronological constraint derived from fault-bounded slivers of high grade crystalline rocks in the footwall
to New Zealand’s Alpine Fault system capt...
Dynamic geochronological constraint derived from fault-bounded slivers of high grade crystalline rocks in the footwall
to New Zealand’s Alpine Fault system captures the early evolution of this plate-bounding structure during the late
Oligocene and early Miocene. This record reveals a telling insight into the way structurally complex crustal fabrics
respond to major change in tectonic forcing.
Initial development of a transform plate boundary through the central South Island of New Zealand saw deformation
dispersed across a broad domain of inherited fault systems and complex crustal architecture. Local transpressional
kinematics imposed on non-optimally aligned structures during this period produced isolated domains of rapid uplift
and corresponding orogenic-scale topography.
Sequential abandonment of these local uplift centres over a c. 3 M.yr. interval marks the progressive evolution of a
more optimally oriented and coherent plate bounding structure.
The switch to oblique-reverse kinematics across the Alpine Fault at 8 Ma and subsequent development of the Southern
Alpine (Kaikoura) Orogeny has consumed or overprinted much of the geological and structural record of this key period
– with remaining insight restricted to these isolated structural windows.
This style of widely dispersed but short-lived activity on inherited structures may provide a model for the temporal
clustering of structurally controlled mineral systems.
wn.com/Geoff Batt Ironing Out The Kinks Oligo Miocene Self Organisation Of The
Dynamic geochronological constraint derived from fault-bounded slivers of high grade crystalline rocks in the footwall
to New Zealand’s Alpine Fault system captures the early evolution of this plate-bounding structure during the late
Oligocene and early Miocene. This record reveals a telling insight into the way structurally complex crustal fabrics
respond to major change in tectonic forcing.
Initial development of a transform plate boundary through the central South Island of New Zealand saw deformation
dispersed across a broad domain of inherited fault systems and complex crustal architecture. Local transpressional
kinematics imposed on non-optimally aligned structures during this period produced isolated domains of rapid uplift
and corresponding orogenic-scale topography.
Sequential abandonment of these local uplift centres over a c. 3 M.yr. interval marks the progressive evolution of a
more optimally oriented and coherent plate bounding structure.
The switch to oblique-reverse kinematics across the Alpine Fault at 8 Ma and subsequent development of the Southern
Alpine (Kaikoura) Orogeny has consumed or overprinted much of the geological and structural record of this key period
– with remaining insight restricted to these isolated structural windows.
This style of widely dispersed but short-lived activity on inherited structures may provide a model for the temporal
clustering of structurally controlled mineral systems.
- published: 04 Nov 2015
- views: 35
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Topo-Europe - Tectonics & Mesopotamian foreland basin
- Order: Reorder
- Duration: 29:04
- Updated: 16 Oct 2014
- views: 369
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https:...
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
wn.com/Charlotte Fillon (Csic Ictja) Barcelona 2014 Topo Europe Tectonics Mesopotamian Foreland Basin
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
- published: 16 Oct 2014
- views: 369
This is New Zealand
- Order: Reorder
- Duration: 124:51
- Updated: 07 Aug 2016
- views: 15
The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous sma...
The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington, while its most populous city is Auckland.
Sometime between 1250 and 1300 CE, Polynesians settled in the islands that would later become New Zealand, and developed a distinctive Māori culture. In 1642, Abel Tasman, a Dutch explorer, became the first European to sight New Zealand.[11] In 1840, representatives of the British Crown and Māori Chiefs signed the Treaty of Waitangi, making New Zealand a British colony. Today, the majority of New Zealand's population of 4.7 million is of European descent; the indigenous Māori are the largest minority, followed by Asians and Pacific Islanders. Reflecting this, New Zealand's culture is mainly derived from Māori and early British settlers, with recent broadening arising from increased immigration. The official languages are English, Māori and New Zealand Sign Language, with English predominant.
New Zealand is a developed country with a market economy. New Zealand is a World Bank high-income economy and ranks highly in international comparisons of national performance, such as health, education, economic freedom and quality of life. Nationally, legislative authority is vested in an elected, unicameral Parliament, while executive political power is exercised by the Cabinet, led by the Prime Minister, who is currently John Key. Queen Elizabeth II is the country's head of state and is represented by a Governor-General. In addition, New Zealand is organised into 11 regional councils and 67 territorial authorities for local government purposes. The Realm of New Zealand also includes Tokelau (a dependent territory); the Cook Islands and Niue (self-governing states in free association with New Zealand); and the Ross Dependency, which is New Zealand's territorial claim in Antarctica. New Zealand is a member of the United Nations, Commonwealth of Nations, ANZUS, Organisation for Economic Co-operation and Development, Pacific Islands Forum, and Asia-Pacific Economic Cooperation.
wn.com/This Is New Zealand
The country geographically comprises two main landmasses – that of the North Island, or Te Ika-a-Māui, and the South Island, or Te Waipounamu – and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of Australia across the Tasman Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New Caledonia, Fiji, and Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinctive biodiversity of animal, fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the Southern Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is Wellington, while its most populous city is Auckland.
Sometime between 1250 and 1300 CE, Polynesians settled in the islands that would later become New Zealand, and developed a distinctive Māori culture. In 1642, Abel Tasman, a Dutch explorer, became the first European to sight New Zealand.[11] In 1840, representatives of the British Crown and Māori Chiefs signed the Treaty of Waitangi, making New Zealand a British colony. Today, the majority of New Zealand's population of 4.7 million is of European descent; the indigenous Māori are the largest minority, followed by Asians and Pacific Islanders. Reflecting this, New Zealand's culture is mainly derived from Māori and early British settlers, with recent broadening arising from increased immigration. The official languages are English, Māori and New Zealand Sign Language, with English predominant.
New Zealand is a developed country with a market economy. New Zealand is a World Bank high-income economy and ranks highly in international comparisons of national performance, such as health, education, economic freedom and quality of life. Nationally, legislative authority is vested in an elected, unicameral Parliament, while executive political power is exercised by the Cabinet, led by the Prime Minister, who is currently John Key. Queen Elizabeth II is the country's head of state and is represented by a Governor-General. In addition, New Zealand is organised into 11 regional councils and 67 territorial authorities for local government purposes. The Realm of New Zealand also includes Tokelau (a dependent territory); the Cook Islands and Niue (self-governing states in free association with New Zealand); and the Ross Dependency, which is New Zealand's territorial claim in Antarctica. New Zealand is a member of the United Nations, Commonwealth of Nations, ANZUS, Organisation for Economic Co-operation and Development, Pacific Islands Forum, and Asia-Pacific Economic Cooperation.
- published: 07 Aug 2016
- views: 15
NewZealand Wellington - سفر به نیوزیلند ولینگتون - (Day 4)
- Order: Reorder
- Duration: 24:05
- Updated: 04 Oct 2016
- views: 25
#Wellington (/ˈwɛlɪŋtən/) (Māori: Te Whanga-nui-a-Tara) is the #capital city and second most populous urban area of #New #Zealand, with 398,300 residents. It is...
#Wellington (/ˈwɛlɪŋtən/) (Māori: Te Whanga-nui-a-Tara) is the #capital city and second most populous urban area of #New #Zealand, with 398,300 residents. It is located at the #south-#western tip of the #North #Island, between #Cook #Strait and the #Rimutaka #Range. #Wellington is the major population centre of the southern North Island and is the administrative centre of the Wellington Region, which also includes the #Kapiti #Coast and #Wairarapa. As the nation's centre of #government, the New Zealand #Parliament, #Supreme #Court and most of the civil service are all based in the city.
The #Beehive is the common name for the #Executive #Wing of the New Zealand Parliament #Buildings, located at the corner of #Molesworth Street and #Lambton Quay, Wellington. It is so-called because of its shape is #reminiscent of that of a traditional #woven form of beehive known as a "#skep". It is registered as a Category I heritage building by #Heritage New Zealand.
New Zealand Listeni/njuːˈziːlənd/ (Māori: Aotearoa [aɔˈtɛaɾɔa]) is an #island nation in the #southwestern #Pacific #Ocean. The country #geographically comprises two main landmasses—that of the North Island, or Te Ika-a-Māui, and the South Island, or Te #Waipounamu—and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of #Australia across the #Tasman #Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New #Caledonia, #Fiji, and #Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinctive biodiversity of #animal, #fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the #Southern #Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is #Wellington, while its most populous city is #Auckland.
wn.com/Newzealand Wellington سفر به نیوزیلند ولینگتون (Day 4)
#Wellington (/ˈwɛlɪŋtən/) (Māori: Te Whanga-nui-a-Tara) is the #capital city and second most populous urban area of #New #Zealand, with 398,300 residents. It is located at the #south-#western tip of the #North #Island, between #Cook #Strait and the #Rimutaka #Range. #Wellington is the major population centre of the southern North Island and is the administrative centre of the Wellington Region, which also includes the #Kapiti #Coast and #Wairarapa. As the nation's centre of #government, the New Zealand #Parliament, #Supreme #Court and most of the civil service are all based in the city.
The #Beehive is the common name for the #Executive #Wing of the New Zealand Parliament #Buildings, located at the corner of #Molesworth Street and #Lambton Quay, Wellington. It is so-called because of its shape is #reminiscent of that of a traditional #woven form of beehive known as a "#skep". It is registered as a Category I heritage building by #Heritage New Zealand.
New Zealand Listeni/njuːˈziːlənd/ (Māori: Aotearoa [aɔˈtɛaɾɔa]) is an #island nation in the #southwestern #Pacific #Ocean. The country #geographically comprises two main landmasses—that of the North Island, or Te Ika-a-Māui, and the South Island, or Te #Waipounamu—and numerous smaller islands. New Zealand is situated some 1,500 kilometres (900 mi) east of #Australia across the #Tasman #Sea and roughly 1,000 kilometres (600 mi) south of the Pacific island areas of New #Caledonia, #Fiji, and #Tonga. Because of its remoteness, it was one of the last lands to be settled by humans. During its long period of isolation, New Zealand developed a distinctive biodiversity of #animal, #fungal and plant life. The country's varied topography and its sharp mountain peaks, such as the #Southern #Alps, owe much to the tectonic uplift of land and volcanic eruptions. New Zealand's capital city is #Wellington, while its most populous city is #Auckland.
- published: 04 Oct 2016
- views: 25
07 Laurent Jolivet - Barcelona 2014 Topo-Europe
- Order: Reorder
- Duration: 31:09
- Updated: 16 Oct 2014
- views: 238
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https:...
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
wn.com/07 Laurent Jolivet Barcelona 2014 Topo Europe
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
- published: 16 Oct 2014
- views: 238
06 Barbara Carrapa - Barcelona 2014 Topo-Europe
- Order: Reorder
- Duration: 29:35
- Updated: 16 Oct 2014
- views: 295
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https:...
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
wn.com/06 Barbara Carrapa Barcelona 2014 Topo Europe
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
Barcelona, September 17-19, 2014
More info and material here:
https://sites.google.com/site/daniggcc/topo-europe-barcelona-2014
http://www.iplusdinnova.com/en/conference/topo-europe-2014-earth-top-down-bottom
Meeting Organizers:
Daniel Garcia-Castellanos, Claudio Faccenna, Sean Willett, Sierd Cloetingh, M. Fernàndez, N. Hovius
Host institution: ICTJA-CSIC, Barcelona, Spain
Venue: CosmoCaixa
PROGRAM:
Wednesday 17th
Opening:
09:10 Enric Banda (La Caixa Foundation), S. Cloetingh (Academia Europaea).
09:30 Karin Sigloch (Oxford, UK)
Continent-arc collisions: an overlooked factor in explaining North American topography during Jura-Cretaceous times.
10:00 Hitoshi Kawakatsu (ERI, Tokyo U.)
Seismic imaging of the Pacific slab beneath Japan and northeast China: deep water transportation and enigma of the off-arc volcanism.
11:30 Carolina Lithgow-Bertelloni (UCL, London)
Details matter: Lithospheric structure, slab morphology, thermodynamics and dynamic topography.
12:00 Thorsten Becker (U. Southern Cal., USA)
Apennines and Atlas: Making mountains in a mobile belt.
12:30 Cesar Ranero (CMIMA, Barcelona)
The Miocene formation and the Pliocene deformation of the Gibraltar Arc System.
14.30 Sergei Lebedev (Dublin)
Seismic Structure, Anisotropy and Dynamics of the Lithosphere and Asthenosphere.
15.00 Laurent Jolivet (UPMC, Paris)
Strain localization in the continental lithosphere, different scales and different approaches.
15.30 Manel Fernandez (ICTJA-CSIC, Barcelona)
Small-scale subduction in odd margins.
17:00 Lars Kaislaniemi
Dynamics of lithospheric thinning and mantle melting by edge-driven convection: Application to Moroccan Atlas mountains.
17:10 Hongliang Wang
Mechanical erosion of subcontinental lithosphere by plume induced flow.
17:20 Gianluca Frasca
Coeval thrusting and strike-slip faulting during Early Miocene collision in the Western Betics (Southern Spain).
17:30 Konstantinos Kydonakis
Mesozoic Tectonics of the Aegean.
17:40 Siddique A. Ehsan
Crustal and Upper Mantle Structural Constraints on the Topography of the southern Central Iberian Zone.
17:50 Jan Globig
African lithosphere geometry: Geoid and elevation constraints on Moho and LAB topography.
18:00 Tasca Santimano
Accretionary wedge evolution seen as a competition between minimum work and critical taper.
18:10 Elisa Calignano
Strain localization in continental compressional settings: insights from analogue models.
Thursday 18th
09.00 Susanne Buiter (Oslo)
How surface processes affect the syn-rift evolution of passive continental margins.
09.30 Taras Gerya (ETH, Zurich)
Two enigmas in lithospheric dynamics: initiation of subduction zones and ridge-transform spreading patterns.
10:00 Jorg Ebbing (Kiel U.)
Structure of the lithosphere from analysis of satellite data.
11.30 Peter Van der Beek (UJF, Grenoble)
Tectonic control on topographic and exhumational segmentation of the Himalaya.
12.00 Yani Najman (Lancaster U.)
Investigating tectonic-erosion interactions: a Himalayan case study.
12:30 Barbara Carrapa (U. Arizona)
Exhumation of the High Himalaya in the Mt. Everest region and India-Asia collision zone: implications for Himalayan tectonics.
14:30 Hugh Sinclair (U. Edinburgh)
Deformation of Himalayan catchments with analysis of the upper Indus River, Ladakh.
15:00 Rob Govers (Utrecht U.)
A single cause for uplift of the Central and Eastern Anatolian plateau?
15:30 Peter DeCelles (U. Arizona)
Hinterland “Bobber” Basins as Recorders of Lithospheric Removal in the Central Andes.
17:00 Martin Stange (Utrecht U.)
Numerical modelling of terrace staircase formation in the Quaternary drainage system of the southern Pyrenees, Ebro basin, NE Iberia.
17:10 Sanjai Mandal
Low denudation recorded by 10Be in Southern Peninsular India.
17:20 Gabriele Calzolari
17:30 Marine Collignon
17:40 Odin Marc
Friday 19th
09:00 Marina Rabineau (U. Brest, France)
Probing connections between deep earth and surface processes in a land-locked ocean basin transformed into a giant saline basin: the Mediterranean DREAM-GOLD project.
09:30 Francisco Sierro (U. Salamanca, Spain)
Deep-Sea Record of Mediterranean Messinian Events (DREAM) multi-phase drilling project. A new challenge for deep sea exploration.
10.00 Iuliana Vasiliev (Utrecht U.)
Recurrent phases of drought in the Miocene of the Black Sea region.
11:30 François Roure (IFP)
Impact of early inversions and recent lithospheric deformations on erosional surfaces and unroofing in circum-Mediterranean thrust belts and margins.
12:00 Charlotte Fillon (CSIC-Barcelona)
Tectonic controls on the Mesopotamian foreland basin evolution: coupled tectonic/surface processes modeling.
12:30 François Guillocheau (Geosc. Rennes)
Cretaceous to Miocene long wavelength landforms of Africa and NW Europe: climate, mantle dynamics and lithosphere deformations controls.
- published: 16 Oct 2014
- views: 295
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6:08
Plate Tectonics and Uplift
published: 18 Mar 2015
Plate Tectonics and Uplift
Plate Tectonics and Uplift
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- published: 18 Mar 2015
- views: 545
2:02
Tectonic uplift - Video Learning - WizScience.com
"Tectonic uplift" is the portion of the total geologic uplift of the mean Earth surface th...
published: 29 Sep 2015
Tectonic uplift - Video Learning - WizScience.com
Tectonic uplift - Video Learning - WizScience.com
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- published: 29 Sep 2015
- views: 748
6:20
Fossils and tectonic uplift in Taranaki
Kyle Bland shows how the fossils at Waihi Beach reveal the story of an uplifting landscape...
published: 18 Jun 2013
Fossils and tectonic uplift in Taranaki
Fossils and tectonic uplift in Taranaki
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- published: 18 Jun 2013
- views: 2277
2:57
Mountain building: Uplift, erosion and exhumation
published: 06 Jun 2015
Mountain building: Uplift, erosion and exhumation
Mountain building: Uplift, erosion and exhumation
- Report rights infringement
- published: 06 Jun 2015
- views: 7235
0:26
Tectonic-uplift Meaning
Video shows what tectonic-uplift means. , noun.. Tectonic-uplift Meaning. How to pronounc...
published: 30 Apr 2015
Tectonic-uplift Meaning
Tectonic-uplift Meaning
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- published: 30 Apr 2015
- views: 46
0:30
Tectonic uplift Meaning
Video shows what tectonic uplift means. The raising of a geographical area as a consequenc...
published: 30 Apr 2015
Tectonic uplift Meaning
Tectonic uplift Meaning
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- published: 30 Apr 2015
- views: 235
0:41
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
Steady state topography development along a vertical cross section. Calculated assuming co...
published: 15 Feb 2012
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
Steady state topography: tectonic uplift + river erosion leading to equilibrium, 1D model
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- published: 15 Feb 2012
- views: 1153
0:55
tectonic uplift final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create anim...
published: 24 Aug 2016
tectonic uplift final
tectonic uplift final
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- published: 24 Aug 2016
- views: 10
2:41
Wax Geology Uplift
How to demonstrate the way geologic forces create conditions where uplift or mountain buil...
published: 21 Nov 2015
Wax Geology Uplift
Wax Geology Uplift
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- published: 21 Nov 2015
- views: 128
1:10
Signs of Himalayan uplift and tectonic plates in Ladakh
Ladakh is a region of Jammu and Kashmir,in the northernmost state of the Republic of India...
published: 13 Feb 2013
Signs of Himalayan uplift and tectonic plates in Ladakh
Signs of Himalayan uplift and tectonic plates in Ladakh
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- published: 13 Feb 2013
- views: 724
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3:28
Llano Uplift, Central Texas
Llano Uplift: Kingsland, Tx
https://en.wikipedia.org/wiki/Greensand
https://en.wikipedia.o...
published: 21 Oct 2016
Llano Uplift, Central Texas
Llano Uplift, Central Texas
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- published: 21 Oct 2016
- views: 30
2:04
BPW up to the uplift
published: 09 Oct 2016
BPW up to the uplift
BPW up to the uplift
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- published: 09 Oct 2016
- views: 15
0:55
tectonic uplift final
-- Created using PowToon -- Free sign up at http://www.powtoon.com/youtube/ -- Create anim...
published: 24 Aug 2016
tectonic uplift final
tectonic uplift final
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- published: 24 Aug 2016
- views: 1
0:21
Modelled uplift history of the Eastern Australian Highlands through time
Modelled topography of the eastern Australian highlands since 150 million years ago. The...
published: 16 Mar 2016
Modelled uplift history of the Eastern Australian Highlands through time
Modelled uplift history of the Eastern Australian Highlands through time
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- published: 16 Mar 2016
- views: 253
4:30
Llano Uplift
This video is about Llano Uplift
published: 12 Dec 2015
Llano Uplift
Llano Uplift
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- published: 12 Dec 2015
- views: 98
0:26
Tectonic Uplift and Climate Change Pdf
http://realbooknow.net/books
published: 25 Nov 2015
Tectonic Uplift and Climate Change Pdf
Tectonic Uplift and Climate Change Pdf
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- published: 25 Nov 2015
- views: 5
0:41
"Nuevos Aires" Uplifted by CUrITa Sheffield
Our first mixed dance style genre event.
Thank you Las Iguanas in the West One Plaza, Shef...
published: 14 Oct 2015
"Nuevos Aires" Uplifted by CUrITa Sheffield
"Nuevos Aires" Uplifted by CUrITa Sheffield
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- published: 14 Oct 2015
- views: 23
2:37
Erosion and tectonics - Video Learning - WizScience.com
The interaction between "erosion and tectonics" has been a topic of debate since the early...
published: 02 Sep 2015
Erosion and tectonics - Video Learning - WizScience.com
Erosion and tectonics - Video Learning - WizScience.com
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- published: 02 Sep 2015
- views: 197
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67:17
What Every Adventist Scientist Should Know: Rates of Erosion and Uplift 3-29-2014 by Ariel Roth
We continue a series on What Every Adventist Scientist Should Know. This fifth week we re...
published: 30 Mar 2014
What Every Adventist Scientist Should Know: Rates of Erosion and Uplift 3-29-2014 by Ariel Roth
What Every Adventist Scientist Should Know: Rates of Erosion and Uplift 3-29-2014 by Ariel Roth
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- published: 30 Mar 2014
- views: 300
31:26
Peter Van der Beek (UJF, Grenoble) - Barcelona 2014 Topo-Europe - Tectonics, Himalayan topography
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
...
published: 16 Oct 2014
Peter Van der Beek (UJF, Grenoble) - Barcelona 2014 Topo-Europe - Tectonics, Himalayan topography
Peter Van der Beek (UJF, Grenoble) - Barcelona 2014 Topo-Europe - Tectonics, Himalayan topography
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- published: 16 Oct 2014
- views: 581
33:56
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-Europe - tectonic-erosion in the Himalayas
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
...
published: 16 Oct 2014
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-Europe - tectonic-erosion in the Himalayas
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-Europe - tectonic-erosion in the Himalayas
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- published: 16 Oct 2014
- views: 242
22:22
New Zealand : Great Walks
New Zealand : Great Walks
New Zealand is an island country in the southwestern Pacific O...
published: 21 Jan 2016
New Zealand : Great Walks
New Zealand : Great Walks
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- published: 21 Jan 2016
- views: 568
49:27
Geoff Batt - Ironing out the Kinks: Oligo-Miocene self-organisation of the
Dynamic geochronological constraint derived from fault-bounded slivers of high grade cryst...
published: 04 Nov 2015
Geoff Batt - Ironing out the Kinks: Oligo-Miocene self-organisation of the
Geoff Batt - Ironing out the Kinks: Oligo-Miocene self-organisation of the
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- published: 04 Nov 2015
- views: 35
29:04
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Topo-Europe - Tectonics & Mesopotamian foreland basin
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
...
published: 16 Oct 2014
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Topo-Europe - Tectonics & Mesopotamian foreland basin
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Topo-Europe - Tectonics & Mesopotamian foreland basin
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- published: 16 Oct 2014
- views: 369
124:51
This is New Zealand
The country geographically comprises two main landmasses – that of the North Island, or Te...
published: 07 Aug 2016
This is New Zealand
This is New Zealand
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24:05
NewZealand Wellington - سفر به نیوزیلند ولینگتون - (Day 4)
#Wellington (/ˈwɛlɪŋtən/) (Māori: Te Whanga-nui-a-Tara) is the #capital city and second mo...
published: 04 Oct 2016
NewZealand Wellington - سفر به نیوزیلند ولینگتون - (Day 4)
NewZealand Wellington - سفر به نیوزیلند ولینگتون - (Day 4)
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- published: 04 Oct 2016
- views: 25
31:09
07 Laurent Jolivet - Barcelona 2014 Topo-Europe
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
...
published: 16 Oct 2014
07 Laurent Jolivet - Barcelona 2014 Topo-Europe
07 Laurent Jolivet - Barcelona 2014 Topo-Europe
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- published: 16 Oct 2014
- views: 238
29:35
06 Barbara Carrapa - Barcelona 2014 Topo-Europe
10th Topo-Europe workshop
Interplay between surface, lithospheric,
and mantle processes
...
published: 16 Oct 2014
06 Barbara Carrapa - Barcelona 2014 Topo-Europe
06 Barbara Carrapa - Barcelona 2014 Topo-Europe
- Report rights infringement
- published: 16 Oct 2014
- views: 295
What Every Adventist Scientist Should Know: Rates ...
Peter Van der Beek (UJF, Grenoble) - Barcelona 201...
Yani Najman (Lancaster U.) - Barcelona 2014 Topo-E...
New Zealand : Great Walks...
Geoff Batt - Ironing out the Kinks: Oligo-Miocene ...
Charlotte Fillon (CSIC-ICTJA) - Barcelona 2014 Top...
This is New Zealand...
NewZealand Wellington - سفر به نیوزیلند ولینگتون ...
07 Laurent Jolivet - Barcelona 2014 Topo-Europe...
06 Barbara Carrapa - Barcelona 2014 Topo-Europe...
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Donald Trump maps out a new administration to bring a seismic shift to Washington
Edit The Independent 10 Nov 2016
Washington began its transition of power Wednesday as the ascendancy of President-elect Donald Trump promised a seismic shift in nearly every facet of the capital city, from military and executive agencies to federal courts and financial and political establishments ... The two men, who spoke by phone early Wednesday morning, plan to meet Thursday ... House Speaker Paul D ... “Now is the time to shake the Earth,” said William J ... Charles E....
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5 shot in downtown Seattle near scene of anti-Trump protests
Edit Business Insider 10 Nov 2016
Police watch as people gather in protest to the election of Republican Donald Trump as the president of the United States in Seattle, Washington, U.S. November 9, 2016. A gunman opened fire in downtown Seattle on Wednesday evening following an argument and wounded five people, one man critically, not far from protests against the surprise victory of Republican Donald Trump in the U.S. presidential election ... Copyright 2016 ... ....
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[VIDEO] Barron Trump Will Be First Son To Live In White House Since JFK Jr.
Edit WorldNews.com 10 Nov 2016
Barron Trump will be America’s first son to live in the White House since John F. Kennedy Jr. in 1963, The Inquisitr reports.President-elect Donald Trump’s youngest son wasn’t old enough to join his much older siblings as a surrogate for his father’s presidential campaign in 2016, but he was at home with his mother watching the polls ... on Nov. 9 ... Kennedy Jr. back in 1963....
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[VIDEO]: Hillary Clinton Concession Speech: 'I'm Sorry We Did Not Win'
Edit WorldNews.com 09 Nov 2016
Addressing the public for the first time since privately conceding the presidential election to Donald Trump, Democratic nominee Hillary Clinton told the nation she wants to work with the president-elect and offered her help on behalf of the country, The Washington Post reported. Surrounded by running mate Virginia Sen ... "Last night, I congratulated Donald Trump and offered to work with him on behalf of our country ... This loss hurts....
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Chinese official named head of Interpol, drawing criticism
Edit Times Free Press 10 Nov 2016
BEIJING (AP) - A top Chinese police official was elected president of Interpol on Thursday, setting off alarm bells among rights advocates over abuses and a lack of transparency within China's legal system, as well as the potential misuse of the police organization to attack Beijing's political opponents ... The Lyon, France-based International Criminal Police Organization has 190 member nations and has the power to issue "red notices." ... ....
UpLift Brings Installment Payments to Travel With Leading Providers
Edit Venture Beat 10 Nov 2016
UpLift, Inc., an innovative start-up that brings digital marketing, travel and fintech expertise to major travel brands, today announced strategic partnerships with leading travel providers. With Pay Monthly, UpLift’s new travel financing service, UpLift’s partners can enable travelers to buy now, but pay later through installment payments offered at the industry’s lowest rates ... About UpLift. ... UpLift, Inc....
'We are scared': Students share fears, teachers calm nerves after election
Edit The Dallas Morning News 10 Nov 2016
At Uplift Education, counselors talked with students who are scared about their families being deported, and classrooms discussed how to be kind to others even when you disagree ... You don’t need to walk around with them bottled up,” said Yasmin Bhatia, CEO of the Uplift charter school network ... Sixty-four percent of Uplift’s 16,000 students are Hispanic, and at some campuses as many as 30 percent of students may be undocumented....
John Lewis’s Christmas Advert 2016: #BusterTheBoxer Clip Features Vaults Cover Of ‘One Day I’ll Fly Away’
Edit Huffington Post 10 Nov 2016
After last year’s tear-jerking Man On The Moon clip, this year’s ad is a whole lot more uplifting - literally - and features a very cute pooch in the form of Buster the Boxer ... was uplifting....
What went right for Donald Trump - and wrong for Hillary Clinton in Florida
Edit Sun Sentinel 10 Nov 2016
Donald Trump's strategist for South Florida got an uplift when, three days before the election, he saw Hillary Clinton on TV in Pembroke Pines — attempting to deliver a speech in a downpour. It confirmed what Blake MacDiarmid, a Republican strategist from Delray Beach, suspected. her candidacy ... ....
WATCH: Baby boy bursts into tears every time he looks at his twin sister
Edit Springfield News-Sun 10 Nov 2016Rural people is getting priority in development and it will continue: HPM Sheikh Hasina (Bangladesh Awami League)
Edit Public Technologies 10 Nov 2016
(Source. Bangladesh Awami League) Published on Wednesday, 09 November 2016 12.51 Hits. 2. Prime Minister Sheikh Hasina said the people of the country have kept their confidence and faith in the Awami League as the rural people are getting more priority in development and this trend would continue ... 'Our uplift would be made from the grassroots stage ... 'Rather they were busy in making their own uplift ... 'This must be done,' she added....
Want a better day at work? Try sunlight
Edit Sydney Morning Herald 10 Nov 2016
I recently moved from an office with no natural sunlight – none at all – to one that now has it flooding in like a wave of nourishment from almost all directions. Of course, there are downsides. Daydreaming has ramped up ... Daniel Pockett ... fascination ... Vitamin D, too, generates a range of positive outcomes such as an enhanced immune system, better sleep cycles and the release of serotonin, which is frequently credited for uplifts in mood....
Why Hillary Clinton - and her husband Bill - wore purple for her concession speech
Edit The Times of India 10 Nov 2016
NEW DELHI. In her uplifting and inspiring concession speech last night, US Democratic Presidential candidate Hillary Clinton wore a pantsuit with a purple shirt and a jacket sporting purple lapels, very likely because it is a colour of an early women's movement, the one that campaigned - hard - for women's right to vote, say Vogue and Vanity Fair, as well as several American social media commentators ... "... RELATED. From around the web....
Editorial: Make the post-election ‘Kumbaya’ moment last
Edit Albuquerque Journal 10 Nov 2016
After what seemed like an endless campaign fueled by invective and vitriol, there was at least a brief respite today ... Trump also had some rare nice words for Clinton ... This is an intramural scrimmage ... Advertisement ... Even if the positive feelings generated by these uplifting messages are short-lived before political reality takes over, it helps to have some respite from the nasty rhetoric, name-calling and posturing of the campaign trail ... ....
Youth and Sports Minister opens Jeux des Jeunes 2016 (Government of the Republic of Mauritius)
Edit Public Technologies 10 Nov 2016
(Source. Government of the Republic of Mauritius) GIS. - 10 November, 2016.'After a memorable sports year 2015, it is clear that we have great ambitions for the Indian Ocean Island Games of 2019 ... Furthermore, the Minister pointed out that the support of the private sector and sponsors play an essential role in government's strategy to uplift our athletes' potential and to achieve a common goal ... Jeux des Jeunes 2016 ... Email ... (noodl....
DBRS Assigns “A” Rating to Caixa Económica Montepio Geral Covered Bonds (Obrigações Hipotecárias - Mortgages - CPT) Series 6 (DBRS Limited)
Edit Public Technologies 10 Nov 2016
(Source. DBRS Limited). Press Releases. Date of Release. November 10, 2016. November 10, 2016. LinkedInShareThisEmail ... -- A two-notch uplift for high recovery prospects ... (1) the CPCA were downgraded below A (low), (2) the LSF Assessment associated with the Programme were downgraded to Average or (3) the quality and consistency of the cover pool (CP) were no longer sufficient to support two notches' uplift for high recovery prospects ... Notes.....
Li Keqiang Meets with President Vladimir Putin of Russia (Ministry of Foreign Affairs of the People's Republic of China)
Edit Public Technologies 10 Nov 2016
(Source. Ministry of Foreign Affairs of the People's Republic of China). On the afternoon of November 8, 2016 local time, Premier Li Keqiang met at the Kremlin Palace in Moscow with President Vladimir Putin of Russia ... Both sides should well implement consensus reached by the two heads of state and uplift China-Russia relations to another new level ... Li Keqiang arrived in Moscow from St ... (noodl. 36236274) ....
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