A drainage divide, water divide, divide or in North Americawatershed is the line that separates neighbouring drainage basins (catchments). In hilly country, the divide lies along topographicalpeaks and ridges, and may be in the form of a single range of hills or mountains (known as a Dividing range). In flat country—especially where the ground is marshy—the divide may an invisible, more or less notional line on the ground on either side of which falling raindrops journey to different rivers, and even to different sides of a region or continent.
Drainage divides hinder river navigation. In pre-industrial times, water divides were crossed at portages. Later, canals connected adjoining drainage basins.
Join award winning teacher Jonathan Bergmann as he explains how rivers flow, drainage basins, watersheds, and other features of river systems. |Uploaded with...
0:41
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from the glacier basin at Triple Divide Peak in Glacier National Park Mont...
13:40
Drainage basin
Drainage basin
Drainage basin
A drainage basin or catchment basin is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins. Similarly, the Missouri and Ohio rivers are each part of their own drainage basins and that of the Mississippi River. Other terms that are used
1:37
The Drainage Basin Song :)
The Drainage Basin Song :)
The Drainage Basin Song :)
A helpful revision song inspired by Geography.
23:52
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of watershed control, flood control, and resulting soil conservation on small towns and farmers.
Public domain film from the Prelinger Archives, slightly cropped to remove uneven edges, with the aspect ratio corrected, and mild video noise reduction applied.
The soundtrack was also processed with volume normalization, noise reduction, clipping reduction, and/or equalization (the resulting sound, though not perfect, is far less noisy than the original).
http://creativecommons.org/licenses/by-sa/3.0/
http://en.wikipedia.org/wiki/Drainage_basin
A drainage basin
13:53
Rajasthan- Its Drainage System 001
Rajasthan- Its Drainage System 001
Rajasthan- Its Drainage System 001
What is drainage, water divide, Arabian, bay of Bangal and Inland drainage system grade X-NTSE.
11:43
Sierra Blanca
Sierra Blanca
Sierra Blanca
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní or Tsisnaasjiní, the Dawn or White Shell Mountain. The mountain is considered to be the eastern boundary of the Dinetah, the traditional Navajo homeland. It is associated with the color white, and is said to be covered in daylight and dawn and fastened to the ground with lightning. It is gendered male.
Robert Ormes noted the first recorded ascent of Blanca by the Wheeler Survey was recorded on August 14, 1874, but to their surprise they found evidence of a stone structure possibly built by Ute Indians.
The volcanic rock that makes up the Blanca massif i
10:42
Canal
Canal
Canal
Canals and navigations are human-made channels for water. In the vernacular both are referred to as 'canals'. The main difference between them is that a navigation parallels a river and shares its drainage basin, while a canal cuts across a drainage divide.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 3.0 (CC-BY-SA-3.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/3.0/
Author-Info: Martin Künzel, Berlin – Edited by Fir0002
Image Source: https://en.wikipedia.org/wiki/File:Alter_Strom.jpg
=======Image-Info=====
16:59
Graubunden: By Julier Pass to St. Moritz
Graubunden: By Julier Pass to St. Moritz
Graubunden: By Julier Pass to St. Moritz
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pass crosses the watershed / drainage divide between the basins of th...
4:01
Wyoming's Great Divide Basin
Wyoming's Great Divide Basin
Wyoming's Great Divide Basin
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate 80 in Wyoming cross the Continental Divide twice? Between the southern Wind River Mountains and the Atlantic Rim, the divide splits, like an oval, arcing to the left and right, and forming the Great Divide Basin.
The Great Divide Basin is a closed drainage basin. None of the rain or snow that falls here goes to the ocean. It encompasses 3,500 square miles. Long ago (56 to 33 million years, during the Eocene Epoch), this area was covered by Lake Gosiute. Though it has long disappeared, Lake Gosiute has shaped the cultural landscape of the Great Divide an
2:59
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
This video shows what happens below the ground to remove nitrates from water when conservation drainage structures are used. It was produced in 2012 by the M...
1:30
Crossing border between Lesotho and Aouth Africa (Maseru)
Crossing border between Lesotho and Aouth Africa (Maseru)
Crossing border between Lesotho and Aouth Africa (Maseru)
Please like my videos, and don't forget to subscribe by clicking the subscribe button up top!
The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Tele River, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.
1:35
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondary mountain range of the Andes called Cordillera de Domeyko. Large volcanoes dominate the landscape, including the Licancabur, Acamarachi, Aguas Calientes and the Láscar. The last is one of the most active volcanoes in Chile. All of them are located along the eastern side of the Salar de Atacama, forming a generally north-south trending line of volcanoes that separate it from smaller endo
0:37
Numerical Simulation of Southern Alps Drainage Evolution
Numerical Simulation of Southern Alps Drainage Evolution
Numerical Simulation of Southern Alps Drainage Evolution
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide And Capture. It illustrates how drainage networks respond to tecton...
Join award winning teacher Jonathan Bergmann as he explains how rivers flow, drainage basins, watersheds, and other features of river systems. |Uploaded with...
0:41
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from the glacier basin at Triple Divide Peak in Glacier National Park Mont...
13:40
Drainage basin
Drainage basin
Drainage basin
A drainage basin or catchment basin is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins. Similarly, the Missouri and Ohio rivers are each part of their own drainage basins and that of the Mississippi River. Other terms that are used
1:37
The Drainage Basin Song :)
The Drainage Basin Song :)
The Drainage Basin Song :)
A helpful revision song inspired by Geography.
23:52
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of watershed control, flood control, and resulting soil conservation on small towns and farmers.
Public domain film from the Prelinger Archives, slightly cropped to remove uneven edges, with the aspect ratio corrected, and mild video noise reduction applied.
The soundtrack was also processed with volume normalization, noise reduction, clipping reduction, and/or equalization (the resulting sound, though not perfect, is far less noisy than the original).
http://creativecommons.org/licenses/by-sa/3.0/
http://en.wikipedia.org/wiki/Drainage_basin
A drainage basin
13:53
Rajasthan- Its Drainage System 001
Rajasthan- Its Drainage System 001
Rajasthan- Its Drainage System 001
What is drainage, water divide, Arabian, bay of Bangal and Inland drainage system grade X-NTSE.
11:43
Sierra Blanca
Sierra Blanca
Sierra Blanca
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní or Tsisnaasjiní, the Dawn or White Shell Mountain. The mountain is considered to be the eastern boundary of the Dinetah, the traditional Navajo homeland. It is associated with the color white, and is said to be covered in daylight and dawn and fastened to the ground with lightning. It is gendered male.
Robert Ormes noted the first recorded ascent of Blanca by the Wheeler Survey was recorded on August 14, 1874, but to their surprise they found evidence of a stone structure possibly built by Ute Indians.
The volcanic rock that makes up the Blanca massif i
10:42
Canal
Canal
Canal
Canals and navigations are human-made channels for water. In the vernacular both are referred to as 'canals'. The main difference between them is that a navigation parallels a river and shares its drainage basin, while a canal cuts across a drainage divide.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 3.0 (CC-BY-SA-3.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/3.0/
Author-Info: Martin Künzel, Berlin – Edited by Fir0002
Image Source: https://en.wikipedia.org/wiki/File:Alter_Strom.jpg
=======Image-Info=====
16:59
Graubunden: By Julier Pass to St. Moritz
Graubunden: By Julier Pass to St. Moritz
Graubunden: By Julier Pass to St. Moritz
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pass crosses the watershed / drainage divide between the basins of th...
4:01
Wyoming's Great Divide Basin
Wyoming's Great Divide Basin
Wyoming's Great Divide Basin
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate 80 in Wyoming cross the Continental Divide twice? Between the southern Wind River Mountains and the Atlantic Rim, the divide splits, like an oval, arcing to the left and right, and forming the Great Divide Basin.
The Great Divide Basin is a closed drainage basin. None of the rain or snow that falls here goes to the ocean. It encompasses 3,500 square miles. Long ago (56 to 33 million years, during the Eocene Epoch), this area was covered by Lake Gosiute. Though it has long disappeared, Lake Gosiute has shaped the cultural landscape of the Great Divide an
2:59
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
This video shows what happens below the ground to remove nitrates from water when conservation drainage structures are used. It was produced in 2012 by the M...
1:30
Crossing border between Lesotho and Aouth Africa (Maseru)
Crossing border between Lesotho and Aouth Africa (Maseru)
Crossing border between Lesotho and Aouth Africa (Maseru)
Please like my videos, and don't forget to subscribe by clicking the subscribe button up top!
The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Tele River, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.
1:35
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondary mountain range of the Andes called Cordillera de Domeyko. Large volcanoes dominate the landscape, including the Licancabur, Acamarachi, Aguas Calientes and the Láscar. The last is one of the most active volcanoes in Chile. All of them are located along the eastern side of the Salar de Atacama, forming a generally north-south trending line of volcanoes that separate it from smaller endo
0:37
Numerical Simulation of Southern Alps Drainage Evolution
Numerical Simulation of Southern Alps Drainage Evolution
Numerical Simulation of Southern Alps Drainage Evolution
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide And Capture. It illustrates how drainage networks respond to tecton...
5:36
Drava by Dr Rudol August 2012
Drava by Dr Rudol August 2012
Drava by Dr Rudol August 2012
All The Copyrights (music and videos) By Zlatko Henezi
Dravais a river in southern Central Europe, which is an important tributary of the Danube. Its source is in Italian South Tyrol, at the drainage divide of Toblach (Dobbiaco) in the Puster Valley.
3:51
PART 0003 2010 BEST BEST OF cruisinwithkenny COLORADO LIVING IN MY TRUCK ON THE Continental Divide
PART 0003 2010 BEST BEST OF cruisinwithkenny COLORADO LIVING IN MY TRUCK ON THE Continental Divide
PART 0003 2010 BEST BEST OF cruisinwithkenny COLORADO LIVING IN MY TRUCK ON THE Continental Divide
THE Documentary thttp://www.facebook.com/profile.php?id=100001983751306 Please check out cruisinwithkenny"s art ..go tohttp://www.cafepress.com/+cruisinwithk...
10:50
Royal Proclamation of 1763
Royal Proclamation of 1763
Royal Proclamation of 1763
The Royal Proclamation of 1763 was issued October 7, 1763, by King George III following Great Britain's acquisition of French territory in North America after the end of the French and Indian War/Seven Years' War, in which it forbade all settlers from settling past a line drawn along the Appalachian Mountains,The purpose of the proclamation was to organize Great Britain's new North American empire and to stabilize relations with Native North Americans through regulation of trade, settlement, and land purchases on the western frontier. The Royal Proclamation continues to be of legal importance to First Nations in Canada and is significant for
1:39
The Sea Of Galilee - Israel
The Sea Of Galilee - Israel
The Sea Of Galilee - Israel
The Kinneret basin is defined as the amalgamation of all groundwater sub-basins whose common drainage area is the Sea of Galilee. The hydrological units comp...
1:39
Triple Divide Peak Glacier National Park
Triple Divide Peak Glacier National Park
Triple Divide Peak Glacier National Park
This video is a 360 degree view from the false summit below triple divide peak in Glacier National Park in Montana, USA. It is one of three places in the wor...
15:57
Caring for Container Hosta
Caring for Container Hosta
Caring for Container Hosta
8:51
Col du San Bernardino / Passo del San Bernardino / BMW R1200GS Moto
Col du San Bernardino / Passo del San Bernardino / BMW R1200GS Moto
Col du San Bernardino / Passo del San Bernardino / BMW R1200GS Moto
De la neige en cette période de mai 2012 et 3-4 degrés au sommet ! La route malgré tout en bon état. Accélération a 4:19 // Acceleration at 4:19 Le col du Sa...
1:02
Iceberg Alley - Newfoundland & Labrador - TV Tourism Commercial - The Travel Channel - Canada
Iceberg Alley - Newfoundland & Labrador - TV Tourism Commercial - The Travel Channel - Canada
Iceberg Alley - Newfoundland & Labrador - TV Tourism Commercial - The Travel Channel - Canada
http://WWW.GAMEZ-GEAR.COM Please Like and comment on our video's Don't forget to SUBSCRIBE to THE TRAVEL CHANNEL YouTube channel and that will help support u...
0:50
3D topographic steady state during the uplift and erosion of a linear mountain range
3D topographic steady state during the uplift and erosion of a linear mountain range
3D topographic steady state during the uplift and erosion of a linear mountain range
Coupled fluvial erosion and orographic precipitation model, using TISC software. Both panels show a top (planform) view: Left: Topography. Dark blue bodies a...
Join award winning teacher Jonathan Bergmann as he explains how rivers flow, drainage basins, watersheds, and other features of river systems. |Uploaded with...
Join award winning teacher Jonathan Bergmann as he explains how rivers flow, drainage basins, watersheds, and other features of river systems. |Uploaded with...
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from the glacier basin at Triple Divide Peak in Glacier National Park Mont...
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from the glacier basin at Triple Divide Peak in Glacier National Park Mont...
A drainage basin or catchment basin is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins. Similarly, the Missouri and Ohio rivers are each part of their own drainage basins and that of the Mississippi River. Other terms that are used to describe drainage basins are catchment, catchment area, drainage area, river basin and water basin. In North America, the term watershed is commonly used to mean a drainage basin, though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide, the former meaning an area, the latter the high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins. In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide. The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier. Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 2.5 (CC BY-SA 2.5)
LicenseLink: http://creativecommons.org/licenses/by-sa/2.5Image Source: https://en.wikipedia.org/wiki/File:Hydrographic_basin.svg
=======Image-Info========
A drainage basin or catchment basin is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins. Similarly, the Missouri and Ohio rivers are each part of their own drainage basins and that of the Mississippi River. Other terms that are used to describe drainage basins are catchment, catchment area, drainage area, river basin and water basin. In North America, the term watershed is commonly used to mean a drainage basin, though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide, the former meaning an area, the latter the high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins. In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide. The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier. Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 2.5 (CC BY-SA 2.5)
LicenseLink: http://creativecommons.org/licenses/by-sa/2.5Image Source: https://en.wikipedia.org/wiki/File:Hydrographic_basin.svg
=======Image-Info========
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of watershed control, flood control, and resulting soil conservation on small towns and farmers.
Public domain film from the Prelinger Archives, slightly cropped to remove uneven edges, with the aspect ratio corrected, and mild video noise reduction applied.
The soundtrack was also processed with volume normalization, noise reduction, clipping reduction, and/or equalization (the resulting sound, though not perfect, is far less noisy than the original).
http://creativecommons.org/licenses/by-sa/3.0/
http://en.wikipedia.org/wiki/Drainage_basin
A drainage basin or watershed (North American English usages) is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins (watersheds). Similarly, the Missouri and American rivers are each part of their own drainage basins/watersheds and that of the Mississippi River.
Other terms that are used to describe drainage basins are catchment, catchment area, catchment basin, drainage area, river basin, and water basin. In North America, the term watershed is commonly used to mean a drainage basin (though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide), the one meaning an area, the other its high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins.
In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide.
The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide or watershed (outside North America) making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier.
Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins...
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of watershed control, flood control, and resulting soil conservation on small towns and farmers.
Public domain film from the Prelinger Archives, slightly cropped to remove uneven edges, with the aspect ratio corrected, and mild video noise reduction applied.
The soundtrack was also processed with volume normalization, noise reduction, clipping reduction, and/or equalization (the resulting sound, though not perfect, is far less noisy than the original).
http://creativecommons.org/licenses/by-sa/3.0/
http://en.wikipedia.org/wiki/Drainage_basin
A drainage basin or watershed (North American English usages) is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins (watersheds). Similarly, the Missouri and American rivers are each part of their own drainage basins/watersheds and that of the Mississippi River.
Other terms that are used to describe drainage basins are catchment, catchment area, catchment basin, drainage area, river basin, and water basin. In North America, the term watershed is commonly used to mean a drainage basin (though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide), the one meaning an area, the other its high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins.
In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide.
The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide or watershed (outside North America) making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier.
Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins...
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní or Tsisnaasjiní, the Dawn or White Shell Mountain. The mountain is considered to be the eastern boundary of the Dinetah, the traditional Navajo homeland. It is associated with the color white, and is said to be covered in daylight and dawn and fastened to the ground with lightning. It is gendered male.
Robert Ormes noted the first recorded ascent of Blanca by the Wheeler Survey was recorded on August 14, 1874, but to their surprise they found evidence of a stone structure possibly built by Ute Indians.
The volcanic rock that makes up the Blanca massif is pre-Cambrian in age, dated at approximately 1.8 billion years old. The major part of the Wet Mountains to the east and the Front Range to the northeast are also pre-Cambrian, also about 1.8 billion years old. In contrast, the Sangre de Cristo Range to the north and the Culebra Range to the south are Permian rock between 250 and 300 million years old.
Blanca Peak is the fifth highest summit of the Rocky Mountains of North America and the U.S. state of Colorado. The ultra-prominent 14,351-foot peak is the highest summit of the Sierra Blanca Massif, and the Sangre de Cristo Range. The fourteener is located north by east of the Town of Blanca, on the drainage divide separating Rio Grande National Forest and Alamosa County from the Sangre de Cristo Land Grant and Costilla County. The summit is the highest point of both counties and the entire drainage basin of the Rio Grande. Blanca Peak is higher than any point in the United States east of its longitude.
The Blanca Peak Tripoint of Alamosa, Costilla, and Huerfano counties is located on the same drainage divide northeast by north of the Blanca Peak summit at the boundary of the San Isabel National Forest. The Blanca Peak Tripoint is the highest point in Huerfano County.
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní or Tsisnaasjiní, the Dawn or White Shell Mountain. The mountain is considered to be the eastern boundary of the Dinetah, the traditional Navajo homeland. It is associated with the color white, and is said to be covered in daylight and dawn and fastened to the ground with lightning. It is gendered male.
Robert Ormes noted the first recorded ascent of Blanca by the Wheeler Survey was recorded on August 14, 1874, but to their surprise they found evidence of a stone structure possibly built by Ute Indians.
The volcanic rock that makes up the Blanca massif is pre-Cambrian in age, dated at approximately 1.8 billion years old. The major part of the Wet Mountains to the east and the Front Range to the northeast are also pre-Cambrian, also about 1.8 billion years old. In contrast, the Sangre de Cristo Range to the north and the Culebra Range to the south are Permian rock between 250 and 300 million years old.
Blanca Peak is the fifth highest summit of the Rocky Mountains of North America and the U.S. state of Colorado. The ultra-prominent 14,351-foot peak is the highest summit of the Sierra Blanca Massif, and the Sangre de Cristo Range. The fourteener is located north by east of the Town of Blanca, on the drainage divide separating Rio Grande National Forest and Alamosa County from the Sangre de Cristo Land Grant and Costilla County. The summit is the highest point of both counties and the entire drainage basin of the Rio Grande. Blanca Peak is higher than any point in the United States east of its longitude.
The Blanca Peak Tripoint of Alamosa, Costilla, and Huerfano counties is located on the same drainage divide northeast by north of the Blanca Peak summit at the boundary of the San Isabel National Forest. The Blanca Peak Tripoint is the highest point in Huerfano County.
Canals and navigations are human-made channels for water. In the vernacular both are referred to as 'canals'. The main difference between them is that a navigation parallels a river and shares its drainage basin, while a canal cuts across a drainage divide.
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Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 3.0 (CC-BY-SA-3.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/3.0/
Author-Info: Martin Künzel, Berlin – Edited by Fir0002
Image Source: https://en.wikipedia.org/wiki/File:Alter_Strom.jpg
=======Image-Info========
Canals and navigations are human-made channels for water. In the vernacular both are referred to as 'canals'. The main difference between them is that a navigation parallels a river and shares its drainage basin, while a canal cuts across a drainage divide.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 3.0 (CC-BY-SA-3.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/3.0/
Author-Info: Martin Künzel, Berlin – Edited by Fir0002
Image Source: https://en.wikipedia.org/wiki/File:Alter_Strom.jpg
=======Image-Info========
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pass crosses the watershed / drainage divide between the basins of th...
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pass crosses the watershed / drainage divide between the basins of th...
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate 80 in Wyoming cross the Continental Divide twice? Between the southern Wind River Mountains and the Atlantic Rim, the divide splits, like an oval, arcing to the left and right, and forming the Great Divide Basin.
The Great Divide Basin is a closed drainage basin. None of the rain or snow that falls here goes to the ocean. It encompasses 3,500 square miles. Long ago (56 to 33 million years, during the Eocene Epoch), this area was covered by Lake Gosiute. Though it has long disappeared, Lake Gosiute has shaped the cultural landscape of the Great Divide and Green River basins since the earliest days of human occupation, at the end of the last Ice Age. Please see this educational video by the Wyoming State Geological Survey, funded by the Wyoming Cultural Trust Fund.
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate 80 in Wyoming cross the Continental Divide twice? Between the southern Wind River Mountains and the Atlantic Rim, the divide splits, like an oval, arcing to the left and right, and forming the Great Divide Basin.
The Great Divide Basin is a closed drainage basin. None of the rain or snow that falls here goes to the ocean. It encompasses 3,500 square miles. Long ago (56 to 33 million years, during the Eocene Epoch), this area was covered by Lake Gosiute. Though it has long disappeared, Lake Gosiute has shaped the cultural landscape of the Great Divide and Green River basins since the earliest days of human occupation, at the end of the last Ice Age. Please see this educational video by the Wyoming State Geological Survey, funded by the Wyoming Cultural Trust Fund.
published:09 Jun 2015
views:3
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
This video shows what happens below the ground to remove nitrates from water when conservation drainage structures are used. It was produced in 2012 by the M...
This video shows what happens below the ground to remove nitrates from water when conservation drainage structures are used. It was produced in 2012 by the M...
Please like my videos, and don't forget to subscribe by clicking the subscribe button up top!
The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Tele River, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.
Please like my videos, and don't forget to subscribe by clicking the subscribe button up top!
The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Tele River, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.
published:19 May 2015
views:8
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondary mountain range of the Andes called Cordillera de Domeyko. Large volcanoes dominate the landscape, including the Licancabur, Acamarachi, Aguas Calientes and the Láscar. The last is one of the most active volcanoes in Chile. All of them are located along the eastern side of the Salar de Atacama, forming a generally north-south trending line of volcanoes that separate it from smaller endorheic basins. The salt flat encompasses 3,000 km2 (1,200 sq mi), is about 100 km (62 mi) long and 80 km (50 mi) wide, which makes it the third largest in the world, after Salar de Uyuni in Bolivia (10,582 km2 (4,086 sq mi) and Salinas Grandes in Argentina (6,000 km2, 2,300 sq mi). Its average elevation is about 2,300 m above sea level. The topography of the core portion of the salar exhibits a high level of roughness, the result of evaporation and ephemeral surface water, unlike the most other salt flats, as for example the Salar de Uyuni, which is periodically covered with shallow water. Some areas of the salt flat form part of Los Flamencos National Reserve. The Laguna Cejar is a sink hole lake in the Salar de Atacama, 18 km from San Pedro, Chile. It has a salt concentration that ranges from 5 to 28% (50 to 280 parts per thousand), producing at the higher end of the range an effect of floating like the Dead Sea. Salar de Atacama basin is bordered on the north by the Salado River basin, which is a sub-basin of the Loa River basin. To the east, the drainage divide approximately coincides with the international border with Bolivia until the Portezuelo del Cajón. The dividing range includes the volcanoes Cerros de Tocorpuri, Sairecabur, Curiquinca, Licancabur and Juriques. Going southward, the water divide runs along a chain of volcanoes that lie entirely in Chilean territory. To the west, the Cordillera Domeyko separates the Salar de Atacama basin from arheic areas.
Its main tributaries are the San Pedro and Vilama rivers, which originate to the north of the salt flat. Salar de Atacama is the world's largest and purest active source of lithium,containing 27% of the world's lithium reserve base, and as of 2008 provided almost 30% of the world's lithium carbonate supply, followed by China with 23%. High lithium concentration in its brine (2,700 parts per million).
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondary mountain range of the Andes called Cordillera de Domeyko. Large volcanoes dominate the landscape, including the Licancabur, Acamarachi, Aguas Calientes and the Láscar. The last is one of the most active volcanoes in Chile. All of them are located along the eastern side of the Salar de Atacama, forming a generally north-south trending line of volcanoes that separate it from smaller endorheic basins. The salt flat encompasses 3,000 km2 (1,200 sq mi), is about 100 km (62 mi) long and 80 km (50 mi) wide, which makes it the third largest in the world, after Salar de Uyuni in Bolivia (10,582 km2 (4,086 sq mi) and Salinas Grandes in Argentina (6,000 km2, 2,300 sq mi). Its average elevation is about 2,300 m above sea level. The topography of the core portion of the salar exhibits a high level of roughness, the result of evaporation and ephemeral surface water, unlike the most other salt flats, as for example the Salar de Uyuni, which is periodically covered with shallow water. Some areas of the salt flat form part of Los Flamencos National Reserve. The Laguna Cejar is a sink hole lake in the Salar de Atacama, 18 km from San Pedro, Chile. It has a salt concentration that ranges from 5 to 28% (50 to 280 parts per thousand), producing at the higher end of the range an effect of floating like the Dead Sea. Salar de Atacama basin is bordered on the north by the Salado River basin, which is a sub-basin of the Loa River basin. To the east, the drainage divide approximately coincides with the international border with Bolivia until the Portezuelo del Cajón. The dividing range includes the volcanoes Cerros de Tocorpuri, Sairecabur, Curiquinca, Licancabur and Juriques. Going southward, the water divide runs along a chain of volcanoes that lie entirely in Chilean territory. To the west, the Cordillera Domeyko separates the Salar de Atacama basin from arheic areas.
Its main tributaries are the San Pedro and Vilama rivers, which originate to the north of the salt flat. Salar de Atacama is the world's largest and purest active source of lithium,containing 27% of the world's lithium reserve base, and as of 2008 provided almost 30% of the world's lithium carbonate supply, followed by China with 23%. High lithium concentration in its brine (2,700 parts per million).
published:28 Jan 2014
views:304
Numerical Simulation of Southern Alps Drainage Evolution
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide And Capture. It illustrates how drainage networks respond to tecton...
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide And Capture. It illustrates how drainage networks respond to tecton...
All The Copyrights (music and videos) By Zlatko Henezi
Dravais a river in southern Central Europe, which is an important tributary of the Danube. Its source is in Italian South Tyrol, at the drainage divide of Toblach (Dobbiaco) in the Puster Valley.
All The Copyrights (music and videos) By Zlatko Henezi
Dravais a river in southern Central Europe, which is an important tributary of the Danube. Its source is in Italian South Tyrol, at the drainage divide of Toblach (Dobbiaco) in the Puster Valley.
published:13 Jul 2015
views:0
PART 0003 2010 BEST BEST OF cruisinwithkenny COLORADO LIVING IN MY TRUCK ON THE Continental Divide
THE Documentary thttp://www.facebook.com/profile.php?id=100001983751306 Please check out cruisinwithkenny"s art ..go tohttp://www.cafepress.com/+cruisinwithk...
THE Documentary thttp://www.facebook.com/profile.php?id=100001983751306 Please check out cruisinwithkenny"s art ..go tohttp://www.cafepress.com/+cruisinwithk...
The Royal Proclamation of 1763 was issued October 7, 1763, by King George III following Great Britain's acquisition of French territory in North America after the end of the French and Indian War/Seven Years' War, in which it forbade all settlers from settling past a line drawn along the Appalachian Mountains,The purpose of the proclamation was to organize Great Britain's new North American empire and to stabilize relations with Native North Americans through regulation of trade, settlement, and land purchases on the western frontier. The Royal Proclamation continues to be of legal importance to First Nations in Canada and is significant for the variation of indigenous status in the United States. It eventually ensured that British culture and laws were applied in Upper Canada after 1791, which was done to attract British settlers to the province. Its geographic location is similar to the Eastern Continental Divide's path running northwards from Georgia to the Pennsylvania-New York State border, and north-eastwards past the drainage divide on the "St. Lawrence Divide" from there northwards through New England.
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The Royal Proclamation of 1763 was issued October 7, 1763, by King George III following Great Britain's acquisition of French territory in North America after the end of the French and Indian War/Seven Years' War, in which it forbade all settlers from settling past a line drawn along the Appalachian Mountains,The purpose of the proclamation was to organize Great Britain's new North American empire and to stabilize relations with Native North Americans through regulation of trade, settlement, and land purchases on the western frontier. The Royal Proclamation continues to be of legal importance to First Nations in Canada and is significant for the variation of indigenous status in the United States. It eventually ensured that British culture and laws were applied in Upper Canada after 1791, which was done to attract British settlers to the province. Its geographic location is similar to the Eastern Continental Divide's path running northwards from Georgia to the Pennsylvania-New York State border, and north-eastwards past the drainage divide on the "St. Lawrence Divide" from there northwards through New England.
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
The Kinneret basin is defined as the amalgamation of all groundwater sub-basins whose common drainage area is the Sea of Galilee. The hydrological units comp...
The Kinneret basin is defined as the amalgamation of all groundwater sub-basins whose common drainage area is the Sea of Galilee. The hydrological units comp...
This video is a 360 degree view from the false summit below triple divide peak in Glacier National Park in Montana, USA. It is one of three places in the wor...
This video is a 360 degree view from the false summit below triple divide peak in Glacier National Park in Montana, USA. It is one of three places in the wor...
De la neige en cette période de mai 2012 et 3-4 degrés au sommet ! La route malgré tout en bon état. Accélération a 4:19 // Acceleration at 4:19 Le col du Sa...
De la neige en cette période de mai 2012 et 3-4 degrés au sommet ! La route malgré tout en bon état. Accélération a 4:19 // Acceleration at 4:19 Le col du Sa...
http://WWW.GAMEZ-GEAR.COM Please Like and comment on our video's Don't forget to SUBSCRIBE to THE TRAVEL CHANNEL YouTube channel and that will help support u...
http://WWW.GAMEZ-GEAR.COM Please Like and comment on our video's Don't forget to SUBSCRIBE to THE TRAVEL CHANNEL YouTube channel and that will help support u...
Coupled fluvial erosion and orographic precipitation model, using TISC software. Both panels show a top (planform) view: Left: Topography. Dark blue bodies a...
Coupled fluvial erosion and orographic precipitation model, using TISC software. Both panels show a top (planform) view: Left: Topography. Dark blue bodies a...
Join award winning teacher Jonathan Bergmann as he explains how rivers flow, drainage basins, watersheds, and other features of river systems. |Uploaded with...
0:41
Triple Divide Peak Waterfall at Glacier National Park (Artic Drainage)
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from th...
Here is a view from the top of the waterfall leading down to Grizzly Medicine Lake from the glacier basin at Triple Divide Peak in Glacier National Park Mont...
13:40
Drainage basin
A drainage basin or catchment basin is an extent or an area of land where surface water fr...
published:06 Aug 2015
Drainage basin
Drainage basin
published:06 Aug 2015
views:1
A drainage basin or catchment basin is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins. Similarly, the Missouri and Ohio rivers are each part of their own drainage basins and that of the Mississippi River. Other terms that are used to describe drainage basins are catchment, catchment area, drainage area, river basin and water basin. In North America, the term watershed is commonly used to mean a drainage basin, though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide, the former meaning an area, the latter the high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins. In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide. The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier. Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins.
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Article text available under CC-BY-SA
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License: Creative Commons Attribution-Share Alike 2.5 (CC BY-SA 2.5)
LicenseLink: http://creativecommons.org/licenses/by-sa/2.5Image Source: https://en.wikipedia.org/wiki/File:Hydrographic_basin.svg
=======Image-Info========
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of wate...
published:14 Dec 2014
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
From the Ridge to the River: The Story of a Watershed circa 1940 USDA Soil Conservation
published:14 Dec 2014
views:22
more at http://quickfound.net/links/agriculture_news_and_links.html
On the impact of watershed control, flood control, and resulting soil conservation on small towns and farmers.
Public domain film from the Prelinger Archives, slightly cropped to remove uneven edges, with the aspect ratio corrected, and mild video noise reduction applied.
The soundtrack was also processed with volume normalization, noise reduction, clipping reduction, and/or equalization (the resulting sound, though not perfect, is far less noisy than the original).
http://creativecommons.org/licenses/by-sa/3.0/
http://en.wikipedia.org/wiki/Drainage_basin
A drainage basin or watershed (North American English usages) is an extent or an area of land where surface water from rain, melting snow, or ice converges to a single point at a lower elevation, usually the exit of the basin, where the waters join another waterbody, such as a river, lake, reservoir, estuary, wetland, sea, or ocean. For example, a tributary stream of a brook that joins a small river is tributary of a larger river, which is thus part of a series of successively smaller area but higher elevation drainage basins (watersheds). Similarly, the Missouri and American rivers are each part of their own drainage basins/watersheds and that of the Mississippi River.
Other terms that are used to describe drainage basins are catchment, catchment area, catchment basin, drainage area, river basin, and water basin. In North America, the term watershed is commonly used to mean a drainage basin (though in other English-speaking countries, it is used only in its original sense, to mean a drainage divide), the one meaning an area, the other its high elevation perimeter of that area. Drainage basins drain into other drainage basins in a hierarchical pattern, with smaller sub-drainage basins combining into larger drainage basins.
In closed ("endorheic") drainage basins the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, dry lake, or a point where surface water is lost underground. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide.
The drainage basin acts as a funnel by collecting all the water within the area covered by the basin and channelling it to a single point. Each drainage basin is separated topographically from adjacent basins by a perimeter, the drainage divide or watershed (outside North America) making up a succession of higher geographical features (such as a ridge, hill or mountains) forming a barrier.
Drainage basins are similar but not identical to hydrologic units, which are drainage areas delineated so as to nest into a multi-level hierarchical drainage system. Hydrologic units are designed to allow multiple inlets, outlets, or sinks. In a strict sense, all drainage basins are hydrologic units but not all hydrologic units are drainage basins...
13:53
Rajasthan- Its Drainage System 001
What is drainage, water divide, Arabian, bay of Bangal and Inland drainage system grade X-...
What is drainage, water divide, Arabian, bay of Bangal and Inland drainage system grade X-NTSE.
11:43
Sierra Blanca
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní o...
published:05 Jul 2015
Sierra Blanca
Sierra Blanca
published:05 Jul 2015
views:11
Blanca Peak is known to the Navajo people as the Sacred Mountain of the East: Sisnaajiní or Tsisnaasjiní, the Dawn or White Shell Mountain. The mountain is considered to be the eastern boundary of the Dinetah, the traditional Navajo homeland. It is associated with the color white, and is said to be covered in daylight and dawn and fastened to the ground with lightning. It is gendered male.
Robert Ormes noted the first recorded ascent of Blanca by the Wheeler Survey was recorded on August 14, 1874, but to their surprise they found evidence of a stone structure possibly built by Ute Indians.
The volcanic rock that makes up the Blanca massif is pre-Cambrian in age, dated at approximately 1.8 billion years old. The major part of the Wet Mountains to the east and the Front Range to the northeast are also pre-Cambrian, also about 1.8 billion years old. In contrast, the Sangre de Cristo Range to the north and the Culebra Range to the south are Permian rock between 250 and 300 million years old.
Blanca Peak is the fifth highest summit of the Rocky Mountains of North America and the U.S. state of Colorado. The ultra-prominent 14,351-foot peak is the highest summit of the Sierra Blanca Massif, and the Sangre de Cristo Range. The fourteener is located north by east of the Town of Blanca, on the drainage divide separating Rio Grande National Forest and Alamosa County from the Sangre de Cristo Land Grant and Costilla County. The summit is the highest point of both counties and the entire drainage basin of the Rio Grande. Blanca Peak is higher than any point in the United States east of its longitude.
The Blanca Peak Tripoint of Alamosa, Costilla, and Huerfano counties is located on the same drainage divide northeast by north of the Blanca Peak summit at the boundary of the San Isabel National Forest. The Blanca Peak Tripoint is the highest point in Huerfano County.
10:42
Canal
Canals and navigations are human-made channels for water. In the vernacular both are refer...
published:05 Aug 2015
Canal
Canal
published:05 Aug 2015
views:0
Canals and navigations are human-made channels for water. In the vernacular both are referred to as 'canals'. The main difference between them is that a navigation parallels a river and shares its drainage basin, while a canal cuts across a drainage divide.
Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
=======Image-Info========
License: Creative Commons Attribution-Share Alike 3.0 (CC-BY-SA-3.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/3.0/
Author-Info: Martin Künzel, Berlin – Edited by Fir0002
Image Source: https://en.wikipedia.org/wiki/File:Alter_Strom.jpg
=======Image-Info========
16:59
Graubunden: By Julier Pass to St. Moritz
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pa...
Julier Pass connects the Engadin valley with the rest of Graubünden. At its summit, the pass crosses the watershed / drainage divide between the basins of th...
4:01
Wyoming's Great Divide Basin
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate ...
published:09 Jun 2015
Wyoming's Great Divide Basin
Wyoming's Great Divide Basin
published:09 Jun 2015
views:3
WY Cultural Geology Guide: The Origin of Landscape - Did you know travelers on Interstate 80 in Wyoming cross the Continental Divide twice? Between the southern Wind River Mountains and the Atlantic Rim, the divide splits, like an oval, arcing to the left and right, and forming the Great Divide Basin.
The Great Divide Basin is a closed drainage basin. None of the rain or snow that falls here goes to the ocean. It encompasses 3,500 square miles. Long ago (56 to 33 million years, during the Eocene Epoch), this area was covered by Lake Gosiute. Though it has long disappeared, Lake Gosiute has shaped the cultural landscape of the Great Divide and Green River basins since the earliest days of human occupation, at the end of the last Ice Age. Please see this educational video by the Wyoming State Geological Survey, funded by the Wyoming Cultural Trust Fund.
2:59
Nabbing Nitrates Before Water Leaves the Farm: Conservation Drainage
This video shows what happens below the ground to remove nitrates from water when conserva...
This video shows what happens below the ground to remove nitrates from water when conservation drainage structures are used. It was produced in 2012 by the M...
1:30
Crossing border between Lesotho and Aouth Africa (Maseru)
Please like my videos, and don't forget to subscribe by clicking the subscribe button up t...
published:19 May 2015
Crossing border between Lesotho and Aouth Africa (Maseru)
Crossing border between Lesotho and Aouth Africa (Maseru)
published:19 May 2015
views:8
Please like my videos, and don't forget to subscribe by clicking the subscribe button up top!
The border between Lesotho and South Africa is 909 kilometres (565 mi) long and forms a complete loop, as Lesotho is an enclave entirely surrounded by South Africa. The border follows the Caledon River, the drainage divide of the Drakensberg mountains, the Tele River, the Orange River, the Makhaleng River, and a series of hills joining the Makhaleng back to the Caledon.
1:35
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of S...
published:28 Jan 2014
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
Salar de Atacama, Atacama Desert, Antofagasta Region, Chile, South America
published:28 Jan 2014
views:304
Salar de Atacama is the largest salt flat in Chile. It is located 55 km (34 mi) south of San Pedro de Atacama, is surrounded by mountains, and has no drainage outlets. In the east it is enclosed by the main chain of the Andes, while to the west lies a secondary mountain range of the Andes called Cordillera de Domeyko. Large volcanoes dominate the landscape, including the Licancabur, Acamarachi, Aguas Calientes and the Láscar. The last is one of the most active volcanoes in Chile. All of them are located along the eastern side of the Salar de Atacama, forming a generally north-south trending line of volcanoes that separate it from smaller endorheic basins. The salt flat encompasses 3,000 km2 (1,200 sq mi), is about 100 km (62 mi) long and 80 km (50 mi) wide, which makes it the third largest in the world, after Salar de Uyuni in Bolivia (10,582 km2 (4,086 sq mi) and Salinas Grandes in Argentina (6,000 km2, 2,300 sq mi). Its average elevation is about 2,300 m above sea level. The topography of the core portion of the salar exhibits a high level of roughness, the result of evaporation and ephemeral surface water, unlike the most other salt flats, as for example the Salar de Uyuni, which is periodically covered with shallow water. Some areas of the salt flat form part of Los Flamencos National Reserve. The Laguna Cejar is a sink hole lake in the Salar de Atacama, 18 km from San Pedro, Chile. It has a salt concentration that ranges from 5 to 28% (50 to 280 parts per thousand), producing at the higher end of the range an effect of floating like the Dead Sea. Salar de Atacama basin is bordered on the north by the Salado River basin, which is a sub-basin of the Loa River basin. To the east, the drainage divide approximately coincides with the international border with Bolivia until the Portezuelo del Cajón. The dividing range includes the volcanoes Cerros de Tocorpuri, Sairecabur, Curiquinca, Licancabur and Juriques. Going southward, the water divide runs along a chain of volcanoes that lie entirely in Chilean territory. To the west, the Cordillera Domeyko separates the Salar de Atacama basin from arheic areas.
Its main tributaries are the San Pedro and Vilama rivers, which originate to the north of the salt flat. Salar de Atacama is the world's largest and purest active source of lithium,containing 27% of the world's lithium reserve base, and as of 2008 provided almost 30% of the world's lithium carbonate supply, followed by China with 23%. High lithium concentration in its brine (2,700 parts per million).
0:37
Numerical Simulation of Southern Alps Drainage Evolution
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide ...
This movie shows a 11 million year simulation of the landscape evolution model DAC-Divide And Capture. It illustrates how drainage networks respond to tecton...
CoreBot infant could grow to painful teenager. IBM threat researcher Limor Kessem has found a new modular malware credential stealer that could become a significant enterprise threat.... ....
San Francisco, Sep 2 (IANS) Google revealed its new logo, which keeps the red, blue, yellow and green colours of the tech giant's original logo but changes the lettering to a simpler, rounded "ProductSans" font. Until now, the firm has used a serif typeface for its logo for more than 16 years ... All of the companies will be overseen by Alphabet, whose CEO will be Google co-founder Larry Page. ....
(CNN)GilbertFlores is shirtless, running in front of a home in San Antonio as the two sheriff's deputies approach him. A minute later, he's putting his hands up. Then the shots ring out, and he falls to the ground. Cell phone video obtained by CNN affiliate KSAT appears to show sheriff's deputies in Bexar County, Texas, shooting and killing the 41-year-old Friday ... They confirmed it was Flores on Monday ... 'Threats to our deputies' lives' ... ....
The mystery of a Nazi gold train said to be buried in Poland has taken another strange turn, after the location where the armoured train is believed to be hidden was engulfed in flames - after the Polish government cast doubt over its existence. The train has caught the imagination of locals in the town of Walbrzych and the international media alike, after two men told the authorities they had pinpointed the location of the train ... AP)....
NEW YORK (AP) -- Markets are turning turbulent again after investors were unnerved by more signs of weakness in China, the world's second-largest economy. U.S. stocks sank 3 percent Tuesday, their third-worst drop this year. The two bigger falls occurred in the last two weeks. The Dow Jones industrial average dropped 469 points, or 2.8 percent, to 16,058. The Standard & Poor's 500 index fell 58 points, or 3 percent, to 1,913 ...U.S ... U.S ... ....
Not far from the spot where Opportunity landed on Mars sits a large basin that looks a lot like the salt flats seen on our own planet. According to a new study out this week in Geology, this location may have been home to one of the final lakes to exist on Mars before the Red Planet turned into the dry desert world we see today ...Eventually, the water level rose high enough to spill over the drainagedivide ... Read this next....
... over the Rio Cachaco drainagedivide Metallurgical testwork on Hole 5 samples well advanced Independent geological review confirms both size and high grade potential at Alpala ... Preliminary geological inspection over the southern drainagedivide of the Rio Cachaco catchment is underway, and will be followed by geological mapping and soil sampling....
The technique focuses on a river network's drainagedivides - ridgelines, such as along mountain ranges, that act as boundaries between two river basins. As rainwater flows down either side of a drainagedivide and into opposing rivers, it erodes the underlying rock ... To reach a balance, they reasoned that a drainagedivide must shift to assume a more stable pattern....
Willett and his colleagues devised a mathematical model focused on migrating drainagedivides — the dividing line between two river basins ...Drainagedivides can move across the landscape if rivers on one side of the divide cut into it faster than rivers on the other side ... The researchers found that by mapping height mismatches across drainagedivides they could predict the directions in which divides would migrate....