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In geology, rock or stone is a naturally occurring solid aggregate of minerals and/or mineraloids.
The Earth's outer solid layer, the lithosphere, is made of rock. Three majors groups of rocks are defined: igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is an essential component of geology.
Rocks are generally classified by mineral and chemical composition, by the texture of the constituent particles and by the processes that formed them. These indicators separate rocks into three types: igneous, sedimentary, and metamorphic. They are further classified according to particle size. The transformation of one rock type to another is described by the geological model called the rock cycle.
Igneous rocks are formed when molten magma cools and are divided into two main categories: plutonic rock and volcanic. Plutonic or intrusive rocks result when magma cools and crystallizes slowly within the Earth's crust (example granite), while volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta (examples pumice and basalt).
This page contains text from Wikipedia, the Free Encyclopedia -
http://en.wikipedia.org/wiki/Rock_(geology)
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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Basics of Geology All About Rocks and Minerals
Basics of Geology All About Rocks and Minerals -
Living Rock An Introduction to Earths Geology
Living Rock An Introduction to Earths GeologyLiving Rock An Introduction to Earths Geology
US Survey series. -
Geology Kitchen: The 3 Types of Rocks
Geology Kitchen: The 3 Types of RocksGeology Kitchen: The 3 Types of Rocks
http://explorermultimedia.org/ Geologist Devin Dennie heads to the kitchen to demonstrate the differences between the three types of rocks. -
BBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep TimeBBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time - Iain Stewart tells the story of James Hutton, the founding father of geology. Uploaded for educational purposes, all mater... -
Geology Rocks Song Practice
Geology Rocks Song PracticeGeology Rocks Song Practice
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through! 1. Professor Rock Has Disappeared 0:07 2. Geologic Time 2:26 3. I Ain't Well 4:24 4. I Am Deep 6:27 5. Oh to be a Fossil Fuel 8:04 6. Erosion 10:24 7. Love Them Plates 12:28 8. Seven Little Miners 14:26 9. Rock Cycle 16:22 10. Professor Rock Has Re-Appeared 18:35 Ready to practice on your own? Click here for instruments only: https://youtu.be/C2zqW_3zqIs These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole -
Basic Rock Identification: Geology
Basic Rock Identification: GeologyBasic Rock Identification: Geology
Visual Study Aid for Physical/Historical Geology Classes. MUSIC: "DISTANCE" by Soilwork, from the "Stabbing the Drama" album. -
Geology for IDiots Episode 1 Rocks Part 2
Geology for IDiots Episode 1 Rocks Part 2Geology for IDiots Episode 1 Rocks Part 2
Part 2 of Episode 1 Geology for IDiots with this episode focusing on Rocks My Blog as Promised: http://hochemon2008.blogspot.com/ Any questions comments or c... -
Fossil Rock Anthem
Fossil Rock AnthemFossil Rock Anthem
Explain/annotate the lyrics on rap genius: http://rapgenius.com/Tom-mcfadden-fossil-rock-anthem-lyrics The song parodies "Party Rock Anthem" by LMFAO. The instrumental was made by DJ Lisan (www.soundcloud.com/dj-lisan) in San Francisco. Female vocals by Nicole Bonsol. Male vocals and lyrics and the animated video by me. Mastered by Hank Kalleen (Ear Jerker). The song covers the California 7th grade standards on Earth & life history. The song and video are part of thesis I'm doing about the impact of music in science education as part of a Master of Science Communication at the University Otago in New Zealand (which began thanks to a Fulbri -
Rock and Mineral Identification
Rock and Mineral IdentificationRock and Mineral Identification
A study guide made for the students of Fleming College in Lindsay Ontario Canada and anybody else who might find it useful. If you like this video check out ... -
Geology Kitchen #3 - Clastic Sedimentary Rocks
Geology Kitchen #3 - Clastic Sedimentary RocksGeology Kitchen #3 - Clastic Sedimentary Rocks
Episode 3 begins to examine the world of sedimentary rocks by looking at how clastic sedimentary rocks form. Various food stuffs of different grain sizes are... -
GEOLOGY ROCKS! (Jasongs)
GEOLOGY ROCKS! (Jasongs)GEOLOGY ROCKS! (Jasongs)
A true "rock" song. Check out the CD quality, stereo version along with a host of other great songs at: http://www.cdbaby.com/jasongs3 itunes, amazon.com LYR... -
Geology, the rock cycle
Geology, the rock cycleGeology, the rock cycle
the rock cycle. -
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Geology Kitchen #5 - Chemical & Biological Sedimentary RocksGeology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Chemical and biological sedimentary rocks are discussed in this video. Carbonates, including limestones and dolomites are discussed, and cave stalactites are made. Evaporites are made in pan on stove experiment, and coal and chert are also examined as other forms of sedimentary rock. This episode is to be paired with the "Clastic Rocks" episode for a complete review of the sedimentary rock types. -
Geology Kitchen #11 - Igneous Rocks
Geology Kitchen #11 - Igneous RocksGeology Kitchen #11 - Igneous Rocks
Igneous rocks are rocks derived from the cooling of magma, molten material originating from the upper Mantle/lower crust. Igneous rocks are classified by the...
- Basalt
- Base metals
- Bronze Age
- Cairn
- Carbonate rock
- Chemical
- Chemical synthesis
- Clastic
- Coal
- Coal mining
- Colorado Springs, CO
- Costa Rica
- Crust (geology)
- Crystallization
- Crystallography
- Denudation
- Detritus
- Diagenesis
- Diamond
- Dimension stone
- Dolostone
- Earth
- Engineering geology
- Erosion
- Evaporite
- Extrusive (geology)
- Factory
- Formation of rocks
- Fossil water
- Freezing
- Gabbro
- Garden of the Gods
- Geochemistry
- Geodesy
- Geodynamics
- Geologic time scale
- Geology
- Geomagnetism
- Geomorphology
- Geophysics
- Glacier
- Glaciology
- Granite
- Historical geology
- Hominids
- Hydrogeology
- Ice
- Igneous
- Igneous rock
- Infrastructure
- Intrusion
- Iron
- Iron Age
- Laboratory
- Latin
- Lava
- Limestone
- List of rock types
- Lithic technology
- Lithosphere
- Magma
- Mantle (geology)
- Mass wasting
- Matter
- Metal
- Metamorphic rock
- Metamorphism
- Mineral
- Mineralogy
- Mineraloid
- Mining
- Moab, Utah
- Mongolia
- Mudstone
- Natural gas
- Oceanography
- Oil shale
- Oldest rock
- Ore
- Organic matter
- Orosí
- Outline of geology
- Ovoo
- Paleoclimatology
- Paleolithic
- Paleontology
- Petrography
- Petroleum
- Petrology
- Planet
- Plate tectonics
- Pluton
- Plutonic
- Potash
- Precious metals
- Prehistory
- Pressure
- Prospecting
- Protolith
- Public domain
- Pumice
- Quarry
- Riprap
- Rock (geology)
- Rock balancing
- Rock cycle
- Sandstone
- Sediment
- Sedimentary
- Sedimentary rock
- Sedimentation
- Seismology
- Shale
- Siltstone
- Sodium chloride
- Solution
- Stone Age
- Stratigraphy
- Structural geology
- Tectonophysics
- Temperature
- Template Geology
- Texture (geology)
- Uranium
- Value (economics)
- Vein (geology)
- Volcanic rock
- Water
- Weathering
- Wind
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Basics of Geology All About Rocks and Minerals
Basics of Geology All About Rocks and MineralsBasics of Geology All About Rocks and Minerals
-
Living Rock An Introduction to Earths Geology
Living Rock An Introduction to Earths GeologyLiving Rock An Introduction to Earths Geology
US Survey series. -
Geology Kitchen: The 3 Types of Rocks
Geology Kitchen: The 3 Types of RocksGeology Kitchen: The 3 Types of Rocks
http://explorermultimedia.org/ Geologist Devin Dennie heads to the kitchen to demonstrate the differences between the three types of rocks. -
BBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep TimeBBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time - Iain Stewart tells the story of James Hutton, the founding father of geology. Uploaded for educational purposes, all mater... -
Geology Rocks Song Practice
Geology Rocks Song PracticeGeology Rocks Song Practice
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through! 1. Professor Rock Has Disappeared 0:07 2. Geologic Time 2:26 3. I Ain't Well 4:24 4. I Am Deep 6:27 5. Oh to be a Fossil Fuel 8:04 6. Erosion 10:24 7. Love Them Plates 12:28 8. Seven Little Miners 14:26 9. Rock Cycle 16:22 10. Professor Rock Has Re-Appeared 18:35 Ready to practice on your own? Click here for instruments only: https://youtu.be/C2zqW_3zqIs These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole -
Basic Rock Identification: Geology
Basic Rock Identification: GeologyBasic Rock Identification: Geology
Visual Study Aid for Physical/Historical Geology Classes. MUSIC: "DISTANCE" by Soilwork, from the "Stabbing the Drama" album. -
Geology for IDiots Episode 1 Rocks Part 2
Geology for IDiots Episode 1 Rocks Part 2Geology for IDiots Episode 1 Rocks Part 2
Part 2 of Episode 1 Geology for IDiots with this episode focusing on Rocks My Blog as Promised: http://hochemon2008.blogspot.com/ Any questions comments or c... -
Fossil Rock Anthem
Fossil Rock AnthemFossil Rock Anthem
Explain/annotate the lyrics on rap genius: http://rapgenius.com/Tom-mcfadden-fossil-rock-anthem-lyrics The song parodies "Party Rock Anthem" by LMFAO. The instrumental was made by DJ Lisan (www.soundcloud.com/dj-lisan) in San Francisco. Female vocals by Nicole Bonsol. Male vocals and lyrics and the animated video by me. Mastered by Hank Kalleen (Ear Jerker). The song covers the California 7th grade standards on Earth & life history. The song and video are part of thesis I'm doing about the impact of music in science education as part of a Master of Science Communication at the University Otago in New Zealand (which began thanks to a Fulbri -
Rock and Mineral Identification
Rock and Mineral IdentificationRock and Mineral Identification
A study guide made for the students of Fleming College in Lindsay Ontario Canada and anybody else who might find it useful. If you like this video check out ... -
Geology Kitchen #3 - Clastic Sedimentary Rocks
Geology Kitchen #3 - Clastic Sedimentary RocksGeology Kitchen #3 - Clastic Sedimentary Rocks
Episode 3 begins to examine the world of sedimentary rocks by looking at how clastic sedimentary rocks form. Various food stuffs of different grain sizes are... -
GEOLOGY ROCKS! (Jasongs)
GEOLOGY ROCKS! (Jasongs)GEOLOGY ROCKS! (Jasongs)
A true "rock" song. Check out the CD quality, stereo version along with a host of other great songs at: http://www.cdbaby.com/jasongs3 itunes, amazon.com LYR... -
Geology, the rock cycle
Geology, the rock cycleGeology, the rock cycle
the rock cycle. -
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Geology Kitchen #5 - Chemical & Biological Sedimentary RocksGeology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Chemical and biological sedimentary rocks are discussed in this video. Carbonates, including limestones and dolomites are discussed, and cave stalactites are made. Evaporites are made in pan on stove experiment, and coal and chert are also examined as other forms of sedimentary rock. This episode is to be paired with the "Clastic Rocks" episode for a complete review of the sedimentary rock types. -
Geology Kitchen #11 - Igneous Rocks
Geology Kitchen #11 - Igneous RocksGeology Kitchen #11 - Igneous Rocks
Igneous rocks are rocks derived from the cooling of magma, molten material originating from the upper Mantle/lower crust. Igneous rocks are classified by the... -
Geology
GeologyGeology
003 - Geology In this video Paul Andersen explains how rock is formed and changed on the planet. The video begins with a brief description of rocks, minerals, and the rock cycle. Plate tectonics is used to describe structure near plate boundaries. Hot spots and natural hazards (like volcanos, earthquake, and tsunamis) are included. Do you speak another language? Help me translate my videos: http://www.bozemanscience.com/translations/ Music Attribution Intro Title: I4dsong_loop_main.wav Artist: CosmicD Link to sound: http://www.freesound.org/people/CosmicD/sounds/72556/ Creative Commons Atribution License Outro Title: String Theory A -
1 05 Petroleum Geology 5 & 6 Reservoir rock properties & Trapping
1 05 Petroleum Geology 5 & 6 Reservoir rock properties & Trapping1 05 Petroleum Geology 5 & 6 Reservoir rock properties & Trapping
-
Geology Rocks @ Maude Price part 1
Geology Rocks @ Maude Price part 1Geology Rocks @ Maude Price part 1
Geology Rocks Musical Play at Maude Price elementary 6.19.2013. -
25 Strangest Geological Formations On Earth
25 Strangest Geological Formations On Earth25 Strangest Geological Formations On Earth
Tweet this video! - http://clicktotweet.com/aVUcD Earth is a big place with a lot of unique flora and fauna, and as strange as it can already be there are st... -
Crossrail Geology: Soil & rock core samples stored 150 metres below Cheshire
Crossrail Geology: Soil & rock core samples stored 150 metres below CheshireCrossrail Geology: Soil & rock core samples stored 150 metres below Cheshire
Crossrail, Europe’s largest infrastructure project, is using one of the UK’s unique underground spaces – a natural, climate controlled storage facility at the UK’s largest salt mine in Cheshire, to store thousands of soil and rock cores from beneath London. The soil and rock cores at DeepStore in Winsford include London Clay, sands and clays of the Lambeth Group, Thanet Sands and Chalk. They tell the story of how geological activity has shaped the earth on which London sits covering a time span of about 35 million years. The oldest Crossrail core is 80 million years old. Mike Black, Crossrail’s Head of Geotechnics said: “These soil and rock -
Geology Kitchen #4 - Metamorphism
Geology Kitchen #4 - MetamorphismGeology Kitchen #4 - Metamorphism
This episode explores the concepts of regional versus contact metamorphism. Heat and pressure are discussed and their roles in changing various rock types in... -
New Haven Elementary 4th Grade Play - Geology Rocks!: Professor Rock is Missing....
New Haven Elementary 4th Grade Play - Geology Rocks!: Professor Rock is Missing....New Haven Elementary 4th Grade Play - Geology Rocks!: Professor Rock is Missing....
-
Geology, The Study of Rock
Geology, The Study of RockGeology, The Study of Rock
Genoa Middle School 6th Grade 2012 Spring/End-of-Year Concert. -
Identifying Igneous Rocks -- Earth Rocks!
Identifying Igneous Rocks -- Earth Rocks!Identifying Igneous Rocks -- Earth Rocks!
A review of igneous rock identification -- as presented for an introductory level Physical Geology class. Version with embedded feedback quizzes and closed-c...
Basics of Geology All About Rocks and Minerals
- Order: Reorder
- Duration: 23:20
- Updated: 09 Mar 2014
- published: 09 Mar 2014
- views: 23594
Living Rock An Introduction to Earths Geology
- Order: Reorder
- Duration: 57:06
- Updated: 02 Sep 2014
- author: Martin Diker
US Survey series.
wn.com/Living Rock An Introduction To Earths Geology
US Survey series.
- published: 03 Jun 2014
- views: 2151
- author: Martin Diker
Geology Kitchen: The 3 Types of Rocks
http://explorermultimedia.org/ Geologist Devin Dennie heads to the kitchen to demonstrate the differences between the three types of rocks.
wn.com/Geology Kitchen The 3 Types Of Rocks
http://explorermultimedia.org/ Geologist Devin Dennie heads to the kitchen to demonstrate the differences between the three types of rocks.
- published: 03 Sep 2011
- views: 112938
- author: tkent22
BBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time - Iain Stewart tells the story of James Hutton, the founding father of geology. Uploaded for educational purposes, all mater...
wn.com/BBC Men Of Rock 1 Of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time - Iain Stewart tells the story of James Hutton, the founding father of geology. Uploaded for educational purposes, all mater...
- published: 31 Oct 2012
- views: 56685
- author: xMaTx4
Geology Rocks Song Practice
- Order: Reorder
- Duration: 20:45
- Updated: 17 May 2015
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through!
1. Professor Rock Has Disappeared 0:07
2. Geologic Time 2:26
3. I Ain't Well 4:24
4. I Am Deep 6:27
5. Oh to be a Fossil Fuel 8:04
6. Erosion 10:24
7. Love Them Plates 12:28
8. Seven Little Miners 14:26
9. Rock Cycle 16:22
10. Professor Rock Has Re-Appeared 18:35
Ready to practice on your own? Click here for instruments only:
https://youtu.be/C2zqW_3zqIs
These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole purpose of this video is for students to practice the song portions of this musical.
wn.com/Geology Rocks Song Practice
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through!
1. Professor Rock Has Disappeared 0:07
2. Geologic Time 2:26
3. I Ain't Well 4:24
4. I Am Deep 6:27
5. Oh to be a Fossil Fuel 8:04
6. Erosion 10:24
7. Love Them Plates 12:28
8. Seven Little Miners 14:26
9. Rock Cycle 16:22
10. Professor Rock Has Re-Appeared 18:35
Ready to practice on your own? Click here for instruments only:
https://youtu.be/C2zqW_3zqIs
These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole purpose of this video is for students to practice the song portions of this musical.
- published: 17 May 2015
- views: 8
Basic Rock Identification: Geology
- Order: Reorder
- Duration: 7:13
- Updated: 05 Sep 2014
- author: devildogmre
Visual Study Aid for Physical/Historical Geology Classes. MUSIC: "DISTANCE" by Soilwork, from the "Stabbing the Drama" album.
wn.com/Basic Rock Identification Geology
Visual Study Aid for Physical/Historical Geology Classes. MUSIC: "DISTANCE" by Soilwork, from the "Stabbing the Drama" album.
- published: 09 Nov 2007
- views: 146443
- author: devildogmre
Geology for IDiots Episode 1 Rocks Part 2
- Order: Reorder
- Duration: 9:17
- Updated: 12 Aug 2014
- author: Hochemon2008
Part 2 of Episode 1 Geology for IDiots with this episode focusing on Rocks My Blog as Promised: http://hochemon2008.blogspot.com/ Any questions comments or c...
wn.com/Geology For Idiots Episode 1 Rocks Part 2
Part 2 of Episode 1 Geology for IDiots with this episode focusing on Rocks My Blog as Promised: http://hochemon2008.blogspot.com/ Any questions comments or c...
- published: 22 Apr 2009
- views: 34563
- author: Hochemon2008
Fossil Rock Anthem
- Order: Reorder
- Duration: 3:16
- Updated: 22 Oct 2012
Explain/annotate the lyrics on rap genius: http://rapgenius.com/Tom-mcfadden-fossil-rock-anthem-lyrics
The song parodies "Party Rock Anthem" by LMFAO. The instrumental was made by DJ Lisan (www.soundcloud.com/dj-lisan) in San Francisco. Female vocals by Nicole Bonsol. Male vocals and lyrics and the animated video by me. Mastered by Hank Kalleen (Ear Jerker).
The song covers the California 7th grade standards on Earth & life history. The song and video are part of thesis I'm doing about the impact of music in science education as part of a Master of Science Communication at the University Otago in New Zealand (which began thanks to a Fulbright scholarship). Data on the song's impact are pretty interesting.
I've also made an accompanying eBook that explains the science in a bit more depth, including why "they're the schist" has an * (hint: schist is a metamorphic rock). I haven't figured out whether to release the PDF to internet yet, but if you're interested in using it for educational purposes, send me a YouTube message.
Thanks to Jessica Hinojosa & Jens Lund Snee for geology consultation, Alex Lubransky for dance consultation, and Andrew Scott for green screen consultation.
wn.com/Fossil Rock Anthem
Explain/annotate the lyrics on rap genius: http://rapgenius.com/Tom-mcfadden-fossil-rock-anthem-lyrics
The song parodies "Party Rock Anthem" by LMFAO. The instrumental was made by DJ Lisan (www.soundcloud.com/dj-lisan) in San Francisco. Female vocals by Nicole Bonsol. Male vocals and lyrics and the animated video by me. Mastered by Hank Kalleen (Ear Jerker).
The song covers the California 7th grade standards on Earth & life history. The song and video are part of thesis I'm doing about the impact of music in science education as part of a Master of Science Communication at the University Otago in New Zealand (which began thanks to a Fulbright scholarship). Data on the song's impact are pretty interesting.
I've also made an accompanying eBook that explains the science in a bit more depth, including why "they're the schist" has an * (hint: schist is a metamorphic rock). I haven't figured out whether to release the PDF to internet yet, but if you're interested in using it for educational purposes, send me a YouTube message.
Thanks to Jessica Hinojosa & Jens Lund Snee for geology consultation, Alex Lubransky for dance consultation, and Andrew Scott for green screen consultation.
- published: 22 Oct 2012
- views: 460343
Rock and Mineral Identification
- Order: Reorder
- Duration: 19:17
- Updated: 06 Sep 2014
- author: SSFCstudybuddy
A study guide made for the students of Fleming College in Lindsay Ontario Canada and anybody else who might find it useful. If you like this video check out ...
wn.com/Rock And Mineral Identification
A study guide made for the students of Fleming College in Lindsay Ontario Canada and anybody else who might find it useful. If you like this video check out ...
- published: 06 Feb 2012
- views: 140761
- author: SSFCstudybuddy
Geology Kitchen #3 - Clastic Sedimentary Rocks
Episode 3 begins to examine the world of sedimentary rocks by looking at how clastic sedimentary rocks form. Various food stuffs of different grain sizes are...
wn.com/Geology Kitchen 3 Clastic Sedimentary Rocks
Episode 3 begins to examine the world of sedimentary rocks by looking at how clastic sedimentary rocks form. Various food stuffs of different grain sizes are...
- published: 31 Aug 2012
- views: 15706
- author: tkent22
GEOLOGY ROCKS! (Jasongs)
- Order: Reorder
- Duration: 3:34
- Updated: 28 Aug 2014
- author: Jason Arvanites
A true "rock" song. Check out the CD quality, stereo version along with a host of other great songs at: http://www.cdbaby.com/jasongs3 itunes, amazon.com LYR...
wn.com/Geology Rocks (Jasongs)
A true "rock" song. Check out the CD quality, stereo version along with a host of other great songs at: http://www.cdbaby.com/jasongs3 itunes, amazon.com LYR...
- published: 15 May 2009
- views: 28834
- author: Jason Arvanites
Geology, the rock cycle
the rock cycle.
wn.com/Geology, The Rock Cycle
the rock cycle.
- published: 16 Oct 2008
- views: 10692
- author: John West
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
- Order: Reorder
- Duration: 5:51
- Updated: 01 Oct 2012
Chemical and biological sedimentary rocks are discussed in this video. Carbonates, including limestones and dolomites are discussed, and cave stalactites are made. Evaporites are made in pan on stove experiment, and coal and chert are also examined as other forms of sedimentary rock. This episode is to be paired with the "Clastic Rocks" episode for a complete review of the sedimentary rock types.
wn.com/Geology Kitchen 5 Chemical Biological Sedimentary Rocks
Chemical and biological sedimentary rocks are discussed in this video. Carbonates, including limestones and dolomites are discussed, and cave stalactites are made. Evaporites are made in pan on stove experiment, and coal and chert are also examined as other forms of sedimentary rock. This episode is to be paired with the "Clastic Rocks" episode for a complete review of the sedimentary rock types.
- published: 01 Oct 2012
- views: 9711
Geology Kitchen #11 - Igneous Rocks
Igneous rocks are rocks derived from the cooling of magma, molten material originating from the upper Mantle/lower crust. Igneous rocks are classified by the...
wn.com/Geology Kitchen 11 Igneous Rocks
Igneous rocks are rocks derived from the cooling of magma, molten material originating from the upper Mantle/lower crust. Igneous rocks are classified by the...
- published: 04 Feb 2013
- views: 11319
- author: tkent22
Geology
- Order: Reorder
- Duration: 11:04
- Updated: 31 Aug 2015
003 - Geology
In this video Paul Andersen explains how rock is formed and changed on the planet. The video begins with a brief description of rocks, minerals, and the rock cycle. Plate tectonics is used to describe structure near plate boundaries. Hot spots and natural hazards (like volcanos, earthquake, and tsunamis) are included.
Do you speak another language? Help me translate my videos:
http://www.bozemanscience.com/translations/
Music Attribution
Intro
Title: I4dsong_loop_main.wav
Artist: CosmicD
Link to sound: http://www.freesound.org/people/CosmicD/sounds/72556/
Creative Commons Atribution License
Outro
Title: String Theory
Artist: Herman Jolly
http://sunsetvalley.bandcamp.com/track/string-theory
All of the images are licensed under creative commons and public domain licensing:
Benbennick, David. English: This Is a Locator Map Showing Kalawao County in Hawaii. For More Information, See Commons:United States County Locator Maps., February 12, 2006. Own work: English: The maps use data from nationalatlas.gov, specifically countyp020.tar.gz on the Raw Data Download page. The maps also use state outline data from statesp020.tar.gz. The Florida maps use hydrogm020.tar.gz to display Lake Okeechobee. https://commons.wikimedia.org/wiki/File:Map_of_Hawaii_highlighting_Kalawao_County.svg.
“Earth.” Wikipedia, the Free Encyclopedia, August 23, 2015. https://en.wikipedia.org/w/index.php?title=Earth&oldid;=677456791.
File:Hawaiien (volcano).svg, n.d. https://commons.wikimedia.org/wiki/File:Hawaiien_(volcano).svg.
File:Structure Volcano Unlabeled.svg, n.d. https://commons.wikimedia.org/wiki/File:Structure_volcano_unlabeled.svg.
Fir0002. A Diagram of the Rock Cycle That Is Modified off of Rockcycle.jpg by User:Woudloper. The Changes Made to This Photo Were Made according to the Conversation at Where the Original Is Being Nominated for Featured Picture Status. It Is Very Important That You Change the Chance of You Getting a Rock of Bandshoe Very Rare Rock Very Costly Too There Are Only 3 Every like It in the World and It Costs 3 Gold Mines and the Mountains Ontop of Them., February 10, 2008. Own work. https://commons.wikimedia.org/wiki/File:Rockcycle_edit.jpg.
“Gneiss.” Wikipedia, the Free Encyclopedia, July 29, 2015. https://en.wikipedia.org/w/index.php?title=Gneiss&oldid;=673627696.
Gringer. English: SVG Version of File:Pacific_Ring_of_Fire.png, Recreated by Me Using WDB Vector Data Using Code Mentioned in File:Worldmap_wdb_combined.svg., February 11, 2009. vector data from [1]. https://commons.wikimedia.org/wiki/File:Pacific_Ring_of_Fire.svg.
H.Stauffer, Brian F. Atwater, Marco Cisternas V. , Joanne Bourgeois, Walter C. Dudley, James W. Hendley II, and Peter. English: Vertical Slice Through a Subduction Zone, 1999. U.S. Geological Survey, Circular 1187 (http://pubs.usgs.gov/circ/c1187/illustrations/BlockDigrm_1.ai). https://commons.wikimedia.org/wiki/File:Eq-gen1.svg.
Karta24. Français : Trois Différents Types de Faille, January 20, 2008. http://earthquake.usgs.gov/learn/glossary/?term=fault earthquake.usgs.gov. https://commons.wikimedia.org/wiki/File:Fault_types.svg.
Khruner. English: commons.wikimedia.org/wiki/File:Rocks_-_Pink_granite_Baveno.JPG.
“Landslide.” Wikipedia, the Free Encyclopedia, August 27, 2015. https://en.wikipedia.org/w/index.php?title=Landslide&oldid;=678171434.
“Landslide.” Wikipedia, the Free Encyclopedia, August 27, 2015. https://en.wikipedia.org/w/index.php?title=Landslide&oldid;=678171434.
“Mount St. Helens.” Wikipedia, the Free Encyclopedia, August 8, 2015. https://en.wikipedia.org/w/index.php?title=Mount_St._Helens&oldid;=675148427.
“Plate Tectonics.” Wikipedia, the Free Encyclopedia, August 17, 2015. https://en.wikipedia.org/w/index.php?title=Plate_tectonics&oldid;=676450570.
“Ring of Fire.” Wikipedia, the Free Encyclopedia, August 20, 2015. https://en.wikipedia.org/w/index.php?title=Ring_of_Fire&oldid;=676950168.
“Tsunami.” Wikipedia, the Free Encyclopedia, July 19, 2015. https://en.wikipedia.org/w/index.php?title=Tsunami&oldid;=672137584.
User:Moondigger. Inside Lower Antelope Canyon, Looking out with the Sky near the Top of the Frame. Characteristic Layering in the Sandstone Is Visible., April 16, 2005. Own work. https://commons.wikimedia.org/wiki/File:Lower_antelope_3_md.jpg.
USGS, derivative work: AnasofiapaixaoEarth_internal_structure png: English: Cutaway Diagram of Earth’s Internal Structure (to Scale) with Inset Showing Detailed Breakdown of Structure (not to Scale), April 27, 2013. Earth_internal_structure.png. https://commons.wikimedia.org/wiki/File:Earth-cutaway-schematic-english.svg.Own work. https://commons.wikimedia.org/wiki/File:Halema%27uma%27u_Crater_in_Kilauea_volcano,_Hawaii..jpg.
wn.com/Geology
003 - Geology
In this video Paul Andersen explains how rock is formed and changed on the planet. The video begins with a brief description of rocks, minerals, and the rock cycle. Plate tectonics is used to describe structure near plate boundaries. Hot spots and natural hazards (like volcanos, earthquake, and tsunamis) are included.
Do you speak another language? Help me translate my videos:
http://www.bozemanscience.com/translations/
Music Attribution
Intro
Title: I4dsong_loop_main.wav
Artist: CosmicD
Link to sound: http://www.freesound.org/people/CosmicD/sounds/72556/
Creative Commons Atribution License
Outro
Title: String Theory
Artist: Herman Jolly
http://sunsetvalley.bandcamp.com/track/string-theory
All of the images are licensed under creative commons and public domain licensing:
Benbennick, David. English: This Is a Locator Map Showing Kalawao County in Hawaii. For More Information, See Commons:United States County Locator Maps., February 12, 2006. Own work: English: The maps use data from nationalatlas.gov, specifically countyp020.tar.gz on the Raw Data Download page. The maps also use state outline data from statesp020.tar.gz. The Florida maps use hydrogm020.tar.gz to display Lake Okeechobee. https://commons.wikimedia.org/wiki/File:Map_of_Hawaii_highlighting_Kalawao_County.svg.
“Earth.” Wikipedia, the Free Encyclopedia, August 23, 2015. https://en.wikipedia.org/w/index.php?title=Earth&oldid;=677456791.
File:Hawaiien (volcano).svg, n.d. https://commons.wikimedia.org/wiki/File:Hawaiien_(volcano).svg.
File:Structure Volcano Unlabeled.svg, n.d. https://commons.wikimedia.org/wiki/File:Structure_volcano_unlabeled.svg.
Fir0002. A Diagram of the Rock Cycle That Is Modified off of Rockcycle.jpg by User:Woudloper. The Changes Made to This Photo Were Made according to the Conversation at Where the Original Is Being Nominated for Featured Picture Status. It Is Very Important That You Change the Chance of You Getting a Rock of Bandshoe Very Rare Rock Very Costly Too There Are Only 3 Every like It in the World and It Costs 3 Gold Mines and the Mountains Ontop of Them., February 10, 2008. Own work. https://commons.wikimedia.org/wiki/File:Rockcycle_edit.jpg.
“Gneiss.” Wikipedia, the Free Encyclopedia, July 29, 2015. https://en.wikipedia.org/w/index.php?title=Gneiss&oldid;=673627696.
Gringer. English: SVG Version of File:Pacific_Ring_of_Fire.png, Recreated by Me Using WDB Vector Data Using Code Mentioned in File:Worldmap_wdb_combined.svg., February 11, 2009. vector data from [1]. https://commons.wikimedia.org/wiki/File:Pacific_Ring_of_Fire.svg.
H.Stauffer, Brian F. Atwater, Marco Cisternas V. , Joanne Bourgeois, Walter C. Dudley, James W. Hendley II, and Peter. English: Vertical Slice Through a Subduction Zone, 1999. U.S. Geological Survey, Circular 1187 (http://pubs.usgs.gov/circ/c1187/illustrations/BlockDigrm_1.ai). https://commons.wikimedia.org/wiki/File:Eq-gen1.svg.
Karta24. Français : Trois Différents Types de Faille, January 20, 2008. http://earthquake.usgs.gov/learn/glossary/?term=fault earthquake.usgs.gov. https://commons.wikimedia.org/wiki/File:Fault_types.svg.
Khruner. English: commons.wikimedia.org/wiki/File:Rocks_-_Pink_granite_Baveno.JPG.
“Landslide.” Wikipedia, the Free Encyclopedia, August 27, 2015. https://en.wikipedia.org/w/index.php?title=Landslide&oldid;=678171434.
“Landslide.” Wikipedia, the Free Encyclopedia, August 27, 2015. https://en.wikipedia.org/w/index.php?title=Landslide&oldid;=678171434.
“Mount St. Helens.” Wikipedia, the Free Encyclopedia, August 8, 2015. https://en.wikipedia.org/w/index.php?title=Mount_St._Helens&oldid;=675148427.
“Plate Tectonics.” Wikipedia, the Free Encyclopedia, August 17, 2015. https://en.wikipedia.org/w/index.php?title=Plate_tectonics&oldid;=676450570.
“Ring of Fire.” Wikipedia, the Free Encyclopedia, August 20, 2015. https://en.wikipedia.org/w/index.php?title=Ring_of_Fire&oldid;=676950168.
“Tsunami.” Wikipedia, the Free Encyclopedia, July 19, 2015. https://en.wikipedia.org/w/index.php?title=Tsunami&oldid;=672137584.
User:Moondigger. Inside Lower Antelope Canyon, Looking out with the Sky near the Top of the Frame. Characteristic Layering in the Sandstone Is Visible., April 16, 2005. Own work. https://commons.wikimedia.org/wiki/File:Lower_antelope_3_md.jpg.
USGS, derivative work: AnasofiapaixaoEarth_internal_structure png: English: Cutaway Diagram of Earth’s Internal Structure (to Scale) with Inset Showing Detailed Breakdown of Structure (not to Scale), April 27, 2013. Earth_internal_structure.png. https://commons.wikimedia.org/wiki/File:Earth-cutaway-schematic-english.svg.Own work. https://commons.wikimedia.org/wiki/File:Halema%27uma%27u_Crater_in_Kilauea_volcano,_Hawaii..jpg.
- published: 31 Aug 2015
- views: 430
1 05 Petroleum Geology 5 & 6 Reservoir rock properties & Trapping
- Order: Reorder
- Duration: 94:10
- Updated: 31 Aug 2014
- author: tawkaw OpenCourseWare
- published: 06 Jun 2014
- views: 169
- author: tawkaw OpenCourseWare
Geology Rocks @ Maude Price part 1
- Order: Reorder
- Duration: 14:38
- Updated: 31 May 2014
- author: yanadane soriano
Geology Rocks Musical Play at Maude Price elementary 6.19.2013.
wn.com/Geology Rocks Maude Price Part 1
Geology Rocks Musical Play at Maude Price elementary 6.19.2013.
- published: 22 Jun 2013
- views: 1593
- author: yanadane soriano
25 Strangest Geological Formations On Earth
Tweet this video! - http://clicktotweet.com/aVUcD Earth is a big place with a lot of unique flora and fauna, and as strange as it can already be there are st...
wn.com/25 Strangest Geological Formations On Earth
Tweet this video! - http://clicktotweet.com/aVUcD Earth is a big place with a lot of unique flora and fauna, and as strange as it can already be there are st...
- published: 26 Jul 2013
- views: 489940
- author: list25
Crossrail Geology: Soil & rock core samples stored 150 metres below Cheshire
- Order: Reorder
- Duration: 3:59
- Updated: 04 Sep 2015
Crossrail, Europe’s largest infrastructure project, is using one of the UK’s unique underground spaces – a natural, climate controlled storage facility at the UK’s largest salt mine in Cheshire, to store thousands of soil and rock cores from beneath London.
The soil and rock cores at DeepStore in Winsford include London Clay, sands and clays of the Lambeth Group, Thanet Sands and Chalk. They tell the story of how geological activity has shaped the earth on which London sits covering a time span of about 35 million years. The oldest Crossrail core is 80 million years old.
Mike Black, Crossrail’s Head of Geotechnics said: “These soil and rock cores played a crucial role in the Crossrail project as they allowed us to build up a detailed picture of the ground conditions below London. The information gained from them can be used by future London tunnelling projects.”
Once removed from the ground, the soil and rock cores lose moisture and slowly deteriorate. The cores at DeepStore are contained 150 metres underground at a consistent humidity level and an ambient temperature of 15 degrees Celsius. This prevents deterioration without the use of a temperature controlled warehouse.
Beginning in 1992, before Crossrail construction began in 2009, comprehensive ground investigations were undertaken where these soil and rock cores were extracted from over 1,400 boreholes along the Crossrail route at depths of up to 70 metres.
Each core was carefully examined, tested and entered into Crossrail’s Geographic Information System (GIS) to provide essential data for the designs of all Crossrail tunnels, portals and shafts and ensured that Crossrail could complete the excavation for the tunnels and stations safely, with minimal subsidence risk to the buildings and infrastructure above.
The awe inspiring space below ground at DeepStore was created when millions of tonnes of salt were excavated from Compass Minerals UK's rock salt mine. DeepStore is now home to 1.8 million square metres of storage space - the equivalent of over 700 football pitches in size.
For more information visit:
http://www.crossrail.co.uk/news/articles/35-million-years-of-londons-geology-preserved-150-metres-underground-in-cheshire
http://www.crossrail.co.uk/
wn.com/Crossrail Geology Soil Rock Core Samples Stored 150 Metres Below Cheshire
Crossrail, Europe’s largest infrastructure project, is using one of the UK’s unique underground spaces – a natural, climate controlled storage facility at the UK’s largest salt mine in Cheshire, to store thousands of soil and rock cores from beneath London.
The soil and rock cores at DeepStore in Winsford include London Clay, sands and clays of the Lambeth Group, Thanet Sands and Chalk. They tell the story of how geological activity has shaped the earth on which London sits covering a time span of about 35 million years. The oldest Crossrail core is 80 million years old.
Mike Black, Crossrail’s Head of Geotechnics said: “These soil and rock cores played a crucial role in the Crossrail project as they allowed us to build up a detailed picture of the ground conditions below London. The information gained from them can be used by future London tunnelling projects.”
Once removed from the ground, the soil and rock cores lose moisture and slowly deteriorate. The cores at DeepStore are contained 150 metres underground at a consistent humidity level and an ambient temperature of 15 degrees Celsius. This prevents deterioration without the use of a temperature controlled warehouse.
Beginning in 1992, before Crossrail construction began in 2009, comprehensive ground investigations were undertaken where these soil and rock cores were extracted from over 1,400 boreholes along the Crossrail route at depths of up to 70 metres.
Each core was carefully examined, tested and entered into Crossrail’s Geographic Information System (GIS) to provide essential data for the designs of all Crossrail tunnels, portals and shafts and ensured that Crossrail could complete the excavation for the tunnels and stations safely, with minimal subsidence risk to the buildings and infrastructure above.
The awe inspiring space below ground at DeepStore was created when millions of tonnes of salt were excavated from Compass Minerals UK's rock salt mine. DeepStore is now home to 1.8 million square metres of storage space - the equivalent of over 700 football pitches in size.
For more information visit:
http://www.crossrail.co.uk/news/articles/35-million-years-of-londons-geology-preserved-150-metres-underground-in-cheshire
http://www.crossrail.co.uk/
- published: 04 Sep 2015
- views: 191
Geology Kitchen #4 - Metamorphism
This episode explores the concepts of regional versus contact metamorphism. Heat and pressure are discussed and their roles in changing various rock types in...
wn.com/Geology Kitchen 4 Metamorphism
This episode explores the concepts of regional versus contact metamorphism. Heat and pressure are discussed and their roles in changing various rock types in...
- published: 24 Sep 2012
- views: 10371
- author: tkent22
New Haven Elementary 4th Grade Play - Geology Rocks!: Professor Rock is Missing....
- Order: Reorder
- Duration: 11:56
- Updated: 20 Jul 2014
- author: Toni Wade Noble
- published: 19 Apr 2013
- views: 834
- author: Toni Wade Noble
Geology, The Study of Rock
- Order: Reorder
- Duration: 3:05
- Updated: 01 Aug 2014
- author: Michael McGee
Genoa Middle School 6th Grade 2012 Spring/End-of-Year Concert.
wn.com/Geology, The Study Of Rock
Genoa Middle School 6th Grade 2012 Spring/End-of-Year Concert.
- published: 17 May 2012
- views: 1523
- author: Michael McGee
Identifying Igneous Rocks -- Earth Rocks!
- Order: Reorder
- Duration: 20:17
- Updated: 05 Sep 2014
- author: Earth Rocks!
A review of igneous rock identification -- as presented for an introductory level Physical Geology class. Version with embedded feedback quizzes and closed-c...
wn.com/Identifying Igneous Rocks Earth Rocks
A review of igneous rock identification -- as presented for an introductory level Physical Geology class. Version with embedded feedback quizzes and closed-c...
- published: 26 Jun 2014
- views: 79
- author: Earth Rocks!
-
Rock cycle - geology for kids
Rock cycle - geology for kidsRock cycle - geology for kids
-
Books of Sedimentary Rock Geology Rocks
Books of Sedimentary Rock Geology RocksBooks of Sedimentary Rock Geology Rocks
Access to read more ebook: http://www.realbooknow.net/books -
Rock-Rock
Rock-RockRock-Rock
This video is just to show the different components of the game Rock-Rock. How to play Rock-Rock: 1. Start with a large rock for the base of game-play. 2. Throw medium sized rocks at the base rock, trying to have it land on the base rock (this is where the video starts). This is the Rock-Rock. 2 points are awarded for sticking the Rock-Rock landing. 3. Throw small pebbles (fine gravel) at the rock-rock to try to knock it off the base-rock. 4 points are awarded for knocking off the Rock-Rock, 3 bonus points if the rock you threw knocks off the Rock-Rock and remains on the base-rock. This rock becomes the new Rock-Rock. If no rocks remain on -
Rock Cycle - Geology For Kids - Learn about Rock
Rock Cycle - Geology For Kids - Learn about RockRock Cycle - Geology For Kids - Learn about Rock
The Rock Cycle is a group of changes. Igneous rock can change into sedimentary rock or into metamorphic rock. Sedimentary rock can change into metamorphic rock or into igneous rock. Metamorphic rock can change into igneous or sedimentary rock. Igneous rock forms when magma cools and makes crystals. Magma is a hot liquid made of melted minerals. The minerals can form crystals when they cool. Igneous rock can form underground, where the magma cools slowly. Or, igneous rock can form above ground, where the magma cools quickly. When it pours out on Earth's surface, magma is called lava. Yes, the same liquid rock matter that you see coming out o -
Geology for Engineers Sedimentary Rocks & Processes
Geology for Engineers Sedimentary Rocks & ProcessesGeology for Engineers Sedimentary Rocks & Processes
Describes the processes that form sedimentary rocks and the classification of sedimentary rocks. This lecture also covers depositional environments and sedimentary structures. -
Geology Rock Cycle Project
Geology Rock Cycle ProjectGeology Rock Cycle Project
-
Identification of fold structures in Sandstone and Shales - Geology Field Trip
Identification of fold structures in Sandstone and Shales - Geology Field TripIdentification of fold structures in Sandstone and Shales - Geology Field Trip
Location: Beach to the west of Long Shank. Description: Sand and rock beach with small stack (Davie's Rock). Geology: anticline cut by intrusions. -
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip GeologyRock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
Location: Rocky foreshore below St Monans Church. Description: Rock platform below Fife Coast Path. Geology: Later dyke cross-cutting the St Monans Neck -
THE ROCK CYCLE GEOLOGY
THE ROCK CYCLE GEOLOGYTHE ROCK CYCLE GEOLOGY
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THE ROCK CYCLE GEOLOGY
THE ROCK CYCLE GEOLOGYTHE ROCK CYCLE GEOLOGY
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Geology of Raven Rock Arch
Geology of Raven Rock ArchGeology of Raven Rock Arch
Geologist Brittany Parrick provides a brief discussion on the geology of Raven Rock Arch in Scioto County, Ohio. Also included is a short explanation of how the Teays River Valley and Ohio River were shaped by glaciers during the Ice Age. -
okayest geology presentation
okayest geology presentationokayest geology presentation
The Rock Cycle by Levi Hanson, Cole Kyllonen, and Tristan Durfee -
Geology Rock Cycle
Geology Rock CycleGeology Rock Cycle
Geology 1120-90 Mercedes Isensee Ningozis White Juliet McLellan Raymond Klitsch Cassandra Deloney -
Engineering Geology Rock in Engineering Construction
Engineering Geology Rock in Engineering ConstructionEngineering Geology Rock in Engineering Construction
Register to Browse more Ebooks Get it Now at : http://mgpdf.net/free -
Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]
Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]
A variety of diverse morphological features are present in this image (21 by 5.5 kilometers) located in the southeastern area of the Nili Fossae region and just northeast of Syrtis Major. This particular region has been studied intensely due to the presence of volcanics from Syrtis Major and impact ejecta from the Isidis Basin. The region is rich in unaltered mafic deposits, in contact with diverse altered deposits rich in clays, carbonates, and sulfates. These deposits make the Nili Fossae region one of the most colorful regions on Mars, which is most distinctive in infrared color composites (IRB). HiRISE IRB color aids in chemical and miner -
Identification of the most common minerals
Identification of the most common mineralsIdentification of the most common minerals
I made this movie for my students about the minerals they have to identify in the lab. I give suggestion about the tools to use to identify them. -
Rock Cycle Geology Sept 8 2015 PD
Rock Cycle Geology Sept 8 2015 PDRock Cycle Geology Sept 8 2015 PD
Okaloosa SCIENCE Initiative Sept 2015 Monthly Professional Development from 9/8/15 featuring Lisa Jones (OCSD) and Dr. Linda Johnson (Yellow River Soil and Water Conservation District). Workshop materials and presentation can be found on the Okaloosa SCIENCE Website (www.okaloosaschools.com/okaloosascience) -
Download Structural geology of folded rocks (Rand McNally geology series) eBook
Download Structural geology of folded rocks (Rand McNally geology series) eBookDownload Structural geology of folded rocks (Rand McNally geology series) eBook
Structural geology of folded rocks (Rand McNally geology series) PDF Download PDF/eBook: http://bit.ly/1UMWjg0 https://www.youtube.com/watch?v=3UQLvYJAOa4 -
Rock (geology) - Video Learning - WizScience.com
Rock (geology) - Video Learning - WizScience.comRock (geology) - Video Learning - WizScience.com
In geology, "rock" is a naturally occurring solid aggregate of one or more minerals or mineraloids. For example, the common rock granite is a combination of the quartz, feldspar and biotite minerals. The Earth's outer solid layer, the lithosphere, is made of rock. Rocks have been used by mankind throughout history. From the Stone Age, rocks have been used for tools. The minerals and metals found in rocks have been essential to human civilization. Three major groups of rocks are defined: igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is an essential component of geology. At a granul -
Slump (geology) - Video Learning - WizScience.com
Slump (geology) - Video Learning - WizScience.comSlump (geology) - Video Learning - WizScience.com
A "slump" is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or rock layers moves a short distance down a slope. Movement is characterized by sliding along a concave-upward or planar surface. Causes of slumping include earthquake shocks, thorough wetting, freezing and thawing, undercutting, and loading of a slope. Translational slumps occur when a detached landmass moves along a planar surface. Common planar surfaces of failure include joints or bedding planes, especially where a permeable layer overrides an impermeable surface. Block slumps are a type of translational slump in which one or more r -
Vein (geology) - Video Learning - WizScience.com
Vein (geology) - Video Learning - WizScience.comVein (geology) - Video Learning - WizScience.com
In geology, a "vein" is a distinct sheetlike body of crystallized minerals within a rock. Veins form when mineral constituents carried by an aqueous solution within the rock mass are deposited through precipitation. The hydraulic flow involved is usually due to hydrothermal circulation. Veins are classically thought of as being the result of growth of crystals on the walls of planar fractures in rocks, with the crystal growth occurring normal to the walls of the cavity, and the crystal protruding into open space. This certainly is the method for the formation of some veins. However, it is rare in geology for significant open space to rema -
Mantle (geology) - Video Learning - WizScience.com
Mantle (geology) - Video Learning - WizScience.comMantle (geology) - Video Learning - WizScience.com
The "mantle" is an interior part of a terrestrial planet or other rocky body large enough to have differentiation by density. The terrestrial planets , Earth's Moon and Jupiter's moon Io, each have a mantle made of silicate rock. Interpretation of spacecraft data suggests that at least three other moons of Jupiter , as well as Titan and Triton each have a mantle made of ice or another solid volatile substance. The interior of Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a layer between the crust and the outer core. Earth's mantle is a silicate rocky shell with an average thickness of 2
Rock cycle - geology for kids
- Order: Reorder
- Duration: 1:27
- Updated: 12 Oct 2015
- published: 12 Oct 2015
- views: 1
Books of Sedimentary Rock Geology Rocks
- Order: Reorder
- Duration: 0:26
- Updated: 12 Oct 2015
Access to read more ebook: http://www.realbooknow.net/books
wn.com/Books Of Sedimentary Rock Geology Rocks
Access to read more ebook: http://www.realbooknow.net/books
- published: 12 Oct 2015
- views: 0
Rock-Rock
- Order: Reorder
- Duration: 0:28
- Updated: 07 Oct 2015
This video is just to show the different components of the game Rock-Rock.
How to play Rock-Rock:
1. Start with a large rock for the base of game-play.
2. Throw medium sized rocks at the base rock, trying to have it land on the base rock (this is where the video starts). This is the Rock-Rock. 2 points are awarded for sticking the Rock-Rock landing.
3. Throw small pebbles (fine gravel) at the rock-rock to try to knock it off the base-rock. 4 points are awarded for knocking off the Rock-Rock, 3 bonus points if the rock you threw knocks off the Rock-Rock and remains on the base-rock. This rock becomes the new Rock-Rock. If no rocks remain on the base rock, a new Rock-Rock is thrown.
1 Bonus point given if you can hit the Rock-Rock and have the throwing rock deflect back to you and you catch it. Max 5 bonus points per game.
Play in teams to 21 points (or by yourself forever). Teams switch turns after each throw. This game works best if you are surrounded by a lot of rocks.
Let me know if these directions don't make sense
Have Fun!
wn.com/Rock Rock
This video is just to show the different components of the game Rock-Rock.
How to play Rock-Rock:
1. Start with a large rock for the base of game-play.
2. Throw medium sized rocks at the base rock, trying to have it land on the base rock (this is where the video starts). This is the Rock-Rock. 2 points are awarded for sticking the Rock-Rock landing.
3. Throw small pebbles (fine gravel) at the rock-rock to try to knock it off the base-rock. 4 points are awarded for knocking off the Rock-Rock, 3 bonus points if the rock you threw knocks off the Rock-Rock and remains on the base-rock. This rock becomes the new Rock-Rock. If no rocks remain on the base rock, a new Rock-Rock is thrown.
1 Bonus point given if you can hit the Rock-Rock and have the throwing rock deflect back to you and you catch it. Max 5 bonus points per game.
Play in teams to 21 points (or by yourself forever). Teams switch turns after each throw. This game works best if you are surrounded by a lot of rocks.
Let me know if these directions don't make sense
Have Fun!
- published: 07 Oct 2015
- views: 58
Rock Cycle - Geology For Kids - Learn about Rock
- Order: Reorder
- Duration: 3:42
- Updated: 07 Oct 2015
The Rock Cycle is a group of changes. Igneous rock can change into sedimentary rock or into metamorphic rock. Sedimentary rock can change into metamorphic rock or into igneous rock. Metamorphic rock can change into igneous or sedimentary rock.
Igneous rock forms when magma cools and makes crystals. Magma is a hot liquid made of melted minerals. The minerals can form crystals when they cool. Igneous rock can form underground, where the magma cools slowly. Or, igneous rock can form above ground, where the magma cools quickly.
When it pours out on Earth's surface, magma is called lava. Yes, the same liquid rock matter that you see coming out of volcanoes.
On Earth's surface, wind and water can break rock into pieces. They can also carry rock pieces to another place. Usually, the rock pieces, called sediments, drop from the wind or water to make a layer. The layer can be buried under other layers of sediments. After a long time the sediments can be cemented together to make sedimentary rock. In this way, igneous rock can become sedimentary rock.
All rock can be heated. But where does the heat come from? Inside Earth there is heat from pressure (push your hands together very hard and feel the heat). There is heat from friction (rub your hands together and feel the heat). There is also heat from radioactive decay (the process that gives us nuclear power plants that make electricity).
So, what does the heat do to the rock? It bakes the rock.
Baked rock does not melt, but it does change. It forms crystals. If it has crystals already, it forms larger crystals. Because this rock changes, it is called metamorphic. Remember that a caterpillar changes to become a butterfly. That change is called metamorphosis. Metamorphosis can occur in rock when they are heated to 300 to 700 degrees Celsius.
When Earth's tectonic plates move around, they produce heat. When they collide, they build mountains and metamorphose (met-ah-MORE-foes) the rock.
The rock cycle continues. Mountains made of metamorphic rocks can be broken up and washed away by streams. New sediments from these mountains can make new sedimentary rock.
The rock cycle never stops.
wn.com/Rock Cycle Geology For Kids Learn About Rock
The Rock Cycle is a group of changes. Igneous rock can change into sedimentary rock or into metamorphic rock. Sedimentary rock can change into metamorphic rock or into igneous rock. Metamorphic rock can change into igneous or sedimentary rock.
Igneous rock forms when magma cools and makes crystals. Magma is a hot liquid made of melted minerals. The minerals can form crystals when they cool. Igneous rock can form underground, where the magma cools slowly. Or, igneous rock can form above ground, where the magma cools quickly.
When it pours out on Earth's surface, magma is called lava. Yes, the same liquid rock matter that you see coming out of volcanoes.
On Earth's surface, wind and water can break rock into pieces. They can also carry rock pieces to another place. Usually, the rock pieces, called sediments, drop from the wind or water to make a layer. The layer can be buried under other layers of sediments. After a long time the sediments can be cemented together to make sedimentary rock. In this way, igneous rock can become sedimentary rock.
All rock can be heated. But where does the heat come from? Inside Earth there is heat from pressure (push your hands together very hard and feel the heat). There is heat from friction (rub your hands together and feel the heat). There is also heat from radioactive decay (the process that gives us nuclear power plants that make electricity).
So, what does the heat do to the rock? It bakes the rock.
Baked rock does not melt, but it does change. It forms crystals. If it has crystals already, it forms larger crystals. Because this rock changes, it is called metamorphic. Remember that a caterpillar changes to become a butterfly. That change is called metamorphosis. Metamorphosis can occur in rock when they are heated to 300 to 700 degrees Celsius.
When Earth's tectonic plates move around, they produce heat. When they collide, they build mountains and metamorphose (met-ah-MORE-foes) the rock.
The rock cycle continues. Mountains made of metamorphic rocks can be broken up and washed away by streams. New sediments from these mountains can make new sedimentary rock.
The rock cycle never stops.
- published: 07 Oct 2015
- views: 3
Geology for Engineers Sedimentary Rocks & Processes
- Order: Reorder
- Duration: 48:11
- Updated: 07 Oct 2015
Describes the processes that form sedimentary rocks and the classification of sedimentary rocks. This lecture also covers depositional environments and sedimentary structures.
wn.com/Geology For Engineers Sedimentary Rocks Processes
Describes the processes that form sedimentary rocks and the classification of sedimentary rocks. This lecture also covers depositional environments and sedimentary structures.
- published: 07 Oct 2015
- views: 4
Geology Rock Cycle Project
- Order: Reorder
- Duration: 2:00
- Updated: 05 Oct 2015
- published: 05 Oct 2015
- views: 3
Identification of fold structures in Sandstone and Shales - Geology Field Trip
- Order: Reorder
- Duration: 22:33
- Updated: 04 Oct 2015
Location: Beach to the west of Long Shank.
Description: Sand and rock beach with small stack (Davie's Rock).
Geology: anticline cut by intrusions.
wn.com/Identification Of Fold Structures In Sandstone And Shales Geology Field Trip
Location: Beach to the west of Long Shank.
Description: Sand and rock beach with small stack (Davie's Rock).
Geology: anticline cut by intrusions.
- published: 04 Oct 2015
- views: 12
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
- Order: Reorder
- Duration: 12:43
- Updated: 04 Oct 2015
Location: Rocky foreshore below St Monans Church.
Description: Rock platform below Fife Coast Path.
Geology: Later dyke cross-cutting the St Monans Neck
wn.com/Rock Platform Below Fife Coast Path With Dyke Cross Cutting Field Trip Geology
Location: Rocky foreshore below St Monans Church.
Description: Rock platform below Fife Coast Path.
Geology: Later dyke cross-cutting the St Monans Neck
- published: 04 Oct 2015
- views: 4
THE ROCK CYCLE GEOLOGY
- Order: Reorder
- Duration: 2:19
- Updated: 24 Sep 2015
- published: 24 Sep 2015
- views: 1
THE ROCK CYCLE GEOLOGY
- Order: Reorder
- Duration: 1:59
- Updated: 22 Sep 2015
- published: 22 Sep 2015
- views: 2
Geology of Raven Rock Arch
- Order: Reorder
- Duration: 2:22
- Updated: 24 Sep 2015
Geologist Brittany Parrick provides a brief discussion on the geology of Raven Rock Arch in Scioto County, Ohio. Also included is a short explanation of how the Teays River Valley and Ohio River were shaped by glaciers during the Ice Age.
wn.com/Geology Of Raven Rock Arch
Geologist Brittany Parrick provides a brief discussion on the geology of Raven Rock Arch in Scioto County, Ohio. Also included is a short explanation of how the Teays River Valley and Ohio River were shaped by glaciers during the Ice Age.
- published: 24 Sep 2015
- views: 21
okayest geology presentation
- Order: Reorder
- Duration: 4:31
- Updated: 23 Sep 2015
The Rock Cycle by Levi Hanson, Cole Kyllonen, and Tristan Durfee
wn.com/Okayest Geology Presentation
The Rock Cycle by Levi Hanson, Cole Kyllonen, and Tristan Durfee
- published: 23 Sep 2015
- views: 15
Geology Rock Cycle
- Order: Reorder
- Duration: 4:20
- Updated: 22 Sep 2015
Geology 1120-90
Mercedes Isensee
Ningozis White
Juliet McLellan
Raymond Klitsch
Cassandra Deloney
wn.com/Geology Rock Cycle
Geology 1120-90
Mercedes Isensee
Ningozis White
Juliet McLellan
Raymond Klitsch
Cassandra Deloney
- published: 22 Sep 2015
- views: 3
Engineering Geology Rock in Engineering Construction
- Order: Reorder
- Duration: 0:18
- Updated: 20 Sep 2015
Register to Browse more Ebooks
Get it Now at :
http://mgpdf.net/free
wn.com/Engineering Geology Rock In Engineering Construction
Register to Browse more Ebooks
Get it Now at :
http://mgpdf.net/free
- published: 20 Sep 2015
- views: 0
![Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]](http://web.archive.org./web/20151027052535im_/http://i.ytimg.com/vi/OlRYsYnRsDI/0.jpg "Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]")
Mars Science: Possible Sulfates in the Northeast Syrtis Major Region [HD]
- Order: Reorder
- Duration: 1:52
- Updated: 16 Sep 2015
A variety of diverse morphological features are present in this image (21 by 5.5 kilometers) located in the southeastern area of the Nili Fossae region and just northeast of Syrtis Major. This particular region has been studied intensely due to the presence of volcanics from Syrtis Major and impact ejecta from the Isidis Basin. The region is rich in unaltered mafic deposits, in contact with diverse altered deposits rich in clays, carbonates, and sulfates. These deposits make the Nili Fossae region one of the most colorful regions on Mars, which is most distinctive in infrared color composites (IRB). HiRISE IRB color aids in chemical and mineral-type mapping, especially when correlated with other MRO instruments such as CRISM.
In this infrared color close-up image (2.6 by 1.2 kilometers: http://static.uahirise.org/images/2015/details/cut/ESP_041893_1975-1.jpg), we can see a mesa, along with aeolian dunes and yellow-colored deposits. A mesa is a flat, steep-sloped hill, which was likely eroded by a combination of wind-driven and landslide processes. These are often formed due to differing rock compositions, which vary in their resistance to erosion, e.g., a weaker and softer rock, such as sediments, lies beneath a stronger and more resistant rock. The flat top surfaces of mesas, termed the “cap” rock, are relatively erosion-resistant rock types, such as igneous lavas or intrusive sills. The looser, yellowish deposits that underlie the cap rock contrast nicely with the purplish-blue cap rock.
Another closeup (0.7 by 1.2 kilometer: http://static.uahirise.org/images/2015/details/cut/ESP_041893_1975-2.jpg) shows an area just north of the mesa that is particularly distinct in this IRB color. Based on a corresponding CRISM image (http://crism-map.jhuapl.edu/summary.php?obs=HRL0000B8C207IF183S&x;=77.09&y;=17.31) providing spectral data, there is some exposed bedrock in the area that likely contains salt-bearing rocks.
Written by: Kayle Hansen, Livio Tornabene, and Elizabeth Silber (16 September 2015)
See more videos about Mars Science Theme:
Composition and Photometry:
https://www.youtube.com/playlist?list=PL6vzpF_OEV8kAbr1eHIHhf-ZR8eTB9iRU
See more videos about HiRISE,
High Resolution Imaging Science Experiment
(Mars Reconnaissance Orbiter Instrument):
http://www.youtube.com/playlist?list=PL6vzpF_OEV8nfAL7zVkUWJpw-_9jkJjtZ
HiRISE, High Resolution Imaging Science Experiment:
"Explore Mars, one giant image at a time."
The Mars Reconnaissance Orbiter Project is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Science Mission Directorate, Washington. JPL is a division of the California Institute of Technology in Pasadena.
HiRISE is operated by the University of Arizona, Tucson. The instrument was built by Ball Aerospace & Technologies Corp., Boulder, Colo. Malin Space Science Systems, San Diego, built and operates the Context Camera.
http://www.uahirise.org/
Credit: NASA/JPL/University of Arizona
wn.com/Mars Science Possible Sulfates In The Northeast Syrtis Major Region Hd
A variety of diverse morphological features are present in this image (21 by 5.5 kilometers) located in the southeastern area of the Nili Fossae region and just northeast of Syrtis Major. This particular region has been studied intensely due to the presence of volcanics from Syrtis Major and impact ejecta from the Isidis Basin. The region is rich in unaltered mafic deposits, in contact with diverse altered deposits rich in clays, carbonates, and sulfates. These deposits make the Nili Fossae region one of the most colorful regions on Mars, which is most distinctive in infrared color composites (IRB). HiRISE IRB color aids in chemical and mineral-type mapping, especially when correlated with other MRO instruments such as CRISM.
In this infrared color close-up image (2.6 by 1.2 kilometers: http://static.uahirise.org/images/2015/details/cut/ESP_041893_1975-1.jpg), we can see a mesa, along with aeolian dunes and yellow-colored deposits. A mesa is a flat, steep-sloped hill, which was likely eroded by a combination of wind-driven and landslide processes. These are often formed due to differing rock compositions, which vary in their resistance to erosion, e.g., a weaker and softer rock, such as sediments, lies beneath a stronger and more resistant rock. The flat top surfaces of mesas, termed the “cap” rock, are relatively erosion-resistant rock types, such as igneous lavas or intrusive sills. The looser, yellowish deposits that underlie the cap rock contrast nicely with the purplish-blue cap rock.
Another closeup (0.7 by 1.2 kilometer: http://static.uahirise.org/images/2015/details/cut/ESP_041893_1975-2.jpg) shows an area just north of the mesa that is particularly distinct in this IRB color. Based on a corresponding CRISM image (http://crism-map.jhuapl.edu/summary.php?obs=HRL0000B8C207IF183S&x;=77.09&y;=17.31) providing spectral data, there is some exposed bedrock in the area that likely contains salt-bearing rocks.
Written by: Kayle Hansen, Livio Tornabene, and Elizabeth Silber (16 September 2015)
See more videos about Mars Science Theme:
Composition and Photometry:
https://www.youtube.com/playlist?list=PL6vzpF_OEV8kAbr1eHIHhf-ZR8eTB9iRU
See more videos about HiRISE,
High Resolution Imaging Science Experiment
(Mars Reconnaissance Orbiter Instrument):
http://www.youtube.com/playlist?list=PL6vzpF_OEV8nfAL7zVkUWJpw-_9jkJjtZ
HiRISE, High Resolution Imaging Science Experiment:
"Explore Mars, one giant image at a time."
The Mars Reconnaissance Orbiter Project is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Science Mission Directorate, Washington. JPL is a division of the California Institute of Technology in Pasadena.
HiRISE is operated by the University of Arizona, Tucson. The instrument was built by Ball Aerospace & Technologies Corp., Boulder, Colo. Malin Space Science Systems, San Diego, built and operates the Context Camera.
http://www.uahirise.org/
Credit: NASA/JPL/University of Arizona
- published: 16 Sep 2015
- views: 62
Identification of the most common minerals
- Order: Reorder
- Duration: 18:29
- Updated: 15 Sep 2015
I made this movie for my students about the minerals they have to identify in the lab.
I give suggestion about the tools to use to identify them.
wn.com/Identification Of The Most Common Minerals
I made this movie for my students about the minerals they have to identify in the lab.
I give suggestion about the tools to use to identify them.
- published: 15 Sep 2015
- views: 7
Rock Cycle Geology Sept 8 2015 PD
- Order: Reorder
- Duration: 42:34
- Updated: 14 Sep 2015
Okaloosa SCIENCE Initiative Sept 2015 Monthly Professional Development from 9/8/15 featuring Lisa Jones (OCSD) and Dr. Linda Johnson (Yellow River Soil and Water Conservation District). Workshop materials and presentation can be found on the Okaloosa SCIENCE Website (www.okaloosaschools.com/okaloosascience)
wn.com/Rock Cycle Geology Sept 8 2015 Pd
Okaloosa SCIENCE Initiative Sept 2015 Monthly Professional Development from 9/8/15 featuring Lisa Jones (OCSD) and Dr. Linda Johnson (Yellow River Soil and Water Conservation District). Workshop materials and presentation can be found on the Okaloosa SCIENCE Website (www.okaloosaschools.com/okaloosascience)
- published: 14 Sep 2015
- views: 6
Download Structural geology of folded rocks (Rand McNally geology series) eBook
- Order: Reorder
- Duration: 0:27
- Updated: 13 Sep 2015
Structural geology of folded rocks (Rand McNally geology series) PDF
Download PDF/eBook: http://bit.ly/1UMWjg0
https://www.youtube.com/watch?v=3UQLvYJAOa4
wn.com/Download Structural Geology Of Folded Rocks (Rand Mcnally Geology Series) Ebook
Structural geology of folded rocks (Rand McNally geology series) PDF
Download PDF/eBook: http://bit.ly/1UMWjg0
https://www.youtube.com/watch?v=3UQLvYJAOa4
- published: 13 Sep 2015
- views: 0
Rock (geology) - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:15
- Updated: 10 Sep 2015
In geology, "rock" is a naturally occurring solid aggregate of one or more minerals or mineraloids. For example, the common rock granite is a combination of the quartz, feldspar and biotite minerals. The Earth's outer solid layer, the lithosphere, is made of rock.
Rocks have been used by mankind throughout history. From the Stone Age, rocks have been used for tools. The minerals and metals found in rocks have been essential to human civilization.
Three major groups of rocks are defined: igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is an essential component of geology.
At a granular level, rocks are composed of grains of minerals, which, in turn, are homogeneous solids formed from a chemical compound that is arranged in an orderly manner. The aggregate minerals forming the rock are held together by chemical bonds. The types and abundance of minerals in a rock are determined by the manner in which the rock was formed. Many rocks contain silica ; a compound of silicon and oxygen that forms 74.3% of the Earth's crust. This material forms crystals with other compounds in the rock. The proportion of silica in rocks and minerals is a major factor in determining their name and properties.
Rocks are geologically classified according to characteristics such as mineral and chemical composition, permeability, the texture of the constituent particles, and particle size. These physical properties are the end result of the processes that formed the rocks. Over the course of time, rocks can transform from one type into another, as described by the geological model called the rock cycle. These events produce three general classes of rock: igneous, sedimentary, and metamorphic.
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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/Rock+(geology), 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.
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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/Rock+(geology), 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/Rock (Geology) Video Learning Wizscience.Com
In geology, "rock" is a naturally occurring solid aggregate of one or more minerals or mineraloids. For example, the common rock granite is a combination of the quartz, feldspar and biotite minerals. The Earth's outer solid layer, the lithosphere, is made of rock.
Rocks have been used by mankind throughout history. From the Stone Age, rocks have been used for tools. The minerals and metals found in rocks have been essential to human civilization.
Three major groups of rocks are defined: igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, which is an essential component of geology.
At a granular level, rocks are composed of grains of minerals, which, in turn, are homogeneous solids formed from a chemical compound that is arranged in an orderly manner. The aggregate minerals forming the rock are held together by chemical bonds. The types and abundance of minerals in a rock are determined by the manner in which the rock was formed. Many rocks contain silica ; a compound of silicon and oxygen that forms 74.3% of the Earth's crust. This material forms crystals with other compounds in the rock. The proportion of silica in rocks and minerals is a major factor in determining their name and properties.
Rocks are geologically classified according to characteristics such as mineral and chemical composition, permeability, the texture of the constituent particles, and particle size. These physical properties are the end result of the processes that formed the rocks. Over the course of time, rocks can transform from one type into another, as described by the geological model called the rock cycle. These events produce three general classes of rock: igneous, sedimentary, and metamorphic.
Wiz Science™ is "the" learning channel for children and all ages.
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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/Rock+(geology), 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.
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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/Rock+(geology), 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: 10 Sep 2015
- views: 0
Slump (geology) - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:31
- Updated: 04 Sep 2015
A "slump" is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or rock layers moves a short distance down a slope. Movement is characterized by sliding along a concave-upward or planar surface. Causes of slumping include earthquake shocks, thorough wetting, freezing and thawing, undercutting, and loading of a slope.
Translational slumps occur when a detached landmass moves along a planar surface. Common planar surfaces of failure include joints or bedding planes, especially where a permeable layer overrides an impermeable surface. Block slumps are a type of translational slump in which one or more related block units move downslope as a relatively coherent mass.
Rotational slumps occur when a slump block, composed of sediment or rock, slides along a concave-upward slip surface with rotation about an axis parallel to the slope. Rotational movement causes the original surface of the block to become less steep, and the top of the slump is rotated backward. This results in internal deformation of the moving mass consisting chiefly of overturned folds called sheath folds.
Slumps have several characteristic features. The cut which forms as the landmass breaks away from the slope is called the scarp and is often cliff-like and concave. In rotational slumps, the main slump block often breaks into a series of secondary slumps and associated scarps to form stairstep pattern of displaced blocks. The upper surface of the blocks are rotated backwards, forming depressions which may accumulate water to create ponds or swampy areas. The surface of the detached mass often remains relatively undisturbed, especially at the top. However, hummocky ridges may form near the toe of the slump. Addition of water and loss of sediment cohesion at the toe may transform slumping material into an earthflow. Transverse cracks at the head scarp drain water, possibly killing vegetation. Transverse ridges, transverse cracks and radial cracks form in displaced material on the foot of the slump.
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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/Slump+(geology), 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/Slump (Geology) Video Learning Wizscience.Com
A "slump" is a form of mass wasting that occurs when a coherent mass of loosely consolidated materials or rock layers moves a short distance down a slope. Movement is characterized by sliding along a concave-upward or planar surface. Causes of slumping include earthquake shocks, thorough wetting, freezing and thawing, undercutting, and loading of a slope.
Translational slumps occur when a detached landmass moves along a planar surface. Common planar surfaces of failure include joints or bedding planes, especially where a permeable layer overrides an impermeable surface. Block slumps are a type of translational slump in which one or more related block units move downslope as a relatively coherent mass.
Rotational slumps occur when a slump block, composed of sediment or rock, slides along a concave-upward slip surface with rotation about an axis parallel to the slope. Rotational movement causes the original surface of the block to become less steep, and the top of the slump is rotated backward. This results in internal deformation of the moving mass consisting chiefly of overturned folds called sheath folds.
Slumps have several characteristic features. The cut which forms as the landmass breaks away from the slope is called the scarp and is often cliff-like and concave. In rotational slumps, the main slump block often breaks into a series of secondary slumps and associated scarps to form stairstep pattern of displaced blocks. The upper surface of the blocks are rotated backwards, forming depressions which may accumulate water to create ponds or swampy areas. The surface of the detached mass often remains relatively undisturbed, especially at the top. However, hummocky ridges may form near the toe of the slump. Addition of water and loss of sediment cohesion at the toe may transform slumping material into an earthflow. Transverse cracks at the head scarp drain water, possibly killing vegetation. Transverse ridges, transverse cracks and radial cracks form in displaced material on the foot of the slump.
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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/Slump+(geology), 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: 04 Sep 2015
- views: 4
Vein (geology) - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:15
- Updated: 02 Sep 2015
In geology, a "vein" is a distinct sheetlike body of crystallized minerals within a rock. Veins form when mineral constituents carried by an aqueous solution within the rock mass are deposited through precipitation. The hydraulic flow involved is usually due to hydrothermal circulation.
Veins are classically thought of as being the result of growth of crystals on the walls of planar fractures in rocks, with the crystal growth occurring normal to the walls of the cavity, and the crystal protruding into open space. This certainly is the method for the formation of some veins. However, it is rare in geology for significant open space to remain open in large volumes of rock, especially several kilometers below the surface. Thus, there are two main mechanisms considered likely for the formation of veins: "open-space filling" and "crack-seal growth".
Open space filling is the hallmark of epithermal vein systems, such as a stockwork, in greisens or in certain skarn environments. For open space filling to take effect, the confining pressure is generally considered to be below 0.5 GPa, or less than 3-5 kilometers. Veins formed in this way may exhibit a colloform, agate-like habit, of sequential selvages of minerals which radiate out from nucleation points on the vein walls and appear to fill up the available open space. Often evidence of fluid boiling is present. Vugs, cavities and geodes are all examples of open-space filling phenomena in hydrothermal systems.
Alternatively, hydraulic fracturing may create a breccia which is filled with vein material. Such breccia vein systems may be quite extensive, and can form the shape of tabular dipping sheets, diatremes or laterally extensive mantos controlled by boundaries such as thrust faults, competent sedimentary layers, or cap rocks.
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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/Vein+(geology), 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/Vein (Geology) Video Learning Wizscience.Com
In geology, a "vein" is a distinct sheetlike body of crystallized minerals within a rock. Veins form when mineral constituents carried by an aqueous solution within the rock mass are deposited through precipitation. The hydraulic flow involved is usually due to hydrothermal circulation.
Veins are classically thought of as being the result of growth of crystals on the walls of planar fractures in rocks, with the crystal growth occurring normal to the walls of the cavity, and the crystal protruding into open space. This certainly is the method for the formation of some veins. However, it is rare in geology for significant open space to remain open in large volumes of rock, especially several kilometers below the surface. Thus, there are two main mechanisms considered likely for the formation of veins: "open-space filling" and "crack-seal growth".
Open space filling is the hallmark of epithermal vein systems, such as a stockwork, in greisens or in certain skarn environments. For open space filling to take effect, the confining pressure is generally considered to be below 0.5 GPa, or less than 3-5 kilometers. Veins formed in this way may exhibit a colloform, agate-like habit, of sequential selvages of minerals which radiate out from nucleation points on the vein walls and appear to fill up the available open space. Often evidence of fluid boiling is present. Vugs, cavities and geodes are all examples of open-space filling phenomena in hydrothermal systems.
Alternatively, hydraulic fracturing may create a breccia which is filled with vein material. Such breccia vein systems may be quite extensive, and can form the shape of tabular dipping sheets, diatremes or laterally extensive mantos controlled by boundaries such as thrust faults, competent sedimentary layers, or cap rocks.
Wiz Science™ is "the" learning channel for children and all ages.
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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/Vein+(geology), 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: 0
Mantle (geology) - Video Learning - WizScience.com
- Order: Reorder
- Duration: 2:20
- Updated: 02 Sep 2015
The "mantle" is an interior part of a terrestrial planet or other rocky body large enough to have differentiation by density. The terrestrial planets , Earth's Moon and Jupiter's moon Io, each have a mantle made of silicate rock. Interpretation of spacecraft data suggests that at least three other moons of Jupiter , as well as Titan and Triton each have a mantle made of ice or another solid volatile substance.
The interior of Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a layer between the crust and the outer core. Earth's mantle is a silicate rocky shell with an average thickness of 2886 km. The mantle makes up about 84% of Earth's volume. It is predominantly solid but in geological time it behaves as a very viscous fluid. The mantle encloses the hot core rich in iron and nickel, which makes up about 15% of Earth's volume. Past episodes of melting and volcanism at the shallower levels of the mantle have produced a thin crust of crystallized melt products near the surface, upon which we live. Information about structure and composition of the mantle either result from geophysical investigation or from direct geoscientific analyses on Earth mantle derived xenoliths and on mantle exposed by mid-oceanic ridge spreading.
Two main zones are distinguished in the upper mantle: the inner asthenosphere composed of plastic flowing rock of varying thickness, on average about 200 km thick, and the lowermost part of the lithosphere composed of rigid rock about 50 to thick. A thin crust, the upper part of the lithosphere, surrounds the mantle and is about 5 to thick. Recent analysis of hydrous ringwoodite from the mantle suggests that there is between one and three times as much water in the transition zone between the lower and upper mantle than in all the world's oceans combined.
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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/Mantle+(geology), 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/Mantle (Geology) Video Learning Wizscience.Com
The "mantle" is an interior part of a terrestrial planet or other rocky body large enough to have differentiation by density. The terrestrial planets , Earth's Moon and Jupiter's moon Io, each have a mantle made of silicate rock. Interpretation of spacecraft data suggests that at least three other moons of Jupiter , as well as Titan and Triton each have a mantle made of ice or another solid volatile substance.
The interior of Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a layer between the crust and the outer core. Earth's mantle is a silicate rocky shell with an average thickness of 2886 km. The mantle makes up about 84% of Earth's volume. It is predominantly solid but in geological time it behaves as a very viscous fluid. The mantle encloses the hot core rich in iron and nickel, which makes up about 15% of Earth's volume. Past episodes of melting and volcanism at the shallower levels of the mantle have produced a thin crust of crystallized melt products near the surface, upon which we live. Information about structure and composition of the mantle either result from geophysical investigation or from direct geoscientific analyses on Earth mantle derived xenoliths and on mantle exposed by mid-oceanic ridge spreading.
Two main zones are distinguished in the upper mantle: the inner asthenosphere composed of plastic flowing rock of varying thickness, on average about 200 km thick, and the lowermost part of the lithosphere composed of rigid rock about 50 to thick. A thin crust, the upper part of the lithosphere, surrounds the mantle and is about 5 to thick. Recent analysis of hydrous ringwoodite from the mantle suggests that there is between one and three times as much water in the transition zone between the lower and upper mantle than in all the world's oceans combined.
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/Mantle+(geology), 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: 2
-
Igneous Rock Geology Lab Tutorial by Nancy
Igneous Rock Geology Lab Tutorial by NancyIgneous Rock Geology Lab Tutorial by Nancy
This is a Igneous Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington. SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO: http://www.mediafire.com/view/si5qz2qxm4fqpf8/Igneous_Rock_Lab_PDFS.pdf -
Geology Rocks instrumental Song Practice
Geology Rocks instrumental Song PracticeGeology Rocks instrumental Song Practice
*Instrumental ONLY* Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through! 1. Professor Rock Has Disappeared 0:07 2. Geologic Time 2:26 3. I Ain't Well 4:24 4. I Am Deep 6:27 5. Oh to be a Fossil Fuel 8:04 6. Erosion 10:24 7. Love Them Plates 12:28 8. Seven Little Miners 14:26 9. Rock Cycle 16:22 10. Professor Rock Has Re-Appeared 18:35 Click here for the original video: https://youtu.be/KCL_v9QK0TQ These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole purpose -
EYEWITNESS | Rock & Mineral
EYEWITNESS | Rock & MineralEYEWITNESS | Rock & Mineral
Rock and Mineral (geology) - July 22, 1996 -
Professor Iain Stewart - Geology's 'Rock Star'
Professor Iain Stewart - Geology's 'Rock Star'Professor Iain Stewart - Geology's 'Rock Star'
Geographer and geologist Iain Stewart is a Professor of Geosciences Communication at the University of Plymouth where his research interests include the mech... -
Sedimentary Rock Geology Lab Tutorial by Nancy
Sedimentary Rock Geology Lab Tutorial by NancySedimentary Rock Geology Lab Tutorial by Nancy
This is a Sedimentary Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington. SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO: http://www.mediafire.com/view/yxqedbb5lx65mqt/Sedimentary_Rock_Lab_PDFS.pdf -
Geology, PLate Tectonics and the Rock Cycle
Geology, PLate Tectonics and the Rock CycleGeology, PLate Tectonics and the Rock Cycle
Queen Nerdling describes geology, plate tectonics and then goes into the rock cycle. -
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organization's new director of research, and also as a speaker for layperson and technical audiences. The addition of Dr. Snelling has further confirmed AiG's effort to meet the highest standards in its research in Creation studies. Dr. Snelling, who spent considerable time serving as a consultant in developing the AiG Creation Museum's large flood-geology room, becomes AiG's first full-time Ph.D. in the field of geology. Dr. Snelling earned his PhD degree in geology from the University of -
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organ... -
Geology Rocks! - Rancho Rosal 2nd Grade 2014
Geology Rocks! - Rancho Rosal 2nd Grade 2014Geology Rocks! - Rancho Rosal 2nd Grade 2014
Mrs. Knauss' and Mrs. Myrick's second grade classes star in "Geology rocks!" - February 11, 2014 at Rancho Rosal Elementary School in Camarillo, CA Written b... -
Relative Dating of Rock Layers
Relative Dating of Rock LayersRelative Dating of Rock Layers
How to determine to geologic sequence of events from a rock cross section. -
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
Engineering Geology Lec 20 Stress Strain Behavior of Soil and RockEngineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock -
Geology of Table Rocks
Geology of Table RocksGeology of Table Rocks
Approximately 48 to 35 million years ago, the Payne Cliffs Formation was being deposited by rivers in the area of the Table Rocks. The Payne Cliffs Formation is made up of river deposited sandstone and conglomerates. From 20 to 10 million years ago the uplift of the nearby Klamath Mountains and the formation of the Rogue Valley took place. About 7 million years ago, a shield volcano erupted a lava flow that was approximately forty-four miles long and spread out over the entire valley, from the Prospect area to Sams Valley. This mass of lava caused the valley floor to rise in elevation to the height of the top of Table Rocks. The 4,864-acre -
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock IIEngineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II -
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
Engineering Geology Lec 19 Index Properties of Rock and Rock MassEngineering Geology Lec 19 Index Properties of Rock and Rock Mass
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass -
Engineering Geology Lec 40 Identification of minerals and rock samples
Engineering Geology Lec 40 Identification of minerals and rock samplesEngineering Geology Lec 40 Identification of minerals and rock samples
Engineering Geology Lec 40 Identification of minerals and rock samples -
Lecture - 10 Igneous Rocks
Lecture - 10 Igneous RocksLecture - 10 Igneous Rocks
Lecture Series on Engineering Geology by Prof.Debasis Roy, Department of Civil Engineering,I.I.T.Kharagpur.For more Courses visit http://nptel.iitm.ac.in.
Igneous Rock Geology Lab Tutorial by Nancy
- Order: Reorder
- Duration: 31:43
- Updated: 05 Apr 2015
This is a Igneous Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington.
SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO:
http://www.mediafire.com/view/si5qz2qxm4fqpf8/Igneous_Rock_Lab_PDFS.pdf
wn.com/Igneous Rock Geology Lab Tutorial By Nancy
This is a Igneous Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington.
SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO:
http://www.mediafire.com/view/si5qz2qxm4fqpf8/Igneous_Rock_Lab_PDFS.pdf
- published: 05 Apr 2015
- views: 12
Geology Rocks instrumental Song Practice
- Order: Reorder
- Duration: 20:45
- Updated: 17 May 2015
*Instrumental ONLY*
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through!
1. Professor Rock Has Disappeared 0:07
2. Geologic Time 2:26
3. I Ain't Well 4:24
4. I Am Deep 6:27
5. Oh to be a Fossil Fuel 8:04
6. Erosion 10:24
7. Love Them Plates 12:28
8. Seven Little Miners 14:26
9. Rock Cycle 16:22
10. Professor Rock Has Re-Appeared 18:35
Click here for the original video:
https://youtu.be/KCL_v9QK0TQ
These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole purpose of this video is for students to practice the song portions of this musical.
wn.com/Geology Rocks Instrumental Song Practice
*Instrumental ONLY*
Practice the songs for Geology Rocks right here! Just click on the individual song links below or practice with the whole video all the way through!
1. Professor Rock Has Disappeared 0:07
2. Geologic Time 2:26
3. I Ain't Well 4:24
4. I Am Deep 6:27
5. Oh to be a Fossil Fuel 8:04
6. Erosion 10:24
7. Love Them Plates 12:28
8. Seven Little Miners 14:26
9. Rock Cycle 16:22
10. Professor Rock Has Re-Appeared 18:35
Click here for the original video:
https://youtu.be/KCL_v9QK0TQ
These are the 10 songs from the Geology Rocks! musical play for Elementary and Middle School Grades 2-6 by Ron Fink and John Heath. The sole purpose of this video is for students to practice the song portions of this musical.
- published: 17 May 2015
- views: 4
EYEWITNESS | Rock & Mineral
- Order: Reorder
- Duration: 28:33
- Updated: 24 Apr 2015
Rock and Mineral (geology) - July 22, 1996
wn.com/Eyewitness | Rock Mineral
Rock and Mineral (geology) - July 22, 1996
- published: 24 Apr 2015
- views: 62
Professor Iain Stewart - Geology's 'Rock Star'
Geographer and geologist Iain Stewart is a Professor of Geosciences Communication at the University of Plymouth where his research interests include the mech...
wn.com/Professor Iain Stewart Geology's 'Rock Star'
Geographer and geologist Iain Stewart is a Professor of Geosciences Communication at the University of Plymouth where his research interests include the mech...
- published: 19 May 2014
- views: 184
- author: SELS
Sedimentary Rock Geology Lab Tutorial by Nancy
- Order: Reorder
- Duration: 23:11
- Updated: 03 Apr 2015
This is a Sedimentary Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington.
SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO:
http://www.mediafire.com/view/yxqedbb5lx65mqt/Sedimentary_Rock_Lab_PDFS.pdf
wn.com/Sedimentary Rock Geology Lab Tutorial By Nancy
This is a Sedimentary Rock Tutorial done by fabulous a teacher named Nancy at a college in Seattle, Washington.
SEE BELOW FOR A FREE PDF. DOWNLOAD OF THIS VIDEO:
http://www.mediafire.com/view/yxqedbb5lx65mqt/Sedimentary_Rock_Lab_PDFS.pdf
- published: 03 Apr 2015
- views: 7
Geology, PLate Tectonics and the Rock Cycle
- Order: Reorder
- Duration: 20:35
- Updated: 19 Jan 2015
Queen Nerdling describes geology, plate tectonics and then goes into the rock cycle.
wn.com/Geology, Plate Tectonics And The Rock Cycle
Queen Nerdling describes geology, plate tectonics and then goes into the rock cycle.
- published: 19 Jan 2015
- views: 3
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
- Order: Reorder
- Duration: 30:03
- Updated: 07 Jun 2011
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organization's new director of research, and also as a speaker for layperson and technical audiences. The addition of Dr. Snelling has further confirmed AiG's effort to meet the highest standards in its research in Creation studies.
Dr. Snelling, who spent considerable time serving as a consultant in developing the AiG Creation Museum's large flood-geology room, becomes AiG's first full-time Ph.D. in the field of geology. Dr. Snelling earned his PhD degree in geology from the University of Sydney in Australia.
Dr. Snelling has extensive experience working in the mining industry in Australia. One of his main areas of research has been the study of methods used in dating rocks, a key area of research for groups like AiG, which are convinced of a young age for the earth. Snelling's research, for example, has shown different radioisotope dates on the same rock samples. In addition, Dr. Snelling's research has indicated that radioactive decay rates must not have been constant in the past, citing the halos in rock crystals, which clearly show radioactive decay was accelerated sometime in the past ( See http://www.youtube.com/watch?v=ZGej0GQF5TQ ).
Dr. Snelling's research has demonstrated that a global flood more than 4,300 years ago explains most rock layers and fossil deposits found around the world. Building from this foundation, Dr. Snelling has made predictions as to what should be found if a catastrophic global flood actually happened (e.g., the existence of extensive rock layers).
Radioisotope dating has been used by the evolutions as the cornerstone of an old earth age and evolutionary theory. Not so says Dr. Snelling. See why Radioisotope dating is not all its cracked up to be.
For more creation scientists and speakers, visit http://www.youngearth.org/past_speakers.htm
Dr. Andrew Snelling
Education
B.S. Applied Geology, The University of New South Wales, Sydney, Australia, First Class Honours Ph.D. Geology, University of Sydney, Sydney, Australia
Associations
Geological Society of Australia
Australasian Institute of Mining and Metallurgy
Geological Society of America
Geological Association of Canada
Mineralogical Society of America
Society of Economic Geologists
Society for Geology Applied to Mineral Deposits
International Association of Geochemistry and Cosmochemistry
Association of Exploration Geochemists
Australian Society of Exploration Geophysicists
Creation Research Society
More of Dr. Snelling's bio here: http://creation.com/andrew-a-snelling
wn.com/Radioisotope Dating Of Rocks Challenging An Icon Of Evolutionary Geology Dr. Snelling Part 1
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organization's new director of research, and also as a speaker for layperson and technical audiences. The addition of Dr. Snelling has further confirmed AiG's effort to meet the highest standards in its research in Creation studies.
Dr. Snelling, who spent considerable time serving as a consultant in developing the AiG Creation Museum's large flood-geology room, becomes AiG's first full-time Ph.D. in the field of geology. Dr. Snelling earned his PhD degree in geology from the University of Sydney in Australia.
Dr. Snelling has extensive experience working in the mining industry in Australia. One of his main areas of research has been the study of methods used in dating rocks, a key area of research for groups like AiG, which are convinced of a young age for the earth. Snelling's research, for example, has shown different radioisotope dates on the same rock samples. In addition, Dr. Snelling's research has indicated that radioactive decay rates must not have been constant in the past, citing the halos in rock crystals, which clearly show radioactive decay was accelerated sometime in the past ( See http://www.youtube.com/watch?v=ZGej0GQF5TQ ).
Dr. Snelling's research has demonstrated that a global flood more than 4,300 years ago explains most rock layers and fossil deposits found around the world. Building from this foundation, Dr. Snelling has made predictions as to what should be found if a catastrophic global flood actually happened (e.g., the existence of extensive rock layers).
Radioisotope dating has been used by the evolutions as the cornerstone of an old earth age and evolutionary theory. Not so says Dr. Snelling. See why Radioisotope dating is not all its cracked up to be.
For more creation scientists and speakers, visit http://www.youngearth.org/past_speakers.htm
Dr. Andrew Snelling
Education
B.S. Applied Geology, The University of New South Wales, Sydney, Australia, First Class Honours Ph.D. Geology, University of Sydney, Sydney, Australia
Associations
Geological Society of Australia
Australasian Institute of Mining and Metallurgy
Geological Society of America
Geological Association of Canada
Mineralogical Society of America
Society of Economic Geologists
Society for Geology Applied to Mineral Deposits
International Association of Geochemistry and Cosmochemistry
Association of Exploration Geochemists
Australian Society of Exploration Geophysicists
Creation Research Society
More of Dr. Snelling's bio here: http://creation.com/andrew-a-snelling
- published: 07 Jun 2011
- views: 3107
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
- Order: Reorder
- Duration: 30:12
- Updated: 04 Sep 2014
- author: RockyMtnCreation
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organ...
wn.com/Radioisotope Dating Of Rocks Challenging An Icon Of Evolutionary Geology Dr. Snelling Part 2
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in geological studies, joined Answers in Genesis in 2007 as the organ...
- published: 07 Jun 2011
- views: 1295
- author: RockyMtnCreation
Geology Rocks! - Rancho Rosal 2nd Grade 2014
- Order: Reorder
- Duration: 32:52
- Updated: 08 Jun 2014
- author: Eric Wenschlag
Mrs. Knauss' and Mrs. Myrick's second grade classes star in "Geology rocks!" - February 11, 2014 at Rancho Rosal Elementary School in Camarillo, CA Written b...
wn.com/Geology Rocks Rancho Rosal 2Nd Grade 2014
Mrs. Knauss' and Mrs. Myrick's second grade classes star in "Geology rocks!" - February 11, 2014 at Rancho Rosal Elementary School in Camarillo, CA Written b...
- published: 12 Feb 2014
- views: 357
- author: Eric Wenschlag
Relative Dating of Rock Layers
- Order: Reorder
- Duration: 26:38
- Updated: 11 May 2014
How to determine to geologic sequence of events from a rock cross section.
wn.com/Relative Dating Of Rock Layers
How to determine to geologic sequence of events from a rock cross section.
- published: 11 May 2014
- views: 5004
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
- Order: Reorder
- Duration: 59:56
- Updated: 22 Sep 2014
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
wn.com/Engineering Geology Lec 20 Stress Strain Behavior Of Soil And Rock
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
- published: 22 Sep 2014
- views: 0
Geology of Table Rocks
- Order: Reorder
- Duration: 24:23
- Updated: 07 May 2015
Approximately 48 to 35 million years ago, the Payne Cliffs Formation was being deposited by rivers in the area of the Table Rocks. The Payne Cliffs Formation is made up of river deposited sandstone and conglomerates. From 20 to 10 million years ago the uplift of the nearby Klamath Mountains and the formation of the Rogue Valley took place.
About 7 million years ago, a shield volcano erupted a lava flow that was approximately forty-four miles long and spread out over the entire valley, from the Prospect area to Sams Valley. This mass of lava caused the valley floor to rise in elevation to the height of the top of Table Rocks.
The 4,864-acre Table Rocks Management Area is cooperatively owned and administered by the Medford District Bureau of Land Management (2,105 acres) and The Nature Conservancy (2,759 acres). Memorandums of Understanding signed in 2011 and 2012 with the Confederated Tribes of the Grand Ronde and the Cow Creek Band of Umpqua Tribe of Indians allow for coordinating resources to protect the Table Rocks for present and future generations. A cooperative management plan for the area was completed in 2013.
The Table Rocks trails are some of the most highly used trails in the Rogue Valley—almost 50,000 people hike the trails to the top each year. You could be one of hundreds of hikers enjoying the wildflowers and scenic vistas on a beautiful spring day, or you could be the lone hiker on a cold, foggy winter day. Some people like to linger and take their time getting to the top, watching for birds and identifying wildflowers on the way, while others run the trail and focus on getting a workout.
During the spring months, BLM Rangers lead large school groups on guided hikes Tuesday through Fridays, stopping often along the trail. To encounter fewer people and school groups, consider hiking in the early morning or early afternoon on weekdays.
To find out more about this stunning area head on over to:
http://blm.gov/19ld
wn.com/Geology Of Table Rocks
Approximately 48 to 35 million years ago, the Payne Cliffs Formation was being deposited by rivers in the area of the Table Rocks. The Payne Cliffs Formation is made up of river deposited sandstone and conglomerates. From 20 to 10 million years ago the uplift of the nearby Klamath Mountains and the formation of the Rogue Valley took place.
About 7 million years ago, a shield volcano erupted a lava flow that was approximately forty-four miles long and spread out over the entire valley, from the Prospect area to Sams Valley. This mass of lava caused the valley floor to rise in elevation to the height of the top of Table Rocks.
The 4,864-acre Table Rocks Management Area is cooperatively owned and administered by the Medford District Bureau of Land Management (2,105 acres) and The Nature Conservancy (2,759 acres). Memorandums of Understanding signed in 2011 and 2012 with the Confederated Tribes of the Grand Ronde and the Cow Creek Band of Umpqua Tribe of Indians allow for coordinating resources to protect the Table Rocks for present and future generations. A cooperative management plan for the area was completed in 2013.
The Table Rocks trails are some of the most highly used trails in the Rogue Valley—almost 50,000 people hike the trails to the top each year. You could be one of hundreds of hikers enjoying the wildflowers and scenic vistas on a beautiful spring day, or you could be the lone hiker on a cold, foggy winter day. Some people like to linger and take their time getting to the top, watching for birds and identifying wildflowers on the way, while others run the trail and focus on getting a workout.
During the spring months, BLM Rangers lead large school groups on guided hikes Tuesday through Fridays, stopping often along the trail. To encounter fewer people and school groups, consider hiking in the early morning or early afternoon on weekdays.
To find out more about this stunning area head on over to:
http://blm.gov/19ld
- published: 07 May 2015
- views: 7
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
- Order: Reorder
- Duration: 59:50
- Updated: 22 Sep 2014
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
wn.com/Engineering Geology Lec 21 Stress Strain Behavior Of Soil And Rock Ii
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
- published: 22 Sep 2014
- views: 0
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
- Order: Reorder
- Duration: 60:30
- Updated: 22 Sep 2014
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
wn.com/Engineering Geology Lec 19 Index Properties Of Rock And Rock Mass
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
- published: 22 Sep 2014
- views: 2
Engineering Geology Lec 40 Identification of minerals and rock samples
- Order: Reorder
- Duration: 59:54
- Updated: 22 Sep 2014
Engineering Geology Lec 40 Identification of minerals and rock samples
wn.com/Engineering Geology Lec 40 Identification Of Minerals And Rock Samples
Engineering Geology Lec 40 Identification of minerals and rock samples
- published: 22 Sep 2014
- views: 0
Lecture - 10 Igneous Rocks
Lecture Series on Engineering Geology by Prof.Debasis Roy, Department of Civil Engineering,I.I.T.Kharagpur.For more Courses visit http://nptel.iitm.ac.in.
wn.com/Lecture 10 Igneous Rocks
Lecture Series on Engineering Geology by Prof.Debasis Roy, Department of Civil Engineering,I.I.T.Kharagpur.For more Courses visit http://nptel.iitm.ac.in.
- published: 07 Jul 2008
- views: 18698
- author: nptelhrd
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23:20
Basics of Geology All About Rocks and Minerals
...
published: 09 Mar 2014
Basics of Geology All About Rocks and Minerals
Basics of Geology All About Rocks and Minerals
- published: 09 Mar 2014
- views: 23594
57:06
Living Rock An Introduction to Earths Geology
US Survey series....
published: 03 Jun 2014
author: Martin Diker
Living Rock An Introduction to Earths Geology
Living Rock An Introduction to Earths Geology
- published: 03 Jun 2014
- views: 2151
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author:
Martin Diker
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8:36
Geology Kitchen: The 3 Types of Rocks
http://explorermultimedia.org/ Geologist Devin Dennie heads to the kitchen to demonstrate ...
published: 03 Sep 2011
author: tkent22
Geology Kitchen: The 3 Types of Rocks
Geology Kitchen: The 3 Types of Rocks
- published: 03 Sep 2011
- views: 112938
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tkent22
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59:07
BBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time - Iain Stewart tells the story of James Hutton, the found...
published: 31 Oct 2012
author: xMaTx4
BBC Men of Rock 1 of 3 Deep Time
BBC Men of Rock 1 of 3 Deep Time
- published: 31 Oct 2012
- views: 56685
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author:
xMaTx4
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20:45
Geology Rocks Song Practice
Practice the songs for Geology Rocks right here! Just click on the individual song links b...
published: 17 May 2015
Geology Rocks Song Practice
Geology Rocks Song Practice
- published: 17 May 2015
- views: 8
7:13
Basic Rock Identification: Geology
Visual Study Aid for Physical/Historical Geology Classes. MUSIC: "DISTANCE" by Soilwork, f...
published: 09 Nov 2007
author: devildogmre
Basic Rock Identification: Geology
Basic Rock Identification: Geology
- published: 09 Nov 2007
- views: 146443
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devildogmre
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9:17
Geology for IDiots Episode 1 Rocks Part 2
Part 2 of Episode 1 Geology for IDiots with this episode focusing on Rocks My Blog as Prom...
published: 22 Apr 2009
author: Hochemon2008
Geology for IDiots Episode 1 Rocks Part 2
Geology for IDiots Episode 1 Rocks Part 2
- published: 22 Apr 2009
- views: 34563
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author:
Hochemon2008
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3:16
Fossil Rock Anthem
Explain/annotate the lyrics on rap genius: http://rapgenius.com/Tom-mcfadden-fossil-rock-a...
published: 22 Oct 2012
Fossil Rock Anthem
Fossil Rock Anthem
- published: 22 Oct 2012
- views: 460343
19:17
Rock and Mineral Identification
A study guide made for the students of Fleming College in Lindsay Ontario Canada and anybo...
published: 06 Feb 2012
author: SSFCstudybuddy
Rock and Mineral Identification
Rock and Mineral Identification
- published: 06 Feb 2012
- views: 140761
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author:
SSFCstudybuddy
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4:00
Geology Kitchen #3 - Clastic Sedimentary Rocks
Episode 3 begins to examine the world of sedimentary rocks by looking at how clastic sedim...
published: 31 Aug 2012
author: tkent22
Geology Kitchen #3 - Clastic Sedimentary Rocks
Geology Kitchen #3 - Clastic Sedimentary Rocks
- published: 31 Aug 2012
- views: 15706
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author:
tkent22
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3:34
GEOLOGY ROCKS! (Jasongs)
A true "rock" song. Check out the CD quality, stereo version along with a host of other gr...
published: 15 May 2009
author: Jason Arvanites
GEOLOGY ROCKS! (Jasongs)
GEOLOGY ROCKS! (Jasongs)
- published: 15 May 2009
- views: 28834
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author:
Jason Arvanites
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3:55
Geology, the rock cycle
the rock cycle....
published: 16 Oct 2008
author: John West
Geology, the rock cycle
Geology, the rock cycle
- published: 16 Oct 2008
- views: 10692
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author:
John West
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5:51
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Chemical and biological sedimentary rocks are discussed in this video. Carbonates, includi...
published: 01 Oct 2012
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
Geology Kitchen #5 - Chemical & Biological Sedimentary Rocks
- published: 01 Oct 2012
- views: 9711
5:57
Geology Kitchen #11 - Igneous Rocks
Igneous rocks are rocks derived from the cooling of magma, molten material originating fro...
published: 04 Feb 2013
author: tkent22
Geology Kitchen #11 - Igneous Rocks
Geology Kitchen #11 - Igneous Rocks
- published: 04 Feb 2013
- views: 11319
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tkent22
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1:27
Rock cycle - geology for kids
...
published: 12 Oct 2015
Rock cycle - geology for kids
Rock cycle - geology for kids
- published: 12 Oct 2015
- views: 1
0:26
Books of Sedimentary Rock Geology Rocks
Access to read more ebook: http://www.realbooknow.net/books...
published: 12 Oct 2015
Books of Sedimentary Rock Geology Rocks
Books of Sedimentary Rock Geology Rocks
- published: 12 Oct 2015
- views: 0
0:28
Rock-Rock
This video is just to show the different components of the game Rock-Rock.
How to play R...
published: 07 Oct 2015
Rock-Rock
Rock-Rock
- published: 07 Oct 2015
- views: 58
3:42
Rock Cycle - Geology For Kids - Learn about Rock
The Rock Cycle is a group of changes. Igneous rock can change into sedimentary rock or int...
published: 07 Oct 2015
Rock Cycle - Geology For Kids - Learn about Rock
Rock Cycle - Geology For Kids - Learn about Rock
- published: 07 Oct 2015
- views: 3
48:11
Geology for Engineers Sedimentary Rocks & Processes
Describes the processes that form sedimentary rocks and the classification of sedimentary ...
published: 07 Oct 2015
Geology for Engineers Sedimentary Rocks & Processes
Geology for Engineers Sedimentary Rocks & Processes
- published: 07 Oct 2015
- views: 4
2:00
Geology Rock Cycle Project
...
published: 05 Oct 2015
Geology Rock Cycle Project
Geology Rock Cycle Project
- published: 05 Oct 2015
- views: 3
22:33
Identification of fold structures in Sandstone and Shales - Geology Field Trip
Location: Beach to the west of Long Shank.
Description: Sand and rock beach with small sta...
published: 04 Oct 2015
Identification of fold structures in Sandstone and Shales - Geology Field Trip
Identification of fold structures in Sandstone and Shales - Geology Field Trip
- published: 04 Oct 2015
- views: 12
12:43
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
Location: Rocky foreshore below St Monans Church.
Description: Rock platform below Fife Co...
published: 04 Oct 2015
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
Rock platform below Fife Coast Path with dyke cross cutting - Field Trip Geology
- published: 04 Oct 2015
- views: 4
2:19
THE ROCK CYCLE GEOLOGY
...
published: 24 Sep 2015
THE ROCK CYCLE GEOLOGY
THE ROCK CYCLE GEOLOGY
- published: 24 Sep 2015
- views: 1
1:59
THE ROCK CYCLE GEOLOGY
...
published: 22 Sep 2015
THE ROCK CYCLE GEOLOGY
THE ROCK CYCLE GEOLOGY
- published: 22 Sep 2015
- views: 2
2:22
Geology of Raven Rock Arch
Geologist Brittany Parrick provides a brief discussion on the geology of Raven Rock Arch i...
published: 24 Sep 2015
Geology of Raven Rock Arch
Geology of Raven Rock Arch
- published: 24 Sep 2015
- views: 21
4:31
okayest geology presentation
The Rock Cycle by Levi Hanson, Cole Kyllonen, and Tristan Durfee...
published: 23 Sep 2015
okayest geology presentation
okayest geology presentation
- published: 23 Sep 2015
- views: 15
4:20
Geology Rock Cycle
Geology 1120-90
Mercedes Isensee
Ningozis White
Juliet McLellan
Raymond Klitsch
Cassandra...
published: 22 Sep 2015
Geology Rock Cycle
Geology Rock Cycle
- published: 22 Sep 2015
- views: 3
0:18
Engineering Geology Rock in Engineering Construction
Register to Browse more Ebooks
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http://mgpdf.net/free...
published: 20 Sep 2015
Engineering Geology Rock in Engineering Construction
Engineering Geology Rock in Engineering Construction
- published: 20 Sep 2015
- views: 0
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31:43
Igneous Rock Geology Lab Tutorial by Nancy
This is a Igneous Rock Tutorial done by fabulous a teacher named Nancy at a college in Sea...
published: 05 Apr 2015
Igneous Rock Geology Lab Tutorial by Nancy
Igneous Rock Geology Lab Tutorial by Nancy
- published: 05 Apr 2015
- views: 12
20:45
Geology Rocks instrumental Song Practice
*Instrumental ONLY*
Practice the songs for Geology Rocks right here! Just click on the in...
published: 17 May 2015
Geology Rocks instrumental Song Practice
Geology Rocks instrumental Song Practice
- published: 17 May 2015
- views: 4
28:33
EYEWITNESS | Rock & Mineral
Rock and Mineral (geology) - July 22, 1996...
published: 24 Apr 2015
EYEWITNESS | Rock & Mineral
EYEWITNESS | Rock & Mineral
- published: 24 Apr 2015
- views: 62
79:55
Professor Iain Stewart - Geology's 'Rock Star'
Geographer and geologist Iain Stewart is a Professor of Geosciences Communication at the U...
published: 19 May 2014
author: SELS
Professor Iain Stewart - Geology's 'Rock Star'
Professor Iain Stewart - Geology's 'Rock Star'
- published: 19 May 2014
- views: 184
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author:
SELS
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23:11
Sedimentary Rock Geology Lab Tutorial by Nancy
This is a Sedimentary Rock Tutorial done by fabulous a teacher named Nancy at a college in...
published: 03 Apr 2015
Sedimentary Rock Geology Lab Tutorial by Nancy
Sedimentary Rock Geology Lab Tutorial by Nancy
- published: 03 Apr 2015
- views: 7
20:35
Geology, PLate Tectonics and the Rock Cycle
Queen Nerdling describes geology, plate tectonics and then goes into the rock cycle....
published: 19 Jan 2015
Geology, PLate Tectonics and the Rock Cycle
Geology, PLate Tectonics and the Rock Cycle
- published: 19 Jan 2015
- views: 3
30:03
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in...
published: 07 Jun 2011
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 1
- published: 07 Jun 2011
- views: 3107
30:12
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
Dr. Andrew Snelling, one of the world's most respected Creation Scientists specializing in...
published: 07 Jun 2011
author: RockyMtnCreation
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
Radioisotope Dating of Rocks: Challenging an Icon of Evolutionary Geology - Dr. Snelling Part 2
- published: 07 Jun 2011
- views: 1295
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author:
RockyMtnCreation
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32:52
Geology Rocks! - Rancho Rosal 2nd Grade 2014
Mrs. Knauss' and Mrs. Myrick's second grade classes star in "Geology rocks!" - February 11...
published: 12 Feb 2014
author: Eric Wenschlag
Geology Rocks! - Rancho Rosal 2nd Grade 2014
Geology Rocks! - Rancho Rosal 2nd Grade 2014
- published: 12 Feb 2014
- views: 357
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author:
Eric Wenschlag
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26:38
Relative Dating of Rock Layers
How to determine to geologic sequence of events from a rock cross section....
published: 11 May 2014
Relative Dating of Rock Layers
Relative Dating of Rock Layers
- published: 11 May 2014
- views: 5004
59:56
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock...
published: 22 Sep 2014
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
Engineering Geology Lec 20 Stress Strain Behavior of Soil and Rock
- published: 22 Sep 2014
- views: 0
24:23
Geology of Table Rocks
Approximately 48 to 35 million years ago, the Payne Cliffs Formation was being deposited b...
published: 07 May 2015
Geology of Table Rocks
Geology of Table Rocks
- published: 07 May 2015
- views: 7
59:50
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II...
published: 22 Sep 2014
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
Engineering Geology Lec 21 Stress Strain Behavior of Soil and Rock II
- published: 22 Sep 2014
- views: 0
60:30
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass...
published: 22 Sep 2014
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
Engineering Geology Lec 19 Index Properties of Rock and Rock Mass
- published: 22 Sep 2014
- views: 2
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Igneous Rock Geology Lab Tutorial by Nancy...
Geology Rocks instrumental Song Practice...
EYEWITNESS | Rock & Mineral...
Professor Iain Stewart - Geology's 'Rock Star'...
Sedimentary Rock Geology Lab Tutorial by Nancy...
Geology, PLate Tectonics and the Rock Cycle...
Radioisotope Dating of Rocks: Challenging an Icon ...
Radioisotope Dating of Rocks: Challenging an Icon ...
Geology Rocks! - Rancho Rosal 2nd Grade 2014...
Relative Dating of Rock Layers...
Engineering Geology Lec 20 Stress Strain Behavior ...
Geology of Table Rocks...
Engineering Geology Lec 21 Stress Strain Behavior ...
Engineering Geology Lec 19 Index Properties of Roc...
Engineering Geology Lec 40 Identification of miner...
Lecture - 10 Igneous Rocks...
photo: US Navy / John F. Williams
The rise of the killer robots -- and why we need to stop them
Edit CNN 26 Oct 2015
(CNN)Lethal autonomous weapons (or as the media like to call them, "killer robots") were back on the agenda at the U.N. last week. The Campaign to Stop Killer Robots launched in 2013, and pleasingly the issue was quickly taken up by the U.N. Convention on Certain Conventional Weapons (CCW) in Geneva ... Here's five of them. 1. Killer robots are near ... This is technically possible today. Professor Toby Walsh. 2. There will be an arms race ... 3 ... 4 ... 5 ... ....
photo: AP / Ammar El-Darwish, File
Apex of Western Hypocrisy Is Executing Seif al-Islam Gaddafi
Edit WorldNews.com 26 Oct 2015
Article by WN.com Correspondent Dallas Darling. When a congressional aide asked Seif al-Islam Gaddafi what Libya needed, his one-word answer was “democracy.” Sitting in a black cage in a Libyan prison and awaiting execution –death by firing squad – Seif al-Islam, second son of late Libyan leader Muammar Gaddafi, is still in search of democracy ... Seif al-Islam, however, knows all about democracy and justice ... (1) www.wikipedia.com ... 222. ....
photo: AP / Channi Anand
Powerful Earthquake Hits Afghanistan, India, Pakistan
Edit Huffington Post 26 Oct 2015
KABUL, Oct 26 (Reuters) - A major earthquake struck northeastern Afghanistan on Monday, the U.S. Geological Survey said, shaking the capital Kabul and sending shockwaves that were felt in north India and Pakistan, where officials said four people had been killed ... Buildings shook for well over a minute in the Indian capital, New Delhi, sending office workers scurrying onto the streets ... ....
photo: Public Domain
Bacon, sausage and other processed meats do cause cancer – WHO
Edit The Miami Herald 26 Oct 2015
A research division of the World Health Organization announced on Monday that bacon, sausage and other processed meats cause cancer, and that red meat probably does, too. The report by the influential group stakes out one of the most aggressive stances against meat yet taken by a major health organization, and it is expected to face stiff criticism in the United States ... The $95 billion U.S ... cancer-who ....
photo: AP / Abdeljalil Bounhar
Morocco poised to become a solar superpower with launch of desert mega-project
Edit The Guardian 26 Oct 2015
World’s largest concentrated solar power plant, powered by the Saharan sun, set to help renewables provide almost half the country’s energy by 2020. The Moroccan city of Ouarzazate is used to big productions ... The project is a key plank in Morocco’s ambitions to use its untapped deserts to become a global solar superpower. Twitter ... The potential for solar power from the desert has been known for decades ... Campaign sign up ... Twitter ... Twitter ... ....
« back to news headlines
‘South Asia suffers more during quakes due to poor infrastructure’
Edit The Hindu 27 Oct 2015
A Geological Exploration of the Himalaya, Karakoram and Tibet ... As continental plates collide, the rocks are shortened by folding and thrusting. When the rocks break along a fault, earthquakes release the built-up stress. During large earthquakes, the rocks can move 5 or even 10 meters instantly ... Please explain the geological blueprint of this earthquake....
63 dead in Afghanistan
Edit Dawn 27 Oct 2015
It was centred near Jurm in northeast Afghanistan, 250 kilometres from Kabul and at a depth of 213.5 kilometres, the US Geological Survey said....
No harm done in Delhi as quake struck deep
Edit The Times of India 27 Oct 2015
The 7.5 magnitude trembler that rocked Afghanistan on Monday afternoon, was felt as far away as Bihar ... The US Geological Survey said that this earthquake occurred due to a rupture on "either a near-vertical reverse fault or a shallowly dipping thrust fault." ... Dr Saumitra Mukherjee, profes sor geology and remote sensing at JNU says that the quake ......
Mysterious Hemlock Stone scanned by drone
Edit BBC News 27 Oct 2015
Experts hope the drone scan will help perfect a 3D model for research ... However, to get a full picture of the monument's geological make-up, extensive scaffolding would have been needed to laser scan it from above ... He said ... It is believed The Hemlock Stone is linked to two other significant stones in Nottinghamshire, the Druid Stone at Blidworth and Bob's Rock at Stapleford ... ....
27.10.15 PAK Completes Elko Exploration Program (Metals Finance Limited)
Edit Public Technologies 27 Oct 2015
Having finalised the exploration program in Q3 2015, the Company has moved forward to advance the geological modelling of the Elko Coal Project and anticipates announcing a JORC (2012) Inferred Resource in Q4 2015 ... The Company engaged Highland GeoComputing (HGC) to lead the exploration program and to update the geological model at Elko ... Map coal seam outcrops, geological outcrops, faults, measured sections....
Energy Ministry Launches Interactive Apps at Gitex Read more (Ministry of Energy of the United ...
Edit Public Technologies 27 Oct 2015
HE Suhail bin Faraj Mohammed Fares Al Mazrouei, the Minister of Energy, today launched the interactive application 'mGeology', which is concerned with geological maps in the United Arab Emirates ... Matar Hamed Al Neyadi, Undersecretary of the Ministry of Energy, said that the Ministry has succeeded in turning the geological and geophysical studies of ......
Dusk Til Dawn Drilling Confirms Gold Discovery (Alloy Resources Limited)
Edit Public Technologies 27 Oct 2015
'The wide zones of mineralisation, along with favourable host rock geology and structural settings and some higher grade gold zones all lead us to believe that Dusk 'til Dawn is a significant new greenfields gold discovery, but is only the first of several potential opportunities within the wider Horse Well Project' ... intermediate volcanic rocks....
New lunar maps let you explore the moon from your couch
Edit Engadget 27 Oct 2015
The existing lunar maps used by the US Geological Survey are two years older than I am. But thanks to the tireless efforts of NASA's Lunar Reconnaissance Orbiter (LRO), Earthbound astronomers can get up close and personal with our planet's Gilligan... ....
Quartz Vs. Granite Countertops - A Geologist's Perspective
Edit Forbes 27 Oct 2015
As a geologist, I am commonly asked about the pros and cons of quartz vs. granite countertops, to identify the mineral assemblages within granite, and many more questions. Here I will outline the geology of granite and quarts, their source, physical attributes, durability, and environmental sustainability. In many ways a natural [...] ... ....
Rauner says union-opposed reforms 'critical' to budget deal
Edit The Washington Times 27 Oct 2015
ROCK ISLAND, Ill. (AP) - Illinois Gov. Bruce Rauner says he doesn't expect a budget agreement to come out of a planned meeting next month with legislative leaders. The Rock Island Argus reports (http.//bit.ly/1XuKxVs) that during a visit Monday to Rock Island, the Republican is insisting he won't agree to ... ....
Elvis Roxx -Helloween tickets
Edit Skiddle 27 Oct 2015
Land Rover Sports And Social Club in Solihull. Friday 30th October 2015 ... Minimum Age. 18. Helloween ELVIS ROXX “A Memphis edged, Hi Octane Rock Fest. Event Info. Venue ... The Cool of The King meets the Rock Gods...Black Sabbath, ... Live Rock Show Plus Monster Mash Disco ... Pop, Rock & Roll....
FEAR THE FALLEN + VOLTS + ARTIZANS + RIVER NORTH + GOD COMPLEX tickets
Edit Skiddle 27 Oct 2015
Formed late 2010 in Darwen Lancashire, Fear The Fallen are a powerful and original band that deliver a heavy rock based eclectic mix of riff-driven rock and classic sounds ... the boys combine rock-driven riffs with poppy vocals to create a unique sound ... The River North are Manchester based alternative rock trio who are loud and hard hitting with a mixture of riff driven songs and catchy choruses ... Alternative, Blues, Indie, Metal, Rock....
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