-
Why There's a Straight Line Through Scotland
If you take a look at a map of Scotland, you'll notice an eerily straight line running through the highlands, this is the Great Glen Fault the product of half a billion years of time and geology.
Hosted by: Stefan Chin
SciShow has a spinoff podcast! It's called SciShow Tangents. Check it out at http://www.scishowtangents.org
----------
Support SciShow by becoming a patron on Patreon: https://www.patreon.com/scishow
----------
Huge thanks go to the following Patreon supporters for helping us keep SciShow free for everyone forever:
Chris Peters, Matt Curls, Kevin Bealer, Jeffrey Mckishen, Jacob, Christopher R Boucher, Nazara, charles george, Christoph Schwanke, Ash, Silas Emrys, KatieMarie Magnone, Eric Jensen, Adam Brainard, Piya Shedden, Alex Hackman, James Knight, GrowingViolet, Sam L...
published: 05 Aug 2021
-
Variscan orogeny
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
Nomenclature.
The name Variscan, comes from the Medieval Latin name for the district Variscia, the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. (Variscite, a rare green mineral first discovered in the Vogtland district of Saxony in Germany, which is in the Variscan belt, has the same etymology.)
Hercynian, on the other hand, derives from the Hercynian Forest. Both words were descriptive terms of strike directions observed by geologists in the field, variscan for southwest to northeast, hercynian for northwe...
published: 26 May 2020
-
Continental drift animation centred on the UK
This animation of continental drift shows how the two part of Britain have coaleced and moved across the equator during the past 450 million years
published: 19 Oct 2011
-
Variská orogeneze/ Variscan orogeny
Během variských horotvorných procesů došlo ke sjednocení různých horninových celků odlišného složení a stáří v jeden celek, který dnes tvoří základ českého masivu. Právě v horninách na území České republiky je zaznamenán tento jedinečný geologický vývojový cyklus, který se odehrával v období středního devonu a karbonu, až v hloubkách 80 km pod tehdejším povrchem.
© Česká geologická služba
During the Variscan mountain-building processes, various rock units of different composition and age were united into one unit, which today forms the base of the Bohemian Massif. This unique geological evolution cycle, which occurred in the Middle Devonian and Carboniferous, is recorded precisely in the rocks in the Czech Republic up to depths of 80 km beneath the then surface.
© Czech geological survey...
published: 13 Nov 2015
-
Variscan orogeny
If you find our videos helpful you can support us by buying something from amazon.
https://www.amazon.com/?tag=wiki-audio-20
Variscan orogeny
=======Image-Copyright-Info========
License: Creative Commons Attribution-Share Alike 1.0 (CC BY-SA 1.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/1.0
Author-Info: Woudloper
Image Source: https://en.wikipedia.org/wiki/File:Hercynides_EN.svg
=======Image-Copyright-Info========
☆Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
image source in video
published: 01 Jan 2016
-
Mountain Building Animation
This animation shows how the collision of India and Eurasia, which started about 50 million years ago and continues to this day, formed the Himalayas and the Tibetan Plateau.
Credit: Kristel Chanard, Tectonics Observatory, California Institute of Technology; Tim Pyle, California Institute of Technology
published: 08 Dec 2010
-
Geographic evolution of Europe
Another video showing the evolution of Southern Europe in each geographic era. Created by adding up morphed still images.
published: 04 Feb 2011
-
Orogeny Geological Formation of North America: 600 Million Years Ago To Present
Sloss Diagram and Phanerozoic Evolution of North America:
This animation shows the relationship of: (1) the geologic evolution of North America from the latest Precambrian (600 Ma) to the Present (right), and (2) the distribution of the six major stratigraphic sequences in time and space for North America, as defined by Larry Sloss (1963) (left).
On the chart, the vertical axis shows geologic time (from 600 million years (base) to the Present). The horizontal scale is in distance and indicates where sedimentation was occurring on the North American continent. The orientation of the diagram is roughly east (right side) to west (left side). The orange areas in the central part of the chart show where no sediments were deposited (i.e. hiatus). The white area indicates where sediments were ...
published: 28 Sep 2018
-
Formation of the Mediterranean and the Alps
Popularized and animated description formation of the Mediterranean west, Pre-Alps and the Leman lake
en français. https://youtu.be/S0YRd978pHE
in italiano: https://youtu.be/OiZMzd6I0RA
en español: https://youtu.be/45J_f8mjC08
published: 29 Apr 2015
-
Assembly of the Alps
This video is a simplified view of the geologic assembly of the European Alps.
published: 28 Feb 2016
3:00
Why There's a Straight Line Through Scotland
If you take a look at a map of Scotland, you'll notice an eerily straight line running through the highlands, this is the Great Glen Fault the product of half a...
If you take a look at a map of Scotland, you'll notice an eerily straight line running through the highlands, this is the Great Glen Fault the product of half a billion years of time and geology.
Hosted by: Stefan Chin
SciShow has a spinoff podcast! It's called SciShow Tangents. Check it out at http://www.scishowtangents.org
----------
Support SciShow by becoming a patron on Patreon: https://www.patreon.com/scishow
----------
Huge thanks go to the following Patreon supporters for helping us keep SciShow free for everyone forever:
Chris Peters, Matt Curls, Kevin Bealer, Jeffrey Mckishen, Jacob, Christopher R Boucher, Nazara, charles george, Christoph Schwanke, Ash, Silas Emrys, KatieMarie Magnone, Eric Jensen, Adam Brainard, Piya Shedden, Alex Hackman, James Knight, GrowingViolet, Sam Lutfi, Alisa Sherbow, Jason A Saslow, Dr. Melvin Sanicas
----------
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----------
Sources:
https://earthquake.usgs.gov/learn/glossary/?term=strike-slip
https://www.geolsoc.org.uk/Plate-Tectonics/Chap4-Plate-Tectonics-of-the-UK/Caledonian-Orogeney
https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1998TC900033
https://www.geo.fu-berlin.de/en/geol/fachrichtungen/geologie/mitarbeiter_neu/Professoren/elinelebreton/LeBreton-etal_13_GGF.pdf
https://www.researchgate.net/publication/258616891_Cenozoic_reactivation_of_the_Great_Glen_Fault_Scotland_additional_evidence_and_possible_causes
https://www.tandfonline.com/doi/full/10.1080/17445647.2013.866369
https://agupubs.onlinelibrary.wiley.com/doi/pdfdirect/10.1029/1998TC900033
https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3585.html
https://www.usgs.gov/science-support/osqi/youth-education-science/cenozoic
https://www.gsi.ie/en-ie/geoscience-topics/geology/Pages/Geology-of-Ireland.aspx
https://www.rte.ie/brainstorm/2018/0315/947589-ireland-on-ice-how-the-ice-age-influenced-our-placenames/
https://www.geolsoc.org.uk/Policy-and-Media/Outreach/Plate-Tectonic-Stories/Great-Glen-Fault
https://courses.lumenlearning.com/suny-earthscience/chapter/tectonic-stress-and-geologic-structures-2/
https://www.nationalgeographic.com/science/article/plate-tectonics
Images:
https://en.wikipedia.org/wiki/Great_Glen#/media/File:Great_Glen_Project_Station_M_-_geograph.org.uk_-_818230.jpg
https://commons.wikimedia.org/wiki/File:Great_Glen_Fault_map.png
https://commons.wikimedia.org/wiki/File:Scotland_from_satellite.jpg
https://wn.com/Why_There's_A_Straight_Line_Through_Scotland
If you take a look at a map of Scotland, you'll notice an eerily straight line running through the highlands, this is the Great Glen Fault the product of half a billion years of time and geology.
Hosted by: Stefan Chin
SciShow has a spinoff podcast! It's called SciShow Tangents. Check it out at http://www.scishowtangents.org
----------
Support SciShow by becoming a patron on Patreon: https://www.patreon.com/scishow
----------
Huge thanks go to the following Patreon supporters for helping us keep SciShow free for everyone forever:
Chris Peters, Matt Curls, Kevin Bealer, Jeffrey Mckishen, Jacob, Christopher R Boucher, Nazara, charles george, Christoph Schwanke, Ash, Silas Emrys, KatieMarie Magnone, Eric Jensen, Adam Brainard, Piya Shedden, Alex Hackman, James Knight, GrowingViolet, Sam Lutfi, Alisa Sherbow, Jason A Saslow, Dr. Melvin Sanicas
----------
Looking for SciShow elsewhere on the internet?
Facebook: http://www.facebook.com/scishow
Twitter: http://www.twitter.com/scishow
Tumblr: http://scishow.tumblr.com
Instagram: http://instagram.com/thescishow
----------
Sources:
https://earthquake.usgs.gov/learn/glossary/?term=strike-slip
https://www.geolsoc.org.uk/Plate-Tectonics/Chap4-Plate-Tectonics-of-the-UK/Caledonian-Orogeney
https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1998TC900033
https://www.geo.fu-berlin.de/en/geol/fachrichtungen/geologie/mitarbeiter_neu/Professoren/elinelebreton/LeBreton-etal_13_GGF.pdf
https://www.researchgate.net/publication/258616891_Cenozoic_reactivation_of_the_Great_Glen_Fault_Scotland_additional_evidence_and_possible_causes
https://www.tandfonline.com/doi/full/10.1080/17445647.2013.866369
https://agupubs.onlinelibrary.wiley.com/doi/pdfdirect/10.1029/1998TC900033
https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3585.html
https://www.usgs.gov/science-support/osqi/youth-education-science/cenozoic
https://www.gsi.ie/en-ie/geoscience-topics/geology/Pages/Geology-of-Ireland.aspx
https://www.rte.ie/brainstorm/2018/0315/947589-ireland-on-ice-how-the-ice-age-influenced-our-placenames/
https://www.geolsoc.org.uk/Policy-and-Media/Outreach/Plate-Tectonic-Stories/Great-Glen-Fault
https://courses.lumenlearning.com/suny-earthscience/chapter/tectonic-stress-and-geologic-structures-2/
https://www.nationalgeographic.com/science/article/plate-tectonics
Images:
https://en.wikipedia.org/wiki/Great_Glen#/media/File:Great_Glen_Project_Station_M_-_geograph.org.uk_-_818230.jpg
https://commons.wikimedia.org/wiki/File:Great_Glen_Fault_map.png
https://commons.wikimedia.org/wiki/File:Scotland_from_satellite.jpg
- published: 05 Aug 2021
- views: 3607718
7:48
Variscan orogeny
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwa...
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
Nomenclature.
The name Variscan, comes from the Medieval Latin name for the district Variscia, the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. (Variscite, a rare green mineral first discovered in the Vogtland district of Saxony in Germany, which is in the Variscan belt, has the same etymology.)
Hercynian, on the other hand, derives from the Hercynian Forest. Both words were descriptive terms of strike directions observed by geologists in the field, variscan for southwest to northeast, hercynian for northwest to southeast. The variscan direction reflected the direction of ancient fold belts cropping out throughout Germany and adjacent countries and the meaning shifted from direction to the fold belt proper.
One of the pioneers in research on the Variscan fold belt was the German geologist Franz Kossmat, establishing a still valid division of the European Variscides in 1927.
The other direction, Hercynian, for the direction of the Harz Mountains in Germany, saw a similar shift in meaning. Today, Hercynian is often used as a synonym for Variscan but is somewhat less used than the latter. In the United States, it is used only for European orogenies; the contemporaneous and genetically linked mountain-building phases in the Appalachian Mountains have different names.
The regional term Variscan underwent a further meaning shift since the 1960s. Geologists generally began to use it to characterize late Paleozoic fold-belts and orogenic phases having an age of approximately 380 to 280 Ma.
Some publications use the term Variscan for fold belts of even younger age, deviating from the meaning as a term for the North American and European orogeny related to the Gondwana-Laurasia collision.
Distribution.
The North American and European Variscan Belt includes the mountains of Portugal and Spain (Galicia, and Pyrenees), southwestern Ireland (i.e. Munster), Cornwall, Devon, Pembrokeshire, the Gower Peninsula and the Vale of Glamorgan. Its effects are present in France from Brittany, below the Paris Basin to the Ardennes, the Massif Central, the Vosges and Corsica.
The Variscan Belt reappears in Sardinia in Italy and in Germany where the Rhine Massif (Ardennes, Eifel, Hunsrück, Taunus and other regions on both sides of Middle Rhine Valley), the Black Forest and Harz Mountains remain as testimony. In southern Iberia it is marked by a classic strike-slip suture zone between very distinct suspect terranes, and clear evidence can be seen of ductile shearing between high-grade metamorphic rocks and lower grade sedimentary rocks in a wide belt north of the Algarve and extending into the northernmost part the autonomous region of Andalusia and southern Extremadura.
In the Czech Republic and southwestern Poland the Bohemian Massif is the eastern end of the unmodified Variscan belt of crustal deformation in Europe. Further Variscan developments to the southeast are partly hidden and overprinted by the Alpine orogeny.
https://wn.com/Variscan_Orogeny
The Variscan or Hercynian orogeny is a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.
Nomenclature.
The name Variscan, comes from the Medieval Latin name for the district Variscia, the home of a Germanic tribe, the Varisci; Eduard Suess, professor of geology at the University of Vienna, coined the term in 1880. (Variscite, a rare green mineral first discovered in the Vogtland district of Saxony in Germany, which is in the Variscan belt, has the same etymology.)
Hercynian, on the other hand, derives from the Hercynian Forest. Both words were descriptive terms of strike directions observed by geologists in the field, variscan for southwest to northeast, hercynian for northwest to southeast. The variscan direction reflected the direction of ancient fold belts cropping out throughout Germany and adjacent countries and the meaning shifted from direction to the fold belt proper.
One of the pioneers in research on the Variscan fold belt was the German geologist Franz Kossmat, establishing a still valid division of the European Variscides in 1927.
The other direction, Hercynian, for the direction of the Harz Mountains in Germany, saw a similar shift in meaning. Today, Hercynian is often used as a synonym for Variscan but is somewhat less used than the latter. In the United States, it is used only for European orogenies; the contemporaneous and genetically linked mountain-building phases in the Appalachian Mountains have different names.
The regional term Variscan underwent a further meaning shift since the 1960s. Geologists generally began to use it to characterize late Paleozoic fold-belts and orogenic phases having an age of approximately 380 to 280 Ma.
Some publications use the term Variscan for fold belts of even younger age, deviating from the meaning as a term for the North American and European orogeny related to the Gondwana-Laurasia collision.
Distribution.
The North American and European Variscan Belt includes the mountains of Portugal and Spain (Galicia, and Pyrenees), southwestern Ireland (i.e. Munster), Cornwall, Devon, Pembrokeshire, the Gower Peninsula and the Vale of Glamorgan. Its effects are present in France from Brittany, below the Paris Basin to the Ardennes, the Massif Central, the Vosges and Corsica.
The Variscan Belt reappears in Sardinia in Italy and in Germany where the Rhine Massif (Ardennes, Eifel, Hunsrück, Taunus and other regions on both sides of Middle Rhine Valley), the Black Forest and Harz Mountains remain as testimony. In southern Iberia it is marked by a classic strike-slip suture zone between very distinct suspect terranes, and clear evidence can be seen of ductile shearing between high-grade metamorphic rocks and lower grade sedimentary rocks in a wide belt north of the Algarve and extending into the northernmost part the autonomous region of Andalusia and southern Extremadura.
In the Czech Republic and southwestern Poland the Bohemian Massif is the eastern end of the unmodified Variscan belt of crustal deformation in Europe. Further Variscan developments to the southeast are partly hidden and overprinted by the Alpine orogeny.
- published: 26 May 2020
- views: 4285
0:46
Continental drift animation centred on the UK
This animation of continental drift shows how the two part of Britain have coaleced and moved across the equator during the past 450 million years
This animation of continental drift shows how the two part of Britain have coaleced and moved across the equator during the past 450 million years
https://wn.com/Continental_Drift_Animation_Centred_On_The_UK
This animation of continental drift shows how the two part of Britain have coaleced and moved across the equator during the past 450 million years
- published: 19 Oct 2011
- views: 137284
0:31
Variská orogeneze/ Variscan orogeny
Během variských horotvorných procesů došlo ke sjednocení různých horninových celků odlišného složení a stáří v jeden celek, který dnes tvoří základ českého masi...
Během variských horotvorných procesů došlo ke sjednocení různých horninových celků odlišného složení a stáří v jeden celek, který dnes tvoří základ českého masivu. Právě v horninách na území České republiky je zaznamenán tento jedinečný geologický vývojový cyklus, který se odehrával v období středního devonu a karbonu, až v hloubkách 80 km pod tehdejším povrchem.
© Česká geologická služba
During the Variscan mountain-building processes, various rock units of different composition and age were united into one unit, which today forms the base of the Bohemian Massif. This unique geological evolution cycle, which occurred in the Middle Devonian and Carboniferous, is recorded precisely in the rocks in the Czech Republic up to depths of 80 km beneath the then surface.
© Czech geological survey
https://wn.com/Variská_Orogeneze_Variscan_Orogeny
Během variských horotvorných procesů došlo ke sjednocení různých horninových celků odlišného složení a stáří v jeden celek, který dnes tvoří základ českého masivu. Právě v horninách na území České republiky je zaznamenán tento jedinečný geologický vývojový cyklus, který se odehrával v období středního devonu a karbonu, až v hloubkách 80 km pod tehdejším povrchem.
© Česká geologická služba
During the Variscan mountain-building processes, various rock units of different composition and age were united into one unit, which today forms the base of the Bohemian Massif. This unique geological evolution cycle, which occurred in the Middle Devonian and Carboniferous, is recorded precisely in the rocks in the Czech Republic up to depths of 80 km beneath the then surface.
© Czech geological survey
- published: 13 Nov 2015
- views: 10233
7:07
Variscan orogeny
If you find our videos helpful you can support us by buying something from amazon.
https://www.amazon.com/?tag=wiki-audio-20
Variscan orogeny
=======Image-Co...
If you find our videos helpful you can support us by buying something from amazon.
https://www.amazon.com/?tag=wiki-audio-20
Variscan orogeny
=======Image-Copyright-Info========
License: Creative Commons Attribution-Share Alike 1.0 (CC BY-SA 1.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/1.0
Author-Info: Woudloper
Image Source: https://en.wikipedia.org/wiki/File:Hercynides_EN.svg
=======Image-Copyright-Info========
☆Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
image source in video
https://wn.com/Variscan_Orogeny
If you find our videos helpful you can support us by buying something from amazon.
https://www.amazon.com/?tag=wiki-audio-20
Variscan orogeny
=======Image-Copyright-Info========
License: Creative Commons Attribution-Share Alike 1.0 (CC BY-SA 1.0)
LicenseLink: http://creativecommons.org/licenses/by-sa/1.0
Author-Info: Woudloper
Image Source: https://en.wikipedia.org/wiki/File:Hercynides_EN.svg
=======Image-Copyright-Info========
☆Video is targeted to blind users
Attribution:
Article text available under CC-BY-SA
image source in video
- published: 01 Jan 2016
- views: 4371
0:16
Mountain Building Animation
This animation shows how the collision of India and Eurasia, which started about 50 million years ago and continues to this day, formed the Himalayas and the Ti...
This animation shows how the collision of India and Eurasia, which started about 50 million years ago and continues to this day, formed the Himalayas and the Tibetan Plateau.
Credit: Kristel Chanard, Tectonics Observatory, California Institute of Technology; Tim Pyle, California Institute of Technology
https://wn.com/Mountain_Building_Animation
This animation shows how the collision of India and Eurasia, which started about 50 million years ago and continues to this day, formed the Himalayas and the Tibetan Plateau.
Credit: Kristel Chanard, Tectonics Observatory, California Institute of Technology; Tim Pyle, California Institute of Technology
- published: 08 Dec 2010
- views: 298153
1:10
Geographic evolution of Europe
Another video showing the evolution of Southern Europe in each geographic era. Created by adding up morphed still images.
Another video showing the evolution of Southern Europe in each geographic era. Created by adding up morphed still images.
https://wn.com/Geographic_Evolution_Of_Europe
Another video showing the evolution of Southern Europe in each geographic era. Created by adding up morphed still images.
- published: 04 Feb 2011
- views: 93301
2:05
Orogeny Geological Formation of North America: 600 Million Years Ago To Present
Sloss Diagram and Phanerozoic Evolution of North America:
This animation shows the relationship of: (1) the geologic evolution of North America from the latest...
Sloss Diagram and Phanerozoic Evolution of North America:
This animation shows the relationship of: (1) the geologic evolution of North America from the latest Precambrian (600 Ma) to the Present (right), and (2) the distribution of the six major stratigraphic sequences in time and space for North America, as defined by Larry Sloss (1963) (left).
On the chart, the vertical axis shows geologic time (from 600 million years (base) to the Present). The horizontal scale is in distance and indicates where sedimentation was occurring on the North American continent. The orientation of the diagram is roughly east (right side) to west (left side). The orange areas in the central part of the chart show where no sediments were deposited (i.e. hiatus). The white area indicates where sediments were being deposited (various shades of blue on the map). The purple triangles on the left and right side of the diagram indicate the timing major orogenies (times of mountain building). The horizontal red line indicates the geologic time being shown on the chart and matches the geologic time shown on the map.
The video demonstrates four concepts:
(1) the movement of geologic plates through time;
(2) the movements of the oceans through time,
(3) how North America has been repeatedly below and above sea level during its geologic history,
(4) the distribution of Sloss sequences and how they are related to the paleo-geographic map view.
The maps are courtesy of and reproduced with the permission of Professor Ron Blakey, Colorado Plateau Geosystems (cpgeosystems.com). Video is created by Jay Austin, Kris Schwendeman, and Paul Weimer. Interactive Geology Project, University of Colorado-Boulder. igp.colorado.edu
Source: https://vimeo.com/84255718
Subscribe to our channel to get notified about our latest videos.
For more information and updates, follow us on our Rockstone Research social media channels.
Facebook: https://www.facebook.com/RockstoneResearch
Twitter: https://twitter.com/RockstoneRes
LinkedIn: https://www.linkedin.com/company/rockstone-research-ltd-/
Media disclaimer: https://www.zimtu.com/media-disclaimer/
https://wn.com/Orogeny_Geological_Formation_Of_North_America_600_Million_Years_Ago_To_Present
Sloss Diagram and Phanerozoic Evolution of North America:
This animation shows the relationship of: (1) the geologic evolution of North America from the latest Precambrian (600 Ma) to the Present (right), and (2) the distribution of the six major stratigraphic sequences in time and space for North America, as defined by Larry Sloss (1963) (left).
On the chart, the vertical axis shows geologic time (from 600 million years (base) to the Present). The horizontal scale is in distance and indicates where sedimentation was occurring on the North American continent. The orientation of the diagram is roughly east (right side) to west (left side). The orange areas in the central part of the chart show where no sediments were deposited (i.e. hiatus). The white area indicates where sediments were being deposited (various shades of blue on the map). The purple triangles on the left and right side of the diagram indicate the timing major orogenies (times of mountain building). The horizontal red line indicates the geologic time being shown on the chart and matches the geologic time shown on the map.
The video demonstrates four concepts:
(1) the movement of geologic plates through time;
(2) the movements of the oceans through time,
(3) how North America has been repeatedly below and above sea level during its geologic history,
(4) the distribution of Sloss sequences and how they are related to the paleo-geographic map view.
The maps are courtesy of and reproduced with the permission of Professor Ron Blakey, Colorado Plateau Geosystems (cpgeosystems.com). Video is created by Jay Austin, Kris Schwendeman, and Paul Weimer. Interactive Geology Project, University of Colorado-Boulder. igp.colorado.edu
Source: https://vimeo.com/84255718
Subscribe to our channel to get notified about our latest videos.
For more information and updates, follow us on our Rockstone Research social media channels.
Facebook: https://www.facebook.com/RockstoneResearch
Twitter: https://twitter.com/RockstoneRes
LinkedIn: https://www.linkedin.com/company/rockstone-research-ltd-/
Media disclaimer: https://www.zimtu.com/media-disclaimer/
- published: 28 Sep 2018
- views: 106934
10:59
Formation of the Mediterranean and the Alps
Popularized and animated description formation of the Mediterranean west, Pre-Alps and the Leman lake
en français. https://youtu.be/S0YRd978pHE
in italiano: ...
Popularized and animated description formation of the Mediterranean west, Pre-Alps and the Leman lake
en français. https://youtu.be/S0YRd978pHE
in italiano: https://youtu.be/OiZMzd6I0RA
en español: https://youtu.be/45J_f8mjC08
https://wn.com/Formation_Of_The_Mediterranean_And_The_Alps
Popularized and animated description formation of the Mediterranean west, Pre-Alps and the Leman lake
en français. https://youtu.be/S0YRd978pHE
in italiano: https://youtu.be/OiZMzd6I0RA
en español: https://youtu.be/45J_f8mjC08
- published: 29 Apr 2015
- views: 93783
7:59
Assembly of the Alps
This video is a simplified view of the geologic assembly of the European Alps.
This video is a simplified view of the geologic assembly of the European Alps.
https://wn.com/Assembly_Of_The_Alps
This video is a simplified view of the geologic assembly of the European Alps.
- published: 28 Feb 2016
- views: 27242