Geological structures exposed - for iPad/Mac/PC
The Open UniversityUnderstanding mountain building involves unraveling how and why rocks deform. Geologists Nigel Harris and John Whalley tour the Scottish segment of the Caledonian orogenic Belt to untangle the kinematics and the chronology of deformation. This material forms part of The Open University course S339, Understanding the continents.
| Publishes | Daily | Episodes | 24 | Founded | 15 years ago |
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| Categories | CoursesEducation | ||||
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Transcript -- A short introduction to this album.
The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.
Transcript -- The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.
Evidence that the Moine Thrust is the result of frictional sliding.
Transcript -- Evidence that the Moine Thrust is the result of frictional sliding.
The ductility of structures of rocks from the Dalradian supergroup.
Transcript -- The ductility of structures of rocks from the Dalradian supergroup.
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