Geological structures exposed - for iPod/iPhone podcast

Geological structures exposed - for iPod/iPhone

The Open University

Understanding 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.

24 Episoden

Geological structures exposed
12.4.2010
0:36
A short introduction to this album.
Transcript -- Geological structures exposed
12.4.2010
Transcript -- A short introduction to this album.
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Overview of the Orogenic Belt
23.6.2009
4:55
The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.
Transcript -- Overview of the Orogenic Belt
23.6.2009
Transcript -- The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.
A history of movement
23.6.2009
4:21
Evidence that the Moine Thrust is the result of frictional sliding.
Transcript -- A history of movement
23.6.2009
Transcript -- Evidence that the Moine Thrust is the result of frictional sliding.
Ductility of the Structures
23.6.2009
1:18
The ductility of structures of rocks from the Dalradian supergroup.
Transcript -- Ductility of the Structures
23.6.2009
Transcript -- The ductility of structures of rocks from the Dalradian supergroup.
Kinematic indicators
23.6.2009
4:54
Evidence of indicators which suggest the direction of movement within slices of rock.
Transcript -- Kinematic indicators
23.6.2009
Transcript -- Evidence of indicators which suggest the direction of movement within slices of rock.

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