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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.

PublishesDailyEpisodes24Founded14 years ago
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A short introduction to this album.

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14 years ago

Transcript -- A short introduction to this album.

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14 years ago

The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.

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15 years ago

Transcript -- The three main components of the Orogenic Belt; Lewisian gneisses, Torridonian sandstone and sediments laid down from Cambrian times.

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15 years ago

Evidence that the Moine Thrust is the result of frictional sliding.

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15 years ago

Transcript -- Evidence that the Moine Thrust is the result of frictional sliding.

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15 years ago

The ductility of structures of rocks from the Dalradian supergroup.

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15 years ago

Transcript -- The ductility of structures of rocks from the Dalradian supergroup.

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15 years ago

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