Geological structures exposed - for iPad/Mac/PC - podcast cover

Geological structures exposed - for iPad/Mac/PC

The Open Universitywww3.open.ac.uk
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.
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Episodes

Overview of the Orogenic Belt

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

Jun 23, 20095 min

A history of movement

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

Jun 23, 20094 min

Kinematic indicators

Evidence of indicators which suggest the direction of movement within slices of rock.

Jun 23, 20095 min

Shear Zone movement

An assymetric porphyroblast reveals a sense of movement within Myelenite gneissic banding.

Jun 23, 20093 min

Locating synforms

Asymmetric fold pairs and ductile structures in the inner zone at Scotlands Kilmore Bay.

Jun 23, 20094 min

Deformation history

Geologist John Whalley explains how in structural chronology downwards facing folds will cause the rock structure to start younging.

Jun 23, 20093 min

Transcript -- Deformation history

Transcript -- Geologist John Whalley explains how in structural chronology downwards facing folds will cause the rock structure to start younging.

Jun 23, 2009

460 million years ago

The evidence for an Arc-continent collision around 460 million years ago in the Scottish Highlands.

Jun 23, 20093 min
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