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Iceland Rift Zone

Plate Tectonics

Professor John Wheeler

All

Students

1. Isostasy

Professor John Wheeler talks about isostasy using an analogue model.

1. IsostasyRead More

Professor John Wheeler

All

Students

2. Isostasy in layers on top of the mantle

Professor John Wheeler talks about the effect of layers on isostasy using an analogue model

2. Isostasy in layers on top of the mantleRead More

Professor John Wheeler talks about the effect of a point load

School

University

Students

3. Effects of a point load on lithospheric flexure

Professor John Wheeler talks about the effect of a point load and flexure of a lithospheric plate using an analogue model

3. Effects of a point load on lithospheric flexureRead More

Professor John Wheeler simulates the formation of a subduction zone

School

University

Students

4. Subduction Zones

Professor John Wheeler simulates the formation of a subduction zone using an analogue model

4. Subduction ZonesRead More

Professor John Wheeler shortening and folding in mountain belts

School

University

Students

5. Folding in mountain belts

Professor John Wheeler shortening and folding in mountain belts using an analogue model

5. Folding in mountain beltsRead More

Professor John Wheeler demonstrates what happens to the earth when an ice sheet melts

School

University

Students

6. The effect of Ice Sheet melting

Professor John Wheeler demonstrates what happens to the earth when an ice sheet melts using an analogue model

6. The effect of Ice Sheet meltingRead More

Pembrokeshire

College

School

Teachers

Global Tectonics

Suitable for school (GCSE) and college (A Level) students.

Global TectonicsRead More

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