Professor John Wheeler talks about isostasy using an analogue model.
All
Students
1. Isostasy
2. Isostasy in layers on top of the mantle
Professor John Wheeler talks about the effect of layers on isostasy using an analogue model
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
4. Subduction Zones
Professor John Wheeler simulates the formation of a subduction zone using an analogue model
5. Folding in mountain belts
Professor John Wheeler shortening and folding in mountain belts using an analogue model
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
Global Tectonics
Suitable for school (GCSE) and college (A Level) students.