Professor John Wheeler demonstrates what happens to the earth when an ice sheet melts using an analogue model
School
University
Students
The effect of Ice Sheet melting
Folding in mountain belts
Professor John Wheeler shortening and folding in mountain belts using an analogue model
Subduction Zones
Professor John Wheeler simulates the formation of a subduction zone using an analogue model
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
Isostasy in layers on top of the mantle
Professor John Wheeler talks about the effect of layers on isostasy using an analogue model
Isostasy
Professor John Wheeler talks about isostasy using an analogue model.
Global Tectonics
Suitable for school (GCSE) and college (A Level) students.