1. Isostasy
Professor John Wheeler talks about isostasy using an analogue model.
All Levels
Students
Professor John Wheeler talks about isostasy using an analogue model.
All Levels
Students
Professor John Wheeler talks about the effect of layers on isostasy using an analogue model
School
University
Students
Professor John Wheeler talks about the effect of a point load and flexure of a lithospheric plate using an analogue model
School
University
Students
Professor John Wheeler simulates the formation of a subduction zone using an analogue model
School
University
Students
Professor John Wheeler shortening and folding in mountain belts using an analogue model
School
University
Students
Professor John Wheeler demonstrates what happens to the earth when an ice sheet melts using an analogue model
College
School
Teachers
Suitable for school (GCSE) and college (A Level) students.