Foulger G., University of Durham

This webpage, published by G.R. Foulger on the website, argues against a simple deep-mantle plume as the origin of the Yellowstone hotspot. Foulger makes his case on the basis of a diverse number of geologic, geophysical, and structural observations, and argues that upper-mantle (< 200 km) processes can explain the observations. The site is accompanied by a variety of illustrations and a bibliography.

This resource is referenced here:
Subject: Geoscience:Geology:Geophysics, Structural Geology, Geochemistry
Resource Type: Audio/Visual:Images/Illustrations
Topics: Time/Earth History, Chemistry/Physics/Mathematics, Solid Earth:Structural Geology, Geochemistry, Solid Earth
Theme: Teach the Earth:Course Topics:Structural Geology, Geophysics, Geochemistry