Geodynamics Seminar
12.753 · Earth, Atmospheric, and Planetary Sciences · Graduate · Spring 2001
Prof. Robert Sohn
<p>The Earth’s crust is primarily composed of melting products from mantle plumes and mid-ocean ridges - both presently and over the course of Earth history. While both systems represent upwelling features in a convective mantle, they can be viewed as end-member systems in that plumes represent buoyant flow whereas mid-ocean ridges represent passive corner flow. This paradigm is not strict - flow beneath ridges may be buoyant in some places, for example, but it does provide a reasonable framewo…
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Prof. Robert Sohn. 12.753 Geodynamics Seminar. Spring 2001. Massachusetts Institute of Technology: MIT OpenCourseWare, https://ocw.mit.edu. License: CC BY-NC-SA 4.0.
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