Do areas of persistent volcanic activity that burn through the lithosphere, the part of Earth's outer layer that contains the crust and the upper part of the mantle, remain in a fixed location as to act as a reference point? Can we use remnants of persistent volcanic activity in the ocean floor to track tectonic plate motion?
Areas like the Hawaiian Islands and large calderas as thought to exist in Yellowstone Park in Wyoming are fed by hot-spots. In common terms hot spots are more or less exactly what the name implies. They are isolated areas of increased heat flow that convect magma from deep within our earth and persist over geological time spans.
Hot-spots are theorized to originate in the upper mantle or as deep as the core-mantle boundary where the D" Layer, a theoretical thin layer of the earth separating the liquid outer core from the solid inner mantle and accompanied by a defiant change in seismic waves and crystal structure of existing rock mass, exists. They do not streamline right to the surface, but rather feed large plumes of hot magma that flow through cracks and find the path of least resistance as the attempt to surface.
They can either cause extrusive or intrusive igneous bodies to form. Extrusive, meaning they surface through volcanic activity or intrusive meaning they do not surface, but rather cool and solidify within the crustal segment of the lithosphere.
As you may recall from reading "China's Earthquake and the Indus-Yarlung Suture Zone", plate tectonic theory divides Earth's crust into thin, rigid segments that move horizontally and adjoin other plates. Hot-spots are thought to remain in a fixed location as tectonic plates float and pass over the plume of hot magma that is fed by these laminar-like flow patterns.
The Hawaiian Islands may be the best example of how a hot spot that feeds island volcanoes has seemingly remained in a fixed location for at least 40 to 80 million years. The erupting magmas have formed what is presently referred to as the Hawaiian-Emperor seamount chain. There is an obvious change in the Pacific Plate motion around 50 to 40 MYA. Other than the sharp bend observed during this time frame, the plate seems to move uniformly. Is this abnormal and can we rely on the superposition of these laminar-like flow patterns to dispel plate motion?
Resources:
http://www.platetectonics.com/book/page_17.asp
http://www.gasd.k12.pa.us/~dpompa/Mini%20Lecture.html
http://en.wikipedia.org/wiki/Hotspot_(geology)
http://www.wwnorton.com/college/geo/egeo2/content/animations/2_6.htm
http://www.gps.caltech.edu/~gurnis/Movies/Animated_GIFs/Pyre_global-plume.gif
http://www.cems.umn.edu/research/wentzcovitch/highlights/science_now_040324.htm
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