RJLiberator said:
What's the difference in using GPS Data vs. using Magnetic anomalies, fracture zones, hot spots to analyze plate motion?
Based on my limited knowledge of geology and geologic mapping, a common technique for analyzing plate motion is placing sensors on either side of the plate, and measuring (via GPS) their relative change in position.
Magnetic anomolies don't necessarily indicate plate motion, as far as I know. They can occur when there are large masses of some ferrous material beneath the surface. They can also occur in "stripes" on either side of a mid-ocean spreading site that is the junction of two plates. New ocean seafloor that is created at the spreading site extends out from the spreading site in two directions. The stripes of opposite polarity magnetism that appear on either side of the spreading zone are thought to occur due to the periodic switching of the Earth's magnetic field, and can be used to give an idea of how fast the seafloor is moving on either side of the spreading zone.
Fracture zones (see
https://en.wikipedia.org/wiki/Fracture_zone) result "from the action of offset
mid-ocean ridge axis segments.are regions in the ocean where there are numerous faults." (Taken from the wiki article.) These fracture zones indicate motion of one plate relative to another.
Hot spots, such as the one currently below Hawaii island (the "big island") and others, such as the one that is believed to cause massive outpourings of lava in Washington state before moving east to produce the caldera at Yellowstone) provide evidence of plate motion. The hot spots are believed to be stationary on the Earth's surface, while the plates slide across it. In the Hawaiian islands, the Pacific Plate is theorized as having moved NNW for a time, and then changing direction to about WNW (see
https://en.wikipedia.org/wiki/Evolution_of_Hawaiian_volcanoes). The most recent volcanic action is off the coast of Hawaii, at Lo ihi sea mount. The oldest volcanoes in the chain are in the Emporor Sea Mounts, many of which are so eroded that they are no longer above sea level.