NASA's Role in Investigating Continental Drift

Plate tectonic theory has been highly successful in explaining many geological phenomena. NASA scientists using Satellite Laser Ranging (SLR) systems, Synthetic Aperture Radars (SAR), and Global Positioning Systems (GPS) study the geodynamics of Earth. Geodynamics is the study of the motion of the earth as well as the forces and processes active in the interior of the Earth. Through geodynamics we can learn how these hidden forces affect the features of the Earth's crust, namely, the continents we live on.

For example, SLR satellites show that the island of Maui, Hawaii, is moving northwest toward Japan at approximately 3 inches (7 cm) per year. Plate tectonic theory predicts motion in that direction of approximately 4 inches (9 cm) per year. Maui also is moving away from South America at approximately 3 inches (8 cm) per year, close to the 2 inches (6 cm) per year predicted by plate tectonics.

The Southern California Integrated GPS Network (SCIGN) is a group of connected GPS receivers which are used to monitor the build-up of strain along the two tectonic plates which are touching in southern California. This is done by measuring very small movements at faults that aren't usually noticeable.


SAR Interferometry results for the 1992 Landers, CA earthquake.

Synthetic Aperture Radars (SAR) produce all-weather, day and night, high quality pictures of the Earth's surface. By combining two or more pictures of the same area, it's possible to make maps that are highly detailed and show useful information about an area. This technique is called SAR interferometry. SAR interferometry has been applied to the study of earthquakes, volcanoes, glacier flow, landslides, and other geologic events.

All these techniques should lead to a better understanding of the occurrence of earthquakes at plate boundaries, vulcanism, and the cause of mountain building. It may eventually tell us if Wegener's theory of continental drift can be explained by plate tectonics.



Updated: January 22, 2003
Picture of LAGEOS II satellite.
The LAGEOS II satellite, built by the Italian Space Agency, Agenzia Spaziale Italiana (ASI), and managed by NASA's Goddard Space Flight Center, measures crustal movement by using Satellite Laser Ranging technology. It is only 24 inches (60 cm) in diameter, yet because of it's brass core, weighs approximately 900 pounds (405 kg). This compact, dense design was selected to make the satellite's orbit as stable as possible. Click here to find out more about LAGEOS I & II.

SLR system in Greenbelt, Maryland.
The above picture is of a Satellite Laser Ranging (SLR) system operating in Greenbelt, Maryland. For more information on SLR systems, click here.


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