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Course Documents
Current Location: Lithospheric Plates
[ Unit 2 - Tectonic Processes and Origin of the Earth ] : [ Class 6: Continents in Motion ] : Lithospheric Plates
Document Class 6: Lithosphere


Visit the following website to obtain both an overview and details about plate tectonics. This site, "The Story of Plate Tectonics," plus the indicated pages in BP, provide very good information and illustrations on all aspects of plate tectonics. We ask that you look at the entire site now by pressing the links provided within each graphic image:

 

continent picture: part of pangea red arrow pointing left The content can be found in the active external links.
HISTORICAL PERSPECTIVE (USGS): The purpose of this website is to introduce the student to the historical perspective of how the earth formed. It provides the multiple paradigms forwarded by geologist’s during the past few centuries.

mid-atlantic ridge 'Developing the Theory of Plate Tectonics': This excellent site from the U. S. Geological Survey provides an historical perspective on development of the theory. You will also find more information on plate motions, hotspots, unanswered questions, and people and plate tectonics. Excellent illustrations and text.

 

diverging plates GEOLOGY- Plate Tectonics: From the Museum of Paleontology at the University of California provides animations of the continents changing positions during geologic time. Go directly to the animations. The animations showing motion of continents relative to one another are very good. Also, there are links to concise information about sea floor spreading, magnetic anomalies on the sea floor, and the historical development of plate tectonics. From this site you will find animations for divergent, convergent, and transformational plate tectonics.

 

transform plate boundaries "The Story of Plate Tectonics." (USGS): It shows divergent (spreading ridge or rift zone), convergent, and transform plate boundaries as illustrated in the Earth. Press the link button entitled “Understanding Plate Motions” to read more information about these types of plate boundaries. Use this lithospheric plate motion site to view simple and effective animations showing how plates move with respect to one-another. As illustrated in the website, hands may be used to demonstrate the concepts of plate movement. (please note: Visit the page below only if you do not recall the different types of plate boundaries.)

 

Question: What are the essential differences between divergent, convergent, and transform plate boundaries?

 

Do we know that lithospheric plates are moving today?

Yes, we now have convincing evidence that the plates are moving! By using the Global Positioning System(GPS), it is possible to demonstrate that lithospheric plates move relative to each other, and determine how far they move each year. GPS consists of a network of 24 satellites, each in circular orbit 20,200 kilometers above the Earth. These satellites send signals to GPS receivers on Earth that enable both the position of the satellite and the distance to the satellite to be known precisely. By knowing our exact distance from a satellite, we know we are somewhere on the surface of an imaginary sphere that has a radius equal to the distance to the satellite. If we know our exact distance to a second satellite, we then know that we are located somewhere on a circle that marks the intersection of two imaginary spheres of known size. With additional satellites and measurements, it is possible to precisely determine our position on Earth relative to all other positions. This makes it possible to determine that the plates move. For example, by determining the position of a point in North America relative to a point in Europe, and then checking the positions a year later, it has been found that the North American plate has moved relative to the Eurasian plate. This determination is possible because distances can be measured with a precision of 5 to 10 mm. Thus, it is possible to detect the small changes in distance associated with the motions of tectonic plates, displacements associated with earthquakes, changes in sea level, movement and melting of ice sheets, etc.

 

If you wish more information about use of GPS in studying Earth processes and natural hazards, then we suggest that you visit this site (optional) by pressing the links provided within the graphic image:

metzger apparatus This site highlihgts some of the practical applications of GPS.


Question: How is GPS used, or how could it be used, in routine or common activities?