1 / 18

PLATE TECTONICS AND BOUNDARIES

PLATE TECTONICS AND BOUNDARIES. How do we know what the Earth is made of?. Geophysical surveys: seismic, gravity, magnetics , electrical, Earth size and shape Acquisition: land, air, sea and satellite Geological surveys: fieldwork, boreholes, mines. Plate Tectonics.

talia
Télécharger la présentation

PLATE TECTONICS AND BOUNDARIES

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. PLATE TECTONICS AND BOUNDARIES

  2. How do we know what the Earth is made of? • Geophysical surveys: seismic, gravity, magnetics, electrical, Earth size and shape • Acquisition: land, air, sea and satellite • Geological surveys: fieldwork, boreholes, mines

  3. Plate Tectonics • The Earth’s crust is divided into 12 major plates which are moved in various directions. • This plate motion causes them to collide, pull apart, or scrape against each other. • Each type of interaction causes a characteristic set of Earth structures or “tectonic” features. • To determine which type of boundary is present, scientists use evidence of earthquakes and volcanoes

  4. World Plates

  5. Three types of plate boundary • Divergent • Convergent • Transform

  6. Divergent Boundaries • Spreading ridges • As plates move apart new material is erupted to fill the gap

  7. Mid-Atlantic Ridge = Divergent Boundary

  8. http://www.geo.lsa.umich.edu/~crlb/COURSES/270/Lec12/spreexamples.jpeghttp://www.geo.lsa.umich.edu/~crlb/COURSES/270/Lec12/spreexamples.jpeg

  9. Iceland: An example of continental rifting • Iceland has a divergent plate boundary running through its middle

  10. Convergent Boundaries • Plates move toward each other • There are three typesof convergent plate boundaries • Continent-continent collision • Continent-oceanic crust collision • Ocean-ocean collision

  11. Continent-Continent Collision • Forms mountains,e.g. European Alps, Himalayas

  12. Collision Zones Two continents hit head-on, crinkling up the land into a high mountain chain.

  13. Himalayas

  14. Continental-Oceanic (Subduction) • Oceanic lithosphere subducts underneath the continental lithosphere • Oceanic lithosphere heats up and melts, then rises, causing volcanism • E.g. The Andes

  15. Ocean-Ocean Plate Collision • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. • The worlds deepest parts of the ocean are found along trenches. • E.g. The Mariana Trench is 11 km deep!

  16. Transform Boundaries • Where plates slide past each other Above: View of the San Andreas transform fault

More Related