'Overriding plate' presentation slideshows

Dynamik von Subduktionszonen

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Chapter 4: Basins due to flexure

Chapter 4: Basins due to flexure This presentation contains illustrations from Allen and Allen (2005) . Basins due to flexure. Flexure at ocean trenches and foreland basins Flexure Theory Continuous plate and Broken plate under a distributed load Controls on rigidity Oceanic lithosphere

1.17k views • 54 slides

Plate tectonics

Plate tectonics. 5.1 Drifting Continents 1910 Alfred Wegener Hypothesized that all the continents were once joined together in a single landmass call Pangea and have since drifted This became known as CONTINENTAL DRIFT

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An Tsunami generate by a earthquake

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Warm-up #43 Mar. 26

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http://www.earthquakes.bgs.ac.uk/earthquakes/education/eq_booklet/dia_seismogram.jpg

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Tsunami Attacks

Tsunami Attacks. Presented By : M.A MALIK. Mesco Grades School. A tsunami (pronounced soo -NAA- mee ) is a series of waves (called a "wave train") generated in a body of water by a pulsating or abrupt disturbance that vertically displaces the water column. Introduction.

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TSUNAMI DESCRIPTION

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EVIDENCE FOR PLATE TECTONICS

EVIDENCE FOR PLATE TECTONICS. Why Do Lithospheric Plates Move?. Heat Flow and Seafloor Elevations. Heat flow is a measure of the amount of heat leaving the rocks of the lithosphere.

223 views • 11 slides