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Documents DIASTROPHISM

DIASTROPHISM Diastrophism or Tectonism is a general term that refers to the deformation of the Earth's crust, and more specifically to folding and faulting. Diastrophism…

Documents HOW DO PLATE TECTONICS WORK

HOW DO PLATE TECTONICS WORK? Tectonic plates are large plates of rock that make up the foundation of the earth's crust and the shape of the continents. The tectonic…

Education Biggest earthquakes

1. Jack Moore 2. Big and Significant Earthquakes Convergent Boundaries Divergent Boundaries 3.   4. South American West Coast Greece Alaska India Japan Southern Mexico Indonesia…

Education Plate tectonics

1. Plate Tectonics 2. Plate Tectonics The model ofplate tectonicsis the starting point for understanding the distribution and formation of many collections of landforms around…

Documents Earthquakes and Faults

1. Taipei, September 21, 1999.FAULT LINES AND EARTHQUAKES 2. FaultsCracks in the earth’s crust along whichmovement takes place. 3. There are threedifferent kinds of faults!…

Technology Chapter 9outline

1. Chapter 9 Plate tectonics 2. An Idea Before Its Time An Idea Before Its Time 1915 – _____________ proposed a radical idea he called__________________ .Wegener’s continental…

Science San francisco Earthquake-Jessica

1. SAN FRANCISCO EARTHQUAKE-1906 By Jessica 2. HOW THE DISASTER SHOOK AMERICA 108 years later the San Francisco earthquake still stands as America’s worst natural disaster…

Documents Inner Structure of the Earth 1.Inner Coredense and solid 4000 miles below surface 2.Outer CoreMolten...

Slide 1 Slide 2 Inner Structure of the Earth Slide 3 1.Inner Coredense and solid 4000 miles below surface 2.Outer CoreMolten or liquid Both are mostly hot and made of hot…

Documents Who Wants to be a Genius? Final Exam Review. _________ are the longest subdivisions of geologic...

Slide 1Who Wants to be a Genius? Final Exam Review Slide 2 _________ are the longest subdivisions of geologic time. 1.Eons 2.Periods 3.Eras 4.Epochs Slide 3 Which mountain…

Documents 1.Tension – stretches rock, they become thin in the middle 2. Compression – pushes rock...

Slide 1 Slide 2 1.Tension – stretches rock, they become thin in the middle 2. Compression – pushes rock together, squeezes rock until it folds or breaks 3. Shearing –…