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Documents AIM: Explain the rock cycle and the role of plate tectonics in the rock cycle? OBJ: Given notes and....

AIM: Explain the rock cycle and the role of plate tectonics in the rock cycle? OBJ: Given notes and activity sheet SWBAT explain the rock cycle and the role of plate tectonics…

Documents Internal Forces of Change Types of Boundaries Convergent –Come together Divergent –Pull apart ...

Internal Forces of Change Types of Boundaries Convergent Come together Divergent Pull apart Transform Slide past each other http://www.cotf.edu/ete/modules/msese/earthsysflr/plates1.html…

Documents Mountain Belts formed at Divergent and Convergent Boundaries

Mountain Belts formed at Divergent and Convergent Boundaries Mountains Formed at Divergent Boundaries Divergent Plate Boundaries Mid Ocean Ridges Continuous underwater mountain…

Documents Star formation (and associated planets) from a nebula.

PowerPoint Presentation Star formation (and associated planets) from a nebula The Earth’s Layers (some editions: TEXT p. 209) “Above the core is the mantle, containing…

Engineering padang 2002 earthquake report

1. T h e P a d a n g I n d o n e s i a E a r t h q u a k e o f S e p t 3 0 , 2 0 0 2 Page 1 MARWADI EDUCATION FOUNDATION’S GROUP OF INSTITUTIONS FACULTY OF ENGINEERING,…

Documents Chapter 4 Continental Margins and Basins. Continental Margins These are the areas of the edges of...

Chapter 4 Continental Margins and Basins Continental Margins These are the areas of the edges of the continents that are under water Passive margins face edges of diverging…

Documents Volcanoes Chapter 9. What is a volcano? A volcano is an opening in the Earth’s surface. Ash and...

Volcanoes Chapter 9 What is a volcano? A volcano is an opening in the Earthâs surface. Ash and lava come out and build up forming a mountain. The word, âvolcanoâ comes…

Documents Volcanoes

Volcanoes Figure 5.4 Volcanoes of the World Magma Sources and Types Magma sources tend to be 50 to 250 km deep into the crust and upper mantle Temperatures increase as depth…

Documents DYNAMIC DISPLACEMENTS OF THE SEA BOTTOM DUE TO SUBDUCTION ZONE EARTHQUAKES A.I. IVASHCHENKO...

DYNAMIC DISPLACEMENTS OF THE SEA BOTTOM DUE TO SUBDUCTION ZONE EARTHQUAKES A.I. IVASHCHENKO Institute of Oceanology, RAS, Moscow L.I. LOBKOVSKY Institute of Oceanology, RAS,…

Documents Geological Processes The crust and mantle.

Geological Processes The crust and mantle Convection cells/currents Internal heat pushes soft rock in the asthenosphere upward. As the rock cools it then moves downward Types…