Effects of Plate Tectonics Part I

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Presentation transcript:

Effects of Plate Tectonics Part I Forces Shape the Land

Definition: Isostasy When plates move, they balance to equilibrium on athenosphere Example: Drop block in water, and it bobs up & down, then floats

Major Forces Stress/Strain: Compression, Shearing, Tension Folding/Deformation: Anticline, Syncline, Monoclines (Rocks don’t break) Faulting: Normal, Reverse, Strike-Slip (Rocks do break) These forces can create: 1) Landform changes 2) Mountains 3) Earthquakes 4) Volcanoes

types of folds Anticline – “A” Shaped

types of folds Syncline – remember “smile” shaped

types of folds Monocline – slightly curved

Folds Animation Link http://ees.as.uky.edu/sites/default/files/elearning/module10swf.swf http://www.wwnorton.com/college/geo/earth3/content/ch11/animations.asp

fault terminology                                                      Fault – fracture in rock along which there has been displacement Hanging wall – rock surface above the fault Footwall – rock surface below the fault Fault scarp – exposed fault surface

Caused by tension forces Hanging wall moves down Normal Faults Caused by tension forces Hanging wall moves down

Reverse Faults Caused by compression forces Hanging wall moves up

Opposing forces cause rock to break Strike-slip Faults Opposing forces cause rock to break Move horizontally

Animation Link: http://www.classzone.com/books/earth_science/terc/content/visualizations/es1103/es1103page01.cfm http://www.iris.edu/gifs/animations/faults.htm

Questions for Review What is isostasy? Explain the difference among compression, shearing, and tension. What is the difference between a fold and a fault? Name the 3 types of folds and their shape. What are the 3 types of faults? What are some effects of plate tectonics?

CE Questions As a volcanic mountain range is built, isostatic adjustment will cause the crust beneath it to: A) Break B) Sink C) Rise D) Fold

CE Questions As a volcanic mountain range is built, isostatic adjustment will cause the crust beneath it to: A) Break B) Sink C) Rise D) Fold

CE Questions Isostatic adjustments continue until the forces pressing the crust up and down are: A) Balanced B) Doubled C) Decreased D) Removed

CE Questions Isostatic adjustments continue until the forces pressing the crust up and down are: A) Balanced B) Doubled C) Decreased D) Removed

CE Questions Folding of rocks is most likely to happen when rocks undergo: Tension Shearing Compression Cooling

CE Questions Folding of rocks is most likely to happen when rocks undergo: Tension Shearing Compression Cooling

CE Questions Rocks deeper in the earth’s crust are less likely to deform by breaking than rocks closer to the earth’s surface because of: A) Lower stresses B) Higher temperature C) Higher strains D) Lower altitude

CE Questions Rocks deeper in the earth’s crust are less likely to deform by breaking than rocks closer to the earth’s surface because of: A) Lower stresses B) Higher temperature C) Higher strains D) Lower altitude

CE Questions Which causes reverse faults? A) Compression B) Shearing C) Tension D) Folding

CE Questions Which causes reverse faults? A) Compression B) Shearing C) Tension D) Folding

CE Questions Where do strike-slip faults often occur? A) At mid-ocean ridges B) In the lower half of the crust C) Between ridges D) Along transform plate boundaries

CE Questions Where do strike-slip faults often occur? A) At mid-ocean ridges B) In the lower half of the crust C) Between ridges D) Along transform plate boundaries

CE Questions Explain the cause and effect of normal, reverse, and strike-slip faults (be specific).

CE Questions What is the result of a….convergent boundary….divergent boundary…transform…? Which produces new crust? Which takes place on continental crust? Which takes place in the ocean? Which boundary is located in California?

Discovery Ed Videos http://app.discoveryeducation.com/player/view/assetGuid/11BE25FF-6271-4C50-B65C-8D680D44AB97 http://app.discoveryeducation.com/player/view/assetGuid/8075217D-2238-4D7C-B45F-0342B5ADCCC5 http://app.discoveryeducation.com/player/view/assetGuid/F302FFD3-A25E-43AE-B6E6-5597DE8C004E