Title | Geology 101 Notes – 10 |
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Course | Introduction To Geology |
Institution | Western Washington University |
Pages | 1 |
File Size | 35 KB |
File Type | |
Total Downloads | 109 |
Total Views | 142 |
These are class notes that I typed directly after class from hand written notes I wrote during class. I go through this two step process to ensure accuracy and enhance organization....
Geology 101 Notes – 10.1.14 Trenches Formed by subduction zones Deep trenches=dense=far traveled=old age Plate tectonics and earthquakes Every plate boundary creates earthquakes, divergent/convergent/transform Deep earthquakes are only created by convergent plate boundaries Depth of the earthquake doesn’t affect strength o Depth does affect how much we feel the earthquake Tectonics of western United States Juan de Fuca plate has a divergent plate boundary with the pacific plate and a convergent plate boundary with the North American plate o Cascadia subduction zone o Very quite, not many earthquakes Ocean-ocean convergent boundary Older and denser plate is the one that subducts Forms island arc Continental-continental convergence Cant shove one under the other o Too thick, too buoyant (not dense) The lithospheres collide, stack and uplifts o Comes together and goes straight up to form very tall mountains (mount Everest) Top of Mt. Everest is made of limestone o Limestone only formed at the bottom of the ocean Transform plate boundary – fracture zones Side to side motion Occurs in association with divergent plate boundaries (usually) No volcanic activity Connect segments of mid-ocean ridges San Andreas fault – an example of a transform boundary Between the pacific plate and the North American plate Some earthquakes Not destroying or creating lithosphere...