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Plate Tectonics: Understanding the Formation of Mountains and Ocean Basins, Exams of Geology

An in-depth exploration of plate tectonics, focusing on the processes behind the formation of mountains and ocean basins. Topics covered include sea floor spreading, continental drift, orogeny, plate margins, convection cells in the mantle, and mantle plumes. Real-world examples and figures are used to illustrate these concepts.

Typology: Exams

Pre 2010

Uploaded on 07/30/2009

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Download Plate Tectonics: Understanding the Formation of Mountains and Ocean Basins and more Exams Geology in PDF only on Docsity! 1 Plate Tectonics GEOL 101 Lecture 22 Prop: Test 3 Invitations The Grand Tetons, Wyoming How Are Mountains Built? First a Brief Review of Sea Floor Spreading Break-Up of a Continent and Origin of an Ocean Basin Spread Centers Feed Subduction Zones 2 Missing Mechanisms for Continental Drift: Sea Floor Spreading & Subduction Continents are Passive ā€œBoatsā€ Subduction Zones: Ocean-Ocean Margin Subduction Zones: Ocean-Continent Margin 5 Continental Lithosphere Will NOT Flush Down Subduction Zones Orogeny Folds Rocks Review: New Lithosphere (Crust + Upper Mantle) is Created at Spread Centers, Consumed at Subduction Zones 6 What About Offsets in Spread Centers? Transform Faults & Fracture Zones Transform Faults 7 San Andreas Fault: Right-Lateral Transform Fault Left-Lateral Offset!! Why?: Fault is Produced by Offset, vs. Offset Produced by Fault Plate Margins: ā€¢ Spread Centers (Mid-Ocean Ridges) ā€¢ Subduction Zones (Trenches) ā€¢ Transform Faults Plate Margins: Trench suction +_ Mantle Plumes Depth (km) Mantle Plumes Under Continents Se cals on uplift 10 11 ā€¢ Known ā€œHot Spotsā€ Hawaiian Islands Mantle Plumes - Hot Spots ā€¢ Numbers = Age of Rock in Millions of Years 12 Sinking of Cool, Dense Plates Seamount Volcanoes Surrounded by Fringing Coral Reefs NASA Atolls: Submerged Volcanos Support Reefs Only in Warm Clear Seas Tuamoto Islands Piedmont Arc Carolina Arc \% | _risiandares. 3 | Ancestal atantc ā€œ> ~e A Cambrian North Piedmoat Carolina Arc ametican cenrane\ 5 \32 ancestal attic aitea a = B _Ordovician-Sillutian (Taconic Orogen North Piedmont Carclira America cerrare terrane craton : ā€˜ics C Devonian-Mi sits ippi (Acadian Orogeny) North piocrron: Carolina American jerane terrane cra ā€˜Ancestral Atlantic trea c Devonian-MisĀ¢esippi (Acadian Orogeny) Piedmont Carolina alleghenan lerane terrane suture ā€˜Altica D Pennsyl.-Permian (Alleghenian Orogeny) Future site of atlantic ā€˜Alleghanian North Arveri suue E Triassic 15 16 Source: http://vishnu.glg.nau. edu/rcb/ WVU WVU Source: http://vishnu.glg.nau. edu/rcb/ WVU Source: http://vishnu.glg.nau. edu/rcb/ WVU 17 Source: http://vishnu.glg.nau. edu/rcb/ WVU Source: http://vishnu.glg.nau. edu/rcb/ Taconic Orogeny Continent-Arc Collision WVU Orogeny: Eastern N. Amer. ā€œMirrorā€ Image of West Coast 20 Source: http://vishnu.glg.nau. edu/rcb/ Alleghenian Orogeny Continent-Continent Collision WVU Allegehenian Orogeny Folded Appalachian Rocks ā€œMirrorā€ Image of West Coast Source: http://vishnu.glg.nau. edu/rcb/Penn.jpg Pangaea = Gondwanaland + Laurasia 21 Source: http://vishnu.glg.nau. edu/rcb/ Alleghenian Orogeny WVU Source: http://vishnu.glg.nau. edu/rcb/Perm.jpg Pangaea = Gondwanaland + Laurasia Ice Sheet Erosion and Isostatic Uplift of the Appalachians Since End of Alleghenian Orogeny 22 Laurasia Gondwanaland Source: http://vishnu.glg.nau.edu/rcb/160_1st.jpg WVU Source: http://vishnu.glg.nau. edu/rcb/ WVU Source: http://vishnu.glg.nau. edu/rcb/ WVU
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