logging in or signing up Ch 20 powerpoint Yuan Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 403 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 03, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Mountain Building: Mountain Building Chapter 20Isostatic Rebound – crust rises as a result of __________________: Isostatic Rebound – crust rises as a result of __________________ This iceberg demonstrates the process of isostatic rebound. removal of massSlide3: Folded rock layers produced by compressional forces. This part of the folded mountain shows a __________. synclineSlide4: Example of new crust being formed at Iceland. _____ type volcano on the mid-Atlantic ridge. SheildConvergent-Boundary Mountains: Convergent-Boundary Mountains The following three slides show mountain types produced when plates move __________. togetherSlide6: Ocean-Ocean Convergence Examples: Aleutian Islands, Phillipines,______ Basaltic magma trench Volcanic island arc JapanSlide7: Ocean-Continental Convergence Examples: ________, Andes Andesitic magma, granitic intrusions volcanic mountains trench metamorphic rock CascadesSlide8: Continental-Continental Convergence Examples: Himalayas,______________ faults folded mountains igneous intrusions metamorphic and sedimentary rock AppalachiansNonconvergent-Boundary Mountains: Nonconvergent-Boundary Mountains The next four slides show mountains formed at divergent boundaries (plates moving _____), hot spots, and areas of faulting or uplift. apartSlide10: Divergent-Boundary Mountain Example: intrusive rock pillow basalts Mid-Atlantic RidgeSlide11: Volcanic Hot Spot Mountain Example: ______, Galapagos extrusive ingneous rock HawaiiSlide12: Uplifted Mountains Example: ____________ intrusive igneous rock, less structural deformation AdirondacksSlide13: Fault-Block Mountains Example: __________, Basin and Range mostly sedimentary rock Grand TetonsMountain Building Review: Mountain Building Review The Galapagos Islands formed as a result of a ___________. The Appalachians are about _________ years old. The Appalachians are a __________ mountain range. The Cascades (Mt St Helens, Mt Rainier,…) are a ___________ mountain range with ___________ eruptions. hot spot 600-700 million folded volcanic explosive You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
Ch 20 powerpoint Yuan Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINTLite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 403 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 03, 2007 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Mountain Building: Mountain Building Chapter 20Isostatic Rebound – crust rises as a result of __________________: Isostatic Rebound – crust rises as a result of __________________ This iceberg demonstrates the process of isostatic rebound. removal of massSlide3: Folded rock layers produced by compressional forces. This part of the folded mountain shows a __________. synclineSlide4: Example of new crust being formed at Iceland. _____ type volcano on the mid-Atlantic ridge. SheildConvergent-Boundary Mountains: Convergent-Boundary Mountains The following three slides show mountain types produced when plates move __________. togetherSlide6: Ocean-Ocean Convergence Examples: Aleutian Islands, Phillipines,______ Basaltic magma trench Volcanic island arc JapanSlide7: Ocean-Continental Convergence Examples: ________, Andes Andesitic magma, granitic intrusions volcanic mountains trench metamorphic rock CascadesSlide8: Continental-Continental Convergence Examples: Himalayas,______________ faults folded mountains igneous intrusions metamorphic and sedimentary rock AppalachiansNonconvergent-Boundary Mountains: Nonconvergent-Boundary Mountains The next four slides show mountains formed at divergent boundaries (plates moving _____), hot spots, and areas of faulting or uplift. apartSlide10: Divergent-Boundary Mountain Example: intrusive rock pillow basalts Mid-Atlantic RidgeSlide11: Volcanic Hot Spot Mountain Example: ______, Galapagos extrusive ingneous rock HawaiiSlide12: Uplifted Mountains Example: ____________ intrusive igneous rock, less structural deformation AdirondacksSlide13: Fault-Block Mountains Example: __________, Basin and Range mostly sedimentary rock Grand TetonsMountain Building Review: Mountain Building Review The Galapagos Islands formed as a result of a ___________. The Appalachians are about _________ years old. The Appalachians are a __________ mountain range. The Cascades (Mt St Helens, Mt Rainier,…) are a ___________ mountain range with ___________ eruptions. hot spot 600-700 million folded volcanic explosive