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1
Intro
2
What Causes Rock to Deform?
3
How Do Rocks Deform? • Elastic, Brittle, and Ductile Deformation
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Rocks Exhibiting Ductile Deformation
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Common Types of Folds
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Domes Versus Basins
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Folds: Rock Structures Formed by Ductile Deformation • Monoclines
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The East Kaibab Monocline, Arizona
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Faults and Joints: Rock Structures Formed by Brittle Deformation
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Hanging Wall Block and Footwall Block
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Normal Faulting in the Basin and Range Province
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Strike Slip Fault
13
Subduction and Mountain Building
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Andean-Type Mountain Building
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Collisional Mountain Belts
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Cordilleran-Type Mountain Building
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North American Cordillera
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Distribution of Modern Day Oceanic Plateaus and Fragments
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Formation of the Himalayas
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Formation of the Appalachians
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Earth's Varied Topography
22
The Principle of Isostasy
23
Erosion and Resulting Isostatic Adjustment of the Crust
Description:
Explore the processes of crustal deformation and mountain building in this 46-minute lecture. Delve into the causes of rock deformation, examining elastic, brittle, and ductile deformations. Learn about various fold types, including domes, basins, and monoclines, with a focus on the East Kaibab Monocline in Arizona. Investigate faults and joints as rock structures formed by brittle deformation, and understand the concepts of hanging wall and footwall blocks. Analyze different mountain-building processes, including Andean-type, collisional, and Cordilleran-type orogenies, with examples such as the formation of the Himalayas and Appalachians. Discover the principle of isostasy and its role in shaping Earth's varied topography. Gain insights into erosion and its impact on isostatic adjustment of the crust, providing a comprehensive understanding of the dynamic processes shaping our planet's surface.

Crustal Deformation and Mountain Building

Sven Holbik
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