Crustal Deformation and Mountain Building

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.

Intro
What Causes Rock to Deform?
How Do Rocks Deform? • Elastic, Brittle, and Ductile Deformation
Rocks Exhibiting Ductile Deformation
Common Types of Folds
Domes Versus Basins
Folds: Rock Structures Formed by Ductile Deformation • Monoclines
The East Kaibab Monocline, Arizona
Faults and Joints: Rock Structures Formed by Brittle Deformation
Hanging Wall Block and Footwall Block
Normal Faulting in the Basin and Range Province
Strike Slip Fault
Subduction and Mountain Building
Andean-Type Mountain Building
Collisional Mountain Belts
Cordilleran-Type Mountain Building
North American Cordillera
Distribution of Modern Day Oceanic Plateaus and Fragments
Formation of the Himalayas
Formation of the Appalachians
Earth's Varied Topography
The Principle of Isostasy
Erosion and Resulting Isostatic Adjustment of the Crust