ENV 110 Lecture Notes - Lecture 2: Basalt, Mafic, Intermediate Composition

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Environmental Studies - Lecture 3
Global Change
Plastic asthenosphere permits tectonic plate motion
Star warm enough to warm Earth and atmosphere (habitable zone)
Liquid is possible allowing weathering and erosion
Biotic evolution continually modifies the biosphere
Earth System
Four descriptions of change
Gradual time variable
Catastrophic extinction
Unidirectional Evolution of Earth or Formation of Moon, go forward and never
backwards
Cyclic Supercontinent cycle, works in a cycle
Supercontinent
Plate tectonics drives continental movement
Ocean basins open and close
Physical Changes
Sea level +/- 300 meters
Layer of the Earth
Deeper one goes; higher the temperature, higher the pressure
Crust: thickest under Mount Range (40 miles), thinnest under mid-ocean ridge (4 miles)
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