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Textbook Notes for Pamela Stephens

CU-BOULDERGEOL 1010Pamela StephensFall

GEOL 1010 Chapter Notes - Chapter 6: Frost Heaving, Weathering, Eluvium

Jake Smooke4 Page
11 Nov 2018
0
Weathering involves the physical breakdown (disintegration) and chemical alteration (cid:894)de(cid:272)o(cid:373)positio(cid:374)(cid:895) of ro(cid:2
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CU-BOULDERGEOL 1010Pamela StephensFall

GEOL 1010 Chapter Notes - Chapter 12: Richard Dixon Oldham, Outer Core, Wave Power

Jake Smooke3 Page
11 Nov 2018
0
Mineral phase change is a change that occurs when a mineral is subjected to intense pressure. In this change, the structure of a mineral may become uns
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CU-BOULDERGEOL 1010Pamela StephensFall

GEOL 1010 Chapter Notes - Chapter 15: Mass Wasting, Regolith, Debris Flow

Jake Smooke3 Page
11 Nov 2018
0
Landslide is the sudden event in which large quantities of rock and soil plunge down a steep slope. They can occur in addition to other major natural d
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CU-BOULDERGEOL 1010Pamela StephensFall

GEOL 1010 Chapter 10: Crustal Deformation

Jake Smooke3 Page
11 Nov 2018
0
Rocks deform when the stress acting on a rock body exceeds its strength. Confining pressure is when stress is applied equally in all directions. Differ
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CU-BOULDERGEOL 1010Pamela StephensFall

GEOL 1010 Chapter Notes - Chapter 9: Atomic Number, Beta Particle, Nonconformist

Jake Smooke3 Page
4 Oct 2018
0
Relative dates are when we place rocks in their proper sequence of formation (order, rock a was formed first, rock b was formed second etc. ) Law of su
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