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Class Notes at University of Toronto Scarborough (UTSC)

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UTSCEESA06H3Nick EylesSpring

EESA06 Lecture 1: How Planet Earth Formed and is Evolving

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 2: Continental Drift, Plate Tectonics, Laurasia

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 6: Kuchinoerabu-Jima

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 8: San Andreas Fault, Syncline, Cascadia Subduction Zone

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Stratigraphy: the sub discipline of geology that studies the evolution of rocks. Uplift results in erosion, the removal of rocks. Conformable successio
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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture 2: How Planet Earth Evolves

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Mercantilism: is global trade using maps of what the earth looked like. Francis bacon (1561 1620) looked at these maps and thought that some of the con
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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 3: Isostasy, Epicenter, Deep Structure And Surface Structure

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UTSCMDSA01H3Sarah KleebFall

MDSA01 Lecture 11: Erotic Analysis and Ecological Analysis

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 4: Basalt, Aphanite, Andesite

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 5: Catastrophism, Uniformitarianism

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 9: Ophiolite, Pleistocene, Mylonite

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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 3: Seismic Tomography, Fault Scarp, Geothermal Gradient

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Earth quakes produces seismic energy that helps us map the earth"s interior. Energy in the form of wave p and s waves. Primary waves are higher velocit
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UTSCEESA06H3Nick EylesSpring

EESA06 Lecture 11: A Wide Ranging Review of Environmental Challenges

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