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Textbook Notes for Nick Eyles

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UTSCEESA06H3Nick EylesSpring

EESA06H3- Final Exam Guide - Comprehensive Notes for the exam ( 23 pages long!)

OC53748823 Page
29 Mar 2018
0
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: Seismic Tomography, Fault Scarp, Geothermal Gradient

OC5374884 Page
9 Mar 2018
0
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

EESA06H3 Lecture 2: How Planet Earth Evolves

OC5374886 Page
9 Mar 2018
0
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 5: Mature Oceans

OC5374885 Page
9 Mar 2018
0
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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 4: East African Rift, Oceanic Crust, Triple Junction

OC5374885 Page
9 Mar 2018
0
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UTSCEESA06H3Nick EylesSpring

EESA06 Final: Complete and Comprehensive 19 Page Final Exam Study Guide - Winter 2016

OC53748820 Page
8 Apr 2016
355
Eesa06 - lecture 1 - how planet earth formed and is evolving. Stratigraphy: the study of layers, basically creating an order of events in history. Para
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UTSCEESA06H3Nick EylesSpring

EESA06 Lecture 11: A Wide Ranging Review of Environmental Challenges

OC5374882 Page
30 Mar 2016
98
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UTSCEESA06H3Nick EylesSpring

EESA06H3 Lecture Notes - Lecture 10: Bryozoa, Crinoid, Scallop

OC5374882 Page
23 Mar 2016
89
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UTSCEESA06H3Nick EylesSpring

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

OC5374881 Page
16 Mar 2016
147
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UTSCEESA06H3Nick EylesSpring

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

OC5374882 Page
8 Mar 2016
73
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 EylesWinter

EESA06H3 Chapter Notes - Chapter 1-4: Gabbro, Seafloor Spreading, Oceanic Crust

OC626929 Page
30 Jun 2014
642
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UTSCEESA06H3Nick EylesWinter

EESA06 Chapter 20

OC45367 Page
5 Apr 2011
259
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UTSCEESA06H3Nick EylesWinter

EESA06 Chapter 16: Chapter 16

OC50105610 Page
27 Mar 2016
269
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UTSCEESA06H3Nick EylesWinter

Chapters 1-3 notes

OC623911 Page
21 Mar 2011
232
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UTSCEESA06H3Nick EylesWinter

EESA06H3 Chapter Notes - Chapter 20: Taconic Orogeny, Grenville Orogeny, Alleghanian Orogeny

OC5010568 Page
29 Mar 2016
232
Canada: a young nation, but an old country. Canada has been in existence since 1867: act of confederation brought together ontario, nb, ns, and quebec,
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UTSCEESA06H3Nick EylesWinter

EESA06 Chapter 19

OC45364 Page
23 Mar 2011
92
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UTSCEESA06H3Nick EylesWinter

EESA06 Chapter 4

OC45364 Page
2 Mar 2011
99
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UTSCEESA06H3Nick EylesSummer

EESA06H3 Chapter Notes - Chapter 15,16,20: Intermontane Belt, Laurasia, Parent Material

OC96280135 Page
8 Sep 2016
12
Groundwater can form caves, sinkholes and petrified wood. Can appear as hot springs and geysers. 97. 2 ocean, 2. 15 glaciers and ice, . 61 groundwater,
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UTSCEESA06H3Nick EylesFall

EESA06H3 Chapter 16, 20: EESA06: Introduction to Planet Earth (Final Exam Notes)

OC59826615 Page
6 Apr 2017
0
Water stored as ice in glaciers came from the oceans. Episodes of glaciation ended about 10,000 years ago. Rock records have evidence of older glaciati
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UTSCEESA06H3Nick EylesWinter

EESA06H3 Chapter Notes - Chapter 1: Gneiss, Proterozoic, Cenozoic

OC7738783 Page
8 Mar 2016
80
Uniformitarianism: principle that geologic processes operating at the present are the same processes that operated in the past (the present is the key
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UTSCEESA06H3Nick EylesWinter

EESA06H3 Chapter Notes - Chapter 19: James Hutton, Uniformitarianism, Relative Dating

OC756711 Page
11 Apr 2011
58
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UTSCEESA06H3Nick EylesWinter

Chapter 19 & 20 Textbook Notes

OC148012 Page
12 Apr 2011
88
 uniformitarianism principle that geologic processes operating at the present are the same processes that operated in the past. The present is the key
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