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Class Notes for EAPS 11200 at Purdue University

PURDUEEAPS 11200Terry WestFall

EAPS 11200 Lecture Notes - Lecture 25: Paleoarchean, Neoarchean, Mesoarchean

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10 Jan 2020
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It ends when there is no more hydrogen and then the sun expands into a big red star and turns into a white dwarf. In 1 or more of the earth"s icehouse
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PURDUEEAPS 11200Terry WestFall

EAPS 11200 Lecture Notes - Lecture 8: Plate Tectonics, Multiple Working, Divergent Boundary

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19 Oct 2019
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture Notes - Lecture 15: Paleoproterozoic, Proterozoic, Hematite

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3 Apr 2019
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture 9: 02042019

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19 Feb 2019
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Concept of geologic time: two different frames of reference, relative dating. Placing geologic events in sequential order: only know the order, not how
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture 5: 01232019 day 1

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5 Feb 2019
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Sedimentary rocks: all start as unconsolidated particles, undergo lithification, two main types, siliciclastic, chemical. Lithification: compaction and
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture 3: 01142019

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21 Jan 2019
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture 1: 01072019

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14 Jan 2019
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Distinguish earth history from earth dynamics: geology is the science of the earth, composition, structure, origin, life forms, physical and chemical p
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PURDUEEAPS 11200Terry WestFall

EAPS 11200 Lecture Notes - Lecture 15: Jean-Baptiste Lamarck, Carl Linnaeus, Georges Cuvier

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19 Oct 2019
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PURDUEEAPS 11200Terry WestFall

EAPS 11200 Lecture Notes - Lecture 13: Cosmic Ray, Roh The Big Bang!, Proterozoic

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19 Oct 2019
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PURDUEEAPS 11200Terry WestFall

EAPS 11200 Lecture Notes - Lecture 3: Plate Tectonics, Igneous Rock, Divergent Boundary

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19 Oct 2019
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture Notes - Lecture 22: Bipedalism, Herbivore, Paleozoic

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16 Apr 2019
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PURDUEEAPS 11200Terry WestSpring

EAPS 11200 Lecture Notes - Lecture 19: Taconic Orogeny, Euramerica, Baltica

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3 Apr 2019
0
Paleozoic - overview of the silurian and devonian periods. Silurian-devonian tectonics: taconic orogeny had ceased in eastern laurentia, erosion had re
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