All Educational Materials for Swanson Terry

UWESS 101Swanson TerryWinter

[ESS 101] - Midterm Exam Guide - Ultimate 28 pages long Study Guide!

28 Page
7 Feb 2017
January 5th, 2017 earth"s cli(cid:373)ate syste(cid:373) (1-3) Different lines give different results because of the use of different proxies: likewise
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UWESS 101Swanson TerryWinter

ESS 101 Study Guide - Midterm Guide: Geothermal Gradient, Melting Point, Continental Crust

3 Page
18 Feb 2017
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UWESS 101

ESS 101 Study Guide - Final Guide: Hydrogen Sulfide, Laptop, Calcite

8 Page
5 Dec 2017
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UWESS 101Swanson TerryFall

ESS 101 Study Guide - Quiz Guide: Sulfur Dioxide, Halliburton, United States Geological Survey

3 Page
15 Apr 2016
Benefit: natural gas as fossil fuel vs. others = amount of energy per atom of carbon is much higher. We can get a lot more work per molecule of co2 emi
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UWFall

ESS 511 Final Exam Fall 2008

4 Page
8 Mar 2019
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UWSpring

PHYS 121 Lecture Notes - Lecture 28: Free Body Diagram, Euclidean Vector

2 Page
21 May 2019
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UWFall

MATH 324 Quiz 2 Solutions

1 Page
8 Mar 2019
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UWFall

MATH 125 Quiz Solutions

1 Page
8 Mar 2019
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UWFall

ECON 471 Quiz 4

2 Page
8 Mar 2019
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UWFall

CHEM 162 Exam

14 Page
8 Mar 2019
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UWWinter

STAT 220 Quiz 1 Winter 2008

5 Page
8 Mar 2019
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UWWinter

MATH 126 Final Exam Winter

1 Page
8 Mar 2019
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UWWinter

MATH 126 Quiz Winter

1 Page
8 Mar 2019
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UWWinter

CHEM 152 Quiz 2 Winter

1 Page
8 Mar 2019
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 17: Magnetic Declination, Mass Wasting, Graph Paper

2 Page
28 Feb 2017
Topographic maps permit measurement of the slope, defined as the change in vertical distance divided by the horizontal distance (rise over run). The gr
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 14: Graph Paper, Oceanic Crust, North American Plate

3 Page
28 Feb 2017
Intra-plate volcanism occurs in two tectonic settings within the continental lithosphere: continental flood volcanism (e. g. the snake river plain and
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 4: Hematite, Covalent Bond, Ion

2 Page
24 Jan 2017
Minerals are the building blocks of rock and solid earth, all minerals: have a specific chemical composition, have a specific atomic arrangement (cryst
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UWESS 101Swanson TerryFall

ESS 101 Lecture Notes - Lecture 1: Seismic Wave, Electromagnet, Silicate Minerals

4 Page
15 Apr 2016
Nebular hypothesis: stars and planetary systems formed in the universe are from nebular dust, nebula condensed into the sun and planets. Supernova and
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UWESS 101Swanson TerryWinter

ESS 101 Lecture 3: ESS 101 Plate Tectonics Notes

5 Page
24 Jan 2017
Lithosphere (cid:858)floats(cid:859) o(cid:374) the partially melted asthenosphere: lithosphere and asthenosphere are in isostatic equilibrium. When a
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UWESS 101

ESS 101 Lecture Notes - Lecture 2: Silt, Olivine, Breccia

7 Page
5 Dec 2017
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UWESS 101Swanson TerryFall

ESS 101 Lecture Notes - Lecture 2: Peridotite, Himalayas, Andes

2 Page
15 Apr 2016
Melt phase < always different composition > solid phase. Melt phase: more sio2 rich (felsic, less fe-mg rich (matic, less dense, lighter mineral color,
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UWESS 101Swanson TerryFall

ESS 101 Lecture Notes - Lecture 4: Uee, Tephra, Diorite

4 Page
26 Feb 2017
Morphology of a volcano is strongly controlled by the viscosity of the magma: the hawaiian shield volcano shown is composed of interlayered basalt flow
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 2: Geothermal Gradient, Methane Clathrate, Ocean Acidification

7 Page
24 Jan 2017
January 9th, 2017 long term climate factors (plate tectonics) Wilson cycle process of plate tectonics. Last supercontinent to be assembled was pangea,
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 3: Time Series, Longwave, Orbital Forcing

3 Page
24 Jan 2017
January 18th, 2017 orbital forcing (chapter 7) Proxies showing this time: deep sea sediments and ice cores (later) C(cid:455)(cid:272)li(cid:272)al var
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 6: Intermediate Composition, Igneous Rock, Dacite

2 Page
27 Feb 2017
Intermediate composition magma can crystallize below the surface beneath subduction zones and create large plutonic bodies composed of coarse grained i
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 7: Cascadia Subduction Zone, Himalayas, Volcanic Arc

3 Page
27 Feb 2017
Obviously the earth is not getting bigger with the creation of new ocean lithosphere, thus it makes sense that the ocean lithosphere must be consumed a
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 5: Magnetite, Scoria, Tuff

2 Page
27 Feb 2017
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 1: Outer Core, Melting Point, Geothermal Gradient

2 Page
27 Feb 2017
Compression/primary (p-waves) waves velocity 6-7 km/sec within the lithosphere (just (cid:396)e(cid:373)e(cid:373)(cid:271)e(cid:396) that they"(cid:39
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UWESS 101Swanson TerryWinter

ESS 101 Study Guide - Midterm Guide: Geothermal Gradient, Melting Point, Continental Crust

3 Page
18 Feb 2017
View Document
UWESS 101Swanson TerryFall

ESS 101 Study Guide - Quiz Guide: Sulfur Dioxide, Halliburton, United States Geological Survey

3 Page
15 Apr 2016
Benefit: natural gas as fossil fuel vs. others = amount of energy per atom of carbon is much higher. We can get a lot more work per molecule of co2 emi
View Document
UWESS 101

ESS 101 Study Guide - Final Guide: Hydrogen Sulfide, Laptop, Calcite

8 Page
5 Dec 2017
View Document
UWESS 101Swanson TerryWinter

[ESS 101] - Midterm Exam Guide - Ultimate 28 pages long Study Guide!

28 Page
7 Feb 2017
January 5th, 2017 earth"s cli(cid:373)ate syste(cid:373) (1-3) Different lines give different results because of the use of different proxies: likewise
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 17: Magnetic Declination, Mass Wasting, Graph Paper

2 Page
28 Feb 2017
Topographic maps permit measurement of the slope, defined as the change in vertical distance divided by the horizontal distance (rise over run). The gr
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 14: Graph Paper, Oceanic Crust, North American Plate

3 Page
28 Feb 2017
Intra-plate volcanism occurs in two tectonic settings within the continental lithosphere: continental flood volcanism (e. g. the snake river plain and
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 4: Hematite, Covalent Bond, Ion

2 Page
24 Jan 2017
Minerals are the building blocks of rock and solid earth, all minerals: have a specific chemical composition, have a specific atomic arrangement (cryst
View Document
UWESS 101Swanson TerryFall

ESS 101 Lecture Notes - Lecture 1: Seismic Wave, Electromagnet, Silicate Minerals

4 Page
15 Apr 2016
Nebular hypothesis: stars and planetary systems formed in the universe are from nebular dust, nebula condensed into the sun and planets. Supernova and
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture 3: ESS 101 Plate Tectonics Notes

5 Page
24 Jan 2017
Lithosphere (cid:858)floats(cid:859) o(cid:374) the partially melted asthenosphere: lithosphere and asthenosphere are in isostatic equilibrium. When a
View Document
UWESS 101

ESS 101 Lecture Notes - Lecture 2: Silt, Olivine, Breccia

7 Page
5 Dec 2017
View Document

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UWESS 101

ESS 101 Lecture Notes - Lecture 2: Silt, Olivine, Breccia

7 Page
5 Dec 2017
View Document
UWESS 101

ESS 101 Study Guide - Final Guide: Hydrogen Sulfide, Laptop, Calcite

8 Page
5 Dec 2017
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 15: Convergent Boundary, Plate Tectonics, Oceanic Crust

2 Page
28 Feb 2017
(1) divergent plate margin (2) convergent plate margin (3) oceanic intra-plate region (4) continental intra-plate region. Divergent plate margins: ocea
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 17: Magnetic Declination, Mass Wasting, Graph Paper

2 Page
28 Feb 2017
Topographic maps permit measurement of the slope, defined as the change in vertical distance divided by the horizontal distance (rise over run). The gr
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 14: Graph Paper, Oceanic Crust, North American Plate

3 Page
28 Feb 2017
Intra-plate volcanism occurs in two tectonic settings within the continental lithosphere: continental flood volcanism (e. g. the snake river plain and
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 16: Isostasy, Laser Rangefinder, Boeing Yal-1

2 Page
28 Feb 2017
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UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 18: Linear Scale, International Date Line

2 Page
28 Feb 2017
Geoscientists utilize many different techniques to study the earth. Many of these te(cid:272)h(cid:374)i(cid:395)ues do (cid:374)ot al(cid:449)a(cid:45
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 7: Cascadia Subduction Zone, Himalayas, Volcanic Arc

3 Page
27 Feb 2017
Obviously the earth is not getting bigger with the creation of new ocean lithosphere, thus it makes sense that the ocean lithosphere must be consumed a
View Document
UWESS 101Swanson TerryWinter

ESS 101 Lecture Notes - Lecture 8: Asthenosphere, Yellowstone Caldera, Continental Crust

2 Page
27 Feb 2017
Granitic magma forms from a partial melt of continental crust, which contains dissolved water. As granitic magma rises, it solidifies as its melting te
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UWESS 101Swanson TerryWinter

ESS 101 Chapter Notes - Chapter 1: Outer Core, Melting Point, Geothermal Gradient

2 Page
27 Feb 2017
Compression/primary (p-waves) waves velocity 6-7 km/sec within the lithosphere (just (cid:396)e(cid:373)e(cid:373)(cid:271)e(cid:396) that they"(cid:39
View Document

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