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Geo 102 Lab #1 Pacific Northwest Geologic Mystery

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Geo 102 Lab #1. Pacific Northwest Geologic Mystery. The Scientific Method. The basic process of the scientific method is as follows: Observe some phenomenon or object you cannot explain. - PowerPoint PPT Presentation

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Page 1: Geo 102 Lab #1

Geo 102 Lab #1

Pacific Northwest Geologic Mystery

Page 2: Geo 102 Lab #1

The Scientific MethodThe basic process of the scientific method is as follows:• Observe some phenomenon or object you cannot explain.• Invent a tentative description or explanation, called a

hypothesis, that is consistent with what you have observed.

• Use the hypothesis to make predictions about future observations and actions.

• Test those predictions by experiments or further observations and modify the hypothesis in the light of your results.

• Make additional predictions based on the revised hypothesis until there are no discrepancies between theory and experiment and/or observation.

Page 3: Geo 102 Lab #1

#1McMinnville

Oregon

Page 4: Geo 102 Lab #1

Jökulhlaups

• Glacial outburst floods, also known as jökulhlaups, occur very rapidly and can release huge amounts of water. In Iceland, many jökulhlaups are triggered by volcanic activity beneath glacial ice.

Page 5: Geo 102 Lab #1

Jökulhlaup in Iceland

Page 6: Geo 102 Lab #1

Erratic - A rock fragment carried by glacial ice, or by floating ice, deposited some distance from the

outcrop from which it was derived…

- Glossary of Geology

Page 7: Geo 102 Lab #1

Erratic State Park in

McMinnville

Page 8: Geo 102 Lab #1

Glacial Erratics in the Willamette

ValleyMcMinnville Erratic

Icebergs near Vatnajokull, Iceland

Page 9: Geo 102 Lab #1

#2Eastern

Washington

Page 10: Geo 102 Lab #1

Satellite Image of Eastern Washington

Page 11: Geo 102 Lab #1

The Palouse

• Ancient loess deposits in eastern Washington derived from the Columbia River and glacial outwash, blown in during the last Ice Age.

• The Palouse consists of rolling hills of very thick, fertile, soil. It known for its rich wheat production.

Page 12: Geo 102 Lab #1

Loess

• Silt, sand, and dust, which are blown by wind. The source of most of the loess in the Pacific Northwest is glacial material blown from the north during the last Ice Age

Page 13: Geo 102 Lab #1

Scablands

• An elevated area, underlain by flat-lying basalt flows, with a thin soil cover and sparse vegetation, and usually with deep dry channels scoured into the surface.

Page 14: Geo 102 Lab #1

Scablands - Near Grand Coulee

Page 15: Geo 102 Lab #1

Map of Eastern

Washington

Dry Falls and Coulee City

Page 16: Geo 102 Lab #1

#3Spokane

Washington

Page 17: Geo 102 Lab #1

Map of Spokane

Area

Rhythmites

Page 18: Geo 102 Lab #1

Rhythmites South of Spokane

Page 19: Geo 102 Lab #1

Rhythmite

• Succession of layers of sediment (silts, clays, etc.) deposited in rhythmic cycles. For example a sand layer followed by a silt layer followed by another sand layer. Varying amounts of time may separate layers.

Page 20: Geo 102 Lab #1

Glacial Varves

Page 21: Geo 102 Lab #1

Varve

• A pair of thin sedimentary layers formed annually by seasonal climatic changes. Usually found in glacial lake deposits, varves consist of a coarse-grained, light-colored summer layer and a finer-grained, dark-colored winter layer. Varves, and the pollen they contain, are useful for interpreting recent climatic history.

Page 22: Geo 102 Lab #1

#4Coulee City Washington

Page 23: Geo 102 Lab #1

Map of Eastern

Washington

Dry Falls and Coulee City

Page 24: Geo 102 Lab #1

Large Boulder Near Grand Coulee Dam

Page 25: Geo 102 Lab #1

#5MissoulaMontana

Page 26: Geo 102 Lab #1

Detroit Dam

Page 27: Geo 102 Lab #1

Detroit Reservoir in March

Page 28: Geo 102 Lab #1

Shorelines above Missoula

Page 29: Geo 102 Lab #1

#6Corvallis Oregon

Page 30: Geo 102 Lab #1

Wallowing in a Mud Puddle

Page 31: Geo 102 Lab #1

#7Camas Prairie

Montana

Page 32: Geo 102 Lab #1

Camas Prairie, Montana

Page 33: Geo 102 Lab #1

Camas Prairie, Montana

Page 34: Geo 102 Lab #1

Ripple Marks

Page 35: Geo 102 Lab #1

Camas Prairie, Montana

Page 36: Geo 102 Lab #1

Camas Prairie Topographic Map

Page 37: Geo 102 Lab #1

#8Dry Falls

Washington

Page 38: Geo 102 Lab #1

Map of Eastern

Washington

Dry Falls and Coulee City

Page 39: Geo 102 Lab #1

Aerial View of Dry Falls

Dry Falls

Page 40: Geo 102 Lab #1

Shutting off Niagara

A De-watered

American Falls

1969

Page 41: Geo 102 Lab #1

Eroded Gully SW of Coulee City

Page 42: Geo 102 Lab #1

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