Erosion and Deposition by Glaciers Chapter 4: Topic 8.

39
Erosion and Deposition by Glaciers Chapter 4: Topic 8

Transcript of Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Page 1: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Erosion and DepositionbyGlaciers

Chapter 4: Topic 8

Page 2: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Animation Links http://highered.mcgraw-hill.com/sites/0072402466/student_view0/

chapter12/animations_and_movies.html# http://phet.colorado.edu/en/simulation/glaciers

Page 3: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Glacier You Tube vids The great lakes – YouTube Glaciers (3 min) Yakety Sax Glacier Cartoon formation of glacier

Page 4: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study Guide- Item #1

1.       A glacier is an enormous mass of ____________________ __________________. They are formed of accumulated and compressed layers of _____________________ that pile up year after year in cold places.

moving ice

snow

Page 5: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide – item #2

___________ ____________ form in high elevations such as the peaks of large mountains. These are also known as ___________________ glaciers since they flow down the slopes of mountains through valleys originally carved out by streams.

Alpine glaciers

valley

Page 6: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Alpine (valley) glacier

Page 7: Erosion and Deposition by Glaciers Chapter 4: Topic 8.
Page 8: Erosion and Deposition by Glaciers Chapter 4: Topic 8.
Page 9: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #3

These types of glaciers (alpine) _____________________ and _________________________ the valleys into a broad ___________ shape.

widen

straighten

U

Page 10: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Valley Glaciation

Page 11: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Glacial Valley (U-shaped)

Page 12: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide – item #4

____________________ _________________________ form near the North and South poles and cover huge amounts of land area. These are pancake-shaped and move outward in all directions form the center. All glacial movement is the result of the force of ________________________ moving ice from higher to lower elevation.

Continental glaciers

gravity

Page 13: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Continental glacier

Page 14: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #5

The size of a glacier changes due to changes in _________________________ - the averages in temperature and precipitation over an extended period of time. This can cause the terminus (the outer or lower edge of the glacier) to appear to move.

• Advance- glaciers grow during periods of global cooling and cover more land (“ice age”)

• Retreat – glaciers shrink and cover less land as a result of global ________________.

climate

warming

Page 15: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Glacial / Interglacial cycles

Page 16: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #6

The most recent ice age ended about __________________________ years ago. At this time, much of midwest (including Ohio) and northeast U.S. was covered by a large continental glacier. The remnants of this glacier covers Greenland today. This glacier started retreating as a result of global warming that continues today. The erosional effects of this glacier created the _________ ______ when it retreated. These are a major source of fresh water, recreation, and transportation today.

10, 000

Great Lakes

Page 17: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

The Great Lakes and Finger lakes

Page 18: Erosion and Deposition by Glaciers Chapter 4: Topic 8.
Page 19: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Formation of Great Lakes

Page 20: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Formation of glacial lakes through differential abrasion

Hard rock Soft rock Hard rock

glacier

Hard rock Soft rock Hard rock

glacier

Hard rock Soft rock Hard rock

Glacial lake

Page 21: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Glacial Grooves- Kelley’s Island

Page 22: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Great Lakes profile

Page 23: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #7

The movement of large, heavy glaciers over the land has the power to erode, weather, and deposit rock. Continental glaciers ___________________ the landscape by scraping and eroding features. Alpine glaciers carve out ____________________ features in the mountain rocks through which they flow. These include:

 

smooth

rugged

Page 24: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Northern and western Ohio (glaciated)

Southeastern Ohio (unglaciated)

Page 25: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

#7- continued

__________________________________ - sharp, pyramid-shaped peaks at the tops of mountains.

Horns

Page 26: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

The Matterhorn

Page 27: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

#7 - continued

__________________________________ - jagged ridges formed between two or more cirques or glacial valleys.

Aretes

Page 28: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

#7- continued

__________________________________ - bowl-shaped depressions where glacial ice cuts into mountain walls.

Cirques

Page 29: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

#7- continued

__________________ ________________ - smaller stream valleys that join a glacial valley by way of a steep, vertical drop. These often result in very tall waterfalls.

Hanging valleys

Yosemite Valley, CA

Page 30: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #8

The moving ice in glaciers has the power to erode (transport) everything from small soil particles to huge boulders. The material carried and eventually deposited by glaciers is called _______________ ____. Eventually this material gets deposited where the ice carrying it melts. This occurs at the terminus (outer or lower edge) of the glacier.

Glacial drift

Page 31: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide- item #9

Glacial deposits form in one of two ways. If the drift is dropped down directly by the melting ice, it creates an unsorted (mix of different size) deposit known as ___________________. This type of deposit often forms ridges at the edge of the glacier called ___________________________.

Till (glacial till)

Moraines (terminal moraines)

Page 32: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

MORAINE

Page 33: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

A moraine

Page 34: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Glacial Erratics (till deposit)

This boulder was transported hundreds of miles by a glacier!

Page 35: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study Guide- item #10

Glacial deposits are often sorted by streams of meltwater flowing from the glacier as it melts. These streams erode and deposit drift by size. These sorted deposits are known as _______ __________. These deposits form a type of alluvial fan called an

___________ __________.

 

Stratified drift

Outwash plain

Page 36: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Outwash

Outwash plain (stratified drift)

Page 37: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Outwash Plain

Page 38: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Study guide – item #11

Within these deposits it is common for blocks of ice that have broken away from the retreating glacier to become buried within the stratified drift. As these melt, they form small, round lakes called _______ _____________.

 

Kettle lakes

Page 39: Erosion and Deposition by Glaciers Chapter 4: Topic 8.

Outwash

Outwash plain (stratified drift)