Top Banner
12

Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Jan 04, 2016

Download

Documents

Paulina Woods
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 2: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Abrasion• In glaciers abrasion occurs when rocks and

stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the glacier as it moves.

Page 3: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Arête• A steep-sided, sharp-edged bedrock ridge formed by two

glaciers eroding away on opposite sides of the ridge.

Page 4: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Drumlin• Drumlins are formed of till. They are elongated features

that can reach a kilometer or more in length, 500m or so in width and over 50m in height. One end is quite step,

whilst the other end tapers away to ground level.

Page 5: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Esker• a long, narrow, winding ridge composed of stratified

sand and gravel deposited by a glacial melt water stream. Eskers may range from 16 to 160 feet in height, from 160 to 1,600 feet in width, and a few hundred feet

to tens of miles in length.

Page 6: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Erratics• Glacial erratics are stones and rocks that were

transported by a glacier, and then left behind after the glacier melted.

Page 7: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Striations• Glacial striations are scratches or gouges

cut into bedrock by glacial abrasion.

Page 8: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Horn• is an angular, sharply-pointed mountain peak which

results from the cirque erosion due to multiple glaciers diverging from a central point.

Page 9: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Kettle Lake• A kettle (kettle hole, pothole) is a shallow, sediment-filled

body of water formed by retreating glaciers or draining floodwaters.

Page 10: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Moraine• are long, sharply crested ridges made up of a mixture of

sand, gravel, and rocks that have been deposited by a melting glacier

Page 11: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Tarn• A tarn is a mountain lake or pool, formed in a cirque

excavated by a glacier. It is formed when either rain or river water fills the cirque. A moraine may form a natural dam below a tarn.

Page 12: Abrasion In glaciers abrasion occurs when rocks and stones are picked up by the glacier and are rubbed against the bedrock at the bottom and side of the.

Cirque• The concave amphitheatre shape is open on the downhill

side corresponding to the flatter area of the stage, while the cupped seating section is generally steep, cliff-like slopes down which ice and glaciated debris combine and converge from the three or more higher sides.