© boardworks ltd 20121 of 8 this icon indicates that the slide contains activities created in...

8
© Boardworks Ltd 2012 1 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not For more detailed instructions, see the Getting Started presentat These icons indicate that teacher’s notes or useful web addresses are available in the Notes Page. Glacial Landforms Part 1

Upload: duane-conley

Post on 17-Dec-2015

216 views

Category:

Documents


1 download

TRANSCRIPT

Page 1: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20121 of 8

This icon indicates that the slide contains activities created in Flash. These activities are not editable.

For more detailed instructions, see the Getting Started presentation.

These icons indicate that teacher’s notes or useful web addresses are available in the Notes Page.

Glacial LandformsPart 1

Page 2: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20122 of 8

Key Questions

What landforms are created by glacial erosion?What landforms are created by glacial deposition?How can glacial features be identified on maps?

Glacial Landforms

Page 3: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20123 of 8

The landforms created by glacial erosion covered in this part are:

Corries Arêtes

Pyramidal peaks

Glacial troughs (U-shaped valley)

Truncated spurs Hanging valleys

Landforms created by glacial erosion

Page 4: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20124 of 8

Snow collects in a natural hollow on the side of a mountain. Over time, further snow collects in the hollow. This extra weight compresses the snow underneath, turning it into ice.

The hollow is deepened and widened by the corrie glacier through the processes of abrasion and plucking.

rock lip

This overdeepening leads to an ‘armchair’ shape characteristic of a corrie and causes a ‘rock lip’ to be formed.

How is a corrie formed?

Page 5: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20125 of 8

Corrie formation

Page 6: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20126 of 8

Diagram of a corrie

Page 7: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20127 of 8

Explain the formation of a corrie

Page 8: © Boardworks Ltd 20121 of 8 This icon indicates that the slide contains activities created in Flash. These activities are not editable. For more detailed

© Boardworks Ltd 20128 of 8

tarn

bowl-shaped corrie

steep backwall

Example of a corrie: Cwm Idwal