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Snow line – where snow remains year round

Snow line – where snow remains year round. Formation of Glacial Ice from Snow

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Page 1: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Snow line – where snow remains year round

Page 2: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 3: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Formation of Glacial Ice from Snow

Page 4: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Forming Glacial Ice

Initial Form

2 weeks

7 weeks

8 weeks

Snow Firn Glacial Ice

Page 5: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 6: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Glacier movement

• When glacier reaches critical mass (> 20m thick), flow occurs

Page 7: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 8: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Types of Glaciers

slip

Plasticdeformation

Ice Deformation with Slip

Page 9: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

What happens as ice melts

• Ice melt flows down to bedrock through crevasses and moulins (large tunnels)

• Water between bedrock and ice sheet acts as lubricant

• Allows ice sheet to move faster toward the coastline

Page 10: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

• Ice movement-rate increases from~30 cm per day in winter to ~40 cm per day in the summer

Page 11: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Terminus

Page 12: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Advance & Retreat: Moraines

Page 13: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Alpine Moraines and Till

Page 14: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Moraine Types

Page 15: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Anatomy of a Glacier

Page 16: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 17: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Piedmont glacier

Page 18: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Types of Glaciers – Piedmont & Tidewater Piedmont: Originally confined alpine, spread at foot of mountains

Calving

Page 19: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Different kinds of glaciers

Page 20: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Ice extent Last Glacial Maximum (21,000 yr BP)

Page 21: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Retreat of North American (Laurentide) ice sheet

Page 22: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 23: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 24: Snow line – where snow remains year round. Formation of Glacial Ice from Snow
Page 25: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Different kinds of glaciers

Page 26: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Ice cap and continental (ice sheet)

Sentinal Range, Antarctica

Page 27: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Ice cap (Vatnakjokull in Iceland)feeds “outlet glaciers”

Page 28: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Greenland Ice Sheet

Page 29: Snow line – where snow remains year round. Formation of Glacial Ice from Snow

Greenland

Page 30: Snow line – where snow remains year round. Formation of Glacial Ice from Snow