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

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Snow line – where snow remains year round
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    21-Dec-2015
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Transcript of Snow line – where snow remains year round. Formation of Glacial Ice from Snow.

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

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Forming Glacial Ice

Initial Form

2 weeks

7 weeks

8 weeks

Snow Firn Glacial Ice

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Glacier movement

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

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

Types of Glaciers

slip

Plasticdeformation

Ice Deformation with Slip

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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

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

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Terminus

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Advance & Retreat: Moraines

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Alpine Moraines and Till

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Moraine Types

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Anatomy of a Glacier

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Piedmont glacier

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

Calving

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Different kinds of glaciers

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

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Retreat of North American (Laurentide) ice sheet

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

Different kinds of glaciers

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Ice cap and continental (ice sheet)

Sentinal Range, Antarctica

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

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Greenland Ice Sheet

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Greenland

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