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GLACIERS AND GLACIATION. GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation.

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Presentation on theme: "GLACIERS AND GLACIATION. GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation."— Presentation transcript:

1 GLACIERS AND GLACIATION

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3 GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation Continental glaciation

4 Ice Ages Northern Europe & North America heavily glaciated –Pleistocene 1.8 million years BP to 10,000 ybp 4 episodes – Peak of glaciation (Wisconsin) 18,000 years ago

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6 Glaciers-Where they are Develop where all of annual snow doesn’t melt away in warm seasons: Accumulation rate rate exceeds ablation (melting) rate – Polar regions – Heavy winter snowfall – High elevations – 85% in Antarctica – 10% in Greenland

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8 Types of Glaciers Valley or Alpine glacier Ice sheet –Continental Glaciers

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12 GLACIERS Wastage of glaciers (“shrinkage”) – Melting more melting at lower elevations – Evaporation – Calving into Icebergs where a glacier flows onto a sea

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14 Movement of Glaciers Valley Glaciers – Gravity driving force – Sliding along its base -basal sliding – Internal flowage- plastic flow – Rigid zone Crevasses may form here Ice sheets – Move downward & outward from central high

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18 Glacial Erosion Under glacier – Abrasion & plucking – Bedrock polished & striated – Rock flour washes out of glacier – Polishing and rounding “Sheep Rocks” – Striations- scratches & grooves on rock Above glacier – Frost wedging takes place – Erosion by glaciers steepens slopes

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21 Erosional Landscapes Associated with Alpine Glaciation Glacial valleys –U-shaped valleys –Hanging valleys –Rock -basin lakes (tarns) –Rounded knobs- rouche moutonnees

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25 Erosional Landscapes Associated with Alpine Glaciation Cirque - at head of valley glacier –Rock steps Rock basin lakes Horn Arete- sharp ridge

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30 Erosional Landscapes Associated with Continental Glaciation Grooved and striated bedrock –Grooves may be channels Rounded hills & mountains

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32 Glacial Deposition Till –Unsorted debris (Boulders to Clay) Erratic- Large Boulders moved from far away Moraine- body of till –Lateral Moraine –Medial Moraine- where tributaries join –End moraine- Terminal Recessional –Drumlin

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35 Glacial Deposition Outwash –Stream-deposited sediment sorted –Braided streams typical –Esker –Kettle

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38 Effects of Past Glaciation Glacial ages Direct effects in North America –Scoured much of Canada –Cut Great Lakes –Deposited till & flattened Midwest –Extensive alpine glaciation in mountains

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