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Glaciation Presentation
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Glaciation Standard Grade Geography Alan Doherty Linlithgow Academy
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Climate Change is not new!
From “Glaciers” by John Gordon Colin Baxter Publications, 2001
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Interglacial periods Glacial periods From “Glaciers” by John Gordon
Colin Baxter Publications, 2001
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Snow collects in hollows
Snow builds up during the winter (accumulation) and melts during the summer (ablation) If accumulation is greater than ablation the snow builds up in layers Pressure gradually turns the snow into ice When the critical mass of ice is reached, the ice begins to move downhill A glacier is born!
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Snowflakes are compressed and squeezed into ice crystals
n.b. the colour changes from white to blue!
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How does ice flow? With difficulty!
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1.SNOW BUILDS UP IN HOLLOWS IN THE HILLSIDE
GLACIATION 1.SNOW BUILDS UP IN HOLLOWS IN THE HILLSIDE 2. THE SNOW COMPACTS INTO ICE 3. THE ICE “FLOWS” DOWN THE MOUNTAINSIDE 4. THE GLACIER PUSHES FORWARD AND MELTS BACK
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Valley Glaciers nasa Denali, in Alaska
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Ice Sheets From “Earth from Above” by Yann Arthus-Bertrand
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If the ice covers the whole area then the mountain tops are rounded e
If the ice covers the whole area then the mountain tops are rounded e.g. Scotland If the mountain tops remain above the ice then frost action makes them “jaggy” e.g.the Alps
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Past and Present Ice Limits
From “Earth Story” By Lamb and Sington
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GLACIATION GLACIERS ERODE TRANSPORT and DEPOSIT
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Glacial Erosion Glaciers erode in two ways
Abrasion - this occurs when stones embedded in the bottom of the glacier scrape across the ground Plucking - this occurs when the bottom layer of ice freezes on to the ground when the ice is stationary. When the glacier begins to move, bedrock material may be torn from the ground.
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Glacial Erosion Cirque = Corrie = Cwm
From “A2 Geography for AQA specification A” by Bowen, A & Pallister, J. Reprinted by permission of Harcourt Education Cirque = Corrie = Cwm
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Aretes or sharp ridges arete corrie corrie tributary glacier
main glacier
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A corrie is a hollow in the hillside
arete End moraine Corrie or cirque Lochan or tarn Mountain top
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Aretes and pyramidal peaks
Arete ridge
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U-shaped valley
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U-shaped valley Hanging valley Misfit stream
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Ribbon Lake
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Transportation Material which is carried along by the ice is called moraine. Large stones which are dropped as the ice melts are called erratics.
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Transportation
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Transportation From “A2 Geography for AQA specification A” by Bowen, A & Pallister, J. Reprinted by permission of Harcourt Education
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by water: fluvio-glacial
Deposition by ice: moraine by water: fluvio-glacial
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by ice: moraine (boulder clay)
Deposition by ice: moraine (boulder clay) by water: fluvio-glacial (sands & gravel)
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Glaciation End of part one Standard Grade Geography
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