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Chapter 3 Section 4 Glaciers. Glaciers. Agent of erosion. Moving mass of ice and snow Form when more snow falls than melts. Glaciers. Advancing Glacier -When the glacier increases in size and slides forward due to gravity.
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Chapter 3 Section 4 Glaciers
Glaciers Agent of erosion • Moving mass of ice and snow • Form when more snow falls than melts
Glaciers Advancing Glacier-When the glacier increases in size and slides forward due to gravity Retreating Glacier-When the glacier decreases in size because it is melting
Valley Glacier (Alpine) Muddy River Glacier, Alaska 1948 • Located in mountainous areas • Snow and ice build up in a long, narrow v-shaped river valley
Continental Glacier • Huge mass of ice and snow (larger than valley glacier) • Usually covers a large portion of land like a continent • Only tallest peaks of land are exposed • Today cover 10% of earth's surface (found in Greenland & Antarctica)
Last Ice Age White is land covered in ice. You are here. Continental glaciers cover large portions of the world at one time http://cabrillo.edu/~crsmith/glacloop.gif
Last Ice Age Blue is land covered in ice. You are here.
Leading Edge of Glacier Person
How do glaciers form and move? Snow accumulates and piles up faster than it melts Weight of snow is great enough to compress bottom layers into ice Ice on bottom partially melts and becomes putty like Whole mass begins to slide on this putty-like layer When the mass of the glacier is too great, gravity pulls
Abrasion & Plucking Abrasion-Glaciers gouge and scratch land below as it moves Plucking-Glacier picking up rocks as it travels
How do glaciers erode Earth’s surface? • As they move, glaciers act as bulldozers pushing loose material out of their path • These eroded sediments are added to the mass of the glacier (plucking) or piled up along its sides • Glaciers also grind rock and soil that isn't loose (abrasion)
Striations The “stripes” scratched into rocks by glacial abrasion.
Where a glacier deposits mounds or ridges of till (sediment) Moraine
The ridge of till at the farthest point reached by a glacier (Long Island & Cape Cod-terminal moraine from last ice age) Terminal Moraine
How do glaciers deposit sediment? • Glaciers begin to melt and lose their energy of motion • Begin to deposit sediments they carry (till ) • Till at the edges of a glacier (moraine) • Till at the end of a glacier (terminal moraine)
How do glaciers shape the land? What kinds of glacial landforms are created?
Kettle Lake Formation Kettle-small depression formed by a chunk of glacial ice left behind
Kettle Lake Contain water all year long Kettle lake- kettle that fills with water from melted ice blocks
Glacial Lake Contain water all year long Glacial lake- Forms like a kettle lake, but high in the mountains
Horn-mountains with sharp pointed peaks Arête-sharp edges that run down mountain sides (separating 2 cirques)
Cirque-a bowl-shaped hollow in mountain side where glacier began
U-shaped valley- a valley carved by glaciers in U-shape, usually from a v-shaped river valley
Fiord (Fjord) Fiord- a coastal valley cut by glacier that fills in with water when seas rise from glacial melt
Drumlin-mounds of till that a glacier slides over and as the glacier melts back the mound becomes uneven Glacier Direction of flow
The following photos are courtesy of a former student’s family vacation to Alaska
What am I showing you? Where a glacier makes an ICEBERG
What am I showing you? The TILL from plucking & abrasion that will be laid down when the glacier melts
What am I showing you? The carving power of a glacier U-SHAPED VALLEY, HORN, ARÊTE
What am I showing you? Drumlin -Which direction was the glacier flowing?
What am I showing you? Glacial Lake
What am I showing you? Valley Glacier