GLACIAL LANDFORMS SHAPE MOUNTAINS Surface features subglacial erosional
GLACIAL LANDFORMS SHAPE MOUNTAINS • • Surface features subglacial erosional depositional
1) Glacier travel: Surface features Crevasses: – V-shaped structures found in the uppermost layer of the glacier. WHY? – brittle deformation – Rarely > 20 m deep
Accumulation area is often heavily crevassed Direction of flow New Zealand
Bergschrund: crevasse that separates flowing ice from stagnant ice at the head of a glacier Glacier on Shorong Yul-lha, Nepal
Icefall: steep, cracked and jumbled ice flows over a drop-off - fast moving!!!! Khumbu Ice fall, Everest
Ogives: alternate bands of light and dark ice on a glacier
Séracs: • Ice towers • Formed by intersecting crevasses, • rapid flow • steep slopes Glacier des Bossons, French Alps photo: MH
Penitentes: spiky columns of snow; formed in dry environments Nev. Coropuna, Peruvian Andes
Melt stream: Glacier can have streams on their surface!! Moulins Very slushy and slippery!! water
SUB-GLACIAL STREAMS
ICE CAVE AT BOTTOM OF GLACIER Pastoruri, Peru
EROSIONAL LANDFORMS OVERVIEW
CIRQUE • a semicircular or amphitheater -shaped bedrock feature created as glaciers scour back into the mountain. • This is where the snow and ice forming the glacier first accumulates.
HANGING GLACIER Occur in tributary glaciers, cause spectacular waterfalls
ARÊTE • steep-sided, sharp-edged bedrock ridge formed by two glaciers eroding away on opposite sides of the ridge
HORN • a pyramid-shaped mountain peak created by glaciers eroding away at different sides of the same mountain.
COL • a low spot or pass along a cirque or an arete.
GLACIAL POLISH Result of abrasion by sand at bottom of glacier
STRIATIONS • result of individual particles embedded in the glacier scratching the underlying bedrock. • lines indicate the orientation of glacial flow.
NUNATAK • Peak surrounded by glaciers but not itself glaciated
TARN • a glacial lake produced by scouring • often found in cirques.
U-shaped valleys • a glacially eroded valley • large, flat valley bottom
ROCHE MOUTONNÉE sheepback , or sheep rock large rock knob that resembles a grazing sheep
DEPOSITION LANDFORMS
Moraines • an accumulation of unconsolidated material deposited by glaciers • unsorted material (different sizes of particles) particles deposited in moraines • material has angular edges.
TERMINAL OR END MORAINE • deposited at the snout end of a glacier • marks the furthest advance of a glacier • caused as a glacier retreats End morraine
LATERAL MORAINE unconsolidated material deposited along the sides of an alpine glacier. Lateral morraine
MEDIAL MORAINE When two alpine glaciers flow together, their lateral moraines join, forming a medial moraine
MORAINES: OVERVIEW Medial Moraine
ERRATICS Large boulders left by glaciers in areas where they obviously don’t belong. Can be 10’s to 100’s of kilometers form point of origin
GLACIER LANDFORMS OVERVIEW
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