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Evidence for Evidence for Glaciers Glaciers Erratics Erratics Striations Striations Polished Bedrock Polished Bedrock
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Glacial Landform

Apr 15, 2017

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Page 1: Glacial Landform

Evidence for GlaciersEvidence for GlaciersErraticsErraticsStriationsStriationsPolished BedrockPolished Bedrock

Page 2: Glacial Landform

Erratic

Page 3: Glacial Landform

ErraticErratic Boulder-sized rock Boulder-sized rock

dumped by a dumped by a glacierglacier

Rock is different Rock is different type than type than surrounding rockssurrounding rocks

Page 4: Glacial Landform
Page 5: Glacial Landform

Striations

Page 6: Glacial Landform

Striations/ Chatter marksStriations/ Chatter marks Grooves carved Grooves carved

into bedrockinto bedrock Formed by Formed by

abrasive action of abrasive action of cobbles and cobbles and pebbles carried at pebbles carried at bottom of glacierbottom of glacier

Direction of Direction of scratches shows scratches shows direction glacier direction glacier movedmoved

Page 7: Glacial Landform

Glacial polishGlacial polish Smooth rock Smooth rock

surfacessurfaces Created as glaciers Created as glaciers

flow over bedrockflow over bedrock

Page 8: Glacial Landform

Glacial Pavement….Glacial Pavement….

Page 9: Glacial Landform

Luis María Benítez.

Page 10: Glacial Landform

Source unknown

Page 11: Glacial Landform

ZONE OF

ACCUMULATION

ZONE OF

ABLATION

The Upper Grindelwald Glacier and the Schreckhorn, in the Bernese Oberland, Switzerland.

Adrian Pingstone

Page 12: Glacial Landform

crevassecrevassessA great fissure or A great fissure or

crack in a glacier.crack in a glacier. They can be more than 30 m deep They can be more than 30 m deep

Page 13: Glacial Landform

The Perito-Moreno Glacier, Argentina

TOP LAYER OF GLACIER CAN FRACTURE…..BRITTLE BEHAVIOR

FROMS CREVASSES

http://www.chmouel.com/geeklog/gallery/gallery_individual.php/argentina/8.html

Page 14: Glacial Landform

Original valley (V-shaped)

Glaciers come and alter landforms

Glaciers retreat and newfeatures appear

Page 15: Glacial Landform
Page 16: Glacial Landform

Landscape Features- Landscape Features- Valley GlaciersValley Glaciers

CIRQUESCIRQUES: : semi-circular shaped bedrock feature semi-circular shaped bedrock feature created as a glacier scours back toward the mountaincreated as a glacier scours back toward the mountain

Page 17: Glacial Landform

ARÊTESARÊTES: : steep-sided, sharp-edged bedrock ridgesteep-sided, sharp-edged bedrock ridge formed by two glaciers eroding away formed by two glaciers eroding away

on opposite sides of a ridgeon opposite sides of a ridge

Page 18: Glacial Landform

CIRQUE

TARN

TARNS:TARNS:glacial lakes glacial lakes produced by glacial scouringproduced by glacial scouringoften found in cirquesoften found in cirques

Page 19: Glacial Landform

HORNSHORNS:: 3 or more cirques adjacent to one 3 or more cirques adjacent to one

anotheranother

Page 20: Glacial Landform

Hanging Valley

Page 21: Glacial Landform

ARÊTE CIRQUE

HANGING VALLEY

U-SHAPED VALLEY

Page 22: Glacial Landform

U-shaped valley

Page 23: Glacial Landform

tilltillUnsorted and Unsorted and unstratified rock unstratified rock material deposited material deposited dirtectly by glacial dirtectly by glacial ice.ice.

Landforms made from Landforms made from glacial till are called glacial till are called moraines. moraines.

Page 24: Glacial Landform

Glacial till sediment, in some places hundreds of feet thick, covers most of New York State.

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Page 25: Glacial Landform

All the ‘stuff’ that’s pushed out of the way by the glacier gets piled up in a big heap,

called moraine.

Terminal moraine

Lateral moraine

Medial moraine

Page 26: Glacial Landform
Page 27: Glacial Landform

Lateral moraine

Dirk Beyer

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Lateral moraine

Page 29: Glacial Landform

Image by Michael Collier

Medial MoraineMedial Moraine

MorainesMoraines Chugach Chugach

Mountains, Mountains, AlaskaAlaska

Image by Bruce Molnia, Terra

Photographics

Page 30: Glacial Landform
Page 31: Glacial Landform
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MORAINESMORAINES: material left behind : material left behind when glacier recedeswhen glacier recedes

Page 33: Glacial Landform

Kettle Lake

Till

Drumlins

Terminal MoraineGlacial Stream

Moraine-dammed lake

Outwash

plain

Esker

Page 34: Glacial Landform

Drumlin

Page 35: Glacial Landform

drumlins

Page 36: Glacial Landform

Kettle Lakes

Page 37: Glacial Landform

eskereskerA long, winding A long, winding ridge formed ridge formed when sand and when sand and gravel fill gravel fill meltwater meltwater tunnels tunnels beneath a beneath a glacier.glacier.

Page 38: Glacial Landform

Eskers

Page 39: Glacial Landform

kamekame A small, cone-A small, cone-shaped hill of shaped hill of stratified sand stratified sand and gravel and gravel formed at a formed at a glacial front by glacial front by meltwater meltwater carrying carrying sediment off sediment off the glacier’s the glacier’s surface.surface.

Page 40: Glacial Landform

http://www.env.duke.edu/eos/geo41/gla2.htm

KAME (WISCONSIN)

Have sorted sediments

Page 41: Glacial Landform

outwashoutwash

When a When a glacier glacier melts, melts, its rock its rock load load remains remains in nearly in nearly the the same same place as place as in the in the glacier.glacier.

Page 42: Glacial Landform

Outwash plainOutwash plainAn outwash An outwash plain will be plain will be crossed by crossed by many many meltwater meltwater streams. streams.