Glaciers.

Slides:



Advertisements
Similar presentations
Glaciers and Long Island
Advertisements

Glaciers, Desert, and Wind
GLACIAL LANDFORMS SHAPE MOUNTAINS
1. 4. Understand how. moving ice acts as an. agent of erosion and
Chapter 13: Glacial Processes, Patterns and Associated Landforms
Glaciers.
Erosion: Deposition: AIM: Erosional and Depositional systems
  Glacier: thick mass of ice, forms over land  Compaction and recrystallization of snow  Glacier Types: Glacier Types:  Valley (alpine) glaciers –
Glaciers and Glaciation Physical Geology, Chapter 22.
Form in high mountains where snow accumulates to sufficient depths so that it is compressed, compacted and recrystallized. For this reason glacial.
Outline GLACIERS 1)Types of glaciers 2)Glacier formation, movement 3)Glacial erosion 4)Glacial landforms and deposits 5)Side effects 6)Ice ages.
Erosion and Deposition by Glaciers Created By: Belinda Schmahl.
Charity I. Mulig.
Principles of Geology Glaciers Mian Liu.
Glaciers and Glacial Landforms
Glaciers.
Glaciers Galore Ice Queen Period 1 Earth Science Honors November 30, 2013 The last Ice Age (Wisconsian) occurred over the last 2-3 million years (1). The.
CHAPTER 5 HONORS EARTH SCIENCE
GLACIERS CHAPTER 5 HONORS EARTH SCIENCE. What is a glacier? a thick mass of moving ice
Erosive Forces Review. Glacial Movement Glacial Erosion Glacial Deposition Wind Coastline Features
Landform Geography Fluvial Systems and Landforms.
Essentials of Earth Science
Ch. 5 Glaciers & Ice Ages p guided notes.
Charity I. Mulig.
‘S‘S. VOCABULARY GLACIER - LARGE MOVING MASS OF ICE THAT FORMS NEAR EARTH’S POLES AND IN MOUNTAINOUS REGIONS AT HIGH ELEVATIONS. GLACIER - LARGE MOVING.
Aim: What are Glaciers? I. Glacier – found at high altitudes and high latitudes. These are locations where more snow falls during the winter than melts.
Nature’s Bulldozers CGF3M Wed. Nov. 6, Glacial Erosion As glaciers move, they erode the land in two ways: plucking and abrasion. - Plucking occurs.
Glaciers.
Glaciers Ch 13.
Glaciers.
Chapter 3 Section 4 Glaciers. Moving mass of ice and snow Form when more snow falls than melts Agent of erosion.
Unit 1: Land and Water Forms Glaciers as Agents of Erosion
Ch 15: p  Enormous masses of moving ice created by the accumulation and compaction of snow.  Powerful agents of erosion ~ have carved some.
World Geography Unit 1: Land and Water Forms Glaciers as Agents of Erosion.
GLACIERS AND GLACIATION. GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation.
Chapter 21: The Glacier Systems and the Ice Age Presentation.
Glaciers and Glaciation. Glaciers Glaciers are parts of two basic cycles Hydrologic cycle Rock cycle Glacier – a thick mass of ice that originates on.
Glaciers Galore Ice Queen Period 1 Earth Science Honors November 30, 2013 The last Ice Age (Wisconsian) occurred over the last 2-3 million years (1). The.
glaciers & glaciation Types of glaciers How do glaciers move?
An introduction to where, how, and why glaciers form
Chapter 18: Glaciers. Introduction Glacier: thick mass of ice that originates on land from the accumulations, compaction and recrystallization of snow.
Glaciers and Erosion Chapter 7 Section 1.
Glacier Notes.
Guided Notes For Glaciers Section 8.3. Glaciers shape the landscape by eroding, transporting, and depositing huge volumes of rock and sediment.
Geologic Features of Glaciation
Glacial Landscapes Glacier = large moving mass of ice. Glacier = large moving mass of ice. Glaciers erode, transport and deposit massive amount of sediment.
Erosive Forces Review. Glacial Movement Glacial Erosion Glacial Deposition Wind Wave Erosion
Mysterious rock formations…….. What could have caused these formations? GLACIERS!!!!!
AIM: How do Glaciers change the landscape? Do Now:
GLACIERS AND GLACIATION. GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation.
Chapter 8 Erosional Forces Section 8-2 Glaciers Note Guide.
Study Guide Chapter What is a glacier? 2.Distinguish between alpine and continental glaciation. 3.Explain how a glacier moves. Explain how a crevass.
Glaciers & Glaciation. Glaciers Glacier: a large, long-lasting mass of ice, formed on land that moves under the influence of gravity and its own weightGlacier:
UNIT 5WEATHERING: (B) GLACIERS Glacier-large long-lasting mass of snow compacted & recrystallized, first into firn then glacial ice. Glaciers part of hydrosphere.
Glacier: Any large mass of ice that moves slowly over land.
Chapter 17 Glaciers.
Glaciers. “ RIVERS OF ICE ” Mass movement of frozen ice on land Mass movement of frozen ice on land Form at high elevations or high altitude Form at high.
Chapter 7.1b Glaciers.
Ice, Ice, Baby! Glaciers and Glacial Features Photo Source:
Glacier Review.
Erosion and Deposition by Ice
Understand how moving ice acts as an agent of erosion and deposition.
Glaciers.
Prairie School Earth Science
Glaciers and Glaciation
GLACIERS A LARGE MASS OF ICE ON LAND THAT FLOWS UNDER THE PRESSURE OF ITS OWN WEIGHT – DOWNHILL OR OUTWARD DUE TO GRAVITY.
Earth Science Chapter 8 Section 3
Glaciers.
Glaciers Glaciers are a part of both the hydrologic cycle and rock cycle Glacier – a thick mass of ice that forms over land from the compaction and recrystallization.
What are Glaciers? Masses of ice formed on land by the compaction of snow.  Factor of glacier movement: gravity (caused by weight of ice)
Presentation transcript:

Glaciers

Glacier - a thick ice mass that originates on land from the accumulation, compaction, and recrystallization of snow. Formation of glacial ice from snow

1. Ice sheets, Continental glacier Glacier Types 1. Ice sheets, Continental glacier Large scale – cover 10% of Earth’s land Greenland – 1.7 million km2 Antartica – 13.9 million km2

Continental Glaciers

2. Valley, Mountain, Alpine Glacier Types 2. Valley, Mountain, Alpine Smaller than ice sheets Lengths greater than widths Only cover a small region

Alpine Glaciers

Greenland

Bylot Island, Canada

Glacier movement 50 meters 100 meters

Glacier movement

Glacier movement Plastic flow – flowing solid 200 m/yr Basal slip – movement over bedrock 200 m/yr http://www.youtube.com/watch?v=xRZaDJxFjIA

http://www.youtube.com/watch?v=sJmWQk492W0 http://www.youtube.com/watch?v=89sOW-FzolI https://www.youtube.com/watch?v=hC3VTgIPoGU

Glacier movement Rotation of Grains Melting & Freezing Internal Slipping

Glacier budget In: Zone of accumulation – snow accumulates Out: Zone of ablation – general term for loss of ice or snow from a glacier Melting Calving - icebergs

Glacier budget

Glacial Calving

Dry calving with recumbent folds

Sub-glacial River

Surface Drainage

Glacier Erosion Plucking – loosen and lift blocks of rock Abrasion – rock flour Striations – grooves scratched in bedrock

Glacial Landforms Mountian Glaciers – tend to accentuate the landscape Continental Glaciers – tend to subdue the landscape

Mountain Glaciers

Mountain Glaciers Landforms Hanging valley – a tributary that enters a glacial trough high above the floor of the trough. Arete – a narrow , knifelike ridge separating two adjacent glaciated valleys. Horn – a pyramid-like peak formed by glacial action in three or more cirques surrounding a mountain summit.

Mountain Glaciers Landforms Tarn – a small lake in a cirque. Cirque – an ampitheater-shaped basin at the head of a glaciated valley. Truncated spurs – eroded triangular shaped cliffs in glaciated valleys. Glacial trough – U-shaped glacial valley

Mountain Glaciers

Ice Dammed Lake

Glacial Deposits Drift (general term) – Sediment deposited on land or in water as a result of glaciation. 1. Till – Unsorted debris transported by glaciers and deposited on land. 2. Sorted Sediments – Sediments transported by melt water are deposited in Eskers and in the Outwash Plain.

Till Deposits Moraines - a pile of debris that has been transported and deposited by a glacier Erratics - boulders left on the surface

Erratic

Terminal Moraine - Debris pushed along in front of the glacier Ground Moraine - debris accumulated under the glacier