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<!-- 1. What is a glacier? Why is the study of glaciers important and how are glaciers studied today? -->
 
<!-- 1. What is a glacier? Why is the study of glaciers important and how are glaciers studied today? -->
 +
A glacier is a large body of ice and snow that moves under its own weight. Glaciers may form in mountains (alpine glaciers) or across broad areas (continental glaciers) through repeated seasonal snowfall that does not melt. Overtime, the snow is compacted to firn and then to ice, squeezing out air bubbles and becoming a solid mass. The weight of a glacier pushes it across the ground or downslope. Alpine glaciers are often referred to as "rivers of ice," an apt description of these very slow-moving solid water bodies.
 +
 +
The study of glaciers, called glaciology, is an interesting science that brings together elements of geology, hydrology, chemistry, physics, climate and paleo-climate studies, among other fields. Studying glaciers provides insights into geological landforms and how they were made, allows study of changing climate over time both through the advance and retreat of glaciers and through studying the layers of compacted ice by drilling ice cores. Chemical analysis of these cores can show changes in relative atmospheric carbon dioxide, for example, or even capture records of past volcanic activity or plant spores. The rate of glacial retreat offers ways to consider and measure the changing climate. At times, glaciers may reveal ancient artifacts or even frozen mummies that offer anthropological and archeological details of past usage of places, lifestyles, and suggestions of climate.
 +
 +
Glaciologists may work in the field, mapping and measuring glaciers by using satellites and drones, tracking advance and retreat by placing lines of poles on active glaciers, or studying past climate and atmosphere through drilling ice cores. Continental glaciers in Antarctica and Greenland may be studies through permanent or seasonal scientific research stations, allowing continued access to the glaciers, where annual precipitation can be tracked, along with any changes in the glacier's movement.
  
 
<!--T:2-->
 
<!--T:2-->
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</noinclude>
 
</noinclude>
 
<!-- a. Crevasse -->
 
<!-- a. Crevasse -->
 +
[[File:Glacier Crevasse.jpg|thumb|A Crevasse on a glacier]] A crevasse is a crack in the surface of a moving glacier. Crevasses may be narrow or wide, shallow or deep.
  
 
<!--T:6-->
 
<!--T:6-->
Line 32: Line 39:
 
</noinclude>
 
</noinclude>
 
<!-- b. Firn -->
 
<!-- b. Firn -->
 +
Firn is a term for snow that has been compressed enough to eliminate air pockets. If it is compressed further, it will become glacial ice.
  
 
<!--T:8-->
 
<!--T:8-->
Line 41: Line 49:
 
</noinclude>
 
</noinclude>
 
<!-- c. Glacial drift -->
 
<!-- c. Glacial drift -->
 +
[[File:Glacial Drift.jpg|thumb|Glacial Drift]]
 +
Glacial drift is the term for sediment and debris moved or deposited by a glacier, whether directly through physical erosion and movement, or indirectly, as in debris moved further by water from a melting glacier. 
  
 
<!--T:10-->
 
<!--T:10-->
Line 50: Line 60:
 
</noinclude>
 
</noinclude>
 
<!-- d. Glacial erratic -->
 
<!-- d. Glacial erratic -->
 +
[[File:Small Glacial Erratics.jpg|thumb|Glacial erratics in a stream]]
 +
A glacial erratic is a rock or boulder transported by a glacier and left behind when the glacier retreats.
  
 
<!--T:12-->
 
<!--T:12-->
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</noinclude>
 
</noinclude>
 
<!-- e. Glacial lake -->
 
<!-- e. Glacial lake -->
 +
[[File:Glacial Lake.jpg|thumb|A glacial lake at the terminus of a former glacier]]A glacial lake is a pool of standing water on, in, or under a glacier, or formed by a glacier, often near its terminus.
  
 
<!--T:14-->
 
<!--T:14-->
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</noinclude>
 
</noinclude>
 
<!-- f. Icefall -->
 
<!-- f. Icefall -->
 +
[[File:Glacial Icefall.jpg|thumb|A glacial icefall - note the more jumbled appearance in the center where the slope is steeper]]
 +
An icefall is the equivalent of a glacial "waterfall," and occurs where a glacier moves over a steep gradient, fracturing the surface of the glacier.
  
 
<!--T:16-->
 
<!--T:16-->
Line 77: Line 92:
 
</noinclude>
 
</noinclude>
 
<!-- g. Kettle lake -->
 
<!-- g. Kettle lake -->
 +
[[File:Glacier Kettle Lakes.jpg|thumb|Several kettle lakes]]
 +
A kettle lake forms when glacial ice in an outwash plain melts in a depression.
  
 
<!--T:18-->
 
<!--T:18-->
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</noinclude>
 
</noinclude>
 
<!-- h. Névé -->
 
<!-- h. Névé -->
 +
Névé refers to the part of a glacier that is permanently covered with snow.
  
 
<!--T:20-->
 
<!--T:20-->
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</noinclude>
 
</noinclude>
 
<!-- i. Paternoster lake -->
 
<!-- i. Paternoster lake -->
 +
Paternoster lakes (referencing a priest, and thus a string of rosary beads) are a series or string of lakes left in a valley by a retreating glacier.
  
 
<!--T:22-->
 
<!--T:22-->
Line 104: Line 123:
 
</noinclude>
 
</noinclude>
 
<!-- j. Plucking -->
 
<!-- j. Plucking -->
 +
In glacial terms, plucking is the process of a moving glacier dislodging or lifting a rock or boulder from the bedrock, thus "plucking" it up from the bedrock and carrying it to deposit later (see glacial erratic).
  
 
<!--T:24-->
 
<!--T:24-->
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</noinclude>
 
</noinclude>
 
<!-- k. Serac -->
 
<!-- k. Serac -->
 +
A serac is a jagged pinnacle or tower of ice on a glacier.
  
 
<!--T:26-->
 
<!--T:26-->
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</noinclude>
 
</noinclude>
 
<!-- l. Subglacial stream -->
 
<!-- l. Subglacial stream -->
 +
[[File:Subglacial Stream r.jpg|thumb|A subglacial stream flowing out from the end of a glacier]]
 +
As the name implies, a subglacial stream is a stream that flows beneath a glacier.
  
 
<!--T:28-->
 
<!--T:28-->
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</noinclude>
 
</noinclude>
 
<!-- m. Tarn -->
 
<!-- m. Tarn -->
 +
A tarn is a lake formed in a cirque (a cirque is bowl-shaped depression at the head of an alpine glacier).
  
 
<!--T:30-->
 
<!--T:30-->
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</noinclude>
 
</noinclude>
 
<!-- n. Terminus -->
 
<!-- n. Terminus -->
 +
[[File:Terminus 3124.jpg|thumb|A glacial terminus ending on land]]
 +
[[File:Tidewater glacier 3017.jpg|thumb|The terminus of a tidewater glacier ends in the water]]
 +
The terminus (or tow) of a glacier is the furthest/lower margin of a glacier - ie the "end" of the glacier.
  
 
<!--T:32-->
 
<!--T:32-->
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</noinclude>
 
</noinclude>
 
<!-- 4. Name the two major types of glaciers and two subtypes of each. -->
 
<!-- 4. Name the two major types of glaciers and two subtypes of each. -->
 +
There are several ways to classify glaciers, but in general, they can be divided into Continental and Alpine Glaciers.
 +
Continental Glaciers are large glaciers that do not necessarily require mountains to form.
 +
 +
The main types of continental glaciers are Ice Sheets (covering more than 50,000 square kilometers, and currently including only the Greenland and Antarctic Ice Sheets) and Ice Caps, which are continental glaciers covering less than 50,000 square kilometers. A further extension of continental glaciers are Ice Shlfs - which are floating extensions of large glaciers into the water.
 +
[[File:Alpine Glacier.jpg|thumb|300px|Apline Glaciers]]
 +
Alpine glaciers form in mountains, are much smaller than continental glaciers, and may in fact be part of larger continental glaciers. Four main categories of alpine glaciers are Cirque Glaciers (which form in bowl-like depressions in the mountains, and may feed other glacier types), Valley Glaciers (glaciers flowing through valleys), Piedmont Glaciers (Glaciers that flow out of valleys and canyons onto flatter lowlands), and Ice Fields, which may be larger conglomerations of glacial ice forming in the mountains and feeding several valley or piedmont glaciers.
 +
 +
  
 
<!--T:36-->
 
<!--T:36-->
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</noinclude>
 
</noinclude>
 
<!-- a. Accumulation zone -->
 
<!-- a. Accumulation zone -->
 +
The area of a glacier where snowfall exceeds loss through melting or other processes
  
 
<!--T:40-->
 
<!--T:40-->
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</noinclude>
 
</noinclude>
 
<!-- b. Ablation zone -->
 
<!-- b. Ablation zone -->
 +
The area of a glacier where loss of ice and snow exceeds accumulation.
  
 
<!--T:42-->
 
<!--T:42-->
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</noinclude>
 
</noinclude>
 
<!-- c. Equilibrium line -->
 
<!-- c. Equilibrium line -->
 +
The area on a glacier between the Accumulation and Ablation zone, where the forces are equal.
  
 
<!--T:44-->
 
<!--T:44-->
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</noinclude>
 
</noinclude>
 
<!-- 7. Know the difference between valleys formed by rivers and streams, and valleys formed by glaciers. -->
 
<!-- 7. Know the difference between valleys formed by rivers and streams, and valleys formed by glaciers. -->
 +
[[File:Glacial valley 0818.jpg|thumb|A U-shaped valley formed by an earlier glacier]]
 +
[[File:U valley 9731.jpg|thumb|A U-shaped glacial valley, still actively being carved by a seasonal glacier]]
 +
In general, a valley formed by a river or stream is described as V shaped, whereas a glacial valley is U shaped.
  
 
<!--T:48-->
 
<!--T:48-->
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</noinclude>
 
</noinclude>
 
<!-- a. Arête -->
 
<!-- a. Arête -->
 +
[[File:Arete 9705.jpg|thumb|Arete - the sharp ridge between glacial cirques]]
 +
An Arête is the sharp, jagged peak that separates two glaciers or cirques.
  
 
<!--T:54-->
 
<!--T:54-->
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</noinclude>
 
</noinclude>
 
<!-- b. Cirque -->
 
<!-- b. Cirque -->
 +
[[File:Cirque 9636.jpg|thumb|A cirque]]
 +
[[File:Cirque 4881.jpg|thumb|A cirque being formed - note how the snowfield is beginning to carve the bowl-shaped deprression]]
 +
A Cirque is a bowl-shaped depression in alpine areas formed by a glacier.
  
 
<!--T:56-->
 
<!--T:56-->
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</noinclude>
 
</noinclude>
 
<!-- c. Col -->
 
<!-- c. Col -->
 +
A Col is a low point or pass in an Arête or ridge that has been formed through erosion.
  
 
<!--T:58-->
 
<!--T:58-->
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</noinclude>
 
</noinclude>
 
<!-- d. Drumlin -->
 
<!-- d. Drumlin -->
 +
A Drumlin is a tear or inverted half-canoe shaped ridge of debris shaped by a glacier. The pointed end points toward the glacier head, the flattened end is often steep.
  
 
<!--T:60-->
 
<!--T:60-->
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</noinclude>
 
</noinclude>
 
<!-- e. Esker -->
 
<!-- e. Esker -->
 +
An Esker is a steep-sided meandering ridge formed by a subglacial or englacial stream and left behind by a retreating glacier.
  
 
<!--T:62-->
 
<!--T:62-->
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</noinclude>
 
</noinclude>
 
<!-- f. Fjord -->
 
<!-- f. Fjord -->
 +
A Fjord is a U-shaped valley formed by a glacier that extends into the water below sea-level.
  
 
<!--T:64-->
 
<!--T:64-->
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</noinclude>
 
</noinclude>
 
<!-- g. Glacial horn -->
 
<!-- g. Glacial horn -->
 +
A Glacial Horn forms when three or more Cirques intersect, shaping a pyramidal mountain peak (think of the Matterhorn).
  
 
<!--T:66-->
 
<!--T:66-->
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</noinclude>
 
</noinclude>
 
<!-- h. Kame -->
 
<!-- h. Kame -->
 +
A Kame is a sand or gravel mound deposited by water flowing over a glacier.
  
 
<!--T:68-->
 
<!--T:68-->
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</noinclude>
 
</noinclude>
 
<!-- i. Nunatak -->
 
<!-- i. Nunatak -->
 +
[[File:Nunatak 9252.jpg|thumb|Nunatuks are visible on the left side of the image, poking through the glacial field]]
 +
A Nunatak is a mountain peak that protrudes through a glacier, or through where two or more glaciers meet and converge.
  
 
<!--T:70-->
 
<!--T:70-->
Line 318: Line 372:
 
</noinclude>
 
</noinclude>
 
<!-- j. Outwash fan -->
 
<!-- j. Outwash fan -->
 +
An Outwash Fan is an alluvial plain of graded debris laid down by glacial melt (think of it as a land-bound alluvial fan).
  
 
<!--T:72-->
 
<!--T:72-->
Line 327: Line 382:
 
</noinclude>
 
</noinclude>
 
<!-- k. Roche moutonnée -->
 
<!-- k. Roche moutonnée -->
 +
Roche moutonnée is the term for an elongated, rounded knob of bedrock shaped by a moving glacier, gently slowing on the "upstream" side and steeper on the "downstream" side. (Compare to a drumlin, which is formed by glacial till, rather than carved out of the bedrock).
  
 
<!--T:74-->
 
<!--T:74-->
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</noinclude>
 
</noinclude>
 
<!-- l. Striation -->
 
<!-- l. Striation -->
 +
[[File:Striations 5594.jpg|thumb|A museum specimen of rock showing striations caused by a passing glacier. ]]
 +
Striations refer to the lines and grooved carved into bedrock by a passing glacier. As the glacier moves, it also drags along rocks and other debris, and this scours the underlying rock, leaving the scratch marks.
  
 
<!--T:76-->
 
<!--T:76-->
Line 345: Line 403:
 
</noinclude>
 
</noinclude>
 
<!-- m. Trim line -->
 
<!-- m. Trim line -->
 +
[[File:Trimline 9736.jpg|thumb|The trim line is visible along the hillside, where the sharper cut can be seen in contrast to the more rolling upper part of the hill]]
 +
The Trim Line is the boundary on a glacial valley wall that shows the previous maximum width of the glacier.
  
 
<!--T:78-->
 
<!--T:78-->
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</noinclude>
 
</noinclude>
 
<!-- 10. What is a moraine? Name and describe three types of moraines. -->
 
<!-- 10. What is a moraine? Name and describe three types of moraines. -->
 +
Moraines are mounds of rock, sand, or other debris pushed up or deposited by a glacier. The main types of Moraines are:
 +
Terminal Moraine, which forms at the terminus or maximum extent of a glacier
 +
Lateral Moraine, which forms along the edge of a glacier from falling debris or eroded from the valley walls
 +
[[File:Medial moraine 9218.jpg|thumb|The medial moraine shows where two upper glaciers came together to form a larger single lower glacier]]
 +
Medial Moraine, which runs parallel to a glacier, but forms wheere two glaciers merge into a single flow
 +
[[File:Recessional moraine 9827.jpg|thumb|A recessional moraine, left behind by a retreating glacier]]
 +
Recessional Moraine, which forms as smaller accumulations behind the terminal moraine, and marks shorter periods of eadvance and retreat
  
 
<!--T:80-->
 
<!--T:80-->
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<noinclude><translate></noinclude>
 
<noinclude><translate></noinclude>
 
==References== <!--T:97-->
 
==References== <!--T:97-->
 +
https://www.dnr.wa.gov/programs-and-services/geology/glaciers#
 +
 +
https://asf.alaska.edu/information/glacier-power/
 +
 +
https://nsidc.org/learn/parts-cryosphere/glaciers
 +
 +
https://mynasadata.larc.nasa.gov/stem-career-connections/science-glaciologist
 +
 +
https://www.antarcticglaciers.org/
 +
 +
https://www.nps.gov/subjects/aknatureandscience/glaciers.htm
 +
 +
https://www.nps.gov/subjects/geology/glacial-landforms.htm
  
 +
http://www.geo.hunter.cuny.edu/~fbuon/GEOL_231/Lectures/Glacial%20Landforms.pdf
 
<!--T:98-->
 
<!--T:98-->
 
<noinclude></translate></noinclude>
 
<noinclude></translate></noinclude>
  
 
{{CloseHonorPage}}
 
{{CloseHonorPage}}

Latest revision as of 19:23, 25 May 2024

Other languages:
English • ‎español
Glaciers

Skill Level

2

Year

2024

Version

07.06.2024

Approval authority

North American Division

Glaciers AY Honor.png
Glaciers
Nature
Skill Level
123
Approval authority
North American Division
Year of Introduction
2024



1

What is a glacier? Why is the study of glaciers important and how are glaciers studied today?


A glacier is a large body of ice and snow that moves under its own weight. Glaciers may form in mountains (alpine glaciers) or across broad areas (continental glaciers) through repeated seasonal snowfall that does not melt. Overtime, the snow is compacted to firn and then to ice, squeezing out air bubbles and becoming a solid mass. The weight of a glacier pushes it across the ground or downslope. Alpine glaciers are often referred to as "rivers of ice," an apt description of these very slow-moving solid water bodies.

The study of glaciers, called glaciology, is an interesting science that brings together elements of geology, hydrology, chemistry, physics, climate and paleo-climate studies, among other fields. Studying glaciers provides insights into geological landforms and how they were made, allows study of changing climate over time both through the advance and retreat of glaciers and through studying the layers of compacted ice by drilling ice cores. Chemical analysis of these cores can show changes in relative atmospheric carbon dioxide, for example, or even capture records of past volcanic activity or plant spores. The rate of glacial retreat offers ways to consider and measure the changing climate. At times, glaciers may reveal ancient artifacts or even frozen mummies that offer anthropological and archeological details of past usage of places, lifestyles, and suggestions of climate.

Glaciologists may work in the field, mapping and measuring glaciers by using satellites and drones, tracking advance and retreat by placing lines of poles on active glaciers, or studying past climate and atmosphere through drilling ice cores. Continental glaciers in Antarctica and Greenland may be studies through permanent or seasonal scientific research stations, allowing continued access to the glaciers, where annual precipitation can be tracked, along with any changes in the glacier's movement.



2

Create a game (such as a matching game, board game, trivia, etc.) that explores and defines the following terms as they relate to glaciers:



2a

Crevasse


A Crevasse on a glacier
A crevasse is a crack in the surface of a moving glacier. Crevasses may be narrow or wide, shallow or deep.



2b

Firn


Firn is a term for snow that has been compressed enough to eliminate air pockets. If it is compressed further, it will become glacial ice.



2c

Glacial drift


Glacial Drift

Glacial drift is the term for sediment and debris moved or deposited by a glacier, whether directly through physical erosion and movement, or indirectly, as in debris moved further by water from a melting glacier.



2d

Glacial erratic


Glacial erratics in a stream

A glacial erratic is a rock or boulder transported by a glacier and left behind when the glacier retreats.



2e

Glacial lake


A glacial lake at the terminus of a former glacier
A glacial lake is a pool of standing water on, in, or under a glacier, or formed by a glacier, often near its terminus.



2f

Icefall


A glacial icefall - note the more jumbled appearance in the center where the slope is steeper

An icefall is the equivalent of a glacial "waterfall," and occurs where a glacier moves over a steep gradient, fracturing the surface of the glacier.



2g

Kettle lake


Several kettle lakes

A kettle lake forms when glacial ice in an outwash plain melts in a depression.



2h

Névé


Névé refers to the part of a glacier that is permanently covered with snow.



2i

Paternoster lake


Paternoster lakes (referencing a priest, and thus a string of rosary beads) are a series or string of lakes left in a valley by a retreating glacier.



2j

Plucking


In glacial terms, plucking is the process of a moving glacier dislodging or lifting a rock or boulder from the bedrock, thus "plucking" it up from the bedrock and carrying it to deposit later (see glacial erratic).



2k

Serac


A serac is a jagged pinnacle or tower of ice on a glacier.



2l

Subglacial stream


A subglacial stream flowing out from the end of a glacier

As the name implies, a subglacial stream is a stream that flows beneath a glacier.



2m

Tarn


A tarn is a lake formed in a cirque (a cirque is bowl-shaped depression at the head of an alpine glacier).



2n

Terminus


A glacial terminus ending on land
The terminus of a tidewater glacier ends in the water

The terminus (or tow) of a glacier is the furthest/lower margin of a glacier - ie the "end" of the glacier.




3

How are glaciers formed? Where can they be found? On a map, highlight the places glaciers can be found today.




4

Name the two major types of glaciers and two subtypes of each.


There are several ways to classify glaciers, but in general, they can be divided into Continental and Alpine Glaciers. Continental Glaciers are large glaciers that do not necessarily require mountains to form.

The main types of continental glaciers are Ice Sheets (covering more than 50,000 square kilometers, and currently including only the Greenland and Antarctic Ice Sheets) and Ice Caps, which are continental glaciers covering less than 50,000 square kilometers. A further extension of continental glaciers are Ice Shlfs - which are floating extensions of large glaciers into the water.

Apline Glaciers

Alpine glaciers form in mountains, are much smaller than continental glaciers, and may in fact be part of larger continental glaciers. Four main categories of alpine glaciers are Cirque Glaciers (which form in bowl-like depressions in the mountains, and may feed other glacier types), Valley Glaciers (glaciers flowing through valleys), Piedmont Glaciers (Glaciers that flow out of valleys and canyons onto flatter lowlands), and Ice Fields, which may be larger conglomerations of glacial ice forming in the mountains and feeding several valley or piedmont glaciers.




5

On a diagram of a glacier, label the following parts and how they work together to cause glacial movement:



5a

Accumulation zone


The area of a glacier where snowfall exceeds loss through melting or other processes



5b

Ablation zone


The area of a glacier where loss of ice and snow exceeds accumulation.



5c

Equilibrium line


The area on a glacier between the Accumulation and Ablation zone, where the forces are equal.




6

Explain how a glacier advances and retreats.




7

Know the difference between valleys formed by rivers and streams, and valleys formed by glaciers.


A U-shaped valley formed by an earlier glacier
A U-shaped glacial valley, still actively being carved by a seasonal glacier

In general, a valley formed by a river or stream is described as V shaped, whereas a glacial valley is U shaped.



8

Describe the two main ways in which glaciers can move.




9

Draw, photograph, model, or describe the following landforms created by glaciers:



9a

Arête


Arete - the sharp ridge between glacial cirques

An Arête is the sharp, jagged peak that separates two glaciers or cirques.



9b

Cirque


A cirque
A cirque being formed - note how the snowfield is beginning to carve the bowl-shaped deprression

A Cirque is a bowl-shaped depression in alpine areas formed by a glacier.



9c

Col


A Col is a low point or pass in an Arête or ridge that has been formed through erosion.



9d

Drumlin


A Drumlin is a tear or inverted half-canoe shaped ridge of debris shaped by a glacier. The pointed end points toward the glacier head, the flattened end is often steep.



9e

Esker


An Esker is a steep-sided meandering ridge formed by a subglacial or englacial stream and left behind by a retreating glacier.



9f

Fjord


A Fjord is a U-shaped valley formed by a glacier that extends into the water below sea-level.



9g

Glacial horn


A Glacial Horn forms when three or more Cirques intersect, shaping a pyramidal mountain peak (think of the Matterhorn).



9h

Kame


A Kame is a sand or gravel mound deposited by water flowing over a glacier.



9i

Nunatak


Nunatuks are visible on the left side of the image, poking through the glacial field

A Nunatak is a mountain peak that protrudes through a glacier, or through where two or more glaciers meet and converge.



9j

Outwash fan


An Outwash Fan is an alluvial plain of graded debris laid down by glacial melt (think of it as a land-bound alluvial fan).



9k

Roche moutonnée


Roche moutonnée is the term for an elongated, rounded knob of bedrock shaped by a moving glacier, gently slowing on the "upstream" side and steeper on the "downstream" side. (Compare to a drumlin, which is formed by glacial till, rather than carved out of the bedrock).



9l

Striation


A museum specimen of rock showing striations caused by a passing glacier.

Striations refer to the lines and grooved carved into bedrock by a passing glacier. As the glacier moves, it also drags along rocks and other debris, and this scours the underlying rock, leaving the scratch marks.



9m

Trim line


The trim line is visible along the hillside, where the sharper cut can be seen in contrast to the more rolling upper part of the hill

The Trim Line is the boundary on a glacial valley wall that shows the previous maximum width of the glacier.




10

What is a moraine? Name and describe three types of moraines.


Moraines are mounds of rock, sand, or other debris pushed up or deposited by a glacier. The main types of Moraines are: Terminal Moraine, which forms at the terminus or maximum extent of a glacier Lateral Moraine, which forms along the edge of a glacier from falling debris or eroded from the valley walls

The medial moraine shows where two upper glaciers came together to form a larger single lower glacier

Medial Moraine, which runs parallel to a glacier, but forms wheere two glaciers merge into a single flow

A recessional moraine, left behind by a retreating glacier

Recessional Moraine, which forms as smaller accumulations behind the terminal moraine, and marks shorter periods of eadvance and retreat



11

With your class, discuss safety while on or around glaciers.




12

Evidence of glaciers that have since disappeared can still be seen all over the world. From a Biblical viewpoint, discuss with your class how these might have been formed.




13

When something is caught in a glacier, it is often preserved like a time capsule for decades or even hundreds of years, giving us great opportunities to study the past. Creatively present one of these discoveries to your group.




14

Do two of the following:



14a

Visit a glacier or a place where glaciation has occurred and discuss with your group or write a 200-word report about what you saw. Include any landforms that you saw.




14b

Watch a video about glaciers and discuss with your group or write a 200-word report about what you saw.




14c

Draw or paint a picture about something you had fun learning about while studying glaciers.




14d

Talk with your group, write about, or make a short video about a real glacier study or conservation project.





References

https://www.dnr.wa.gov/programs-and-services/geology/glaciers#

https://asf.alaska.edu/information/glacier-power/

https://nsidc.org/learn/parts-cryosphere/glaciers

https://mynasadata.larc.nasa.gov/stem-career-connections/science-glaciologist

https://www.antarcticglaciers.org/

https://www.nps.gov/subjects/aknatureandscience/glaciers.htm

https://www.nps.gov/subjects/geology/glacial-landforms.htm

http://www.geo.hunter.cuny.edu/~fbuon/GEOL_231/Lectures/Glacial%20Landforms.pdf


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