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Virtual
Exploration #2
How do Glaciers
Move?

This image was taken by Matthew Durant
at the Northwestern Glacier.
Home
What is a Glacier?
How do Glaciers Form?
How do Glaciers Move?
How do Glaciers Shape the Land?
Questions
How do Glaciers
Move?
Text
Message
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---Classified---
Text Message #3:
Tasks
From: Crystal
Subject: Your
Tasks
Pack your snowshoes and crampons. We're off
on a Virtual Exploration to the Harding Ice Field in the Kenai
Fjords National Park (South Central Alaska). We'll be in
the heart of glacier country and we will have many great opportunities to explore how
glaciers move. Hurry, we have to get
back to Alaska.
We will:
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Embark on our Virtual
Exploration #2: How do Glaciers
Move?
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Use the Online resources
to learn more about how glaciers are formed.
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Get Hands-On:
Conduct a scientific experiment where you will apply the
knowledge of glaciers that you have gained.
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Use the "Spy Kids"
assessment guide, to see how you are doing.
Good Luck!!!
Crystal
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I want to embark on Virtual Exploration #2 
Virtual
Exploration
Virtual Exploration #2
How do Glaciers Move?

This image was taken by Matthew Durant
at the Northwestern Glacier.
Many people refer to glaciers as "Rivers of Ice". It's not a bad metaphor because glaciers actually do
slowly move. In South Central Alaska, the snow piles up
fast. Most years, this part of Alaska gets over 700 inches. All the snow begins to add
pressure to the snow
below and it slowly transforms it into firn and then glacial
ice. Finally, the pressure builds so high that it squeezes
glacier ice over the sides and the glacier moves slowly
downhill.
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Harding Ice Field
Way up here on the Harding Ice Field, the
snow accumulates and metamorphoses into moving glacial ice.
Here on the Harding Ice Field, we are about one mile high on top
of the Chugach Mountains. We
cannot even see the other side of the Ice Field because it
covers nearly 700 square miles. The ice here is
amazingly thick. Scientists think that the ice is
thousands of feet deep. As you look around, it dawns on you
that you can see forever over these flat ice fields.
There are only a few hills which your computer tells you are
actually the tops of several mountains that are sticking up above the glacial ice. The Alaskan Natives
called these granite mountain tops, Nunataks, which means
"lonely peaks".
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Glaciers Begin To Move
Near the edge of the ice field you can see
where the pressure has pushed the glacial ice over the edge.
You are seeing the beginning point of the Northwestern Glacier
as it starts flowing down
towards the Pacific Ocean. Your computer tells you that
the Northwestern Glacier is one of thirteen named
glaciers and a host of other unnamed glaciers that flow from
the Harding Ice Field.
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Glaciers that
Move Listen to that Glacier!!!
Do you hear those creaks, groans, scrapings, and booms?
That's what a glacier sounds like when it moves. I know
you can't see it moving because it is moving so slowly but it
is. A glacier moves
forward (advances) when there is a lot of snow falling up in
the ice field. That new snow adds pressure to the
snow, firn and glacier ice below. The pressure builds
and builds until it squeezes the glacier ice over the side of
the ice field and it starts flowing downhill. In the
Winter when it is really cold and the glacier gets a lot of
snow, it will advance. |
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Regelation
When glaciers are moving slowly downhill,
they may be forced to move one way or another to go around a
valley wall. Other times a glacier will move around smaller objects
that are in
the way. When a glacier flows into an object in
its way, the uphill side of the glacier continues to press downward,
making it come under extreme pressure. That causes a thin layer
of the glacier ice to melt. A super thin layer of water
flows around the small object and freezes on the downhill side. By
transferring ice in this manner, glaciers can move slowly
around small objects.
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"Warm Glaciers"
Look over there. See that river
flowing from below the glacier. That river is made up of
melt water, water from the glacier melting. Sometimes,
glaciers move when a thin layer of this melt water gets
trapped between the glacier and the bedrock. This
trapped melt water provides
lubrication for the massive glacier above to flow over the
bedrock below. As the glacier moves, it generates lots of
friction, which creates more heat, leading to more water
below, which make the glacier move more.
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Crevasses
As the glacier flows over a steep drop, the
strength of the ice is stretched to its maximum limit and it breaks
apart. This results in crevasses. You would not
want to hike across that crevasse area. Some of those crevasses
are hundreds of feet deep.
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Calving When it is warmer and
sunny, the glacier melts enough so that it recedes or
shrinks. Our fellow scientists call this ablation.
Remember, at the Northwestern
Glacier when that huge chunk of ice calved into the
ocean? That was
one sign of
ablation. Remember, the river
flowing from Exit Glacier on that warm sunny day last July? That was another sign of
ablation. Over the
course of the year the glacier will move forward and
ablate. |
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Measuring Glacial Movement
Your fellow scientists have been using a Doppler Laser to measure the amount of glacial movement at
Exit Glacier and other Alaskan glaciers. In less
than a minute, they can determine minute distance changes as
little as .000001 inches per second. When researchers
have compared their Doppler Laser findings of Exit Glacier to
measurements taken in the 1950's, they found that the glacier
has thinned and retreated by about 150 feet.
Many other glaciers are showing ablation as
well. Glaciers have been shrinking all over the state.
But, why? Global Warming? |
Online
Resources
Further
Reading
Alaska's Glaciers. Alaska Geographic volume 9, number
1, 1982.
An observer's guide to the glaciers of Prince William Sound,
Alaska. Valdez, AK: Prince William Sound Books,
1987.
Glacier. R. H. Bailey and the Editors of Time-Life Books
Alexandria, VA: Time-Life Books, 1982.
Glaciers John Gordon. Stillwater, MN Voyageur
Press, 2001.
Glaciers, Natures Frozen Rivers. H. H. Nixon and J. L. Nixon.
New York: Dodd, Mead, 1980.
Glaciers of North America: A Field Guide. S. A. Ferguson.
Golden, CO: Fulcrum Press, 1992.
Blue Ice in Motion: The Story of
Alaska's Glaciers S. Wiley. Alaska Natural History Assn. 1995.
Hands-On
Activity
Regelation of Glaciers
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Discussion: What do you know about
how glaciers move?
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Place your model glacier from your
last activity onto a cookie cooling rack. Place the board and
rocks back on top of the glacier to simulate the pressure that
glaciers get from the massive amounts of snow above. Place the
whole thing back into the freezer.
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Hypothesis: What do you think
is going to happen to your model glacier?
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Observe your glacier once each week for
one month. Take notes and make a sketch in your science journal of
any changes that take place.
Make a PowerPoint Presentation to show evidence
that glaciers move.
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Discussion: What do you know about
how glaciers move?
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Create a PowerPoint Presentation to
teach others about how glaciers move.
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Gather images that show evidence
of glacier moving, using this website and other web sites (see online
resources).
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Use Google Image Search to look
for evidence of glacier movement on these major Alaskan
glaciers:
(Exit Glacier, Hubbard Glacier, Berring Glacier, Northwestern
Glacier, Portage Glacier, Columbia Glacier, Worthington Glacier,
Kennicott Glacier, Meares glacier, Talkeetna Glacier, Matanuska
Glacier, Mandhall Glacier)
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Remember to ask for and receive
permission before you use images you get from the
Internet.
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Place your images into a
PowerPoint Presentation. PowerPoint is a great tool to
show people what you are talking about. Use lots of images
with a few key words.
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Share your PowerPoint
Presentation with your friends.
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E-mail your PowerPoint
Presentation to (powerpoint@iwebquest.com)
and we'll put it up on the Internet to share with the other scientists
on our team.
Assessment
Guide
Click here to see a rubric to
help you assess and revise your own work.
Revisit the
Question
How do Glaciers
Move?
Home
What is a Glacier?
How do Glaciers Form?
How do Glaciers Move?
How do Glaciers Shape the Land?

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