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Virtual
Exploration #3
How do Glaciers Shape the Land?

This image was taken by Matthew
Durant
at Wrangell St. Elias National Park.
Home
What is a Glacier?
How do Glaciers Form?
How do Glaciers Move?
How do Glaciers Shape the Land?
Questions
How do Glaciers Shape the Land?
Text
Message
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---Classified---
Text Message #4:
Tasks
From: Crystal
Subject: Your
Tasks
Pack lightly!
The small plane that will fly us to Denali National
Park doesn't have much room. Denali is a magnificent
place to witness the awesome forces that
glaciers have on the land. We'll see massive
u-shaped glacial valleys, sort through piles of
glacial till, climb on glacial erratics, and wade in
freezing cold glacial streams. Hurry, our plane is
leaving soon.
We will:
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Embark on our Virtual
Exploration #3: How do Glaciers Shape the
Land?
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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 #3 
Virtual
Exploration
Virtual
Exploration #3
How do Glaciers Shape the Land?

Glaciers change the land by
eroding it in some places and depositing the rocks that are
plucked up elsewhere. We'll explore these things: how
glaciers carve out awesome u-shaped valleys; spit out
massive amounts of rock that pile up into glacial moraine;
we'll climb on massive boulders (glacier erratics) that were
dropped on the tundra plane; we'll soak our sore feet in
kettle lakes that were made by glacial erosion; we'll marvel
at rock striations; and we'll watch cloudy rivers rage on
and on. Let's go!!!
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U-shaped Valleys
We are only a few miles into Denali National
Park, at Riley Creek. Already, we see a wide, u-shaped valley!
About 70,000 years ago, a glacier passed through this river
valley (v-shaped) and scraped away (eroded) rock creating a
u-shaped valley with a broad floor and steep sides. Later,
this glacier receded, leaving only a broad, u-shaped valley.
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Glacial
Moraine Look at all
of those small
rocks all around and on that glacier. As the
glacier moved forward and then receded, it scraped up rocks from the
bedrock. These rocks got stuck in the ice and are moved
along with the glacier. Our fellow scientists call these
rocks till.
As the glacier moves and recedes it creates three basic types
of moraine. Check the
computer to learn more about three types
of moraine. |
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Glacial Erratics
You pass huge boulder after boulder on
your hike to the glacier. They seem oddly out of place, like
they were dropped down
from somewhere far away. In a way, they were. The
glacier in front of us once spread far out onto the
tundra. It bulldozed huge rocks in front of it as it
pushed forward. As it began receding back
into the mountains, it dropped the huge rocks. Today, we
see huge boulders far out on the flat tundra. These are
called glacial erratics.
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Kettle Lakes
Wow, check that out, it's
beautiful! You see the clear
reflection of Mt. Denali on the mirror-like surface of Wonder
Lake and you think how beautiful the reflection is. Your
friend interrupts your thoughts by saying,
"The reflection is beautiful but that kettle lake is
amazing!!!" You already
know that as a glacier moves ahead it scrapes up pieces of
the bedrock. This scraping forms depressions in the ground.
Many years later, as the ancient glacier receded, it dropped a
huge chunk of ice that melted and flowed into that depression. This
formed Wonder Lake (a Kettle Lake). |
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Glacial Striation When
you look closely at the till in the moraine, you see lots of
signs of glacial erosion. On the bottom of this rock
there are long scrape marks. Wow, that must have been a
lot of pressure to scrape those rocks like that. As
the glacier moves, the till trapped in the ice gets scraped
along the bedrock. Pieces of the bedrock get worn off
and the till gets scrape marks in it.
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Glacial Flour Look
closely at the Toklat River over there. It is flowing from the
glacier. See it's milky
gray color. That gray color is rock scrapings and small
pebbles that were rubbed off of the bedrock as the glacier
passed over. The glacier's melt water
comes roaring out. The
current is so strong and the water is only about 35 degrees Fahrenheit.
All of these rock particles in the water are
known as glacial flour. The
rocks, pebbles, and glacial flour that get caught up in the
Toklat River eventually slow and drop to the
riverbed. The great amount of dropped sediment create a gravel
bar that diverts the river into another braid. Soon,
more sediment is dropped that creates another, and another, and
yet another braid. Then, a wide glacier river flows
swiftly through many ever-changing braids as it flows to the
north. |
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
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Discussion: What do you
know about how glaciers shape the land?
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Make a new small model
glacier in a plastic cup.
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Add about 1/2 an
inch of rocks and sand at the bottom of the
cup.
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Cover the soil and rocks with snow from
outside or shaved ice that you create by placing broken ice
cubes (carefully hammer ice cubes in a towel) into a
food processor.
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To simulate the massive amount of pressure
that snow above has on the snow below, place a a small rock on top of the packed snow.
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To simulate the cold Alaskan winter, place
the shoebox with packed snow into a freezer
overnight.
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The next day, add more snow to your glacier
and pack down with more weight. Place it back into the
freezer and freeze overnight.
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Repeat step E for several days.
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Take your model glacier out of the freezer
and remove the rock. Slightly warm the sides
of your plastic cup by running it under warm water. Do this
just long enough to get the model glacier out of the
plastic cup when the sides are tapped.
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To simulate your glacier flowing over
bedrock, rub your glacier slowly over a brick, pressing
down fairly hard. What happens to the piece of
wood? Focus your observations on the shavings that
are scraped up. Take notes, make a sketch, and label what you observe in your science
journal.
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How does your model glacier simulate
what happens in the wild with Alaskan glaciers?
Assessment
Guide
Click here to see a rubric to
help you assess and revise your own work.
Revisit the
Question
How do Glaciers Shape the Land?
Home
What is a Glacier?
How do Glaciers Form?
How do Glaciers Move?
How do Glaciers Shape the Land?

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