Glaciers - Reading Comprehension Test

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Name: __________________________________________________ Date: _______________ Period: _________
GLACIERS
What is a glacier?
Snow falls and accumulates on the ground everywhere in New York State. In the highest parts of the
Adirondack Mountains, winter snow often lasts into early summer before it is completely melted. If the mountains
were 1000 or 2000 meters higher, the reduced warmth of summer would not be able to melt winter snow. Each year
more snow would accumulate and exert pressure on the underlying snow. This pressure would change the snow to ice
and gravity would make the ice begin to flow downhill. This is how glaciers form. The reason that no glaciers exist
today in New York State is that there are no places where the snow does not completely melt before the following
winter.
Snow and ice exist as crystals. When snow falls,the flakes are usually light and feathery. After the flakes reach
the ground and are buried under fresh snow,the delicate crystals gradually change to solid ice over a period of time
that depends on such factors as speed of burial and temperature. Is ice a solid or a liquid? Ice is composed of water in
the crystalline solid form. It fits the definition of a solid. Under short-term stress, ice behaves as a solid. An ice cube
in an environment below freezing has a fixed shape. Hit it with a hammer and it breaks into smaller pieces. Yet, ice in
a glacier flows. Glaciers do not flow because the ice is melting. They flow because solid ice responds to long-term
stress by bending and deforming.
1. Briefly describe how glaciers form.
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2. Why are there currently no glaciers in New York State?
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3. What causes ice, a solid material, to be able to flow downhill like a liquid?
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Types of Glaciers
Types of Glaciers
C ont i nent al Gl ac i ers
Val l ey Gl ac i ers
A continental glacier flows outward from a zone of
Once permanent ice has formed atop mountains, it
accumulation to cover a large part of a continent. If the
begins to flow downhill under the influence of gravity.
process could be speeded up, it might resemble what
Valley glaciers, which begin high in mountain areas,
pancake batter looks like as it is poured onto a griddle.
flow from the high ice fields through valleys to lower
Ice sheets that are several kilometers thick now cover
elevations. Most valley glaciers descend to an elevation
most of Greenland and Antarctica. Scientists have
where it is warm enough to melt the ice as quickly as it
studied both regions to gain an understanding of ice
advances. If the ice in the glacier is moving forward at a
caps and how they flow outward and down to the
rate of 1 meter/day, but the ice is also melting back 1
oceans. Ice flowing into an ocean breaks away from the
meter/day, the front of the glacier will not appear to
main body of the glacier to float away as icebergs.
move. This is known as a dynamic equilibrium because
Because ice is less dense than water, icebergs do not
the rate of flow and the rate of melting are in balance.
sink. Icebergs from Greenland and Antarctica are large
Even though the end of the glacier may be in the same
enough to pose a threat to the shipping industry. A
place from year to year, the ice is, in fact, constantly
number of vessels, for example the Titanic, have sunk
moving downhill. Ice in a small glacier may advance
due to damage from collisions with icebergs.
only a few millimeters a day while larger ones may
Fortunately, icebergs break up and melt before they
advance a few centimeters a day. As gradient and
can invade most ocean areas.
volume affect the speed of water in rivers, they also
influence the speed of ice flow in glaciers. Also, like the
water in most rivers, ice moves fastest near the center
and near the surface of a glacier.
4. What is the main difference between a continental glacier and a valley glacier?
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The diagram on the left shows the extent to which the last continental ice sheet extended during the last ice age,
approximately 20,000 years ago.

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