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lrg2013-06-06 ߣ ԴڣZWվ

20120414ձԇC

Glacial Lakes

Throughout the earths history the climate has fluctuated and at times the temperatures have been cooler than they are now. This change in temperature can last somewhere between 2 to 10 million years and is referred to as an ice age. There have been at least five major ice ages in the past one billion years, the most recent of which, the Pleistocene Ice Age, began about 2 million years ago. Glaciers did not continually cover the earth during this time; there have been interglacial periods where temperatures warm slightly and the glaciers melt and retreat. Repeated advance and retreat of a glacier scours the bedrock, preparing the way for the formation of lakes. By the time glaciers completely melted around 10,000 years ago, numerous glacial lakes were formed when the water from melted glaciers fill the hole or space formerly created.

c~R

1.         Fluctuated: sth ~, it changes a lot in an irregular way, n. fluctuation

2.         Be referred to asQ

3.         Pleistocene Ice Age['plaistəusi:n] from two million to 11 thousand years ago; extensive glaciations of the northern hemisphere; the time of human evolution; ӕr

4.         Glacieran extremely large mass of ice which moves very slowly, often down a mountain valley,

5.         Interglacial periods|gӕr

6.         Retreatv. pull back or move away, or backward,

7.         Scorev. make small marks into the surface of, ӛ̖

8.         Bedrockthe solid rock in the ground which supports all the soil above it, r

 

}

temperature fluctuates; Pleistocene Ice Age; glaciers melt and retreat; glacial lacks were formed; 

 

It was at the end of this last Ice Age that a finger of the Cordilleran ice sheetƵw crept southward into the Idaho panhandle, forming a large ice dam that blocked the mouth of the Clark Fork River, creating a massive lake 2000 feet deep and containing more than 500 cubic miles of water. Glacial Lake Missoula stretched eastward for some 200 miles and contained more water than Lake Erie() and Lake Ontario(Ժ) combined.

c~R

1.         Creep: sth~ somewhere, it moves very slowly, uu

2.         Ice damˮČW

3.         Massivevery large in size, quantity or extent. ߴ//Ҏģdz

4.         Stretchsomething ~ over an area or distance covers or exists in the whole of that are or distance,

 

}

crept southward into; stretched eastward for ; form a large ice dam;

 

Periodically, the ice dam would fail and bring about catastrophic consequences. A large flood of ice-filled and dirt-filled water would burst through the dam, shooting out at a rate 10 times the combined flow of all the rivers of the world. This towering mass of water and ice literally shook the ground as it thundered toward the Pacific Ocean, stripping away hundreds of feet of soil and cutting deep canyons into the underlying bedrock. With flood speeds approaching 65 miles per hour, the lake would have drained in as little as 48 hours.

c~R

1.         Fail: become gradually weaker or less effective, ˥

2.         Catastrophicsth causes a sudden terrible disaster,

3.         A large flood ofa large number of sth, һ

4.         Toweringsth is very tall and therefore impressive, –ģČWԣ

5.         Literallyto emphasize that what you are saying is true, even though it seems exaggerated or surprising, _

6.         Stripv. to remove everything that covers it, x

7.         Canyona long, narrow valley with very steep sides, {

 

}

Periodically, the ice dam would fail and bring about catastrophic consequences.

 

Over time the Cordilleran ice sheet continued moving south and blocked the Clark Fork River again and again, recreating Glacial Lake MissoulaK. Over approximately 2,500 years, the lake, ice dam and flooding sequence was repeated dozens of times, leaving a lasting mark on the landscape. Grand Coulee, Dry Fallsٲ, Palouse Fallsɪٲ were all created by these flood waters, as were the Missoula and Spokane ground-water resources, numerous wetlands and the fertile Willamette Valley÷عȣՌݣ and Quincy Basin.أ

c~R

1.         Lasting: to describe a situation, result or agreement that continues to exist or have an effect for a very long date ־õ

2.         Wetland:

3.         Dry FallsλAʢDňDСr܇ǬFٲzַ

 

}

Recreate; leave a lasting mark on the landscape; all created by flood waters

 

Among the most varied features left by glaciers are ice-contact deposits due to continental glaciations(). These landforms develop along the margin or outwash of the glacier, leaving behind ice deposits. Glacial outwash is generated when streams of melt water flow away from the glacier and deposit sediment to form broad outwash plains called sandurs.ˮeƽԭ

c~R

1.         Deposits: an amount of a substance that has been left somewhere as a result of a chemical or geological process, eVdeposit sediment

2.         Landformany natural feature of the Earths surface, such as a hill, a lake or a beach, ò

3.         Marginthe ~ of a place or area is the extreme edge of it, ߅

4.         Outwasha mass of gravel, sand, etc, carried and deposited by the water derived from melting glaciers, |ˮeڣ_g

 

}

     Ice-contact deposits due to continental glaciations; to form broad outwash plains;

 

The floods caused by receding glaciers or the sudden drainage of an ice-dammed lake often rapidly deposit large quantities of sediment onto the sandur surface. During this process, kettle holes are often formed by the melting of a detached mass of glacial ice that has broken off a glacier and became wholly or partly buried, leaving a depression in a glacial outwash drift. In most cases, kettle holes eventually will fill with water from surface or underground rivers or streams and becomes kettle lakes.

c~R

1.         Recede: sth becomes weaker, smaller or less intense, p

2.         Drainagethe system or process by which water or other liquids are drained from a place, ˮˮϵy

3.         Kettle holes|WѨ

4.         Detachedno longer connected or joined,

5.         Depressionan area which is lower than the parts surrounding, ݵ

6.         Outwash drift|WˮƯe

7.         Kettle lake

 

}

Kettle holes/lakes formed due to sediment onto the sandur surface

Generally speaking, kettle lakes are the result of continental glaciations and are found in northern areas of North America and Europe. In contrast to this kind of lake, alpine(ɽģ˹ɽ) glacial lakes, including paternoster lakes and tarns, are formed by alpine glaciations and are mostly found in mountainous areas. Paternoster lakes are a chain of lakes that may develop in a valley with glacial steps, often each step having a lake. They are so named because of their resemblance with the beads on a rosary. Examples of paternoster lakes occur in the Sierra Nevada Mountains(A_ɽ})  in California and Glacier National Parkұ@ in Montana. A tarn is a lake that forms when water along with additional snowmelt seep down into the depression of a cirque, the bowl or amphitheater-shaped valley head characteristic of all alpine glacial landforms. The head and sidewalls of a cirque may be nearly vertical, while the floor is often carved into a shallow basin. Excellent examples of tarns lakes are found in North Cascades and Rocky Mountain National Parks.

c~R

Paternoster lakes: ˮČW,

Tarns: ˮġ ɽС

Resemblancesimilarity in appearance or external or superficial details, ֮̎

Beada small drop of liquid, ˮ

Seeppass gradually or leak through or as if through small openings,

Cirque a steep-walled semicircular basin in a mountain, may contain a lake, /ع

Amphitheater-shaped

 

}

Alpine glacial lakes: paternoster lakes and tarns;

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