Columbia Icefield
The Columbia Icefield is a huge glacier covering up to 325 square kilometers.� The glacier became this big since it is located very close to some of the tallest peaks in the Rocky  Mountains.� In the last 125 years the glacier has retreated almost 2 kilometers (approximately 16 meters a year).� This fast retreat has been rapidity increasing up in recent years due to global warming.
North American Glaciers
Columbia Icefield
Alaska Glacier
Glacier National Park
References
When examining the effects of the glacier melting this quickly, the results are alarming.� The glacier retreating so fast is adding a lot of fresh water into the local streams, rivers and lakes.� Most of this fresh water will end up in the ocean, contributing to the ocean water-level rising.�
If you are examining the effects this glacier melting has on local residents it means the rivers and streams are flowing much faster.� There is a positive for the residence that live near the glacier since the glacier is a massive source of fresh water.� The water which is locked in the glacier is water in its most purist form.� This is because the water has been frozen for thousands of years, long before there was pollution or acid rain.�
The results of this glacier are not all positive though.� Residences now must deal with flooding of river beds in the summer, since the rivers and streams cannot hold the amount of water which is melting.� Animals in the local area now have to deal with faster currents.� In the spring with the baby animals this is a problem; since the water is faster moving the animal could fall in and not be able to get out.� Another major problem is fish cannot jump up the stream as easily do to the current being so fast.� This will mean less fish will be able to reach spawning locations, which results in less fish.
For local animals, such as bears, they are now forced to find other sources of food.� Due to bears being hungry they could start coming closer to human camps to eat human foods.� Though bear attacks are very unlikely in Alberta, they are starting to occur more often.�
Top: west side of the Columbia Glacier. Bottom: A picture showing the whole glacier.
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