Glaciers and How They Form
What is a Glacier?
A glacier is a large body of ice, created by the accumulation of snow, that persists over several years, often lasting centuries. Glaciers occur in the earth's polar regions as well as mountainous areas.
There are a number of phases that these massive chunks of ice go through which include their initial formation, continual growth, and flow. This process is called glaciation.
Glaciers are an important indication of climate change, so scientists often monitor and study them in an effort to better understand the effect humans have on the earth's climate. While not much is known in regards to why glaciers are disappearing, scientists do know how they are created.
Where Can Glaciers Be Found?
Glaciers only form in areas of colder temperatures where snow is unable to completely melt. 1 Polar regions such as Antarctica or Greenland are known for having most of the world's glaciers. This is because these areas are so cold that any snow that accumulates doesn't melt away.
Glaciers can also be found in areas of high altitude, where the air is cold year-round. For example, a number of glaciers are located in the Himalayas, the Alps, and the Andes.
Since the creation of glaciers depends heavily on snowfall, they do not exist in cold deserts. While these areas often experience frigid weather, because it does not often snow, glaciers are unable to form.
How Glaciers Form
When snow does not melt, it accumulates. As more and more snow builds up, its weight is pressed down onto older layers. This compression causes the snow to crystallize and become more dense, essentially turning sheets of snow into compacted ice.2
Compressed snow is called firn. New firn, found on the upper layers of a glacier, is made up of granules of ice, each about the size of a grain of sugar. As firn is further compressed by new snowfall, the granules fuse together creating even larger crystals of ice. As it further compresses, it becomes considerably more dense than the newer firn. After enough compression, it turns into what is called glacial ice.
How much weight and pressure is needed to cause firn to become glacial ice? Firn usually turns into glacial ice when it's around 150 feet deep. This is when the weight of the upper layers of the glacier puts so much pressure on the older firm that it's crystallized into solid ice.
Did you know?
If Antarctica's ice sheet completely melted, the oceans would rise about 210 feet!
The Movement & Anatomy of Glaciers
In mountainous regions, gravity and deformations in the ice cause the top layers of glaciers to flow downward to the valley below. This very slow process causes stress on various parts of a glacier which often causes deformities like crevasses and seracs.
The area where the glacier originates is called the glacier head, or the accumulation zone. As the ice flows away from the accumulation zone, it is replaced by new firn, which will eventually become a part of the glacier as well.
As glaciers move, glaciers often carve their way through soil and rock, creating unique landforms. They also sometimes pick up and carry large rocks and boulders, which are left behind when the glacier eventually melts.3 Because of this, huge boulders left by glaciers that occurred thousands of years ago can be found all over the world!
Glaciers melt as they move to warmer areas, and provide the land with fresh water, an invaluable resource. As you may have guessed, glaciers are major storehouses of water. In fact, they store about 69% of the world's freshwater!4
The "glacier foot" is where the glacier ends. The glacier can end in a valley where the foot may melt (creating "meltwater") or end in a large body of water, where chunks of ice often break off and float away (icebergs.)
"Where Glaciers Are Found." NPS.gov. National Park Service.
"How Are Glaciers Formed?" NSIDC.org. National Snow & Ice Data Center.
"Glaciers." Niu.edu. Northern Illinois University.
"Glaciers and Icecaps: Storehouses of Freshwater." USGS.gov. US Geological Survey, 9 March, 2012.
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