The Matanuska Glacier is a valley glacier and is 24 miles long and four miles wide. This article is about the geographical formation. ...
Matanuska is located in Alaska, United States and is the largest glacier accessible by car in the state. The glacier is a two hour drive northeast of Anchorage. The Matanuska Glacier is "active" and expands around 1 foot per day. It is open to the public from March to October 31. State nickname: The Last Frontier, The Land of the Midnight Sun Other U.S. States Capital Juneau Largest city Anchorage Governor Frank Murkowski (R) Official languages English Area 1,717,854 km² (1st) - Land 1,481,347 km² - Water 236,507 km² (13. ... Note: an anchorage is a place where a ship lays anchor. ... March is the third month of the year in the Gregorian Calendar and one of seven Gregorian months with the length of 31 days. ... October 31 is the 304th day of the year (305th in leap years) in the Gregorian Calendar, with 61 days remaining, as the final day of October. ...
An unusual feature of the Matanuska Glacier is the presence of a weather hole, making the weather unusually clear and sunny.
The MatanuskaGlacier is a large ice flow, 24 miles long and 4 miles wide at the terminus, averaging approximately 2 miles in width.
This glacier is a valley glacier; it exists on a valley floor.
The density of glacier ice allows the entire spectrum of light to be absorbed with the exception of the blue light which is reflected, and can therefore be seen by your eye.
Evenson's analysis of the "basal-stratified ice" beneath the MatanuskaGlacier also found traces of tritium, an isotope of hydrogen that has been released into the atmosphere during the past 50 years by nuclear weapons testing.
Glaciers located in flat areas, like the Matanuska, says Evenson, are more likely than most mountain glaciers, including those in the Alps or the Cascades, to permit the supercooling necessary for basal-stratified ice to form.
After studying the MatanuskaGlacier, Evenson and his colleagues tried to determine if basal-stratified ice was forming in a similar manner at other warm glaciers.
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