Why There Is Still Glister Up To Now?
The set of ice that solidified at the beginning of the ice age in North America called people with the term "Continental Glister". who has the thickest possible covering 15.000 feet when measured at its central point.
a very board set of glister is thought to have been formed and melts again at least four times during the last ice age.
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Please Read Ice Age And How End Of The Ice Age
ice ages or glacial period that took place in other parts of the world it still hasn't got a chance to experience the melting, for example, the largest island in the world, namely Greenland, still encased by glister continental, except for one narrow path round the edges.
on the island, in glister it often reaches an altitude of over 10,000 feet, thick covering between 10.000 to 12.000 feet in some place.
so what exactly are we still have glister in a few areas on Earth?, no other glister-glister because it still hasn't got a chance to thaw since the ice age.
although most of the glister contained in this newly formed now in recent centuries, the glister-glister is generally is the kind of glister that we find in the valleys.
How Glister Is Formed
glister-glister it began to form in the board valley, steep and high -walled like a form of ceremonial performances such as have many stairs, the snow down and exhaled by the wind and then go to into the valleys or gliding in the form of snow falls from the wall slopes located higher.
the snow that does not melt in the summer, but the snow was deeper the longer reams from year to year, naturally then there was heavy pressures above, plus it simultaneously with the onset of the process of melting and freezing again in some places.
this causes heavy pressure of air from the bottom being lifted out, so a layer of snow that changed shape into a solid ice layer and intact, further, the pressure caused by weighing the amount of ice and snow from the top of the stack, causing ice increasingly depressed, so start creeping slowly sliding down the driven valley.
the movement of the ice tongue running slowly is what is called the glister valley, there are more than 1.200 such glister valley in the Alps in Europe, there are also glister in the mountains of Pyrenea, the Carpathians, the Caucasus Mountains and in Europe.
there are also glister in the mountainous region of South Asia, in the area South of Alaska there are tens of thousand of glester of this kind, which among them have length up to 25-50 miles.
that's the article about Glister And Why There Are Still Glister To The Present.
Please Read Iceberg And How Iceberg Is Formed
