A glacier that forms in an area where more snow falls than melts is known as an accumulation glacier. This type of glacier grows as snow accumulates over time, compacting into ice due to the pressure from the layers above. Accumulation glaciers are typically found in regions with consistent, heavy snowfall, such as polar regions or high mountain ranges. They play a crucial role in the Earth's hydrological cycle and can influence sea levels when they melt.
A glacier forms under certain terrain conditions and where more snow falls in the winter than melts in the summer.
A glacier forms in a place where snow builds up for years. The main thing is that it has to be in a place where the snow does not melt in the summer. After so long, the weight of the snow compresses and becomes as, and as long as more snow falls on top of that glacier, that is what happens..... ^.^ I hope this answer helped!
The most important condition for the growth of glaciers is a balance between snow accumulation and snowmelt. When more snow falls in a glacier area than melts during the summer, the glacier can grow and advance. Temperature and precipitation patterns also play a significant role in glacier growth.
A confined glacier is a glacier that is confined by topography. For example, a glacier that forms on a mountain. Continental glaciers, by contrast, are not affected. The glaciers on Antarctica and Greenland are continental glaciers. The glaciers at Glacier Bay National Park, or on a mountain are confined glaciers.
A glacier is formed through the accumulation of snow that compresses into ice over time. As more snow falls and compacts, it displaces air and forms glacial ice. This process is aided by the weight of the overlying snow, which causes the lower layers to compress and recrystallize into ice.
The Continentail glacier are the largest glacial bodies which are several kilometers deep and cover a large area of more than thousands of kilometers. There are only two continental glaciers the one which covers most of the area of Antarctica and Greenland.
Glaciers form where more snow falls than melts. So, it really depends where the glacier is. If the area snows like crazy a lot, the size of the glacier would be big. If it doesn't snow that much there, the glacier would probably melt much faster, and be less big.
A melting glacier gets smaller, but a growing glacier gets bigger.
In New Zealand there are Franz Josef glacier and Fox glacier In the French Alps there is the Mer de Glace The largest glaciers in the world are the ice sheets on Greenland, the second largest glacier in the world, and the ice sheet on Antarctica is the largest in the world. glaciers are riveres of ice that moves very slowly.
A retreating glacier is one that is diminishing more in length that its upper supply regions can compete with. The snout of the glacier is retreating, but the main body of the glacier is still moving forwards. If this situation continues, the glacier will disappear.
The zone of wastage refers to the area of a glacier where more ice is melting or sublimating than is being replenished by snow accumulation. It is typically at the lower end of a glacier where temperatures are warmer, causing increased melting.
A glacier is older than an iceberg, because an iceberg is a piece of ice that fell off a glacier.