no
weather and climate changes cause difference in size of crystals. or erosion
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 glacier has a snowline at the same height as the wastage line.
composition, size, weight
Depending on when it was formed, the size and speed it is moving it could be either an Avalanche or Glacier. If it is an incredibly old, slow moving, large, ice mass it is likely a Glacier; however if it is a quickly moving, small (relatively), ice mass it is an Avalanche.
no
Temperature influences glacier size.
weather and climate changes cause difference in size of crystals. or erosion
A glacier can not do any damage to earth and it depends on the size of the glacier if it is huge it may flood
Temperature influences glacier size.
weather and climate changes cause difference in size of crystals. or erosion
Glaciers develop and grow through a complex process that involves the accumulation and compaction of snow over long periods of time. Here is an overview of the process of glacier development and growth: Snow Accumulation: Glacier formation begins with the accumulation of snow in an area that experiences more snowfall during the winter than it loses through melting in the summer. This accumulation of snow is crucial to the glacier's growth. Over time, more and more snow accumulates, creating a layer of firn, which is granular snow that has partially compacted but is not yet fully transformed into glacial ice. Compression and Compaction: As new layers of snow accumulate on top of each other, the weight of the overlying snow causes the lower layers to become more compacted. This compaction forces out air and eventually transforms the firn into dense, granular ice. This process can take several years or even centuries, depending on the climate and the rate of snow accumulation. Glacier Formation: With continued snow accumulation and compaction, the granular ice eventually transitions into glacial ice, which is much denser and flows like a slow-moving river of ice under the influence of gravity. This is the point at which a glacier is considered to have formed. Flow and Glacier Movement: Glaciers are not stationary; they flow and move downslope due to their own weight and the force of gravity. The movement of glaciers is very slow, often just a few centimeters to meters per day, depending on the glacier's size and the terrain it flows over. This movement is what distinguishes a glacier from a static ice field or ice cap. Zone of Accumulation and Zone of Ablation: Glaciers have two distinct regions: the "zone of accumulation" and the "zone of ablation." The zone of accumulation is the upper part of the glacier where snow accumulation exceeds melting and sublimation. The zone of ablation is the lower part of the glacier where the ice melts or sublimates more than it accumulates. These two zones are in dynamic balance, and the boundary between them may shift over time in response to changes in climate. Glacier Growth: For a glacier to grow, the zone of accumulation must receive more snow and ice than the zone of ablation loses through melting and sublimation. Over time, this net gain in ice causes the glacier to advance and grow in size. Response to Climate: Glaciers are highly sensitive to changes in temperature and precipitation. Warmer temperatures or reduced snowfall can cause a glacier to retreat as the zone of ablation expands and overtakes the zone of accumulation. Conversely, colder temperatures and increased snowfall can lead to glacier advance. The process of glacier development and growth is a continuous cycle, with the glacier advancing and retreating in response to changes in climate and the balance between snow accumulation and ice loss. Glaciers are valuable indicators of climate change, and their behavior is closely monitored by scientists to understand the Earth's changing climate.
Glacier size is dependent on snowfall and temperature.
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.
The Lambert Glacier in Antarctica is the largest glacier on earth. Its roughly 40 000 sq km (25 000 sq mi) in size.
the sise is about 1/2 cm
climate size be predicted by area's