The zone of accumulation.
The zone above the snowline on a glacier is called the zone of accumulation. In this area, snowfall exceeds melting and sublimation, leading to the buildup of ice and snow. This zone is crucial for the glacier's mass balance, as it is where the glacier gains ice over time. Below the snowline, in contrast, is the zone of ablation, where ice and snow are lost.
The zone of accumulation.
a glacier has a snowline at the same height as the wastage line.
The equilibrium line of a glacier is the boundary where there is an equal balance between the amount of ice gained through snow accumulation and the amount lost through melting or iceberg calving. It divides the accumulation zone (above the equilibrium line) from the ablation zone (below the equilibrium line). Glaciers will advance or retreat depending on the position of their equilibrium line.
The line dividing the zone of accumulation from the zone of ablation on a valley glacier is called the equilibrium line. This line marks the point where accumulation (snowfall) equals ablation (melting and sublimation), influencing the glacier's overall mass balance and movement.
The zone above the snowline on a glacier is called the accumulation zone. This is where snowfall exceeds melting, leading to an increase in glacier mass.
The zone above the snowline on a glacier is called the zone of accumulation. In this area, snowfall exceeds melting and sublimation, leading to the buildup of ice and snow. This zone is crucial for the glacier's mass balance, as it is where the glacier gains ice over time. Below the snowline, in contrast, is the zone of ablation, where ice and snow are lost.
The zone of accumulation.
a glacier has a snowline at the same height as the wastage line.
Snowline
The equilibrium line of a glacier is the boundary where there is an equal balance between the amount of ice gained through snow accumulation and the amount lost through melting or iceberg calving. It divides the accumulation zone (above the equilibrium line) from the ablation zone (below the equilibrium line). Glaciers will advance or retreat depending on the position of their equilibrium line.
The "accumalation zone."
a snowline is where you put cocaine on your girls booty and snort it.
Glacier is in the mountain time zone, and most of Texas is in the central time zone. Therefore, Glacier is one hour "behind" Texas. If it's 6:00 in Texas, it's 5:00 in Glacier.
The middle layer of a glacier is called the "firn zone". This layer is composed of partially compacted snow that is in the process of being transformed into ice. The firn zone is found between the surface snow accumulation zone and the deeper layers of glacier ice.
The line dividing the zone of accumulation from the zone of ablation on a valley glacier is called the equilibrium line. This line marks the point where accumulation (snowfall) equals ablation (melting and sublimation), influencing the glacier's overall mass balance and movement.
Snowline, in the following website: <http://www.primarygames.com/holidays/christmas/games/snowline/index.htm>, is a good game even though it doesn't have any action or adventure; Snowline takes strategies and knowledge of gravity to win.