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.
periglacial climate
a glacier has a snowline at the same height as the wastage 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.
periglacial climate
it is called the pelagic zone.
a glacier has a snowline at the same height as the wastage line.
The zone above the water table where water is suspended is called the unsaturated zone or vadose zone. This zone contains both air and water in the soil or rock pores.
The zone above the water table is called the unsaturated zone or vadose zone. This area contains both air and water, with the water content decreasing as you move up towards the surface.
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 hydrosphere
The narrow zone on the mid-ocean ridge crest where most geologic activity occurs is called the rift zone. It is characterized by high heat flow, volcanic eruptions, and tectonic spreading, creating new oceanic crust as magma rises to the surface and solidifies.
Yes, the zone of aeration is located above the zone of saturation. The zone of aeration contains spaces filled with both air and water, whereas the zone of saturation is where all available spaces are filled with water.