I think the depth of a glacier depends on it height
bottom is the heaviest
Yes, the deeper you are (be it in air, water or any medium) increases as you go deeper, as there is a column of mass pressing down on you, toward the centre of gravity for the earth. The pressure at sea level (average) is 1 bar, which is 100,000 kilopascals! (so, and inflated tire will have a pressure relative to that of 60 or so pascals. Tiny, eh?)
The pressure at the top of the container will also increase if the pressure at the bottom is increased. This is because pressure in a fluid increases with depth due to the weight of the fluid above creating a greater force pushing down.
Moraines carried at the bottom of glaciers are called basal or ground moraines. They consist of rocks, soil, and other debris that have been plucked and eroded by the moving glacier. Basal moraines are typically deposited at the glacier's terminus or along its path as the glacier retreats.
The process in which rock fragments freeze to the bottom of a glacier and are then carried away when the glacier moves is called plucking. After the last ice age, stranded ice blocks left behind by the continental glacier melted and formed kettles.
Yes, it does. The more you advance towards the bottom of the ocean, the more the water pressure increases. Which is why you implode before reaching the bottom.
increases due to the increased weight of the liquid. This is because the liquid's weight creates a force that is spread out over the bottom of the beaker, leading to an increase in pressure.
Basal slip occurs when the glacier rests on a slope. Pressure causes a small amount of ice at the bottom of the glacier to melt, creating a thin layer of water. This reduces friction enough that the glacier can slide down the slope. Loose soil underneath a glacier can also cause basal slip.
The pressure at the bottom of a pond depends on the depth of the water above it and the density of the water. The pressure increases with depth because of the weight of the water column exerting force downward.
bottom is the heaviest
Yes, the deeper you are (be it in air, water or any medium) increases as you go deeper, as there is a column of mass pressing down on you, toward the centre of gravity for the earth. The pressure at sea level (average) is 1 bar, which is 100,000 kilopascals! (so, and inflated tire will have a pressure relative to that of 60 or so pascals. Tiny, eh?)
The pressure at the top of the container will also increase if the pressure at the bottom is increased. This is because pressure in a fluid increases with depth due to the weight of the fluid above creating a greater force pushing down.
The pressure at the bottom of the pitcher of water 35cm deep is higher than at the bottom of the bathtub of water 30cm deep. Pressure in a fluid increases with depth, so the deeper the water column, the greater the pressure at the bottom. This is due to the weight of the water above exerting a force on the bottom.
Glaciers can slide down slope for several reasons. First, a glacier is made of ice, which is frozen water. Liquid water is slippery. That is important to remember. Second, gravity is pulling on them making them want to move downhill. Third, when ice is put under a lot of pressure, it can melt. The pressure above the bottom of the glacier can cause some melting on the bottom layer. That can make the glacier slide. Fourth, the sun shining on the top of the glacier can make the top of the glacier melt. The water from that melting can go to the bottom of the glacier and help lubricate the bottom. That can help it slide. Mountain glaciers are always sliding downhill. Snow replenishes glaciers and adds ice to the top. If glaciers melt faster than they are replenished they vanish. Some mountain glaciers have vanished within the last 100 years. A few more are likely to vanish in the next decade.
Ground Moraines are abrasive elements that are carried in the bottom of a frozen glacier. Lateral Moraines are unsorted material deposited along the side of a valley glacier.
Moraines carried at the bottom of glaciers are called basal or ground moraines. They consist of rocks, soil, and other debris that have been plucked and eroded by the moving glacier. Basal moraines are typically deposited at the glacier's terminus or along its path as the glacier retreats.
Glacier ice moves more quickly in the center of the glacier where there is less friction with the valley walls. It moves more slowly along the sides and bottom of the glacier where there is more friction with the rock and sediment beneath it.