first before depostion happens erosion happenes that pushes the rocks down instead of up so when tht happens the depostion makes it where when the rocks are puuled downthey are also moved or possibly melt from climate change.
The debris of boulders and coarse material carried by glaciers is known as moraine. Moraines can be found at the edge, sides, and base of glaciers and are deposited as the glacier moves and melts. They can vary in size and shape depending on the glacier's movement and the type of material being transported.
The materials deposited by water, wind, and melting glaciers are collectively referred to as "sediments." These sediments can take various forms, such as sand, silt, clay, and gravel, and are often classified based on their size and origin. When these sediments accumulate over time, they can form sedimentary rocks or contribute to soil development.
Some of it is carried up the shore and deposited higher up the beach. Some is deposited on the seabed.
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 rock material deposited by glaciers is called "glacial till." This sediment consists of a mixture of clay, silt, sand, gravel, and boulders that glaciers grind and transport as they move. When glaciers melt, they leave behind this unsorted debris, which can form various landforms such as moraines and drumlins.
Glacial Drift
Glacial drift
Glacial plains are formed by the deposition of sediments carried by glaciers as they advance and retreat. When glaciers move, they pick up rocks, soil, and other materials, which are then deposited when the glacier melts. Over time, these deposited materials accumulate to create flat, wide expanses of land known as glacial plains.
bearem
an accumulation of boulders, stones, or other debris carried and deposited by a glacier.
The debris of boulders and coarse material carried by glaciers is known as moraine. Moraines can be found at the edge, sides, and base of glaciers and are deposited as the glacier moves and melts. They can vary in size and shape depending on the glacier's movement and the type of material being transported.
The term for soil that settles in water is sediment. Sediment is the material that is carried and deposited by water, wind, or glaciers.
The materials deposited by water, wind, and melting glaciers are collectively referred to as "sediments." These sediments can take various forms, such as sand, silt, clay, and gravel, and are often classified based on their size and origin. When these sediments accumulate over time, they can form sedimentary rocks or contribute to soil development.
Moraine.
A moraine is a pile of rocks and dirt deposited in a heap, usually at the end of a glacier. An erratic is a large stone or boulder that has been deposited in a similar way when glaciers retreated, being of a totally different type of rock to that on which it was deposited.
A moraine is the accumulation of solid material - rock, gravels, sand and clay, carried by a glacier, and deposited when the glacier shrank. The material is mainly from avalanches off surrounding mountains, which include rocky material as well as ice and snow.
Some of it is carried up the shore and deposited higher up the beach. Some is deposited on the seabed.