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Drumlins and eskers are found in glacial areas. Drumlins are hills made of glacial sediment and till, while eskers are long ridges of glacial drift.
A ridge or mound of debris chiefly composed of boulders, gravel, sand, and clay is called a moraine. Moraines are deposited by glaciers and can be found in various formations, such as lateral moraines along the sides of glaciers or terminal moraines at the end of a glacier's advance. Moraines are important features in understanding past glacial activity.
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 closer the sediment is to the mid-ocean ridge, the younger it is. The oldest bedrock is found the farthest away from it.
Smaller sediment, such as silt and clay. It is smaller, so it can be carried higher into stronger winds, which blow the small sediment far from its source.
Unsorted and not layered
Drumlins and eskers are found in glacial areas. Drumlins are hills made of glacial sediment and till, while eskers are long ridges of glacial drift.
A ridge or mound of debris chiefly composed of boulders, gravel, sand, and clay is called a moraine. Moraines are deposited by glaciers and can be found in various formations, such as lateral moraines along the sides of glaciers or terminal moraines at the end of a glacier's advance. Moraines are important features in understanding past glacial activity.
Glaciers carved large U-shaped valleys in higher mountains of the Sierra Nevada, Cascades, Klamath Mountains, and northern Coast Range. The outwash and moraines from melting and receding glaciers are found in nearby valley bottoms. The signs of former glaciers are found in erratic boulders, glacial polish, and high lake basins. Glacial erosion has been significant in the mountain areas.
Marl as lacustrine sediment is common in post-glacial lake bed sediments, often found underlying peat bogs. It has been used as a soil conditioner and acid soil neutralizing agent.
Fossils and sediment
The glacial formation of the collection of loosely arranged glacial debris which may include rock and soil that occurs in recently glaciated and previously glaciated parts on Earth is called moraine. It may contain debris ranging in size from sand-sized glacial flour to huge boulders.
It is found in faeces
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.
A moraine is a unsorted deposit of material left behind at the head (the front of a Glacier
wind carrying small sediment particles as in a desert sandstormstreams and rivers carrying sediment loads as seen in the muddy Mississippi Riverglaciers plucking and carrying rocks as evidenced by glacial erratics and soils found in the Midwestlandslidesheadward erosion as seen in the Grand Canyon and Niagra Fallstsunamis scouring inland surfacesfloods, which transport great amounts of rock and soil
small and large sediment