Moraine
An esker is a long, winding ridge of sand and gravel deposited by a melting glacier. It is typically formed in tunnels within or beneath the ice and can stretch for many kilometers. Eskers are a common feature in glaciated regions.
Bars: Accumulations of sediment that form along the river's edges, typically made up of sand and gravel. Braided channels: Multiple shallow, interconnected channels separated by sand and gravel bars, often forming in areas with high sediment load. Point bars: Accumulations of sediment on the inner curve of a meander, formed by the slower flow and deposition of sediment on the inside of the bend.
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.
All types of glacier sedimentary deposits are called drift. Winding ridges of sand and small bits of gravel formed by the out wash of melting ice from glaciers are called eskers kames, or moraines. Moraines are also found on the surface of glaciers. Kames form on flat or inclined ice, in holes, or in cracks. They may also be called scree and talus which also come from eroding mountains.
All types of glacier sedimentary deposits are called drift. Winding ridges of sand and small bits of gravel formed by the out wash of melting ice from glaciers are called eskers kames, or moraines. Moraines are also found on the surface of glaciers. Kames form on flat or inclined ice, in holes, or in cracks. They may also be called scree and talus which also come from eroding mountains.
A long winding ridge made from deposits of sand and gravel is called an esker. Eskers are formed by the melting of glaciers and the deposition of sediment as the flowing water carries and deposits material in a sinuous ridge-like form.
eskers
Eskers are long, winding ridges of gravel and sand left behind by melting glaciers, while kames are irregularly shaped mounds of sediment deposited by glacial meltwater. Both formations are composed of stratified layers of sand and gravel that were sorted and deposited by flowing water during the glacier's retreat.
Alluvial deposits, which are created by the movement of water and include sediments like sand, clay, and gravel. Glacial deposits, formed by the movement and melting of glaciers, leaving behind materials such as moraines, till, and outwash. Delta deposits, which are sediment accumulations at the mouths of rivers where water flow slows and sediment is dropped, forming features like distributaries and levees.
I think road salt it made of salt, gravel and sand. The salf lowers the melting point of the snow/ice, so therefore melting it, and the sand and gravel give a car grip.
Steams flowing in tunnels beneath glaciers deposit sand and gravel
No, eskers are not caused by glacial erosion. Eskers are long, winding ridges of sand and gravel that are formed by meltwater streams flowing in tunnels within or under glaciers. Glacial erosion refers to the process by which glaciers carve and shape the land through the movement of ice and debris.