answersLogoWhite

0

unlike till,outwash usually consists of particles that are all about the same sizes.

User Avatar

Wiki User

14y ago

What else can I help you with?

Continue Learning about Earth Science

What is th difference between outwash and a moraine?

Outwash is sediment or debris washed away and deposited by meltwater from a retreating glacier, often forming a flat plain. A moraine is a deposit of glacial till or sediment left behind by a glacier as it advances or retreats, creating distinctive ridges or mounds. In summary, outwash results from flowing water from a glacier, while moraines are debris deposited directly by the glacier itself.


What is the difference between sediments in the outwash and sediments in the moraines?

Sediments in outwash are typically well-sorted and composed of sand and gravel, deposited by meltwater streams flowing from glaciers. In contrast, sediments in moraines are unsorted and contain a mix of various sizes of rocks, debris, and till that has been directly deposited by the glacier. Outwash sediments are usually sorted by size and shape, while moraine sediments are unsorted and show a wider range of material types.


What is the sediment laid down by glacial meltwater?

The sediment laid down by glacial meltwater is called glacial outwash or till. Glacial outwash consists of sorted sediments like sand, gravel, and silt that are deposited by flowing water, while till is unsorted sediment deposited directly by the glacier as it melts and retreats.


What are the different types of glacial deposition?

The main types of glacial deposition are till, moraines, drumlins, eskers, and outwash plains. Till is unsorted sediment deposited directly by the glacier, while moraines are ridges of till deposited at the glacier's margin. Drumlins are smooth, elongated hills formed under glacial ice, eskers are winding ridges of sand and gravel deposited by meltwater streams, and outwash plains are flat areas of sorted sediment deposited beyond the glacier by meltwater.


What is a glacial outwash?

Glacial PlainA l outwash plain is a stratified deposit of sand and gravel transported by water from a melting glacial ice sheet.

Related Questions

Till and outwash are both deposits of sediments from what?

Glaciers


How are till and outwash different?

Basically till is unsorted and outwash is sorted. Outwash is sorted by the melt water streams, which have the ability to smooth rocks and pebbles. The till is carried by the glacier which means that all sorts of rocks and boulders can be carried with the ice, creating sharp surfaces on the rocks.


What is the sediment laid down by glacial meltwater called?

There are several names: outwash is one and moraines are another. The outwash forms a flat area sometimes called outwash planes and the moraines are hilly.


Is sediment of different sized particles left by ice from glaciers called outwash?

No, sediment of different sized particles left by ice from glaciers is called glacial till. Outwash is sediment deposited by meltwater streams flowing away from a glacier.


What is th difference between outwash and a moraine?

Outwash is sediment or debris washed away and deposited by meltwater from a retreating glacier, often forming a flat plain. A moraine is a deposit of glacial till or sediment left behind by a glacier as it advances or retreats, creating distinctive ridges or mounds. In summary, outwash results from flowing water from a glacier, while moraines are debris deposited directly by the glacier itself.


What is the difference between sediments in the outwash and sediments in the moraines?

Sediments in outwash are typically well-sorted and composed of sand and gravel, deposited by meltwater streams flowing from glaciers. In contrast, sediments in moraines are unsorted and contain a mix of various sizes of rocks, debris, and till that has been directly deposited by the glacier. Outwash sediments are usually sorted by size and shape, while moraine sediments are unsorted and show a wider range of material types.


What is the sediment laid down by glacial meltwater?

The sediment laid down by glacial meltwater is called glacial outwash or till. Glacial outwash consists of sorted sediments like sand, gravel, and silt that are deposited by flowing water, while till is unsorted sediment deposited directly by the glacier as it melts and retreats.


What landform would be created by outwash?

It would create outwash plains, eskers, and kames.


What are the different types of glacial deposition?

The main types of glacial deposition are till, moraines, drumlins, eskers, and outwash plains. Till is unsorted sediment deposited directly by the glacier, while moraines are ridges of till deposited at the glacier's margin. Drumlins are smooth, elongated hills formed under glacial ice, eskers are winding ridges of sand and gravel deposited by meltwater streams, and outwash plains are flat areas of sorted sediment deposited beyond the glacier by meltwater.


When deposits of till build up What is left behind?

When deposits of till build up, they can leave behind various landforms such as moraines, drumlins, eskers, and outwash plains. These features are created by the movement of glaciers and the deposition of sediments as the glacier retreats.


What is till deposited at the end of glaciers?

Till is deposited by glacial ice. Till is deposited almost exclusively in the ablation zone either by being plastered onto the underlying glacial bed by flowing ice or by sloughing off the glacier's surface as the ice melts. Till are generally unstratified and commonly consist of large rock fragments surrounded by a finer grained matrix of sand, silt, and clay.Outwash is Sand and gravel deposited by melt water. Outwash are typicaly well sorted and stratified so they differ sharply from tills, which are unsorted and unstratified


What are two typyes of glacial deposits?

Two types of glacial deposits are moraines, which are formations of mixed sediment pushed by and deposited from a glacier, and drumlins, which are elongated hills made of glacial till that form parallel to the direction of ice flow.