Drift and/or till.
They are called implied lines.
commisioned
Stereopticon
grammar
Etching.
No, a glacier cannot
There are actually two (2) types of deposits created - Glacial Tills or Fluvials/Outwashes.Tills are basically formed when the receding ice drops what it picked up in piles of debris fields. These can be located at the receding end of the glacier, but can also be formed underneath the glacier as it moves downhill.Fluvials are basically formed when the deposited debris is moved away from the receding glacier by water or wind to a different location sometimes far away from the glacier.The rock content of the Glacial Tills and Fluvials can be left as anything from whole, big boulders or a pile of flour. Rock flour, that is.Rock flour, also known as Glacier Meal, is the pulverized remains of all those boulders that the glacier grinds down into a fine powder as it heads "downstream." This powder can be extremely fine, down to .0006mm (that's almost seven times smaller than a human hair).As the water from the melting ice and snow gathers into a stream, it often carries with it the rock flour turning the water a milky-white haze that's known as Glacier Milk. The glacial milk is swept away from the glacier until the flowing water slows enough for the fine, powdery rock flour to settle to the bottom of a pool, lake or even the ocean forming a fluvial.
Glaciers can pick up and drop boulders Glaciers dig furrows in the ground where they have passed Glaciers are able to move mountains out of their way
Yes, when a glacier stops moving forward, it may deposit an outwash of sediment and debris in front of it. This outwash is typically comprised of materials that were previously carried by the glacier and are now released as it melts or retreats. It can create features like moraines and eskers in the landscape.
As a glacier moves into a stream valley, it can create a U-shaped valley by eroding the valley floor and walls. The glacier may also deposit sediment along the valley as it retreats, forming features like moraines and outwash plains. Additionally, meltwater from the glacier can lead to the formation of kettle lakes and braided streams in the valley.
A common offshore deposit of sand is called a sandbar or shoal. These formations can create shallow areas in bodies of water, making them hazardous for navigation.
This can create volcanic mudflows called lahars.
It melts and leaves a canyon
There are four types of sediments that create sedimentary rocks. The fours types of rocks are sandstone, mudrocks, biochemical and chemical.
The process of gluing sediments together to form sedimentary rock is called lithification. It involves the compaction of sediments under pressure and the cementation of particles by minerals such as calcite, quartz, or iron oxide. Over time, these processes create a solid rock from loose sediment.
Cirques are formed
In a process called "abrasion," a glacier scours the bedrock as it moves, grinding away the surface and shaping the underlying rock through the friction of debris carried along by the glacier. This process helps to create glacial valleys, cirques, and other landforms shaped by glacial erosion.