There are actually two (2) types of deposits created - Glacial Tills or Fluvials/Outwashes.
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.
Yes, glaciers played a significant role in shaping various landscapes. As they advance and retreat, they carve out valleys, create fjords, and deposit sediments that form features like moraines and drumlins. This glacial activity has contributed to the topography of many regions, including parts of North America and Europe. Overall, glaciers are key architects of the Earth's surface.
glaciers didnt help in formation of earth crust! if you mean how DO they then i would say that they create valleys or craters with their weight and deposit fresh sediments while frozen and also when they melt.
The direct geologic effect of glaciers includes the formation of various landforms through processes such as erosion and deposition. Glaciers carve out valleys, create fjords, and shape mountains through their movement, leading to features like U-shaped valleys and cirques. Additionally, as glaciers melt, they deposit sediments, forming moraines, outwash plains, and drumlins, which can significantly alter the landscape. These processes contribute to soil formation and influence ecosystems in glaciated regions.
When multiple glaciers flow downward from a single point, they create a feature known as a "piedmont glacier." This occurs when the glaciers spread out and merge as they move into a broader lowland area, often resulting in a lobe-like formation. Piedmont glaciers can significantly reshape the landscape by eroding and depositing sediments as they advance and retreat.
Glaciers that create cirques on the sides of mountains are called cirque glaciers. These glaciers form in bowl-shaped depressions on the slopes of mountains and are responsible for eroding and shaping the characteristic amphitheater-like features known as cirques. Examples of cirque glaciers can be found in mountain ranges around the world, such as the Alps, Andes, and Himalayas.
Drift and/or till.
When glaciers move, they erode the land beneath them by scraping and plucking rocks and sediments. This process can create valleys, fjords, and other landforms. Additionally, as glaciers melt and retreat, they deposit the sediments and rocks they have carried with them, shaping the landscape further.
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, glaciers can profoundly shape mountains through the processes of erosion, transportation, and deposition of sediments. Glaciers carve out U-shaped valleys, create cirques and aretes, and deposit moraines, all of which contribute to the unique features of mountain landscapes. Additionally, the weight of glaciers can cause the Earth's crust to bend and uplift, influencing mountain formation.
glaciers didnt help in formation of earth crust! if you mean how DO they then i would say that they create valleys or craters with their weight and deposit fresh sediments while frozen and also when they melt.
When glaciers advance or retreat, the sediments left behind create a moraine. Drumlins are created by the flow of glaciers that mold sediment into streamlined, elongated hills.
Glaciers can transport and deposit large amounts of soil, rocks, and gravel as they move. This process, called glaciation, can erode bedrock and reshape landscapes. Glacial deposits can also create distinctive landforms like moraines, drumlins, and eskers.
As glaciers pass over land they erode it, changing its features. Rocks frozen in the glaciers scrape across the bedrock, wearing it downand making scratches called striations. Eroded sediments get pushed in front of a glacierand piled up along its sides. These are called moraines. When glaciers begin to melt and retreat, the meltwater forms channels and deposites. Sediment in new locations. Large rocks called erratics can be left behind, many kilometersfrom their source.
Glaciers that create cirques on the sides of mountains are called cirque glaciers. These glaciers form in bowl-shaped depressions on the slopes of mountains and are responsible for eroding and shaping the characteristic amphitheater-like features known as cirques. Examples of cirque glaciers can be found in mountain ranges around the world, such as the Alps, Andes, and Himalayas.
Glaciers create various landforms such as U-shaped valleys, moraines, drumlins, and fjords through processes like erosion, deposition, and melting. For example, as glaciers move, they erode the land beneath them, forming U-shaped valleys. When glaciers retreat, they leave behind piles of debris called moraines. Drumlins are elongated hills formed by glaciers depositing sediments, and fjords are deep, narrow inlets created by glaciers moving through valleys and subsequently melting.
Glaciers shape Earth by eroding rocks and forming valleys, lakes, and fjords through the process of glaciation. The ice movement, melting, and refreezing of glaciers contribute to the shaping of landscapes and the redistribution of sediments. Additionally, the water released from melting glaciers can create rivers, provide freshwater sources, and contribute to changes in the Earth's hydrological cycle.
beacause alpine glaciers are bad for the enviromental energy called phleux that makes chemicals interact with each other smoothing the landscape