Glacial drift
All
Glaciers move slowly.
When glaciers move as they grow, they grind the ground and rock underneath them. These pieces are pushed forward while they grow. When they final begin to melt, the water that is in the glaciers flows out from underneath them. This often carried sand and small bits of gravel. As they melted further and faster, larger gravel and stones wash out. Finally very large rocks and boulders are left behind. All of these are called deposition.
Suspended load: All organic and inorganic material carried in moving water Dissolved load: All organic and inorganic material carried in solution by moving water Bed load: Coarse materials such as gravel, stones. These things move along the bottom of the river by rolling, or sliding.
Australia.Australia
Glacial Drift
To answer this, think about the way water moves and how ice moves. Now think of steady fast-moving streams of water and massive hulking glaciers scraping across the land. Streams push sediments along and sort them into normalized groups. Sand is separated from stones of different sizes. Glacier pick up rocks in their slow progress and deposit them later as the ice melts. The streams' depositions are very regular; the glaciers' depositions are very irregular.
till is the name of the material. In most cases all glacial-related deposits are unsorted and unstratified.
Till is a mixture of sediment and rock that is deposited directly by a glacier, while outwash is the material carried away from a glacier by meltwater and deposited in a different location. Till tends to be unsorted and can have a range of sizes of particles, while outwash is typically well-sorted and composed of smaller particles.
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.
No, the matter is carried off by wind or water and is re-deposited to form new rocks.
Below are the four agents of erosion, so take what you need:Fluvial erosion - rivers mainly. Rivers erode by hydraulic action, abrasion, attrition and solution. Deposition occurs because the river has run out of energy, or energy is low.Marine erosion - oceans and seas. These erode by hydraulic action and abrasion mainly, as the ocean has great sheer force. They do not transport much material, as most of the work is done by gravity, so most material is left directly under where it came from, but separate nonetheless.Glacial erosion - glaciers. Glaciers erode by plucking and abrasion, then deposit the moraine (glacial load) at the snoutAeolian erosion - wind. Wind erodes mainly by blasting sediment at rocks, which is classic abrasion. Sediment is often deposited as a dune.All agents of erosion cause both erosion and deposition as ultimately all eroded material is deposited.
All
Glaciers move slowly.
Glaciers move slowly.
Glacial deposits, often referred to as glacial drift, are the general term for all sediments deposited by a glacier. This can include material like till, moraine, and glacial erratics left behind as the glacier moves and melts.
Glaciers are fallen snow :thats how it's formed