Loess is a fine-grained, wind-blown sediment that can accumulate near glaciers due to the processes of glacial erosion and deposition. As glaciers advance and retreat, they grind down rocks into silt-sized particles, which can then be carried away by wind once the glacier retreats. This wind can deposit the silt in areas adjacent to the glacier, creating loess deposits. Additionally, the cold, dry conditions around glaciers can facilitate the formation and preservation of loess.
loess deposits
This is known as a Lateral moraine. Please see the related link for more information.
I'll just name a handful of them. Or atleast the ones you can usually see. The Worthington Glacier on the Richardson Highway, The Valdez Glacier down Airport Road, Shoup Glacier in Shoup Bay, Anderson Glacier (you can see coming over a mountain) Columbia Glacier and Mears Glacier you can view if you take a Stan Stephens or Lu Lu Belle cruise out of Valdez or take your own boat out.
Loess forms by wind. It is thought that loess, a kind of silt or clay, is formed from deposits of wind-blown dust.
The rock and soil debris accompanying the glacier is moraine. lateral moraine at the sides where avalanches have dropped it, terminal moraine where the glacier finishes, and medial moraine formed from the lateral moraines of two contributory glaciers when they join.
loess deposits
which river rises from a glacier near Mansarover in Tibet ?
loess
loess
loess
loess
loess
The Huang he is yellow due to the sediment that has been take from the loess plateau near the source of the river. This causes it to be yellow
A till.
This is known as a Lateral moraine. Please see the related link for more information.
Loess is deposited by wind.
by melting