I think... Glaciers begin to form when snow remains in the same area year-round, where enough snow accumulates to transform into ice. Each year, new layers of snow bury and compress the previous layers. This compression forces the snow to re-crystallize, forming grains similar in size and shape to grains of sugar. Gradually the grains grow larger and the air pockets between the grains get smaller, causing the snow to slowly compact and increase in density. After about two winters, the snow turns into firn -- an intermediate state between snow and glacier ice. At this point, it is about half as dense as water. Over time, larger ice crystals become so compressed that any air pockets between them are very tiny. In very old glacier ice, crystals can reach several inches in length. For most glaciers, this process takes over a hundred years.
The Lambert Glacier is in Antarctica. (The Fisher Glacier is its prominent western tributary.) A link is provided to the Wikipedia article on this, the world's longest glacier.
it was discovered in1952 by John H Roscoe
Antarctica.
Antartica
The Maquoketa caves in Iowa were formed through years of natural non-glacial erosion.
Corrie lake.
Conical hills are the remains/remnants of a limestone surface and all are usually the same height above sea level
drumlins
Long island .
Eskers
glacial till.
what is a ridge formed from deposits are
The dry falls were formed by glacial activity
Windblown glacial sediments.
Yes they are
Glacial Erosion formed Yosemite Valley and the Sierra Nevada
Drumlin
Fjords
you tell me
It was caused by deposition. Of glacial moraine.
Arete, cirques,and horns