Want this question answered?
The zone of fracture experiences tension hen the glacier moves over irregular terrain. This tension results in gaping cracks called crevasses. Crevasses can be 50 meters deep. They are often hidden by snow and make travel across glaciers dangerous.
Glaciers are formed from the compaction of snow, therefore they are strictly a fresh water formation.
Roughly 40,000 meters from sea level.
8m3
the Cenote at Ik-Kil, according to our tour guide, is 50 meters deep and the water surface is about 30 meters below ground
The zone of fracture experiences tension hen the glacier moves over irregular terrain. This tension results in gaping cracks called crevasses. Crevasses can be 50 meters deep. They are often hidden by snow and make travel across glaciers dangerous.
A crevasse is a large fissure, or crack, in something although it is usually applied to a glacier.
Crevasses
crevasses
Antarctica is not known for its caves. However, as glaciers calve off the continent forming ice tongues, there are essentially 'inverted crevasses' that one can enter from the beach. Since these are movable, ventures into these structures is temporary and not deep.
Plastic flow occurs below that depth.
Petrels normally live in deep rock crevasses or in rocky cliffs.
Answer: 200 meters deep = 656.167 feet deep.
I only know that alpine glaciers can carve deep u-shaped valleys in the mountains.
lake sebago is <2000 metres deep.
In meters, Lake Erie is 64 meters deep.
fjord