The zone that seals the base of a crevasse is known as the "crevasse floor" or "crevasse base." This area is typically composed of dense, compacted ice that has formed as a result of pressure and accumulation. The crevasse floor can be smooth or rough, depending on the ice's characteristics and the dynamics of the surrounding glacier. It plays a crucial role in the stability and evolution of the crevasse as the glacier continues to move.
Hey, people! The seals live in the Antarctic, Alantic, And ... PACIFIC! (Drumroll please...)
Into the Crevasse was created on 2009-10-22.
Sauvé's Crevasse happened in 1849.
an antonym for that would be at the mountains base
A crevasse slip is a type of glacier movement where the upper portion of the glacier slides down relative to the lower portion, causing the opening of crevasses or cracks on the surface. This movement can be triggered by internal glacier stress, changes in temperature, or the presence of water at the base of the glacier. Crevasse slips can pose risks to glacier travelers and mountaineers.
What best to describes a crevasse is a crack in the topmost section of a glacier.
the earthquake resulted a huge crevasse in the small town
Bonnet Carré Crevasse happened in 1871.
smooth
Seals are typically found in various marine environments, including the sunlit zone, also known as the euphotic zone, where sunlight penetrates and supports photosynthesis. This zone extends from the surface down to about 200 meters (656 feet) in the ocean. Seals often inhabit coastal areas within this zone to access food sources like fish and squid. However, they can also dive deeper into darker waters for foraging, depending on the species and available prey.
A huge crack in the ice
True Heroes - 2008 Crevasse was released on: USA: 12 February 2008