These glaciers typically move via basal sliding or subglacial deformation under wet (warm)- based ice in the accumulation area, but only by
internal ice deformation in the colder parts.
Not exact matches
The
ice streams in Antarctica will be flowing rapidly due to basal sliding — so it is incorrect to say that all glaciers are flowing by
internal deformation only.
The current flow speeds at the terminus are too fast to be caused solely by
internal deformation of the
ice, implying that an increase in basal sliding forced by additional meltwater production is the probable cause of the velocity increases.
Glacier - A mass of land
ice that flows downhill under gravity (through
internal deformation and / or sliding at the base) and is constrained by
internal stress and friction at the base and sides.