1 gram = 15.432 358 353 grain In thâ¦e US, in medicine, the use of grains is disappearing and seems to be somewhat approximate: A 60 mg dose may be described as 1 grain, but you should expect 1 grain to be about 65 mg, or 0.065 grams.
The two types of glaciers are Valley or Alpine glaciers Continental glaciers. The difference between them is where they flow. Valley glaciers flow in mountain valleys from high to low elevations. Continental glaciers or ice sheets flow over vast unconfined land areas.
The bottom half of a glacier behaves like a plastic while the top is brittle. Crevasses or cracks on the surface forms as a glacier descend down a mountain. Glacier types. There are two types of glaciers: Alpine glaciers-glaciers that occupy mountain valleys. Continental glaciers-glaciers that occupy land masses. Depending on the type of glaciers, they leave behind characteristic erosional features. Glacier or U-shaped valleys-glaciers carve out existing valleys and leave behind U-shaped valleys. www.geology.wisc.edu. Cirques-half bowl shaped hollow that is located high or at the head of the glacier.