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.
Simply stated, a glacier is a large, slow-moving mass of ice. While there are many types of glaciers, they can be divided into two categories: alpine and continental. Alpine glaciers are found in a mountainous region and flow down valleys.Continental glaciers are dome-shaped glaciers that flow away from a central region and are largely unaffected by the landâs topography. The Greenland and Antarctic ice sheets are examples of continental glaciers.Smaller masses of ice, called ice caps, are also considered continental glaciers. Alpine glaciers are further classified by their shape as well as the surface they flow onto.lpine glaciers flow down valleys, and continental glaciers flow outward in all directions from a central point. Glaciers move by two mechanisms: internal deformation and sliding. Internal deformation occurs when the enormous mass of a glacier causes it to spread out due to gravity.