Continental glaciers are the ice that covers part of the continents. The flow of the glaciers is facilitated by the elevation levels from thick to thin areas.
Glaciers characterized by their presence on flat surfaces like the continent are called continental glaciers. They don't have a restricted movement like valleys and cover an area of the mountain. Compared to the valley or Alpine glaciers they are thicker and larger.
Unlike the Alpine glacier they don't flow down the slope but from the area of higher elevation to the lower elevation. It flows the glacier from thick deposition towards the thinner ice deposition.
Therefore, the flow of continental glaciers depends on elevation.
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