le Neve (1714).
These processes are accompanied by a gradual descent down the mountain side, during which the neve suffers consolidation, until it becomes compact glacier-ice.
The neve is thus the feeding ground of the glacier (q.v.).
- See C. Le Neve Foster's Ore and Stone Mining (6th ed., London, 1905), or G.
On the north and west the slopes of Great Ararat are covered with glittering fields of unbroken neve.