Reynolds, Osborne, 1842-1912, Brightmore, Arthur William, 1864-, Moorby, William Henry, 1872- · Cambridge [Eng.] The University Press · leaf 233
ther different from thatdescribed above. These, however, are exceptional; and to whatever causesthey may owe their peculiarities, these causes cannot affect the stones towhich I am referring. Again, on careful examination, it is seen that the ordinary hailstones aredenser and firmer towards their… … Fig. 2. Broken Hailstone. When the particle first starts, it will be moving slowly, and the force withwhich the particles impinge upon it will be slight and, consequently, itstexture loose; as, however, it grows in size and its velocity increases it willstrike the particles it overtakes with…
