When the lower air is warm enough partially to melt the crystals, they form minute balls. When raindrops, formed in the upper air, fall through a cold current, they are often frozen, producing sleet instead of snow.

WHERE PERMANENT
SNOW EXISTS

Though the winter snows upon the plains, and the slopes of mountains of medium height, disappear during the warm season; yet, in all latitudes, the tops of high mountains are covered with a layer of permanent snow, which the summer heat of these great altitudes is not sufficient to melt.

The lower limit of perpetual snow, called the snow line, is found, within the tropics, about three miles above the level of the sea. In temperate latitudes it occurs at the height of a little less than two miles; and at the northern limit of the continents, it is about half a mile above the level of the sea, or, perhaps, even less than this.

On the Arctic Islands, vast fields of snow remain permanently, at a few hundred feet above the sea level.

The winter snows, falling into the icy waters of the polar oceans, are but partially dissolved; and, remaining upon the freezing surface, they help to form those vast ice floes which encumber the polar seas at all times.

The following table gives the observed height of the snow line in the different latitudes:—

HEIGHT OF THE SNOW LINE

Lat. N.New WorldFeet
75°North Greenland2,300
54°Unalaska3,500
48°Mt. Baker, Oregon, about8,000
43°Rocky Mountains12,500
39°Rocky Mountains14,500
38°Sierra Nevada11,000
19°Popocatepetl, Mexico14,900
Tolima, Columbia15,300
Lat. S. 1°Andes of Ecuador15,800
17°Andes of Bolivia, west side18,500
17°Andes of Bolivia, east side15,700
33°Andes of central Chili14,700
42°Andes of Patagonia6,000
54°Andes of Straits of Magellan3,700
75°Bear Island600
71°Mageroe, Cape North2,300
67°Sulitelma, Lapland3,800
61°Scandinavian Alps5,300
50°Altai Mountains7,000
46°Alps, north side8,800
46°Alps, south side9,200
43°Caucasus11,000
35°Hindu Kush13,000
31°Himalaya, south side16,200
31°Himalaya, north side17,400
12°Abyssinian Mountains14,000
Lat. S. 3°Kilimanjaro16,000
44°New Zealand Alps7,500
HOW SNOW AND ICE FORM
GLACIERS AND ICEBERGS