Although the natural and physical conditions in those ranges loosely called the Himalaya are probably more diverse than in any other mountain region in the world, still a certain amount of generalization is possible.

General Considerations

Configuration.

Essentially, we find two more or less parallel ranges. The southern and highest is visible from the plains. On this stand the great peaks whose names are familiar to us. This outer range is pierced by numerous rivers which burst through a series of deep, narrow gorges. The low elevation of these river valleys brings an almost tropical fauna and flora up to the foot of the Snows. The snowline on this range, owing to greater precipitation, reaches down lower than on the second range, that to the north. This second, or northern, range constitutes the local water-parting between India and the countries to the north. It is reached by broad, open, treeless valleys almost Tibetan in character as in fauna. Its snowline is high owing to the drier climate. The peaks seldom attain 25,000 feet, and, in general, are not so precipitous as the great line of peaks to the south.

Even in Kashmir this arrangement of two parallel ranges may be traced; but though there is plenty of fine climbing on the ranges which enclose between them the Vale of Kashmir, most of which have already fallen to the attacks of residents and British officers, yet the eyes of the mountaineer from England will be fixed on the vast range of the Karakoram beyond the Indus.

THE HIMALAYA
C. F. MEADE

This grand chain has a character of its own, though there are points of resemblance to both ranges of the Himalaya. The glaciers are the largest outside the Polar regions. The peaks are very high and very precipitous. It is the country par excellence for the mountain explorer; but for the mountain climber the greatest drawback is the journey of four to six weeks from England to the scene of operations.

Climbing Conditions.

Rock climbing is the same all the world over in that the conditions vary on every mountain in any range. Also, a rock peak cannot be really reconnoitred from a distance; we must come to grips with the rocks before we can know the practicability of a route. As to snow and ice, I think conditions are worse in the Himalaya than in the Alps or Caucasus, chiefly owing to greater variations of temperature. Avalanches of all kinds are bigger, and great caution must be exercised in the choice of camps and bivouacs. Snow and ice slopes in the Alps appear to me to look steeper than they eventually turn out to be. In the Caucasus they are about as steep as they look. In the Himalaya I have usually found them markedly steeper than their distant appearance led me to expect.