the heart of the basin, through beds of zauchneria, and manzanita chaparral, where the bears love to feed, you follow the main stream past a series of cascades and falls until you find yourself between the two lateral moraines that come sweeping down in curves from the shoulders of Red and Black mountains. These henceforth will be your guide, for they belonged to the grand old glacier, of which Black Mountain Glacier is a remnant, one that has endured until now the change of climate which has transformed a wilderness of ice and snow into a wilderness of warm exuberant life. Pushing on over this glacial highway you pass lake after lake set in solid basins of granite, and many a well-watered meadow where the deer with their young love to hide; now clanking over smooth shining rock where not a leaf tries to grow, now wading plushy bogs knee deep in yellow and purple sphagnum, or brushing through luxuriant garden patches among larkspurs eight feet high and lilies with thirty flowers on a single stalk. The lateral moraines bounding the view on either side are like artificial embankments, and are covered with a superb growth of silver-firs and pines, many specimens attaining a height of 200 feet or more.
But this garden and forest luxuriance is soon left behind. The trees are dwarfed, the gardens become exclusively alpine, patches of the heath-like bryanthus and cassiope begin to appear, and arctic willows pressed into flat close carpets by the weight of the winter snow. The lakes, which a few miles down the valley are so deeply embedded in the tall woods, or embroidered with flowery meadows, have here, at an elevation of 10,000 feet above sea level, only thin mats of carex, leaving bare glaciated rock bosses around more than half their shores. Yet amid all this alpine suppression, the sturdy brown-barked mountain pine is seen tossing his storm-beaten branches on edges and buttresses of Red Mountain, some specimens over a hundred feet high and twenty-four feet in circumference, seemingly as fresh and vigorous as if made wholly of sunshine and snow. If you have walked well and have not lingered among the beauties of the way, evening will be coming on as you enter the grand fountain amphitheater in which the glacier lies. It is about a mile wide in the middle, and rather less than two miles long. Crumbling spurs and battlements of Red Mountain bound it on the north, the sombre rudely sculptured precipices of Black Mountain on the south, and a hacked and splintered col curves around from mountain to mountain at the head, shutting it in on the east.
You will find a good campground on the brink of a glacier lake, where a thicket of Williamson spruce affords shelter from the night wind, and wood for your fire.
As the night advances the mighty rocks looming darkly about you seem to come nearer, and the starry sky stretches across from wall to wall, fitting closely down into all the spiky irregularities of the summits in most impressive grandeur. Then, as you lie by your fireside, gazing into this strange weird beauty, you fall into the clear, death-like sleep that comes to the tired mountaineer.
In the early morning the mountain voices are hushed, the night wind dies away, and scarce a leaf stirs in the groves. The birds that dwell here, and the marmots, are still crouching in their nests. The stream, cascading from pool to pool, seems alone to be awake and doing. But the spirit of the opening, blooming day calls to action. The sunbeams stream gloriously through jagged openings of the eastern wall, glancing on ice-burnished pavements, and lighting the mirror surface of the lake, while every sunward rock and pinnacle bums white on the edges like melting iron in a furnace.
Passing round the northern shore of the lake, and tracing the stream that feeds it back into its upper recesses, you are led past a chain of small lakes set on bare granite benches and connected by cascades and falls. Here the scenery becomes more rigidly arctic. The last dwarf pine is left far below, and the streams are bordered with icicles. The sun now with increasing warmth loosens rock masses on shattered portions of the wall that come bounding down gullies and couloirs in dusty, spattering avalanches, echoing wildly from crag to crag. The main lateral moraines, that stretch so formally from the huge jaws of the amphitheater into the middle of the basin, are continued along the upper walls in straggling masses wherever the declivity is sufficiently low to allow loose material to rest, while separate stones, thousands of tons in weight, are lying stranded here and there out in the middle of the channel. Here too you may observe well characterized frontal moraines ranged in regular order along the south wall of Black Mountain, the shape and size of each corresponding with the daily shadows cast by the wall above them.
Tracing the main stream back to the last of its chain of lakelets, you may notice that the stones on the bottom are covered with a deposit of fine grey mud, that has been ground from the rocks in the bed of the glacier and transported by its draining stream, which is seen issuing from the base of a raw, fresh looking moraine still in process of formation. Not a plant or weather-stain is visible on its rough unsettled surface. It is from 60 to more than 100 feet in height and plunges down in front at an angle of 38°, which is the steepest at which this form of moraine material will lie. Climbing it is therefore no easy undertaking. The slightest touch loosens ponderous blocks that go rumbling to the bottom, followed by a train of smaller stones and sand.
Cautiously picking your way, you at length gain the top, and there outspread in full view is the little giant glacier swooping down from the sombre precipices of Black Mountain in a finely graduated curve, fluent in all its lines, yet seemingly as rugged and immovable as the mountain against which it is leaning. The blue compact ice appears on all the lower portions of the glacier sprinkled with dirt and stones embedded in its surface. Higher, the ice disappears beneath coarsely granulated snow. The face is still further characterized by dirt bands and the outcropping edges of blue veins, that sweep across from side to side in beautiful concentric curves, showing the laminated structure of the mass; and at the head of the glacier where the névé joins the mountain it is traversed by a huge yawning bergschrund, in some places twelve to fourteen feet in width, and bridged at intervals by the remains of snow avalanches. Creeping along the lower edge holding on with benumbed fingers, clear sections are displayed where the bedded and ribbon structure of glaciers are beautifully illustrated. The surface snow, though everywhere sprinkled with stones shot down from the cliffs, is in some places almost pure white, gradually becoming crystalline, and changing to porous whitish ice of varying shades, and this again changing at a depth of 20 or 30 feet to blue, some of the ribbon-like bands of which are nearly pure and solid, and blend with the paler bands in the most gradual and exquisite manner imaginable, reminding one of the way that color bands come together in the rainbow.
Should you wish to descend into the weird ice-world of the 'schrund, you may find a way or make a way, by cutting steps with an axe. Its chambered hollows are hung with a multitude of clustered icicles, amidst which thin subdued light pulses and shimmers with ineffable loveliness. Water drips and tinkles among the icicles overhead, and from far below there come strange solemn murmurs from currents that are feeling their way in the darkness among veins and fissures on the bottom. Ice creations of this kind are perfectly enchanting, notwithstanding one feels strangely out of place in their cold fountain beauty. Dripping and shivering you are glad to seek the sunshine, though it is hard to turn away from the delicious music of the water, and the still more delicious beauty of the light in the crystal chambers. Coming again to the surface you may see stones of every size setting out on their downward journey with infinite deliberation, to be built into the terminal moraine. And now the noonday warmth gives birth to a network of sweet-voiced rills that run gracefully down the glacier, curling and swirling in their shining channels, and cutting clear sections in which the structure of the ice is beautifully revealed, their quick, gliding, glancing movements contrasting widely with the invisible flow of the glacier itself on whose back they are all riding. The series of frontal moraines noted further down, forming so striking a picture of the landscape, correspond in every particular with those of this active glacier; and the cause of their distribution with reference to shadows, is now plainly unfolded. When those climatic changes came on that broke up the main glacier that once filled the amphitheater from wall to wall, a series of residual glaciers was left in the cliff shadows, under whose protection they lingered until the terminal moraines under consideration were formed. But as the seasons became yet warmer, or the snow supply less abundant, they wasted and vanished in succession, all excepting the one we have just seen; and the causes of its longer life are manifest in the greater extent of snow in its more perfect shelter from the action of the sun. How much
