Deadly was the task of storming such a place. The breech-loading rifles of the Indians thrust through chinks between the rocks were ready to pick off every soldier who showed himself for a moment, while the Indians lay utterly invisible. They were familiar with byways both over and under ground, and could at any time sink suddenly out of sight like squirrels among the loose boulders. Our bewildered soldiers heard them shooting, now before, now behind them, as they glided from place to place through fissures and subterranean passes, all the while as invisible as Gyges wearing his magic ring. To judge from the few I have seen, Modocs are not very amiable-looking people at best. When, therefore, they were crawling stealthily in the gloomy caverns, unkempt and begrimed and with the glare of war in their eyes, they must have seemed very demons of the volcanic pit.
Captain Jack's cave is one of the many somber cells of the castle. It measures twenty-five or thirty feet in diameter at the entrance, and extends but a short distance in a horizontal direction. The floor is littered with the bones of the animals slaughtered for food during the war. Some eager archaeologist may hereafter discover this cabin and startle his world by announcing another of the Stone Age caves. The sun shines freely into its mouth, and graceful bunches of grass and eriogonums and sage grow about it, doing what they can toward its redemption from degrading associations and ****** it beautiful.
Where the lava meets the lake there are some fine curving bays, beautifully embroidered with rushes and polygonums, a favorite resort of waterfowl. On our return, keeping close along shore, we caused a noisy plashing and beating of wings among cranes and geese. The ducks, less wary, kept their places, merely swimming in and out through openings in the rushes, rippling the glassy water, and raising spangles in their wake. The countenance of the lava beds became less and less forbidding. Tufts of pale grasses, relieved on the jet rocks, looked like ornaments on a mantel, thick-furred mats of emerald mosses appeared in damp spots next the shore, and I noticed one tuft of small ferns. From year to year in the kindly weather the beds are thus gathering beauty--beauty for ashes.
Returning to Sheep Rock and following the old emigrant road, one is soon back again beneath the snows and shadows of Shasta, and the Ash Creek and McCloud Glaciers come into view on the east side of the mountain. They are broad, rugged, crevassed cloudlike masses of down-grinding ice, pouring forth streams of muddy water as measures of the work they are doing in sculpturing the rocks beneath them; very unlike the long, majestic glaciers of Alaska that riverlike go winding down the valleys through the forests to the sea. These, with a few others as yet nameless, are lingering remnants of once great glaciers that occupied the canyons now taken by the rivers, and in a few centuries will, under present conditions, vanish altogether.
The rivers of the granite south half of the Sierra are outspread on the peaks in a shining network of small branches, that divide again and again into small dribbling, purling, oozing threads drawing their sources from the snow and ice of the surface. They seldom sink out of sight, save here and there in the moraines or glaciers, or, early in the season, beneath the banks and bridges of snow, soon to issue again. But in the north half, laden with rent and porous lava, small tributary streams are rare, and the rivers, flowing for a time beneath the sky of rock, at length burst forth into the light in generous volume from seams and caverns, filtered, cool, and sparkling, as if their bondage in darkness, safe from the vicissitudes of the weather in their youth, were only a blessing.
Only a very small portion of the water derived from the melting ice and snow of Shasta flows down its flanks on the surface. Probably ninety-nine per cent of it is at once absorbed and drained away beneath the porous lava-folds of the mountain to gush forth, filtered and pure, in the form of immense springs, so large, some of them, that they give birth to rivers that start on their journey beneath the sun, full-grown and perfect without any childhood. Thus the Shasta River issues from a large lake-like spring in Shasta Valley, and about two thirds of the volume of the McCloud gushes forth in a grand spring on the east side of the mountain, a few miles back from its immediate base.
To find the big spring of the McCloud, or "Mud Glacier," which you will know by its size (it being the largest on the east side), you make your way through sunny, parklike woods of yellow pine, and a shaggy growth of chaparral, and come in a few hours to the river flowing in a gorge of moderate depth, cut abruptly down into the lava plain. Should the volume of the stream where you strike it seem small, then you will know that you are above the spring; if large, nearly equal to its volume at its confluence with the Pitt River, then you are below it; and in either case have only to follow the river up or down until you come to it.
Under certain conditions you may hear the roar of the water rushing from the rock at a distance of half a mile, or even more; or you may not hear it until within a few rods. It comes in a grand, eager gush from a horizontal seam in the face of the wall of the river gorge in the form of a partially interrupted sheet nearly seventy-five yards in width, and at a height above the riverbed of about forty feet, as nearly as I could make out without the means of exact measurement.
