Soon after this camp—the fourth and the last in Marble Canyon—was left behind us, the walls began to widen out, especially on the north-northwest, and by noon we had passed from the narrow, direct canyon, into one with slopes and plateaus breaking the sheer walls, the wall on the left or southeast side being much the lower of the two, and more nearly perpendicular, rising to a height of 3200 feet, while the northwest side lifted up to the Kaibab Plateau, one point—miles back from the river—rising 6000 feet above us.
We halted at noon beside the Nancoweep Valley. A wide tributary heading many miles back in the plateau the right, with a ramified series of canyons running into it, and with great expanses of sage-covered flats between. Deer tracks were found on these flats, deer which came down from the forest of the Buckskin Mountains. This was the point selected by Major Powell for the construction of a trail when he returned from his voyage of exploration to study the geology of this section. The trail, although neglected for many years, is still used by prospectors from Kanab, Utah, who make a yearly trip into the canyons to do some work on a mineral ledge a few miles below here.
What a glorious, exhilarating run we had that day! From here to the end of Marble Canyon the rapids were almost continuous, with few violent drops and seldom broken by the usual quiet pools. It was the finest kind of water for fast travelling, and we made the most of it. The only previous run we had made that could in any way compare with it was in Whirlpool and Split Mountain canyons, when the high water was on. As we travelled, occasional glimpses were had of familiar places on Greenland Point—that thirty-mile peninsula of the Kaibab Plateau extending between Marble Canyon and the Grand Canyon—where we had gone deer-hunting, or on photographic expeditions with Rust.
Another valley from the right was passed, then a peak rose before us close to the river, with its flat top rising to a height equal to the south wall. This was Chuar Butte. Once more we were in a narrow canyon, narrowing by this peak, but a canyon just the same. Soon we were below a wall we once had photographed from the mouth of the Little Colorado; then the stream itself came into view and we were soon anchored beside it. This was the beginning of the Grand Canyon.
CHAPTER XIX
SIGNALLING OUR CANYON HOME
How long we had waited for this view! How many memories it recalled—and how different it seemed to our previous visit there! Then, the high water was on, and the turquoise-tinted mineral water of the Colorado Chiquito was backed up by the turbid flood waters of the Rio Colorado, forty feet or more above the present level. Now it was a rapid stream, throwing itself with wild abandon over the rocks and into the Colorado. There was the same deserted stone hut, built by a French prospector, many years before, and a plough that he had packed in over a thirty-mile trail—the most difficult one in all this rugged region! There was the little grass-plot where we pastured the burro, while we made a fifteen-mile walk up the bed of this narrow canyon! What a hard, hot journey it had been! A year and a half ago we sat on that rock, and talked of the day when we should come through here in boats! Even then we talked of building a raft, and of loading the burro on it for a spin on the flood waters. Lucky for us and for the burro that we didn't! We understand the temper of these waters now.
Cape Desolation, a point of the Painted Desert on the west side of the Little Colorado, was almost directly above us, 3200 feet high. Chuar Butte, equally as high and with walls just as nearly perpendicular, extended on into the Grand Canyon on the right side, making the narrowest canyon of this depth that we had seen. The Navajo reservation terminated at the Little Colorado, although nothing but the maps indicated that we had passed from the land of the Red man to that of the White. Both were equally desolate, and equally wonderful. With the entrance of the new stream the canyon changes its southwest trend and turns directly west, and continues to hold to this general direction until the northwest corner of Arizona is reached.
But we must be on again! Soon familiar segregated peaks in the Grand Canyon began to appear. There was Wotan's Throne on the right, and the "Copper Mine Mesa" on the left. Three or four miles below the junction a four-hundred foot perpendicular wall rose above us. The burro, on our previous visit, was almost shoved off that cliff when the pack caught on a rock, and was only saved by strenuous pulling on the neck-rope and pack harness. Soon we passed some tunnels on both sides of the river where the Mormon miners had tapped a copper ledge. At 4.15 P.M. we were at the end of the Tanner Trail, the outlet of the Little Colorado Trail to the rim above. It had taken seven hours of toil to cover the same ground we now sped over in an hour and a quarter. Major Powell, in 1872, found here the remnant of a very small hut built of mesquite logs, but whether the remains of an Indian's or white man's shelter cannot be stated. The trail, without doubt was used by the Indians before the white man invaded this region.
The canyon had changed again from one which was very narrow to one much more complex, greater, and grander. The walls on top were many miles apart; Comanche Point, to our left, was over 4000 feet above us; Desert View, Moran Point, and other points on the south rim were even higher. On the right we could see an arch near Cape Final on Greenland Point, over 5000 feet up, that we had photographed, from the top, a few years before. Pagoda-shaped temples—the formation so typical of the Grand Canyon—clustered on all sides. The upper walls were similar in tint to those in Marble Canyon, but here at the river was a new formation; the algonkian, composed of thousands of brilliantly coloured bands of rock, standing at an angle—the one irregularity to the uniform layers of rock—a remnant of thousands of feet of rock which once covered this region, then was planed away before the other deposits were placed. All about us, close to the river, was a deep, soft sand formed by the disintegration of the rocks above, as brilliantly coloured as the rocks from which they came. What had been a very narrow stream above here spread out over a thousand feet wide, ran with a good current, and seemed to be anything but a shallow stream at that.