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The universal geography : earth and its inhabitants

The universal geography : earth and its inhabitants

The universal geography : earth and its inhabitants

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—THE COLOEADO BASIN. 897the Colorado valley, where the river is older thau the hills through which it hassawn <strong>its</strong> way-Geographers have divided the great chasm into several secondary gorges,which have been named in descending order Cataract, Narrow, Glen, Marble,<strong>and</strong> Gr<strong>and</strong> Canon, this last the longest of all (about 220 miles). <strong>The</strong> northernsection, south of the Kaibab plateau, is altogether unrivalled for the strangegr<strong>and</strong>eur <strong>and</strong> wildness of <strong>its</strong> scenerj'. <strong>The</strong> bed of the current st<strong>and</strong>s 5,000 <strong>and</strong>even 0,000 feet below the edge of <strong>its</strong> rockj^ walls, which, however, have not retainedtheir vertical position. <strong>The</strong>y have been eaten away to great depths in such away as to form vast lateral cirques separated by bluffs or headl<strong>and</strong>s, which riselike pillars or huge towers, girdled round with stratified rocks, all varying in size,slope, <strong>and</strong> colour. In this region of the river valley the caiion broadens outupwards, the distance from brink to brink varying from 5 to 12 miles. <strong>The</strong>enormous mass of rock now missing between the opposite escarpments has beencompletely swept away by the action of the stream. Nowhere else in the wholeworld can there be seen a river ^•alley exhibiting the phenomena of erosion on agr<strong>and</strong>er scale. <strong>The</strong> prodigious dimensions of the eroded chasms, the architecturalarrangement of the stratified rocks, " Babels piled on Babels," the sharp sky-lineof the cliils st<strong>and</strong>ing out against the azui-e vault above, the brilliant tints of therocks hidden by no patch of verdure, the fantastic forms affected by the colossalsculptures which adorn the imposing s<strong>and</strong>stone, marble, granite or lava facadesall combine to make up a picture varying with every hour of the daj', with everyturn of the stream, a picture of unrivalled gr<strong>and</strong>eur <strong>and</strong> diversity of strangeoutlines. On reading their descriptions we begin to underst<strong>and</strong> the expressionsof wonder mingled with awe employed by the geologists engaged in the study ofthe Gr<strong>and</strong> Canon, those especially who have descended to the river bed, lost, asit were, in the bottomless pit while gazing on the gloomy current here <strong>and</strong> therestill rulflcd b}' reefs <strong>and</strong> rapids. So early as 1867 the miner "White, pursued byIndians, had embarked with a companion on a raft, <strong>and</strong> committed himself to theunknown stream. His comrade perished in a whirlpool, but White succeeded insaving his life. Two years later Powell ventured also to embark on the perilousjourney, drifting with the stream from the head to the outlet of the gorge.Twenty years afterwards some engineers repeated the exploit with a view to theconstruction of a railway along the bottom of the caiion. But the first attemptwas unsuccessful. After losing their chief <strong>and</strong> two boatmen the exploring parlyhad to make their way back across the plateau under great hardships to the pointwhence they had started. A few mouths after their return they again set out,with a fresh equipment of boats especially constructed for this strange voyage,<strong>and</strong> this time Stanton successfully navigated the river from Gr<strong>and</strong> Junction, thatis, from the coniluence of the Gr<strong>and</strong> <strong>and</strong> Gunnison Rivers, to the mouth of theColorado, at the head of the Gulf of California.In the stretch of 500 miles in the region of the canons properly so called theriver bed has not a single vertical break like that of Niagara. <strong>The</strong> total descentof 4,200 feet is dccompusi-d into 520 cataracts, falls or rapids, like those of the

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