Steep Trails - California - Utah - Nevada - Washington - Oregon - The Grand Canyon By John Muir












































































































































 -   Immediately to the north of
the deepest part of the canyon it rises in a series of subordinate
plateaus, diversified - Page 157
Steep Trails - California - Utah - Nevada - Washington - Oregon - The Grand Canyon By John Muir - Page 157 of 159 - First - Home

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Immediately To The North Of The Deepest Part Of The Canyon It Rises In A Series Of Subordinate Plateaus, Diversified With Green Meadows, Marshes, Bogs, Ponds, Forests, And Grovy Park Valleys, A Favorite Indian Hunting Ground, Inhabited By Elk, Deer, Beaver, Etc.

But far the greater part of the plateau is good sound desert, rocky, sandy, or fluffy with loose ashes

And dust, dissected in some places into a labyrinth of stream-channel chasms like cracks in a dry clay-bed, or the narrow slit crevasses of glaciers - blackened with lava flows, dotted with volcanoes and beautiful buttes, and lined with long continuous escarpments - a vast bed of sediments of an ancient sea-bottom, still nearly as level as when first laid down after being heaved into the sky a mile or two high.

Walking quietly about in the alleys and byways of the Grand Canyon city, we learn something of the way it was made; and all must admire effects so great from means apparently so simple; rain striking light hammer blows or heavier in streams, with many rest Sundays; soft air and light, gentle sappers and miners, toiling forever; the big river sawing the plateau asunder, carrying away the eroded and ground waste, and exposing the edges of the strata to the weather; rain torrents sawing cross-streets and alleys, exposing the strata in the same way in hundreds of sections, the softer, less resisting beds weathering and receding faster, thus undermining the harder beds, which fall, not only in small weathered particles, but in heavy sheer-cleaving masses, assisted down from time to time by kindly earthquakes, rain torrents rushing the fallen material to the river, keeping the wall rocks constantly exposed. Thus the canyon grows wider and deeper. So also do the side canyons and amphitheaters, while secondary gorges and cirques gradually isolate masses of the promontories, forming new buildings, all of which are being weathered and pulled and shaken down while being built, showing destruction and creation as one. We see the proudest temples and palaces in stateliest attitudes, wearing their sheets of detritus as royal robes, shedding off showers of red and yellow stones like trees in autumn shedding their leaves, going to dust like beautiful days to night, proclaiming as with the tongues of angels the natural beauty of death.

Every building is seen to be a remnant of once continuous beds of sediments, - sand and slime on the floor of an ancient sea, and filled with the remains of animals, - and every particle of the sandstones and limestones of these wonderful structures to be derived from other landscapes, weathered and rolled and ground in the storms and streams of other ages. And when we examine the escarpments, hills, buttes, and other monumental masses of the plateau on either side of the canyon, we discover that an amount of material has been carried off in the general denudation of the region compared with which even that carried away in the making of the Grand Canyon is as nothing.

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