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They might judge of the long curvature of the conformation of the range just here, for on the opposite height was visible at intervals the road they had traveled, winding in and out among the trees, ascending the mountain in serpentine coils; they beheld the Cove beneath from a new angle, and further yet the barren cherty slope on which, despite the distance, the witch-face could still be discerned by eyes practiced in marking its lineaments, trained to trace the popular fantasy.
Brahma is seven thousand five hundred and fifty-four feet in elevation. Behind Brahma is another butte, which, however, cannot always be dissevered from the main wall. It has no cap of cherty limestone. It can be readily discerned, therefore, by its flat-topped appearance. It is Deva Temple, seven thousand three hundred and forty-four feet above sea level. Buddha Temple and Cloister; Manu Temple.
The highest point is only fifty feet above the level of the sea, and the entire circumference is under three-quarters of a mile. This small point rises abruptly out of the depths of the ocean. Its mineralogical constitution is not simple; in some parts the rock is of a cherty, in others of a feldspathic nature, including thin veins of serpentine.
First there is the band of cherty limestone, from which a sloped talus leads to the creamy sugary sandstone. Immediately below this begins the "red," which descends in strata of varying width and color down to a rather narrow-appearing slope of red talus, which leads the eye to the widest member of all the Grand Canyon strata. This is the so-called red-wall limestone.
There was the grim Big Injun Mountain to the right, with its bare, beetling sandstone crags. There was the long line of cherty hills to the left, covered by a dark growth of stunted pines.
Then it winds its way down and around the cherty limestone, to the top of the cross-bedded sandstone, down which zigzags and steps lead one to the spring itself. This is located in a picturesque spot. Picture a great, overhanging wall at the very bottom of the cross-bedded sandstone, from twelve to fifty and more feet high, the recess being perhaps thirty or forty feet back.
The face of this wall, close before us, is carved into numerous alcoves, and as we near its base, we observe to the right a vast double-cornered recess known as Angel Alcove. From here it is interesting to look up to the rim and observe the peculiar and varied contour of the many pinnacles cut by wind and storm out of the cherty limestone. Buddha and Manu Temples.
As Sol started off with the alertness of a scurrying rabbit, she shrilly called out in a frenzy of warning: "Go the other way, Sol up through the pawpaws! Them cherty rocks will cut yer feet like a knife." Sol had nerves of his own. Her sharp cry had caused him to spring precipitately backward, frightened, but uncomprehending his danger.
Thus the streams below are alternately choked and cleared from period to period. To the south of the Vermilion Cliffs the last series or zone of plateaus north of the Grand Canyon is found. The summits of these plateaus are of cherty limestone.
The topmost is the cherty limestone, the layers of which lead the eye to the crossbedded sandstone, a creamy buff in color, and composed of a soft, sugary sand. Each of these walls is from five hundred to six hundred feet high, though in some parts of the Canyon they are reduced to not more than four hundred feet. Maricopa and El Tovar Points.
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