The Grand Canyon of Arizona [14]
red strata above. In reality, it is a rich creamy lime, but only where the red strata above have been degraded and washed away does the natural color of this wall appear.
The Plateau. Below the red-wall limestone, there are several strata of red and gray and olive rocks that slope to the plateau. This plateau is not quite so wide on the north side as on the south, owing to El Tovar being located in the recess of a great amphitheatre. It is from these plateaus that the finest views of the real Canyon can be obtained. The visitor, sitting on the porch or on the rim at El Tovar, cannot realize that below his feet, as it were, there is an almost exact duplication of the wall and slopes of talus, the thrilling precipices, the alcoves, recesses, promontories and the like, that he sees on the north side. And yet a trip down the trail on to the plateaus reveals these stupendous facts in a manner that is surprising even to those who, for years, have been familiar with them. How much more, then, is such an experience to a tyro. I have met men who were world-wide travelers, and who were visiting the Canyon for the first time; some of these were expert geologists, yet they refused to go down the trail, with the excuse that they could fully grasp the scenery from the rim. But that is impossible. The human mind cannot realize the effects of vastness and power this Canyon scenery produces, except when one stands below the cliffs and looks up. And where the opportunity is given of looking both up to towering walls, and down over beetling precipices, the effect is enhanced.
The Tonto Sandstones. Below the plateau, slight slopes lead the eye to the last of the stratified rocks, the Tonto sandstones of the Cambrian period. These are readily distinguished, mainly by their deep buff color and the fact that generally they are found resting on the archaean or unstratified rocks, locally though incorrectly termed the granite, which makes the Inner Gorge through which the river runs. This "granite" is in the main a blackish gneiss.
The Algonkian Strata. Though the Tonto sandstones usually occupy the location named, there is a deviation from this in the presence of some remnants of strata of the Algonkian period, directly opposite El Tovar. This deviation is discussed in the chapter "How the Canyon was Formed." These remarkable rocks occur to the left (west) of Bright Angel Creek, and lie immediately above the gneiss. Their brilliant red reveals them, and they can be followed up under the base of the Cheops and to a small wash to the left of Osiris. At the mouth of Bright Angel, they rest upon the archaean, with the Tonto sandstones above them, but just in front of the Battleship a break in the gneiss occurs, and on the portion nearest us the Algonkian strata totally disappear, for the Tonto strata rest directly upon the gneiss.
Zoroaster, Brahma and Deva Temples. Now, in turn, let the eye rest upon the temples, towers and buttes that stand in the heart of the Canyon, more or less detached from the main wall. To the right of Bright Angel Creek, striking buttes keep guard. The nearest is an angular mass of solid, unrelieved rock, sloping in a peculiarly oblique fashion. It is Zoroaster Temple, seven thousand one hundred and thirty-six feet in elevation. Close behind it is a more ornate and dignified mass, Brahma Temple, named after the first of the Hindoo triad, the supreme creator, to correspond with the Shiva Temple, soon to be described, on the right. Shiva, the destroyer; Brahma, the creator. The one controlling the forces that have destroyed the strata; the other dominating the powers that have brought these structures into existence. 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 Plateau. Below the red-wall limestone, there are several strata of red and gray and olive rocks that slope to the plateau. This plateau is not quite so wide on the north side as on the south, owing to El Tovar being located in the recess of a great amphitheatre. It is from these plateaus that the finest views of the real Canyon can be obtained. The visitor, sitting on the porch or on the rim at El Tovar, cannot realize that below his feet, as it were, there is an almost exact duplication of the wall and slopes of talus, the thrilling precipices, the alcoves, recesses, promontories and the like, that he sees on the north side. And yet a trip down the trail on to the plateaus reveals these stupendous facts in a manner that is surprising even to those who, for years, have been familiar with them. How much more, then, is such an experience to a tyro. I have met men who were world-wide travelers, and who were visiting the Canyon for the first time; some of these were expert geologists, yet they refused to go down the trail, with the excuse that they could fully grasp the scenery from the rim. But that is impossible. The human mind cannot realize the effects of vastness and power this Canyon scenery produces, except when one stands below the cliffs and looks up. And where the opportunity is given of looking both up to towering walls, and down over beetling precipices, the effect is enhanced.
The Tonto Sandstones. Below the plateau, slight slopes lead the eye to the last of the stratified rocks, the Tonto sandstones of the Cambrian period. These are readily distinguished, mainly by their deep buff color and the fact that generally they are found resting on the archaean or unstratified rocks, locally though incorrectly termed the granite, which makes the Inner Gorge through which the river runs. This "granite" is in the main a blackish gneiss.
The Algonkian Strata. Though the Tonto sandstones usually occupy the location named, there is a deviation from this in the presence of some remnants of strata of the Algonkian period, directly opposite El Tovar. This deviation is discussed in the chapter "How the Canyon was Formed." These remarkable rocks occur to the left (west) of Bright Angel Creek, and lie immediately above the gneiss. Their brilliant red reveals them, and they can be followed up under the base of the Cheops and to a small wash to the left of Osiris. At the mouth of Bright Angel, they rest upon the archaean, with the Tonto sandstones above them, but just in front of the Battleship a break in the gneiss occurs, and on the portion nearest us the Algonkian strata totally disappear, for the Tonto strata rest directly upon the gneiss.
Zoroaster, Brahma and Deva Temples. Now, in turn, let the eye rest upon the temples, towers and buttes that stand in the heart of the Canyon, more or less detached from the main wall. To the right of Bright Angel Creek, striking buttes keep guard. The nearest is an angular mass of solid, unrelieved rock, sloping in a peculiarly oblique fashion. It is Zoroaster Temple, seven thousand one hundred and thirty-six feet in elevation. Close behind it is a more ornate and dignified mass, Brahma Temple, named after the first of the Hindoo triad, the supreme creator, to correspond with the Shiva Temple, soon to be described, on the right. Shiva, the destroyer; Brahma, the creator. The one controlling the forces that have destroyed the strata; the other dominating the powers that have brought these structures into existence. 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.