When, Later, This Exquisitely Pure And Beautiful Side Stream Was Reached, The Great Explorer Determined That As One Stream Had Been Named After The Prince Of The Powers Of Darkness, He Would Name This After The Bright And Beautiful Powers, - Hence The Name "Bright Angel."

A reference to the chapter "How the Canyon was Formed," will explain how this side gorge came into existence, and

Also account for the great upthrust of the granitic rock at its mouth, for the most casual observer cannot fail to note the presence of this rock much higher than it is seen elsewhere.

The North Wall. Before paying particular attention to the vast forms that crowd the interior of the Canyon, let us follow the "build" of the massive wall on the north side. This is part of the great Kaibab Plateau, the highest wall of the whole Canyon system. Its elevation is eight thousand three hundred, as against six thousand eight hundred and sixty-six feet at El Tovar, and it is thirteen miles in an air line from the south rim, where the hotel is located, to the north rim.

The reason for this difference in elevation is explained in the chapter "How the Canyon was Formed." In brief, it is that, during a process of " faulting," the north wall was thrust up above the level of the south wall.

Features above Bright Angel Creek. In any other region but here, this Bright Angel Gorge and the massive figures of rock that sentinel and guard it would be regarded as a scenic marvel, but here it is a mere trivial incident in the greater scenery of the greater Canyon. Yet it is well to note the massive red sandstone points that are lined up on either side on the plateau, above the darkest recesses of the gorge, reminding one of the rows of sphinxes that guard the entrances of some of the Egyptian temples.

Up Bright Angel Creek. Occasionally parties cross the river (either by boat or in an iron cage suspended by a cable), and ascend to the north rim by means of a rude trail up Bright Angel Creek. As the trail for a part of the way ascends the floor of the gorge, down which the stream flows, and as it is exceedingly narrow and without any way of escape in case of severe rain or flood, it is not always safe. To one, however, who loves a rough and adventurous trip, the ascent of this gorge will probably give great satisfaction. A little more than a third of the way up, a waterfall is passed, called "Ribbon Falls." The trail winds and twists with the course of the stream, and finally reaches the summit at an elevation of eight thousand five hundred feet, not far from Greenland Spring. From here one may go east over the Walhalla Plateau to Niji Point, and overlook the Chuar Valley at the mouth of Marble Canyon, where Dr. Walcott spent a winter studying the Algonkian strata of that region.

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