The Grand Canyon of Arizona; how to see it by George Wharton James
page 52 of 265 (19%)
page 52 of 265 (19%)
![]() | ![]() |
|
completely hidden and embowered in foliage. 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. From the rocks above, with a drop of about fifteen feet, seeping through a green cluster of maidenhair ferns, the pure water of the spring drips into a stone trough placed to receive it. Day and night, winter and summer, fair weather or foul, it seldom varies its quick, tinkling, merry drip, drip into the receptacle below. Below the trough, a natural cavity in the rocks receives the overflow, and here, within the pool and on its edges, aquatic and other plants grow in profusion. By the side of this ever-flowing water, Louis Boucher, the builder of the trail, has his simple home camp. Two tents, placed end to end, rest against the wall, well protected from sun and rain, though the morning's sun shines in freely. Below is a corral for horses, mules and burros used on the trail. Hermit Basin. Here, after lunch, one continues on his trail trip to the river. For three miles the trail winds in and out of the recesses, on the easily rolling ground of the plateau. There are no sharp descents. For about half a mile the trail is in Dripping Spring Amphitheatre, an alcove on the edge of Hermit Basin, so named by Louis P. Brown, a miner and prospector, who, in the early eighties, made this basin his home while engaged in prospecting operations in the Canyon. As the plateau passes across the basin and out to the open Canyon, the scene becomes more and more enlarged, until it is stupendous and vast beyond description. Down on the right, Hermit Creek cuts its narrow path deeper and deeper, until it reaches the red-wall limestone, where it makes |
|