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The main branches of the Merced Glacier are, perhaps, best suited to our purpose, because their basins, full of telling inscriptions, are the ones most attractive and accessible to the Yosemite visitors who like to look beyond the valley walls. They number five, and may well be called Yosemite glaciers, since they were the agents Nature used in developing and fashioning the grand Valley.

When the Yosemite Indians made raids on the settlers of the lower Merced, they withdrew with their spoils into Yosemite Valley; and the Modocs boasted that in case of war they had a stone house into which no white man could come as long as they cared to defend it.

With a good mustang he rides the peninsula thoroughly. He visits the old Presidio on the outskirts of the growing city. He rides far over the pass of Lake Merced, to where the broken gap in the coast hills leaves a natural causeway for the railway of the future. Philip Hardin, fisher of men, is keeping open house near the plaza.

A wonderful volume of water dashes over the cliff, unbroken by intercepting rocks, and drops a straight distance of six hundred feet. Then it drops three hundred feet more in dancing cascades to the floor of the valley and divides up into three good-sized streams which empty into the Merced River. When once started on its downward course, the water seems all spray.

At length, after I had rounded a precipitous headland that puts out from the west wall of the valley, every peak vanished from sight, and I pushed rapidly along the frozen meadows, over the divide between the waters of the Merced and Tuolumne, and down through the forests that clothe the slopes of Cloud's Rest, arriving in Yosemite in due time which, with me, is any time.

Back by the Coulterville trail, the peaks of Sierra Nevada in sight, across the North Fork of the Merced, by Gentry's Gulch, over hills and through cañons, to Fremont's again, and thence to Stockton and San Francisco all this at the end of August, when there has been no rain for four months, and the air is dear and very hot, and the ground perfectly dry; windmills, to raise water for artificial irrigation of small patches, seen all over the landscape, while we travel through square miles of hot dust, where they tell us, and truly that in winter and early spring we should be up to our knees in flowers; a country, too, where surface gold-digging is so common and unnoticed that the large, six-horse stage-coach, in which I travelled from Stockton to Hornitos, turned off in the high road for a Chinaman, who, with his pan and washer, was working up a hole which an American had abandoned, but where the minute and patient industry of the Chinaman averaged a few dollars a day.

There was another solemn fast about this time, in honour of a saint having had a tooth drawn, or some equally important event, and Don Hombrecillo and I had been at the evening service in the church of the convent of La Merced, situated, as I have already mentioned, directly opposite his house, on the other side of the lane; and this being over, we were on the eve of returning home, when the flannel robed superior came up and invited us into the refectory, whereunto, after some palaver, we agreed to adjourn, and had a good supper, and some bad Malaga wine, which, however, seemed to suit the palates of the Frailes, if taking a very decent quantity thereof were any proof of the same.

The gold dust we found here was coarser than it was where I worked before, down south on the Merced River. Before I came to California I always supposed that gold dust was really dust, and about as fine as flour. We went up the North Fork about a mile or two above town and camped on Wisconsin Flat to begin our mining operations.

Once they say it spouted fire, but that was long ago, and all our volcanoes are dead. But perhaps not so long ago. The Indians tell the strange story that their grandfathers remembered when this bay was a valley covered with oak trees, and the rivers of the north flowed through and emptied into Lake Merced and a rift by the Fort.

Over large areas below the sources of the Tuolumne and Merced the granite is porphyritic; feldspar crystals in inch or two in length in many places form the greater part of the rock, and these, when planed off level with the general surface, give rise to a beautiful mosaic on which the happy sunbeams plash and glow in passionate enthusiasm. Here lie the brightest of all the Sierra landscapes.