At several points, however, we observed the bluffs abounded in slate shales, and other coal-bearing earths; and as we suspected then, the Union Pacific Railroad has already developed a vast deposit of coal there. Bitter Creek itself flowed sluggishly by us for a day or so, and was a little miserable stream, that just managed to crawl--usually at the bottom of a deep gulch or abrupt cañon--its chalky color proclaiming its alkali taint even before you tasted it. We must have followed it for a hundred miles or more, and yet it continued very nearly the same in size throughout. What water it drained in one locality was largely evaporated in another, and its wretched, villanous character made it everywhere an eye-sore, instead of a pleasing feature in the landscape as it should have been. But enough of Bitter Creek, and its God-forsaken region. Past Green river, here a considerable stream, we entered the Butte region, and one evening just before sunset approached Church Butte, the most famous of them all. It was too late in the day to explore it, but we had a grand view of it in the shifting sunlight, as we drove slowly by. On the box with the driver, a portion of it was pointed out, that resembled a colossal Dutchman, about lifting to his mouth a foaming beaker. Further on, as we rolled westward, the Teuton faded out, and the church-like character of the Butte more fully appeared. Seen from the west, it presents a very wonderful likeness to an old-time cathedral, of the Gothic type, and at a distance might well be taken for the crumbling ruins of some such edifice, though of cyclopean proportions. Porch, nave, dome, caryatides, fluted columns, bas-reliefs, broken roof and capitals--all are there in shapes more or less perfect, and the illusion was very striking in the shadowy twilight. The Butte itself, like most others there, is a vast mass of sandstone, covered with tenacious blue clay, both of which are being constantly chiseled down by wind and rain. These buttes all seemed either to have been upheaved from the dead level around them, or else to be the surviving portions of great mountain chains, from which the earth has been washed or blown away, leaving their skeletons--so to speak--behind in solitary grandeur. The latter theory seemed more probable, judging by the general direction of the buttes themselves. Much of the scenery about here for a hundred miles or so, was enlivened by sandstone bluffs, cut and chiseled by the elements into castles, fortresses, etc., that frowned majestically at us in the distance; but we were only too glad to quit their grandeur and sublimity, that turned only to barren rocks as we approached, and to hail some signs of cultivation again as we neared Fort Bridger. No doubt the wind has been an important agency in fashioning all these, though scarcely to the extent that is claimed by some travellers. In Bowles' "_Across the Continent_," he tells a story