128 CROFUTI’S NEW OVERLAND TOURIST further, making of tramway 41¢ miles; whole length of road 2014 miles. The tramway is built on the south side of the canyon, away up on the side of the mountain. fine view of the canyon, Bingham, the mines and mills in the neighboring ravines and on the opposite mountain side, and the miners atthe bottom ofthe canyon, working over the old “placer diggings.” At the end of this tramway is located the old Telegraph mine, one of the richest in the Territory, from which over 200 tons o ore a day is shipped, down over the tram and railroad to the smelters in the valley. The cars are hauled up by mules, and low- | ered down tothe “iron horse” below Bing- ham by the car brakes. The mines are numerous in and around Bingham, but we have not the space for a description of them, but will return to the | junction on the Utah Southern, and one mile further arrive at Sanpy—This station is 13 miles south of Salt Lake City, and one of considerable im- portance. | At Sandy is to be seen immense quanti- | ties of ore—ore in sacks, ore loose by the car load, ore in warehouses 500 feet long, with a train unloading on one side and an- other loading on the other; in fact, this is the greatest shipping, smelting and sam- pling point in all Utah. At Sandy are three sampling works, and | twosmelting works, and a lively town of 700 inhabitants, the greater portion em- ployed in the handling and manipulation of ores. Here we find another railroad branching off; this time itis the Wasatch & Jordan Walley. Principal offices at Salt Lake City. GC. W.. SGHOPTBIAD...... nna - cen encin sere President. Ezra Humpueey.... Treas. and Superintendent. This road isa threefoot narrow-gauge, 16 miles in length, running to Alta, at the head of Little Cottonwood Canyon. Itis operated by narrow gauge steam engines for 8.5 miles, and the other 7.5 by broad gauge mules. The road was commenced | in 1870, finished to Wasatch in 1872, and to Alta in 1876. Letus take a trip over it and note a few of the sights. From Sandy the train runs north a short distance, and then turnsto the east, directly for the Wasatch Mountains, leaving the old Flagstaff smelter on the left-hand side of the track, just above the station. The grade is heavy, the soil is stony, and cov- From the cars can be had a ered more orless with sage-brush, and traversed by irrigating ditches conveying the water toa more productive and less stony soil below. Nearing the mountains, about six miles from Sandy, we come to a deep gorge on the left, through which Little Cottonwood Creek has worn its way tothe valley. From this point we bear away to the southward around a low butte, then turn again to the east and northward and run along on an elevated plateau where a most beautiful f| view can be had. On the west, the Jordan Valley, in all its magnificent shades of green and gold, is at our feet, with the brown old mountains bordering the hori- zon in the distance. To the north, fifteen miles away, over as beautiful asuccession of little streams, well-cultivated fields, white cottages, orchards and gardens, as are to be found within the same number of miles in this sce! Fig “Zion” in full view, embowered in green, with the dome of the monster Tabernacle glistening like some half-obscured “silver moon,” sinking at the mountain base; while far beyond, and more to the westward, lays the Great Salt Lake—a mysterious problem. Away to the south, is Utah Lake, looking like one large sheet of burnished silver, surrounded by a net-work of green and gold, while to the east looms up towering granite walls, cleftfrom summit to base, forming a nar- row gorge only sufficiently wide to allow our little road to be built beside a little rippling creek of crystal water. lling along, our train rounds the head of a ravine, through « deep cut, passes the old Davenport Smelting Works on the left, enters the mouth of the canyon be- tween great walls of ite, crosses and re- crosses the little creek, and soon stops at Wasatcu—the end of the steam road, 8.5 miles from Sandy Junction. This isa smal! station with postoffice, store, and a few dwellings ee a population of about 100, more than half of whom are en- gaged in the stone quarries on the north side of the station. At Wasatch all the granite is got out and shaped for the Temple in Salt Lake City. The stone is the best yet discovered in the Territory, being of close, fine grain, of light gray color, and of beautiful birds-eye appearance. The granite on the south side appears much darker than that on the north side of the canyon. From almost every nook and crevice of these mountain cliffs—from the station away