A History of the Comstock Silver Lode & Mines / Nevada and the Great Basin Region; Lake Tahoe and the High Sierras

by Dan De Quille

Other Springs.

Near Elko are several hot springs, with fine springs of cold water in their immediate vicinity. Here, too, is a “chicken-soup” spring. The springs are situated to the northwest of the town, and a bathing-house has been erected for the accommodation of the rheumatic public.

At Golconda are some very large hot springs, near which are others of ordinary temperature. Some of the hot springs are occasionally utilized for scalding hogs. In the cool pools connected with the flow from the hot springs, carp and some other kinds of fish have been planted. It is said that the carp grown in the ponds often venture upon darting through places where water almost boiling hot is bubbling up. These springs are near the Central Pacific Railroad station. Also half a mile south of the track of the Central Pacific road there are, at Hot Springs Station, near the sink of the Humboldt, several springs that send up columns of steam.

There are only a few of the hot springs that are situated near main lines of travel. In Thousand Spring Valley, on the Upper Humboldt, there are literally thousands of springs, some of which send out whole brooks of water. The majority of these, however, are cold. In Churchill County, north of the Sand Springs salt marsh, are hot springs which are 50, 80, and even 100 feet in diameter. They are on the edge of a desert at the foot of a range of rocky hills burnt to a brick-red by volcanic fires. Here, too, are seen thick veins of pure native sulphur. There are hot springs and scalding pools and brooks in every county in the State. In Nye County there are many hot springs in Hot Creek Valley, in Big Smoky Valley, and Lone Valley. There is also in this county the Cabezon Valley Hot Spring, which is medicinal. On the Rio Virgin, in Lincoln County, is one of the finest purgative springs on the Pacific Coast. With other ingredients amounting to 311 grains of solid matter to the gallon, it contains 67 grains of sulphate of soda, 54 grains of sulphate of magnesia, and 3 grains of sulphate of potassa.

Railroads in Nevada.

Although Nevada would appear at a first glance a difficult region in which to construct railroads, the fact is that it is quite the contrary. Between the parallel ranges of mountains running north and south, there are long level valleys, tracts of desert land, requiring very little grading. These valleys and deserts are linked together and connected by plains from the northern to the southern boundary of the State. As these valleys and deserts once formed the beds and connecting channels of chains of lakes now extinct, it is evident that in following their course a line of railroad might be very cheaply constructed. In many places for miles on miles there would be little to do but put down the ties and rails. In many places, too, there are remarkable passages leading east and west from valley to valley, called “gates.” There are clean level east and west cuts through ranges of mountains running north and south. The only difficulty to be encountered in railroad building in Nevada is in running roads to special points (as to mines) high above the general level of the country, as in the case of the Virginia to Truckee when it leaves the valley region to climb the Mount Davidson Range to the Comstock Lode. The whole plateau through which was upheaved the north and south ranges of mountains has a mean elevation of 5,000 feet above the level of the sea in all central Nevada; to the southward it gradually slopes downward, until at the south line of the State, on the Colorado River, the altitude above sea-level is only 800 feet.

The Central Pacific.

The largest stretch of railroad in Nevada is the Central Pacific. Its length within the boundaries of the State, from where it enters, near Verdi, to where it passes out, near Tecoma, is a little over 450 miles. Though this is an east and west road (the course across the interior parallel mountain ranges), yet no great difficulties were encountered in crossing the State. The road enters Nevada from California along the course of the Truckee River, which stream it follows as far east as Wadsworth. Leaving Wadsworth the road traverses a level, sandy plain till the Humboldt River is reached. The road then follows the course of the Humboldt to Cedar Pass, not far from the Utah line.

The Virginia and Truckee.

Having already given a description of this road, it will not be necessary in this place to do more than to mention the distance from point to point between Reno and Virginia City. Soon after leaving Reno the dumps of the flumes that bring wood and lumber down from the pine forests of the Sierras will be seen to the right of the road. The first of these is four miles from Reno; three miles farther on, near Huffaker’s Station, is another, and at Brown’s is a third. Others will be seen about Washoe Valley and Franktown. They are from ten to twenty miles in length, and of the same V-shape as that at Carson City. Steamboat Springs Station is eleven miles from Reno; Washoe, sixteen miles; Franktown, twenty-one miles; Carson City, thirty-one miles; Carson to Empire, three miles; Mexican Mill, three and one-fourth; Morgan Mill, four; Brunswick, five; Merrimac, five and one-half; Vivian, six; Santiago Mill, seven miles; Mound House, ten; Silver Switch, twelve and three-fourths; Scales, sixteen and one-half; Baltic Switch, seventeen and one-half; Crown Point, eighteen; Gold Hill, nineteen; Virginia City, twenty-one miles from Carson and fifty-two from Reno.