By the pan processes in the early days there were immense losses in the precious metals and in quicksilver. While the pans might be much alike in construction almost every millman was making experiments with some secret process of his own for the amalgamation of the ore. It now seems ridiculous, but some millmen were actually using sagebrush tea in their pans, and others a decoction of cedar bark. They tried all manner of trash, both mineral and vegetable. It was at that time that untold millions in gold, silver, and quicksilver were swept away into the Carson River with the tailings; for the ore on which all these experiments were tried was almost pure silver. Although scores of amalgamating pans of various patterns have been invented and patented, there is still room for improvement. The improvements made from time to time have resulted in saving a large per cent of the precious metals contained in the ores operated upon, and also in a smaller loss of quicksilver, yet none of the apparatus in use is perfect. Experiments having in view further savings are still constantly being made. The Comstock as a School for Miners. The Comstock is the mother of silver mining in America. In this lode hundreds of men have obtained a thorough practical knowledge of mining in all its forms and departments. Men who were graduated on the Comstock are now to be found in all parts of the world. They early went to Idaho, Montana, Utah, Colorado, New Mexico, Arizona, Alaska, and British Columbia. Old Comstock foremen and superintendents are to-day in charge of mines in Mexico, Central America, South America, Australia, Africa, China, Japan, and all other regions where there is mining for the precious metals. Already they are in the gold fields of the Amoor River—having pushed their way across from Alaska—and they are ready to push their way to the ends of the earth in search of the precious metals. Virginia City and its Surroundings. Virginia City, the county seat of Storey County, is situated on the eastern face of Mount Davidson, the culminating peak of a range of rocky hills running northeast and southwest, and having a length of about thirty-two miles. Mount Davidson rises to a height of 7,775 feet above the level of the sea, and is a rocky, treeless peak. On the slope of this mountain, about 1,775 feet below its summit, lies Virginia City. It may be said that the city occupies a position about midway between the base and the apex of the mountain, as the Carson River, which flows along near the eastern foot of the range, is 1,700 feet below the town. It is literally “a city set on a hill.”