The salt exhibit was made up from a very complete set of specimens in sample jars taken from the Museum collections, and a large number of packages from the manufacturers. The salt of New York is obtained from the salina formation in the western part of the State. The industry is of great importance. The deposits are described in State Museum Bulletin 11 by Dr. F. J. H. Merrill. One of the most interesting varieties shown was the solar salt, which has been made on the Onondaga Salt Reservation, Syracuse, since 1788. Blocks of rock salt were shown from the Retsof and Livonia shafts. Most of the salt produced, however, is from wells bored down through the rock salt beds, and is pumped up in the form of brine and evaporated by artificial heat. SOLVAY PROCESS COMPANY The Solvay Process Company, of Syracuse, made a splendid display of soda ash. The plant of this company uses an immense amount of salt which is obtained from the Tully districts and carried by pipes to Solvay. The raw materials used were shown in the lower sections of two cases especially constructed for the exhibit, which also held a set of barrels and other packages in which the soda is shipped. In the upper sections were shown a series of large glass jars with the various products. These were supplied with a series of labels completely describing the process of manufacture and the chemical changes which take place. Above the case there was a set of photographs of the works, illustrating the social life of the work-people employed and the growth of the establishment. USEFUL MINERALS The exhibit of the useful minerals of the State was principally prepared by H. P. Whitlock of the Museum staff. One case contained a set of the abrasive materials, the most important of these being garnet, which is found in great quantities in the Adirondacks. Crude garnet from several mines, the ground and cleaned garnet, and grades of garnet paper were shown. A small millstone to represent the celebrated Esopus grit, emery ore from Peekskill, and quartz and sand from many localities were also exhibited in this case. Another case was filled with feldspar, mica and quartz, which usually occur associated with each other in the form of pegmetite dikes in the crystalline rocks of the Adirondacks and the Highlands of the Hudson. These materials are not as yet very extensively mined but an increasing demand for them is bringing to light many promising localities. GRAPHITE Another valuable mineral which occurs in the State in great quantities is graphite. Specimens of both the crude ore and manufactured graphite were exhibited. The deposits of this material in the form of graphitic limestone cover miles of territory, but more satisfactory processes for its concentration are needed to make it available for use, especially in the higher grades. MUSEUM PUBLICATIONS