The Blackwater Prospects are characterized as a volcanic hosted precious-metal hydrothermal cell located in the California Desert.
The Blackwater flow dome complex is characterized by; (1) acid-sulfate alteration assemblages, brecciation and silicification, and (3) anomalous precious metal and trace element values which suggest this prospect represents the upper portion of a hydrothermal gold-silver system.
The Blackwater Prospect is located approximately twenty miles east of the Randsburg-Johannesburg Mining District in San Bernardino County, in Sections 26, 27, 34, and 35, Township 29 South, Range 43 East. The prospect area is readily accessible by gravel roads east of U.S. Highway Route 395.
The area is located west of the Blackwater Well Wilderness Study Area, north of the Historical Site at Blackwater Well, and south of the China Lake Weapons Testing Center.
No production or any record of activity was found in a literature search for the area. However, numerous prospect pits, shafts, adits, dumps and access roads reflect historic exploration activity. It is hypothesized, due to the proximity to the Randsburg-Johannesburg Mining District and Blackwater Well, the prospects on the Butte were investigated for precious metals during the late 1800's and early 1900's. Later, in the 1950's-1960's, adits were driven to determine mineralization.
The Blackwater Well Historical Site, south of the Butte, was a watering station for the 20 mule teams which hauled borax from Death Valley to Mohave.
Westmont (formerly Nicor) staked the property in 1984 and conducted an initial evaluation. In 1987, the area was restaked by P. Drobeck, J.P. Rogowski and L.W. Watson, who leased the unpatented claims to Homestake Mining Company in 1988. A detailed evaluation has been conducted and a drilling program proposed to test this hypothesis.
Summary of Geochemistry
High Values Background Values
Au 2.1 ppm 0.020 ppm
Ag 213 ppm 0.10 ppm
Sb 1300 ppm 5 ppm
Hg 60 ppm 0.10 ppm
The anomalous precious metal values and trace element signatures indicate the existence of a precious metal hydrothermal system at Blackwater Butte and have aided in the identification of numerous target areas. Precious metals and trace element values and exposed alteration assemblages suggest high to moderate potential exists for concealed precious metal mineralization.[1]