|Quadrangle map, 1:250,000-scale||AR|
|Quadrangle map, 1:63,360-scale||B-2|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||Approximately 1.5 miles west of the Shunghak Rivers, section 29, T. 22 N., R. 10 E., of the Kateel River Meridian, at approximately 3,200 ft in elevation. The coordinates are accurate to within 500 feet.|
The Cliff South prospect is in a highly complex deformed sequence of predominantly country rock schists and greenstones. Exposures are found along a prominent north-south trending cliff. Two inter-layered sequences of metamorphosed Devonian-Mississippian volcanic, volcaniclastic, and sedimentary rocks have been identified; these contain the Cliff North/Horse Creek and Cliff South mineral showings. The structure is very complicated and all three prospects are different parts of a larger structure. The Horse Creek (AR029) occurrence is on the north limb of an north-dipping overturned syncline, the Cliff North occurrence is on the south limb of the overturned syncline, while Cliff South is on the open south limb of a corresponding anticline between Cliff South and Cliff North (Ellis, 1980).Mineralization is characterized by copper, lead, zinc, and silver occurring as massive, semi-massive, and disseminates sulfide found in outcrop and by diamond drilling. Detailed mapping of this zone indicated that the mineral horizons contain widespread mineralization, with locally calcareous lenses of massive sulfides up to 8 feet thick (Ellis, 1980).
|Geologic map unit||(, )|
|Mineral deposit model||Kuroko massive sulfide (Cox and Singer, 1986; model 28a).|
|Mineral deposit model number||28a|
|Age of mineralization||Devonian, based on age of host rock (Ellis, 1980).|
|Alteration of deposit||Strong sulfide oxidation. Quartz, chlorite, calcite, and sericite alteration is associated with mineralization; there is also sericite-altered quartz -muscovite-schist (Ellis, 1980).|
|Workings or exploration||Initial exploration efforts started in the mid 1970s. Exploration efforts to date includes geochemical surveys such as rock, soil, and stream sediment sampling, geophysical surveys that included induced polarity (IP) and electromagnetic (EM) survey, and three diamond drill holes. Gossan samples assayed as high as 13,000 parts per million (ppm) Cu, 19,000 ppm Pb, 9,000 ppm Zn, and 220 ppm Ag. The mineralized zones in drill holes averaged 25 feet thick of 0.25 percent copper, 1.0 lead, 3.0 percent zinc and 1.0 ounce per ton silver. The majority of this work was completed between 1976 and 1983 by Sunshine Mining Company (Ellis, 1980, 1983).|
|Indication of production||None|
Additional commentsCliff South is referred to under Horse Creek (AR029) generally as 'Cliff'. In 2014, Cliff South (and Cliff North) was created as a separate record from Horse Creek since both are on separate parts of a large overturned syncline and the prospects are separated by about a mile (W.T. Ellis, Vice President, Alaska Earth Sciences, Inc., oral communication, 2014).
Cox, D.P., and Singer, D.A., eds., 1986, Mineral deposit models: U.S. Geological Survey Bulletin 1693, 379 p.
Ellis, W.T., 1980, Ambler River Project, Alaska, Project Memorandum No. 7, Summary Report of Past Field Investigations and 1980 Field Investigations, Sunshine Mining Company, 114 p. (Report held at Alaska Earth Sciences, Inc., Anchorage, AK).
Ellis, W.T., 1983, Ambler River Project, Alaska, Project Memorandum No. 10, 1983 Field Investigations, Sunshine Mining Company, 49 p. (Report held at Alaska Earth Sciences, Inc., Anchorage, AK).
|Reporters||A. Angel (Alaska Earth Sciences, Inc.); V.C. Zinno (Alaska Earth Sciences, Inc.)|
|Last report date||3/11/2014|