|Quadrangle map, 1:250,000-scale||TE|
|Quadrangle map, 1:63,360-scale||A-2|
|Nearby scientific data||Find additional scientific data near this location|
|Location and accuracy||Christophosen Creek is a stream on the north flank of the Kigluaik Mountains whose mouth is on Windy Cove of Imuruk Basin. This creek is not identified by name on USGS topographic maps; its name comes from a location map made by Coats (1944). It is located 0.2 mile east from the center of section 30, T. 5 S., R. 35 W., of the Kateel River Meridian. The graphite deposit at this locality is 1.75 miles southeast of the mouth of the creek and 8.5 miles due east of the White River. It is at the abrupt break in slope on the north side of the mountain front, just upslope of the surface trace of the active Kigluaik normal fault. The graphite-bearing rocks are in the footwall of this fault. This location was not shown by Cobb and Sainsbury (1972), but Cobb (1975) summarized relevant references under the name 'Christophosen Cr.' Location is accurate within 500 feet.|
Christophosen Creek is now encompassed as part of the Graphite Creek record (TE105).
Flake graphite occurs as disseminations and high-grade tabular lenses within amphibolite facies metasedimentary rocks (Coats, 1944). The metamorphic rocks are primarily biotite-quartz schist with some sillimanite and garnet (Sainsbury, 1972). Small granitic plugs, dikes, and sills locally intrude the metamorphic rocks. The graphite-bearing schists are sharply bound to the north by the recently active Kigluaik fault, the principal fault along which late Cenozoic uplift of the Kigluaik Mountains has taken place (Hudson and Plafker, 1978). The graphite-bearing schists strike approximately parallel to the mountain front and dip north between 25 and 65 degrees. They form a zone along the mountain front that is 200 to 400 feet thick and possibly 20,000 feet long (Hudson, 1981; also see Ruby Creek (TE104) and Graphite Creek (TE105) localities to the east). To the south, the graphite-bearing schists are in conformable contact with other amphibolite facies metasedimentary rocks. The latter appear to be feldspathic and contain much less graphite. The graphite-bearing schists make up two general sequences; (1) a heterogeneous sequence of garnet-sillimanite-biotite-quartz schist with disseminated graphite and graphite-rich lenses, and (2) a more evenly layered biotite-quartz schist with disseminated graphite. The latter contains disseminated pyrrhotite and commonly weathers orange.
Claims were first staked on this deposit in 1900 but most of the work appears to have taken place between 1912 and 1917 (Cobb, 1975). Coats (1944) describes 25-foot thick schist units containing 10 percent disseminated graphite. Lenses in these schists, a few inches to 18 inches thick, can contain 50 to 90 percent coarse graphite by volume. The length of the lenses appears to be 10 to 15 times their width. The graphite flakes are commonly 0.004 to 0.04 inches in diameter although some are greater than 0.1 inch across. Two samples (Coats, 1944) contained 24.9 percent and 56.6 percent graphite of which 76 percent and 82 percent was coarser than 30 mesh per inch. Samples of schist with disseminated graphite from this locality appeared to have a few to 15 percent graphite in thin section but laboratory analyses indicated only 4 to 6 percent (Wolgemuth, 1982).During 2011 and 2012, Graphite One conducted exploration work at the Graphite Creek Property. The majority of the exploration work was completed during the summer 2012 including: a time-domain helicopter-borne electromagnetic survey; geological mapping; surface grab, channel and bulk pit sampling; and an 18 drillhole program to test the graphitic units at depth (Duplessis and others, 2013). In 2013, a 10 drillhole program expanded the area of mineralization both easterly and westerly, more than doubling the length of the graphite zone, which was about 2.2 kilometers in 2012, and became 4.8 kilometers in 2013 (Eccles and Nicholls, 2014).
|Geologic map unit||(-165.631645974838, 65.0252391437082)|
|Mineral deposit model||Disseminated flake graphite (Orris and Bliss, 1992; model 37f).|
|Mineral deposit model number||37f|
|Age of mineralization||The metamorphism that has developed coarse graphite in these rocks is Late Jurassic to Early Cretaceous in age.|
|Alteration of deposit||Some shearing and deformation of graphite-rich lenses has accompanied faulting and oxidation of disseminated pyrrhotite has led to orange-staining of graphite-bearing rocks but other types of alteration are not identified.|
|Workings or exploration||
Small surface pits are the principal workings here. Exploration activity in the general area took place in 1994 (Swainbank and others, 1995) as well as in 2011 to 2013 (Duplessis and others, 2013; Graphite One Resources, 2014).During 2011 and 2012, Graphite One conducted exploration work at the Graphite Creek Property. The majority of the exploration work was completed during the summer 2012 including: a time-domain helicopter-borne electromagnetic survey; geological mapping; surface grab, channel and bulk pit sampling; and an 18 drillhole program to test the graphitic units at depth (Duplessis and others, 2013). In 2013, a 10 drillhole program expanded the area of mineralization both easterly and westerly, more than doubling the length of the graphite zone, which was about 2.2 kilometers in 2012, and became 4.8 kilometers in 2013 (Eccles and Nicholls, 2014).
|Indication of production||Yes; small|
A stock pile of hand-sorted material is estimated to contain 50 tons and the few miles of strike between the area of the Christophosen Creek deposit and the Graphite Creek deposit to the east has been estimated to contain 65,000 tons averaging about 60 percent graphite (Coats, 1944). This zone has also been estimated to contain, overall, more than 10 million tons of 10 percent or more graphite (Weiss, 1973).
The first mineral resource estimate for Graphite Creek (TE105), which also includes Christophosen Creek and Ruby Creek (TE104), was prepared by Claude Duplessis, Eng., senior consultant for SGS Canada Inc. (SGS), and an independent Qualified Person under National Instrument (NI) 43-101, using the Canadian Institute of Mining, Metallurgy and Petroleum (CIM) Standards on Mineral Resources and Reserves, Definitions and Guidelines (Duplessis and others, 2013), which was updated the following year to include 2013 drill program results (Eccles and Nicholls, 2014).They report an inferred resource of 186.86 million tonnes of schist containing 5.5 percent graphite with a recommended cut-off grade of 3 percent graphitic carbon (by LECO CR-412 Carbon Analyzer ) and an inferred resource in-situ graphite of 10.34 million tonnes. For the list of other cut-off grades, refer to Eccles and Nicholls, 2014.
|Production notes||About 130 tons of hand-sorted high-grade material were shipped in 1916 (Mertie, 1918) and other small shipments of similar material may have occurred.|
Additional commentsIn January 2012, Graphite One Resources entered an option agreement to earn 100 percent interest in claims encompassing known graphite showings over a three year period through exploration work totaling approximately $1.525 million, which Graphite One has completed with its 2012 summer exploration program. The total Graphite Creek Property land package comprises 129 claims totaling 16,801 acres (6,799 hectares), essentially controlling all prospective lands of known graphite mineralization in the region (Duplessis and others, 2013). The historically-named Christophosen Creek prospect is part of the overall Graphite Creek Project (Eccles and Nicholls, 2014).
|Reporters||Travis L. Hudson (Applied Geology); V.C. Zinno (Alaska Earth Sciences, Inc.), F.H. Wilson (USGS)|
|Last report date||3/15/2016|