Lookout; Conundrum Prospect, Niblack Anchorage, Moira Sound, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi

Regional Level Types
Lookout; Conundrum Prospect	Prospect
Niblack Anchorage	Occurrence
Moira Sound	Occurrence
Prince of Wales Island	Island
Ketchikan Mining District	Mining District
Prince of Wales-Hyder Census Area	Census Area
Alaska	State
USA	Country

Location: The Lookout prospect is at an elevation of about 1,800 feet, about 0.2 mile northeast of elevation 2230 and about 0.1 mile north-northeast of the southwest corner of section 34, T. 78 S., R 88 E. From the late 1970's to the present (2004), there has been nearly continuous exploration of several geologically similar deposits in an area of about a square mile southeast of the old Niblack Mine (CR216). Those deposits are described separately (CR217-223), but in the recent literature, the Lookout prospect and other deposits in the area are commonly grouped together under the name 'Niblack,' or 'Niblack project'.
Geology: The Lookout prospect as described by Brooks (1902) and Wright and Wright (1908) consists of a mineralized zone up to 300 feet thick in quartz-sericite schist. Within the zone, mineralized bands consist largely of covellite, chalcopyrite, and pyrite. Locally, there are quartz veinlets that have gold values. Brooks (1902) notes silicification adjacent to the veinlets. As of 1908, the workings consisted of two adits, one 160 feet long and the other 60 feet long, and several trenches. Beginning in the mid-70's, a succession of companies, including Cominco-Alaska, Inc., Anaconda Minerals, Noranda Exploration, Houston Oil and Minerals, Long Lac Minerals, and, beginning in 1995, Abacus Minerals, have carried out extensive exploration on several deposits in the Niblack Mine area (CR217-223), testing the now widely accepted theory that they are volcanogenic, stratabound, massive-sulfide deposits. Those deposits are commonly grouped with the old Niblack Mine under the name 'Niblack' or 'Niblack Project'. The exact location of most of the recent exploration in the Niblack area, including several generations of drilling, is not well documented in the public literature. Anaconda Minerals drilled at least two holes in 1978. Green and others (1989) note that Noranda and Lac Minerals drilled 24,000 feet on the deposits in the Niblack area through 1988, and Abacus Minerals drilled 39,000 feet in 1996 (1997?) (Swainbank and others, 1998). The exploration has been mentioned frequently in the annual reports of the Alaska Division of Geological and Geophysical Surveys since the early 80's. In their most recent annual report (Swainbank, and others, 2002), the deposits are grouped under the name 'Niblack'. The area currently is being explored by Abacus Minerals, and information about their work can be found on their web site (www.amemining.com/properties/niblack_project/ ; Jan. 26. 2004). After Abacus Minerals obtained the Lookout prospect in 1995, they drilled at least 45 holes in 1996 and 1997 on it. They have defined an inferred resource of 2.78 millions tons of material grading 2.77 grams of gold and 35.46 grams of silver per ton, 1.71 percent copper, and 3.22 percent zinc (www.amemining.com/properties/niblack_project/ ; Jan. 26. 2004). (This resource is attributed to the 'Niblack' or 'Niblack Project' in recent annual reports of the Alaska Division of Geological and Geophysical Surveys (Swainbank and others, 2002), but it is entirely at the Lookout prospect.). As described by Lac Minerals USA Inc.(1989) and Maas and others (1995), and from a cross-section by Abacus Minerals (www.abacusminerals.com/niblackxsec.htm; April 18, 2000), the area features several large folds that trend west-northwest. The folds consist of a layered sequence of rhyolitic flows and volcaniclastic rocks that host the ore deposits, a hanging wall of mafic flows and sedimentary rocks, and a foot wall of amygdaloidal mafic flows. All of the rocks are regionally metamorphosed to greenschist grade. Maas and others (1991) describe three types of deposits at the Lookout prospect (CR221). It is the best- known deposit and probably typifies the other deposits in the area, including the one at the Niblack Mine. The three types are: 1) volcanogenic massive-sulfide bodies up to 20 feet thick with values of up to 4.9 percent copper, 8.0 percent zinc, 0.265 ounce of gold per ton, and 4.6 ounces of silver per ton; 2) stringer-type sphalerite mineralization in lithic tuffs in the footwalls of the massive sulfide bodies; and 3) auriferous, pyrite-bearing volcaniclastic rocks and polylithic breccias that typically contain about 0.05 ounce of gold per ton, 0.5 to 1.0 ounce of silver per ton, and 1 percent combined copper-zinc across widths of more than 50 feet. The age of the rocks in the area has been variously interpreted. Eberlein and others (1983) mapped the strata as locally metamorphosed graywacke of Silurian or Ordovician age, near a large Paleozoic or Mesozoic granitic intrusion. Gehrels (1992) and Maas and others (1995) mapped them as pre-Ordovician metamorphosed volcanic and sedimentary rocks near a Silurian or Ordovician granitic intrusion. Brew (1996) called them Late Proterozoic and Cambrian Wales Group schist, phyllite, and marble, near a Tertiary granitic intrusion of intermediate composition. Most recently, Slack and others (2002) and S.M. Karl (oral communication, 2003) mapped the strata as Silurian and Ordovician, low-grade, regionally metamorphosed sedimentary and volcanic rocks. Slack and others (2002) also demonstrate that the volcanogenic massive-sulfide deposits in the Niblack area are of Silurian or Ordovician age.
Workings: As of 1908, the workings consisted of two adits, one 160 feet long and and the other 60 feet long, and several trenches. After Abacus Minerals obtained the Lookout prospect in 1995, they drilled at least 45 holes in 1996 and 1997 on it.
Age: Silurian or Ordovician.
Alteration: Not specifically noted, but probably typical of volcanogenic massive-sulfide deposits. Brooks (1902) noted silicification adjacent to the gold-bearing quartz veinlets.
Reserves: Abacus Minerals have defined an inferred resource of 2.78 millions tons of material grading 2.77 grams of gold and 35.46 grams of silver per ton, 1.71 percent copper, and 3.22 percent zinc (www.amemining.com/properties/niblack_project/; Jan. 26. 2004). (This resource is attributed to the 'Niblack' or 'Niblack Project' in recent annual reports of the Alaska Division of Geological and Geophysical Surveys (Swainbank and others, 2002), but it is entirely at the Lookout prospect.)

Commodities (Major) - Ag, Au, Cu, Zn
Development Status: None
Deposit Model: Besshi-type volcanogenic Ag-Au-Cu massive-sulfide deposit (Cox and Singer, 1986

Other Databases

Link to USGS - Alaska:	CR221

Other Regions, Features and Areas containing this locality

References