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Unnamed (Lindblom Pit lode and lode on Byron Association Placer claim, U.S. Mineral Survey No. 1835)

Prospect in Alaska, United States with commodities Gold, Silver, Lead, Zinc
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Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Alteration
  8. Mineral occurrence model information
  9. Host and associated rocks
  10. Nearby scientific data
  11. Economic information about the deposit and operations
  12. Mining district
  13. Links to other databases
  14. Bibliographic references
  15. General comments
  16. Reporter information

Geologic information

Identification information

Deposit ID 10307994
Record type Site
Current site name Unnamed (Lindblom Pit lode and lode on Byron Association Placer claim, U.S. Mineral Survey No. 1835)

Geographic coordinates

Geographic coordinates: -165.43948, 64.61828 (WGS84)
Relative position This prospect is on the lower southwest slopes of Mount Byrnteson between Lindblom Creek and Rock Creek. The map site is on the northeast end line of a patented claim (U. S Mineral Survey 1835), in the SE1/4 section 15, T. 10 S., R. 34 W., Kateel River Meridian. This site is the approximate boundary between a prospect locally called Lindblom Pit (above 250 feet elevation) and a lode on Byron Association patented placer claim U.S. Mineral Survey No. 1835 (below 250 feet elevation). It is accurate to within about 500 feet.

Site location context

Political divisions (FIPS codes)

Nome(Census area)

Alaska(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Nome C-1(quadrangle 1:63,360 scale)

Solomon NW(quadrangle 1:100,000 scale)

Nome(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Nome(hydrologic unit)

Norton Sound(hydrologic accounting unit)

Northwest(hydrologic subregion)

Alaska(hydrologic region)

Geographic areas

Country State
United States Alaska

Commodities

Commodity Importance
Gold Primary
Silver Secondary
Lead Secondary
Zinc Critical Secondary

Materials information

Materials Type of material
Arsenopyrite Ore
Galena Ore
Gold Ore
Pyrite Ore
Sphalerite Ore
Albite Gangue
Calcite Gangue
Quartz Gangue

Alteration

  • (Local) Albitization, silicification, and sulfidization.

Mineral occurrence model information

Model code 273
USGS model code 36a
Deposit model name Low-sulfide Au-quartz vein
Mark3 model number 27

Host and associated rocks

  • Host or associated Host
    Rock type
    Stratigraphic age (youngest) Barremian

Nearby scientific data

(1) -165.43948, 64.61828
ListMap

Economic information

Comments on the geologic information

  • Geologic Description = The informally named Lindblom Pit prospect crops out and is exposed in trenches between elevations of about 300 to 400 feet on the hill slope between Lindblom and Rock Creeks. The deposit consists of sulfide-bearing sheeted quartz veins that cut pelitic schist, marble, and quartzite, probably of early Paleozoic protolith age (Hummel, 1962 [MF 247]; Sainsbury, Hummel, and Hudson, 1972 [OFR 72-326]; Till and Dumoulin, 1994; Bundtzen and others, 1994). The deposit is dominantly arsenic- and albite-rich; grades locally exceed 0.3 ounce of gold per ton, but at least four drill holes found little continuity in the veins. Kennecott Exploration Company subsequently optioned and explored the Byron Association Placer Claim (U.S. Mineral Survey No. 1835), which extends uphill to about 250 feet in elevation about on strike (northeast) with the deposit at Lindblom Pit. Trenches and shallow drill holes on the northeast part of the placer claim disclosed a sheeted vein system, superficially like the one at Rock Creek (NM207). Quartz veins in steep norhteast-striking fissures contain arsenopyrite, galena, pyrite, and sphalerite but have relatively low gold contents. The best trench intercept was about 40 feet of material containing 0.02-0.03 ounce of gold per ton. The sheeted vein complex was developed above a low-angle arsenic-rich fault zone (Ben Porterfield, oral communication, 2000).. The Lindblom Pit lode is northeast of the northeast end line of the patented claim (U.S. Mineral Survey No. 1835). Holes drilled on the Lindblom Pit prospect by Newmont Mining Company in 1992 were collared between approximate elevations of 325 and 380 feet. In about 1995, Kennecott Exploration Company obtained a lease on the patented claim and explored the southwest projection of the lode deposit at elevations between 150 and 250 feet. Both prospects are within a very large arsenic soil anomaly. This anomaly was first defined by BHP in about 1989-90 and extended by Kennecott in 1994 and 1995. The anomaly is marked by soils containing greater than 400 ppm arsenic; extensive areas contain more than 2,000 ppm arsenic. The anomalous area is separated from similar arsenic-rich rocks by the Brynteson fault. This fault strikes N 5-10 E; it is almost certainly post-mineral and separates the Lindblom lode prospect area from the Rock Creek area (NM207 to NM215). Small amounts of placer gold and scheelite are present on Lindblom Creek (NM205) immediately north of this lode prospect. Some placer gold was produced from 4- to 5-foot-thick gravels in the narrow, 25-foot-wide part of the upper creek (Collier and others, 1908; Moffit, 1913). Some scheelite-bearing quartz veins are also reported in the drainage (Coats, 1944; Anderson, 1947; Thorne and others, 1948).
  • Age = Probably mid-Cretaceous or younger, the time of regional metamorphism of the host rocks.

Economic information about the deposit and operations

Development status Prospect

Comments on exploration

  • Status = Active?

Mining district

District name Nome

Comments on the workings information

  • Workings / Exploration = Prospect pits, small trenches, and drill holes have explored this prospect. It is within a large soil geochemical anomaly characterized by high arsenic content. An association placer claim was located in 1908 and was patented by Elizabeth Joliffe in 1925 (Byron Association, U.S. Mineral Survey No. 1835). The claim was explored by long northeast-aligned cuts that may have exposed small residual placer deposits, which were not extensively developed. The Lindblom Pit area appears to have been discovered or relocated in about 1986 by R.V. Bailey, a geologist of Denver, Colorado, during work on the nearby Rock Creek deposits (for example, NM207). The area was within a large geochemical soil survey carried out by BHP in 1990. The deposit was trenched and drilled by Newmont Mining Company in 1992. Kennecott Exploration Company subsequently optioned the Byron Association claim and explored it with trenches and drill holes (Ben Porterfield, oral communication, 2000).

Reference information

Bibliographic references

Comments on the references

  • Primary Reference = This report

General comments

Subject category Comment text
Deposit Model Name = Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a).

Reporter information

Type Date Name Affiliation Comment
Reporter 10-JUL-00 Hawley, C.C. and Hudson, Travis L. Hawley Resource Group

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

Maps centered on this site

Authoritative Alaska resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.