Curtis Nickel Sulfide Prospect
Bantam, Connecticut
41.7331°N 73.2741°W
41.7331°N 73.2741°W
The Curtis Nickel Sulfide Prospect is near Bantam, Connecticut. Historically the site has been part of the Mount Prospect Mining District. The Curtis Nickel Sulfide Prospect was closed at the time of data entry with no known plans to re-open. Past operations took place from 1835 to 1837. The ore mined is composed of pentlandite, pyrite and chalcopyrite with waste material consisting primarily of plagioclase, hypersthene and pyroxene. Data from 1982 show the ore was formed by replacement processes of unknown dimensions. Associated rock in this area is pyroxenite from the Lower Devonian epoch 419.20 to 393.30 million years ago. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
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CONTRACT NO J0155043 ENTERED 1976 REVISIONS BY DK HARRISON T REC 080 COLS 35-75 INFO ON DEPOSIT DIMENSIONS ARE NOT AVAILA REC 010 COLS 22-28 THERE ARE INDICATIONS THAT COBALT AND COP BE PRESENT (WMR 91. 308) TPO REVISIONS-ADDED COBALT TO REC 010. ALSO ADDED REC 718& 8.
TOTAL$: US
AREA OF REPEATED MAFIC INTRUSIVES DURING EARLY DEFORMATION PERIOD FOLLOWED BY EMPLACEMENT OF NUMEROUS, SMALL, NON-SULFIDE BEARING GRANITE DIKES; ONLY OUTCROP SEEN OF MASSIVE HYPERSTHENE PYROXENITE.
AREA OF REPEATED MAFIC INTRUSIVES DURING EARLY DEFORMATION PERIOD FOLLOWED BY EMPLACEMENT OF NUMEROUS, SMALL, NON-SULFIDE BEARING GRANITE DIKES; ONLY OUTCROP SEEN OF MASSIVE HYPERSTHENE PYROXENITE.
Minerals or other materials present in the mine.
Characteristics of the ore body.
Geological materials at the site.
Physiographic area where the resource is found.
FIGURES LACKING; PROBABLY ONLY SMALL QUANTITIES OF HIGH GRADE MASSIVE SULFIDE PRESENT.
Other deposits in the same region.
Grannis Nickel Sulfide Mine
Buck Nickel Sulfide Mine
Hardy Nickel Sulfide Mine
Nickel Sulfide Prospect
Pool Nickel Sulfide Mine
Nickel Sulfide Prospect
Unnamed Silver Mine
Unnamed Magnetite Occurrence
Magnetite Iron Mine
Sulfur-Pyrite Occurrence
* Mine bounds on map indicate the general area that a mine occupies. For an detailed map, refer to the overseeing BLM field office.
** The mine central point is based on an average of the mine's bounding box(es) and does not necessarily fall on the claim itself.
1 World-class significance is determined by total endowment of the contained commodity. This includes all past production and remaining reserves. Each commodity is considered separately and commodities cannot be combined to arrive at a significant size. The tonnage thresholds are from the mine model grade-tonnage studies. As of June 2008, many entries were classified as significant under less strict rules.
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Notes
ABUNDANT SULFIDES RATHER UNIFORMILY DISTRIBUTED AS FINE GRAINS AND AGGREGATES. DEPOSIT EXPOSED BY SHALLOW PIT; NICKELIFEROUS SULFIDES IN PROSPECT PIT FOUND MOSTLY IN MASSIVE PYROXENITE RATHER THAN HYPERSTHENE; MOST SULFIDES IN MT. PROSPECT AREA FOUND MOS.
ABUNDANT SULFIDES RATHER UNIFORMILY DISTRIBUTED AS FINE GRAINS AND AGGREGATES. DEPOSIT EXPOSED BY SHALLOW PIT; NICKELIFEROUS SULFIDES IN PROSPECT PIT FOUND MOSTLY IN MASSIVE PYROXENITE RATHER THAN HYPERSTHENE; MOST SULFIDES IN MT. PROSPECT AREA FOUND MOSTLY IN LESS FELDSPATHIC NORITE.