Sphalerite Vein Quartz Occurrence
Farmington, Connecticut
41.7072°N 72.8295°W
41.7072°N 72.8295°W
The Sphalerite Vein Quartz Occurrence is near Farmington, Connecticut. Historically the site has been part of the Farmington Mining District. Ore mineralization has been found at this location, however the precise grade, tonnage, and extent of the mineralization are not known. There has been no production and little to no activity other than routine claim maintenance since the mineral discovery. The ore mined is composed of prehnite, sphalerite and calcite. The mineralization at this location is from the Upper Triassic epoch 237.00 to 201.30 million years ago. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
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SIMPSON'S MAP AT 1:24000 LOCATES OCCURRENCE BY LETTER SYMBOL.; INFORMATION SOURCE: 1 PUB LIT.
TOTAL$: US
CLOSELY FAULTED CONN. VALLEY BASIN. SHUTTLE MEADOW UNDERLAIN BY TALCOTT BASALT FLOWS; NEAR CONTACT WITH OVERLYING HOLYOKE BASALT FLOWS.
Geological materials at the site.
Physiographic area where the resource is found.
Controls on emplacement of ore such as faults or other structural features.
INFORMATION LACKING. PROBABLY ONLY SMALL AMOUNT OF LOW GRADE SPHALERITE ORE AVAILABLE FROM SMALL FAULT ZONE.
Other deposits in the same region.
Bristol Copper Mine
Mattabesset River Lead Mine
Unnamed Lead Mine
American Steel And Aluminum Processing Plant
Magnetite Iron Mine
Unnamed Magnetite Occurrence
Unnamed Lead Mine
Unnamed Copper Mine
Unnamed Copper Mine
New Haven Mineral Company Barite Mine
* 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
INFORMATION LACKING. FAULT TRENDS NORTH; ONE OF MANY IN AREA. FAULT IN SANDSTONE, SILTSTONE AND SHALE BEDS, ABOUT 270 TO 340 FEET THICK, WHICH ARE UNDERLAIN BY BASALT FLOWS, ABOUT 200 FEET THICK, WITH OCCURRENCE LOCATED NEAR CONTACT OF OVERLYING BASALT FLOWS, ABOUT 250 FEET THICK.