Roxbury Iron Mine
Roxbury, Connecticut
41.5673°N 73.3440°W
41.5673°N 73.3440°W
The Roxbury Iron Mine is near Roxbury, Connecticut. Historically the site has been part of the Southeast Berkshire Highlands Mining District. The Roxbury Iron Mine was closed at the time of data entry with no known plans to re-open. Past operations took place from 1760 to about 1815. The ore mined is composed of pyrite, galena and chalcopyrite with waste material consisting primarily of quartz. The mineralization at this location is from the Holocene epoch 11,784 years ago to present. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
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Additional textual information about a site or mine.
GATES' MAP LOCATES MINE BY SYMBOL. USGS TOPO, 1955, ROXBURY, 1:24, 000, MINE DUMP SHOWS AS TOPOGRAPHIC EXPRESSION ON WEST VALLEY BOTTOM OF SHEPAUG RIVER.; INFORMATION SOURCE: 1 PUB LIT.
GATES' MAP LOCATES MINE BY SYMBOL. USGS TOPO, 1955, ROXBURY, 1:24, 000, MINE DUMP SHOWS AS TOPOGRAPHIC EXPRESSION ON WEST VALLEY BOTTOM OF SHEPAUG RIVER.; INFORMATION SOURCE: 1 PUB LIT.
DATE OF COMMENTS: JUNE, 1976. COMMODITIES 2 (QTZ ); AND 3 (SIDERITE ARE RECOVERABLE GANGUE MINERALS. CURRENT OPERATIONAL STATUS IS P (IRON) PRODUCER. INFORMATION ON THIS DEPOSIT COMES LARGELY F REF 700 INCLUDING LOCATION COORDINATES.
Formal or informal mining district names.
TOTAL$: US
WALL ROCK FOLIATION STRIKE EAST-WEST, FOLIATION DIP 10 DEGREES NORTH. MINE HILL GRANITE GNEISS CONSIDERED SYNTECTONIC INTRUSIVE INTO CAMBRO-ORDOVICIAN HARTLAND FORMATION OF INTERLAYERED MICAQUARTZITE AND SCHIST.
WALL ROCK FOLIATION STRIKE EAST-WEST, FOLIATION DIP 10 DEGREES NORTH. MINE HILL GRANITE GNEISS CONSIDERED SYNTECTONIC INTRUSIVE INTO CAMBRO-ORDOVICIAN HARTLAND FORMATION OF INTERLAYERED MICAQUARTZITE AND SCHIST.
Geological materials at the site.
Physiographic area where the resource is found.
NO FIGURES AVAILABLE; ESTIMATE LARGE TONNAGE OF VEIN QUARTZ WITH SULFIDES AND CARBONATE AVAILABLE.
Other deposits in the same region.
Roxbury Siderite Mine
Roxbury Iron Mine
Siderite Iron Mine
Sulfur-Pyrite Occurrence
Woodbury Pegmatite Quarry Mica Mine
Brookfield Lead Mine
Roebling Mica-Feldspar-Beryl Mine
Magnetite Iron Mine
Unnamed Magnetite Occurrence
Gold And Silver 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
PROSPECTED 1750 BY HURLBUT AND HAWLEY, MINED 1760 BY BRONSONS' BROTHERS, SANK MINE SHAFT 175 FEET DEEP, VENTILATION SHAFT NOT SO DEEP, BOTH PARTIES MINED SPHALERITE FOR SILVER, BOTH PARTIES WENT BANKRUPT, SILVER IS REPORTED. THREE OTHER PARTIES TRIED FOR SI.
PROSPECTED 1750 BY HURLBUT AND HAWLEY, MINED 1760 BY BRONSONS' BROTHERS, SANK MINE SHAFT 175 FEET DEEP, VENTILATION SHAFT NOT SO DEEP, BOTH PARTIES MINED SPHALERITE FOR SILVER, BOTH PARTIES WENT BANKRUPT, SILVER IS REPORTED. THREE OTHER PARTIES TRIED FOR SILVER BY OPEN PIT, ALL FAILED; LAST MINED FOR SIDERITE BUT METALLURGY TOO DIFFICULT. LAST OWNED BY DAVID J. STILES (1831) TWO PARALLEL VEIN QUARTZ WITH SIDERITE. FIRST VEIN 200 TO 300 FEET LONG PINCHES OUT INTO HILL SIDE; MAIN ORE VEIN WORKED ALONG STRIKE FOR 1500 FEET OR MORE BY TWO ADITS, WHICH STOPED BOTH VEINS THROUGH VERTICAL INTERVAL OF 50 TO 75 FEET. VEIN QUARTZ 2 TO 8 FEET WIDE, AVERAGES 3 TO 4 FEET WIDE. STRIKE OF VEIN QUARTZ N 60 DEG. WEST, DIP VERTICAL. VEINS MAY EXTEND FOR MORE THAN 2500 FEET.