Gillette Quarry Mine
Haddam, Connecticut
41.4924°N 72.5114°W
41.4924°N 72.5114°W
The Gillette Quarry Mine is near Haddam, Connecticut. Historically the site has been part of the East Haddam Mining District. The Gillette Quarry Mine was closed at the time of data entry with no known plans to re-open. Documentation from 1982 describes a single ore body as having a lenticular or lens shaped form reaching 107 meters (351 feet) long and 61 meters (200 feet) wide. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
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** 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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Deposit
RECORDS 800-824 OF 1975 ENTRY RECORD 700/ REC. 070-072 RECORD 701/ GENERAL INFO FOR ALL RECORDS RECORD 702/ TIN INFORMATION RECORD 703/ REC. 070-072 RECORD 704/ GENERAL INFO FOR ALL RECORDS. RECORD 040/ DEPOSIT IS ABOUT 10 MILES SOUTHEAST OF MIDDLETOW MAX. SUR. AREA DISTURBED WAS ROUGHLY MEASURED OFF A MAP BY C ET. AL. (REC. 704) RECORD 050/ E. N CAMERON ET. AL. EXAMINED AND MAPPED THE MINE. REC 060/PEG INTRUDED INTERBEDDED QTZ-MICA SCHISTS, MICA-QTZI CALC-SILICATE GNEISS, AND MARBLE OF THE BOLTON SCHIST REC 070/ MINERALOGY OF THE PEGMATITE. REC 080/ CASSITERITE IS MENTIONED AS OCCURRING IN PEG BUT IN CONCERNING ITS CHARACTER IS UNAVAILABLE. MANY GEM AND MIN SP OCCUR IN POCKETS 8-10 IN. IN DIA. IRREGULARLY DISTRIBUTED TH PEG. GEM MINERALS WERE MORE EXTENSIVELY MINED IN THE WESTERN OF THE DEPOSIT DEP. CONSISTS OF INTERCONNECTED, LENTICULAR PEG BODIES 15-80 THICK WHICH ARE GEN. ORIENTED ALONG FOLIATION OF COUNTRY ROC ING N 35 W AND DIPPING STEEPLY EAST. THE PEG WALLS HAVE IRRE ROLLS AND KEELS BUT CONTACT WITH HOST ROCK IS SHARP. PEG IS AND CAVITIES ARE NOTED PARTICULARLY IN QTZ-PERTHITE ZONE SAND AND GRAVEL OVERBURDEN UP TO 10 FEET THICK MIN. ZONE DIMENTIONS FROM MAP AND X-SECTIONS IN REC 701.