Clove Spring Limonite Mine
Beekman, New York
41.6755°N 73.6834°W
41.6755°N 73.6834°W
The Clove Spring Limonite Mine is near Beekman, New York. Historically the site has been associated with the Fishkill Belt Mining District which is now part of the Appalachian National Scenic Trail. The site was first discovered in 1850. The Clove Spring Limonite Mine was closed at the time of data entry with no known plans to re-open. Mine operations consist of surface workings extending 1.58 hectares (3.90 acres). There is one known shaft. The ore mined is composed of limonite. The ore body takes a sheet-like form 274 meters (900 feet) long, 60 meters (200 feet) wide, and 39 meters (129 feet) thick. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
Additional textual information about a site or mine.
DISCOVERY YEAR: 1800'S
DEPOSIT OCCURS IN OVERTHRUST FAULT ZONE.
USGS TOPO, 1960, VERBANK, 1:24, 000, SHOWS MINE PIT AS POND; INFORMATION SOURCE: 1 PUB LIT.
EARLY IRON MANUFACTURING AND MINING AREA, 1734-1900; IRON ORE USED LOCALLY.
Workings at the site.
ORE MIXED WITH GLACIAL MATERIAL AND MASSES OF FRESH CARBONATE BEDROCK.
Processes that concentrated or enriched the mineralization of the mine.
SIDERITE AND PYRITE BEDS NOT REPORTED; CARBONATE BED; NEAR CONTACT WITH OVERTHRUST FAULT OF MID ORDOVICIAN BERKSHIRE PHYLLITE AND SCHIST FORMATION; GREY LIMESTONE BEDS CUT BY PIT WALLS.; MINE PIT WALLS LIMESTONE; ON GEOLOGIC MAP PIT IN FAULT ZONE NEAR BERKSHIRE SCHISTS.
Characteristics of the ore body.
Geologic structural features affecting or characterizing the site or mine.
Physiographic area where the resource is found.
Mineralogical and chemical alteration at or near the site, which may help to indicate the geographic extent of the geological processes producing the mine.
Controls on emplacement of ore such as faults or other structural features.
NO FIGURES AVAILABLE BUT PROBABLY LARGE AMOUNT OF LOW GRADE ORE IS PRESENT.
NO FIGURES AVAILABLE, BUT LOW GRADE IRON ORE PROBABLY AVAILABLE IN LARGE QUANTITIES ALONG FAULT ZONE CONTINUATIONS.
NO FIGURES AVAILABLE, ESTIMATED LARGE AMOUNTS OF LOW GRADE IRON ORE PRESENT.
Other deposits in the same region.
Clove Spring Limonite Mine
Clove Spring Limonite Mine
Clove Iron Mine
Clove Limonite Mine
Unnamed Limonite Mine
Unnamed Iron Mine
Unnamed Limonite Mine
Foss Ore Bed White Iron Mine Dover Mine
Dover Iron Mine
Unnamed Limonite 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
TOPO SHOWS POND 900 FEET LONG NE-SW, 200 FEET WIDE EAST-WEST, AND REPORTED 130 FEET DEEP; MINE PIT 500 FEET NORTH OF CLOVE MINE PIT. ORE COMPACT, MUST BE BLASTED; OVERLAIN BY GLACIAL MATERIAL; LIMESTONE BEDROCK PRESENT. MANGANESE AND ZINC ARE PROBABLY PRESENT BUT NOT TESTED FOR.