Sylvan Lake Limonite Mine
Beekman, New York
41.6036°N 73.7426°W
41.6036°N 73.7426°W
The Sylvan Lake 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 1825 by An Unknown Prospector. The Sylvan Lake Limonite Mine was closed at the time of data entry with no known plans to re-open. Past operations took place from 1882. Mine operations consist of surface workings extending 1.10 hectares (2.71 acres). There is one known shaft. The ore mined is composed of limonite. The ore body is described as tabular shaped 152 meters (500 feet) long, 76 meters (250 feet) wide, and 18 meters (60 feet) thick. The New England Upland Section of the Appalachian Highlands characterize the geomorphology of the surrounding area.
Site identification and general characteristics. Learn about USGS mines.
Additional textual information about a site or mine.
DUE NORTH EXTENSION OF TOWER FISHKILL MINE PIT. THE THICKNESS OF THE DEPOSIT RANGES FROM 50-60 FEET
USGS TOPO, 1960, POUGHQUAG, 1:24, 000, MAP SYMBOL AS POND. LIMONITE ORE ON SURFACE AND OVERLAIN BY AS MUCH AS 30 FEET OF GLACIAL DRIFT; BEDROCK NOT ENCOUNTERED; INFORMATION SOURCE: 1 PUB LIT.
DISCOVERY YEAR: EARLY 1800'S
EARLY IRON PRODUCING DISTRICT, 1734-1900; LOCAL IRON MARKET.
Workings at the site.
MINING SERIOUSLY HAMPERED BY WATER INFLOW.
Processes that concentrated or enriched the mineralization of the mine.
BEDROCK NOT ENCOUNTERED; CARBONATE; DEEPLY WEATHERED FAULT ZONE; DEEP MASS WEATHERING OF FRACTURE ZONE.
Characteristics of the ore body.
Geologic structural features affecting or characterizing the site or mine.
Tectonic setting in which the site or deposit is situated.
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, PROBABLY MODERATE LOW GRADE ORE RESERVES.
NO FIGURES AVAILABLE, PROBABLY MODERATE LOW GRADE ORE RESOURCES.
PROBABLY LOW GRADE ORE REMAINS, DRAINAGE A PROBLEM.
Other deposits in the same region.
Tower Fishkill Limonite Mine
Old Fishkill Limonite Mine
Sylvan Lake Limonite Mine
Fishkill Iron Mine
Sylvan Lake Limonite Mine
Unnamed Limonite Prospect
Horton Limonite Mine
Beekman Limonite Mine
Horton Iron Mines
Beekman Iron 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
PIT IS NORTHERN PART OF POND; THE SOUTHERN TWO-THIRDS OF POND BEING THE PIT OF THE LARGER TOWER FISHKILL LIMONITE MINE (HARTFORD 2 DEG. SHEET, NO. 32 ). SYLVAN LAKE POND ON TOPO SHEET EXTENDS DUE NORTH; LENGTH 500 FEET, WIDTH 250 FEET, ABOUT 90 FEET DEEP. PROBABLY MANGANESE AND ZINC PRESENT BUT NOT STUDIED OR TESTED.