Amenia Limonite Mine
Amenia, New York
41.8527°N 73.5603°W
41.8527°N 73.5603°W
The Amenia Limonite Mine is in Amenia, New York. Historically the site has been part of the New York Salisbury Iron Mining District. The site was first discovered in 1825 by An Unknown Prospector. The Amenia Limonite Mine was closed at the time of data entry with no known plans to re-open. Mine operations consist of surface workings extending 3.72 hectares (9.18 acres). There is one known shaft. The ore mined is composed of limonite and siderite. The ore body is described as tabular shaped 762 meters (2,500 feet) long, 121 meters (400 feet) wide, and 35 meters (114 feet) thick. The Taconic 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.
COMPOSED OF GRIDLEY, PALMER AN WEED PITS.
USGS TOPO, 1958, AMENIA, 1:24, 000, MAP SHOWS PITS AS PONDS. HOBB'S SKETCH MINE MAP SHOWS FAULT.; INFORMATION SOURCE: 1 PUB LIT.
DISCOVERY YEAR: EARLY 1800'S
Formal or informal mining district names.
MAJOR IRON PRODUCING DISTRICT 1735 TO 1900, IRON ORE USED LOCALLY, GOOD MANGANESE IRON.
Workings at the site.
SURFACE AREA OF 4 PITS
Processes that concentrated or enriched the mineralization of the mine.
SIDERITE MINED AS IRON ORE; IRON BEARING CARBONATES AND SCHISTS; MINE PIT AT CONTACT OF MID ORDOVICIAN BERKSHIRE PHYLLITE AND SCHIST FORMATION; LIMESTONE UNDERLIES MINE PIT, EAST WALL FORMED OF SCHIST OVERLYING LIMESTONE (SMOCK, 1889 ); IRON DEPOSITS BOTTOM IN CARBONATE BEDS ADJACENT TO SCHIST BEDS.
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 AMOUNTS OF LOW GRADE IRON ORE IS PRESENT.
NO FIGURES AVAILABLE BUT PROBABLY LARGE AMOUNTS OF LOW GRADE IRON ORE PRESENT IN AREA.
NO FIGURES AVAILABLE; PROBABLY LARGE AMOUNTS OF LOW GRADE ORE REMAIN.
Other deposits in the same region.
Amenia Manganese Mine
Gridley Iron Mine
Squabble Hole Limonite Mine
Gridley Limonite Mine
General Bush Copper Mine
Squabble Hole Limonite Mine
Manhattan Iron Mine
Manhattan Sharon Limonite Mine
Manhattan Sharon Limonite Mine
Smithfield Lead 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 TWO SMALL PONDS AND ONE LARGE POND, THE NORTHERN PART OF WHICH IS THE PALMER PIT OF THE AMENIA MINE, AND THE SMALLER SOUTHERN PART IS THE GRIDLEY MINE PIT (HARTFORD SHEET, NO. 54 ). THE PALMER PIT IS 700 FEET LONG NORTH-SOUTH, 200 FEET WIDE EAST-WEST, AND 115 FEET DEEP. OF THE TWO SMALL PONDS ARE THE WEED MINE WORKINGS. EACH PIT IS ABOUT 400 FEET LONG NORTH-SOUTH, 150 FEET WIDE EAST-WEST, AND ABOUT 20 FEET DEEP.