Paddock mine, Lyman, Grafton County, New Hampshire, USAi
Regional Level Types | |
---|---|
Paddock mine | Mine |
Lyman | Township |
Grafton County | County |
New Hampshire | State |
USA | Country |
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Latitude & Longitude (WGS84):
44° 16' 45'' North , 71° 58' 2'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Barnet | 129 (2017) | 6.8km |
Monroe | 808 (2017) | 7.3km |
Lisbon | 980 (2017) | 8.6km |
Bath | 951 (2017) | 12.5km |
Sugar Hill | 600 (2017) | 15.1km |
Mindat Locality ID:
6104
Long-form identifier:
mindat:1:2:6104:2
GUID (UUID V4):
194acda5-3a9e-44ef-9da1-e862ff7b2894
Other/historical names associated with this locality:
Oro, Osgood, Osborn, New Hampshire Silver Lead Co.
Paddock Company. This is the largest of all the copper companies, embracing partly in fee simple the entire land and partly the mineral rights upon four of the original lots of the town of Lyman, and therefore supposed to contain 1200 acres. The course of the veins is more than three miles in length, reaching from the Titus farm upon the south to an unoccupied tract called on our map the Penhallow lot. J. H. Paddock, Esq.. of St. Johnsbury, Vt., is the principal proprietor, and the manager of the mine and mill. He has brought together several of the tracts known ten years ago as the Oro, Osgood, Osborn, New Hampshire Silver Lead Co., etc. What were formerly the Oro and Osgood openings are now the No. 1 and No. 2 shafts of the Paddock mine. Concerning these two mines, I wrote as follows in 1869:
βThe next is called the Osgood mine, embracing about 700 acres of the land on the east slope of Gardner's mountain. I examined four or five openings. The first, near the south line, was ten feet deep, exhibiting five feet width of copper schists. The second shows a width of ten feet of copper schists. The third is a shaft thirty-five feet deep. Eighty feet below is a short tunnel eighty feet long, and designed to cut the vein. A large pile of good specimens of this copper may be seen near the shaft.
βThe next north is the Oro mine. Here is a shaft sixty-five feet deep, a shaft house, easily seen from a great distance on account of its conspicuous position, two drifts fourteen and sixteen feet long, and a vein from four to seven feet wide, carrying more ore near the hanging than the foot wall. Sixty tons, part yielding 10.80, and part 9.+ per cent of copper, have been shipped from the mine to Boston. There are one hundred and seventy-five acres of land connected with this property, and the vein is eighty-eight rods long."
βThe next is called the Osgood mine, embracing about 700 acres of the land on the east slope of Gardner's mountain. I examined four or five openings. The first, near the south line, was ten feet deep, exhibiting five feet width of copper schists. The second shows a width of ten feet of copper schists. The third is a shaft thirty-five feet deep. Eighty feet below is a short tunnel eighty feet long, and designed to cut the vein. A large pile of good specimens of this copper may be seen near the shaft.
βThe next north is the Oro mine. Here is a shaft sixty-five feet deep, a shaft house, easily seen from a great distance on account of its conspicuous position, two drifts fourteen and sixteen feet long, and a vein from four to seven feet wide, carrying more ore near the hanging than the foot wall. Sixty tons, part yielding 10.80, and part 9.+ per cent of copper, have been shipped from the mine to Boston. There are one hundred and seventy-five acres of land connected with this property, and the vein is eighty-eight rods long."
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
10 valid minerals.
Detailed Mineral List:
β Ankerite Formula: Ca(Fe2+,Mg)(CO3)2 |
β 'Biotite' ? Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
β Chalcopyrite Formula: CuFeS2 |
β 'Chlorite Group' ? |
β Galena Formula: PbS |
β Galena var. Silver-bearing Galena Formula: PbS with Ag |
β Linarite ? Formula: PbCu(SO4)(OH)2 |
β Microcline Formula: K(AlSi3O8) |
β Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
β 'Plagioclase' ? Formula: (Na,Ca)[(Si,Al)AlSi2]O8 |
β Pyrite Formula: FeS2 |
β Pyrrhotite Formula: Fe1-xS |
β Quartz Formula: SiO2 |
β Sphalerite Formula: ZnS |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Sphalerite | 2.CB.05a | ZnS |
β | Chalcopyrite | 2.CB.10a | CuFeS2 |
β | Pyrrhotite | 2.CC.10 | Fe1-xS |
β | Galena | 2.CD.10 | PbS |
β | var. Silver-bearing Galena | 2.CD.10 | PbS with Ag |
β | Pyrite | 2.EB.05a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
β | Quartz | 4.DA.05 | SiO2 |
Group 5 - Nitrates and Carbonates | |||
β | Ankerite | 5.AB.10 | Ca(Fe2+,Mg)(CO3)2 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
β | Linarite ? | 7.BC.65 | PbCu(SO4)(OH)2 |
Group 9 - Silicates | |||
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | Microcline | 9.FA.30 | K(AlSi3O8) |
Unclassified | |||
β | 'Biotite' ? | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
β | 'Chlorite Group' ? | - | |
β | 'Plagioclase' ? | - | (Na,Ca)[(Si,Al)AlSi2]O8 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
H | β Linarite | PbCu(SO4)(OH)2 |
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
C | Carbon | |
C | β Ankerite | Ca(Fe2+,Mg)(CO3)2 |
O | Oxygen | |
O | β Ankerite | Ca(Fe2+,Mg)(CO3)2 |
O | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
O | β Linarite | PbCu(SO4)(OH)2 |
O | β Microcline | K(AlSi3O8) |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Quartz | SiO2 |
O | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
F | Fluorine | |
F | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Na | Sodium | |
Na | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Mg | Magnesium | |
Mg | β Ankerite | Ca(Fe2+,Mg)(CO3)2 |
Mg | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Al | Aluminium | |
Al | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Al | β Microcline | K(AlSi3O8) |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Si | Silicon | |
Si | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Si | β Microcline | K(AlSi3O8) |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Quartz | SiO2 |
Si | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
S | Sulfur | |
S | β Chalcopyrite | CuFeS2 |
S | β Galena | PbS |
S | β Linarite | PbCu(SO4)(OH)2 |
S | β Pyrite | FeS2 |
S | β Pyrrhotite | Fe1-xS |
S | β Sphalerite | ZnS |
S | β Galena var. Silver-bearing Galena | PbS with Ag |
K | Potassium | |
K | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
K | β Microcline | K(AlSi3O8) |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Ca | Calcium | |
Ca | β Ankerite | Ca(Fe2+,Mg)(CO3)2 |
Ca | β Plagioclase | (Na,Ca)[(Si,Al)AlSi2]O8 |
Ti | Titanium | |
Ti | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Fe | Iron | |
Fe | β Ankerite | Ca(Fe2+,Mg)(CO3)2 |
Fe | β Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Fe | β Chalcopyrite | CuFeS2 |
Fe | β Pyrite | FeS2 |
Fe | β Pyrrhotite | Fe1-xS |
Cu | Copper | |
Cu | β Chalcopyrite | CuFeS2 |
Cu | β Linarite | PbCu(SO4)(OH)2 |
Zn | Zinc | |
Zn | β Sphalerite | ZnS |
Ag | Silver | |
Ag | β Galena var. Silver-bearing Galena | PbS with Ag |
Pb | Lead | |
Pb | β Galena | PbS |
Pb | β Linarite | PbCu(SO4)(OH)2 |
Pb | β Galena var. Silver-bearing Galena | PbS with Ag |
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Ganderia DomainDomain
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