New Milford, Litchfield County, Connecticut, USAi
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New Milford | Town |
Litchfield County | County |
Connecticut | State |
USA | Country |
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Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities26 valid minerals. 1 erroneous literature entry.
Rock Types Recorded
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Rock list contains entries from the region specified including sub-localities
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Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Albite Formula: Na(AlSi3O8) Habit: anhedral Colour: white Description: Major component of the pegmatite. Reference: Januzzi, 1976. Mineral Localities of CT and Southeastern NY State; USGS Prof Paper 255; Rocks & Minerals (1995) 70:396-409 |
✪ Almandine Formula: Fe2+3Al2(SiO4)3 Habit: trapezohedral and rhombic dodecahedral Colour: maroon to nearly black Description: An accessory in the pegmatites, also abundant subhedral metacrysts of garnet in the schist adjacent to the contacts with pegmatite. Januzzi (1959) reports finding in one isolated pegmatite mass, scores of two types of garnet crystals having both distinct dodecahedral and trapezohedral forms. Ewell (1937) writes: "The garnets were extra large, some weighing one pound each." Reference: Van King; USGS Prof Paper 255; Januzzi (1959); Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1. |
ⓘ Annite Formula: KFe2+3(AlSi3O10)(OH)2 Habit: anhedral Colour: black Description: fka biotite, a minor accessory in the pegmatites. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State; Cameron et al (1954): USGS Prof Paper 255 |
ⓘ Bertrandite ? Formula: Be4(Si2O7)(OH)2 Description: Included in the reference in a list of minerals with no supporting information. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
✪ Beryl Formula: Be3Al2(Si6O18) Habit: anhedral elongated prisms Colour: pale green, yellow to honey, blue Description: According to Cameron et al (1954), beryl is concentrated in the quartz-perthitic microcline zone in the the southwest half of no. 1 quarry as pale greenish-white, short, subhedral prisms, 3 inches in average length and 2 inches in average diameter. A 300-pound block of quartz and plagioclase found in the backfill contains at least 8 percent beryl. Also an accessory of the pegmatites in the no. 2 quarry. Sterrett (1923) reports “many crystals of beryl, some of them more than a foot in diameter”. Crystals are usually sheathed in mica and are poorly formed but internally contain some of the best gem beryl rough found in Connecticut. Reference: Januzzi, 1976. Mineral Localities of CT and Southeastern NY State; USGS Prof Paper 255; Rocks & Minerals (1995) 70:396-409; Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1. |
✪ Beryl var. Aquamarine Formula: Be3Al2Si6O18 Habit: subhedral elongated prisms Colour: blue, blue-green Description: Much more rare than the common green beryl or yellow beryl, but a 40.44-carat aquamarine (no. 1037) is in the Smithsonian. Reference: Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1.; Rocks & Minerals (1995) 70:396-409 |
✪ Beryl var. Heliodor Formula: Be3Al2(Si6O18) Colour: yellow to honey Description: Crystals poorly formed, but internally hide some of the best gem rough from Connecticut, with deep golden yellow to honey color. Reference: Rocks & Min.: 70:379; Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1. |
ⓘ Calcite Formula: CaCO3 Reference: Weber, Marcelle H. and Earle C. Sullivan. (1995), Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue), 70(6): 398. |
ⓘ Chondrodite Formula: Mg5(SiO4)2F2 Habit: granular Colour: light brown Fluorescence: light yellow under SW UV Reference: Weber, Marcelle H. and Earle C. Sullivan. (1995), Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue), 70(6): 398. |
ⓘ Columbite-(Fe) Formula: Fe2+Nb2O6 Reference: Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1. |
✪ Diopside Formula: CaMgSi2O6 Habit: flattened short to elongated prisms Colour: white to very pale green Fluorescence: light blue-gray under SW Description: pseudomorphed by tremolite (originally called Canaanite) Reference: Harold Moritz collection |
ⓘ Fluorapatite Formula: Ca5(PO4)3F Description: Included in just a list of minerals in one reference, but it is such a common accessory that it is certainly present. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 Description: Probably almandine as is most pegmatitic garnet in Connecticut. Reference: Ryerson, Kathleen H. (1972) Rock Hounds Guide to Connecticut |
✪ 'Gummite' Description: Associated with uraninite, meta-autunite, uranophane, other alteration products. Fine gummite and uranophane pseudomorphs after uraninite have been found here. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Hematite ? Formula: Fe2O3 Description: Included in the reference in a list of minerals with no supporting documentation. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ 'Limonite' Description: Common surficial alteration product staining other rocks and minerals. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Meta-autunite Formula: Ca(UO2)2(PO4)2 · 6H2O Description: Associated with uraninite, uranophane, "gummite" and other alteration products. Reference: Januzzi (1959); Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1. |
ⓘ Metatorbernite Formula: Cu(UO2)2(PO4)2 · 8H2O Description: Associated with uraninite, meta-autunite, uranophane, "gummite" and other alteration products. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Microcline Formula: K(AlSi3O8) Habit: anhedral Description: A major component of the pegmatites. In the perthitic microcline-quartz zone of the No.1 quarry, in large anhedral crystals as much as 10 feet long. In the eastern part of the north wall, the zone is richest in massive perthitic microcline toward the center of the pegmatite, and this suggests the presence of a perthitic microcline core. Locally, the microcline is veined and partly replaced with granular milky quartz, deformed muscovite and pink-red garnet. Graphic granite is fairly common. Reference: Cameron and other (1954): Pegmatite Investigations New England. USGS Prof. Paper 255. |
ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 Habit: tabular subhedral Colour: green to pale ruby Description: In the microcline-quartz zone of the no. 1 quarry it occurs in small quantities as books 3 inches in diameter. The muscovite-microcline unit of this pegmatite consists chiefly of diversely oriented scrap muscovite books forming 70 to 90 percent of the total volume. One block of “solid mica” of irregular shape blasted loose from this zone measured 4 feet thick and 8 feet long. http://www.mindat.org/photo-204409.html
Crystals average 1 inch in diameter but range from 1/8 to 6 inches across. There are three types of mica deposits in the 4 pegmatites of the no. 2 quarry: pod, wall-zone, and disseminated. Pegmatite A has a concentration of books as much as 1 foot in diameter, Pegmatite B exhibits a lean book mica-bearing zone composed of quartz, albite, and muscovite. The books are 3 to 4 inches in average diameter. Pegmatites C and D are disseminated mica deposits. Reference: Januzzi, 1976. Mineral Localities of CT and Southeastern NY State; USGS Prof Paper 255, Sterrett (1923) |
ⓘ Opal Formula: SiO2 · nH2O Habit: encrustations Fluorescence: green Description: Commonly forms crusts in cracks and joints in pegmatites, best found by its bright green fluorescence under SW UV illumination. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Opal var. Opal-AN Formula: SiO2 · nH2O Habit: encrustations Fluorescence: green Description: Commonly forms crusts in cracks and joints in pegmatites, best found by its bright green fluorescence under SW UV illumination. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Phlogopite Formula: KMg3(AlSi3O10)(OH)2 Habit: granular Colour: brown Fluorescence: pale yellow-brown under SW UV Reference: Weber, Marcelle H. and Earle C. Sullivan. (1995), Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue), 70(6): 398. |
ⓘ Phosphuranylite Formula: KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
ⓘ Pyrite Formula: FeS2 Habit: granular to cuboctahderal Description: good crystals can reach 5-6 cm Reference: Field observations |
ⓘ Formula: Mn4+O2 Locality: New England Mining Company Quarry (Roebling Mine; Hewitt's Mine), Upper Merryall, New Milford, Litchfield County, Connecticut, USA - erroneously reported Description: No pyrolusite dendrite or staining in a granite pegmatite in the world has been verified as pyrolusite. The name was a mistake in the nineteenth century which has been widely publicized. Reference: Januzzi, 1976. Mineral Localities of CT and Southeastern NY State |
ⓘ Quartz Formula: SiO2 Localities: Reference: Samuel Robinson (1825) A Catalogue of American Minerals, with their localities. Boston |
ⓘ 'Scapolite' Reference: Weber, Marcelle H. and Earle C. Sullivan. (1995), Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue), 70(6): 398. |
ⓘ Schorl Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) Habit: subhedral, elongated prisms Colour: black Description: Common accessory in the pegmatites, especially in the border zone forming subhedral needles from ¼ inch to 3 inches long, oriented normal to the contact, and in the surrounding schist. Reference: Januzzi, (1976): Mineral Localities of CT and Southeastern NY State; |
ⓘ Siderite Formula: FeCO3 Reference: Samuel Robinson (1825) A Catalogue of American Minerals, with their localities. Boston |
ⓘ 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z Reference: Elwell, Wilbur. (1937): Some Old Localities in Connecticut. Rocks and Minerals, vol 12, no. 9, pp. 270-1.; USGS Prof Paper 255 |
✪ Tremolite Formula: ◻{Ca2}{Mg5}(Si8O22)(OH)2 Habit: Primary - bladed, pseudomorphs after diopside are flattened short to elongated prisms Colour: white, pale gray, pale green Fluorescence: light blue-gray under SW Description: as primary crystal or as pseudomorphs after diopside (originally called canaanite) Reference: Weber, Marcelle H. and Earle C. Sullivan. (1995), Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue), 70(6): 398. |
ⓘ Uraninite Formula: UO2 Habit: octahedral Description: Associated with secondaries, sometimes pseudomorphed by uranophane and "gummite". Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State; Rocks & Minerals (1995) 70:396-409 |
✪ Uranophane Formula: Ca(UO2)2(SiO3OH)2 · 5H2O Description: Associated with uraninite, meta-autunite, "gummite", other alteration products. Fine gummite and uranophane pseudomorphs after uraninite have been found here. Reference: Januzzi (1976): Mineral Localities of CT and Southeastern NY State |
ⓘ Zircon Formula: Zr(SiO4) Colour: brown Description: Accessory in the pegmatites. Reference: Fred E Davis collection |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Pyrite | 2.EB.05a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Columbite-(Fe) | 4.DB.35 | Fe2+Nb2O6 |
ⓘ | Hematite ? | 4.CB.05 | Fe2O3 |
ⓘ | Opal | 4.DA.10 | SiO2 · nH2O |
ⓘ | var. Opal-AN | 4.DA.10 | SiO2 · nH2O |
ⓘ | Pyrolusite ? | 4.DB.05 | Mn4+O2 |
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | Uraninite | 4.DL.05 | UO2 |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Calcite | 5.AB.05 | CaCO3 |
ⓘ | Siderite | 5.AB.05 | FeCO3 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
ⓘ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
ⓘ | Meta-autunite | 8.EB.10 | Ca(UO2)2(PO4)2 · 6H2O |
ⓘ | Metatorbernite | 8.EB.10 | Cu(UO2)2(PO4)2 · 8H2O |
ⓘ | Phosphuranylite | 8.EC.10 | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Group 9 - Silicates | |||
ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
ⓘ | Annite | 9.EC.20 | KFe2+3(AlSi3O10)(OH)2 |
ⓘ | Bertrandite ? | 9.BD.05 | Be4(Si2O7)(OH)2 |
ⓘ | Beryl | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | var. Aquamarine | 9.CJ.05 | Be3Al2Si6O18 |
ⓘ | var. Heliodor | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | Chondrodite | 9.AF.45 | Mg5(SiO4)2F2 |
ⓘ | Diopside | 9.DA.15 | CaMgSi2O6 |
ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
ⓘ | Phlogopite | 9.EC.20 | KMg3(AlSi3O10)(OH)2 |
ⓘ | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
ⓘ | Tremolite | 9.DE.10 | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
ⓘ | Uranophane | 9.AK.15 | Ca(UO2)2(SiO3OH)2 · 5H2O |
ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
Unclassified Minerals, Rocks, etc. | |||
ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
ⓘ | 'Gummite' | - | |
ⓘ | 'Limonite' | - | |
ⓘ | 'Scapolite' | - | |
ⓘ | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Tremolite | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
H | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
H | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
H | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
H | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
H | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
H | ⓘ Opal | SiO2 · nH2O |
H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
H | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
H | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
H | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
Be | Beryllium | |
Be | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Be | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
Be | ⓘ Beryl | Be3Al2(Si6O18) |
Be | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
B | Boron | |
B | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
C | Carbon | |
C | ⓘ Calcite | CaCO3 |
C | ⓘ Siderite | FeCO3 |
O | Oxygen | |
O | ⓘ Tremolite | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
O | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
O | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
O | ⓘ Beryl | Be3Al2(Si6O18) |
O | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
O | ⓘ Diopside | CaMgSi2O6 |
O | ⓘ Calcite | CaCO3 |
O | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
O | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | ⓘ Fluorapatite | Ca5(PO4)3F |
O | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
O | ⓘ Uraninite | UO2 |
O | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
O | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
O | ⓘ Quartz | SiO2 |
O | ⓘ Siderite | FeCO3 |
O | ⓘ Garnet Group | X3Z2(SiO4)3 |
O | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
O | ⓘ Zircon | Zr(SiO4) |
O | ⓘ Opal | SiO2 · nH2O |
O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
O | ⓘ Chondrodite | Mg5(SiO4)2F2 |
O | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
O | ⓘ Albite | Na(AlSi3O8) |
O | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
O | ⓘ Microcline | K(AlSi3O8) |
O | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
O | ⓘ Hematite | Fe2O3 |
O | ⓘ Pyrolusite | Mn4+O2 |
F | Fluorine | |
F | ⓘ Fluorapatite | Ca5(PO4)3F |
F | ⓘ Chondrodite | Mg5(SiO4)2F2 |
Na | Sodium | |
Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Na | ⓘ Albite | Na(AlSi3O8) |
Mg | Magnesium | |
Mg | ⓘ Tremolite | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
Mg | ⓘ Diopside | CaMgSi2O6 |
Mg | ⓘ Chondrodite | Mg5(SiO4)2F2 |
Mg | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
Al | Aluminium | |
Al | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Al | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
Al | ⓘ Beryl | Be3Al2(Si6O18) |
Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
Al | ⓘ Albite | Na(AlSi3O8) |
Al | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Al | ⓘ Microcline | K(AlSi3O8) |
Si | Silicon | |
Si | ⓘ Tremolite | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
Si | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Si | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
Si | ⓘ Beryl | Be3Al2(Si6O18) |
Si | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Si | ⓘ Diopside | CaMgSi2O6 |
Si | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
Si | ⓘ Zircon | Zr(SiO4) |
Si | ⓘ Opal | SiO2 · nH2O |
Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Si | ⓘ Chondrodite | Mg5(SiO4)2F2 |
Si | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
Si | ⓘ Albite | Na(AlSi3O8) |
Si | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Si | ⓘ Microcline | K(AlSi3O8) |
Si | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
P | Phosphorus | |
P | ⓘ Fluorapatite | Ca5(PO4)3F |
P | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
P | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
P | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
S | Sulfur | |
S | ⓘ Pyrite | FeS2 |
K | Potassium | |
K | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
K | ⓘ Phlogopite | KMg3(AlSi3O10)(OH)2 |
K | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
K | ⓘ Microcline | K(AlSi3O8) |
Ca | Calcium | |
Ca | ⓘ Tremolite | ◻{Ca2}{Mg5}(Si8O22)(OH)2 |
Ca | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Ca | ⓘ Diopside | CaMgSi2O6 |
Ca | ⓘ Calcite | CaCO3 |
Ca | ⓘ Fluorapatite | Ca5(PO4)3F |
Ca | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Ca | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
Mn | Manganese | |
Mn | ⓘ Pyrolusite | Mn4+O2 |
Fe | Iron | |
Fe | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Fe | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
Fe | ⓘ Siderite | FeCO3 |
Fe | ⓘ Pyrite | FeS2 |
Fe | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Fe | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Fe | ⓘ Hematite | Fe2O3 |
Cu | Copper | |
Cu | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
Zr | Zirconium | |
Zr | ⓘ Zircon | Zr(SiO4) |
Nb | Niobium | |
Nb | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
U | Uranium | |
U | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
U | ⓘ Uraninite | UO2 |
U | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
U | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
U | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
Fossils
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Wikipedia: | https://en.wikipedia.org/wiki/New_Milford,_Connecticut |
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Wikidata ID: | Q977989 |
GeoNames ID: | 4839435 |
Localities in this Region
- Connecticut
- Litchfield County
Other Regions, Features and Areas that Intersect
North America PlateTectonic Plate
- Laurentides DomainDomain
- Piedmontia DomainDomain
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New England Mining Company Quarry, Upper Merryall, New Milford, Litchfield County, Connecticut, USA