Upper Merryall, New Milford, Litchfield County, Connecticut, USAi
Regional Level Types | |
---|---|
Upper Merryall | Village |
New Milford | Town |
Litchfield County | County |
Connecticut | State |
USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
41° 39' 44'' North , 73° 25' 19'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
New Preston | 1,182 (2017) | 6.0km |
Kent | 2,858 (2017) | 8.3km |
New Milford | 6,523 (2017) | 9.5km |
Washington | 3,466 (2017) | 9.9km |
Sherman | 3,827 (2017) | 11.1km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Danbury Mineralogical Society | Danbury, Connecticut | 30km |
Bristol Gem & Mineral Club | Bristol, Connecticut | 39km |
Mid-Hudson Valley Gem and Mineral Society Inc. | Poughkeepsie, New York | 42km |
Mindat Locality ID:
248929
Long-form identifier:
mindat:1:2:248929:5
GUID (UUID V4):
bba046f0-127d-4d86-9d6d-327a841683a2
No description has been added for this locality. Can you add one?
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
Mineral list contains entries from the region specified including sub-localities19 valid minerals. 1 erroneous literature entry.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Rock list contains entries from the region specified including sub-localities
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Albite Formula: Na(AlSi3O8) Habit: anhedral Colour: white Description: Major component of the pegmatite. |
✪ 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." |
ⓘ Annite Formula: KFe2+3(AlSi3O10)(OH)2 Habit: anhedral Colour: black Description: fka biotite, a minor accessory in the pegmatites. |
ⓘ Bertrandite ? Formula: Be4(Si2O7)(OH)2 Description: Included in the reference in a list of minerals with no supporting information. |
✪ 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. |
✪ 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. |
✪ 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. |
ⓘ Columbite-(Fe) Formula: Fe2+Nb2O6 |
ⓘ 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. |
ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 Description: Probably almandine as is most pegmatitic garnet in Connecticut. |
✪ 'Gummite' Description: Associated with uraninite, meta-autunite, uranophane, other alteration products. Fine gummite and uranophane pseudomorphs after uraninite have been found here. |
ⓘ Hematite ? Formula: Fe2O3 Description: Included in the reference in a list of minerals with no supporting documentation. |
ⓘ 'Limonite' Description: Common surficial alteration product staining other rocks and minerals. |
ⓘ Meta-autunite Formula: Ca(UO2)2(PO4)2 · 6H2O Description: Associated with uraninite, uranophane, "gummite" and other alteration products. |
ⓘ Metatorbernite Formula: Cu(UO2)2(PO4)2 · 8H2O Description: Associated with uraninite, meta-autunite, uranophane, "gummite" and other alteration products. |
ⓘ 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. |
ⓘ 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. |
ⓘ 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. |
ⓘ 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. |
ⓘ Phosphuranylite Formula: KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
ⓘ 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. |
ⓘ Quartz Formula: SiO2 Habit: anhedral Colour: milky to smoky Description: Major component of the pegmatite. |
ⓘ 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. |
ⓘ 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z |
ⓘ Uraninite Formula: UO2 Habit: octahedral Description: Associated with secondaries, sometimes pseudomorphed by uranophane and "gummite". |
✪ 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. |
ⓘ Zircon Formula: Zr(SiO4) Colour: brown Description: Accessory in the pegmatites. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
ⓘ | Hematite ? | 4.CB.05 | Fe2O3 |
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | Opal | 4.DA.10 | SiO2 · nH2O |
ⓘ | var. Opal-AN | 4.DA.10 | SiO2 · nH2O |
ⓘ | Pyrolusite ? | 4.DB.05 | Mn4+O2 |
ⓘ | Columbite-(Fe) | 4.DB.35 | Fe2+Nb2O6 |
ⓘ | Uraninite | 4.DL.05 | UO2 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
ⓘ | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
ⓘ | Metatorbernite | 8.EB.10 | Cu(UO2)2(PO4)2 · 8H2O |
ⓘ | Meta-autunite | 8.EB.10 | Ca(UO2)2(PO4)2 · 6H2O |
ⓘ | Phosphuranylite | 8.EC.10 | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Group 9 - Silicates | |||
ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
ⓘ | Uranophane | 9.AK.15 | Ca(UO2)2(SiO3OH)2 · 5H2O |
ⓘ | Bertrandite ? | 9.BD.05 | Be4(Si2O7)(OH)2 |
ⓘ | Beryl var. Heliodor | 9.CJ.05 | Be3Al2(Si6O18) |
ⓘ | 9.CJ.05 | Be3Al2(Si6O18) | |
ⓘ | var. Aquamarine | 9.CJ.05 | Be3Al2Si6O18 |
ⓘ | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
ⓘ | Annite | 9.EC.20 | KFe2+3(AlSi3O10)(OH)2 |
ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
Unclassified | |||
ⓘ | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
ⓘ | 'Limonite' | - | |
ⓘ | 'Gummite' | - | |
ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
H | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
H | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
H | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
H | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
H | ⓘ Opal | SiO2 · nH2O |
H | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
H | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Be | Beryllium | |
Be | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Be | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
Be | ⓘ Beryl | Be3Al2(Si6O18) |
Be | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
B | Boron | |
B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
B | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | Oxygen | |
O | ⓘ Albite | Na(AlSi3O8) |
O | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
O | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
O | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
O | ⓘ Beryl | Be3Al2(Si6O18) |
O | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
O | ⓘ Fluorapatite | Ca5(PO4)3F |
O | ⓘ Hematite | Fe2O3 |
O | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
O | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
O | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
O | ⓘ Microcline | K(AlSi3O8) |
O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
O | ⓘ Opal | SiO2 · nH2O |
O | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
O | ⓘ Pyrolusite | Mn4+O2 |
O | ⓘ Quartz | SiO2 |
O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
O | ⓘ Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | ⓘ Uraninite | UO2 |
O | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
O | ⓘ Zircon | Zr(SiO4) |
O | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
O | ⓘ Garnet Group | X3Z2(SiO4)3 |
F | Fluorine | |
F | ⓘ Fluorapatite | Ca5(PO4)3F |
Na | Sodium | |
Na | ⓘ Albite | Na(AlSi3O8) |
Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | Aluminium | |
Al | ⓘ Albite | Na(AlSi3O8) |
Al | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Al | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Al | ⓘ Beryl | Be3Al2(Si6O18) |
Al | ⓘ Microcline | K(AlSi3O8) |
Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
Si | Silicon | |
Si | ⓘ Albite | Na(AlSi3O8) |
Si | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Si | ⓘ Beryl var. Aquamarine | Be3Al2Si6O18 |
Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Si | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
Si | ⓘ Beryl | Be3Al2(Si6O18) |
Si | ⓘ Opal var. Opal-AN | SiO2 · nH2O |
Si | ⓘ Microcline | K(AlSi3O8) |
Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | ⓘ Opal | SiO2 · nH2O |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Si | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Si | ⓘ Zircon | Zr(SiO4) |
Si | ⓘ Beryl var. Heliodor | Be3Al2(Si6O18) |
Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
P | Phosphorus | |
P | ⓘ Fluorapatite | Ca5(PO4)3F |
P | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
P | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
P | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
K | Potassium | |
K | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
K | ⓘ Microcline | K(AlSi3O8) |
K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
K | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Ca | Calcium | |
Ca | ⓘ Fluorapatite | Ca5(PO4)3F |
Ca | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
Ca | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Ca | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Mn | Manganese | |
Mn | ⓘ Pyrolusite | Mn4+O2 |
Fe | Iron | |
Fe | ⓘ Annite | KFe32+(AlSi3O10)(OH)2 |
Fe | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Fe | ⓘ Columbite-(Fe) | Fe2+Nb2O6 |
Fe | ⓘ Hematite | Fe2O3 |
Fe | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
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 | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
U | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
U | ⓘ Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
U | ⓘ Uraninite | UO2 |
U | ⓘ Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Localities in this Region
- Connecticut
- Litchfield County
- New Milford
- Litchfield County
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Laurentides DomainDomain
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.