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Pegmatite quarry and ultramafic rock, Harwinton, Litchfield County, Connecticut, USAi
Regional Level Types
Pegmatite quarry and ultramafic rockQuarry
Harwinton- not defined -
Litchfield CountyCounty
ConnecticutState
USACountry

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Latitude & Longitude (WGS84):
41° 45' 58'' North , 73° 5' 12'' West
Latitude & Longitude (decimal):
Locality type:
Nearest Settlements:
PlacePopulationDistance
Northwest Harwinton3,252 (2017)1.3km
Torrington34,906 (2017)4.8km
West Torrington36,000 (2017)7.5km
Litchfield1,215 (2017)8.7km
Thomaston1,910 (2017)10.3km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Bristol Gem & Mineral ClubBristol, Connecticut16km
Lapidary and Mineral Society of Central ConnecticutMeriden, Connecticut34km


A small quarry in a granite pegmatite (Nonewaug granite outlier) along the power line right-of-way just south of state Route 118 and west of Hill Road. Nothing has apparently been written about it, but specimens occasionally show up in old collections.

Along the SE side of the pegmatite is a small body of altered ultramafic rock, with another one situated about 300 m to the SW (Martin, 1970). Given their proximity to the pegmatite quarry, one or both of these may be the source of various specimens in collections labeled only as "Harwinton", though there are other such bodies north of state Route 118 also. These are green to olive, massive Ca/Mg-silicate assemblage from alteration of an ultramafic rock body containing minerals like green (Cr-rich) and white fibrous tremolite, green (Cr-rich) grossular (assumed), diopside, actinolite, epidote, calcite, quartz, magnetite, etc. They match the description in Martin (1970).

Yale Peabody Museum has a specimen of "halotrichite" with "Hill Road" as the locality. An SEM-EDS analysis of a similar sample in another collection (again labelled only as "Harwinton") shows it to be pickeringite, the Mg end member of the visually indistinguishable halotrichite-pickeringite series. It may have formed from weathering of a Mg-rich ultramafic body. Given that Hill Road is very long but otherwise has very little rock exposure along it, the ultramafic bodies near its north end appear to be the likely source.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


15 valid minerals.

Detailed Mineral List:

β“˜ Actinolite
Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Habit: acicular
Colour: dark green
Description: Layers of bedded needles with coarse-grained chrome-tremolite in altered ultramafic rock.
Reference: Harold Moritz collection, Former Richard Schooner collection
β“˜ Albite
Formula: Na(AlSi3O8)
Reference: Ed Force collection
β“˜ Beryl
Formula: Be3Al2(Si6O18)
Reference: Ed Force collection
β“˜ Calcite
Formula: CaCO3
Habit: massive
Colour: white
Description: Massive material in altered ultramafic rock.
Reference: Harold Moritz collection, Former Ed Force collection
β“˜ Diopside
Formula: CaMgSi2O6
Habit: massive
Colour: Pale green-brown
Description: Part of altered ultramafic rock assemblage.
Reference: Harold Moritz collection, Former Ed Force collection
β“˜ Epidote
Formula: {Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Habit: subhedral elongated prisms to massive
Colour: olive green
Description: Part of ultramafic rock assemblage.
Reference: Harold Moritz collection, Former Ed Force collection
β“˜ Grossular
Formula: Ca3Al2(SiO4)3
Habit: granular
Colour: emerald green
Description: Tiny but bright green grains in ultramafic rock assemblage, assumed to be Cr-rich grossular rather than the much rarer uvarovite.
Reference: Harold Moritz collection, Former Ed Force collection
β“˜ Halotrichite ?
Formula: FeAl2(SO4)4 · 22H2O
Habit: fibrous
Colour: off-white to pale yellow
Description: Spongy mass of tiny fibrous crystals with included weathered-out mica flakes. May be all or in part pickeringite.
Reference: Yale Peabody Museum collection
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
Habit: granular
Colour: black
Description: Tiny grains in altered ultramafic rock.
Reference: Harold Moritz collection, Former Ed Force collection
β“˜ Microcline
Formula: K(AlSi3O8)
Reference: Ed Force collection
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Reference: Ed Force collection
β“˜ Pickeringite
Formula: MgAl2(SO4)4 · 22H2O
Habit: fibrous
Colour: pale yellow
Description: Spongy mass of tiny fibrous crystals with included weathered-out mica flakes.
Reference: Harold Moritz collection, former Ed Force collection
β“˜ Quartz
Formula: SiO2
Colour: smoky to colorless
Description: Major component of the pegmatite, mostly massive but euhedral pocket crystals are known. Minor constituent in altered ultramafic rock.
Reference: Ed Force collection; Harold Moritz collection
β“˜ Schorl
Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Reference: Ed Force collection
βœͺ Tremolite
Formula: ◻{Ca2}{Mg5}(Si8O22)(OH)2
Habit: massive to subhedral prismatic, acicular, fibrous
Colour: emerald green, white
Description: Coarse-grained green (Cr-rich) material with beds of white finer-grained, aciular to fibrous massive crystals in altered ultramafic rock.
Reference: Harold Moritz collection, Former Richard Schooner collection, Former Ed Force collection.

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Calcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Halotrichite ?7.CB.85FeAl2(SO4)4 Β· 22H2O
β“˜Pickeringite7.CB.85MgAl2(SO4)4 Β· 22H2O
Group 9 - Silicates
β“˜Actinolite9.DE.10β—»Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
β“˜Albite9.FA.35Na(AlSi3O8)
β“˜Beryl9.CJ.05Be3Al2(Si6O18)
β“˜Diopside9.DA.15CaMgSi2O6
β“˜Epidote9.BG.05a{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
β“˜Grossular9.AD.25Ca3Al2(SiO4)3
β“˜Microcline9.FA.30K(AlSi3O8)
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Tremolite9.DE.10β—»{Ca2}{Mg5}(Si8O22)(OH)2

List of minerals for each chemical element

HHydrogen
Hβ“˜ Tremolite◻{Ca2}{Mg5}(Si8O22)(OH)2
Hβ“˜ PickeringiteMgAl2(SO4)4 · 22H2O
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Hβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Hβ“˜ HalotrichiteFeAl2(SO4)4 · 22H2O
BeBeryllium
Beβ“˜ BerylBe3Al2(Si6O18)
BBoron
Bβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
CCarbon
Cβ“˜ CalciteCaCO3
OOxygen
Oβ“˜ Tremolite◻{Ca2}{Mg5}(Si8O22)(OH)2
Oβ“˜ PickeringiteMgAl2(SO4)4 · 22H2O
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ QuartzSiO2
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ MicroclineK(AlSi3O8)
Oβ“˜ BerylBe3Al2(Si6O18)
Oβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Oβ“˜ GrossularCa3Al2(SiO4)3
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ CalciteCaCO3
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Oβ“˜ HalotrichiteFeAl2(SO4)4 · 22H2O
NaSodium
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
MgMagnesium
Mgβ“˜ Tremolite◻{Ca2}{Mg5}(Si8O22)(OH)2
Mgβ“˜ PickeringiteMgAl2(SO4)4 · 22H2O
Mgβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Mgβ“˜ DiopsideCaMgSi2O6
AlAluminium
Alβ“˜ PickeringiteMgAl2(SO4)4 · 22H2O
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ MicroclineK(AlSi3O8)
Alβ“˜ BerylBe3Al2(Si6O18)
Alβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ GrossularCa3Al2(SiO4)3
Alβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Alβ“˜ HalotrichiteFeAl2(SO4)4 · 22H2O
SiSilicon
Siβ“˜ Tremolite◻{Ca2}{Mg5}(Si8O22)(OH)2
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ QuartzSiO2
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ MicroclineK(AlSi3O8)
Siβ“˜ BerylBe3Al2(Si6O18)
Siβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Siβ“˜ GrossularCa3Al2(SiO4)3
Siβ“˜ DiopsideCaMgSi2O6
Siβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
SSulfur
Sβ“˜ PickeringiteMgAl2(SO4)4 · 22H2O
Sβ“˜ HalotrichiteFeAl2(SO4)4 · 22H2O
KPotassium
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ MicroclineK(AlSi3O8)
CaCalcium
Caβ“˜ Tremolite◻{Ca2}{Mg5}(Si8O22)(OH)2
Caβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Caβ“˜ GrossularCa3Al2(SiO4)3
Caβ“˜ CalciteCaCO3
Caβ“˜ DiopsideCaMgSi2O6
Caβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
FeIron
Feβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Feβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ Epidote{Ca2}{Al2Fe3+}(Si2O7)(SiO4)O(OH)
Feβ“˜ HalotrichiteFeAl2(SO4)4 · 22H2O

References

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Year (asc) Year (desc) Author (A-Z) Author (Z-A)
Martin, Charles W. (1970) The Bedrock Geology of the Torrington Quadrangle. State Geological and Natural History Survey of Connecticut: Quadrangle Report No. 25: 44.

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