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Haddam, Middlesex County, Connecticut, USAi
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Haddam- not defined -
Middlesex CountyCounty
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05751030017058704082572.jpg
View of Higganum from Seymour State Park

Haddam, Middlesex County, Connecticut, USA
Latitude & Longitude (WGS84):
41° 28' 38'' North , 72° 30' 45'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Higganum1,698 (2017)4.3km
East Haddam9,042 (2017)5.0km
Moodus1,413 (2017)5.9km
Chester Center1,558 (2017)9.8km
East Hampton2,691 (2017)11.0km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Lapidary and Mineral Society of Central ConnecticutMeriden, Connecticut25km
New Haven Mineral ClubNew Haven, Connecticut39km
Bristol Gem & Mineral ClubBristol, Connecticut42km
Mindat Locality ID:
4574
Long-form identifier:
mindat:1:2:4574:5
GUID (UUID V4):
8893b693-db8c-4d1e-a00d-ba7b76ee40be


A town incorporated in October 1668 as "Hadham", it was later renamed Haddam due to people saying "Hadham" too fast. Haddam is the only town in Connecticut divided by the Connecticut River. Besides Haddam center, the town includes other villages andneighborhoods such as Haddam Neck (on the east side of the Connecticut River), Higganum, Tylerville, Shailerville, Ponset, Little City, and West Haddam. Haddam has a long history of quarrying, mineral discoveries and production. Its proximity to universities studying mineralogy (Wesleyan, Yale, Harvard, Amherst) and historic finds of chrysoberyl (world’s first in-situ crystals), fine epidote, columbite (first confirmed North American locality and probably first known locality), heliodor, and of course, the pocket elbaites and other minerals of the Gillette Quarry made it world famous.

Haddam displays rugged topography, with hills reaching over 600 feet above mean sea level. It is primarily underlain by Ordovician metamorphosed, plutonic, volcanic, and sedimentary rocks of the Bronson Hill volcanic arc terrane, with Ordovician to Silurian metasedimentary rocks of the Central Maine and Merrimack oceanic terranes under the town’s east. The oldest rocks are metaplutonic rocks of the northern Killingworth dome complex (fka Monson Gneiss), found in a generally north-south belt under Higganum, Ponset, Little City, West Haddam and Hidden Lake areas. These are predominantly gray orthogneisses; the Boulder Lake gneiss and the Pond Meadow gneiss. However, the Mississippian Hidden Lake gneiss occurs as a pluton in the core of the Killingworth dome.

Flanking the dome on the northwest and east are Ordovician metavolcanics of the Higganum Gneiss and Middletown Formation, consisting of amphibolites and mafic gneiss and schist with local areas rich in gedrite, anthophyllite, sillimanite, staurolite, kyanite, cordierite, almandine and schorl. Further out from the Middletown Formation are belts of the Collins Hill Formation, a mix of metasedimentary rocks consisting of schist, gneiss, amphibolite, calc-silicate, marble, and quartzite. The western belt of Collins Hill rocks crosses the extreme northwest corner of town, the eastern belt trends north-south from east of Rock Landing in Haddam Neck, through Haddam center and down to Turkey Hill Reservoir. It is most famous for hosting spectacular epidote crystals and other calc-silicate minerals found long ago in a solution cavity on the Hazen farm.

Immediately east of the eastern Collins Hill Formation is a belt of Monson Gneiss that was heavily quarried on Quarry Hill (above Injun Hollow Road in Haddam Neck), on Great Hill and on Long Hill. The first quarries, in Haddam Neck, were opened by Deacon Ezra Brainerd in 1762 and are among the first in the nation. The quarry on Great Hill opened in 1794. Easy access to the river and abundant rock allowed the Brainerd and Arnold families and others in Haddam to ship stone for building, paving, and fortifications all over the east coast for many decades. The favored rock on the west edge of the belt is a vertically foliated bluish-grey, biotite to hornblende gneiss that split easily into large slabs and was known locally as the β€œAllen vein” after its discoverer, quarryman David Allen. The exterior of the old county jail at the corner of state Route 154 and Jail Hill Road in Haddam center is faced with this stone.

The easternmost part of Haddam is underlain by calc-silicate gneiss and granofels of the Hebron Formation, part of the Merrimack oceanic terrane that is separated from the Bronson Hill terrane rocks to the west by the Cremation Hill Fault Zone. The fault is named for the hill in Haddam just south of Shailerville.

A minor but noteworthy rock is the Higganum Dike, an early Jurassic diabase intrusion that was a feeder dike for the Holyoke Basalt in the nearby Hartford Mesozoic Basin. The dike extends from nearly Long Island Sound, cuts diagonally northeast through Haddam, and continues well into northern New England. It is associated with Mesozoic brittle faulting that affected all of Connecticut. Where such faulting brecciated quartzite on the west side of Long Hill, abundant and large (over 25 cm) quartz crystals formed in the open spaces.

Permian pegmatites, both large and small, can be found cross-cutting all of Haddam’s bedrock. The larger ones intrude mostly the Middletown and Collins Hill Formations on both sides of the Killingworth Dome. They generally stand out as topographic ridges. Most of the feldspar quarrying took place in internally zoned pegmatites in the eastern belt of these rocks, especially at the Rock Landing and Gillette Quarries in Haddam Neck. The latter pegmatite, opened in 1895, contains miarolitic cavities that produced spectacular euhedral pocket crystals of elbaite, one of the few places in North America, plus abundant smoky quartz, albite, beryl, fluorapatite, topaz, microcline, and lepidolite crystals. It is the first reported locality for the lithian muscovite variety schernikite, named for early Gillette gem miner Ernest Schernikow. A similar pegmatite, the Sawmill or Hewitt Gem Quarry, occurs on the west flank of Long Hill. Numerous small, cross-cutting pegmatites were encountered in the gneiss quarries working the Allen vein from Haddam Neck southward well into Long Hill. These narrow but sharply zoned pegmatites produced abundant gem grade aquamarine, plus schorl, almandine, columbite, and occasionally molybdenite. Some were worked for feldspar also. Pegmatites in the Higganum area are unzoned and simple, with reddish microcline that discouraged quarrying. Their main asset is abundant euhedral magnetite crystals, which also occur in pegmatitic zones in the Pond Meadow Gneiss SE of Higganum.

In 1810 Archibald Bruce discovered chrysoberyl at the Cephus Brainerd house on Walkley Hill Road, the first place the mineral was found in-situ. This odd-ball rock consists of albite variety oligoclase, quartz, beryl, spessartine, schorl, chrysoberyl, cordierite, gahnite, columbite-(Fe), and talc and was studied for decades. The rock layer is conformable with the host rocks and lacks K-feldspar and so is more like a metamorphic rock and is unlike the true, cross-cutting granitic pegmatites in the area. Similar rocks composed mainly of oligoclase, quartz, cordierite and schorl are found elsewhere along strike at Tim’s Hill and at the state Route 9 interchange 8. The presence of columbite-(Fe) is also noteworthy because the first crystal (named simply columbite) was described by Hatchett in England in 1802 and was collected over 100 years earlier from an unknown Connecticut locality. The recognition of this new mineral lead to new finds in Haddam (first confirmed North American locality) and Middletown, intense study, and speculation that the first crystal came from this area, perhaps from Nat Cook's columbite prospect.

The combination of varied bedrock; abundant simple to complex pegmatites; faulting; intense quarrying for stone, feldspar, and gems; and mineralogists at nearby universities made this small town famous in the mineral world, as related by traveling doctor Frederick Hall (1840):

I could not pass by Haddam --- a place known all over civilized earth, for the richness and variety of its mineral productions. I therefore begged the captain to put me on shore, that I might have the pleasure of spending a few days in rambling among the rocks, and examining the fine quarries of granite and gneiss, which are very numerous, and are said to be extremely lucrative to their proprietors. The barren hills are, indeed, alive with human beings, hard at work, with the wedge, the crowbar, the drill, and the sledge¬hammer. Thousands of tons of the stone are already got out, and prepared for the builder's hand, waiting to be transported to New York, and other more Southern markets.

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Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

132 valid minerals. 1 (FRL) - first recorded locality of unapproved mineral/variety/etc. 2 erroneous literature entries.

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 Diagram

Detailed Mineral List:

β“˜ Actinolite
Formula: ◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Localities: Reported from at least 7 localities in this region.
β“˜ Aegirine
Formula: NaFe3+Si2O6
Colour: greenish
Description: Accompanies black hastingsite
β“˜ Albite
Formula: Na(AlSi3O8)
Localities: Reported from at least 29 localities in this region.
Habit: either flattened parallel to b {010} or elongated parallel to x {bar101}, and aggregated in parallel or twin-position to form a group which presents the aspect of a large crystal elongated in the direction of the axis b.
Colour: colorless to white
Description: A major component of the pegmatite, but also lining miarolitic cavities with clear, colorless to white, well-developed crystals to 2.5 cm in diameter, sometimes displaying a beautiful opalescence (Scovil, 1992).
β“˜ Albite var. Cleavelandite
Formula: Na(AlSi3O8)
Habit: tabular
Colour: white to colorless
Description: Significant component of the pegmatite. Excellent crystals, an inch or more in diameter, have come from cavities.
β“˜ Albite var. Oligoclase
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
Habit: anhedral but in large cleavable masses
Colour: white to pale green
Description: Gemmy and in large cleavable masses.
β“˜ Allanite-(Ce)
Formula: (CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Colour: black
Description: striated, terminated crystals up to 1 cm
β“˜ 'Allanite Group'
Formula: (A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
β“˜ Alleghanyite
Formula: Mn2+5(SiO4)2(OH)2
Colour: reddish
Description: Found by Dick Schooner. A segregation over a foot in diameter, it consisted mainly of reddish alleghanyite and pinkish kutnohorite, with accessories. Unfortunately, only a few specimens were saved.
β“˜ Almandine
Formula: Fe2+3Al2(SiO4)3
Localities: Reported from at least 13 localities in this region.
Habit: Trapezohedral
Colour: maroon, red-brown
Description: Crystals fairly common and well formed in quartz, but generally small, typically <2 cm.
βœͺ 'Almandine-Spessartine Series'
Habit: trapezohedral
Colour: deep maroon, reddish black
Description: XRF analyses by Harold Moritz show that most crystals in the pegmatites of the district are almandine with substantial spessartine component. Crystals from this locality were not tested.
β“˜ Annite
Formula: KFe2+3(AlSi3O10)(OH)2
Localities: Reported from at least 12 localities in this region.
Description: fka biotite, mostly as grains in the surrounding gneiss
β“˜ Anorthite
Formula: Ca(Al2Si2O8)
Habit: anhedral
Colour: white
Fluorescence: pale blue-white
Description: Part of the rock matrix.
β“˜ Anorthite var. Labradorite
Formula: (Ca,Na)[Al(Al,Si)Si2O8]
Habit: anhedral
Colour: white
Fluorescence: pale blue-white
Description: Part of the rock matrix.
β“˜ Anthophyllite
Formula: ◻{Mg2}{Mg5}(Si8O22)(OH)2
Localities: Reported from at least 6 localities in this region.
Habit: prismatic
Colour: dark green
Description: As pure layers cm thick and as isolated to radial sprays of crystals to several cm long in a granular quartz-albite matrix.
β“˜ 'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Habit: hexagonal
Colour: yellow to yellow-green
Description: In the tourmaline-bearing schist, apatite occurs in clear yellow to yellow green hexagonal x1s, mostly micro. However, one greenish xl about 1 3/8" x 3/4" was found (Yedlin, 1967).
β“˜ Aragonite
Formula: CaCO3
Description: Reference cited lists it as occurring at "Various Building-stone Quarries", there are several, the principal on being the Arnold Quarry, which has a mindat page.
β“˜ Augelite ?
Formula: Al2(PO4)(OH)3
Description: Schooner (circa 1980s) reported it with scorzalite in pieces from the Charles Thomas collection. He also reported fairfieldite, augelite, siderite, graftonite and triphylite in these pieces. Thus possible they really came from the Palermo mine.
β“˜ Autunite
Formula: Ca(UO2)2(PO4)2 · 10-12H2O
Habit: flakes, crusts
Colour: pale yellow green
Fluorescence: green
Description: Thin crusts and flaky crystals, hard to see without a UV lamp but very common on black, smoky quartz and around altered uraninite. Should properly be listed as meta-autunite as all autunite dehydrates.
β“˜ Axinite-(Fe)
Formula: Ca2Fe2+Al2BSi4O15OH
Colour: lavender
Description: With tan titanite and pink feldspar.
β“˜ 'Axinite Group' ?
Description: Included in a list copied from Schooner (1958) but with no supporting details. May have occurred in the calc-silicate vein found in the gneissic wall rock.
β“˜ Azurite
Formula: Cu3(CO3)2(OH)2
Habit: crust
Colour: light blue
Description: A few scanty crusts of light blue azurite, with malachite and chalcopyrite, on amphibolite (Schooner, circa 1985).
β“˜ Babingtonite
Formula: Ca2(Fe,Mn)FeSi5O14(OH)
β“˜ Baryte
Formula: BaSO4
Habit: cleavable masses
Colour: white
Description: White cleavages, up to two inches broad, accompanied tirodite in the spessartine lens at the Jail Hill quarry in Haddam. This was X-rayed for verification.
β“˜ Bavenite
Formula: Ca4Be2Al2Si9O26(OH)2
Habit: blades, needles, platey, massive, in hemispherical and 2-D radiating aggregates
Colour: white to pale green
Description: probably the best material for the species in Connecticut.
βœͺ Becquerelite
Formula: Ca(UO2)6O4(OH)6 · 8H2O
Habit: pseudomorphs after uraninite
Colour: yellow
Description: "A soft yellow pseudomorph after a uraninite crystal was X-rayed, and proved to be becquerelite." Schooner (circa 1980s).
β“˜ Bementite ?
Formula: Mn7Si6O15(OH)8
Description: Reported by Dick Schooner, reference gives no details.
β“˜ Bertrandite
Formula: Be4(Si2O7)(OH)2
Habit: Hemispherical aggregates and 2-dimensional sprays of radiating, acicular crystals
Colour: white
β“˜ Beryl
Formula: Be3Al2(Si6O18)
Localities: Reported from at least 20 localities in this region.
Habit: elongated hexagonal prisms, terminated with pinacoids and partial pyramids {11bar21}
Colour: yellow, peach, pale green, pink overgrowths on pale green cores, aqua, colorless
Fluorescence: blue-white
Description: Crystals to 2 feet (60 cm) across have been found. Most typical are colorless to pale green or pink overgrowths on pale green cored ("reverse watermelon") crystals, usually less than 15 cm long. Commonly frozen in quartz and associated with fluorapatite, cleavelandite, elbaite. Pocket crystals rare.
β“˜ Beryl var. Aquamarine
Formula: Be3Al2Si6O18
Localities: Reported from at least 6 localities in this region.
Habit: hexagonal prisms
Colour: pale blue
Description: Subordinate in quantity to the typical pale green and pink beryl, but gem quality crystals were found and cut. Some highly etched crystals also exist.
β“˜ Beryl var. Goshenite
Formula: Be3Al2(Si6O18)
Habit: elongated hexagonal prisms, terminated with pinacoids and partial pyramids {11bar21}
Colour: colorless
Fluorescence: blue-white
Description: Beryl crystals to 2 feet (60 cm) across have been found. Crystals usually less than 15 cm long. In large crystals, color grades from colorless to rose externally with pale green cores. Commonly frozen in quartz and associated with fluorapatite, cleavelandite, elbaite. Some gem material in smaller crystals from pockets.
β“˜ Beryl var. Heliodor
Formula: Be3Al2(Si6O18)
Colour: yellow to orange-brown
Description: Typically in radiating groups with tiny columbites. Good gem crystals rare.
β“˜ Beryl var. Morganite
Formula: Be3Al2(Si6O18)
Habit: elongated hexagonal prisms, terminated with pinacoids and partial pyramids {11bar21}
Colour: pink, commonly with green cores
Description: Beryl crystals to 2 feet (60 cm) across have been found. Crystals usually less than 15 cm long. Color zoning in large crystals typically consists of colorless to rose externally, with pale green cores. Commonly frozen in quartz and associated with fluorapatite, cleavelandite, elbaite. Some pocket gem material.
β“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Localities: Reported from at least 6 localities in this region.
References:
β“˜ Birnessite
Formula: (Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Habit: encrustation
Colour: black
Description: "This is one of the manganese oxides identified as a component of the soft black alteration crusts on tephroite, etc."
β“˜ Bismuthinite
Formula: Bi2S3
Localities: Reported from at least 6 localities in this region.
Habit: Acicular
Colour: gray metallic
β“˜ Bismutite
Formula: (BiO)2CO3
Description: Found "very sparingly".
β“˜ Bismutotantalite
Formula: Bi(Ta,Nb)O4
Habit: anhedral
Colour: gray exterior, brown interior
Description: Very small grains to a couple of mm in matrix of albite, muscovite, quartz, elbaite. Analyzed in 2017 by Peter Cristofono and Tom Mortimer.
β“˜ Bustamite
Formula: CaMn2+(Si2O6)
Habit: cleavable masses
Colour: light pink
Description: When the author discovered a large lens of spessartine at the Jail Hill quarry, in the 1950s, a few good specimens of pink "rhodonite" were collected. Two different shades were associated differently, one with spessartine and calcite (or dolomite), the other with tephroite and pyrophanite. X-ray and spectrographic tests have shown the lighter pink mineral to be bustamite, and the darker one pyroxmangite. In some cases, bustamite is intimately intergrown with johannsenite (probably an exsolution product).
βœͺ 'Calciomicrolite'
Habit: octahedron modified by dodecahedron, trapezohedron and hexahedron.
Colour: dark yellow green, brown, black
Description: Typically as micro-crystals but can reach 8mm, most easily found in the aplitic zone, but in the intermediate zone and core margin also. At least 4 crystals (tiny subhedral grains, 2 octahedral microcrystals and a single 21mm fragment) have been analyzed via SEM-EDS and in all cases the best match is calciomicrolite, with very little Na or Nb. Zones within the 21mm fragment were also analyzed and showed a Ca-Ta oxide with minor Nb (and no Na or Ti)...this could also be microlite, or perhaps calciotantite, which can occur as an inclusion in microlite.
β“˜ Calcite
Formula: CaCO3
Habit: massive
Description: In the calc-silicate vein with vesuvianite in a vein in the wall rock.
β“˜ Caryopilite
Formula: Mn2+3Si2O5(OH)4
Description: This was identified (at the University of Michigan) as a very minor component of "ore" from the manganese pod at the Jail Hill quarry in Haddam.
βœͺ Cassiterite
Formula: SnO2
Colour: dark brownish black
Description: good crystals to 1 cm, can be highly modified, lustrous, microcrystals in cleavelandite
β“˜ 'Chabazite'
Localities: Reported from at least 6 localities in this region.
Habit: phacolite twins
Colour: orange
β“˜ Chalcopyrite
Formula: CuFeS2
Localities: Reported from at least 10 localities in this region.
β“˜ 'Chlorite Group'
Localities: Reported from at least 6 localities in this region.
β“˜ 'Chlorophyllite'
Habit: coarse, micaceous pseudomorphs after cordierite
Colour: green
Description: Term used loosely to describe the micaceous mineral of the cordierite pseudomorphs.
β“˜ Chrysoberyl
Formula: BeAl2O4
Habit: Typically flat, striated, cyclic twins, sometimes fully 6-sided.
Colour: yellow-green, pale green
Description: First locality where it was found in-situ. Intensely studied in the 19th century - crystal drawings are in Dana's System of Mineralogy and Goldschmidt's Atlas der Krystallformen. Shepard (1837) writes: "occurs in large distinct crystals, simple and compound (see fig. 136 of my Mineralogy) as well as massive". Crystals reached up to about 7.5 cm across, typically translucent but not gemmy.
β“˜ Columbite-(Fe)
Formula: Fe2+Nb2O6
Habit: elongated tabular prisms
Colour: black with iridescence
Description: Well-formed iridescent crystals to 2 cm long, usually enclosed in microcline. The identification was made by Petr Cerny at the University of Manitoba, using microprobe analysis (Scovil 1992).
β“˜ 'Columbite-(Fe)-Columbite-(Mn) Series'
Localities: Reported from at least 6 localities in this region.
Colour: Black
Description: Micro crystals in the pegmatite matrix, species undetermined.
β“˜ Cookeite
Formula: (LiAl4◻)[AlSi3O10](OH)8
Habit: globular masses of radial hexagonal plates
Colour: yellowish-white
Fluorescence: yellow
Description: Globules typically a few mm across, encrusting pocket albite, smoky quartz, microcline, lepidolite, elbaite terminations. When naturally removed, leave hemispherical pits on quartz crystal surfaces.
β“˜ Cordierite
Formula: (Mg,Fe)2Al3(AlSi5O18)
Habit: Anhedral to blocky, also Subhedral
Colour: gray-green to violet
β“˜ Cronstedtite
Formula: Fe2+2Fe3+((Si,Fe3+)2O5)(OH)4
Habit: radial groups of flattened crystals
Colour: greenish-brown to almost black
Description: A drab greenish-brown to almost black mineral, abundantly associated with grunerite, siderite, and marcasite, was identified as chamosite. Careful restudy of X-ray data indicates cronstedtite as a better fit.
β“˜ Cummingtonite
Formula: ◻{Mg2}{Mg5}(Si8O22)(OH)2
β“˜ Dickite
Formula: Al2(Si2O5)(OH)4
Habit: massive
Colour: bluish-gray
Description: nepheline-sodalite rock has been extensively replaced by fine-grained bluish-gray dickite and white natrolite.
β“˜ Diopside
Formula: CaMgSi2O6
Habit: elongated narrow prismatic
Colour: gray-green
Description: Fan-shaped aggregates of radiating crystals about 1-1.5 cm wide and 15 cm long frozen in quartz. Found in a glacial boulder near the quarry.
β“˜ Dolomite
Formula: CaMg(CO3)2
β“˜ Dravite
Formula: NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜ Elbaite
Formula: Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Habit: Elongated trigonal prisms, antilogous pole terminated with rhombohedral pyramids {1bar11}, analgous pole dominated by a pedion.
Colour: prisms mostly green, blue-green, rarely pink. Terms. green, yellow, pink, blue, combinations
Description: Hundreds of crystals in some pockets, often "piercing" smoky quartz. Flawless crystals are rare; usually fractured. Large pocket crystals vary but are usually striated to silky, slender and elongated, from small needles up to 30 cm, but typically a few cm long. Color zoning is usually longitudinal, short and terminal in shades of green, pink, golden yellow and blue with up to 5 colors. Antilogous poles typically pale green, yellow, pink; analogous poles usually colorless, pale green, aqua. w/thin indigo cap, or sometimes with a narrow pale colored zone immediately beneath and parallel to the pedion. Tiny crystals may be any color throughout. Concentric β€œwatermelon” zoning is not common. Some fragments of green prisms are overgrown by later pink zones. Also found frozen in matrix with beryl, fluorapatite, fluorite, muscovite, smoky quartz, lepidolite, microlite, columbite.
β“˜ Enstatite
Formula: Mg2Si2O6
Habit: elongated prismatic
Colour: dark brown-black
Description: dark but translucent, elongated crystals frozen in actinolite matrix, micro-crystals in tiny voids
β“˜ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Localities: Reported from at least 9 localities in this region.
Habit: elongated prisms
Colour: pale green
Description: Reportedly one of the better localities in Conn., Davis (1901) says: "some crystals doubly-terminated and six inches long, with brilliant faces and rich color. The color at this locality is particularly fine and many of the smaller crystals are transparent"
β“˜ 'Fahlunite'
Formula: (Mg,Fe)Al2Si3O10 · 2H2O
Habit: pseudomorphs after cordierite
Colour: dull olive green
Description: "The pinite [later fahlunite] variety, though generally occurring in indeterminate shaped pieces, yet nevertheless is occasionally seen in forms of the same shape and regularity as the iolite, from which, however, it differs essentially in color and hardness. The peculiar tint affected by the pinite is a pale, bluish, chloride green. Its lustre is pearly, and not particularly shining, except in a few specimens, where the color approaches silver-white. Hardness 2.5. Laminae neither flexible nor elastic. "in rhombic prisms in great abundance at the Iolite locality, and desirable specimens are easily obtainable. Many of these specimens upon being broken show clear blue Iolite in the interior, from which mineral it, is derived as alteration." (Davis, 1901).
β“˜ Fairfieldite ?
Formula: Ca2Mn2+(PO4)2 · 2H2O
Colour: white
Description: "The white mineral partly replacing graftonite from the Rock Landing quarry is very likely fairfieldite." Schooner (circa 1980s) reported in pieces from the Charles Thomas collection. He who also reported scorzalite, augelite, graftonite, siderite, and triphylite in these pieces. Thus possible they really came from the Palermo mine.
β“˜ 'Fayalite-Forsterite Series'
β“˜ Ferri-ghoseite
Formula: ◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
Habit: lamellar or bladed
Colour: tan or green
Description: Reported by Dick Schooner as "Tirodite", reference below provides no details. An XRD analysis of a sample labeled "tirodite" from Dick Schooner's collection could not differentiate it from actinolite. However, Schooner (circa 1990) reports: "Tan or green tirodite, lamellar and bladed, was rather common at the Jail Hill quarry, usually with only spessartine or barite. Masses two inches across have been preserved. A few little silky-fibrous tufts proved to be tirodite, also. This material was studied at the University of Michigan." A dark green amphibole-rich Schooner specimen labeled as "tirodite" (photo 983892) was analysed via SEM-EDS by Micromounters New England in 2019 and was found to be ferro-actinolite (no Mn).
β“˜ Ferro-actinolite
Formula: ◻Ca2Fe2+5(Si8O22)(OH)2
Habit: anhedral
Colour: very dark green
Description: As sub-cm grains in amphibolite rock with frosty, fine-grained scapolite.
β“˜ Fluorapatite
Formula: Ca5(PO4)3F
Localities: Reported from at least 10 localities in this region.
Habit: short hexagonal prisms or tabular, terminated by pinacoids with modified edges
Colour: pale gray-green or rose pink to purple
Fluorescence: bright yellow
Description: Gray-green opaque crystals up to 2 cm common in quartz, albite, beryl, elbaite, lepidolite matrix. Translucent to clear crystals in pockets, either as stout hexagonal prisms or with a central fluorescent prism surrounded by tapered, non-fluorescent overgrowths up to a few cm across. Gray-green crystals show more forms than the rose pink to purple crystals.
β“˜ Fluorite
Formula: CaF2
Colour: red
Description: see variety chlorophane for details
β“˜ Fluorite var. Chlorophane
Formula: CaF2
Habit: anhedral to modified octahedral
Colour: micro crystals colorless to pale pink with purple zones at the tips, larger crystals and masses are red to reddish black
Fluorescence: blue-green in SW, purple in LW, green phosphorescence
Description: Crystals mostly micros in pockets in the aplitic zone, larger crystals to a few cm rare, but they typically crumble into fragments when found. Typically as irregular masses to 10 cm. SW fluorescence is eventually lost if left exposed to any light, so immediately place and keep any finds in an opaque container to preserve this property.
β“˜ Fourmarierite
Formula: Pb(UO2)4O3(OH)4 · 4H2O
Habit: pseudomorphs after uraninite
Colour: reddish
Description: "In a study at Harvard University, in 1964, both fourmarierite and vandendriesscheite were identified, by X-ray diffraction, as components of hard "gummite" pseudomorphs after uraninite from the Rock Landing quarry. Fourmarierite is reddish; vandendriesscheite, yellow. The material came from the Charles Thomas collection." Schooner (circa 1980s).
β“˜ Gahnite
Formula: ZnAl2O4
Description: Mentioned by Foye (1922) as occurring there, but specimens are lacking.
β“˜ Galaxite ?
Formula: Mn2+Al2O4
Colour: dark green
Description: A dusting of a dark green mineral is seen in alleghanyite-kutnohorite specimens from the Jail Hill quarry. X-ray diffraction of a mixed sample shows faint peaks that correspond rather well to galaxite.
β“˜ 'Garnet Group'
Formula: X3Z2(SiO4)3
Localities: Reported from at least 7 localities in this region.
Colour: ruby red
Description: The crystals an seldom perfect, usually only half crystallized, but those faces that are shown are very brilliant and of a rich ruby red color. (Davis, 1901)
β“˜ Gedrite ?
Formula: ◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Habit: acicular prisms in 2-D rosettes and sprays
Description: Identified by Lundgren (1979), but not confirmed by 2016 ion microprobe analysis
β“˜ Goethite
Formula: Ξ±-Fe3+O(OH)
Habit: massive
Colour: brown
Description: Forming bog iron ore encrusting plant debris.
β“˜ Gonnardite
Formula: (Na,Ca)2(Si,Al)5O10 · 3H2O
β“˜ Graftonite ?
Formula: Fe2+Fe2+2(PO4)2
Description: Reported by Schooner (circa 1980s) as occurring in pieces from the Charles Thomas collection, along with triphylite, scorzalite, siderite, fairfieldite, augelite. Possible they could have come from the Palermo mine.
β“˜ Graphite
Formula: C
β“˜ Grossular
Formula: Ca3Al2(SiO4)3
Habit: dodecahedral
Colour: reddish-brown, orange-brown
Description: Good crystals to several cm.
β“˜ Groutite ?
Formula: Mn3+O(OH)
Description: Reportedly one of the black Mn-rich alteration crusts.
β“˜ Grunerite
Formula: ◻{Fe2+2}{Fe2+5}(Si8O22)(OH)2
Description: siderite layers up to 1/2 inch were common in a vein of marcasite, cronstedtite, grunerite, and quartz (Schooner, circa 1985).
β“˜ 'Gummite'
Colour: orange, yellow, red
Description: According to Schooner (circa 1980s) analyzed by Clifford Frondel at Harvard and found to be mix of fourmarierite and vandendriesschite.
β“˜ Gypsum
Formula: CaSO4 · 2H2O
Habit: clusters of micro crystals
Colour: white to gray
Description: As clusters of very delicate white or gray crystals on protected ledges of schist and gneiss, formed from the oxidation of sulfides in these rocks surrounding the pegmatite.
β“˜ Hastingsite
Formula: NaCa2(Fe2+4Fe3+)(Si6Al2)O22(OH)2
Habit: subhedral prismatic
Colour: black
β“˜ Hematite
Formula: Fe2O3
Habit: pseudo-hexagonal
Colour: brown
Description: as brown pseudo-hexagonal inclusions in muscovite, often producing fascinating patterns
β“˜ 'Heulandite Subgroup'
Formula: (Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
β“˜ 'Hornblende Root Name Group'
Formula: ◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
β“˜ Ilmenite
Formula: Fe2+TiO3
β“˜ Ilmenite var. Iron(III)-bearing Ilmenite
Formula: (Fe2+,Fe3+)TiO3
β“˜ 'Indicolite'
Formula: A(D3)G6(T6O18)(BO3)3X3Z
β“˜ Jacobsite
Formula: Mn2+Fe3+2O4
Description: "Specimens of tephroite from the Jail Hill quarry contain magnetic grains, shown (by X-ray and microprobe study at the University of Michigan) to be jacobsite. The material ranges from ferroan jacobsite to manganoan magnetite, within individual grains. A few specimens show it rather abundantly." Specimens are in the Harvard Mineralogical Museum.
β“˜ Johannsenite ?
Formula: CaMn2+Si2O6
Colour: tan or gray
Description: Fibrous tan or gray johannsenite is intergrown with pink bustamite in a few specimens from the Jail Hill quarry. The X-ray pattern indicates a clinopyroxene, and spectrographic analysis shows calcium and manganese as the principal cations of both minerals. The association is entirely characteristic.
β“˜ 'K Feldspar'
Habit: wedge-shaped
Colour: white
Description: In hexagonal voids from dissolved beryl, with clays and bertrandite.
β“˜ 'K Feldspar var. Adularia'
Formula: KAlSi3O8
Habit: wedge-shaped
Colour: white
Description: In hexagonal voids from dissolved beryl, with clays and bertrandite.
β“˜ Kutnohorite
Formula: CaMn2+(CO3)2
Habit: massive
Colour: pink
Description: "Light pink kutnohorite (verified at the University of Michigan) is the matrix for abundant reddish grains of alleghanyite (or an alleghanyite-like mineral) in the material collected, around 1960, at the Jail Hill quarry. Tephroite, jacobsite, and pyrophanite are also associated."
β“˜ Kyanite
Formula: Al2(SiO4)O
Colour: blue
Description: Some magnificent specimens of a rich blue color have been plowed up on a Haddam Neck farm, but I think the original vein has never been discovered. One of the finest of these specimens is in the collection of Mr. F. P. Per¬kins, Port Chester, N. Y. (Davis, 1901).
β“˜ Laumontite
Formula: CaAl2Si4O12 · 4H2O
Habit: elongated prisms
Colour: white
Description: Associated with prehnite. "...fine little obliquely-terminated white prisms on reniform prehnite from amphibole gneiss. Ben Hayes collected some fine specimens." Schooner circa 1990.
β“˜ 'Lepidolite'
Habit: pseudo-hexagonal crystals, granular
Colour: purple
Description: As distinct crystals, up to 10 cm across; as overgrowths on a core of green muscovite and in turn overgrown by parallel schernikite fibers - all cleavable as one unit. As peach-blossom red crystals, often penetrated by elbaite. Fine-grained, granular masses in matrix with smoky quartz, cleavelandite, elbatite, beryl, fluorapatite.
β“˜ 'Limonite'
β“˜ Maghemite
Formula: (Fe3+0.670.33)Fe3+2O4
Habit: massive
Colour: brown
Description: Alteration of magnetite found on biotite gneiss in the rock quarry uphill from the pegmatite. Referenced and photographed by Weissmand and Nikischer of Excalibur Mineral Corp. Harold Moritz collection contains a similar specimen purchased from them.
β“˜ Magnetite
Formula: Fe2+Fe3+2O4
Localities: Reported from at least 13 localities in this region.
Habit: Striated octahedrons to dodecahedrons
Colour: metallic gray to black
Description: Typically coated with a thin layer of muscovite that can be carefully removed.
β“˜ Malachite
Formula: Cu2(CO3)(OH)2
Habit: crust
Description: A few scanty crusts of light blue azurite, with malachite and chalcopyrite, on amphibolite (Schooner, circa 1985).
β“˜ 'Manganese Oxides'
β“˜ 'Manganese Oxides var. Manganese Dendrites'
β“˜ Marcasite
Formula: FeS2
Description: met with occasionally in the gneiss quarries (Davis, 1901)
β“˜ Meionite
Formula: Ca4Al6Si6O24CO3
β“˜ Melanterite
Formula: Fe2+(H2O)6SO4 · H2O
Description: Alteration of pyrite, pyrrhotite.
β“˜ Meta-autunite
Formula: Ca(UO2)2(PO4)2 · 6H2O
Localities: Reported from at least 6 localities in this region.
Habit: flakes, crusts
Colour: pale yellow-green
Fluorescence: green
Description: Thin crusts and flaky crystals, hard to see without a UV lamp but very common on black, smoky quartz and around altered uraninite.
β“˜ Metatorbernite
Formula: Cu(UO2)2(PO4)2 · 8H2O
β“˜ Microcline
Formula: K(AlSi3O8)
Localities: Reported from at least 27 localities in this region.
Habit: blocky to prismatic
Colour: white and salmon-pink
Fluorescence: bluish-white
Description: Crystals in cavities reach 20 cm or more across, and up to 120 cm across as crude crystals in the core. One large crystal was presented to the American Museum of Natural History, NYC by E. Schernikow. As "perthite", a major component of the pegmatite in general.
β“˜ Microcline var. Amazonite
Formula: K(AlSi3O8)
Habit: massive to subhedral prismatic
Colour: pale green
Description: Concentrated at the intermediate/quartz core zone boundary where inward oriented, subhedral prismatic crystals reach 30 cm. Color is generally pale and patchy within crytals, but some zones approach aqua.
βœͺ Microcline var. Hyalophane
Formula: (K,Ba)[Al(Si,Al)Si2O8]
Habit: prismatic
Colour: pale yellow-white
Description: "A few nicely formed yellowish hyalophane crystals (adularia type) were found in vugs of spessartine crystals at the Jail Hill quarry in Haddam, associated with a lens of manganese silicates and oxides. Spectrographic analysis indicates the hyalophane is manganoan." Schooner (circa 1985). Crystals reach about 1 cm.
β“˜ 'Microlite Group'
Formula: A2-mTa2X6-wZ-n
Habit: modified octahedra
Colour: brown to black
Description: Crystals up to 1.1 cm, resinous, some are radioactive and surrounded by dark halos, associated with dark smoky quartz, sharp little crystals of muscovite, acicular green tourmaline, beryl, fluorite, cleavelandite.
β“˜ Molybdenite
Formula: MoS2
Localities: Reported from at least 10 localities in this region.
β“˜ Monazite-(Ce)
Formula: Ce(PO4)
β“˜ Montmorillonite ?
Formula: (Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Colour: white (stained brown)
Description: Pocket clay that Schooner (1958) speculates is montmorillonite. David London's 2008 book "Pegmatites" points out that miarolitic pocket clays are poorly studied, but in at least the San Diego Co. area of California includes montmorillonite plus several other species.
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Localities: Reported from at least 25 localities in this region.
Habit: pseudo-hexagonal tabular
Colour: silvery-white to greenish
Description: A major accessory of the pegmatite in general, in books up to 45 cm in diameter and 20 cm thick. Books often contain beautiful inclusions of green elbaite and black schorl, as well as hexagonal hematite platelets and flattened magnetite octahedra. Some muscovite crystals are surrounded by overgrowths of lepidolite and schernikite that cleave as a single unit.
β“˜ Muscovite var. Illite
Formula: K0.65Al2.0[Al0.65Si3.35O10](OH)2
Habit: earthy
Colour: pastel pink
Description: clay-like masses in small voids in the aplitic zone of the pegmatite.
β“˜ Muscovite var. Schernikite (FRL)
Formula: KAl2(AlSi3O10)(OH)2
Habit: Rhombic fibers in parallel or twin-position
Colour: white, tan, pink
Description: A variety of pink fibrous muscovite so far unique to Gillette, as described by Scovil (1992): "Bowman (1902) goes into great detail in his analysis of muscovite and lepidolite from Gillette. The two form interesting overgrowths, with pale green muscovite at the center. This core is surrounded by a sharply defined zone of pink lepidolite. The lepidolite was subsequently overgrown by pink fibrous muscovite. The fibers are rhombic in cross section and are in parallel or twin-position so that the mass can be cleaved as if a single crystal...The fibrous muscovite also occurs as inclusions in quartz crystals. The muscovite starts at a pin point in the quartz crystals interior and becomes a divergent sub-parallel bundle of fibers as it reaches the surface where it is often the preferred site for a cookeite hemisphere."
β“˜ Natrolite
Formula: Na2Al2Si3O10 · 2H2O
β“˜ Nepheline
Formula: Na3K(Al4Si4O16)
Habit: anhedral to subhedral grains
Colour: pale gray
Description: Major component of the rock.
β“˜ Nontronite
Formula: Na0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Habit: clay
Colour: greenish
Description: A greenish clay mineral, forming a vein or zone, near the contact of a nepheline-bearing dike and granite gneiss has been identified as nontronite. It was studied by X-ray diffraction.
β“˜ Opal
Formula: SiO2 · nH2O
Localities: Reported from at least 6 localities in this region.
Habit: encrustations
Colour: colorless
Fluorescence: bright green
Description: Gelatinous coatings and encrustations, some easily visible without using a UV lamp, on both pegmatite and host gneiss. UV response best in SW, progressively less in MW to LW.
β“˜ Opal var. Opal-AN
Formula: SiO2 · nH2O
Localities: Reported from at least 6 localities in this region.
Habit: encrustations
Colour: colorless
Fluorescence: bright green
Description: Gelatinous coatings and encrustations, some easily visible without using a UV lamp, on both pegmatite and host gneiss. UV response best in SW, progressively less in MW to LW.
β“˜ Orthoclase
Formula: K(AlSi3O8)
Description: "The single specimen at Yale described by Scovil (1992) from the old Brush collection was labeled before results reported by Cameron, Eugene N. and others. (1954) PEGMATITE INVESTIGATIONS 1942-45 NEW ENGLAND. U.S. Geological Survey, Professional Paper 255 and Stugard (1958) Pegmatites of the Middletown Area, Connecticut USGS Bulletin 1042-Q, that show the K-feldspar of the Middletown pegmatite district to be microcline." (Harold Moritz information)
β“˜ Oxy-dravite
Formula: Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
β“˜ Paragonite
Formula: NaAl2(AlSi3O10)(OH)2
Habit: anhedral
Colour: white to gray
Description: Sillimanite, collected in a quartz vein through schist, is altered, in a few samples, to a very soft, greasy-feeling, white or gray material. X-ray study indicates a mixture of fine-grained paragonite and subsidiary pyrophyllite. A fingernail easily scratches it.
β“˜ Phenakite ?
Formula: Be2SiO4
Description: Richard Schooner collected a specimen showing a few "tiny colorless" crystals described as "short-prismatic, with compound terminations" in a vug with spessartine crystals. Gunnar Bjareby identified them as phenakite. Anthony Albini now possesses what appears to be this specimen. The crystals visually resemble fluorapatite as described by Seaman and Gallant (1960), have the hardness of fluorapatite and fluoresce yellow-white.
β“˜ Phlogopite
Formula: KMg3(AlSi3O10)(OH)2
Description: reported as a small amount, probably in the enclosing schist at pegmatites are notoriously Mg-poor.
β“˜ Phosphuranylite
Formula: KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Description: "Phosphouranylite is associated with autunite, torbernite, and uranophane (or their dehydrated forms) on old specimens from...the Rock Landing quarry. The identification was made by Clifford Frondel." Schooner (circa 1980s).
β“˜ Piemontite
Formula: (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
β“˜ 'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
β“˜ Pollucite
Formula: (Cs,Na)2(Al2Si4O12) · 2H2O
Habit: massive, granular
Colour: white
Description: White masses identified by the inclusion of thin bands of lepidolite.
β“˜ Powellite
Formula: Ca(MoO4)
Habit: powdery
Colour: white, yellowish or greenish
Description: powdery white, yellowish or greenish material lining vugs, or as excellent plates alternating with plates of molybdenite.
β“˜ Prehnite
Formula: Ca2Al2Si3O10(OH)2
β“˜ Pyrite
Formula: FeS2
Localities: Reported from at least 13 localities in this region.
Habit: cubic and octahedral
Description: Large crystals imbedded in pyrrhotite; wonderfully perfect cubes and octahedrons.
β“˜ 'Pyrochlore Group'
Formula: A2Nb2(O,OH)6Z
Description: Included in a list of minerals with no supporting information.
β“˜ Pyrolusite
Formula: Mn4+O2
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.
β“˜ Pyrophanite
Formula: Mn2+TiO3
Habit: tabular
Colour: dark red to black
Description: "Very small brilliant tabular crystals, looking black through dark red under strong magnification, are commonly embedded in tephroite, kutnohorite, pyroxymangite, and spessartine from the Jail Hill quarry. Studies at the USGS and the University of Michigan have confirmed the identification."
β“˜ Pyrophyllite
Formula: Al2Si4O10(OH)2
Description: Sillimanite, collected in a quartz vein through schist, is altered, in a few samples, to a very soft, greasy-feeling, white or gray material. X-ray study indicates a mixture of fine-grained paragonite and subsidiary pyrophyllite. A fingernail easily scratches it.
β“˜ Pyroxmangite
Formula: Mn2+SiO3
Habit: cleavable masses
Colour: pink
Description: Bustamite and pyroxmangite occurred at the Jail Hill quarry; one light pink, with spessartine and dolomite; the other a deeper pink, and with a more fibrous cleavage, associated with tephroite and yellow spessartine. X-ray patterns were carefully studied and spectrographic tests made. Only a few rich specimens were found. Earlier, both of these minerals had been dismissed as "rhodonite".
β“˜ Pyrrhotite
Formula: Fe1-xS
Description: Schooner (1958) reports "one distinct little crystal"
β“˜ Quartz
Formula: SiO2
Localities: Reported from at least 34 localities in this region.
Habit: massive to euhedral prismatic or scepter overgrowths
Colour: smoky
Description: Mostly massive as part of the pegmatite matrix, but good pocket crystals are found at the outer edge of the quartz core zone near the amazonite crystals. Crystals to over 30 cm can form parts of the pocket walls, though most loose crystals are up to several cm. Can be doubly-terminated or complex scepters.
β“˜ Quartz var. Amethyst
Formula: SiO2
Description: The Min. Record reference cited lists amethyst localities. The inclusion of Haddam refers to Dick Schooner's 1961 Mineralogy of Connecticut, which states the following: "The author has seen a three inch specimen of amethyst crystals, with albite, from a pegmatite in Haddam; this was exhibited at the Peabody Museum of Yale University." A check with the Peabody collection turned up YPM MIN 058341 described by staff as "mostly massive quartz (sorta smoky), some albite with muscovite, and what appears to be a secondary fracture or cavity (not enough there to know) filling of quartz that starts as a thin layer (~1mm) of white quartz against the massive quartz, that expands into a cluster of amethyst crystals. Nice color." Donated by J. F. Schairer. No specific locality recorded.
β“˜ Quartz var. Rose Quartz
Formula: SiO2
Habit: massive
Colour: pink
β“˜ Quartz var. Smoky Quartz
Formula: SiO2
Localities: Reported from at least 16 localities in this region.
Habit: hexagonal prisms with rhombohedral terminations, sometimes flattened or etched, or oddly shaped overgrowths on earlier fragments
Colour: pale gray to black, brown
Description: Besides being a major component of the pegmatite matrix in general, where it is massive, it is abundant in miarolitic cavities as euhedral crystals. Some show phantoms or inclusions of schernikite fibers and elbaite and some are encrusted with cookeite blebs or show surface pit scars where cookeite was naturally removed. One 1.8-meter pocket contained nothing but jet-black smoky quartz crystals up to 14 cm in length. Etched crystals or oddly-shaped overgrowths on earlier fragments of quartz also known. Beautiful, doubly terminated crystals are often penetrated by elbaite. "One of these crystals, very flat and with several tourmalines inclosed, was worn as a watch-charm by the son of M. P. Gillette. This crystal in its natural state has as fine a polish as though it had just come from the lapidary's hand." (Davis, 1901).
β“˜ Rhodochrosite
Formula: MnCO3
Habit: granular
Colour: pink
Description: Grains with granular spessartine and tephroite.
β“˜ Rhodonite
Formula: CaMn3Mn[Si5O15]
Habit: subhedral grains
Colour: pink
Description: The validity of this species here has flip-flopped over the decades. Some reference refute it, saying confusion with bustamite and pyroxmangite, but at least one specimen confirmed by Raman spectroscopy by Paul Bartholomew, U. of New Haven, 2014.
β“˜ Rutile
Formula: TiO2
Habit: grains and rounded micro crystals
Colour: red to black
Description: Transparent red to black-appearing grains and rounded xls in and on feldspar in the schist.
β“˜ 'Scapolite'
Habit: granular
Description: coarse-grained scapolite accompanied epidote, calcite, and altered nepheline
β“˜ Scheelite
Formula: Ca(WO4)
Fluorescence: blue-white
Description: minute grains in quartz-tourmaline matrix; an incomplete one inch white crystal at the Gillette Quarry in Haddam Neck; small masses are scattered through the vesuvianite and quartz in the calc-silicate vein in the wall rock.
β“˜ Schorl
Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
Localities: Reported from at least 19 localities in this region.
Habit: short trigonal prisms, doubly-terminated
Colour: black
Description: "Excellent doubly-terminated crystals of black tourmaline, 1 to 2 inches in length, and 1/2 to 1 inch in diameter are found at the Iolite locality, often covered with incrustation of autunite." (Davis, 1901).
β“˜ Scorzalite ?
Formula: Fe2+Al2(PO4)2(OH)2
Colour: blue
Description: "Several lean examples of scorzalite and siderite, labeled "Rock Landing quarry", came from the Charles Thomas collection. They had been obtained when the locality was active in the late 1930s. The scorzalite, erroneously called "vivianite" on the label, is of a rich blue color and partly crystallized. The X-ray pattern suggests a composition somewhere between scorzalite and lazulite. A little augelite is intergrown." Schooner (circa 1980s).
β“˜ 'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
β“˜ Siderite
Formula: FeCO3
Habit: drusy
Colour: brown
Description: siderite layers up to 1/2 inch were common in a vein of marcasite, cronstedtite, grunerite, and quartz. Nice little curved brown drusy crystals are present on a few specimens.
β“˜ SillΓ©nite ?
Formula: Bi12SiO20
Habit: coating
Colour: white or yellowish
Description: According to Schooner (circa 1980s) a "thin white or yellowish coating on bismuthinite crystals" may be this mineral. Needs confirmation.
β“˜ Sillimanite
Formula: Al2(SiO4)O
β“˜ Sodalite
Formula: Na4(Si3Al3)O12Cl
Colour: white
Description: Much altered to zeolites.
β“˜ Spessartine
Formula: Mn2+3Al2(SiO4)3
Habit: trapezohedral modified by the hexoctahedron and dodecahedron
Colour: dark red to orange-red to yellowish-orange
Description: Mostly massive, cherty looking with conchoidal fracture, hundreds of pounds have been recovered; the small crystals, which range from microscopic up to a half of an inch in diameter, are of a brighter orange-red color. Most of the small crystals show the trapezohedron as the dominant crystal form modified by the hexoctahedron. Some show the trapezohedron modified by both the hexoctahedron and the dodecahedron. Associated with quartz, bustamite-pyroxmangite-alleghanyite, tephroite, actinolite. Confirmed as spessartine using XRD, XRF and Raman spectroscopy. One of the few bona-fide spessartine localities in Connecticut.
β“˜ Sphalerite
Formula: ZnS
Description: "observed with limonite and black tourmaline" Schooner (1958)
β“˜ Spinel
Formula: MgAl2O4
β“˜ Spodumene ?
Formula: LiAlSi2O6
Description: Given the absence of common spodumene crystals, the casually reported gemstones of the pink variety kunzite could simply have been morganite beryl; and a waxy butterscotch colored purported spodumene crystal measuring 1.5 x 2.0 x 5.0 cm altered to β€œpinite” is likely a muscovite pseudomorph after topaz, which are documented and in this size range.
β“˜ 'Stilbite Subgroup'
Formula: M6-7[Al8-9Si27-28O72] · nH2O
Localities: Reported from at least 6 localities in this region.
β“˜ Talc
Formula: Mg3Si4O10(OH)2
β“˜ 'Tantalite'
Formula: (Mn,Fe)(Ta,Nb)2O6
β“˜ Tantalite-(Mn)
Formula: Mn2+Ta2O6
Habit: Tabular prism
Colour: very dark maroon
Description: Slightly translucent microcrystals to a few mm in granular albite zone.
β“˜ Tephroite
Formula: Mn2+2SiO4
Habit: anhedral
Colour: tan, brown, dark brown
Description: Reported by Dick Schooner. Specimens mostly are pure masses of anhedral grains, or scattered grains associated with bustamite and spessartine, all with black staining. According to Schooner: "Several bodies of more complex mineralogy, within the spessartine, consisted for the most part of brownish tephroite, intimately intergrown with dolomite and kutnohorite, as well as yellow spessartine, alleghanyite, jacobsite, pyrophanite, etc. A few solid dark gray resinous-looking cleavages, up to an inch, were obtained. The main concentration was eventually removed as a boulder, over two feet in diameter, which may well hold the world's record for toughness; it took the author two days of steady pounding to reduce it!"
β“˜ Thorite
Formula: Th(SiO4)
Description: Yale Peabody Museum specimen 044598.
β“˜ Thorite var. Thorogummite
Formula: (Th,U)(SiO4)1-x(OH)4x
Habit: pseudomorphous after thorianite
Colour: white to pale yellow-gray
Description: Waxy/earthy replacements of thorianite crystals, usually micros.
β“˜ Titanite
Formula: CaTi(SiO4)O
Localities: Reported from at least 9 localities in this region.
Description: Schooner (circa 1980s) states that there were rich specimens of anatase that are pseudomorphs after titanite.
β“˜ Todorokite ?
Formula: (Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Colour: black
Description: Reportedly one of the black Mn-rich alteration crusts.
β“˜ Topaz
Formula: Al2(SiO4)(F,OH)2
Habit: equant or flattened with multiple terminal forms
Colour: colorless to pale blue, orange (altered)
Description: First found in the mid-1950s and so often unrecognized in earlier collections, topaz occurs rarely as equant, rhombic cross-section crystals up to 1 cm in the cavities or more commonly up to 5.6 cm embedded in quartz-albite-muscovite matrix. Greasy, orange-brown crystals are partially or wholly altered to muscovite and were earlier mistaken for "pinite" pseudomorphs after spodumene.
β“˜ Torbernite
Formula: Cu(UO2)2(PO4)2 · 12H2O
Habit: tabular, micros
Colour: green
Description: Associated with other uranium minerals. Properly it is metatorbernite.
β“˜ 'Tourmaline'
Formula: AD3G6 (T6O18)(BO3)3X3Z
Localities: Reported from at least 7 localities in this region.
Habit: elongated, striated, trigonal prisms capped by pinacoids or rhombohedra
Colour: black to green, rarely pink to colorless, with yellow, pink, pale green, blue terminations
Description: See comments under elbaite and schorl.
β“˜ 'Tourmaline var. Achroite'
Formula: A(D3)G6(T6O18)(BO3)3X3Z
β“˜ 'Tourmaline var. Rubellite'
Formula: A(D3)G6(T6O18)(BO3)3X3Z
β“˜ Triphylite
Formula: LiFe2+PO4
Description: Reported by Schooner (circa 1980s) as occurring in pieces from the Charles Thomas collection, along with graftonite, scorzalite, siderite, fairfieldite, augelite. Possible they could have come from the Palermo mine.
β“˜ Uraninite
Formula: UO2
Localities: Reported from at least 8 localities in this region.
Habit: octahedral
Colour: Black
β“˜ Uranophane
Formula: Ca(UO2)2(SiO3OH)2 · 5H2O
Habit: coatings near and replacements of uraninite
Colour: pale yellow
β“˜ Vandendriesscheite
Formula: PbU7O22 · 12H2O
Habit: pseudomorphs after uraninite
Colour: yellow
Description: "In a study at Harvard University, in 1964, both fourmarierite and vandendriesscheite were identified, by X-ray diffraction, as components of hard "gummite" pseudomorphs after uraninite from the Rock Landing quarry. Fourmarierite is reddish; vandendriesscheite, yellow. The material came from the Charles Thomas collection." Schooner (circa 1980s).
β“˜ Vesuvianite
Formula: Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Habit: columnar aggregates of striated elongate crystals
Colour: light brown
Description: With other calc-silicate minerals in a vein in the gneissic wall rock. Found by Schooner in 1953 and 1954. Confirmed by an x-ray diffraction test made by Mary E. Mrose of the U. S. Geological Survey. The largest specimen was six inches in length and half as wide.
β“˜ Vivianite ?
Formula: Fe2+Fe2+2(PO4)2 · 8H2O
Description: "replaces triphylite on specimens of graftonite" from the Charles Thomas collection as reported by Schooner (circa 1980s), along with augelite, fairfieldite, graftonite, siderite, and scorzalite, suggesting the pieces came from the Palermo mine.
β“˜ Xenotime-(Y)
Formula: Y(PO4)
Habit: bipyramidal
Colour: brown
Description: Microcrystals in pegmatite matrix found in 2019. SEM-EDS spectra here https://www.mindat.org/photo-1007556.html https://www.mindat.org/photo-1007557.html
β“˜ Zircon
Formula: Zr(SiO4)
Localities: Reported from at least 6 localities in this region.
β“˜ Zircon var. Cyrtolite
Formula: Zr[(SiO4),(OH)4]
Description: Tiny crystals usually in the aplitic zone.
β“˜ Zoisite
Formula: (CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Habit: subhedral, striated, elongated prismatic
Colour: pink
Fluorescence: purple
Description: Crystals in matrix can reach a few cm. Associated with anorthite, quartz, actinolite, scapolite.
β“˜ Zoisite var. Thulite
Formula: {Ca2}{Al,Mn3+3}(Si2O7)(SiO4)O(OH)
Habit: subhedral, striated, elongated prismatic
Colour: pink
Fluorescence: purple
Description: Crystals in matrix can reach a few cm. Associated with anorthite, quartz, actinolite, scapolite.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
β“˜Graphite1.CB.05aC
Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrrhotite2.CC.10Fe1-xS
β“˜Bismuthinite2.DB.05Bi2S3
β“˜Molybdenite2.EA.30MoS2
β“˜Pyrite2.EB.05aFeS2
β“˜Marcasite2.EB.10aFeS2
Group 3 - Halides
β“˜Fluorite3.AB.25CaF2
β“˜var. Chlorophane3.AB.25CaF2
Group 4 - Oxides and Hydroxides
β“˜'Microlite Group'4.00.A2-mTa2X6-wZ-n
β“˜'Pyrochlore Group' ?4.00.A2Nb2(O,OH)6Z
β“˜Goethite4.00.Ξ±-Fe3+O(OH)
β“˜Chrysoberyl4.BA.05BeAl2O4
β“˜Galaxite ?4.BB.05Mn2+Al2O4
β“˜Gahnite4.BB.05ZnAl2O4
β“˜Spinel4.BB.05MgAl2O4
β“˜Jacobsite4.BB.05Mn2+Fe3+2O4
β“˜Magnetite4.BB.05Fe2+Fe3+2O4
β“˜Maghemite4.BB.15(Fe3+0.67β—»0.33)Fe3+2O4
β“˜Pyrophanite4.CB.05Mn2+TiO3
β“˜Ilmenite
var. Iron(III)-bearing Ilmenite
4.CB.05(Fe2+,Fe3+)TiO3
β“˜4.CB.05Fe2+TiO3
β“˜Hematite4.CB.05Fe2O3
β“˜SillΓ©nite ?4.CB.70Bi12SiO20
β“˜Quartz
var. Amethyst
4.DA.05SiO2
β“˜4.DA.05SiO2
β“˜var. Smoky Quartz4.DA.05SiO2
β“˜var. Rose Quartz4.DA.05SiO2
β“˜Opal
var. Opal-AN
4.DA.10SiO2 Β· nH2O
β“˜4.DA.10SiO2 Β· nH2O
β“˜Rutile4.DB.05TiO2
β“˜Cassiterite4.DB.05SnO2
β“˜Pyrolusite ?4.DB.05Mn4+O2
β“˜Tantalite-(Mn)4.DB.35Mn2+Ta2O6
β“˜Columbite-(Fe)4.DB.35Fe2+Nb2O6
β“˜Bismutotantalite4.DE.30Bi(Ta,Nb)O4
β“˜Todorokite ?4.DK.10(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 Β· 3-4H2O
β“˜Uraninite4.DL.05UO2
β“˜Groutite ?4.FD.10Mn3+O(OH)
β“˜Birnessite4.FL.45(Na,Ca)0.5(Mn4+,Mn3+)2O4 Β· 1.5H2O
β“˜Becquerelite4.GB.10Ca(UO2)6O4(OH)6 Β· 8H2O
β“˜Fourmarierite4.GB.25Pb(UO2)4O3(OH)4 Β· 4H2O
β“˜Vandendriesscheite4.GB.40PbU7O22 Β· 12H2O
Group 5 - Nitrates and Carbonates
β“˜Siderite5.AB.05FeCO3
β“˜Calcite5.AB.05CaCO3
β“˜Rhodochrosite5.AB.05MnCO3
β“˜Dolomite5.AB.10CaMg(CO3)2
β“˜Kutnohorite5.AB.10CaMn2+(CO3)2
β“˜Aragonite5.AB.15CaCO3
β“˜Azurite5.BA.05Cu3(CO3)2(OH)2
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
β“˜Bismutite5.BE.25(BiO)2CO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Baryte7.AD.35BaSO4
β“˜Melanterite7.CB.35Fe2+(H2O)6SO4 Β· H2O
β“˜Gypsum7.CD.40CaSO4 Β· 2H2O
β“˜Scheelite7.GA.05Ca(WO4)
β“˜Powellite7.GA.05Ca(MoO4)
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Triphylite8.AB.10LiFe2+PO4
β“˜Graftonite ?8.AB.20Fe2+Fe2+2(PO4)2
β“˜Xenotime-(Y)8.AD.35Y(PO4)
β“˜Monazite-(Ce)8.AD.50Ce(PO4)
β“˜Scorzalite ?8.BB.40Fe2+Al2(PO4)2(OH)2
β“˜Augelite ?8.BE.05Al2(PO4)(OH)3
β“˜Fluorapatite8.BN.05Ca5(PO4)3F
β“˜Vivianite ?8.CE.40Fe2+Fe2+2(PO4)2 Β· 8H2O
β“˜Fairfieldite ?8.CG.05Ca2Mn2+(PO4)2 Β· 2H2O
β“˜Torbernite8.EB.05Cu(UO2)2(PO4)2 Β· 12H2O
β“˜Autunite8.EB.05Ca(UO2)2(PO4)2 Β· 10-12H2O
β“˜Metatorbernite8.EB.10Cu(UO2)2(PO4)2 Β· 8H2O
β“˜Meta-autunite8.EB.10Ca(UO2)2(PO4)2 Β· 6H2O
β“˜Phosphuranylite8.EC.10KCa(H3O)3(UO2)7(PO4)4O4 Β· 8H2O
Group 9 - Silicates
β“˜Phenakite ?9.AA.05Be2SiO4
β“˜Tephroite9.AC.05Mn2+2SiO4
β“˜Grossular9.AD.25Ca3Al2(SiO4)3
β“˜Spessartine9.AD.25Mn2+3Al2(SiO4)3
β“˜Almandine9.AD.25Fe2+3Al2(SiO4)3
β“˜Zircon9.AD.30Zr(SiO4)
β“˜var. Cyrtolite9.AD.30Zr[(SiO4),(OH)4]
β“˜Thorite
var. Thorogummite
9.AD.30(Th,U)(SiO4)1-x(OH)4x
β“˜9.AD.30Th(SiO4)
β“˜Sillimanite9.AF.05Al2(SiO4)O
β“˜Kyanite9.AF.15Al2(SiO4)O
β“˜Topaz9.AF.35Al2(SiO4)(F,OH)2
β“˜Alleghanyite9.AF.45Mn2+5(SiO4)2(OH)2
β“˜Titanite9.AG.15CaTi(SiO4)O
β“˜Uranophane9.AK.15Ca(UO2)2(SiO3OH)2 Β· 5H2O
β“˜Bertrandite9.BD.05Be4(Si2O7)(OH)2
β“˜Axinite-(Fe)9.BD.20Ca2Fe2+Al2BSi4O15OH
β“˜Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
β“˜Piemontite9.BG.05a(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
β“˜Allanite-(Ce)9.BG.05b(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
β“˜Zoisite
var. Thulite
9.BG.10{Ca2}{Al,Mn3+3}(Si2O7)(SiO4)O(OH)
β“˜9.BG.10(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
β“˜Vesuvianite9.BG.35Ca19Fe3+Al4(Al6Mg2)(β—»4)β—»[Si2O7]4[(SiO4)10]O(OH)9
β“˜Beryl
var. Aquamarine
9.CJ.05Be3Al2Si6O18
β“˜var. Morganite9.CJ.05Be3Al2(Si6O18)
β“˜var. Goshenite9.CJ.05Be3Al2(Si6O18)
β“˜9.CJ.05Be3Al2(Si6O18)
β“˜var. Heliodor9.CJ.05Be3Al2(Si6O18)
β“˜Cordierite9.CJ.10(Mg,Fe)2Al3(AlSi5O18)
β“˜Oxy-dravite9.CK.05Na(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
β“˜Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Dravite9.CK.05NaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Elbaite9.CK.05Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Enstatite9.DA.05Mg2Si2O6
β“˜Diopside9.DA.15CaMgSi2O6
β“˜Johannsenite ?9.DA.15CaMn2+Si2O6
β“˜Aegirine9.DA.25NaFe3+Si2O6
β“˜Spodumene ?9.DA.30LiAlSi2O6
β“˜Anthophyllite9.DD.05β—»{Mg2}{Mg5}(Si8O22)(OH)2
β“˜Gedrite ?9.DD.05β—»{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
β“˜Cummingtonite9.DE.05β—»{Mg2}{Mg5}(Si8O22)(OH)2
β“˜Grunerite9.DE.05β—»{Fe2+2}{Fe2+5}(Si8O22)(OH)2
β“˜Actinolite9.DE.10β—»Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
β“˜Ferro-actinolite9.DE.10β—»Ca2Fe2+5(Si8O22)(OH)2
β“˜Hastingsite9.DE.15NaCa2(Fe2+4Fe3+)(Si6Al2)O22(OH)2
β“˜Ferri-ghoseite9.DE.20β—»[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
β“˜Bavenite9.DF.25Ca4Be2Al2Si9O26(OH)2
β“˜Bustamite9.DG.05CaMn2+(Si2O6)
β“˜Babingtonite9.DK.05Ca2(Fe,Mn)FeSi5O14(OH)
β“˜Rhodonite9.DK.05CaMn3Mn[Si5O15]
β“˜Pyroxmangite9.DO.05Mn2+SiO3
β“˜Prehnite9.DP.20Ca2Al2Si3O10(OH)2
β“˜Talc9.EC.05Mg3Si4O10(OH)2
β“˜Pyrophyllite9.EC.10Al2Si4O10(OH)2
β“˜Muscovite
var. Schernikite (TL)
9.EC.15KAl2(AlSi3O10)(OH)2
β“˜9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Paragonite9.EC.15NaAl2(AlSi3O10)(OH)2
β“˜Muscovite
var. Illite
9.EC.15K0.65Al2.0[Al0.65Si3.35O10](OH)2
β“˜Annite9.EC.20KFe2+3(AlSi3O10)(OH)2
β“˜Phlogopite9.EC.20KMg3(AlSi3O10)(OH)2
β“˜Montmorillonite ?9.EC.40(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 Β· nH2O
β“˜Nontronite9.EC.40Na0.3Fe2((Si,Al)4O10)(OH)2 Β· nH2O
β“˜Cookeite9.EC.55(LiAl4β—»)[AlSi3O10](OH)8
β“˜Dickite9.ED.05Al2(Si2O5)(OH)4
β“˜Cronstedtite9.ED.15Fe2+2Fe3+((Si,Fe3+)2O5)(OH)4
β“˜Caryopilite9.ED.15Mn2+3Si2O5(OH)4
β“˜Bementite ?9.EE.05Mn7Si6O15(OH)8
β“˜Nepheline9.FA.05Na3K(Al4Si4O16)
β“˜Microcline
var. Amazonite
9.FA.30K(AlSi3O8)
β“˜Orthoclase9.FA.30K(AlSi3O8)
β“˜Microcline
var. Hyalophane
9.FA.30(K,Ba)[Al(Si,Al)Si2O8]
β“˜9.FA.30K(AlSi3O8)
β“˜Anorthite9.FA.35Ca(Al2Si2O8)
β“˜Albite
var. Oligoclase
9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
β“˜var. Cleavelandite9.FA.35Na(AlSi3O8)
β“˜9.FA.35Na(AlSi3O8)
β“˜Anorthite
var. Labradorite
9.FA.35(Ca,Na)[Al(Al,Si)Si2O8]
β“˜Sodalite9.FB.10Na4(Si3Al3)O12Cl
β“˜Meionite9.FB.15Ca4Al6Si6O24CO3
β“˜Gonnardite9.GA.05(Na,Ca)2(Si,Al)5O10 Β· 3H2O
β“˜Natrolite9.GA.05Na2Al2Si3O10 Β· 2H2O
β“˜Pollucite9.GB.05(Cs,Na)2(Al2Si4O12) Β· 2H2O
β“˜Laumontite9.GB.10CaAl2Si4O12 Β· 4H2O
Unclassified
β“˜'Serpentine Subgroup'-D3[Si2O5](OH)4
β“˜'Hornblende Root Name Group'-β—»Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
β“˜'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
β“˜'K Feldspar'-
β“˜'Garnet Group'-X3Z2(SiO4)3
β“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
β“˜'Tantalite'-(Mn,Fe)(Ta,Nb)2O6
β“˜'Tourmaline
var. Achroite'
-A(D3)G6(T6O18)(BO3)3X3Z
β“˜'Columbite-(Fe)-Columbite-(Mn) Series'-
β“˜'Manganese Oxides
var. Manganese Dendrites'
-
β“˜''-
β“˜'Apatite'-Ca5(PO4)3(Cl/F/OH)
β“˜'Axinite Group' ?-
β“˜'Calciomicrolite'-
β“˜'Scapolite'-
β“˜'Chabazite'-
β“˜'Fayalite-Forsterite Series'-
β“˜'Almandine-Spessartine Series'-
β“˜'Stilbite Subgroup'-M6-7[Al8-9Si27-28O72] Β· nH2O
β“˜'Chlorophyllite'-
β“˜'Chlorite Group'-
β“˜'Fahlunite'-(Mg,Fe)Al2Si3O10 Β· 2H2O
β“˜'Gummite'-
β“˜'Heulandite Subgroup'-(Na/Ca/K)5-6[Al8-9 Si27-28 O72] Β· nH2O
β“˜'Indicolite'-A(D3)G6(T6O18)(BO3)3X3Z
β“˜'Lepidolite'-
β“˜'Limonite'-
β“˜'K Feldspar
var. Adularia'
-KAlSi3O8
β“˜'Tourmaline'-AD3G6 (T6O18)(BO3)3X3Z
β“˜'var. Rubellite'-A(D3)G6(T6O18)(BO3)3X3Z
β“˜'Allanite Group'-(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)

List of minerals for each chemical element

HHydrogen
Hβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Hβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Hβ“˜ AlleghanyiteMn52+(SiO4)2(OH)2
Hβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Hβ“˜ Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Hβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Hβ“˜ AzuriteCu3(CO3)2(OH)2
Hβ“˜ AugeliteAl2(PO4)(OH)3
Hβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Hβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Hβ“˜ BecquereliteCa(UO2)6O4(OH)6 · 8H2O
Hβ“˜ BementiteMn7Si6O15(OH)8
Hβ“˜ BertranditeBe4(Si2O7)(OH)2
Hβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hβ“˜ Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Hβ“˜ CaryopiliteMn32+Si2O5(OH)4
Hβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Hβ“˜ CronstedtiteFe22+Fe3+((Si,Fe3+)2O5)(OH)4
Hβ“˜ Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2
Hβ“˜ DickiteAl2(Si2O5)(OH)4
Hβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Hβ“˜ FairfielditeCa2Mn2+(PO4)2 · 2H2O
Hβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Hβ“˜ Ferro-actinolite◻Ca2Fe52+(Si8O22)(OH)2
Hβ“˜ FourmarieritePb(UO2)4O3(OH)4 · 4H2O
Hβ“˜ Gedrite◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Hβ“˜ GoethiteΞ±-Fe3+O(OH)
Hβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Hβ“˜ GroutiteMn3+O(OH)
Hβ“˜ Grunerite◻{Fe22+}{Fe52+}(Si8O22)(OH)2
Hβ“˜ GypsumCaSO4 · 2H2O
Hβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Hβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Hβ“˜ Opal var. Opal-ANSiO2 · nH2O
Hβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Hβ“˜ LaumontiteCaAl2Si4O12 · 4H2O
Hβ“˜ MalachiteCu2(CO3)(OH)2
Hβ“˜ MelanteriteFe2+(H2O)6SO4 · H2O
Hβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Hβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Hβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Hβ“˜ NatroliteNa2Al2Si3O10 · 2H2O
Hβ“˜ OpalSiO2 · nH2O
Hβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Hβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Hβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Hβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Hβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
Hβ“˜ PrehniteCa2Al2Si3O10(OH)2
Hβ“˜ Pyrochlore GroupA2Nb2(O,OH)6Z
Hβ“˜ PyrophylliteAl2Si4O10(OH)2
Hβ“˜ Muscovite var. SchernikiteKAl2(AlSi3O10)(OH)2
Hβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ ScorzaliteFe2+Al2(PO4)2(OH)2
Hβ“˜ Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Hβ“˜ TalcMg3Si4O10(OH)2
Hβ“˜ Thorite var. Thorogummite(Th,U)(SiO4)1-x(OH)4x
Hβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Hβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Hβ“˜ TopazAl2(SiO4)(F,OH)2
Hβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
Hβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Hβ“˜ VandendriesscheitePbU7O22 · 12H2O
Hβ“˜ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Hβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Hβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Hβ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Hβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Hβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Hβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Hβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
Hβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Hβ“˜ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
LiLithium
Liβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Liβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Liβ“˜ SpodumeneLiAlSi2O6
Liβ“˜ TriphyliteLiFe2+PO4
BeBeryllium
Beβ“˜ Beryl var. AquamarineBe3Al2Si6O18
Beβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Beβ“˜ BertranditeBe4(Si2O7)(OH)2
Beβ“˜ BerylBe3Al2(Si6O18)
Beβ“˜ ChrysoberylBeAl2O4
Beβ“˜ Beryl var. MorganiteBe3Al2(Si6O18)
Beβ“˜ PhenakiteBe2SiO4
Beβ“˜ Beryl var. HeliodorBe3Al2(Si6O18)
Beβ“˜ Beryl var. GosheniteBe3Al2(Si6O18)
BBoron
Bβ“˜ Tourmaline var. AchroiteA(D3)G6(T6O18)(BO3)3X3Z
Bβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Bβ“˜ IndicoliteA(D3)G6(T6O18)(BO3)3X3Z
Bβ“˜ Tourmaline var. RubelliteA(D3)G6(T6O18)(BO3)3X3Z
Bβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Bβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
Bβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
CCarbon
Cβ“˜ AragoniteCaCO3
Cβ“˜ AzuriteCu3(CO3)2(OH)2
Cβ“˜ Bismutite(BiO)2CO3
Cβ“˜ CalciteCaCO3
Cβ“˜ DolomiteCaMg(CO3)2
Cβ“˜ GraphiteC
Cβ“˜ KutnohoriteCaMn2+(CO3)2
Cβ“˜ MalachiteCu2(CO3)(OH)2
Cβ“˜ MeioniteCa4Al6Si6O24CO3
Cβ“˜ RhodochrositeMnCO3
Cβ“˜ SideriteFeCO3
OOxygen
Oβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Oβ“˜ K Feldspar var. AdulariaKAlSi3O8
Oβ“˜ AegirineNaFe3+Si2O6
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Oβ“˜ AlleghanyiteMn52+(SiO4)2(OH)2
Oβ“˜ Microcline var. AmazoniteK(AlSi3O8)
Oβ“˜ Quartz var. AmethystSiO2
Oβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Oβ“˜ AnorthiteCa(Al2Si2O8)
Oβ“˜ Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Oβ“˜ Beryl var. AquamarineBe3Al2Si6O18
Oβ“˜ AragoniteCaCO3
Oβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Oβ“˜ AzuriteCu3(CO3)2(OH)2
Oβ“˜ AugeliteAl2(PO4)(OH)3
Oβ“˜ AlmandineFe32+Al2(SiO4)3
Oβ“˜ Tourmaline var. AchroiteA(D3)G6(T6O18)(BO3)3X3Z
Oβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Oβ“˜ BaryteBaSO4
Oβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Oβ“˜ BecquereliteCa(UO2)6O4(OH)6 · 8H2O
Oβ“˜ BementiteMn7Si6O15(OH)8
Oβ“˜ BertranditeBe4(Si2O7)(OH)2
Oβ“˜ BismutotantaliteBi(Ta,Nb)O4
Oβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oβ“˜ Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Oβ“˜ Bismutite(BiO)2CO3
Oβ“˜ BustamiteCaMn2+(Si2O6)
Oβ“˜ BerylBe3Al2(Si6O18)
Oβ“˜ CalciteCaCO3
Oβ“˜ CaryopiliteMn32+Si2O5(OH)4
Oβ“˜ CassiteriteSnO2
Oβ“˜ ChrysoberylBeAl2O4
Oβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Oβ“˜ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Oβ“˜ CronstedtiteFe22+Fe3+((Si,Fe3+)2O5)(OH)4
Oβ“˜ Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2
Oβ“˜ DickiteAl2(Si2O5)(OH)4
Oβ“˜ DiopsideCaMgSi2O6
Oβ“˜ DolomiteCaMg(CO3)2
Oβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ EnstatiteMg2Si2O6
Oβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Oβ“˜ FairfielditeCa2Mn2+(PO4)2 · 2H2O
Oβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Oβ“˜ Ferro-actinolite◻Ca2Fe52+(Si8O22)(OH)2
Oβ“˜ Columbite-(Fe)Fe2+Nb2O6
Oβ“˜ FluorapatiteCa5(PO4)3F
Oβ“˜ FourmarieritePb(UO2)4O3(OH)4 · 4H2O
Oβ“˜ GahniteZnAl2O4
Oβ“˜ GalaxiteMn2+Al2O4
Oβ“˜ Gedrite◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Oβ“˜ GoethiteΞ±-Fe3+O(OH)
Oβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Oβ“˜ GraftoniteFe2+Fe22+(PO4)2
Oβ“˜ GrossularCa3Al2(SiO4)3
Oβ“˜ GroutiteMn3+O(OH)
Oβ“˜ Grunerite◻{Fe22+}{Fe52+}(Si8O22)(OH)2
Oβ“˜ GypsumCaSO4 · 2H2O
Oβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Oβ“˜ HematiteFe2O3
Oβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Oβ“˜ Opal var. Opal-ANSiO2 · nH2O
Oβ“˜ Microcline var. Hyalophane(K,Ba)[Al(Si,Al)Si2O8]
Oβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Oβ“˜ IlmeniteFe2+TiO3
Oβ“˜ IndicoliteA(D3)G6(T6O18)(BO3)3X3Z
Oβ“˜ JacobsiteMn2+Fe23+O4
Oβ“˜ JohannseniteCaMn2+Si2O6
Oβ“˜ KutnohoriteCaMn2+(CO3)2
Oβ“˜ KyaniteAl2(SiO4)O
Oβ“˜ Anorthite var. Labradorite(Ca,Na)[Al(Al,Si)Si2O8]
Oβ“˜ LaumontiteCaAl2Si4O12 · 4H2O
Oβ“˜ Tantalite-(Mn)Mn2+Ta2O6
Oβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
Oβ“˜ MagnetiteFe2+Fe23+O4
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ Ilmenite var. Iron(III)-bearing Ilmenite(Fe2+,Fe3+)TiO3
Oβ“˜ MeioniteCa4Al6Si6O24CO3
Oβ“˜ MelanteriteFe2+(H2O)6SO4 · H2O
Oβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Oβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Oβ“˜ MicroclineK(AlSi3O8)
Oβ“˜ Monazite-(Ce)Ce(PO4)
Oβ“˜ Beryl var. MorganiteBe3Al2(Si6O18)
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Oβ“˜ NephelineNa3K(Al4Si4O16)
Oβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Oβ“˜ NatroliteNa2Al2Si3O10 · 2H2O
Oβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Oβ“˜ OpalSiO2 · nH2O
Oβ“˜ OrthoclaseK(AlSi3O8)
Oβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Oβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Oβ“˜ PhenakiteBe2SiO4
Oβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Oβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Oβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
Oβ“˜ PowelliteCa(MoO4)
Oβ“˜ PrehniteCa2Al2Si3O10(OH)2
Oβ“˜ Pyrochlore GroupA2Nb2(O,OH)6Z
Oβ“˜ PyrolusiteMn4+O2
Oβ“˜ PyrophaniteMn2+TiO3
Oβ“˜ PyrophylliteAl2Si4O10(OH)2
Oβ“˜ PyroxmangiteMn2+SiO3
Oβ“˜ QuartzSiO2
Oβ“˜ RhodochrositeMnCO3
Oβ“˜ RhodoniteCaMn3Mn[Si5O15]
Oβ“˜ Quartz var. Rose QuartzSiO2
Oβ“˜ Tourmaline var. RubelliteA(D3)G6(T6O18)(BO3)3X3Z
Oβ“˜ RutileTiO2
Oβ“˜ ScheeliteCa(WO4)
Oβ“˜ Muscovite var. SchernikiteKAl2(AlSi3O10)(OH)2
Oβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ ScorzaliteFe2+Al2(PO4)2(OH)2
Oβ“˜ SideriteFeCO3
Oβ“˜ SillimaniteAl2(SiO4)O
Oβ“˜ SillΓ©niteBi12SiO20
Oβ“˜ Quartz var. Smoky QuartzSiO2
Oβ“˜ SodaliteNa4(Si3Al3)O12Cl
Oβ“˜ SpessartineMn32+Al2(SiO4)3
Oβ“˜ SpinelMgAl2O4
Oβ“˜ SpodumeneLiAlSi2O6
Oβ“˜ Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Oβ“˜ TalcMg3Si4O10(OH)2
Oβ“˜ Tantalite(Mn,Fe)(Ta,Nb)2O6
Oβ“˜ TephroiteMn22+SiO4
Oβ“˜ ThoriteTh(SiO4)
Oβ“˜ Thorite var. Thorogummite(Th,U)(SiO4)1-x(OH)4x
Oβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Oβ“˜ TitaniteCaTi(SiO4)O
Oβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Oβ“˜ TopazAl2(SiO4)(F,OH)2
Oβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
Oβ“˜ TourmalineAD3G6 (T6O18)(BO3)3X3Z
Oβ“˜ TriphyliteLiFe2+PO4
Oβ“˜ UraniniteUO2
Oβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Oβ“˜ VandendriesscheitePbU7O22 · 12H2O
Oβ“˜ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Oβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Oβ“˜ Xenotime-(Y)Y(PO4)
Oβ“˜ ZirconZr(SiO4)
Oβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Oβ“˜ Beryl var. HeliodorBe3Al2(Si6O18)
Oβ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Oβ“˜ Beryl var. GosheniteBe3Al2(Si6O18)
Oβ“˜ Albite var. CleavelanditeNa(AlSi3O8)
Oβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Oβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Oβ“˜ Garnet GroupX3Z2(SiO4)3
Oβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Oβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Oβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
Oβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
Oβ“˜ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
FFluorine
Fβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fβ“˜ Fluorite var. ChlorophaneCaF2
Fβ“˜ FluorapatiteCa5(PO4)3F
Fβ“˜ FluoriteCaF2
Fβ“˜ TopazAl2(SiO4)(F,OH)2
Fβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Fβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Naβ“˜ AegirineNaFe3+Si2O6
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Naβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Naβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Naβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Naβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Naβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Naβ“˜ Anorthite var. Labradorite(Ca,Na)[Al(Al,Si)Si2O8]
Naβ“˜ MeioniteCa4Al6Si6O24CO3
Naβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Naβ“˜ NephelineNa3K(Al4Si4O16)
Naβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Naβ“˜ NatroliteNa2Al2Si3O10 · 2H2O
Naβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Naβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Naβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
Naβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Naβ“˜ SodaliteNa4(Si3Al3)O12Cl
Naβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Naβ“˜ Albite var. CleavelanditeNa(AlSi3O8)
Naβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Naβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Naβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
MgMagnesium
Mgβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Mgβ“˜ Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Mgβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mgβ“˜ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Mgβ“˜ Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2
Mgβ“˜ DiopsideCaMgSi2O6
Mgβ“˜ DolomiteCaMg(CO3)2
Mgβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Mgβ“˜ EnstatiteMg2Si2O6
Mgβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Mgβ“˜ Gedrite◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Mgβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Mgβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Mgβ“˜ SpinelMgAl2O4
Mgβ“˜ TalcMg3Si4O10(OH)2
Mgβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Mgβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Mgβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Mgβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
AlAluminium
Alβ“˜ K Feldspar var. AdulariaKAlSi3O8
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Alβ“˜ Microcline var. AmazoniteK(AlSi3O8)
Alβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Alβ“˜ AnorthiteCa(Al2Si2O8)
Alβ“˜ Beryl var. AquamarineBe3Al2Si6O18
Alβ“˜ AugeliteAl2(PO4)(OH)3
Alβ“˜ AlmandineFe32+Al2(SiO4)3
Alβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Alβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alβ“˜ BerylBe3Al2(Si6O18)
Alβ“˜ ChrysoberylBeAl2O4
Alβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Alβ“˜ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Alβ“˜ DickiteAl2(Si2O5)(OH)4
Alβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Alβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Alβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Alβ“˜ GahniteZnAl2O4
Alβ“˜ GalaxiteMn2+Al2O4
Alβ“˜ Gedrite◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Alβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Alβ“˜ GrossularCa3Al2(SiO4)3
Alβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Alβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Alβ“˜ Microcline var. Hyalophane(K,Ba)[Al(Si,Al)Si2O8]
Alβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Alβ“˜ KyaniteAl2(SiO4)O
Alβ“˜ Anorthite var. Labradorite(Ca,Na)[Al(Al,Si)Si2O8]
Alβ“˜ LaumontiteCaAl2Si4O12 · 4H2O
Alβ“˜ MeioniteCa4Al6Si6O24CO3
Alβ“˜ MicroclineK(AlSi3O8)
Alβ“˜ Beryl var. MorganiteBe3Al2(Si6O18)
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Alβ“˜ NephelineNa3K(Al4Si4O16)
Alβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Alβ“˜ NatroliteNa2Al2Si3O10 · 2H2O
Alβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Alβ“˜ OrthoclaseK(AlSi3O8)
Alβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Alβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Alβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Alβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
Alβ“˜ PrehniteCa2Al2Si3O10(OH)2
Alβ“˜ PyrophylliteAl2Si4O10(OH)2
Alβ“˜ Muscovite var. SchernikiteKAl2(AlSi3O10)(OH)2
Alβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ ScorzaliteFe2+Al2(PO4)2(OH)2
Alβ“˜ SillimaniteAl2(SiO4)O
Alβ“˜ SodaliteNa4(Si3Al3)O12Cl
Alβ“˜ SpessartineMn32+Al2(SiO4)3
Alβ“˜ SpinelMgAl2O4
Alβ“˜ SpodumeneLiAlSi2O6
Alβ“˜ Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Alβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Alβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Alβ“˜ TopazAl2(SiO4)(F,OH)2
Alβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Alβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Alβ“˜ Beryl var. HeliodorBe3Al2(Si6O18)
Alβ“˜ Beryl var. GosheniteBe3Al2(Si6O18)
Alβ“˜ Albite var. CleavelanditeNa(AlSi3O8)
Alβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Alβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Alβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
SiSilicon
Siβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Siβ“˜ K Feldspar var. AdulariaKAlSi3O8
Siβ“˜ AegirineNaFe3+Si2O6
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Siβ“˜ AlleghanyiteMn52+(SiO4)2(OH)2
Siβ“˜ Microcline var. AmazoniteK(AlSi3O8)
Siβ“˜ Quartz var. AmethystSiO2
Siβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Siβ“˜ AnorthiteCa(Al2Si2O8)
Siβ“˜ Anthophyllite◻{Mg2}{Mg5}(Si8O22)(OH)2
Siβ“˜ Beryl var. AquamarineBe3Al2Si6O18
Siβ“˜ AlmandineFe32+Al2(SiO4)3
Siβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Siβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Siβ“˜ BementiteMn7Si6O15(OH)8
Siβ“˜ BertranditeBe4(Si2O7)(OH)2
Siβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siβ“˜ BustamiteCaMn2+(Si2O6)
Siβ“˜ BerylBe3Al2(Si6O18)
Siβ“˜ CaryopiliteMn32+Si2O5(OH)4
Siβ“˜ Cookeite(LiAl4◻)[AlSi3O10](OH)8
Siβ“˜ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Siβ“˜ CronstedtiteFe22+Fe3+((Si,Fe3+)2O5)(OH)4
Siβ“˜ Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2
Siβ“˜ DickiteAl2(Si2O5)(OH)4
Siβ“˜ DiopsideCaMgSi2O6
Siβ“˜ DraviteNaMg3Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ EnstatiteMg2Si2O6
Siβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Siβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Siβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Siβ“˜ Ferro-actinolite◻Ca2Fe52+(Si8O22)(OH)2
Siβ“˜ Gedrite◻{Mg2}{Mg3Al2}(Al2Si6O22)(OH)2
Siβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Siβ“˜ GrossularCa3Al2(SiO4)3
Siβ“˜ Grunerite◻{Fe22+}{Fe52+}(Si8O22)(OH)2
Siβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Siβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Siβ“˜ Opal var. Opal-ANSiO2 · nH2O
Siβ“˜ Microcline var. Hyalophane(K,Ba)[Al(Si,Al)Si2O8]
Siβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Siβ“˜ JohannseniteCaMn2+Si2O6
Siβ“˜ KyaniteAl2(SiO4)O
Siβ“˜ Anorthite var. Labradorite(Ca,Na)[Al(Al,Si)Si2O8]
Siβ“˜ LaumontiteCaAl2Si4O12 · 4H2O
Siβ“˜ MeioniteCa4Al6Si6O24CO3
Siβ“˜ MicroclineK(AlSi3O8)
Siβ“˜ Beryl var. MorganiteBe3Al2(Si6O18)
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Siβ“˜ NephelineNa3K(Al4Si4O16)
Siβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Siβ“˜ NatroliteNa2Al2Si3O10 · 2H2O
Siβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Siβ“˜ OpalSiO2 · nH2O
Siβ“˜ OrthoclaseK(AlSi3O8)
Siβ“˜ ParagoniteNaAl2(AlSi3O10)(OH)2
Siβ“˜ PhenakiteBe2SiO4
Siβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Siβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Siβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
Siβ“˜ PrehniteCa2Al2Si3O10(OH)2
Siβ“˜ PyrophylliteAl2Si4O10(OH)2
Siβ“˜ PyroxmangiteMn2+SiO3
Siβ“˜ QuartzSiO2
Siβ“˜ RhodoniteCaMn3Mn[Si5O15]
Siβ“˜ Quartz var. Rose QuartzSiO2
Siβ“˜ Muscovite var. SchernikiteKAl2(AlSi3O10)(OH)2
Siβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ SillimaniteAl2(SiO4)O
Siβ“˜ SillΓ©niteBi12SiO20
Siβ“˜ Quartz var. Smoky QuartzSiO2
Siβ“˜ SodaliteNa4(Si3Al3)O12Cl
Siβ“˜ SpessartineMn32+Al2(SiO4)3
Siβ“˜ SpodumeneLiAlSi2O6
Siβ“˜ Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Siβ“˜ TalcMg3Si4O10(OH)2
Siβ“˜ TephroiteMn22+SiO4
Siβ“˜ ThoriteTh(SiO4)
Siβ“˜ Thorite var. Thorogummite(Th,U)(SiO4)1-x(OH)4x
Siβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Siβ“˜ TitaniteCaTi(SiO4)O
Siβ“˜ TopazAl2(SiO4)(F,OH)2
Siβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Siβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Siβ“˜ ZirconZr(SiO4)
Siβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Siβ“˜ Beryl var. HeliodorBe3Al2(Si6O18)
Siβ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
Siβ“˜ Beryl var. GosheniteBe3Al2(Si6O18)
Siβ“˜ Albite var. CleavelanditeNa(AlSi3O8)
Siβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Siβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Siβ“˜ Garnet GroupX3Z2(SiO4)3
Siβ“˜ Oxy-draviteNa(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3O
Siβ“˜ Serpentine SubgroupD3[Si2O5](OH)4
Siβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
Siβ“˜ Allanite Group(A12+REE3+)(M13+M23+M32+)O[Si2O7][SiO4](OH)
PPhosphorus
Pβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Pβ“˜ AugeliteAl2(PO4)(OH)3
Pβ“˜ FairfielditeCa2Mn2+(PO4)2 · 2H2O
Pβ“˜ FluorapatiteCa5(PO4)3F
Pβ“˜ GraftoniteFe2+Fe22+(PO4)2
Pβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Pβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Pβ“˜ Monazite-(Ce)Ce(PO4)
Pβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Pβ“˜ ScorzaliteFe2+Al2(PO4)2(OH)2
Pβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
Pβ“˜ TriphyliteLiFe2+PO4
Pβ“˜ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Pβ“˜ Xenotime-(Y)Y(PO4)
Pβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
Sβ“˜ BaryteBaSO4
Sβ“˜ BismuthiniteBi2S3
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ GypsumCaSO4 · 2H2O
Sβ“˜ MarcasiteFeS2
Sβ“˜ MeioniteCa4Al6Si6O24CO3
Sβ“˜ MelanteriteFe2+(H2O)6SO4 · H2O
Sβ“˜ MolybdeniteMoS2
Sβ“˜ PyriteFeS2
Sβ“˜ PyrrhotiteFe1-xS
Sβ“˜ SphaleriteZnS
ClChlorine
Clβ“˜ MeioniteCa4Al6Si6O24CO3
Clβ“˜ SodaliteNa4(Si3Al3)O12Cl
Clβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Clβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
Kβ“˜ K Feldspar var. AdulariaKAlSi3O8
Kβ“˜ Microcline var. AmazoniteK(AlSi3O8)
Kβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Kβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Kβ“˜ Microcline var. Hyalophane(K,Ba)[Al(Si,Al)Si2O8]
Kβ“˜ Muscovite var. IlliteK0.65Al2.0[Al0.65Si3.35O10](OH)2
Kβ“˜ MicroclineK(AlSi3O8)
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Kβ“˜ NephelineNa3K(Al4Si4O16)
Kβ“˜ OrthoclaseK(AlSi3O8)
Kβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Kβ“˜ PhlogopiteKMg3(AlSi3O10)(OH)2
Kβ“˜ Muscovite var. SchernikiteKAl2(AlSi3O10)(OH)2
Kβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
CaCalcium
Caβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Caβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Caβ“˜ AnorthiteCa(Al2Si2O8)
Caβ“˜ AragoniteCaCO3
Caβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Caβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Caβ“˜ BaveniteCa4Be2Al2Si9O26(OH)2
Caβ“˜ BecquereliteCa(UO2)6O4(OH)6 · 8H2O
Caβ“˜ Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Caβ“˜ BustamiteCaMn2+(Si2O6)
Caβ“˜ CalciteCaCO3
Caβ“˜ Fluorite var. ChlorophaneCaF2
Caβ“˜ DiopsideCaMgSi2O6
Caβ“˜ DolomiteCaMg(CO3)2
Caβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Caβ“˜ FairfielditeCa2Mn2+(PO4)2 · 2H2O
Caβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Caβ“˜ Ferro-actinolite◻Ca2Fe52+(Si8O22)(OH)2
Caβ“˜ FluorapatiteCa5(PO4)3F
Caβ“˜ FluoriteCaF2
Caβ“˜ Gonnardite(Na,Ca)2(Si,Al)5O10 · 3H2O
Caβ“˜ GrossularCa3Al2(SiO4)3
Caβ“˜ GypsumCaSO4 · 2H2O
Caβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Caβ“˜ Heulandite Subgroup(Na/Ca/K)5-6[Al8-9 Si27-28 O72] · nH2O
Caβ“˜ JohannseniteCaMn2+Si2O6
Caβ“˜ KutnohoriteCaMn2+(CO3)2
Caβ“˜ Anorthite var. Labradorite(Ca,Na)[Al(Al,Si)Si2O8]
Caβ“˜ LaumontiteCaAl2Si4O12 · 4H2O
Caβ“˜ MeioniteCa4Al6Si6O24CO3
Caβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Caβ“˜ Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2O
Caβ“˜ Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Caβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Caβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Caβ“˜ PowelliteCa(MoO4)
Caβ“˜ PrehniteCa2Al2Si3O10(OH)2
Caβ“˜ RhodoniteCaMn3Mn[Si5O15]
Caβ“˜ ScheeliteCa(WO4)
Caβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Caβ“˜ TitaniteCaTi(SiO4)O
Caβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Caβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Caβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Caβ“˜ Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)
Caβ“˜ Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Caβ“˜ Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Caβ“˜ ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Tiβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Tiβ“˜ IlmeniteFe2+TiO3
Tiβ“˜ Ilmenite var. Iron(III)-bearing Ilmenite(Fe2+,Fe3+)TiO3
Tiβ“˜ PyrophaniteMn2+TiO3
Tiβ“˜ RutileTiO2
Tiβ“˜ TitaniteCaTi(SiO4)O
MnManganese
Mnβ“˜ AlleghanyiteMn52+(SiO4)2(OH)2
Mnβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Mnβ“˜ BementiteMn7Si6O15(OH)8
Mnβ“˜ Birnessite(Na,Ca)0.5(Mn4+,Mn3+)2O4 · 1.5H2O
Mnβ“˜ BustamiteCaMn2+(Si2O6)
Mnβ“˜ CaryopiliteMn32+Si2O5(OH)4
Mnβ“˜ FairfielditeCa2Mn2+(PO4)2 · 2H2O
Mnβ“˜ GalaxiteMn2+Al2O4
Mnβ“˜ GroutiteMn3+O(OH)
Mnβ“˜ JacobsiteMn2+Fe23+O4
Mnβ“˜ JohannseniteCaMn2+Si2O6
Mnβ“˜ KutnohoriteCaMn2+(CO3)2
Mnβ“˜ Tantalite-(Mn)Mn2+Ta2O6
Mnβ“˜ Piemontite(CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH)
Mnβ“˜ PyrolusiteMn4+O2
Mnβ“˜ PyrophaniteMn2+TiO3
Mnβ“˜ PyroxmangiteMn2+SiO3
Mnβ“˜ RhodochrositeMnCO3
Mnβ“˜ RhodoniteCaMn3Mn[Si5O15]
Mnβ“˜ SpessartineMn32+Al2(SiO4)3
Mnβ“˜ Tantalite(Mn,Fe)(Ta,Nb)2O6
Mnβ“˜ TephroiteMn22+SiO4
Mnβ“˜ Zoisite var. Thulite{Ca2}{Al,Mn33+}(Si2O7)(SiO4)O(OH)
Mnβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
Mnβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
FeIron
Feβ“˜ Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2
Feβ“˜ AegirineNaFe3+Si2O6
Feβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Feβ“˜ AnniteKFe32+(AlSi3O10)(OH)2
Feβ“˜ AlmandineFe32+Al2(SiO4)3
Feβ“˜ BabingtoniteCa2(Fe,Mn)FeSi5O14(OH)
Feβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ Cordierite(Mg,Fe)2Al3(AlSi5O18)
Feβ“˜ CronstedtiteFe22+Fe3+((Si,Fe3+)2O5)(OH)4
Feβ“˜ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feβ“˜ Fahlunite(Mg,Fe)Al2Si3O10 · 2H2O
Feβ“˜ Axinite-(Fe)Ca2Fe2+Al2BSi4O15OH
Feβ“˜ Ferro-actinolite◻Ca2Fe52+(Si8O22)(OH)2
Feβ“˜ Columbite-(Fe)Fe2+Nb2O6
Feβ“˜ GoethiteΞ±-Fe3+O(OH)
Feβ“˜ GraftoniteFe2+Fe22+(PO4)2
Feβ“˜ Grunerite◻{Fe22+}{Fe52+}(Si8O22)(OH)2
Feβ“˜ HastingsiteNaCa2(Fe42+Fe3+)(Si6Al2)O22(OH)2
Feβ“˜ HematiteFe2O3
Feβ“˜ IlmeniteFe2+TiO3
Feβ“˜ JacobsiteMn2+Fe23+O4
Feβ“˜ Maghemite(Fe3+0.670.33)Fe23+O4
Feβ“˜ MagnetiteFe2+Fe23+O4
Feβ“˜ Ilmenite var. Iron(III)-bearing Ilmenite(Fe2+,Fe3+)TiO3
Feβ“˜ MarcasiteFeS2
Feβ“˜ MelanteriteFe2+(H2O)6SO4 · H2O
Feβ“˜ NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2O
Feβ“˜ PyriteFeS2
Feβ“˜ PyrrhotiteFe1-xS
Feβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Feβ“˜ ScorzaliteFe2+Al2(PO4)2(OH)2
Feβ“˜ SideriteFeCO3
Feβ“˜ Tantalite(Mn,Fe)(Ta,Nb)2O6
Feβ“˜ TriphyliteLiFe2+PO4
Feβ“˜ VivianiteFe2+Fe22+(PO4)2 · 8H2O
Feβ“˜ VesuvianiteCa19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9
Feβ“˜ Ferri-ghoseite◻[Mn2+Na][Mg4Fe3+]Si8O22(OH)2
CuCopper
Cuβ“˜ AzuriteCu3(CO3)2(OH)2
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ MalachiteCu2(CO3)(OH)2
Cuβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Cuβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
ZnZinc
Znβ“˜ GahniteZnAl2O4
Znβ“˜ SphaleriteZnS
SrStrontium
Srβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
YYttrium
Yβ“˜ Xenotime-(Y)Y(PO4)
ZrZirconium
Zrβ“˜ ZirconZr(SiO4)
Zrβ“˜ Zircon var. CyrtoliteZr[(SiO4),(OH)4]
NbNiobium
Nbβ“˜ BismutotantaliteBi(Ta,Nb)O4
Nbβ“˜ Columbite-(Fe)Fe2+Nb2O6
Nbβ“˜ Pyrochlore GroupA2Nb2(O,OH)6Z
Nbβ“˜ Tantalite(Mn,Fe)(Ta,Nb)2O6
MoMolybdenum
Moβ“˜ MolybdeniteMoS2
Moβ“˜ PowelliteCa(MoO4)
SnTin
Snβ“˜ CassiteriteSnO2
CsCaesium
Csβ“˜ Pollucite(Cs,Na)2(Al2Si4O12) · 2H2O
BaBarium
Baβ“˜ BaryteBaSO4
Baβ“˜ Microcline var. Hyalophane(K,Ba)[Al(Si,Al)Si2O8]
Baβ“˜ Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 · 3-4H2O
CeCerium
Ceβ“˜ Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)
Ceβ“˜ Monazite-(Ce)Ce(PO4)
TaTantalum
Taβ“˜ BismutotantaliteBi(Ta,Nb)O4
Taβ“˜ Tantalite-(Mn)Mn2+Ta2O6
Taβ“˜ Microlite GroupA2-mTa2X6-wZ-n
Taβ“˜ Tantalite(Mn,Fe)(Ta,Nb)2O6
WTungsten
Wβ“˜ ScheeliteCa(WO4)
PbLead
Pbβ“˜ FourmarieritePb(UO2)4O3(OH)4 · 4H2O
Pbβ“˜ VandendriesscheitePbU7O22 · 12H2O
BiBismuth
Biβ“˜ BismutotantaliteBi(Ta,Nb)O4
Biβ“˜ BismuthiniteBi2S3
Biβ“˜ Bismutite(BiO)2CO3
Biβ“˜ SillΓ©niteBi12SiO20
ThThorium
Thβ“˜ ThoriteTh(SiO4)
Thβ“˜ Thorite var. Thorogummite(Th,U)(SiO4)1-x(OH)4x
UUranium
Uβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Uβ“˜ BecquereliteCa(UO2)6O4(OH)6 · 8H2O
Uβ“˜ FourmarieritePb(UO2)4O3(OH)4 · 4H2O
Uβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Uβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Uβ“˜ PhosphuranyliteKCa(H3O)3(UO2)7(PO4)4O4 · 8H2O
Uβ“˜ Thorite var. Thorogummite(Th,U)(SiO4)1-x(OH)4x
Uβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
Uβ“˜ UraniniteUO2
Uβ“˜ UranophaneCa(UO2)2(SiO3OH)2 · 5H2O
Uβ“˜ VandendriesscheitePbU7O22 · 12H2O

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References

 
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