New England Mining Company Quarry (Roebling Mine; Hewitt's Mine), Upper Merryall, New Milford, Litchfield County, Connecticut, USAi
Regional Level Types | |
---|---|
New England Mining Company Quarry (Roebling Mine; Hewitt's Mine) | Quarry |
Upper Merryall | Village |
New Milford | Town |
Litchfield County | County |
Connecticut | State |
USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
41° 39' 22'' North , 73° 26' 5'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
New Preston | 1,182 (2017) | 7.2km |
Kent | 2,858 (2017) | 8.4km |
New Milford | 6,523 (2017) | 9.1km |
Sherman | 3,827 (2017) | 9.9km |
Washington | 3,466 (2017) | 10.7km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
Club | Location | Distance |
---|---|---|
Danbury Mineralogical Society | Danbury, Connecticut | 29km |
Bristol Gem & Mineral Club | Bristol, Connecticut | 40km |
Mid-Hudson Valley Gem and Mineral Society Inc. | Poughkeepsie, New York | 41km |
Mindat Locality ID:
6817
Long-form identifier:
mindat:1:2:6817:1
GUID (UUID V4):
0cc0903a-1c89-4e98-a405-928e7901aec0
Several granite pegmatites that, according to Sterrett (1923), were first mined by the New England Mining Co. (Elwell, 1937) in 2 quarries for mica and feldspar between 1880-1900, but gem beryl proved to be a valuable by-product. Many crystals of beryl, some of them more than a foot in diameter, were found in the quarry. In 1896 4,000 gemstones were reportedly cut (Hawes, 1984). Five cut beryl gemstones of various colors "all from Litchfield County" (Clarke, 1889) were donated to the Smithsonian. The catalog (Merrill, 1922) also shows two others, the largest of all being 40.44 carats (no. 1037). At that time the mine was owned by S. L. Wilson and George Roebling. The operation was financed in part by Washington A. Roebling of New Jersey, an avid mineralogist and son of Brooklyn Bridge designer John A. Roebling.
At the turn of the century, new operators discovered uranium salts there and charged patrons to sit and bask in natural radiation thought to cure arthritis (Hawes, 1984).
George Roebling solely owned it in 1914, when he still had a few specimens showing the quality of the gem material.
Cameron and others (1954) reported that in 1944 the property was owned by Henry Orzech. One ton of beryl is said to have been recovered from the no. 1 quarry by Mr. Orzechβs sons since 1936. It was worked sporadically after then. In the summer of 1944, Cyril Ulman of Guilford, Conn., worked the no. 2 quarry for mica for a period of 2 weeks.
Inspired by Roebling's finds, prospector Howard Hewitt worked the property extensively for gem beryl from at least 1953 until the 1970s. In August 1953, Hewitt shipped 2,300 pounds of beryl to the Beryllium Corporation in Reading, Pennsylvania, which may have netted him between $300 and $600/ton (Anonymous, 1953). During the 1970s until his death in 1981, Howard Hewitt reportedly worked Roebling only sporadically. During this time he worked mainly at the Sawmill Quarry in Haddam (after his brother Herb, who had previously worked Sawmill, passed away).
After Howard, the quarry was more vigorously worked for gem beryl, much of the remaining intact pegmatite was quarried and, with previously loose material, was screened through a trommel.
As of 2013, the property is still owned by the Orzech family and remains closed.
Note: Collectors who were there in the 1970s report seeing minerals from the Sawmill Quarry near Howard's work shack at Roebling. A 1970s advertisement the Hewitt's created shows gemstones mostly from Roebling, but also from Sawmill. The Hewitt's also traded minerals with the owners of the Slocum Prospect http://www.mindat.org/loc-6346.html in East Hampton, Conn. and the Walden Gem Mine http://www.mindat.org/loc-6749.html in Portland, Conn. (both fee collecting sites in the 1960s and 1970s). So some specimens in collections reportedly from or associated with Roebling material may be from these other localities.
The best geological description comes from Cameron et al (1954), below are excerpts:
The workings consist of two opencuts, from one of which a short underground crosscut and drift have been run. The no. 1 quarry is 420 feet long and 60 feet in maximum width and depth. It is covered by vegetation and partly backfilled. The no. 2 quarry is 90 feet long, 40 feet wide and 20 feet deep.
Five pegmatite sheets or lenses have been mined. The bodies dip moderately to steeply northwest and are enclosed in silicified quartz-mica schist [Dalton Formation]. The schist has been injected with narrow pegmatites. Contact metamorphism has produced abundant subhedral metacrysts of garnet and tourmaline in the schist adjacent to the contacts with pegmatite.
The no. 1 quarry is in a pegmatite body that averages 30 feet in thickness, strikes N. 55Β° E., and dips 60Β° NW. Sterrett (p. 64) states that it is reported to be thinner near the bottom of the cut than at the surface. The small part of the pegmatite exposed in 1944 consisted of three lithologic units:
1. Border zone, lying adjacent to the wall rock contact.
2. Perthite [microcline]-quartz zone, lying inside the border zone. [This zone contained visible beryl in 1944]
3. Muscovite-perthite [microcline] unit, poorly exposed near the center of the pegmatite.
Accessory minerals are biotite [annite], and tourmaline [schorl], garnet [probably almandine], and beryl.
Four pegmatites (A to D, fig. 125) are exposed in the no. 2 quarry. They strike N. 40Β° E. and dip to the north at moderate to steep angles. Probably the two northermost pegmatites are roots of a single pegmatite which lay directly above the present topographic surface. Outcrops on the southwestern side of the quarry indicate a similar relationship between the two southernmost pegmatites.
The pegmatites range from 5 to 20 feet in thickness and consist essentially of quartz and perthite [microcline] with various amounts of muscovite, plagioclase [albite], and accessory biotite [annite], and tourmaline [schorl], garnet [probably almandine], and beryl. Small biotite [annite] and muscovite books occur as fracture fillings in joints cutting pegmatite A.
Five pegmatite sheets or lenses have been mined. The bodies dip moderately to steeply northwest and are enclosed in silicified quartz-mica schist [Dalton Formation]. The schist has been injected with narrow pegmatites. Contact metamorphism has produced abundant subhedral metacrysts of garnet and tourmaline in the schist adjacent to the contacts with pegmatite.
The no. 1 quarry is in a pegmatite body that averages 30 feet in thickness, strikes N. 55Β° E., and dips 60Β° NW. Sterrett (p. 64) states that it is reported to be thinner near the bottom of the cut than at the surface. The small part of the pegmatite exposed in 1944 consisted of three lithologic units:
1. Border zone, lying adjacent to the wall rock contact.
2. Perthite [microcline]-quartz zone, lying inside the border zone. [This zone contained visible beryl in 1944]
3. Muscovite-perthite [microcline] unit, poorly exposed near the center of the pegmatite.
Accessory minerals are biotite [annite], and tourmaline [schorl], garnet [probably almandine], and beryl.
Four pegmatites (A to D, fig. 125) are exposed in the no. 2 quarry. They strike N. 40Β° E. and dip to the north at moderate to steep angles. Probably the two northermost pegmatites are roots of a single pegmatite which lay directly above the present topographic surface. Outcrops on the southwestern side of the quarry indicate a similar relationship between the two southernmost pegmatites.
The pegmatites range from 5 to 20 feet in thickness and consist essentially of quartz and perthite [microcline] with various amounts of muscovite, plagioclase [albite], and accessory biotite [annite], and tourmaline [schorl], garnet [probably almandine], and beryl. Small biotite [annite] and muscovite books occur as fracture fillings in joints cutting pegmatite A.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
19 valid minerals. 1 erroneous literature entry.
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
β Albite Formula: Na(AlSi3O8) Habit: anhedral Colour: white Description: Major component of the pegmatite. |
βͺ Almandine Formula: Fe2+3Al2(SiO4)3 Habit: trapezohedral and rhombic dodecahedral Colour: maroon to nearly black Description: An accessory in the pegmatites, also abundant subhedral metacrysts of garnet in the schist adjacent to the contacts with pegmatite. Januzzi (1959) reports finding in one isolated pegmatite mass, scores of two types of garnet crystals having both distinct dodecahedral and trapezohedral forms. Ewell (1937) writes: "The garnets were extra large, some weighing one pound each." |
β Annite Formula: KFe2+3(AlSi3O10)(OH)2 Habit: anhedral Colour: black Description: fka biotite, a minor accessory in the pegmatites. |
β Bertrandite ? Formula: Be4(Si2O7)(OH)2 Description: Included in the reference in a list of minerals with no supporting information. |
βͺ Beryl Formula: Be3Al2(Si6O18) Habit: anhedral elongated prisms Colour: pale green, yellow to honey, blue Description: According to Cameron et al (1954), beryl is concentrated in the quartz-perthitic microcline zone in the the southwest half of no. 1 quarry as pale greenish-white, short, subhedral prisms, 3 inches in average length and 2 inches in average diameter. A 300-pound block of quartz and plagioclase found in the backfill contains at least 8 percent beryl. Also an accessory of the pegmatites in the no. 2 quarry. Sterrett (1923) reports βmany crystals of beryl, some of them more than a foot in diameterβ. Crystals are usually sheathed in mica and are poorly formed but internally contain some of the best gem beryl rough found in Connecticut. |
βͺ Beryl var. Aquamarine Formula: Be3Al2Si6O18 Habit: subhedral elongated prisms Colour: blue, blue-green Description: Much more rare than the common green beryl or yellow beryl, but a 40.44-carat aquamarine (no. 1037) is in the Smithsonian. |
βͺ Beryl var. Heliodor Formula: Be3Al2(Si6O18) Colour: yellow to honey Description: Crystals poorly formed, but internally hide some of the best gem rough from Connecticut, with deep golden yellow to honey color. |
β Columbite-(Fe) Formula: Fe2+Nb2O6 |
β Fluorapatite Formula: Ca5(PO4)3F Description: Included in just a list of minerals in one reference, but it is such a common accessory that it is certainly present. |
β 'Garnet Group' Formula: X3Z2(SiO4)3 Description: Probably almandine as is most pegmatitic garnet in Connecticut. |
βͺ 'Gummite' Description: Associated with uraninite, meta-autunite, uranophane, other alteration products. Fine gummite and uranophane pseudomorphs after uraninite have been found here. |
β Hematite ? Formula: Fe2O3 Description: Included in the reference in a list of minerals with no supporting documentation. |
β 'Limonite' Description: Common surficial alteration product staining other rocks and minerals. |
β Meta-autunite Formula: Ca(UO2)2(PO4)2 · 6H2O Description: Associated with uraninite, uranophane, "gummite" and other alteration products. |
β Metatorbernite Formula: Cu(UO2)2(PO4)2 · 8H2O Description: Associated with uraninite, meta-autunite, uranophane, "gummite" and other alteration products. |
β Microcline Formula: K(AlSi3O8) Habit: anhedral Description: A major component of the pegmatites. In the perthitic microcline-quartz zone of the No.1 quarry, in large anhedral crystals as much as 10 feet long. In the eastern part of the north wall, the zone is richest in massive perthitic microcline toward the center of the pegmatite, and this suggests the presence of a perthitic microcline core. Locally, the microcline is veined and partly replaced with granular milky quartz, deformed muscovite and pink-red garnet. Graphic granite is fairly common. |
β Muscovite Formula: KAl2(AlSi3O10)(OH)2 Habit: tabular subhedral Colour: green to pale ruby Description: In the microcline-quartz zone of the no. 1 quarry it occurs in small quantities as books 3 inches in diameter. The muscovite-microcline unit of this pegmatite consists chiefly of diversely oriented scrap muscovite books forming 70 to 90 percent of the total volume. One block of βsolid micaβ of irregular shape blasted loose from this zone measured 4 feet thick and 8 feet long. http://www.mindat.org/photo-204409.html
Crystals average 1 inch in diameter but range from 1/8 to 6 inches across. There are three types of mica deposits in the 4 pegmatites of the no. 2 quarry: pod, wall-zone, and disseminated. Pegmatite A has a concentration of books as much as 1 foot in diameter, Pegmatite B exhibits a lean book mica-bearing zone composed of quartz, albite, and muscovite. The books are 3 to 4 inches in average diameter. Pegmatites C and D are disseminated mica deposits. |
β Opal Formula: SiO2 · nH2O Habit: encrustations Fluorescence: green Description: Commonly forms crusts in cracks and joints in pegmatites, best found by its bright green fluorescence under SW UV illumination. |
β Opal var. Opal-AN Formula: SiO2 · nH2O Habit: encrustations Fluorescence: green Description: Commonly forms crusts in cracks and joints in pegmatites, best found by its bright green fluorescence under SW UV illumination. |
β Phosphuranylite Formula: KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
β 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 Quartz Formula: SiO2 Habit: anhedral Colour: milky to smoky Description: Major component of the pegmatite. |
β Schorl Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) Habit: subhedral, elongated prisms Colour: black Description: Common accessory in the pegmatites, especially in the border zone forming subhedral needles from ΒΌ inch to 3 inches long, oriented normal to the contact, and in the surrounding schist. |
β 'Tourmaline' Formula: AD3G6 (T6O18)(BO3)3X3Z |
β Uraninite Formula: UO2 Habit: octahedral Description: Associated with secondaries, sometimes pseudomorphed by uranophane and "gummite". |
βͺ Uranophane Formula: Ca(UO2)2(SiO3OH)2 · 5H2O Description: Associated with uraninite, meta-autunite, "gummite", other alteration products. Fine gummite and uranophane pseudomorphs after uraninite have been found here. |
β Zircon Formula: Zr(SiO4) Colour: brown Description: Accessory in the pegmatites. References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 4 - Oxides and Hydroxides | |||
---|---|---|---|
β | Hematite ? | 4.CB.05 | Fe2O3 |
β | Quartz | 4.DA.05 | SiO2 |
β | Opal | 4.DA.10 | SiO2 Β· nH2O |
β | var. Opal-AN | 4.DA.10 | SiO2 Β· nH2O |
β | Pyrolusite ? | 4.DB.05 | Mn4+O2 |
β | Columbite-(Fe) | 4.DB.35 | Fe2+Nb2O6 |
β | Uraninite | 4.DL.05 | UO2 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
β | Fluorapatite | 8.BN.05 | Ca5(PO4)3F |
β | Metatorbernite | 8.EB.10 | Cu(UO2)2(PO4)2 Β· 8H2O |
β | Meta-autunite | 8.EB.10 | Ca(UO2)2(PO4)2 Β· 6H2O |
β | Phosphuranylite | 8.EC.10 | KCa(H3O)3(UO2)7(PO4)4O4 Β· 8H2O |
Group 9 - Silicates | |||
β | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
β | Zircon | 9.AD.30 | Zr(SiO4) |
β | Uranophane | 9.AK.15 | Ca(UO2)2(SiO3OH)2 Β· 5H2O |
β | Bertrandite ? | 9.BD.05 | Be4(Si2O7)(OH)2 |
β | Beryl var. Heliodor | 9.CJ.05 | Be3Al2(Si6O18) |
β | 9.CJ.05 | Be3Al2(Si6O18) | |
β | var. Aquamarine | 9.CJ.05 | Be3Al2Si6O18 |
β | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
β | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
β | Annite | 9.EC.20 | KFe2+3(AlSi3O10)(OH)2 |
β | Microcline | 9.FA.30 | K(AlSi3O8) |
β | Albite | 9.FA.35 | Na(AlSi3O8) |
Unclassified | |||
β | 'Tourmaline' | - | AD3G6 (T6O18)(BO3)3X3Z |
β | 'Limonite' | - | |
β | 'Gummite' | - | |
β | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Annite | KFe32+(AlSi3O10)(OH)2 |
H | β Bertrandite | Be4(Si2O7)(OH)2 |
H | β Opal var. Opal-AN | SiO2 · nH2O |
H | β Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
H | β Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
H | β Muscovite | KAl2(AlSi3O10)(OH)2 |
H | β Opal | SiO2 · nH2O |
H | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
H | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
H | β Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Be | Beryllium | |
Be | β Beryl var. Aquamarine | Be3Al2Si6O18 |
Be | β Bertrandite | Be4(Si2O7)(OH)2 |
Be | β Beryl | Be3Al2(Si6O18) |
Be | β Beryl var. Heliodor | Be3Al2(Si6O18) |
B | Boron | |
B | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
B | β Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | Oxygen | |
O | β Albite | Na(AlSi3O8) |
O | β Annite | KFe32+(AlSi3O10)(OH)2 |
O | β Beryl var. Aquamarine | Be3Al2Si6O18 |
O | β Almandine | Fe32+Al2(SiO4)3 |
O | β Bertrandite | Be4(Si2O7)(OH)2 |
O | β Beryl | Be3Al2(Si6O18) |
O | β Columbite-(Fe) | Fe2+Nb2O6 |
O | β Fluorapatite | Ca5(PO4)3F |
O | β Hematite | Fe2O3 |
O | β Opal var. Opal-AN | SiO2 · nH2O |
O | β Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
O | β Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
O | β Microcline | K(AlSi3O8) |
O | β Muscovite | KAl2(AlSi3O10)(OH)2 |
O | β Opal | SiO2 · nH2O |
O | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
O | β Pyrolusite | Mn4+O2 |
O | β Quartz | SiO2 |
O | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
O | β Tourmaline | AD3G6 (T6O18)(BO3)3X3Z |
O | β Uraninite | UO2 |
O | β Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
O | β Zircon | Zr(SiO4) |
O | β Beryl var. Heliodor | Be3Al2(Si6O18) |
O | β Garnet Group | X3Z2(SiO4)3 |
F | Fluorine | |
F | β Fluorapatite | Ca5(PO4)3F |
Na | Sodium | |
Na | β Albite | Na(AlSi3O8) |
Na | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | Aluminium | |
Al | β Albite | Na(AlSi3O8) |
Al | β Annite | KFe32+(AlSi3O10)(OH)2 |
Al | β Beryl var. Aquamarine | Be3Al2Si6O18 |
Al | β Almandine | Fe32+Al2(SiO4)3 |
Al | β Beryl | Be3Al2(Si6O18) |
Al | β Microcline | K(AlSi3O8) |
Al | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Al | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Al | β Beryl var. Heliodor | Be3Al2(Si6O18) |
Si | Silicon | |
Si | β Albite | Na(AlSi3O8) |
Si | β Annite | KFe32+(AlSi3O10)(OH)2 |
Si | β Beryl var. Aquamarine | Be3Al2Si6O18 |
Si | β Almandine | Fe32+Al2(SiO4)3 |
Si | β Bertrandite | Be4(Si2O7)(OH)2 |
Si | β Beryl | Be3Al2(Si6O18) |
Si | β Opal var. Opal-AN | SiO2 · nH2O |
Si | β Microcline | K(AlSi3O8) |
Si | β Muscovite | KAl2(AlSi3O10)(OH)2 |
Si | β Opal | SiO2 · nH2O |
Si | β Quartz | SiO2 |
Si | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Si | β Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Si | β Zircon | Zr(SiO4) |
Si | β Beryl var. Heliodor | Be3Al2(Si6O18) |
Si | β Garnet Group | X3Z2(SiO4)3 |
P | Phosphorus | |
P | β Fluorapatite | Ca5(PO4)3F |
P | β Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
P | β Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
P | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
K | Potassium | |
K | β Annite | KFe32+(AlSi3O10)(OH)2 |
K | β Microcline | K(AlSi3O8) |
K | β Muscovite | KAl2(AlSi3O10)(OH)2 |
K | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Ca | Calcium | |
Ca | β Fluorapatite | Ca5(PO4)3F |
Ca | β Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
Ca | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
Ca | β Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Mn | Manganese | |
Mn | β Pyrolusite | Mn4+O2 |
Fe | Iron | |
Fe | β Annite | KFe32+(AlSi3O10)(OH)2 |
Fe | β Almandine | Fe32+Al2(SiO4)3 |
Fe | β Columbite-(Fe) | Fe2+Nb2O6 |
Fe | β Hematite | Fe2O3 |
Fe | β Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
Cu | Copper | |
Cu | β Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
Zr | Zirconium | |
Zr | β Zircon | Zr(SiO4) |
Nb | Niobium | |
Nb | β Columbite-(Fe) | Fe2+Nb2O6 |
U | Uranium | |
U | β Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
U | β Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
U | β Phosphuranylite | KCa(H3O)3(UO2)7(PO4)4O4 · 8H2O |
U | β Uraninite | UO2 |
U | β Uranophane | Ca(UO2)2(SiO3OH)2 · 5H2O |
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Laurentides DomainDomain
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.