Green's Farm locality (Roxbury garnet mine; Roxbury Falls garnet mine; Garnet Hill), Roxbury, Litchfield County, Connecticut, USAi
| Regional Level Types | |
|---|---|
| Green's Farm locality (Roxbury garnet mine; Roxbury Falls garnet mine; Garnet Hill) | Quarry (Abandoned) |
| Roxbury | Town |
| Litchfield County | County |
| Connecticut | State |
| USA | Country |
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Latitude & Longitude (WGS84):
41° 30' 24'' North , 73° 18' 11'' West
Latitude & Longitude (decimal):
Type:
Quarry (Abandoned) - last checked 2023
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Heritage Village | 3,736 (2017) | 5.9km |
| Southbury | 19,836 (2017) | 8.0km |
| Woodbury | 9,755 (2017) | 8.9km |
| Woodbury Center | 1,294 (2017) | 9.2km |
| Newtown | 1,967 (2017) | 10.3km |
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 | 18km |
| Bristol Gem & Mineral Club | Bristol, Connecticut | 35km |
| New Haven Mineral Club | New Haven, Connecticut | 38km |
| Lapidary and Mineral Society of Central Connecticut | Meriden, Connecticut | 41km |
An almandine garnet occurrence in schist. Dodecahedral almandine porphyroblast crystals are extremely abundant and well-formed and reach over 2.5 cm along a crystal edge. Staurolite is also common, rarer as 60 x 120-degree twins though. The other minerals are rare or are rock-forming.
The open pit mine is just north of the county line, in Roxbury (the southern part of town is called Roxbury Falls). Lane (1904) visited just after the operations closed:
Hiller (1983) provides a summary of the mine's operations. He notes that it was listed by Edward Dana of Yale University in his 1860s thesis on mineralogy and that the deposit was listed in editions of Dana's Textbook of Mineralogy as an original Dana locality.
Elwell (1938) noted the presence of garnet in local roads, largely unpaved at that time:
"This place has been overgrown with bushes but recently the owner cut them down and is now charging collectors and others 25c to go on the dumps. Some of the material of the dumps has been used for top dressing on old back roads in that section; one day I picked up 2,000 garnets off such roads."
Yedlin (1947) reports that the charge was 50c on August 10, 1941. He believed that the owner of the property was Lyman Greene.
NOTE: As of November 2012 access to the site was closed by the new owners of the Perkins Road (Southbury) property immediately to the south of the quarries.
The open pit mine is just north of the county line, in Roxbury (the southern part of town is called Roxbury Falls). Lane (1904) visited just after the operations closed:
There are three mines, all owned by different companies, a mile or more apart, and all deserted now. The last one was worked in 1901 and 1902 by the Armour Company of Chicago, but was abandoned before much work had been done.
The garnets were separated from the white, shiny, talcose schist by being ground and run over shakers, leaving the garnets whole or nearly so, to be put in bags to be shipped to be ground for garnet paper, and other abrasive purposes.
As the mines and buildings were closed and deserted, I could get very little information, but the garnets were used for the different grades of garnet paper, and owing to the lack of water for the boilers, and also for separating the materials, the mines were abandoned.
Another version was that Carborundum could be made cheaper and used to better advantage.
The largest mine—as it is called—though it looks like three great reservoirs, one below the other, are great pits or open quarries, about 400 feet in diameter and 50 feet deep, with garnets in sight everywhere in great quantities, like raisins in a pudding, but like the pudding, not many in a small piece, unless you are lucky. The other two mines have only one small opening apiece.
The size of the garnets run very near the same size, not many an inch in diameter, and rarely one is found two inches, but most of them are half an inch, and as they become exposed to the atmosphere, become rusty and dull.
Then again there are more black...found than any other color and very few show color. When the mines were working and they opened a new vein, some very perfect ones were secured, though most of them were bruised by the blasting.
It is a hard job to find a nice group in a schist matrix that can be developed sufficiently to grace the collector's cabinet, and the larger ones are most always found in single crystals.
The miners say that there was an offer of a thousand dollars for a perfect garnet, and I can safely say that I never heard of any one that was able to claim it.
I will not try to describe them, as all collectors are familiar with the garnets of this locality, but will say that their form is a dodecahedron, and a few have their edges truncated, but no complex crystals have been reported.
The ledges and rocks in the vicinity, especially where they are weathered or uncovered, are coated with crystals of staurolite, and some very perfect, though not large ones, are found, but they are seldom over an inch long.
The garnets were separated from the white, shiny, talcose schist by being ground and run over shakers, leaving the garnets whole or nearly so, to be put in bags to be shipped to be ground for garnet paper, and other abrasive purposes.
As the mines and buildings were closed and deserted, I could get very little information, but the garnets were used for the different grades of garnet paper, and owing to the lack of water for the boilers, and also for separating the materials, the mines were abandoned.
Another version was that Carborundum could be made cheaper and used to better advantage.
The largest mine—as it is called—though it looks like three great reservoirs, one below the other, are great pits or open quarries, about 400 feet in diameter and 50 feet deep, with garnets in sight everywhere in great quantities, like raisins in a pudding, but like the pudding, not many in a small piece, unless you are lucky. The other two mines have only one small opening apiece.
The size of the garnets run very near the same size, not many an inch in diameter, and rarely one is found two inches, but most of them are half an inch, and as they become exposed to the atmosphere, become rusty and dull.
Then again there are more black...found than any other color and very few show color. When the mines were working and they opened a new vein, some very perfect ones were secured, though most of them were bruised by the blasting.
It is a hard job to find a nice group in a schist matrix that can be developed sufficiently to grace the collector's cabinet, and the larger ones are most always found in single crystals.
The miners say that there was an offer of a thousand dollars for a perfect garnet, and I can safely say that I never heard of any one that was able to claim it.
I will not try to describe them, as all collectors are familiar with the garnets of this locality, but will say that their form is a dodecahedron, and a few have their edges truncated, but no complex crystals have been reported.
The ledges and rocks in the vicinity, especially where they are weathered or uncovered, are coated with crystals of staurolite, and some very perfect, though not large ones, are found, but they are seldom over an inch long.
Hiller (1983) provides a summary of the mine's operations. He notes that it was listed by Edward Dana of Yale University in his 1860s thesis on mineralogy and that the deposit was listed in editions of Dana's Textbook of Mineralogy as an original Dana locality.
[In the 1880s] A mill was constructed at Roxbury Falls. In Roxbury, another mill was built, about 1890, by the Armour Company. When the railroad was completed through Roxbury in 1867, the little rural farming town awakened. Opportunity came with the railroad and it became economically feasable [sic] to transport heavy loads to the New York and southern Connecticut markets. A burst of mining and quarrying activity occured [sic], with the reopening of the iron deposits at Mine Hill, Roxbury, and the quarrying of building stone near the iron mine.
The garnet production was accomplished by a milling process. The rocks were crushed and sorted by gravity to separate the garnets from the much lighter schist matrix. Then, using differing grades of screens, the garnets were sorted to grit sizes for industrial applications....The soft mica matrix was soon quarried out and a harder quartz based matrix was encountered. This made it more difficult to separate the garnets from the matrix. Operations came to a halt before 1900 when discoveries in Massachusetts, Vermont and Canada were made. The Canadian deposit was more concentrated and had a softer matrix. The milling equipment from the Roxbury Falls operation was dissassembled [sic] and transported to Canada.
The land which had been cleared for mining operations was now suitable for a more traditional Connecticut industry, dairy farming. As seen during a visit in the 1950's, the farm was a producing operation, run by Mr. Green for whom the garnet deposit is now named. At that time it was necessary to be careful in harvesting loose garnets on the surface because some apparent "garnets" were dropped by Mr. Green's sheep! The farm is no longer in operation; it closed with the passing of Mr. Green in the late 1970's. The current owner of the land at the end of Perkin's Road allows collectors to park their cars on her property for a $1.00 fee per car. The town of Roxbury has the rights to excavate the mine dumps for use as road fill. Some roadbeds, especially the dirt roads near Judd's Bridge in northern Roxbury, were constructed with this material and show fine garnets loose in the soil at the roadside. Passing cars pop them out of the matrix and clean them, but seldom crush them.
The garnet production was accomplished by a milling process. The rocks were crushed and sorted by gravity to separate the garnets from the much lighter schist matrix. Then, using differing grades of screens, the garnets were sorted to grit sizes for industrial applications....The soft mica matrix was soon quarried out and a harder quartz based matrix was encountered. This made it more difficult to separate the garnets from the matrix. Operations came to a halt before 1900 when discoveries in Massachusetts, Vermont and Canada were made. The Canadian deposit was more concentrated and had a softer matrix. The milling equipment from the Roxbury Falls operation was dissassembled [sic] and transported to Canada.
The land which had been cleared for mining operations was now suitable for a more traditional Connecticut industry, dairy farming. As seen during a visit in the 1950's, the farm was a producing operation, run by Mr. Green for whom the garnet deposit is now named. At that time it was necessary to be careful in harvesting loose garnets on the surface because some apparent "garnets" were dropped by Mr. Green's sheep! The farm is no longer in operation; it closed with the passing of Mr. Green in the late 1970's. The current owner of the land at the end of Perkin's Road allows collectors to park their cars on her property for a $1.00 fee per car. The town of Roxbury has the rights to excavate the mine dumps for use as road fill. Some roadbeds, especially the dirt roads near Judd's Bridge in northern Roxbury, were constructed with this material and show fine garnets loose in the soil at the roadside. Passing cars pop them out of the matrix and clean them, but seldom crush them.
Elwell (1938) noted the presence of garnet in local roads, largely unpaved at that time:
"This place has been overgrown with bushes but recently the owner cut them down and is now charging collectors and others 25c to go on the dumps. Some of the material of the dumps has been used for top dressing on old back roads in that section; one day I picked up 2,000 garnets off such roads."
Yedlin (1947) reports that the charge was 50c on August 10, 1941. He believed that the owner of the property was Lyman Greene.
NOTE: As of November 2012 access to the site was closed by the new owners of the Perkins Road (Southbury) property immediately to the south of the quarries.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
14 valid minerals.
Detailed Mineral List:
| ✪ Almandine Formula: Fe2+3Al2(SiO4)3 Habit: dodecahedral Colour: maroon to purple, nearly black Fluorescence: none Description: Crystals can reach over 2.5 cm on an edge. Unpublished XRF analysis by Harold Moritz found 98% Fe of total Fe+Mn content. Hiller (1983) noted that some gem quality garnets will show 4-star rays if properly cut. |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ Chalcopyrite Formula: CuFeS2 References: |
| ⓘ Clinochlore Formula: Mg5Al(AlSi3O10)(OH)8 |
| ⓘ Gypsum Formula: CaSO4 · 2H2O Habit: microscopic clusters Description: Found as small clusters under overhanging ledges. |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Ilmenite Formula: Fe2+TiO3 References: |
| ⓘ Kyanite Formula: Al2(SiO4)O |
| ⓘ 'Limonite' |
| ⓘ Löllingite Formula: FeAs2 |
| ⓘ Magnetite Formula: Fe2+Fe3+2O4 References: |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Pyrrhotite Formula: Fe1-xS |
| ⓘ Quartz Formula: SiO2 |
| ✪ Staurolite Formula: Fe2+2Al9Si4O23(OH) Habit: elongated prisms, penetration twins Colour: dark brown Description: Crystals reach about 3 cm long, but typically around 1 cm. |
| ⓘ 'Tourmaline' Formula: AD3G6(T6O18)(BO3)3X3Z Habit: elongated prisms with trigonal termiations Colour: black to dark brown Description: Very small crystals to 3.5 mm in the schist matrix. Probably dravite or schorl. References: |
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrrhotite | 2.CC.10 | Fe1-xS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Löllingite | 2.EB.15a | FeAs2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Magnetite | 4.BB.05 | Fe2+Fe3+2O4 |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | Ilmenite | 4.CB.05 | Fe2+TiO3 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Gypsum | 7.CD.40 | CaSO4 · 2H2O |
| Group 9 - Silicates | |||
| ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
| ⓘ | Kyanite | 9.AF.15 | Al2(SiO4)O |
| ⓘ | Staurolite | 9.AF.30 | Fe2+2Al9Si4O23(OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Clinochlore | 9.EC.55 | Mg5Al(AlSi3O10)(OH)8 |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ⓘ | 'Limonite' | - | |
| ⓘ | 'Tourmaline' | - | AD3G6(T6O18)(BO3)3X3Z |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| H | ⓘ Gypsum | CaSO4 · 2H2O |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| B | Boron | |
| B | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| O | Oxygen | |
| O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| O | ⓘ Gypsum | CaSO4 · 2H2O |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Ilmenite | Fe2+TiO3 |
| O | ⓘ Kyanite | Al2(SiO4)O |
| O | ⓘ Magnetite | Fe2+Fe23+O4 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| O | ⓘ Tourmaline | AD3G6(T6O18)(BO3)3X3Z |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Mg | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| Al | Aluminium | |
| Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| Al | ⓘ Kyanite | Al2(SiO4)O |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| Si | Silicon | |
| Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Clinochlore | Mg5Al(AlSi3O10)(OH)8 |
| Si | ⓘ Kyanite | Al2(SiO4)O |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| S | Sulfur | |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Gypsum | CaSO4 · 2H2O |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Pyrrhotite | Fe1-xS |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Gypsum | CaSO4 · 2H2O |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Ti | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | Iron | |
| Fe | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Ilmenite | Fe2+TiO3 |
| Fe | ⓘ Löllingite | FeAs2 |
| Fe | ⓘ Magnetite | Fe2+Fe23+O4 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Pyrrhotite | Fe1-xS |
| Fe | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| As | Arsenic | |
| As | ⓘ Löllingite | FeAs2 |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Piedmontia DomainDomain
- Taconic ArcVolcanic Arc
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Green's Farm locality, Roxbury, Litchfield County, Connecticut, USA