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Copper Valley Mine, Cheshire, New Haven County, Connecticut, USAi
Regional Level Types
Copper Valley MineMine
CheshireTown
New Haven CountyCounty
ConnecticutState
USACountry

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Latitude & Longitude (WGS84):
41° 29' 7'' North , 72° 52' 5'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Cheshire29,443 (2017)3.1km
Cheshire Village5,786 (2017)3.2km
Wallingford17,712 (2017)4.9km
Wallingford Center18,209 (2017)5.7km
Meriden59,988 (2017)7.8km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Lapidary and Mineral Society of Central ConnecticutMeriden, Connecticut8km
New Haven Mineral ClubNew Haven, Connecticut20km
Bristol Gem & Mineral ClubBristol, Connecticut22km
Danbury Mineralogical SocietyDanbury, Connecticut50km
Mindat Locality ID:
10340
Long-form identifier:
mindat:1:2:10340:7
GUID (UUID V4):
0
Other/historical names associated with this locality:
Belcher's Mine, Bellamy's Mine, Munson's Mine


A complex of pits, adits and shafts in two clusters straddling a diabase dike. Coordinates are for the northern cluster, the southern cluster is at 41.483309 -72.869056.

Harte (1944) provides some details of its history:

In what was then a part of Wallingford, but now in the southeast corner of Cheshire, one John Parker, in 1711, was reported to have found copper and perhaps other valuable metals on his farm, which was on “Milkingyard Hill”....

Shortly after this, William Partridge of Newbury and Jonathan Belcher of Boston, merchant, both of the Province of Massachusetts Bay, entered into Articles of Agreement with the town of Wallingford for the opening of mines there, the miners, artificers and laborers connected with them to be exempted from all civil and military duties and all taxes; the lease to run eight years, with the privilege of renewal for a period “not exceeding 500 years in the whole”.


On June 16, 1714 John Parker was given 10 shillings so that "Parker be forever hereafter quiet and contented with respect to ye mine money."

Mining continued through at least 1724, after which Harte (1944) says there are no records until:

October of 1854 Truman Bristol granted Sanderson Smith mining rights on a 30 acre tract of land at 'Copper Valley'. Smith failed to meet his obligations, and in September of 1866 Bristol gave Charles Munson and Leonard Pardee the entire and exclusive right of mining, quarrying, digging, and excavating, for minerals and metals...

There is practically nothing regarding the amount of ore raised. Munson seems to have worked the mine himself part of the time, and on other occasions to have leased the property. In 1874 Nathan Peck and Isaac Anderson, lessees, agreed to spend $25,000 'because of the increasing flow of water in shafts and levels'; to deepen the shaft somewhat for a water receiver; to extend easterly the drift on the line of the east and west vein; and to install a portable steam hoisting engine.

Munson took great interest in the mine, and personally went to great lengths to make it a success. Ore of a superior quality was obtained, but the shafts, sunk to a depth of more than one hundred feet, and the drifts run from them, encountered water in greater quantity than could be controlled. Munson is said to have sunk $50,000 of his own money in the project, and various lessees also spent substantial sums, but to no avail, and the leased property eventually reverted to Truman Bristol. However, Mr. George R. Johnson of Copper Valley said that Mr. Munson, at that time in his ninetieth year, wrote him that he had not lost faith in the mine; that he felt that they not gone down deep enough 'to remove the cover off the precious metal'.


However Shepard (1837) apparently fills in some of the missing years with this account of what appears from it's geographical location to be the same place:

It was commenced in 1812 [sic - he must mean 1712], by commissioners appointed by the King's bench. Tradition says that a shaft ninety feet deep was sunk, and of a size sufficient in two places to receive a large dwelling house. Two ship-loads of ore, it is also reported, were transmitted at this period to England. Some attempts were made to renew the enterprise early the present century, but were soon abandoned. The mine is at present owned by Mr. AARON BELLAMY of Otsego, N. Y., who is a descendant of the individual interested in the first exploration. This gentleman, aided by a company in Canada, commenced the clearing of the mine in 1836. The shaft was completely occupied by timbers and rubbish. A small steam-engine is made use of for lifting out the water. They had descended about twenty-five feet in August last, and among the materials brought up, good vitreous copper [chalcocite] was observed, often associated with heavy spar [barite], and occasionally in distinct crystals (578b). On the north side of the shaft, a dyke of trap is visible, having the width of three feet, in contact with which the ore seems to occur. The intersected sandstone for several feet on each side, is more or less stained with malachite.


Schairer (1931) had this to say:

Large chunks of chalcocite and bornite covered with malachite are still available both on the dumps and in the exposed vein in trap rock. Calcite crystals (dog-tooth spar) are common; talc is rare.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


10 valid minerals.

Detailed Mineral List:

Allophane
Formula: (Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Habit: encrustations
Colour: pale blue
Baryte
Formula: BaSO4
Habit: cleavable masses
Colour: white
Bornite
Formula: Cu5FeS4
Habit: massive
Description: Large chunks of chalcocite and bornite covered with malachite (Schairer, 1931).
Calcite
Formula: CaCO3
Habit: scalenohedral
Fluorescence: orange-red to deep pink
Description: Forms much of the gangue.
Chalcocite
Formula: Cu2S
Habit: massive and crystallized
Colour: b
Description: "Large chunks of chalcocite and bornite covered with malachite" (Schairer, 1931). "At Bellamy's mine in Cheshire, it is both massive and crystallized. The crystals have the form represented by figs. 461 and 462 of my Mineralogy. It is usually disseminated through sandstone-conglomerate, and is often attended by green malachite, calcareous spar [calcite] and heavy spar [barite]" (Shepard, 1837).
Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Habit: encrustations
Colour: blue-green
Description: Encrustations, less abundant than malachite.
Cuprite
Formula: Cu2O
Habit: encrustations
Colour: maroon
Description: Thin secondary crusts on other minerals but associated with the primary chalcocite and bornite. Easy to mistake for hematite.
Malachite
Formula: Cu2(CO3)(OH)2
Habit: encrustations
Colour: green
Description: Post-mine formations on bornite and chalcocite.
'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
Habit: massive, pseudomorph after unknown mineral
Colour: olive green
Description: A small, 1 cm rectangular pseudomorph of serpentine after an unknown mineral in massive calcite with bornite.
Talc
Formula: Mg3Si4O10(OH)2
Willemite
Formula: Zn2SiO4
Habit: aggregates of acicular crystals
Colour: white
Fluorescence: green
Description: Solid aggregates to about 1 cm of unterminated clear/white crystals embedded in calcite with bornite, barite, malachite typical of the locality.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcocite2.BA.05Cu2S
Bornite2.BA.15Cu5FeS4
Group 4 - Oxides and Hydroxides
Cuprite4.AA.10Cu2O
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Baryte7.AD.35BaSO4
Group 9 - Silicates
Willemite9.AA.05Zn2SiO4
Talc9.EC.05Mg3Si4O10(OH)2
Allophane9.ED.20(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
'Serpentine Subgroup'-D3[Si2O5](OH)4

List of minerals for each chemical element

HHydrogen
H Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
H ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
H MalachiteCu2(CO3)(OH)2
H TalcMg3Si4O10(OH)2
H Serpentine SubgroupD3[Si2O5](OH)4
CCarbon
C CalciteCaCO3
C MalachiteCu2(CO3)(OH)2
OOxygen
O Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
O BaryteBaSO4
O CalciteCaCO3
O ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
O CupriteCu2O
O MalachiteCu2(CO3)(OH)2
O TalcMg3Si4O10(OH)2
O WillemiteZn2SiO4
O Serpentine SubgroupD3[Si2O5](OH)4
MgMagnesium
Mg TalcMg3Si4O10(OH)2
AlAluminium
Al Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Al ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
SiSilicon
Si Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Si ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Si TalcMg3Si4O10(OH)2
Si WillemiteZn2SiO4
Si Serpentine SubgroupD3[Si2O5](OH)4
SSulfur
S BaryteBaSO4
S BorniteCu5FeS4
S ChalcociteCu2S
CaCalcium
Ca CalciteCaCO3
FeIron
Fe BorniteCu5FeS4
CuCopper
Cu BorniteCu5FeS4
Cu ChalcociteCu2S
Cu ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cu CupriteCu2O
Cu MalachiteCu2(CO3)(OH)2
ZnZinc
Zn WillemiteZn2SiO4
BaBarium
Ba BaryteBaSO4

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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