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Strickland Quarry (Eureka Quarry), Strickland pegmatite (Strickland-Cramer Quarry; Strickland-Cramer Mine; Strickland-Cramer Feldspar-Mica Quarries), Collins Hill, Portland, Middlesex Co., Connecticut, USA

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Key
Lock Map
Latitude & Longitude (WGS84): 41° 35' 31'' North , 72° 35' 30'' West
Latitude & Longitude (decimal): 41.59222,-72.59167
GeoHash:G#: drkks5sk7
Locality type:Quarry
Köppen climate type:Dfa : Hot-summer humid continental climate


A former feldspar-mica-Be-Nb-Ta-REE-Sn quarry in granite pegmatite located on the west side and near the summit of Collins Hill, 2½ miles (4 km) NE of Portland. It operated in the Strickland pegmatite along with the separate, underground Schoonmaker or Cramer Mine to the immediate north (a separate locality), though the two were not connected until perhaps the last few years of operations. All the dumps formerly around the quarry except the largest, northernmost one belonged to the Strickland Quarry. The northernmost dump belonged to the Schoonmaker or Cramer Mine. Because most collectors did not realize the northern dump belonged to a different operation, most specimens are referred to as coming from the Strickland Quarry no matter where collected. The difference is largely academic anyway because all the minerals came from the same pegmatite and the mineralogy, pegmatite zoning, and host rocks of the Strickland Quarry and Schoonmaker Mine are similar. Any specimen can be generically attributed to the Strickland pegmatite. When a golf course on the site was constructed in the 1990s all of the dumps were removed, and although the flooded quarry pit is still present, collecting is no longer allowed or possible.

Mining supposedly began in the 1840s according to Foye (1922) who stated:

"The quarry was opened as early as 1840. There is a pitcher, bearing in gilt the name of Strickland, now preserved in Wesleyan Museum, which was made from feldspar taken from the quarry at that early date."

If so, it must have been a minor operation as it is not mentioned in Beers' (1884) History of Middlesex County. Ralph Pelton's quarry is mentioned, but this is a separate locality just east of Collins Hill.

Strickland Quarry was operated by F. E. Strickland from 1904 to 1945. It was leased to Eureka Flint & Spar Co., Eureka Mining & Operating Co. or Eureka Mica & Mining Co. Successive operators were F. E. Strickland, George Wilkes, and William Wilkes.

Mostly it was involved in feldspar production before 1937 but was a big mica producer 1930-37, 1942-45, and 1952-53 (from wall zones). It produced 2,000 to 5,000 long tons of feldspar per year and 200 to 400 tons of mica after 1927; also quartz, beryl, and gemstones. Workings include an open cut 300 feet long by 200 feet wide and 140 feet deep. The east cut quarried up to 100 feet deep & connected mines worked 1914-37. Wall zones were mined underground mostly to the north in the 1940s & 1950s.

Cameron (1954) summarized the pegmatite and its zones as follows:

Exposed in east quarry cut and for over 720 ft N-S by 240 ft E-W, 8-60 ft thick. Dips west 30-75 degrees.
Five lithologic zones:
1. quartz-muscovite-plagioclase border zone, 1-8 in. thick
2. plagioclase-quartz-muscovite wall zone, 1-7 ft thick (mica zone – books up to 6 feet!)
3. microcline perthite-graphic granite-quartz-plagioclase intermediate zone 1-22 ft thick (perthite crystals up to 22 ft!)
4. plagioclase (cleavelandite)-quartz intermediate zone up to 45 ft thick
5. quartz core

Mineralization is a pegmatite deposit (Deposit Model code 33; USGS model code 13a; name: Be-Li pegmatites) Late Permian in age, hosted in the Ordovician Collins Hill Formation (= Partridge Formation of New Hampshire). The ore body strikes N-S and dips 35-40/50W at a thickness of 6.71/9 meters, a width of 73 meters and a length of 229 meters, covering an area of 4.8 HA. It is lenticular in shape. The primary mode of origin was magmatic differentiation and secondary was hydrothermal. Primary ore control was bedding. There is moderate wall rock alteration (silicification).

Located in the Middletown Pegmatite District comprising a swarm of Permian (~260 mya) pegmatite dikes; locally in a north-trending zone, mostly in the Ordovician Collins Hill Formation; but dikes are also present in eastward adjacent Ordovician Glastonbury Gneiss and westward adjacent Ordovician Middletown Formation.

The most diverse mineralogy and miarolitic pockets were mostly found with pale blue to white cleavelandite in zone 4. Descriptions of gem elbaite-rich pockets are found in Bastin (1910), Shannon (1920), Sterrett (1923), and Stearns (1983). Most elbaite is green, but there are concentrically zoned crystals with an olive green exterior, blue intermediate zone, on a core of schorl; classic watermelon tourmaline; and a plethora of pastel shades of gray, pink, green, blue, lavender to colorless. The miarolitic pockets were shattered after initial crystallization as most elbaite crystals are fragmented along with quartz and cleavelandite, with some dissolution of these minerals and so are seldom terminated. If they are terminated they may have a dark blue terminal zone with simple pedion or a very shallow rhombohedral form. Capillary overgrowths cause a schiller effect on many small crystals. Subsequently to pocket collapse, K-rich albite crystallized as separate micro-crystals and as overgrowths on cleavelandite along with quartz as overgrowths on quartz fragments and as tiny microcrystals among the K-rich albite. The latter white to tan colored mineral formed fine-grained masses or druses that host fragmented elbaite and very late forming minerals such as purple fluorapatite, white hydroxylapatite, cookeite, fluorite, pyrite, calcite, chlorite, bertrandite, schernikite, rare zeolites, and masses of fine-grained, secondary, capillary to hairy tourmaline.

The host Collins Hill Formation is a gray, rusty-weathering, medium- to coarse-grained, poorly layered schist, composed of quartz, oligoclase, muscovite, biotite, and garnet, generally graphitic, interlayered with fine-grained two-mica gneiss, especially to the west, and with calc-silicate and amphibolite layers, also rare quartz-almandine [coticule] layers with rare rutile. The schist units contain kyanite, ilmenite, cordierite, pyrrhotite and chalcopyrite in quartz pods and small alpine-cleft type openings with albite (oligoclase), muscovite, pyrite, chlorite, and anatase. The calc-silicate (skarn) units contain a typical Barrovian assemblage of anorthite, actinolite, augite, calcite, diopside, scapolite, grossular, zoisite, vesuvianite, etc. Within this rock, a rare assemblage of wollastonite with gehlenite, spurrite, larnite, grossular, quartz, diopside, vesuvianite, and calcite was documented by Schooner (circa 1985). These and other host rock primary and secondary (gypsum, pickeringite, melanterite, epsomite, sulfur, etc.) minerals are included in the locality species list.

Mindat Articles

History and Mineralology of the Strickland Quarry by Rowan Lytle




Mineral List

Actinolite ?

Albite

var: Cleavelandite

var: Oligoclase

Allanite-(Ce)

Almandine

Amblygonite

Analcime

Anatase

Anglesite ?

Annite

Anorthite

'Apatite'

Aragonite

Arsenolite ?

Arsenopyrite

Augelite

Augite

var: Fassaite

Autunite

Bavenite

Bazzite

Bertrandite

Beryl

var: Aquamarine

var: Heliodor

var: Morganite

Bismite ?

Bismuthinite ?

Bismutite ?

Bityite

Brazilianite

Calcite

Cassiterite

Chalcopyrite

'Chlorite Group'

Chrysotile

Clinozoisite

Columbite-(Fe)

Cookeite

Cordierite

Crandallite ?

Dickinsonite-(KMnNa)

Diopside

Elbaite

Eosphorite

Epsomite

Eucryptite

Euxenite-(Y)

Fairfieldite

Fluorapatite

var: Mn-bearing Fluorapatite

Fluorite

Foitite

Gahnite ?

Galena

Gehlenite

Gobbinsite

Goethite

Goslarite ?

Graphite

Greenockite ?

Grossular

Groutite

Gypsum

'Halloysite'

Hematite

Hureaulite

Hydroxylapatite

Hydroxylherderite

Ilmenite ?

Kaolinite

Kyanite

Lacroixite

Larnite

'Lepidolite'

'Limonite'

Lithiophilite

Löllingite

Magnesio-hornblende

Magnetite

'Manganese Oxides'

'var: Manganese Dendrites'

Manganite

Masutomilite

Melanterite

Meta-autunite

Metatorbernite ?

Microcline

Microlite Group

Mitridatite

Molybdenite

Monazite-(Ce)

Montebrasite

Montmorillonite

Moraesite

Morinite ?

Muscovite

var: Schernikite

'Natromontebrasite'

Natrophilite

Opal

var: Opal-AN

Orthoclase

Parsonsite

Petalite

Phenakite

Phlogopite ?

Pickeringite

'Pinite'

Planerite

Pollucite

Purpurite

Pyrite

Pyrochlore Group

Pyrolusite

Pyrrhotite

Quartz

var: Amethyst

var: Citrine

var: Milky Quartz

var: Rock Crystal

var: Rose Quartz

var: Smoky Quartz

Reddingite ?

Rhodochrosite

Rhodonite

'Rubellite'

Rutile

Samarskite-(Y) ?

'Scapolite' ?

Scheelite

Schorl

Scorodite ?

Sicklerite

Siderite

Spessartine

Sphalerite

Spodumene

var: Kunzite

Spurrite

Staurolite

Stewartite ?

'Stilbite'

Sulphur

Tantalite-(Mn)

Titanite

Topaz

'Tourmaline'

Triplite

Uraninite

Uranophane

'Verdelite'

Vesuvianite ?

Vivianite ?

Wardite

Wodginite

Wollastonite

Wurtzite

var: Voltzite

Xenotime-(Y)

'Zinnwaldite'

Zircon

var: Cyrtolite

Zoisite


119 valid minerals. 15 erroneous literature entries.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Devonian - Silurian
358.9 - 443.8 Ma



ID: 3186140
Paleozoic sedimentary and volcanic rocks

Age: Paleozoic (358.9 - 443.8 Ma)

Lithology: Mudstone-carbonate-sandstone-conglomerate

Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529. [154]

Late Ordovician - Middle Ordovician
443.8 - 470 Ma



ID: 2978277
Collins Hill Formation

Age: Ordovician (443.8 - 470 Ma)

Stratigraphic Name: Collins Hill Formation

Description: ( = Partridge Formation of New Hampshire) - Gray, rusty-weathering, medium- to coarse-grained, poorly layered schist, composed of quartz, oligoclase, muscovite, biotite, and garnet, and commonly staurolite, kyanite, or sillimanite, generally graphitic, interlayered with fine-grained two-mica gneiss, especially to the west, and with calc-silicate and amphibolite layers, also rare quartz-spessartine (coticule) layers.

Comments: Part of Eastern Uplands; Iapetus (Oceanic) Terrane - Bronson Hill Anticlinorium; Brimfield Schist and equivalent formations (includes Collins Hill Formation) (Upper? and Middle Ordovician).

Lithology: Major:{schist}, Minor:{gneiss}, Incidental:{amphibolite, calc silicate rock}

Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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.

References

Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
J. H. Beers & Co. (1884) The History of Middlesex County 1635-1885.
Bastin, Edson S. (1910) Economic Geology of the Feldspar Deposits of the United States. United States Geological Survey Bulletin 420, Government Printing Office.
Schrader, Frank C., Stone, Ralph W., and Sanford, Samuel (1917) Useful Minerals of the United States. U. S. Geological Survey Bulletin 624: 97-101.
Foye, Wilbur G. (1919) A New Occurrence of Rhodonite. American Mineralogist: 4(10): 124.
Shannon, Earl V. (1920) Strickland's Quarry, Portland, Connecticut. American Mineralogist: 5(3): 51-54.
Foye, Wilbur. G. (1922) Mineral Localities in the Vicinity of Middletown, Connecticut. American Mineralogist: 7(1): 4-12.
Sterrett, Douglas B. (1923) Mica Deposits Of The United States. USGS Bulletin 740: 65-67.
Schairer, J. F. (1926) Lithiophilite and Other Rare Phosphates from Portland, Connecticut. American Mineralogist: 11(4): 101-104.
Schairer, J. F. and Lawson. C. C. (1926) Pickeringite from Portland, Connecticut. American Journal of Science: 11: 301-4.
Rice, W. N. and Foye, Wilbur G. (1927) Guide To The Geology Of Middletown, Connecticut, and vicinity. State Geological and Natural History Survey Of Connecticut Bulletin 41: 87-90.
Schairer, J. F. (1931) The Minerals of Connecticut. State Geological and Natural History Survey Bulletin 51.
Otersen, Lillian (1934) Report on New Haven Mineral Trip to Strickland Quarry (Rocks & Minerals Association National Outing, May 20, 1934). Rocks & Minerals: 9(6): 104.
Jenks, William F. (1935) Pegmatites at Collins Hill, Portland, Conn. American Journal of Science: s. 5, 30: 177-197.
Zodac, Peter (1937) Minerals of the Strickland Quarry. Rocks & Minerals: 12: 131-144.
Federal Writer's Project (1938) Connecticut: A Guide to Its Roads, Lore, and People: 402.
Little, L. W. (1942) Recent Finds of Minerals in Central Connecticut. Rocks & Minerals: 17(8).
Confidential unpublished war min. report (1944) Reg. file Nos. E-816, Strickland Mica-Feldspar Mine, Middlesex County, Connecticut, 1944, 19 [page No. - ?].
Cameron, Eugene N., Larrabee, David M., McNair, Andrew H., Page, James T., Stewart, Glenn W., and Shainin, Vincent E. (1945) Structural And Economic Characteristics Of New England Mica Deposits. Economic Geology: 11(6): 378-380.
Palache, C., Berman, H., and Frondel, C. (1951) The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana, Yale University 1837-1892, Volume II: 667, 851.
Cameron, Eugene N., Larrabee, David M., McNair, Andrew H., Page, James T., Stewart, Glenn W., and Shainin, Vincent E. (1954) Pegmatite Investigations 1942-45 New England; USGS Professional Paper 255: 333-338.
Schooner, Richard (1955) 90 Minerals from 1 Connecticut Hill. Rocks & Minerals: 30(7-8): 351-8.
Schooner, Richard (1958) The Mineralogy of the Portland-East Hampton-Middletown-Haddam Area in Connecticut (With a few notes on Glastonbury and Marlborough). Published by Richard Schooner; Ralph Lieser of Pappy’s Beryl Shop, East Hampton; and Howard Pate of Fluorescent House, Branford, Connecticut.
Stugard, Frederick, Jr. (1958) Pegmatites of the Middletown Area, Connecticut. USGS Bulletin 1042-Q.
Jones, Robert W. (1960) Luminescent Minerals of Connecticut, a Guide to Their Properties and Locations.
Schooner, Richard (1961) The Mineralogy of Connecticut. Fluorescent House, Branford, Connecticut.
Killeen, P. L., and Newman, W. L. (1965) USGS MR-44: 3, - TI.
Brookins, D.G., Fairbairn, H.W., Hurley, P.M., and Pinson, W.H. (1969) A Rb-Sr Geochronologic Study of the Pegmatites of the Middletown Area, Connecticut). Contributions to Mineralogy and Petrology 22: 157-168.
Ryerson, Kathleen (1972) Rock Hound's Guide to Connecticut. Pequot Press.
Henderson, William A., Jr. (1975) The Bertrandites of Connecticut. Mineralogical Record: 6(3): 114-123.
Januzzi, Ronald E. (1976) Mineral Localities of Connecticut and Southeastern New York State (Taylor Assoc./Mineralogical Press).
Webster, Bud (1978) Mineral Collector’s Field Guide Connecticut.
Albini, Anthony J. (1979) Selected Pegmatite Quarries of the Central Connecticut Region. Masters thesis. Central Connecticut State College, New Britain, Connecticut.
Webster, Bud and Bill Shelton (1979) Mineral Collector’s Field Guide the Northeast.
Stearns, H. T. (1983) Memoirs of a Geologist: From Poverty Peak to Piggery Gulch. Hawaii Institute of Geophysics, Honolulu.
Schooner, Richard (circa 1985) Untitled manuscript on central Connecticut mineralogy.
Robinson, George W. and Vandall T. King (1988) What's New in Minerals? Mineralogical Record: 19(5): 332.
Jarnot, Bruce (1989) Minerals New to the Portland Area Pegmatites of Central Connecticut. Abstract from the 16th Rochester Mineralogical Symposium April 7, 1989, in Rocks & Minerals: 64(12): 471.
Januzzi, Ronald. E. (1994) Mineral Data Book - Western Connecticut and Environs. Mineralogical Press, Danbury, Connecticut.
Robbins, Manuel. (1994) Fluorescence: Gems and Minerals Under Ultraviolet Light. Geoscience Press, Inc., Phoenix, Arizona.
Henderson, William A. (1995) Microminerals of Connecticut. Rocks & Minerals: 70(6): 420-425.
Jarnot, Bruce (1995) Connecticut Gems and Gem Minerals. Rocks & Minerals: 70(6): 378-382.
Weber, Marcelle H. and Earle C. Sullivan. (1995) Connecticut Mineral Locality Index. Rocks & Minerals (Connecticut Issue): 70(6): 403.
USGS GSC ID # LIST (1995) (July 1995).
Moore, P. B. (2000) Analyses of Primary Phosphates from Pegmatites in Maine and Other Localities, in V. T. King (editor), Mineralogy of Maine. Mining History, Gems, and Geology, Maine Geological Survey, Augusta, Maine: 333-336.
Pawloski, John A. (2006) Connecticut Mining (Mt. Pleasant, SC: Arcadia Publishing): 50-51, 61.
USGS (2005) Mineral Resources Data System (MRDS): U.S. Geological Survey, Reston, Virginia, loc. file ID #10067599 & 10264493.
Jarnot, Bruce M. (2011) Letters: Connecticut Update. Rocks & Minerals: 86(4): 299.
U.S. Bureau of Mines, Minerals Availability System (MAS) file ID #0090070003.

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