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Witt Hill Chrysoberyl locality, Greenwood, Oxford County, Maine, USAi
Regional Level Types
Witt Hill Chrysoberyl localityOccurrence
GreenwoodTown
Oxford CountyCounty
MaineState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
44° 17' 19'' North , 70° 37' 50'' West
Latitude & Longitude (decimal):
44.28874,-70.63067
GeoHash:
G#: drvgby82d
GRN:
N30W37
Type:
Occurrence
KΓΆppen climate type:
Dfb : Warm-summer humid continental climate
Nearest Settlements:
PlacePopulationDistance
Greenwood834 (2017)3.7km
West Paris1,790 (2017)6.0km
Woodstock1,263 (2017)9.7km
Norway2,748 (2017)10.8km
Paris5,073 (2017)10.8km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Oxford County Mineral and Gem AssociationSouth Paris, Maine12km
Mindat Locality ID:
6045
Long-form identifier:
mindat:1:2:6045:8
GUID (UUID V4):
4161de1f-d9da-465a-b93c-f39138af9134


A specimen - gemstone mine (chrysoberyl) in pegmatite. Once owned by Nathaniel H. Perry (1870's). Oxford pegmatite field.

(NOTE: This site is often incorrectly listed as being in the town of Norway, immediately to the south. There may be sites on hill to the south of the Greenwood town line; but the main collecting locality is in Greenwood.) [The inclusion of sillimanite on the mineral list is not a mistake - its presence in fibrous form is an unusual characteristic of the rock here.]
(Inaccurately located by Morrill, 1958).

The locality is reached by going west from the town of Norway on route 118 and up the Greenwood Road. When you cross in Greenwood from Norway the next road East where the Richardson Hollow Road turns east towards West Paris. Leave the Richardson Hollow Road toward Camp Sierra and go beyond it. You will soon come to a turn in the road - a right angle left. Within a short distance (about 100 feet) the clear road goes slightly north by northeast. Leave the cleared road and go slightly north westward along a barely recognizable woods road. You can see the eventual connection with the Young Hill Road on Google maps and the suture of the tree tops shows the location of the straight road from Young Hill Road to Richardson Hollow. The discontinued road may be navigable up an incline and there used to be a farmer's rock wall which formed a right angle separating the woods road from the old farm land. Walk northwest from the inside corner of the rock wall fence and you should reach a naturally rounded rock ledge, about 15-20 feet high. The ledge is probably 150-200 feet west from the abandoned woods road. Walk north along the east side of the ledge until you get to a small depression with water (20 x 30 feet, depending on the season) abutting the ledge. Scramble up the low ledge. You should be on the chrysoberyl occurrence. The top surface of the ledge is fairly flat and the area is probably thickly wooded unless some logging was done. You will have to search for float boulders to find chrysoberyl and sillimanite. I am not sure how extensive the productive area is. Bring drinking water and don't collect on a hot day.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


14 valid minerals.

Detailed Mineral List:

β“˜ Albite
Formula: Na(AlSi3O8)
β“˜ Almandine
Formula: Fe2+3Al2(SiO4)3
β“˜ Autunite
Formula: Ca(UO2)2(PO4)2 · 10-12H2O
β“˜ 'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
βœͺ Chrysoberyl
Formula: BeAl2O4
β“˜ Gahnite
Formula: ZnAl2O4
β“˜ Meta-autunite
Formula: Ca(UO2)2(PO4)2 · 6H2O
β“˜ Metatorbernite
Formula: Cu(UO2)2(PO4)2 · 8H2O
β“˜ Microcline
Formula: K(AlSi3O8)
β“˜ Muscovite
Formula: KAl2(AlSi3O10)(OH)2
β“˜ Quartz
Formula: SiO2
β“˜ Schorl
Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜ Sillimanite
Formula: Al2(SiO4)O
β“˜ Torbernite
Formula: Cu(UO2)2(PO4)2 · 12H2O
β“˜ Zircon
Formula: Zr(SiO4)

Gallery:

BeAl2O4β“˜ Chrysoberyl

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
β“˜Chrysoberyl4.BA.05BeAl2O4
β“˜Gahnite4.BB.05ZnAl2O4
β“˜Quartz4.DA.05SiO2
Group 8 - Phosphates, Arsenates and Vanadates
β“˜Autunite8.EB.05Ca(UO2)2(PO4)2 Β· 10-12H2O
β“˜Torbernite8.EB.05Cu(UO2)2(PO4)2 Β· 12H2O
β“˜Meta-autunite8.EB.10Ca(UO2)2(PO4)2 Β· 6H2O
β“˜Metatorbernite8.EB.10Cu(UO2)2(PO4)2 Β· 8H2O
Group 9 - Silicates
β“˜Almandine9.AD.25Fe2+3Al2(SiO4)3
β“˜Zircon9.AD.30Zr(SiO4)
β“˜Sillimanite9.AF.05Al2(SiO4)O
β“˜Schorl9.CK.05NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)
β“˜Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
β“˜Microcline9.FA.30K(AlSi3O8)
β“˜Albite9.FA.35Na(AlSi3O8)
Unclassified
β“˜'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2

List of minerals for each chemical element

HHydrogen
Hβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Hβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Hβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Hβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Hβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Hβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Hβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
BeBeryllium
Beβ“˜ ChrysoberylBeAl2O4
BBoron
Bβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
OOxygen
Oβ“˜ AlbiteNa(AlSi3O8)
Oβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Oβ“˜ AlmandineFe32+Al2(SiO4)3
Oβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Oβ“˜ ChrysoberylBeAl2O4
Oβ“˜ GahniteZnAl2O4
Oβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Oβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Oβ“˜ MicroclineK(AlSi3O8)
Oβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Oβ“˜ QuartzSiO2
Oβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Oβ“˜ SillimaniteAl2(SiO4)O
Oβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
Oβ“˜ ZirconZr(SiO4)
FFluorine
Fβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
NaSodium
Naβ“˜ AlbiteNa(AlSi3O8)
Naβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
MgMagnesium
Mgβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
AlAluminium
Alβ“˜ AlbiteNa(AlSi3O8)
Alβ“˜ AlmandineFe32+Al2(SiO4)3
Alβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Alβ“˜ ChrysoberylBeAl2O4
Alβ“˜ GahniteZnAl2O4
Alβ“˜ MicroclineK(AlSi3O8)
Alβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Alβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Alβ“˜ SillimaniteAl2(SiO4)O
SiSilicon
Siβ“˜ AlbiteNa(AlSi3O8)
Siβ“˜ AlmandineFe32+Al2(SiO4)3
Siβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Siβ“˜ MicroclineK(AlSi3O8)
Siβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
Siβ“˜ QuartzSiO2
Siβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
Siβ“˜ SillimaniteAl2(SiO4)O
Siβ“˜ ZirconZr(SiO4)
PPhosphorus
Pβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Pβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Pβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Pβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
KPotassium
Kβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Kβ“˜ MicroclineK(AlSi3O8)
Kβ“˜ MuscoviteKAl2(AlSi3O10)(OH)2
CaCalcium
Caβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Caβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
TiTitanium
Tiβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
FeIron
Feβ“˜ AlmandineFe32+Al2(SiO4)3
Feβ“˜ BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Feβ“˜ SchorlNaFe32+Al6(Si6O18)(BO3)3(OH)3(OH)
CuCopper
Cuβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Cuβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O
ZnZinc
Znβ“˜ GahniteZnAl2O4
ZrZirconium
Zrβ“˜ ZirconZr(SiO4)
UUranium
Uβ“˜ AutuniteCa(UO2)2(PO4)2 · 10-12H2O
Uβ“˜ Meta-autuniteCa(UO2)2(PO4)2 · 6H2O
Uβ“˜ MetatorberniteCu(UO2)2(PO4)2 · 8H2O
Uβ“˜ TorberniteCu(UO2)2(PO4)2 · 12H2O

Other Regions, Features and Areas containing this locality

North America PlateTectonic Plate

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

Jacobson, Mark L. (1987) Four Obscure Pegmatite Mineral Localities in Oxford County, Maine. Rocks & Minerals, 62(6), 401-405.
Thompson, W.B. Joyner, D.L., Woodman, R.G., King, V.T. (1988) A Collector's Guide to Maine Mineral Localities. Maine Geological Survey Department of Conservation, 133 pages.
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