Witt Hill Chrysoberyl locality, Greenwood, Oxford County, Maine, USAi
| Regional Level Types | |
|---|---|
| Witt Hill Chrysoberyl locality | Occurrence |
| Greenwood | Town |
| Oxford County | County |
| Maine | State |
| USA | Country |
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Latitude & Longitude (WGS84):
44° 17' 19'' North , 70° 37' 50'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Greenwood | 834 (2017) | 3.7km |
| West Paris | 1,790 (2017) | 6.0km |
| Woodstock | 1,263 (2017) | 9.7km |
| Norway | 2,748 (2017) | 10.8km |
| Paris | 5,073 (2017) | 10.8km |
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 |
|---|---|---|
| Oxford County Mineral and Gem Association | Bethel, Maine | 12km |
Oxford pegmatite field.
A specimen—gemstone mine (chrysoberyl) in pegmatite. Once owned by Nathaniel H. Perry (1870s).
Note: This site is often incorrectly listed as being in the town of Norway, immediately to the south. There may be sites on the hill to the south of the Greenwood town line, but the main collecting locality is in Greenwood.
Note on the mineral list: 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 into Greenwood from Norway, the next road east is 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 northwestward 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 treetops 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 that formed a right angle separating the woods road from the old farmland. 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 of 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 at 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.
A specimen—gemstone mine (chrysoberyl) in pegmatite. Once owned by Nathaniel H. Perry (1870s).
Note: This site is often incorrectly listed as being in the town of Norway, immediately to the south. There may be sites on the hill to the south of the Greenwood town line, but the main collecting locality is in Greenwood.
Note on the mineral list: 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 into Greenwood from Norway, the next road east is 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 northwestward 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 treetops 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 that formed a right angle separating the woods road from the old farmland. 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 of 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 at 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 ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
14 valid minerals.
Detailed Mineral List:
| ⓘ Albite Formula: Na(AlSi3O8) |
| ⓘ Almandine Formula: Fe2+3Al2(SiO4)3 |
| ⓘ Autunite Formula: Ca(UO2)2(PO4)2 · 10-12H2O |
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| ✪ Chrysoberyl Formula: BeAl2O4 References: |
| ⓘ Gahnite Formula: ZnAl2O4 |
| ⓘ Meta-autunite Formula: Ca(UO2)2(PO4)2 · 6H2O |
| ⓘ Metatorbernite Formula: Cu(UO2)2(PO4)2 · 8H2O |
| ⓘ Microcline Formula: K(AlSi3O8) |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Quartz Formula: SiO2 |
| ⓘ Schorl Formula: NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ Sillimanite Formula: Al2(SiO4)O |
| ⓘ Torbernite Formula: Cu(UO2)2(PO4)2 · 12H2O |
| ⓘ Zircon Formula: Zr(SiO4) |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Chrysoberyl | 4.BA.05 | BeAl2O4 |
| ⓘ | Gahnite | 4.BB.05 | ZnAl2O4 |
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Autunite | 8.EB.05 | Ca(UO2)2(PO4)2 · 10-12H2O |
| ⓘ | Torbernite | 8.EB.05 | Cu(UO2)2(PO4)2 · 12H2O |
| ⓘ | Meta-autunite | 8.EB.10 | Ca(UO2)2(PO4)2 · 6H2O |
| ⓘ | Metatorbernite | 8.EB.10 | Cu(UO2)2(PO4)2 · 8H2O |
| Group 9 - Silicates | |||
| ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Sillimanite | 9.AF.05 | Al2(SiO4)O |
| ⓘ | Schorl | 9.CK.05 | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
| ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
| Unclassified | |||
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| H | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| H | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| H | ⓘ Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| Be | Beryllium | |
| Be | ⓘ Chrysoberyl | BeAl2O4 |
| B | Boron | |
| B | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | Oxygen | |
| O | ⓘ Albite | Na(AlSi3O8) |
| O | ⓘ Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| O | ⓘ Chrysoberyl | BeAl2O4 |
| O | ⓘ Gahnite | ZnAl2O4 |
| O | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| O | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| O | ⓘ Microcline | K(AlSi3O8) |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | ⓘ Sillimanite | Al2(SiO4)O |
| O | ⓘ Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| O | ⓘ Zircon | Zr(SiO4) |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Na | Sodium | |
| Na | ⓘ Albite | Na(AlSi3O8) |
| Na | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | Aluminium | |
| Al | ⓘ Albite | Na(AlSi3O8) |
| Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Al | ⓘ Chrysoberyl | BeAl2O4 |
| Al | ⓘ Gahnite | ZnAl2O4 |
| Al | ⓘ Microcline | K(AlSi3O8) |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Al | ⓘ Sillimanite | Al2(SiO4)O |
| Si | Silicon | |
| Si | ⓘ Albite | Na(AlSi3O8) |
| Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| Si | ⓘ Microcline | K(AlSi3O8) |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Si | ⓘ Sillimanite | Al2(SiO4)O |
| Si | ⓘ Zircon | Zr(SiO4) |
| P | Phosphorus | |
| P | ⓘ Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| P | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| P | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| P | ⓘ Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| K | ⓘ Microcline | K(AlSi3O8) |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| Ca | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
| 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 | ⓘ Schorl | NaFe32+Al6(Si6O18)(BO3)3(OH)3(OH) |
| Cu | Copper | |
| Cu | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| Cu | ⓘ Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
| Zn | Zinc | |
| Zn | ⓘ Gahnite | ZnAl2O4 |
| Zr | Zirconium | |
| Zr | ⓘ Zircon | Zr(SiO4) |
| U | Uranium | |
| U | ⓘ Autunite | Ca(UO2)2(PO4)2 · 10-12H2O |
| U | ⓘ Meta-autunite | Ca(UO2)2(PO4)2 · 6H2O |
| U | ⓘ Metatorbernite | Cu(UO2)2(PO4)2 · 8H2O |
| U | ⓘ Torbernite | Cu(UO2)2(PO4)2 · 12H2O |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Ganderia DomainDomain
- GranderiaPassive Margin
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Witt Hill Chrysoberyl locality, Greenwood, Oxford County, Maine, USA