Lyman Viaduct at Dickinson Creek, Westchester, Colchester, New London County, Connecticut, USAi
Regional Level Types | |
---|---|
Lyman Viaduct at Dickinson Creek | Creek |
Westchester | - not defined - |
Colchester | - not defined - |
New London County | County |
Connecticut | State |
USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
41° 33' 49'' North , 72° 26' 59'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
East Hampton | 2,691 (2017) | 4.6km |
Lake Pocotopaug | 3,436 (2017) | 6.3km |
Moodus | 1,413 (2017) | 6.8km |
Terramuggus | 1,025 (2017) | 8.1km |
Colchester | 4,781 (2017) | 9.9km |
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 |
---|---|---|
Lapidary and Mineral Society of Central Connecticut | Meriden, Connecticut | 30km |
Bristol Gem & Mineral Club | Bristol, Connecticut | 43km |
New Haven Mineral Club | New Haven, Connecticut | 49km |
Mindat Locality ID:
54243
Long-form identifier:
mindat:1:2:54243:9
GUID (UUID V4):
5eb498b9-3cc2-4549-9b04-278fc98a0e5b
Former popular gem "pyrope" garnet (really almandine) digging locality, in Dickinson Creek stream bed at the culvert outfall under the Lyman Viaduct on the Air Line Trail (former railroad bed) in the Salmon River State Forest. Rounded alluvial garnet crystals up to 1 cm. Cut gems up to 2.5 carets are known.
Connecticut's only authenticated diamond (0.8mm cubic grey crystal) was found during analyses of garnet sands from here in the late 1960s.
In 2012, mainly to stop the diving and swimming that went on here, the state filled the plunge pool with large boulders.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
✪ Almandine Formula: Fe2+3Al2(SiO4)3 Colour: ruby red Description: Rounded alluvial garnet crystals up to 1 cm. Cut gems up to 2.5 carets are known.
References: |
ⓘ ' Formula: Mg3Al2(SiO4)3 Description: Although many local amateur gem cutters believe the garnets here to be pyrope-dominant, analyses show them to be almandine-dominant. |
ⓘ 'Amphibole Supergroup' Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 References: |
ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 References: |
ⓘ Diamond Formula: C Habit: cubic Colour: grey Description: Single alluvial crystal 0.8mm |
ⓘ Formula: Mg3Al2(SiO4)3 Description: Although many local amateur gem cutters believe the garnets here to be pyrope-dominant, analyses show them to be almandine-dominant. |
ⓘ Quartz Formula: SiO2 References: |
ⓘ Staurolite Formula: Fe2+2Al9Si4O23(OH) References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Diamond | 1.CB.10a | C |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Quartz | 4.DA.05 | SiO2 |
Group 9 - Silicates | |||
ⓘ | Almandine | 9.AD.25 | Fe2+3Al2(SiO4)3 |
ⓘ | Pyrope ? | 9.AD.25 | Mg3Al2(SiO4)3 |
ⓘ | Staurolite | 9.AF.30 | Fe2+2Al9Si4O23(OH) |
Unclassified | |||
ⓘ | 'Amphibole Supergroup' | - | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
ⓘ | 'Almandine-Pyrope Series var. Rhodolite' ? | - | Mg3Al2(SiO4)3 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
H | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
C | Carbon | |
C | ⓘ Diamond | C |
O | Oxygen | |
O | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
O | ⓘ Almandine | Fe32+Al2(SiO4)3 |
O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
O | ⓘ Pyrope | Mg3Al2(SiO4)3 |
O | ⓘ Quartz | SiO2 |
O | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
O | ⓘ Almandine-Pyrope Series var. Rhodolite | Mg3Al2(SiO4)3 |
F | Fluorine | |
F | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
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 | ⓘ Pyrope | Mg3Al2(SiO4)3 |
Mg | ⓘ Almandine-Pyrope Series var. Rhodolite | Mg3Al2(SiO4)3 |
Al | Aluminium | |
Al | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Al | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Al | ⓘ Pyrope | Mg3Al2(SiO4)3 |
Al | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
Al | ⓘ Almandine-Pyrope Series var. Rhodolite | Mg3Al2(SiO4)3 |
Si | Silicon | |
Si | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
Si | ⓘ Almandine | Fe32+Al2(SiO4)3 |
Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Si | ⓘ Pyrope | Mg3Al2(SiO4)3 |
Si | ⓘ Quartz | SiO2 |
Si | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
Si | ⓘ Almandine-Pyrope Series var. Rhodolite | Mg3Al2(SiO4)3 |
Cl | Chlorine | |
Cl | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
K | Potassium | |
K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 |
Ti | Titanium | |
Ti | ⓘ Amphibole Supergroup | AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
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 | ⓘ Staurolite | Fe22+Al9Si4O23(OH) |
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Ganderia DomainDomain
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.