Log InRegister
Quick Links : The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Kyanite from
Rock Brook, Harwinton, Litchfield County, Connecticut, USA


Classification
Species:Kyanite
Formula:Al2(SiO4)O
Confirmation
Validity:Confirmed
Confirmation Methods:Visually Identified
Data
Mineral Data:Click here to view Kyanite data
Locality Data:Click here to view Rock Brook, Harwinton, Litchfield County, Connecticut, USA
Photo GalleryView Gallery (6 photos)
Data Identifiers
Mindat Occurrence Record ID:725453
Long-form Identifier:1:3:725453:6
GUID (UUID V4):c3ff2703-9a11-4f51-a977-bf27261de018
Nearest other occurrences of Kyanite
2.7km (1.7 miles) Lead Mine Brook, Harwinton, Litchfield County, Connecticut, USA
3.0km (1.9 miles) Harwinton, Litchfield County, Connecticut, USA
5.5km (3.4 miles) Thomaston Dam railroad cut, Thomaston Dam, Thomaston, Litchfield County, Connecticut, USA
8.1km (5.0 miles) Thomaston, Litchfield County, Connecticut, USA
10.5km (6.5 miles) Reynolds Bridge, Thomaston, Litchfield County, Connecticut, USA
10.8km (6.7 miles) Town Farm Road, Litchfield, Litchfield County, Connecticut, USA
11.3km (7.0 miles) Taine Mountain, Burlington, Hartford County, Connecticut, USA
11.5km (7.1 miles) Waterbury Road quarry, Thomaston, Litchfield County, Connecticut, USA
12.7km (7.9 miles) Soapstone quarry, Torrington (Wolcottville), Litchfield County, Connecticut, USA
13.7km (8.5 miles) Hancock Brook Dam, Plymouth, Litchfield County, Connecticut, USA
References
Reference Search (possible matching items)
Report (issue)
THE MIDDLE RADDAM QUADRANGLE, MIDDLESEX COUNTY, CONNECTICUT By Gordon P. Eaton and John.L. Rosenfeld...hornblende-ebiotite schist IPOr AMPHIBQLITE OF RESERVOIR BROOK dark-gray to black, massive to flaggy, mainly- schistose...ilmenite; and, locally, microcline. Less abundant rock types include biotiteoligoclase schist and gneiss...(the total of which constitutes 9.2 percent of the rock), and also biotite, locally with minor sphene, garnet...actinolite or hornblende-diopside calc-silicate rock, containing subordinate sphene, graphite, and rarely
Journal (article/letter/editorial)
Upland 1252 3. Section of rusty quartzite along brook 1J 3. Rocks and structures in Monadnock miles southwest...to join the Ashuelot River, and finally the Connecticut River. Their headwaters are typical youthful... the gorge of Minnewawa Brook east of Marlboro, and the gorge of Otter Brook southwest of East Sullivan...drumlins and outwash with only occasional exposures of rock. Possibly, when passing over Mt. Monadnock, the...moraines are present. The 3j-mile section of Otter Brook north of South Keene is in a broad preglacial valley
Book
Sciences, Natural Environment Research Council, Brook Road, Wormley, Godaiming, Surrey GU8 5UB, England...Resources, Inc., 287 Riverside Avenue, Westport, Connecticut 06880 Harold Williams, Memorial University...to sima? Did vast invasions of ultrabasic igneous rock radi¬ cally change to specific gravity? Was the...considerations, ex¬ tensive exposures of igneous rock on the gently sloping offshore flanks are rare and...the presumed principal source of oceanic igneous rock impinging against that margin. Several much smaller
 
Mineral and/or Locality  
Mindat Discussions Facebook Logo Instagram Logo Discord Logo
Mindat.org is an outreach project of the Hudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2024, except where stated. Most political location boundaries are © OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 by Jolyon Ralph.
Privacy Policy - Terms & Conditions - Contact Us / DMCA issues - Report a bug/vulnerability Current server date and time: April 19, 2024 04:01:20
Go to top of page