| Locality type: | Quarry |
| Classification |
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| Species: | Amphibole Supergroup var: Uralite |
| Formula: | AX2Z5((Si,Al,Ti)8O22)(OH,F,Cl,O)2 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Uralite data |
| Locality Data: | Click here to view Sherrer Quarry, C.K. Williams Quarry complex, Chestnut Hill, Easton, Northampton County, Pennsylvania, USA |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 146887 |
| Long-form Identifier: | 1:3:146887:8 |
| GUID (UUID V4): | a4f0e100-c7f8-4206-9280-f727e35b4033 |
| References |
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| Reference Search (possible matching items) |
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 | | Report (volume) | | THE DELAWARE WATER GAP AND EASTON QUADRANGLES, NEW JERSEY AND PENNSYLVANIA BY W. S. BAYLEY UNITED STATES...area._________________________________________ Chestnut Hill area_-----_------_-_---______-._-_____Structure...mines-----__----_-_------___--__-_-__.___________ Williams shaft.___-____-.---_-_-__-_-______-__________... bank of Delaware River about 2 miles north of Easton, Pa.; B, Photomicrograph of quartzsericite schist...Tewkesbury County, N. J.; B, Photomicrograph of Byram gneiss, road half a mile north of Williams mine, Vernon |  | | Journal (volume) | | The powder patterns were recorded with a Debye-Sherrer camera (diameter 114. 6 mm) using filtered CuKa...oolites (1954) from the Appalachian folding in Pennsylvania describes a special case of stretching subparallel...The disappearance of lineation within a gneiss complex thus may indicate a considerable amount of melting...dipping basic rocks (so-called metabasites, or uralite diabases ) and by some pegmatite dikes . In places...recommended because the map tends to become too complex and the iso-radon curves usually cannot be reproduced |  | | Journal (volume) | | The powder patterns were recorded with a Debye-Sherrer camera (diameter 114. 6 mm) using filtered CuKa...oolites (1954) from the Appalachian folding in Pennsylvania describes a special case of stretching subparallel...The disappearance of lineation within a gneiss complex thus may indicate a considerable amount of melting...dipping basic rocks (so-called metabasites, or uralite diabases ) and by some pegmatite dikes . In places...recommended because the map tends to become too complex and the iso-radon curves usually cannot be reproduced |
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