| Locality type: | Cliff |
| Classification |
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| Species: | 'Garnet Group' (not an IMA approved species) |
| Formula: | X3Z2(SiO4)3 |
| Comments: | Occurs in waterworn pebbles originating from a rodingite vein. |
| Confirmation |
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|
| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Garnet Group data |
| Locality Data: | Click here to view Eastern Cliff, Kennack Cove (Kennack Sands), Kennack, Grade-Ruan, Cornwall, England, UK |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 693501 |
| Long-form Identifier: | 1:3:693501:6 |
| GUID (UUID V4): | 0d37d8c4-beee-46d6-895f-fcb92b8b0688 |
| Nearest other occurrences of Garnet Group |
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| 14.9km (9.2 miles) | ⓘWheal Trannack, Trannack, Wendron, Cornwall, England, UK |
| 24.4km (15.2 miles) | ⓘClyjah and Wentworth Mine (Perseverance Mine), Redruth, Cornwall, England, UK |
| 25.4km (15.8 miles) | ⓘCarharrack Mine, Gwennap, Cornwall, England, UK |
| 25.4km (15.8 miles) | ⓘSouth Crofty Tin Project (South Crofty Mine; South Wheal Crofty), Pool, Carn Brea, Cornwall, England, UK |
| 25.7km (16.0 miles) | ⓘNew Roskear Shaft, Dolcoath Mine, Camborne, Cornwall, England, UK |
| 25.8km (16.0 miles) | ⓘSt Michael's Mount, Cornwall, England, UK |
| 29.4km (18.3 miles) | ⓘLamorna Cove, St Buryan, Cornwall, England, UK |
| 29.7km (18.4 miles) | ⓘRosemodress Cliff, St Buryan, Cornwall, England, UK |
| 34.6km (21.5 miles) | ⓘWheal Devonshire, St Agnes, Cornwall, England, UK |
| 39.5km (24.6 miles) | ⓘGreat Retallack Mine, Perran Iron Lode (Great Perran Iron Lode), Perranzabuloe, Cornwall, England, UK |
| References |
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| Reference Search (possible matching items) |
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 | | Book | | PO Box 315. Harpenden. Hertfordshire AL5 2ZD. England Telephone: +44 (0)1582 762413 Fax: +44 (0)870 055.............................. 529 G: gadolinite group to gyrolite ......................... 226 X: xanthiosite...the production of e0pper. the mining areas of Cornwall and Devon became important producers of b th tin...Oxford University Museum of Natural History; Royal Cornwall Museum, Truro; Sedgwick Museum, University of...further 154 species are unconfirmed. If all the group, series, variety and discredited species names are |  | | Book (volume) | | INTRODUCTION Geological Setting of Eastern Hokkaido The eastern area of Hokkaido includes the southwest¬...Quaternary volca¬ noes of the volcanic belt in Eastern Hokkaido, extending from the Kuril Islands, also...occur in the northern area. The strata in the eastern area of Hokkaido are not as de¬ formed as those...volcano (Stop 2) Mashu volcano, which erupted on the eastern wall of Kutcharo caldera, east Hokkaido, is famous...the lower part. The Saroma group which unconformably overlies the Nikoro group, is Coniassian to Campanian |
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