| Classification |
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| Species: | Zoisite |
| Formula: | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) |
| Confirmation |
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| Validity: | Confirmed |
| Confirmation Methods: | Visually Identified |
| Data |
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| Mineral Data: | Click here to view Zoisite data |
| Locality Data: | Click here to view Sgurr Aoidhe, Loch Duich, Highland, Scotland, UK |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 708290 |
| Long-form Identifier: | 1:3:708290:0 |
| GUID (UUID V4): | 0b87e867-89f9-4a69-8199-37916d25f221 |
| Nearest other occurrences of Zoisite |
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| 0.3km (0.2 miles) | ⓘAllt a Mhuilin, Keppoch, Dornie, Lochalsh, Wester Ross， Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 0.8km (0.5 miles) | ⓘAn Leth Alt, Loch Duich, Highland, Scotland, UK |
| 1.7km (1.1 miles) | ⓘCreag Reidh Raineach, Dornie, Lochalsh, Wester Ross， Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 4.8km (3.0 miles) | ⓘBeinn Fhada, Glenelg, Wester Ross, Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 7.3km (4.5 miles) | ⓘAllt Mor, Glenelg, Wester Ross, Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 10.0km (6.2 miles) | ⓘCorrary, Glen Beag, Glenelg, Wester Ross, Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 11.8km (7.3 miles) | ⓘAllt an Fhaing, Glen Beag, Glenelg, Wester Ross, Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 14.7km (9.1 miles) | ⓘLoch na Lochain, Upper Sandaig, Glenelg, Wester Ross, Strathpeffer and Lochalsh, Highland, Scotland, UK |
| 19.0km (11.8 miles) | ⓘMhuineil, Barrisdale Bay, Loch Hourn Complex, Highland, Scotland, UK |
| 30.0km (18.6 miles) | ⓘCoire Dhorrcail incl Allt Coire Dhorrcail, Knoydart, Caol and Mallaig, Highland, Scotland, UK |
| References |
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| Reference Search (possible matching items) |
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 | | Book | | deposited. The large area of Lewisian rocks north of Loch Duich extends westwards into the Glenelg district (Sheet...psammite during sliding. The Lewisian north of Loch Duich and in the Glenelg area (Sheet 71 E) consists...separated by a major tectonic dislocation, the Sgurr Beag Slide. The complexity of the folding and lack...Nevertheless both of the lower two divi sions, and the Sgurr Beag Slide, have been recognised in the Kintail...main valleys were reoccupied by glaciers during the Loch Lomond Stadia}, at about 11 000 to 10 000 BP, and |
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