| Locality type: | Pit |
| Classification |
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| Species: | Muscovite var: Illite |
| Formula: | K0.65Al2.0[Al0.65Si3.35O10](OH)2 |
| Confirmation |
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| Validity: | Believed Valid |
| Data |
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| Mineral Data: | Click here to view Illite data |
| Locality Data: | Click here to view Lisowice clay pit, Lubliniec County, Silesian Voivodeship, Poland |
| Data Identifiers |
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| Mindat Occurrence Record ID: | 1097776 |
| Long-form Identifier: | 1:3:1097776:5 |
| GUID (UUID V4): | 8ba4e1c7-fd99-444d-bc9c-dc9e4333d764 |
| Nearest other occurrences of Illite |
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| 40.5km (25.1 miles) | ⓘFaustianka, Gmina Rudniki, Olesno County, Opole Voivodeship, Poland |
| 51.3km (31.9 miles) | ⓘMyszków Cu-Mo deposit, Gmina Żarki, Myszków County, Silesian Voivodeship, Poland |
| 52.5km (32.6 miles) | ⓘ"Alpy" dump, Wełnowiec-Józefowiec, Katowice, Silesian Voivodeship, Poland |
| 57.6km (35.8 miles) | ⓘRudniki iron mine, Rudniki, Gmina Włodowice, Zawiercie County, Silesian Voivodeship, Poland |
| 58.2km (36.2 miles) | ⓘDębieńsko Mine heap, Gmina Czerwionka-Leszczyny, Rybnik County, Silesian Voivodeship, Poland |
| 61.5km (38.2 miles) | ⓘŁosień, Dąbrowa Górnicza, Silesian Voivodeship, Poland |
| 62.7km (39.0 miles) | ⓘKawa, Dąbrowa Górnicza, Silesian Voivodeship, Poland |
| 68.5km (42.6 miles) | ⓘStarzykowiec coal-mining dump, Chwałowice, Rybnik, Silesian Voivodeship, Poland |
| 70.4km (43.8 miles) | ⓘRydułtowy heap (Szarlota heap), ROW Ruch Rydułtowy Mine, Rydułtowy, Wodzisław County, Silesian Voivodeship, Poland |
| 76.3km (47.4 miles) | ⓘSanidine and pyroxene hornfels outcrops, Gracze, Gmina Niemodlin, Opole County, Opole Voivodeship, Poland |
| References |
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| Reference Search (possible matching items) |
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 | | Report (issue) | | biotic crisis—Evidence from continental strata in Poland . . . . . . . . . . . . . . . . 263 Grzegorz Pieńkowski...the Triassic–Jurassic continental sediments of Poland and assess their effect on the end-Triassic mass...permission from the Rare Book Room, Buffalo & Erie County Public Library. elephant, the “Siberian Mammoth...with the absence of the characteristic boundary clay layer containing shocked minerals, suggests that...the characteristic Cretaceous-Paleogene boundary clay complex, 21 which contains shocked minerals and |
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