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Norsk versjon | ||||
| THE INDUSTRIAL MINERAL DATABASE | |||||
| Deposit Area 806 - 309 | |||||
| (Last updated 05.des.2024) | |||||
Name of Deposit Area : Flittig pike |
| (Object Id : 0806,309,00,00) |
| Location |
| County : | Telemark (08) | Municipality : | Skien (0806) |
| Map 1:50000: | Nordagutu (1713-4) | Map 1:250000: | Skien |
| Marking point: | Longitude: | 9.5773440 | Latitude: | 59.3191340 |
| EU89-UTM Zone 32 | (Coordinates IS confirmed) |
| X-coord: | 532862 m. | Y-coord: | 6575731 m. |
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| Commodity |
| Main Type: | Other industrial minerals | Sub Type: | Apatite |
| Importance |
| Public: | (No data) |
| Economical: | Not classified/evaluated |
Mineralization |
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| Main texture: | Min. distribution: |
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Information(s) in free text format |
| Free text |
| The occurrence of Flittig pike is an 10 m long, 3 m wide and 3 m deep old excavation pit. We updated the GPS coordinates. The occurrence is located at the contact between the syenites from the Siljan intrusion and the Skien B1 basalts. The rock is characterized by a large concentration of euhedral zircon crystlas, constituting 15% modal of the rock and associated with diopside (40%), magnetite and hemo-ilmenite (30%), feldspar (10%), accessory apatite, biotite, chlorite, and quartz. Whole rock analyses indicate concentration of more than 2 wt% zirconium, around 2000 ppm Y+TREE and more than 1000 ppm niobium. The occurrence is very small and not significant economically; however, such anomalous concentrations in high field strength elements are worth recording. |
Bibliography: |
| References not to be found in NGU's Reference Archive.: |
| Wang, Y., Coint, N., Mansur, E. T., Acosta-Gongora, P., Miranda, A. C. R., Nasuti, A. & Baranwal, V. C. (2024). Leveraging Domain Expertise in Machine Learning for Critical Metal Prospecting in the Oslo Rift: A Case Study for Fe-Ti-P-Rare Earth Element Mineralization. Minerals 14, 377. |
| The fact sheet was created on 17.01.2026 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2026 Geological Survey of Norway |