Kaolinite occurrence maximum 2-3m thick. Geologically interesting because of the possibility to see the close connection between kaoline and almost unweathered grey gneiss.
Local productionof white clay& kaolin.
References
Bergström, J. & Shaikh, N.A.: (1980): Malmer, industriella mineral och bergarter i Kristianstads län. SGU Rapporter och meddelanden 22. 90 p
Mineral List
5 entries listed. 2 valid minerals.
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