The paper presents the results of geological investigations in the adit after uranium prospecting works
in Jagniątków. A detailed morphological plan and a geological map was shown. The basic rock types and
tectonic structures have been distinguished. In the adit, there is a contact of main Karkonosze granite
types, paralell dislocation zones and signs of various mineralization are well visible.
REFERENCES(3)
1.
BORKOWSKA M., Petrografia granitu Karkonoszy, Geologia Sudetica vol. II 1966, 7–119.
SZTUK H., ADAMSKI W., GAWOR F., Inwentaryzacja uszkodzeń środowiska na skutek prowadzenia poszukiwań i eksploatacji złóż uranowych, Arch. Inst. Górn. Polit. Wr. 29, 1992.
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