(Jedová hora (Dědova hora) u Neřežína)
Abandoned sedimentary Fe-Hg deposit in Ordovician volcanosedimentary rocks od Barrandien. Iron ores are developed in two stratiform bodies composed of siderite and hematite. Bodies are intersected by the system of vertical fissures with hydrothermal mineralization (quartz, siderite, ankerite, pyrite, cinnabar and baryte).
Ref.: Velebil, D.: Jedová hora (Dědova hora) u Neřežína. Bulletin mineralogicko-petrografického oddělení Národního muzea v Praze, 2003, roč. 11, s. 86-99.
Mineral List:24 entries listed. 24 valid minerals.
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