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Zapachitsa Cu deposit (Zapacica; Zapachica Mine), Bov, Svoge Obshtina, Sofiya Oblast (Sofia Oblast), Bulgaria

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Location is approximate, estimate based on other nearby localities.
Latitude & Longitude (WGS84): 42° North , 23° East (est.)
Margin of Error:~26km

A copper deposit located in the Western Stara-Planina Mts.

Mineral List

22 valid minerals. 1 (TL) - type locality of valid minerals.

The above list contains all mineral locality references listed on This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.


Minceva-Stefanova, J. (1962): New minerals for Bulgaria: tyrolite, cornwallite, conichalcite, euchroite and cuproadamite. - Bull. Geol. Inst., Bulg. Acad. Sci., 10, 23-38 (in Bulgarian with German summary).

Minceva-Stefanova, J. (1964): Zink-Olivenit aus der Lagerstätte Zapačica und uber den Chemismus und die Ablagerung der Kupferarsenate. - Chemie der Erde, 23, 4, 248-258.

Minceva-Stefanova, J. (1968): Strashimirite - a new hydrated copper arsenate. - Zap. Vses. Mineral. Obsht. 97, 4, 470-477 (in Russian).

Minceva-Stefanova, J. (1986): Parageneses of strashimirite. - Geochem., Mineral. and Petrol., 20-21, 49-57 (in Bulgarian).

Minceva-Stefanova, J. (1993): Cornubite in paragenesis with cornwallite from Zapachitsa Deposit, Western Stara Planina, Bulgaria. - Compt. rend. Acad. bulg. Sci., 46, 4, 65-68.

Minceva-Stefanova, J. (1999): Arseniosiderite and kolfanite from Zapachitsa deposit, Western Balkan, Bulgaria. - Compt. rend. Acad. bulg. Sci., 52, 5/6, 65-68.

Minceva-Stefanova, J. (2001): Arsenate minerals diversity in oxidation zones of the polymetallic stratabound deposits in Western Balkan Mountain. - Compt. rend. Acad. bulg. Sci., 54, 6, 39-42.

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