Zagi Mountain (Zegi Mountain; "Shinwaro"), Hameed Abad Kafoor Dheri, Peshawar, Khyber Pakhtunkhwa (North-West Frontier Province), Pakistan
This page is currently not sponsored. Click here to sponsor this page.
|Location is approximate, estimate based on other nearby localities.|
|Latitude & Longitude (WGS84):||34° North , 72° East (est.)|
|Margin of Error:||~87km|
|Köppen climate type:||Cfa : Humid subtropical climate|
|Name(s) in local language(s):||Zaga Ghar|
Alpine-type veins, hosted in alkaline granite gneiss of the Warsak igneous complex. Located near Hameed Abad Kafoor Dheri and approximately 5.5 km southeast of the Warsak Dam, about 40 km NNW of Peshawar, NWFP, Pakistan. Zagi Mountain covers an area of approximately 3 x 5 km, with an elevation of approximately 175 m above its surroundings.
Bastnäsite specimens from this locality were originally said to come from Shinwaro, "high in the mountains" of Konar Province, Afghanistan, when they first appeared on the market in 1999. This turned out to be a bogus locality in 2001 (Obodda & Leavens, 2004).
Although Zagi Mountain is fairly near Peshawar, the capital of the Khyber Pakhtunkhwa (North-West Frontier Province) and also the administrative centre (but not the capital) of the Federally Administered Tribal Areas (FATA) of Pakistan, it is not situated in Mulla Ghori (FATA).
27 valid minerals.
This page contains all mineral locality references listed on mindat.org. 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 mindat.org 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.
Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
- Obodda, H.P. and Leavens, P.B. (2004): Zagi mountain - Northwest frontier province, Pakistan. The Mineralogical Record, 35(3), 205-220.