Ma'ale Adumim (Ma'aleh Adumim; Maale Adummim), Hatrurim formation, West Bank, Palestine
This page is currently not sponsored. Click here to sponsor this page.
|Location is approximate, estimate based on other nearby localities.|
|Latitude & Longitude (WGS84):||31° North , 35° East (est.)|
|Margin of Error:||~23km|
|Köppen climate type:||Csa : Hot-summer Mediterranean climate|
Clefts in Upper Cretaceous limestones exposed along the Jerusalem-Jericho road. These limestones belong to the Hatrurim Formation (qv), metamorphosed by endogenous heating (mud volcano).
Located about 5 km NW of the Nabi Musa hill.
Note: Although chromatite's type locality is given in some references as in Jordan, and the area was technically part of Jordan when chromatite was described, the West Bank is now Palestine and is no longer claimed by Jordan.
20 valid minerals. 1 (TL) - type locality of 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)
E. Sokol, I. Novikov, S. Zateeva, Ye. Vapnik, R. Shagam and O. Kozmenko (2010): Combustion metamorphism in the Nabi Musa dome: new implications for a mud volcanic origin of the Mottled Zone, Dead Sea area. Basin Resarch 22, 414-438.
Sokol, E.V., Gaskova, O.L., Kokh, S.N., Kozmenko, O.A., Seryotkin, Y.V., Vapnik, Y., Murashko, M.N. (2011): Chromatite and its Cr3+- and Cr6+-bearing precursor minerals from the Nabi Musa Mottled Zone complex, Judean Desert. American Mineralogist 96, 659-674.