Le Mazet vein, Échassières, Ébreuil, Allier, Auvergne-Rhône-Alpes, France
|Latitude & Longitude (WGS84):||46° 11' 56'' North , 2° 57' 32'' East|
|Latitude & Longitude (decimal):||46.19889,2.95889|
|Köppen climate type:||Cfb : Temperate oceanic climate|
|Name(s) in local language(s):||Filon du Mazet, Échassières, Ebreuil, Allier, Auvergne, France|
|Other/historical region names associated with this locality:||Auvergne; Rhône-Alpes|
On the right of the road, just 50 m before the first building of Le Mazet ore dressing, coming from Echassières.
During may 2008, trees were cut down and Le Mazet vein dumps became accessible.
The mineralization is similar to that of the Les Montmins mine (Ste Barbe vein), although the micromounts are usually not as spectacular.
NOTE: A detailed article on the mineralogy, including several new determinations for the whole Échassières area, is currently in preparation (U. Kolitsch, 2008-2016).
67 valid minerals.
This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.
Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org
|Permian - Carboniferous|
252.17 - 358.9 Ma
|Carboniferous-Permian plutonic rocks|
Age: Paleozoic (252.17 - 358.9 Ma)
Comments: Deep-seated to high-level intrusions are included. Many charnockites, anorthosites, and large ophiolites, classified as plutons, are distinguished in the database using the SIGNIF item. Ophiolites were classified as plutons, even where remnants may be extrusive and/or sedimentary.
Lithology: Plutonic rocks
Reference: Geological Survey of Canada. Generalized geological map of the world and linked databases. doi:10.4095/195142. Open File 2915d.