|Latitude & Longitude (WGS84):||45° 16' 6'' North , 7° 28' 53'' East|
|Latitude & Longitude (decimal):||45.26855,7.48161|
|Other regions containing this locality:||The Alps, Europe|
|Köppen climate type:||Cfb : Temperate oceanic climate|
|Name(s) in local language(s):||Ponte del Diavolo (Ponte del Roch), Lanzo Torinese, Valli di Lanzo, Massiccio di Lanzo, Torino, Piemonte, Italia|
Serpentinite outcrops of Mt. Buriasco and Mt. Basso, rispectively on the left and right banks of the River Stura di Lanzo, in proximity of the medieval bridge known as Ponte del Diavolo or Ponte del Roch.
Minerals are found in Alpine metamorphic veins in serpentinite.
13 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
145 - 201.3 Ma
|Cambrian - Proterozoic|
485.4 - 2500 Ma
|Precambrian-Phanerozoic crystalline metamorphic rocks|
Age: to Cambrian (485.4 - 2500 Ma)
Lithology: Crystalline metamorphic rocks
Reference: Chorlton, L.B. Generalized geology of the world: bedrock domains and major faults in GIS format: a small-scale world geology map with an extended geological attribute database. doi: 10.4095/223767. Geological Survey of Canada, Open File 5529.