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Diesrut Alp, Vrin, Lumnezia, Surselva Region, Grisons, Switzerlandi
Regional Level Types
Diesrut AlpMountain
VrinVillage
LumneziaMunicipality
Surselva RegionRegion
GrisonsCanton
SwitzerlandCountry

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Latitude & Longitude (WGS84):
46° 38' 52'' North , 9° 4' 59'' East
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Vrin273 (2017)1.5km
Lumbrein428 (2017)5.7km
Vignogn175 (2017)8.0km
Vals Platz1,006 (2017)8.2km
Obersaxen757 (2017)11.4km
Mindat Locality ID:
239096
Long-form identifier:
mindat:1:2:239096:6
GUID (UUID V4):
0
Name(s) in local language(s):
Alp Diesrut, Vrin, Val Lugnez (Val Lumnezia), Graubünden (Grisons; Grischun), Schweiz (Suisse; Svizzera)


South-eastern slopes of Artg Diesrut mountain, about 5 km south-west of Vrin. This locality is part of the Parker (1973) locality of Piz Vrin on pages 216 and 225.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


3 valid minerals.

Detailed Mineral List:

Anatase
Formula: TiO2
References:
Quartz
Formula: SiO2
References:
Rutile
Formula: TiO2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Rutile4.DB.05TiO2
Anatase4.DD.05TiO2

List of minerals for each chemical element

OOxygen
O AnataseTiO2
O QuartzSiO2
O RutileTiO2
SiSilicon
Si QuartzSiO2
TiTitanium
Ti AnataseTiO2
Ti RutileTiO2

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate
  • AlpsAccretionary Complex
EuropeContinent

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.
 
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