Sandsøya Southeast, Sandsøya, Sande, Møre og Romsdal, Norwayi
| Regional Level Types | |
|---|---|
| Sandsøya Southeast | Outcrop |
| Sandsøya | Island |
| Sande | Municipality |
| Møre og Romsdal | County |
| Norway | Country |
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Latitude & Longitude (WGS84):
62° 14' 49'' North , 5° 29' 23'' East
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Larsnes | 511 (2010) | 6.7km |
| Tjørvåg | 352 (2013) | 13.1km |
| Kvalsvik | 265 (2013) | 13.5km |
| Haddal | 320 (2013) | 20.0km |
| Ulsteinvik weather pws station | 5,000 (2013) | 21.2km |
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Olivin Steinklubb | Fiskå | 16km |
| Ålesund og Omegn Geologiforening | Ålesund | 41km |
Other Languages:
Norwegian:
Sandsøya nordøst, Sandsøya , Sande, Møre og Romsdal, Norge
Outcrop of a garnet–biotite amphibolite.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsMineral List
Rock Types Recorded
Note: data is currently VERY limited. Please bear with us while we work towards adding this information!
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Root, D.B, Hacker, B.R., Gans ,P.B., Duceaa, M.N. Eide ,E.A. and Mosenfelder, J. L. (2005) Discrete ultrahigh-pressure domains in the Western Gneiss Region, Norway: implications for formation and exhumation. Journal of Metamorphic Geology, 23,45–61 |
| ⓘ 'Garnet Group' Formula: X3Z2(SiO4)3 Reference: Root, D.B, Hacker, B.R., Gans ,P.B., Duceaa, M.N. Eide ,E.A. and Mosenfelder, J. L. (2005) Discrete ultrahigh-pressure domains in the Western Gneiss Region, Norway: implications for formation and exhumation. Journal of Metamorphic Geology, 23,45–61 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Unclassified Minerals, Rocks, etc. | |||
|---|---|---|---|
| ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| ⓘ | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| O | Oxygen | |
| O | ⓘ Garnet Group | X3Z2(SiO4)3 |
| O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| F | Fluorine | |
| F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Mg | Magnesium | |
| Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Al | Aluminium | |
| Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Si | Silicon | |
| Si | ⓘ Garnet Group | X3Z2(SiO4)3 |
| Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| K | Potassium | |
| K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Ti | Titanium | |
| Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
| Fe | Iron | |
| Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Geochronology
Mineralization age: Neoproterozoic : 992 ± 5 Ma to 894 ± 7 MaImportant note: This table is based only on rock and mineral ages recorded on mindat.org for this locality and is not necessarily a complete representation of the geochronology, but does give an indication of possible mineralization events relevant to this locality. As more age information is added this table may expand in the future. A break in the table simply indicates a lack of data entered here, not necessarily a break in the geologic sequence. Grey background entries are from different, related, localities.
| Geologic Time | Rocks, Minerals and Events | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Precambrian | ||||||||||
| Proterozoic | ||||||||||
| Neoproterozoic | ||||||||||
| Tonian |
| |||||||||
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A)Root, D.B, Hacker, B.R., Gans ,P.B., Duceaa, M.N. Eide ,E.A. and Mosenfelder, J. L. (2005) Discrete ultrahigh-pressure domains in the Western Gneiss Region, Norway: implications for formation and exhumation. Journal of Metamorphic Geology, 23,45–61
Other Regions, Features and Areas containing this locality
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