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Landås 07 Feldspar Quarries (Beinmyr quarries), Landås, Iveland, Aust-Agder, Norway

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Latitude & Longitude (WGS84): 58° 30' 3'' North , 7° 51' 36'' East
Latitude & Longitude (decimal): 58.50108,7.86001
GeoHash:G#: u4msfcg3r
Other regions containing this locality:Scandinavia
Locality type:Group of Quarries
Köppen climate type:Dfc : Subarctic climate


Bjørlykke locality n° 47.

Barth (1931) designates this as Landås III (not to be confused with Landås 3 Feldspar Quarry).

The Landås 7 quarries comprise at least eight separate quarries and prospects, all working in the same pegmatite.

A map Stensrud (2009) has drawn shows only four quarries.

It seems he overlooked the largest of all Landås 7 quarries, which lies just north of his 7 and 7b localities.

Corneliussen at pegmatite.no lists eight localities, some of which are hard to see on the altitude map.

The coordinates are given for a point in the middle of the quarries.

There are probable prospects at:
58.50184°N 7.85898°E
58.50108°N 7.85963°E
58.50115°N 7.86144°E
58.50101°N 7.85981°E

North of Beinmyr 8 there has been prospected at several places, difficult to recognize with certainty at the altitude map:
58.50109°N 7.86214°E
58.50105°N 7.86205°E
58.50103°N 7.8622°E
58.50131°N 7.86249°E
etc.

Coordinates © Kartverket - https://www.kartverket.no


Commodity List

This is a list of exploitable or exploited mineral commodities recorded from this region.


Mineral List

Mineral list contains entries from the region specified including sub-localities

16 valid minerals.

Rock Types Recorded

Note: this is a very new system on mindat.org and data is currently VERY limited. Please bear with us while we work towards adding this information!

Rock list contains entries from the region specified including sub-localities

Select Rock List Type

Alphabetical List Tree Diagram

Regional Geology

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

Proterozoic
541 - 2500 Ma



ID: 3186372
Proterozoic crystalline metamorphic rocks

Age: Proterozoic (541 - 2500 Ma)

Lithology: Granitoid gneiss; orthogneiss/paragneiss

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. [154]

Mesoproterozoic - Paleoproterozoic
1000 - 2500 Ma



ID: 3133829
Proterozoic I gabbro

Age: Proterozoic (1000 - 2500 Ma)

Description: undifferentiated metamorphic

Lithology: Major:{gabbro}, Minor{diorite,plutonic ultramafic group,meta-gabbro}

Reference: Asch, K. The 1:5M International Geological Map of Europe and Adjacent Areas: Development and Implementation of a GIS-enabled Concept. Geologisches Jahrbuch, SA 3. [147]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License


Localities in this Region
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References

Sort by Year (asc) | by Year (desc) | by Author (A-Z) | by Author (Z-A)
Barth, T.F.W. (1931) Feltspat III. Forekomster i Iveland og Vegusdal i Aust-Agder og i flere herreder i Vest-Agder. Norges Geologiske Undersøkelse nr 128b, 111-150.
Bjørlykke, H. (1934) The Mineral Paragenesis and Classification of the Granite Pegmatites of Iveland, Setesdal, Southern Norway. Norsk Geologisk Tidsskrift 14, 211-311.
Jensen, B. and Frigstad, O.F. (1967) Large beryl crystals. in Geologisk Museum. Interne notater 1961-1990. Published by Geologisk Museums Venner, Oslo 1991, p 16.
Pedersen, R. (ed.) (2007) Iveland V: Gruvedrift. Iveland Bygdesogenemd. 382 p.
Stensrud, S. (2009) De opptredende mineraler på granittpegmatittganger i Iveland og Evje. Unpublished paper based on 4 previous papers written together with Johan Løchen.

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