English version
MALMDATABASEN
Registrering 3114 - 004 Haugengruva (Våler)
(Objekt Id: 6628)
(Sist oppdatert: 09.07.2025)

Lokalisering
Fylke: Østfold Kommune: Våler (3114)
Kart 1:50000: Vannsjø (1913-4) Kart 1:250000: Oslo
Koordinatsystem: EU89-UTM Zone 32
Øst: 609839 m. Nord: 6593611 m.
Lengdegrad: 10.9383120 Breddegrad: 59.4666120
Kartvisning

Ressurs
Ressurstype: Jernlegeringsmetaller (Cr,Ni,Co,V,Mo,W) Ressursundertype: Nikkel
Element(er): Ni Cu
Betydning
Råstoffbetydning: Liten betydning (reg. 18.02.2015)

Ressurser og produksjon
Aktivitet: Prøvedrift Reserver:
Driftsmetode: Dag- og underjordsdrift Historisk produksjon: ,1 tusen tonn


Produkt
Element/produkt Gehalt/Kvalitet Reg. dato
Ni 1.5 % 18.02.2005

Mineralisering
Æra: Proterozoikum Periode: Mesoproterosoikum
Genese: Ortomagmatisk Form: Uregelmessig
Hovedtekstur: Strukturløs Min. fordeling: Semi-massiv
Kornstørrelse: Finkornet (<1 mm) Hovedomvandling:
Strøk/Fall: Retning:
Feltstupning:
Stratigrafisk klassifikasjon av vertsbergart
Æra: Proterozoikum Periode: Mesoproterosoikum
Provins: Østnorske grunnfjellsprovins
Geotek.enhet: Østfoldkomplekset
Tektonisk complex:
Intrusivt komplex: Iddefjordbatolitten
Gruppe: Formasjon:

Mineralogi
Relasjon Mineral Mengde
Gangmineral Plagioklas Hovedmineral (>10%)
Gangmineral Amfibol Hovedmineral (>10%)
Malmmineral Magnetkis Hovedmineral (>10%)
Malmmineral Kobberkis Underordnet mineral (1-10%)
Malmmineral Pentlanditt Underordnet mineral (1-10%)

Litologi:
Relasjon Bergart Opprinnelse
Vertsbergart Metagabbro Intrusiv
Opprinnelig bergart :Gabbro
Metamorf fase :Amfibolitt

Opplysning(er) i fritekstformat
Fri tekst
Er det denne som er Haugen gruve/Haugengruva/gruva i Haugenskogen? Foslie (1926) lister opp Haugen skjerp, med omtrentlig samme plassering. I følge Rekstad (1921) skal malmen består av magnetkis med litt kobberkis.
Beliggenhet
En vegbeskrivelse fra rv115 ved Skjønnerød: Følg skogsbilveg fra gokart-banen. Etter ca 500 meter, følg merket løype (blå) i ca 800 m fra skogsbilvegen og over et hogsfelt og ned i en kløft. Haugengruva ligger på venstre side av stien når du kommer nordøstfra.

Litteraturfortegnelser:
Fra NGU's Referansearkiv.:
Rekstad, J. , 1921
Eidsberg. De geologiske forhold innen rektangelkartet Eidsbergs område
;Norges geologiske undersøkelse;KARTBESKRIVELSE; BOK;NGU; No.88;76 sider
Abstrakt:
The territory is situated in south-eastern Norway to the east of the Oslofjord. It is an inland district which at no place reaches the sea. Glomma is the chief river which runs through the country in a southerly direction. The rocks occurring here are gneiss, granite, gabbro and schistose amphibolite, all of them of Archean age. Gneiss occupies a large area of the region. The rock has a varied appearance. Partly it is rich in mica (mica gneiss), partly it contains hornblende (hornblende-gneiss), partly it is coarse-grained and of granitoid texture. This latter form embraces also granite which has been deformed by powerful mechanical forces. This granite is intermixed with the gneiss in such a way as to make it impossible to separate them on the map. For the most part there is no distinctive demarcation between them, but the one passes into the other. The gneiss is mostly stratified, with well defined strike and dip. The granite intermixed is younger than the gneiss, but it belongs to the oldest known granites of Scandinavia. The gneiss is for the most part of igneous origin. Gabbro and amphibolite occur as numerous lenses injected into the gneiss. Connected with the gabbro here occurs nickelferous pyrrhotite. The greatest of these occurrences is at Romsås.

Foslie, Steinar , 1925
Syd-Norges gruber og malmforekomster.
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.126;1-89 + ka sider
Abstrakt:
On the map accompanying this paper all the mines and ore deposits of Southern Norway are collected for the first time.The material has been gathered from printed and unprinted sources, communications from mining engineers and geologists, and through personal visits. Included are all mines and ore deposits of former, present and future importance. Among the 1407 deposits on the map, there are furthermore included all of doubtful value and many which are quite unworkable, but of geological interest, or those which mark the distribution of ore bearing formations. For this reason it has been necessary to mark the deposits with signs of different size. The object is only to facilitate a comprehensive view of the map, and is not an effort of economic classification, which for most of them would be quite impossible. The sizes refer to the presumed importance of the ore deposit, and has nothing to do with the extent of the mining operations. Mines and deposits out of work during the period 1913-1923 have been separately marked (see the legend), also deposits which were formerly of much greater importance than now. For the smallest mines and deposits no distinction has been made in these respects. Among them are represented partly those, which are in reality unworkable, partly those which are little investigated.

Navn på lokalitet: Stollinngang
(Objekt Id: 40659 4,01,00)

Lokalisering
Fylke: Østfold Kommune: Våler (3114)
Kart 1:50000: Vannsjø (1913-4) Kart 1:250000: Oslo
Koordinatsystem: EU89-UTM Zone 32
Øst: 609823 m. Nord: 6593624 m.
Lengdegrad: 10.9380190 Breddegrad: 59.4667250
Kartvisning

Ressurs
Ressurstype: Jernlegeringsmetaller (Cr,Ni,Co,V,Mo,W) Ressursundertype: Nikkel
Element(er): Ni Cu
Ressurser og produksjon
Aktivitet: Prøvedrift Reserver:
Driftsmetode: Underjordsdrift Historisk produksjon:


Faktaarket ble generert 15.07.2025

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