Norsk versjon
THE ORE DATABASE
Occurence 1806 - 052 Hestvikåsen
(Object Id: 2492)
(Last updated: 07.02.2024)

Location
County: Nordland Municipality: Narvik (1806)
Map 1:50000: Skjomen (1331-1) Map 1:250000: Narvik
Coordinate system: EU89-UTM Zone 33
East: 576791 m. North: 7587797 m.
Longitude: 16.8688620 Latitude: 68.3925620
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Resource
Resource Type: Ferrous metals(Fe, Mn, Ti) Resource Subtype: Manganese
Element(s): Fe Mn
Importance
Raw material meaning: Not Assessed (reg. 18.02.2015)

Resources and production
Activity: Pitting Reserves:
Operating method: Underground mining Historical production:


Products
Element/product Crude ore grade or quality Reg. date
Fe-mag. 30.5 % 04.01.1993
Fe-total 33.5 % 04.01.1993
MnO 1-10 % 04.01.1993
P 0.38 % 04.01.1993
S 0.004 % 04.01.1993

Operations
From - To Activity Comments
1899 - 1906 Pitting Company/Institution :A/S Håfjellets jernfelter
1935 - 1945 Geology Company/Institution :NGU
1976 - 1977 Geology Company/Institution :Rana Gruber

Mineralization
Era: Proterozoic Period: Neoproterozoic
Genesis: Sedex Form: Lens
Main texture: Banded Min. distribution: Semi-massive (20-50 % ore minerals)
Main grain size: Medium grained (1-3 mm) Main alteration:
Strike/Dip: 240 / 70 Direction: 260
Plunge: 20
Stratigraphic classification of host rock
Era: Proterozoic Period: Neoproterozoic
Province: Caledonides
Geotec.unit: Seve-Køli Nappe Complex
Tectonic complex: Upper allochton
Igneous complex:
Group: Salangen-group Formation: Håfjell iron formation

Mineralogy
Relationship Mineral Amount
Gangue mineral Garnet Major mineral (>10%)
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Apatite Subordinate mineral (1-10%)
Gangue mineral Amphibole Subordinate mineral (1-10%)
Ore mineral Hematite Major mineral (>10%)
Ore mineral Magnetite Major mineral (>10%)

Lithology:
Relationship Rock Origin
Host rock Calcite marble Sedimentary
Original rock :Limestone
Metamorphic facies :Amphibolite
Host rock Calcite bearing mica schist Sedimentary
Original rock :Argillaceous sediment
Metamorphic facies :Amphibolite
Wall rock (Garnet) mica schist Sedimentary
Original rock :Marl
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Wall rock Primary layering Strike/Dip :240 / 60 Syn-mineralisation ;...Effect :None
Wall rock Fold axis Strike/Dip :270 / 20 Post-mineralisation ;...Effect :Modifies

Information(s) in free text format
Free text
Dette er et langt malmdrag som går fra Ofotfjorden ved Hestvika i SV-retning forbi Aspelund gård mot Toppåsen. Forekomsten strekker seg fra Hestvikneset, over Hestvikåsen, over Aspelund gård og til Heggåelva. Draget er 700 m langt. Mineraliseringen er også blottet i veiskjæring ved Aspelund gård. Ved Hestvikneset er det en hovedmineralisering og 3 andre mineraliserte lag litostratigrafisk over. Hestvikneset viser et godt blottet profil prøvetatt av T. Sørdal og I. Lindahl 04.09.92. Prøvene fra 1 til 7 er tatt nedenfra og oppover i litostratigrafien (mot senter av mulden) Ca. 5 røskegrøfter med sprengning er gjort langs draget. Kornstørrelsen varierer fra middelskornig (mt.-malm) til mer finkornig hem.malm. Stedvis er det en skarn type malm med høyt granatinnhold. Malmen ligger i en variert glimmerskifer sone som er omtrent 50 m tykk omgitt av kalmarmor. Ingen rapporter i Bergarkivet går direkte på forekomsten.

Bibliography:
From NGU's Reference Archive:
Foslie, Steinar , 1949
Håfjellsmulden i Ofoten og dens sedimentære jern-mangan-malmer. Søndre Ofotens malmforekomster II.
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.174;1-129 + f pages
Abstract:
The sedimentary hematite-magnetite ores of marine origin, occurring within the crystalline mica schists of the caledonian mountain of Northern Norway, belong to a characteristic type of iron ore deposits, internationally known as the Dunderland ore type. Such deposits are known from latitude 65 degrees 20' to 69 degrees 40' N, thus covering a distance along the mountain chain of about 550 km. Transversely to this direction, they are known for at most 90 km, but generally much less. It is significant, that they do not occur farther southwards along the mountain chain, nor in its eastern part. The reason seems to be, taht they are connected with the so-called western development or the mountain chain formations, which disappear below the ocean in the Trondheim district. Compared with the eastern development, it is characterized by greater thickness of the sedimentary series, a far more considerable part of crystalline limestones and - so faar as now known - absence of the basic lavas (greenstone formation), which are important in the east and south. It belongs to a more central part of the geosyncline. The southern and greater part of the ore-bearing district is so strongly folded, that it has been difficult to establish the stratigraphic relation between the different deposits or their proper place within the formations.

Fieldsamples
Sample No. Sample type Miscellanrous
Hestvik-1 Bedrock
Sampler: Bjerkgård/Raaness/...Stored: Løkken
Comment: Finkornet mangangranat med magnetittslirer
No. of registrated oxide analyses = 1
Hestvik-2 Bedrock
Sampler: Bjerkgård/Raaness/...Stored: Løkken
Comment: Båndet magnetitt med noe mangan
No. of registrated oxide analyses = 1
Hestvik-3 Bedrock
Sampler: Bjerkgård/Raaness/...Stored: Løkken
Comment: Kvarts- og biotitt-amfibolbåndet med mm-cm hematitt og magnetittbånd
No. of registrated oxide analyses = 1
NO0354.02 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Magnetite skarn ore, 1 metres thick.
No. of registrated element analyses = 1
NO0354.03 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Banded relatiuvely poor ore of 1.5 metres.
No. of registrated element analyses = 1
NO0354.04 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Banded magnetite - hematite ore.
No. of registrated element analyses = 1
NO0354.05 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Magnetite - hematite skarn ore.
No. of registrated element analyses = 1
NO0354.06 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Banded coarse grained hematite- magnetite ore
No. of registrated element analyses = 1
NO0354.07 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Sulphide bearing layer i uopper part of iron formation.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Sample point: Aspelund
(Object Id: 4036 52,00,01)

Location
County: Nordland Municipality: Narvik (1806)
Map 1:50000: Skjomen (1331-1) Map 1:250000: Narvik
Coordinate system: EU89-UTM Zone 33
East: 576462 m. North: 7587554 m.
Longitude: 16.8606590 Latitude: 68.3904730
Show on map

Resource
Resource Type: Ferrous metals(Fe, Mn, Ti) Resource Subtype: Manganese
Element(s): Fe


Fieldsamples
Sample No. Sample type Miscellanrous
NO0354.01 Bedrock
Sampler: Lindahl, I./...Stored: Løkken
Comment: Hematie ore in road cut.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Sample point: Prøvepunkt
(Object Id: 39471 52,00,02)

Location
County: Nordland Municipality: Narvik (1806)
Map 1:50000: Skjomen (1331-1) Map 1:250000: Narvik
Coordinate system: EU89-UTM Zone 33
East: 576759 m. North: 7587810 m.
Longitude: 16.8680700 Latitude: 68.3926960
Show on map

Resource
Resource Type: Ferrous metals(Fe, Mn, Ti) Resource Subtype: Manganese
Element(s): Fe Mn


Fieldsamples
Sample No. Sample type Miscellanrous
obs.pkt.52 Bedrock
Sampler: Bjerkgård/Raaness/...Stored: Løkken
Comment: Båndet kvarts-amfibol-magnetittmineralisering
No. of registrated oxide analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 1806 - 052 Hestvikåsen

Element analyses

( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.)
Sample No. Sample Type Cu* Zn* Pb* Co* Ni* Ag* Au#
NO0354.01 Bedrock 8 153 87 74 53 .3 9.0
NO0354.02 Bedrock 13 694 414 150 220 .6 6.0
NO0354.03 Bedrock 2 415 370 34 22 .1 4.0
NO0354.04 Bedrock 7 63 16 14 7 .1 8.0
NO0354.05 Bedrock 4 85 41 82 76 .4 4.0
NO0354.06 Bedrock 2 57 33 21 7 .1 12.0
NO0354.07 Bedrock 38 56 9 12 45 .1 2.0
------------------
Sample No. Pt# Pd# As* Cd* Ba* Mo* Sb* Bi* S%
NO0354.01 3.0 3.0 14 .3 19 1.00 2 2 .03
NO0354.02 3.0 3.0 5 1.8 15 1.00 2 3 .18
NO0354.03 3.0 3.0 2 1.2 164 1.00 5 5 .12
NO0354.04 3.0 3.0 2 .2 162 1.00 2 2 .01
NO0354.05 3.0 3.0 4 .8 37 1.00 2 2 .01
NO0354.06 3.0 3.0 5 .2 20 1.00 2 2 .02
NO0354.07 3.0 3.0 2 .2 15 1.00 2 3 2.68
------------------
Sample No. V* Cr* Mn* Fe% Th* U* W* Sr* La*
NO0354.01 12 12 13458 14.59 2.00 5.00 1 170.0 10.00
NO0354.02 42 18 12738 21.49 2.00 5.00 1 155.0 4.00
NO0354.03 34 16 5828 22.68 2.00 5.00 1 103.0 6.00
NO0354.04 37 21 579 19.46 2.00 13.00 1 34.0 7.00
NO0354.05 18 16 9390 13.77 2.00 5.00 1 260.0 10.00
NO0354.06 24 14 2857 19.25 2.00 5.00 1 92.0 5.00
NO0354.07 5 17 87 4.00 12.00 5.00 2 39.0 25.00
------------------
Sample No. B*
NO0354.01 2
NO0354.02 2
NO0354.03 2
NO0354.04 2
NO0354.05 2
NO0354.06 3
NO0354.07 3

Oxide analyses

( All values are in % )
Sample No. Sample Type SiO2 Al2O3 TiO2 Fe2O3 MnO MgO CaO
Hestvik-1 Bedrock 50.33 12.56 0.66 10.33 15.58 1.96 5.96
Hestvik-2 Bedrock 30.41 3.70 0.18 55.43 5.74 1.44 3.07
Hestvik-3 Bedrock 28.54 2.96 0.19 34.18 0.40 5.69 15.20
obs.pkt.52 Bedrock 34.32 3.13 0.26 54.53 0.19 2.55 4.13
------------------
Sample No. Na2O K2O P2O5 Loss Sum
Hestvik-1 -0.01 0.08 0.16 3.18 101.00
Hestvik-2 -0.01 0.05 0.49 0.58 101.00
Hestvik-3 0.62 0.10 0.34 12.12 100.00
obs.pkt.52 0.29 0.10 0.47 0.44 100.00


The fact sheet was created on 29.04.2024

Questions or comments regarding the fact sheet can be emailed to:
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