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THE ORE DATABASE
Deposit Area 1919 - 005
(Last updated 07.feb.2024)

Name of Deposit Area : Storvatnet
(Object Id : 1919,005,00,00)

Location
County : Troms (19) Municipality : Gratangen (1919)
Map 1:50000: Gratangen (1432-3) Map 1:250000: Narvik
Marking point: Longitude: 17.6604560 Latitude: 68.6230580
EU89-UTM Zone 33 (Coordinates IS confirmed)
X-coord: 608193 m. Y-coord: 7614671 m.

Commodity
Main Type: Ferrous metals(Fe, Mn, Ti) Sub Type: Iron
Element(s): Fe
Production
Activity: Exploration Reserves:
Prod. method: Production:
Prod. status: Volume of dump:

Importance
Public: Little Importance (reg. 18.02.2015)
Economical: Minor interest , (Confirmed 18.feb.2005 by Peter Ihlen)

Mineralization
Era: Period:
Dating: Method:
Genesis: Sedex Form: Layer
Main texture: Banded Min. distribution: Semi-massive (20-50 % ore minerals)
Main grain size: Fine grained (< 1 mm) Main alteration:
Strike/Dip: 35 / 40 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Period:
Province:
Geotec.unit:
Tectonic complex:
Igneous complex:
Group: Formation:

Mineralogy
Relationship Mineral Amount
Gangue mineral Amphibole Major mineral (>10%)
Ore mineral Magnetite Major mineral (>10%)

Lithology:
Relationship Rock Origin
Host rock amfibolitt Extrusive
Original rock :Tuff
Metamorphic facies :Amphibolite
Wall rock kalkspatmarmor Sedimentary
Original rock :Limestone
Metamorphic facies :Amphibolite

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Foliation Strike/Dip :35 / 40 Post-mineralisation ;...Effect :None

Information(s) in free text format
Free text
Det ble ikke funnet skjerp eller mineralisering øst for Storvatnet eller ved Mellomvasselva, hvor Gustavson (1974)sier det skal finnes. I veiskjæring langs E6, ved UTM 608200 7614650, er det en tynn magnetitt-mineralisering. I en vekslende enhet av kalkspatmarmor, kvartsittisk- og kalkglimmerskifer er det et vel 10cm mektig lag av finkornet amfibolitt med semimassiv til massiv magnetitt (prøve 01 og 02).

Bibliography:
From NGU's Reference Archive:
Gustavson, Magne; Vogt, Thorolf , 1974
Narvik. Beskrivelse til det berggrunnsgeologiske gradteigskart N9 - 1:100 000 (med fargetrykt kart).
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL; KARTBESKRIVELSE;NGU; Skrifter; No.308; 13;1-34 + ka pages
Abstract:
The geological map Narvik, published in 1950, is briefly described. The bedrock of this map area can be subdivided into autochthonous and allochthonous rocks. The autochthonous rocks comprise the Precambrian (mainly the Rombak window) and overlying conglomerate and sandstone of supposed Lower Cambrian age. An angular unconformity separates the Precambrian from Lower Cambrian. The allochthonous, Caledonian sequence can be subdivided into three thrust units. The main part of this sequence is probably Cambro-Silurian in age, but slices of deformed Precambrian granite occur at the base of the middle unit. Metamorphism of the allochthonous sequence took place in the epidote-amphibolite and almandine-amphibolite facies (up to kyanite grade). A chapter on the economic geology of the area and an excursion guide are included.

Fieldsamples
Sample No. Sample type Miscellanrous
Storvann-1 Bedrock
Sampler :Bjerkgård/Raaness/...Stored :Løkken
Comment :biotitt-amfibolskifer med bånd av magnetitt
No. of registrated oxide analyses = 1
TR0421.01 Bedrock
Sampler :Wilberg, R./...Stored :Løkken
Comment :Amfibolitt med semimassiv mt.
TR0421.02 Bedrock
Sampler :Wilberg, R./...Stored :Løkken
Comment :Amfibolitt med semimassiv mt.
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 1919 - 005 Storvatnet

Oxide analyses

( All values are in % )
Sample No. Sample Type SiO2 Al2O3 TiO2 Fe2O3 MnO MgO CaO
Storvann-1 Bedrock 40.85 3.09 0.15 47.93 0.80 1.71 5.53
------------------
Sample No. Na2O K2O P2O5 Loss Sum
Storvann-1 0.55 0.51 0.53 -1.11 101.00


The fact sheet was created on 09.12.2025

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