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THE ORE DATABASE
Deposit 5026 - 011 Killingdal
(Object Id: 4403)
(Last updated: 07.11.2023)
Drill Cores: Killingdal

Location
County: Trøndelag Municipality: Holtålen (5026)
Map 1:50000: Ålen (1720-4) Map 1:250000: Røros
Coordinate system: EU89-UTM Zone 32
East: 626124 m. North: 6965217 m.
Longitude: 11.4731540 Latitude: 62.7954240
Show on map

Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Zinc
Element(s): Zn Cu Kis
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

Resources and production
Activity: Mining Reserves: 283 thousand tons
Operating method: Underground mining Historical production: 2959 thousand tons


Products
Element/product Crude ore grade or quality Reg. date
Cu 1,7 % 24.09.2001
Pb 0,4 % 24.09.2001
S 45,0 % 24.09.2001
Zn 5,5 % 24.09.2001

Operations
From - To Activity Comments
1677 - 1692 Regular production Company/Institution :Røros Kobberverk o.a.
Nordre grube
1791 - 1809 Regular production Company/Institution :Røros Kobberverk
Søndre grube
1822 - 1890 Test mining Company/Institution :Diverse interessenter
1891 - 1986 Regular production Company/Institution :A/S Killingdal Grubeselskap
Ulike eiere: 1888-1895 A. Huitfeldt & Co. 1895-1945 leid av The Bede Metal & Chemical Co. Ltd.

Mineralization
Era: Paleozoic Period: Ordovician
Genesis: Volcex Form: Plate
Main texture: Banded Min. distribution: Massive (>50 % ore minerals)
Main grain size: Fine grained (< 1 mm) Main alteration: Sericitisation
Strike/Dip: Direction: 270
Plunge: 30
Stratigraphic classification of host rock
Era: Paleozoic Period: Ordovician
Province: Caledonides
Geotec.unit: Trondheim Nappe Complex
Tectonic complex:
Igneous complex:
Group: Formation: Hersjø

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Calcite Subordinate mineral (1-10%)
Gangue mineral Chlorite Subordinate mineral (1-10%)
Gangue mineral Muscovite Subordinate mineral (1-10%)
Ore mineral Sphalerite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Pyrrhotite Subordinate mineral (1-10%)
Ore mineral Chalcopyrite Subordinate mineral (1-10%)
Ore mineral Bournonite Accessory mineral (<1%)
Ore mineral Molybdenite Accessory mineral (<1%)
Ore mineral Mackinawite Accessory mineral (<1%)
Ore mineral Tetrahedrite Accessory mineral (<1%)
Ore mineral Arsenopyrite Accessory mineral (<1%)
Ore mineral Galena Accessory mineral (<1%)
Ore mineral Covellite Accessory mineral (<1%)

Lithology:
Relationship Rock Origin
Wall rock Hornblende schist Extrusive
Original rock :Basalt
Metamorphic facies :Greenschist
Wall rock Quartz-sericite schist Extrusive
Original rock :Basalt
Metamorphic facies :Greenschist
Wall rock Chlorite schist Extrusive
Original rock :Basalt
Metamorphic facies :Greenschist
Wall rock Calcareous phyllite Sedimentary
Original rock :Argillaceous sediment
Metamorphic facies :Greenschist

Information(s) in free text format
Free text
The Killingdal deposit is hosted by massive greenstone, locally with relict pillow structures. There also are subordinate thin layers of felsic metavolcanic rocks in the area. The deposit consists of two ore bodies, the Main Orebody and the North Orebody, which are strongly elongated, with approximately lens-shaped cross sections and occur in the hinge of a regional-scale, isoclinal fold structure. The ore bodies are parallel for about 2500 m of known length and dips about 30o W. At higher levels, the width of the Main Orebody varies at 40–80 m, and has a mean thickness of about 3.5 m, with a maximum at 10–12 m. The cross section of the North Orebody is considerably less than that of the Main Orebody and it has been exploited to a lesser extent. Pyrite is the dominant mineral, while sphalerite and chalcopyrite are subordinate phases. The principal gangue minerals are quartz and muscovite. Bands of pyrrhotite-rich ore up to a couple of centimetres in thickness are located preferentially near the hanging wall. Chemical analyses show that the Main Orebody is rather homogeneous in composition, with a high bulk sulphide–gangue ratios in relation to the North Orebody. Production from the latter was also higher in zinc and lower in copper than the Main Orebody. The mine was worked to a depth of 1400 m along the dip of the ore, and about 3 Mt with 1.7 % Cu, 5.5 % Zn, 0.4 % Pb and 45 % S was produced during more than 300 years of mining.

Bibliography:
From NGU's Reference Archive:
Vogt, J.H.L.
Killingdal gruve.
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 2555;3 pages
Abstract:
Rapporten er en tysk rapport med fundament i Norges Malmforekomster 1906, og omhandler gruven.

M.E. , 1907
Killingdal Pyrites Mine, Norway.
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 3691;5 pages
Abstract:
Rapporten er en økonomisk vurdering av forekomsten.

Aasgaard, Gunnar , 1927
Gruber og skjerp i kisdraget Øvre Guldal-Tydal.
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.129;1-196 pages
Abstract:
The occurences described in this paper form a connection between th mining districts around Røros to the south and those around Meråker to the north. The occurences lie in mountain regions partly above the forest line. The list on page 12 contains the names of all known occurrences of whatever size within the district considered. Pl. I is a geological outline map of the district, compiled from maps in the Norwegian Geological Survey. In a geological summary on pages 18-27 it is shown that no pyrite occurrences of economic importance so far have been found in an eastern zone along the Swedish boundary where the rocks consist of hard schist with sparagmites, and igneous rocks. Neither have such occurrences been found in a zone of "Stuedalsskifer" and an other zone of "Gulaskifer" towards west, both indicated on the map. The occurrences of pyrite are chiefly found in connection with fine grained, light green or gravish, partly feldspar bearing schist and in connection with green schists, mostly fine grained hornblende schists. All these zones of schist gnereally strike north and dip west. The pyrite bearing schist lie on both sildes of a large zone of igneous rocks extending from Kjølifjell in the south over Hyllingen and Melshogna to Fangen in the Meråker district in the north.

Rui, Ingolf J. , 1968
Geologiske og petrografiske undersøkelser i traktene rundt Killingdal grube i Ålen, Sør.Trøndelag. Forsøk på å løse genetiske problemer i tilknytning til kismineraliseringen.
;UiO Geografisk inst.;AVHANDLING

Birkeland, Anne , 1986
Mineralogisk og geokjemisk undersøkelse av Killingdal gruven, Sør-Trøndelag.
;UiO Geologisk fellesråd;AVHANDLING

Nilsen, O.; Wolff, Fr.Chr. , 1989
Røros og Sveg. Berggrunnskart Røros og Sveg M 1:250 000; trykt i farger
;Norges geologiske undersøkelse;KART;1 kart pages
Abstract:
Beskrivelsen finnes på kartet.

References not to be found in NGU's Reference Archive.:
Rui, I. 1973: Structural Control and Wall Rock Alteration at Killingdal Mine, Central Norwegian Caledonides. Econ. Geology, 68, pp. 859-883.


Carlsen, Kjell B. 1984: A/S Killingdal Grubeselskap: Vurdering av fremtidig drift. BV7291

Fieldsamples
Sample No. Sample type Miscellanrous
Bh10 N64, 85.5-86.0 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh10 N64, 88.25-89.0 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh13 N64,17.85-19.25 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh8 N64, 49.3-50.0 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh9 N64, 63.0-64.0 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh9 N64, 64.0-65.3 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
Bh9 N64, 66.1-67.0 Core
Sampler: T. Bjerkgård/J.S. Sandstad
No. of registrated element analyses = 1
399862 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399863 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399864 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399865 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399866 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399868 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399869 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Killingdal Nord
(Object Id: 10030 11,01,00)

Location
County: Trøndelag Municipality: Holtålen (5026)
Map 1:50000: Ålen (1720-4) Map 1:250000: Røros
Coordinate system: EU89-UTM Zone 32
East: 626067 m. North: 6965654 m.
Longitude: 11.4723680 Latitude: 62.7993620
Show on map

Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Zinc
Element(s): Zn Cu Kis
Resources and production
Activity: Test mining Reserves:
Operating method: Underground mining Historical production:

Photo(s) from the Deposit area:
Photo no. 1 showing Killingdal nord"

Fieldsamples
Sample No. Sample type Miscellanrous
ST0200.01 Dump
Sampler: Sandstad, J.S./...Stored: Løkken/...Size(kg): 2
Comment: po+cpy malm, massive bånd (2-5 mm) i kvarts-amfibol bergart.
No. of registrated element analyses = 1
ST0200.02 Dump
Sampler: Sandstad, J.S./...Stored: Løkken/...Size(kg): 2
Comment: po bånd i mørk kloritttskifer, litt cpy rundt kvartlinser
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 5026 - 011 Killingdal

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#
Bh10 N64, 85.5-86.0 Core 3890 45200 2120 136 54 22.6 67.0
Bh10 N64, 88.25-89.0 Core 917 113000 8490 84 12 85.7 94.0
Bh13 N64,17.85-19.25 Core 3900 89500 5180 174 18 41.1 192.0
Bh8 N64, 49.3-50.0 Core 30100 44100 1635 642 11 26.8 178.0
Bh9 N64, 63.0-64.0 Core 20900 4400 106 291 10 22.0 288.0
Bh9 N64, 64.0-65.3 Core 18300 33900 3400 275 13 35.1 226.0
Bh9 N64, 66.1-67.0 Core 6850 210000 14900 89 35 74.8 232.0
ST0200.01 Dump 942 333 46 53 171 .7 21.0
ST0200.02 Dump 785 705 104 88 299 .8 24.0
399862 Dump 12000 78000 4405 123 23 21.9 67.0
399863 Dump 77000 19000 1074 107 12 19.7 68.0
399864 Dump 22000 4048 397 185 15 12.7 50.0
399865 Dump 6380 69000 2101 20 15 16.8 107.0
399866 Dump 1917 15000 8633 45 17 12.8 20.0
399868 Dump 8315 67000 5503 431 52 41.4 273.0
399869 Dump 6827 102000 7436 138 25 64.7 93.0
------------------
Sample No. Pt# Pd# As* Cd* Ba* Mo* Sn* Sb* Bi*
Bh10 N64, 85.5-86.0 2.5 4.0 441 115.5 1000 4.83 6 9 20
Bh10 N64, 88.25-89.0 2.5 2.0 1475 277.0 90 6.09 12 27 116
Bh13 N64,17.85-19.25 2.5 2.0 501 222.0 660 17.00 5 17 57
Bh8 N64, 49.3-50.0 2.5 .5 792 87.3 70 17.40 6 18 40
Bh9 N64, 63.0-64.0 2.5 .5 290 12.6 100 8.40 3 3 23
Bh9 N64, 64.0-65.3 2.5 .5 1320 75.5 60 10.75 8 88 54
Bh9 N64, 66.1-67.0 2.5 .5 1235 527.0 80 5.75 26 91 114
ST0200.01 12.0 38.0 319 1.6 65 8.00 -3 -3
ST0200.02 9.0 8.0 168 4.6 56 28.00 -3 -3
399862 149 142.2 12 20.00 8 30
399863 146 51.2 27 4.00 5 3
399864 378 11.2 7 24.00 7 3
399865 156 202.4 19 10.00 17 19
399866 139 33.5 36 13.00 32 13
399868 184 173.5 14 18.00 16 62
399869 222 213.0 17 12.00 17 180
------------------
Sample No. Se* Ga* Ge* In* S% V* Cr* Mn* Fe%
Bh10 N64, 85.5-86.0 33.00 16.35 0.23 2.15 10.00 75 27 144 27.10
Bh10 N64, 88.25-89.0 28.00 9.90 0.22 7.10 10.00 4 3 269 37.40
Bh13 N64,17.85-19.25 48.00 24.60 0.29 3.03 10.00 50 17 725 33.30
Bh8 N64, 49.3-50.0 127.00 10.05 0.51 3.62 10.00 13 3 127 40.60
Bh9 N64, 63.0-64.0 59.00 12.45 0.30 1.14 10.00 112 14 420 26.50
Bh9 N64, 64.0-65.3 50.00 9.93 0.29 2.42 10.00 25 13 84 29.60
Bh9 N64, 66.1-67.0 26.00 18.60 0.20 13.75 10.00 43 20 1250 26.20
ST0200.01 7.73 318 54 1640 15.96
ST0200.02 11.88 185 43 610 26.09
399862 1 165 252 10.00
399863 8 35 784 19.50
399864 2 107 404 10.00
399865 2 118 178 14.90
399866 8 152 78 14.60
399868 7 67 268 10.00
399869 1 48 168 10.00
------------------
Sample No. Th* U* W* Rb* Sr* Y* Zr* Nb* Ta*
Bh10 N64, 85.5-86.0 1.84 3.20 1 35.9 8.9 10.8 113 0.60 0.05
Bh10 N64, 88.25-89.0 0.03 0.40 1 1.3 0.8 0.3 1 0.05 0.03
Bh13 N64,17.85-19.25 2.35 2.40 1 20.4 22.5 13.6 76 1.50 0.09
Bh8 N64, 49.3-50.0 0.43 0.80 1 5.4 2.7 1.1 13 0.30 0.03
Bh9 N64, 63.0-64.0 0.67 0.70 1 22.5 24.7 9.3 63 2.00 0.12
Bh9 N64, 64.0-65.3 0.39 0.80 1 6.0 1.6 0.7 8 0.10 0.03
Bh9 N64, 66.1-67.0 1.51 0.70 1 17.6 33.9 5.2 15 0.60 0.05
ST0200.01 8.00 -8.00 -2 15.0
ST0200.02 8.00 -8.00 -2 7.0
399862 3.0
399863 4.0
399864 4.0
399865 3.0
399866 5.0
399868 5.0
399869 3.0
------------------
Sample No. Cs* La* Ce* B* Li* Be* P* Sc* Ti*
Bh10 N64, 85.5-86.0 0.27 6.60 19.05 6 0 90 9.00 760
Bh10 N64, 88.25-89.0 0.05 0.25 0.35 1 0 5 0.10 25
Bh13 N64,17.85-19.25 0.51 5.90 13.80 7 1 230 2.30 550
Bh8 N64, 49.3-50.0 0.16 0.90 2.02 3 0 10 0.40 70
Bh9 N64, 63.0-64.0 0.78 4.10 11.10 10 0 330 15.00 3070
Bh9 N64, 64.0-65.3 0.08 1.90 3.02 2 0 5 0.80 90
Bh9 N64, 66.1-67.0 1.19 6.30 13.30 5 0 120 3.00 490
ST0200.01 64.00 -3
ST0200.02 31.00 -3
399862 0.50 30
399863 4.00 300
399864 3.00 30
399865 6.00 30
399866 0.50 30
399868 3.00 30
399869 0.50 30
------------------
Sample No. Te* Hf* Re* Tl*
Bh10 N64, 85.5-86.0 0.35 3.10 0 17
Bh10 N64, 88.25-89.0 0.78 0.05 0 10
Bh13 N64,17.85-19.25 2.27 2.20 0 27
Bh8 N64, 49.3-50.0 2.73 0.40 0 11
Bh9 N64, 63.0-64.0 1.86 1.70 0 16
Bh9 N64, 64.0-65.3 1.53 0.20 0 15
Bh9 N64, 66.1-67.0 0.83 0.50 0 28
ST0200.01
ST0200.02
399862
399863
399864
399865
399866
399868
399869


The fact sheet was created on 20.04.2024

Questions or comments regarding the fact sheet can be emailed to:
ressursdatabaser@ngu.no
Copyright © 2024 Geological Survey of Norway