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THE ORE DATABASE
Occurence 5026 - 026 Svenskmenna
(Object Id: 4419)
(Last updated: 07.11.2023)

Location
County: Trøndelag Municipality: Holtålen (5026)
Map 1:50000: Ålen (1720-4) Map 1:250000: Røros
Coordinate system: EU89-UTM Zone 32
East: 628568 m. North: 6968942 m.
Longitude: 11.5238910 Latitude: 62.8279710
Show on map

Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Copper
Element(s): Kis Cu Zn
Importance
Raw material meaning: Not Assessed (reg. 18.02.2015)

Resources and production
Activity: Mining Reserves:
Operating method: Underground mining Historical production: 8 thousand tons


Products
Element/product Crude ore grade or quality Reg. date
Cu 1.37 % 22.11.1994
S 42.46 % 22.11.1994
Zn 1.80 % 22.11.1994

Operations
From - To Activity Comments
1870 - 1880 Pitting
1882 - 1884 Regular production Company/Institution :Os-Hommelvikselskapet
1912 - 1914 Test mining Company/Institution :Verstraete & fils
1915 - 1918 Regular production Company/Institution :A. Huitfeldt & Co.

Mineralization
Era: Paleozoic Period: Ordovician
Genesis: Sedex Form: Plate
Main texture: Porphyroblastic Min. distribution: Massive (>50 % ore minerals)
Main grain size: Very unevenly grained Main alteration: Chloritisation
Strike/Dip: 170 / 10 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Paleozoic Period: Cambrian
Province: Caledonides
Geotec.unit: Trondheim Nappe Complex
Tectonic complex: Meråkerdekket
Igneous complex:
Group: Aursund Formation: Røsjø

Mineralogy
Relationship Mineral Amount
Gangue mineral Chlorite Major mineral (>10%)
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Garnet Accessory mineral (<1%)
Ore mineral Pyrrhotite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Chalcopyrite Subordinate mineral (1-10%)
Ore mineral Magnetite Accessory mineral (<1%)
Ore mineral Sphalerite Accessory mineral (<1%)

Lithology:
Relationship Rock Origin
Host rock Klorittskifer Sedimentary
Original rock :Argillaceous sediment
Metamorphic facies :Greenschist
Wall rock Sparagmittisk sk. Sedimentary
Original rock :Greywacke
Metamorphic facies :Greenschist
Wall rock Kvartsglimmerskifer Sedimentary
Original rock :Argillaceous sediment
Metamorphic facies :Greenschist

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Host rock Primary layering Strike/Dip :220 / 20 Syn-mineralisation ;...Effect :Controls
Host rock Crenulation cleavage Post-mineralisation ;...Effect :None

Information(s) in free text format
Free text
Forekomsten ligger i en svakt skrånenede, flat elvedal med Mennaelva i vest og gruveområdet i øst. Idag finnes en stor tipp, rester av gruveutstyret og to inngjerdede sjakter (gjenrast). Området ligger rett østfor en to m høy foss i elva (ca. 100 m). Her finnes en forskifret rustsone <1 m mektig; denne er sikkert en av de få indikasjoner på malm i området. Rett ved denne fossen er det en vannfylt synk (Menna II) i tilknytning til denne rustsonen. Driften var på en <2 m mektig og py-po-cp-malm med gjennomsnittlig mektighet 1/2 - 3/4 m. Det er relativt lite malmstykker på tippen, som domineres av umineralisert klorittisk skifer. Denne bergarten viser dels krenulasjon, ellers homogen. Enkelte prøver med glinsende klorittskifer med 100 % kloritt? I tilknytning til malmen finnes bånd og slirer av klorittstykker, dels gnidd inn i malmen. 3 typer malm ble funnet ved befaringen: - Finkornet py-po-cp-malm, svakt utviklet bånding. Dels noe innblandet kvarts (matriks). Vanligste type . - Grovkornet py-po-malm med < 1 cm store porfyroblastiske py-korn og dels utviklet metamorf tekstur (durchbewegung). Smuldrer lett opp! - Semimassiv, stripet po-cp-malm, uregelmessig i kvartsrik skifer. Remobilisert cp i kvartslinser, evt. på stikk i kloritt (+ po). Malmen er også påtruffet i flere borhull rundt gruveområdet, max. 169 cm kis, ellers noe kisimpregnasjon.

Photo(s) from the Deposit area:
Photo no. 1 showing Svenkmenna gruvefelt"

Bibliography:
From NGU's Reference Archive:
Rui, Ingolf J.; Bakke, Inge , 1975
Stratabound sulphide mineralization in the Kjøli area, Røros district, Norwegian Caledonides.
;Norsk geologisk forening;TIDSSKRIFTARTIKKEL;Norsk geologisk tidsskrift; No.55 (1);51-75 pages
Abstract:
Two important sulphide ore-bearing formations have been recognized in the Cambro-Silurian succession of the Røros district. One is composed of submarine greenstones and quartz keratophyres (the Hersjø Formation). The other one, which is studied here, consists of a heterogeneous series of banded meta-argillites and meta-greywackes with subordinate thin green interlayers of probable volcanogenic origin (the Røsjø Formation). These two formations are embedded in a thick succession of various clastic sedimentary rocks which have undergone metamorphism and folding during the Silurian orogeny. The numerous sulphide deposits which occur in the Kjøli area are largely confined to the Røsjø Formation. The sulphide bodies are chiefly composed of massive pyrite and/or pyrrhotite showing variable chalcopyrite and sphalerite grades. The massive sulphides often occur as thin, extensive sheets, locally as irregular, small lenses which rarely exceed one metre in thickness. It is probable that the sulphides have been precipitated primarily on the sea-floor, but there is no clear evidence of a volcanogenic origin. Local discordant relationships between the massive sulphides and the wall rocks are ascribed to metamorphic mobilization of the sulphides. The thicker sulphide lenses may themselves represent mobilized portions of thinner sulphide-rich units.

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.

Fieldsamples
Sample No. Sample type Miscellanrous
ST0217.01 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Homogen, småfoldet (krenulasjonskløv) klorittskifer.
ST0217.02 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Skifrig klorittbergart, spesielt klorittrik, imidlertid underordnet på tippen, men typisk omv.fenomen v/malmen.
ST0217.03 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Sprøforvitret, grov py-po-malm.
ST0217.04 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Massiv po-py-cp-malm.
ST0217.05 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Uregelmessige bånd og klumper av cp-po-malm i kvarts.
ST0217.06 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Massiv, fink. py-po-mt-malm; uvanlig malmtype på tippen. Svartspettet (kvarts-mt-biotitt) i partier. Vasskisaktig.
ST0217.07 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Py-po-bånd i klorittskifer, subparallell skifrigheten.
ST0217.08 Dump
Sampler: Størseth, L.R./...Stored: Løkken
Comment: Massiv-semimassiv po-cp-malm med tynne klorittrike lag (spalteplan) og kvartskorn (begynnende metamorf tekstur).
399768 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399769 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399770 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399772 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399773 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399774 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399775 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399794 Dump
Sampler: MINDEX ASA
No. of registrated element analyses = 1
399795 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: Menna II
(Object Id: 6665 26,01,00)

Location
County: Trøndelag Municipality: Holtålen (5026)
Map 1:50000: Ålen (1720-4) Map 1:250000: Røros
Coordinate system: EU89-UTM Zone 32
East: 628418 m. North: 6968942 m.
Longitude: 11.5209500 Latitude: 62.8280240
Show on map

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


Name of Locality: Menna III
(Object Id: 6666 26,02,00)

Location
County: Trøndelag Municipality: Holtålen (5026)
Map 1:50000: Ålen (1720-4) Map 1:250000: Røros
Coordinate system: EU89-UTM Zone 32
East: 628419 m. North: 6968792 m.
Longitude: 11.5208350 Latitude: 62.8266790
Show on map

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



Analyse Results
from
Deposit Area 5026 - 026 Svenskmenna

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#
399768 Dump 10000 1364 88 220 32 3.3 47.0
399769 Dump 19000 5791 83 540 77 6.5 44.0
399770 Dump 5321 805 22 19 16 2.2 45.0
399772 Dump 12000 9707 163 398 37 7.4 1248.0
399773 Dump 8965 36000 314 214 30 9.2 113.0
399774 Dump 3224 36000 153 228 28 4.1 193.0
399775 Dump 48000 2146 94 16 23 11.8 571.0
399794 Dump 507 349900 83600 24 30 136.8 198.0
399795 Dump 3031 146900 284 39 41 14.2 193.0
------------------
Sample No. As* Cd* Ba* Mo* Sb* Bi* V* Cr* Mn*
399768 207 2.2 7 13.00 3 31 54 131 487
399769 213 27.3 2 16.00 3 108 6 110 182
399770 147 1.6 70 6.00 3 3 28 243 215
399772 394 65.6 5 16.00 3 129 11 152 118
399773 221 54.4 1 12.00 3 60 1 138 70
399774 224 82.4 4 11.00 3 38 9 118 199
399775 97 7.1 5 10.00 3 36 12 156 165
399794 51 474.4 2 13.00 35 213 3 52 785
399795 58 234.6 10 15.00 3 15 19 154 138
------------------
Sample No. Fe% Sr* La* Ti*
399768 10.00 7.0 10.00 120
399769 10.00 3.0 0.50 30
399770 7.98 7.0 7.00 180
399772 10.00 4.0 0.50 60
399773 10.00 3.0 0.50 30
399774 10.00 4.0 2.00 30
399775 10.00 3.0 1.00 120
399794 15.86 4.0 0.50 60
399795 16.37 12.0 3.00 240


The fact sheet was created on 25.04.2024

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