|
|
Norsk versjon | ||||
| THE ORE DATABASE | |||||
| Deposit Area 2017 - 023 | |||||
| (Last updated 19.jan.2022) | |||||
Name of Deposit Area : Bachkes gruve |
| (Object Id : 2017,023,00,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7271700 | Latitude: | 70.4057880 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602042 m. | Y-coord: | 7813415 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu Fe U |
| Production |
| Activity: | Mining | Reserves: | 19 thousand tons | |
| Prod. method: | Underground mining | Production: | 11 thousand tons | |
| Prod. status: | Disused, closed | Volume of dump: | 1000 m3 |
| Importance |
| Public: | Little Importance (reg. 18.02.2015) |
| Economical: | Minor interest , (Confirmed 03.feb.2005 by Peter Ihlen) |
Products |
| Element/product | Crude ore grade or quality | |
| CU | 1.95 % |
Operations |
| From - To | Activity | Comments | |
| 1900 - 1903 | Regular production | Company/Institution :Vesterdalens Grubeselskap | |
| 1903 - 1903 | Regular production | Company/Institution :Kaafjord Kobberverk | |
| 1904 - 1906 | Regular production | Company/Institution :Vesterdalen Kobbergruver | |
| 1926 - 1927 | Core drilling | Company/Institution :A/S Porsa Kobbergruver | |
| 1928 - 1928 | Test mining | Company/Institution :A/S Porsa Kobbergruver | |
| 1929 - 1931 | Regular production | Company/Institution :A/S Porsa Kobbergruver |
Mineralization |
| Era: | Proterozoic | Period: | Paleoproterozoic | |
| Dating: | 0 million year | Method: | ||
| Genesis: | Hydrothermal vein | Form: | Plate | |
| Main texture: | Porphyroblastic | Min. distribution: | Irregular (scattered) |
| Main grain size: | Very unevenly grained | Main alteration: | No country rock alteration |
| Strike/Dip: | 140 / 80 | Direction: | ||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Proterozoic | Period: | Paleoproterozoic |
| Province: | Caledonian Basement Province | |
| Geotec.unit: | Komagfjord-Repparfjord Greenstone Belt | |
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Nussir | Formation: | Svartfjell |
Mineralogy |
| Relationship | Mineral | Amount | |
| Gangue mineral | Quartz | Major mineral (>10%) | |
| Gangue mineral | Calcite | Major mineral (>10%) | |
| Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
| Gangue mineral | Hornblende | Subordinate mineral (1-10%) | |
| Gangue mineral | Muscovite | Subordinate mineral (1-10%) | |
| Gangue mineral | Feldspar | Subordinate mineral (1-10%) | |
| Ore mineral | Chalcopyrite | Major mineral (>10%) | |
| Ore mineral | Pyrite | Major mineral (>10%) | |
| Ore mineral | Hematite | Subordinate mineral (1-10%) | |
| Ore mineral | Magnetite | Subordinate mineral (1-10%) | |
| Ore mineral | Uraninite | Accessory mineral (<1%) |
Lithology: |
| Relationship | Rock | Origin | |
| Host rock | Grønnstein | Extrusive Original rock :Basalt |
|
| Metamorphic facies :Greenschist |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Wall rock | Joints/Fractures | Strike/Dip :330 / 90 | Pre-mineralisation ;...Effect :Controls |
Information(s) in free text format |
| Free text |
| The Bachke deposit was discovered in 1900 and mining was carried out periodically by several companies until 1931. Mining exploited four parallel quartz-carbonate veins that are up to 100 m long and 1–1.5 m thick. The veins are hosted by greenstones of the Nussir Group and have a NW strike and a variable but generally steep dip. The main sulphide minerals are chalcopyrite and pyrite, and magnetite and haematite occur in subordinate amounts. Uraninite is an accessory mineral in crosscutting veinlets. The vein matrix is composed of quartz, calcite, albite, chlorite and wall rock fragments. |
Bibliography: |
| From NGU's Reference Archive: |
| Geis, H.P. , 1967 |
| Porsa Grube Kvalsund, Finnmark. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 6618;1 pages |
| Abstract: | |
| Rapporten konkluderer med at man anser A/S Porsa konsesjonsområde ikke drivverdig, - og Elkem - Spigerverket lar konsesjonen tilfalle Staten. Kartbilagene viser geologisk kartlegging med prøvetakingsprofiler i det mineraliserte feltet. Forekomstnr. forts.: 50076-84 og 50397. Forekomstens koordinater forts.: 35 6131 78251. |
| Kvalheim, A. , 1942 |
| Kort geologisk oversikt over Porsa gruvedistrikt. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 302;11 pages |
| Abstract: | |
| Lok. Nr. 50067-68, 50076-84, 50397. Rapporten gir en geologisk oversikt over Porsafeltet. Deretter beskrives de viktigste malmforekomstene. De er kvarts-karbonat ganger med kobberkis som med et unntak opptrer i grønnstein. En mineralisert gang finnes også i en skiferhorisont. Kjemisk analyse av malm, kobberkonsentrat og flotasjonsavgang er presentert. Gruvedriften ble avsluttet i 1929. |
| Krause, Michael , 1980 |
| Some uranium mineralizations in the Raipas Suite of the Komagfjord tectonic window, Finnmark, Norway. |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.355;49-52 pages |
| Abstract: | |
| Uranium mineralizations have been discovered in the northwest part of the Komagfjord tectonic window. The mineralizations are found in two mines of the old Porsa-Neverfjord copper mining district. Pitchblende and brannerite occur as primary minerals. Black slates are considered to be the source rocks of the uranium-bearing fluids. |
| Kvalheim, A. , 1928 |
| Rapport over Bachkes grube pr. 29/8-1928. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 304;8 pages |
| Abstract: | |
| Lok. Nr. 50067-68, 50076-84, 50397. Bergfangsten i Bachkes gruve i perioden 1900-1906 er beregnet å være ca. 13500 t hvorav av ca. 10000 t var malm. Vurderinger av gjenstående malm i Bachkes gruve, Puntervolds gang og Schutz gruve er gjort. Mineraliseringene i Bachkes gruve antaes å ha økonomisk intresse. Videre undersøkelser anbefales i alle tre gruver. |
| Kvalheim, A. , 1927 |
| Oversikt over diamantborhullene ved Bachke Grube. |
| ;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 305;6 pages |
| Abstract: | |
| Lok. Nr. 50067-68, 50076-84, 50397. Utbredelsen av malmen i Bachkes gruve er undersøkt med tre diamantborhull. Foreløpig er den beregnet å være minst 140 m lang og går ned til et dyp av minst 100 m. Boringene fortsetter i Schutz gruve. |
| Reitan, Paul H. , 1963 |
| The geology of the Komagfjord tectonic window of the Raipas suite, Finnmark, Norway. |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.221;1-71 + kar pages |
| Abstract: | |
| The report is based on four summers (1956-59) of field work in an area of approximately 860 km2. The area is located in western Finnmark, northern Norway, between 70 degrees 10' and 70 degrees 31' N latitude and 12 degrees 40' and 13 degrees 50' E Oslo longitude. The purpose of the investigation was to study the rocks within a hitherto mainly unexamined area of Precambrian rocks surrounded by Caledonian rocks. Portions of the area near the sea had been visited by a few geologists prior to the initiation of this investigation. It was therefor quite certain that the rocks were Precambrian in age and constituted a window in the Caledonides, but the size of the window was unknown nor had most of the window been studied geologically. This report establishes the Precambrian age of the rocks and delineates the boundaries of the window. The Precambrian rocks along the western coast of Finnmark were previously called the Raipas formation and known to outcrop in (at least) two windows. As this report differentiates seven formations which constitute two groups whithin the Komagfjord (the northernmost) tectonic window, it is purposed that the Precambrian rocks of the two windows be known as the Raipas suite. |
| Torgersen, J.C. , 1931 |
| Rapport som omhandler Porsa Gruber. |
| ;Norges geologiske undersøkelse;TEKNISK RAPPORT;Bergarkivet; No.BA 3827;12 pages |
| Abstract: | |
| Rapporten gjør opp status for gruvedriften inntil rapportdato. For året 1930 har driften gått med stort underskudd. Regnskap over utgifter og inntekter dette år gis. Det fremsettes forslag til tekniske forbedringer for å øke lønnsomheten. samt undersøkelsesarbeider for å finne rikere malm. Forfatter er bergmesteren i Finnmark, og rapporten er skrevet til gruveselskapet A/S Porsa. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||||
| FI0132.82-2 | Dump |
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| FI0132.82-4 | Dump |
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| FI0132.82-5 | Dump |
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| FI0132.82-6 | Dump |
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| FI0132.82-7 | Dump |
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| FI0132.82-8 | Dump |
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| FI0132.82-9 | Dump |
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| HA-P-012 | Bedrock |
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| HA-P-013 | Bedrock |
|
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| HA-P-014 | Bedrock |
|
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| HA-P-015 | Bedrock |
|
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| 82-1 | Dump |
|
| NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Kvalsundstollen |
| (Object Id : 2017,023,01,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7295950 | Latitude: | 70.4045220 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602140 m. | Y-coord: | 7813278 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Mining | Reserves: | ||
| Prod. method: | Underground mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||||
| HA-P-011 | Bedrock |
|
| NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Puntervolds gruve |
| (Object Id : 2017,023,02,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7285690 | Latitude: | 70.4048520 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602099 m. | Y-coord: | 7813313 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Mining | Reserves: | ||
| Prod. method: | Underground mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
Name of Locality : Lunds synk |
| (Object Id : 2017,023,03,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7248600 | Latitude: | 70.4061480 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 601954 m. | Y-coord: | 7813451 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Mining | Reserves: | ||
| Prod. method: | Underground mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
Name of Locality : Schutz gruve |
| (Object Id : 2017,023,04,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7288670 | Latitude: | 70.4066780 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602101 m. | Y-coord: | 7813517 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Mining | Reserves: | ||
| Prod. method: | Underground mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
Name of Locality : Skjerp 5 |
| (Object Id : 2017,023,05,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7381970 | Latitude: | 70.4118690 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602424 m. | Y-coord: | 7814111 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Pitting | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: |
Name of Locality : Hans gruve |
| (Object Id : 2017,023,06,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7262710 | Latitude: | 70.4130620 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 601973 m. | Y-coord: | 7814224 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Pitting | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: |
Information(s) in free text format |
| Free text |
| Forekomsten ligger på østsida av elva i Vesterdalen, ca. 240 m rett øst for Malakittskjerpene. Den består av en 1,2 m bred og 1,5 m høy stoll som minst er 20 m lang. Retningen på stollen er 170°. Kobbermalmen finnes i en minst 10 cm bred karbonatgang som ligger i grønnstein. Gangen fører hyppig linser/slirer av sidesteinen og det er skarp kontakt til denne. Kobberkis opptrer som aggregater i karbonat og i strenger/årer langs kontakten mellom karbonatgangen og grønnsteinen. Grønnsteinen er finkornet, mørk grønn og magnetittførende. En tipp med volum ca. 50 m3 ligger nedover lia. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||
| HA-P-018 | Bedrock |
|
|||
| HA-P-019 | Bedrock |
|
| NB! All analyse values are shown at the end of the printout.: |
Name of Locality : Hallingstad gruve |
| (Object Id : 2017,023,07,00) |
| Location |
| County : | Finnmark (20) | Municipality : | Kvalsund (2017) |
| Map 1:50000: | Vargsund (1935-4) | Map 1:250000: | Hammerfest |
| Marking point: | Longitude: | 23.7295780 | Latitude: | 70.4131920 |
| EU89-UTM Zone 34 | (Coordinates IS confirmed) |
| X-coord: | 602095 m. | Y-coord: | 7814244 m. |
|
|
| Commodity |
| Main Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Sub Type: | Copper | |
| Element(s): | Cu |
| Production |
| Activity: | Pitting | Reserves: | ||
| Prod. method: | Production: | |||
| Prod. status: | Volume of dump: |
Information(s) in free text format |
| Free text |
| Forekomsten ligger på østsida av elva i Vesterdalen, ca. 120 m rett øst for Hans gruve. Den består av en 15 m lang dagskjæring som er opptil 6-7 m høy. Skjæringa ender i sør i et mindre, uregelmessig tverrslag. Kobberkis finnes på flere subparallelle, tilnærmet vertikale karbonatårer som er 1-10 cm brede. Det er trolig flere faser med avsetning av fin- til grovkornet karbonat i årene. Den siste i korte ekstensjonsårer/-linser. Kobberkis danner aggregater og er disseminert i årene. Sidesteinen er mørk grønnstein som i Hans gruve. En tipp med volum ca. 50 m3 ligger nedover lia. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||
| HA-P-020 | Bedrock |
|
|||
| HA-P-021 | Bedrock |
|
| NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
| from |
| Deposit Area 2017 - 023 Bachkes gruve |
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# |
| FI0132.82-2 | Dump | 62304 | 1 | 6 | 575 | 8 | 2.5 | 159.0 |
| FI0132.82-4 | Dump | 2695 | 9 | 28 | 23 | 6 | .1 | 30.0 |
| FI0132.82-5 | Dump | 75886 | 1 | 2 | 147 | 12 | 3.1 | 365.0 |
| FI0132.82-6 | Dump | 1083 | 17 | 3 | 17 | 24 | .1 | 15.0 |
| FI0132.82-7 | Dump | 11140 | 1 | 4 | 20 | 14 | 1.0 | 56.0 |
| FI0132.82-8 | Dump | 100 | 28 | 4 | 26 | 36 | .1 | 7.0 |
| FI0132.82-9 | Dump | 165 | 24 | 2 | 15 | 31 | .1 | 4.0 |
| HA-P-011 | Bedrock | 15948 | 61 | 4 | 374 | 39 | 1.1 | 116.0 |
| HA-P-012 | Bedrock | 721 | 2 | 6 | 10 | 4 | .4 | 1.0 |
| HA-P-013 | Bedrock | 17808 | 44 | 2 | 931 | 50 | .9 | 79.0 |
| HA-P-014 | Bedrock | 25456 | 65 | 2 | 72 | 9 | 1.0 | 204.0 |
| HA-P-015 | Bedrock | 37356 | 90 | 4 | 154 | 13 | 1.2 | 210.0 |
| HA-P-018 | Bedrock | 17412 | 43 | 8 | 17 | 27 | .4 | 228.0 |
| HA-P-019 | Bedrock | 19212 | 41 | 2 | 11 | 8 | .8 | 327.0 |
| HA-P-020 | Bedrock | 62195 | 172 | 2 | 34 | 66 | 1.2 | 557.0 |
| HA-P-021 | Bedrock | 41805 | 99 | 2 | 28 | 24 | .8 | 231.0 |
| 82-1 | Dump | 543 | 67 | 3 | 56 | 52 | .1 | 7.0 |
| ------------------ |
| Sample No. | Pt# | Pd# | Rh# | As* | Cd* | Ba* | Mo* | Sb* | Bi* |
| FI0132.82-2 | 2.0 | 7.0 | 2.0 | 12 | 1.0 | 14 | 17.00 | 2 | 24 |
| FI0132.82-4 | 9.0 | 8.0 | 2.0 | 3 | 1.0 | 34 | 88.00 | 2 | 2 |
| FI0132.82-5 | 2.0 | 2.0 | 2.0 | 7 | 3.0 | 9 | 3.00 | 2 | 14 |
| FI0132.82-6 | 6.0 | 10.0 | 2.0 | 2 | 1.0 | 33 | 10.00 | 2 | 2 |
| FI0132.82-7 | 10.0 | 14.0 | 2.0 | 2 | 1.0 | 14 | 7.00 | 2 | 2 |
| FI0132.82-8 | 14.0 | 17.0 | 2.0 | 3 | 1.0 | 50 | 1.00 | 2 | 2 |
| FI0132.82-9 | 6.0 | 15.0 | 2.0 | 2 | 1.0 | 70 | 1.00 | 2 | 2 |
| HA-P-011 | 8.0 | 9.0 | 1.0 | 5 | 2.2 | 20 | 1.00 | 2 | 2 |
| HA-P-012 | 2.0 | 1.0 | 1.0 | 2 | .7 | 7 | 1.00 | 2 | 3 |
| HA-P-013 | 14.0 | 34.0 | 1.0 | 41 | 1.9 | 11 | 1.00 | 2 | 2 |
| HA-P-014 | 3.0 | 5.0 | 1.0 | 3 | 2.2 | 5 | 1.00 | 2 | 4 |
| HA-P-015 | 1.0 | 3.0 | 1.0 | 7 | 3.2 | 9 | 17.00 | 2 | 23 |
| HA-P-018 | 2.0 | 1.0 | 1.0 | 3 | 1.2 | 15 | 11.00 | 2 | 6 |
| HA-P-019 | 1.0 | 1.0 | 1.0 | 3 | 1.7 | 18 | 1.00 | 2 | 7 |
| HA-P-020 | 6.0 | 8.0 | 1.0 | 3 | 5.8 | 28 | 44.00 | 2 | 2 |
| HA-P-021 | 3.0 | 29.0 | 1.0 | 2 | 3.7 | 21 | 7.00 | 2 | 21 |
| 82-1 | 11.0 | 19.0 | 2.0 | 3 | 2.0 | 138 | 1.00 | 2 | 2 |
| ------------------ |
| Sample No. | S% | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* |
| FI0132.82-2 | 8.89 | 10 | 1 | 514 | 8.70 | 2.00 | 9.00 | 1 | 26.0 |
| FI0132.82-4 | .29 | 76 | 19 | 528 | 7.52 | 4.00 | 90.00 | 1 | 23.0 |
| FI0132.82-5 | 9.68 | 36 | 1 | 1354 | 14.81 | 3.00 | 5.00 | 1 | 43.0 |
| FI0132.82-6 | .11 | 100 | 32 | 493 | 5.60 | 1.00 | 5.00 | 1 | 18.0 |
| FI0132.82-7 | .29 | 113 | 34 | 149 | 9.26 | 1.00 | 5.00 | 1 | 4.0 |
| FI0132.82-8 | .02 | 114 | 54 | 346 | 4.26 | 1.00 | 5.00 | 2 | 3.0 |
| FI0132.82-9 | .02 | 155 | 58 | 237 | 8.00 | 1.00 | 5.00 | 1 | 2.0 |
| HA-P-011 | 6.22 | 111 | 63 | 366 | 19.62 | 1.00 | 5.00 | 1 | 4.0 |
| HA-P-012 | .12 | 97 | 9 | 1088 | 14.16 | 1.00 | 9.00 | 1 | 36.0 |
| HA-P-013 | 11.23 | 101 | 69 | 335 | 21.22 | 1.00 | 5.00 | 1 | 10.0 |
| HA-P-014 | 5.16 | 83 | 13 | 2175 | 14.94 | 1.00 | 6.00 | 1 | 69.0 |
| HA-P-015 | 5.46 | 31 | 12 | 1134 | 8.17 | 1.00 | 7.00 | 1 | 41.0 |
| HA-P-018 | 3.11 | 21 | 31 | 1816 | 3.87 | 1.00 | 5.00 | 1 | 237.0 |
| HA-P-019 | 2.58 | 4 | 17 | 3515 | 3.95 | 1.00 | 5.00 | 1 | 132.0 |
| HA-P-020 | 10.02 | 108 | 63 | 708 | 10.35 | 1.00 | 5.00 | 3 | 54.0 |
| HA-P-021 | 7.26 | 31 | 24 | 1841 | 6.15 | 1.00 | 5.00 | 1 | 172.0 |
| 82-1 | .05 | 228 | 70 | 528 | 13.10 | 3.00 | 26.00 | 1 | 11.0 |
| ------------------ |
| Sample No. | La* | B* | Na* | Mg* | Al* | P* | K * | Ca* | Ti* |
| FI0132.82-2 | 2.00 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 |
| FI0132.82-4 | 4.00 | 2 | 0 | 1 | 1 | 0 | 1 | 4 | 0 |
| FI0132.82-5 | 2.00 | 2 | 0 | 0 | 0 | 0 | 0 | 10 | 0 |
| FI0132.82-6 | 2.00 | 2 | 0 | 1 | 1 | 0 | 1 | 3 | 0 |
| FI0132.82-7 | 4.00 | 2 | 0 | 0 | 1 | 0 | 0 | 1 | 0 |
| FI0132.82-8 | 2.00 | 2 | 0 | 2 | 2 | 0 | 1 | 1 | 1 |
| FI0132.82-9 | 2.00 | 2 | 0 | 1 | 1 | 0 | 1 | 1 | 0 |
| HA-P-011 | 2.00 | 2 | 0 | 1 | 1 | 0 | 1 | 0 | 0 |
| HA-P-012 | 3.00 | 2 | 0 | 0 | 0 | 0 | 0 | 9 | 0 |
| HA-P-013 | 3.00 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 |
| HA-P-014 | 2.00 | 2 | 0 | 0 | 0 | 0 | 0 | 17 | 0 |
| HA-P-015 | 2.00 | 2 | 0 | 0 | 0 | 0 | 0 | 12 | 0 |
| HA-P-018 | 5.00 | 2 | 0 | 1 | 1 | 0 | 0 | 20 | 0 |
| HA-P-019 | 3.00 | 2 | 0 | 3 | 0 | 0 | 0 | 23 | 0 |
| HA-P-020 | 13.00 | 2 | 0 | 1 | 1 | 0 | 1 | 6 | 0 |
| HA-P-021 | 10.00 | 2 | 0 | 1 | 0 | 0 | 0 | 19 | 0 |
| 82-1 | 2.00 | 2 | 0 | 3 | 4 | 0 | 3 | 0 | 0 |
| The fact sheet was created on 19.04.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |