Norsk versjon | |||||
THE ORE DATABASE | |||||
Occurence 919 - 012 Bøylestad | |||||
(Object Id: 0919,012,00,00) (Last updated: 15.03.2024) |
Drill Cores: Bøylestad |
|
Location |
County: | Aust-Agder (09) | Municipality: | Froland (0919) |
Map 1:50000: | Nelaug (1612-3) | Map 1:250000: | Arendal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 482929 m. | North: | 6492539 m. |
Longitude: | 8.7065090 | Latitude: | 58.5729620 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis Co |
Importance |
Raw material meaning: | Not Assessed (reg. 20.03.2017) |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Open pit and underground mining | Historical production: | 6 thousand tons |
Products |
Element/product | Crude ore grade or quality | Reg. date | |
Cu | 0.9 % | 15.03.2024 | |
Zn | 1.7 % | 15.03.2024 |
Operations |
From - To | Activity | Comments | |
1866 - 1882 | Regular production | Company/Institution :Bøilestad kobberverk | |
I følge produksjonsstatistikk (Ba 3681). Andre kilder angir drift i 70 år. | |||
1983 - 1983 | Geology | Company/Institution :ARCO Norway, Inc. | |
2000 - 2000 | Sampling | Company/Institution :NGU |
Mineralization |
Era: | Proterozoic | Period: | Mesoproterozoic | |
Genesis: | Volcex | Form: | Plate | |
Main texture: | Structureless | Min. distribution: | Massive (>50 % ore minerals) |
Main grain size: | Medium grained (1-3 mm) | Main alteration: | Silicification |
Strike/Dip: | 28 / 70 | Direction: | ||
Plunge: |
Stratigraphic classification of host rock |
Era: | Proterozoic | Period: | Mesoproterozoic |
Province: | South Norwegian Basement Province | |
Geotec.unit: | Bamble Complex | |
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Calcite | Subordinate mineral (1-10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Gangue mineral | Garnet | Accessory mineral (<1%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :15 / 65 | Post-mineralisation ;...Effect :Modifies | |
Wall rock | Schistosity | Strike/Dip :16 / 60 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Mining in the Bøylestad area consists of several minor pits and, and the 1-3 m thick ore has been exploited to a depth of 120 m. At least 6000 tonnes has been mined over a period of 70 years in the 19th century. The massive ore is located within altered amphibolite and comprises massive pyrrhotite and sphalerite and veinlets of chalcopyrite and pyrrhotite. |
Photo(s) from the Deposit area: |
|
Bibliography: |
From NGU's Reference Archive: |
Bech, Lone , 1984 |
Detailed geological mapping of the Skyttemyr-Bøylestad ore and ist host-rock package, Bamble section, 1983. |
;ARCO Norway;RAPPORT;Report; No.84-230-20;22 s. + v pages |
Abstract: | |
The formerly mined Skyttemyr-Bøylestad ore is situated in the Froland district of the Bamble belt, Norway. The ore is a 2.5 km long horizon with Au-bearing, massive pyrrhotite-chalcopyrite-bodies, centrally located in the at least 15 km long north-east-striking Skyttemyr sulfide zone. This zone marks the border between a thick "normal" volcanic-sedimentary package to the east. Alternating biotite-quartz gneiss, garnet amphibolite, sillimmanite gneiss, quartzites, calc-silicates, carbonates, albitites and sulfide-bearing or rusty units constitute the last mentioned. The Skyttemyr sone is the most Au and sulfide-rich zone in the Al-rich package. East of this only traces of sulfide are found. Highest Au-values (max. = 2.94 ppm) are clearly confined to the central-most Cu-rich massive ore at Skyttemyr, and the Au-content decreases to trace values 1 km north and south of this location. Zn seems partly to show a reverse behaviour. [...] |
Froland copper property, Norway. |
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 4156;5 pages |
Abstract: | |
Forekomsten omfatter Skytmyr, Boilestad og Sletne gruver sammen med flere skjerp. Malmsonen er omgitt av gneiser og kan følges opptil 3,2 km. Mineraliseringen er svovel og magnetkis med noe kobber. Det blir gitt en beskrivelse av gruvene og skjerpene mellom dem, hvor det tilslutt er behandlet gruvenes økonomi. |
, 1885 (?) |
Bøilestad, Skytmyr. |
;Norges geologiske undersøkelse;TEKNISK RAPPORT;Bergarkivet; No.BA 3681;5 pages |
Abstract: | |
Oversikt / tall for drift 1866-1885. Rapporten som er håndskrevet, gir gruvetekniske opplysninger. |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
AA0159.04 | Dump |
|
||||
AA0159.05 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Midtre Bøylestad |
(Object Id: 0919,012,01,00) |
|
Location |
County: | Aust-Agder (09) | Municipality: | Froland (0919) |
Map 1:50000: | Nelaug (1612-3) | Map 1:250000: | Arendal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 482909 m. | North: | 6492539 m. |
Longitude: | 8.7061650 | Latitude: | 58.5729610 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis |
Resources and production |
Activity: | Mining | Reserves: | ||
Operating method: | Open pit and underground mining | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Gangue mineral | Sillimanite | Accessory mineral (<1%) | |
Gangue mineral | Garnet | Accessory mineral (<1%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :6 / 55 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Det midtre dagbruddet har retning 12º og ligger 80 m sør for dobbelsjaktene i hovedbruddet. Det er et 35 m langt, opptil 6 m dypt og 1,5-2 m bredt dagbrudd med en vannfylt sjakt midt i og en mindre stoll i sørenden. En liten skråsjakt fører ned til denne stollen fra sørvest. Massiv malm er ikke blottet i bruddet, kun svak disseminasjon av magnetkis og dels kobberkis opptrer i veggene som består av dels silisifisert og biotittisert amfibolitt med foliasjon 6º/55º. Sidebergartene er dermed de samme som i hovedbruddet. Enkelte kvarts- og pegmatittslirer finnes også. Ved skråsjakta finnes en 40 cm bred sone med kraftig disseminasjon og mange årer/strenger av sulfider; i hovedsak magnetkis og kobberkis (prøve .02). Bergartene svinger der mer sørvest og malmsona har retning 50º/80º. Videre sørover stryker bergartene mer nord-sør igjen. Semi-massiv magnetkis+sinblende breksjetype malm med kvartsøyne og bergartsfragmenter er tatt fra mineraliserte blokker i nordenden av bruddet (.03). |
Photo(s) from the Deposit area: |
|
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
AA0159.02 | Bedrock |
|
||||
AA0159.03 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Søndre Bøylestad |
(Object Id: 0919,012,02,00) |
|
Location |
County: | Aust-Agder (09) | Municipality: | Froland (0919) |
Map 1:50000: | Nelaug (1612-3) | Map 1:250000: | Arendal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 482889 m. | North: | 6492409 m. |
Longitude: | 8.7058310 | Latitude: | 58.5717930 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Biotite | Subordinate mineral (1-10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Biotite gneis | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :14 / 45 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Det sørligste bruddet har retning 8º og ligger lengst sør i hogstfeltet. Det er 12 m langt, 2-3 m bredt og opptil 3 m dypt, og er dels gjenrast og gjengrodd. Kraftig forvitra og skifrig biotittgneis i heng har foliasjon 14º/45º. En tipphaug sørøst for åpningen inneholder de samme bergartene og mineraliseringstypene som ved bruddene i nord. I tillegg finnes magnetkis-kobberkis aggregater/strenger i grovkornet, kvarts-feltspat pegmatitt (prøve .01). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
AA0159.01 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Sletne sør |
(Object Id: 0919,012,03,00) |
|
Location |
County: | Aust-Agder (09) | Municipality: | Froland (0919) |
Map 1:50000: | Nelaug (1612-3) | Map 1:250000: | Arendal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 482699 m. | North: | 6491770 m. |
Longitude: | 8.7026130 | Latitude: | 58.5660380 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis |
Resources and production |
Activity: | Test mining | Reserves: | ||
Operating method: | Underground mining | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Gangue mineral | Chlorite | Subordinate mineral (1-10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Information(s) in free text format |
Free text |
Forekomsten består av en loddsjakt med 2,5 x 4 m lange vegger omgitt av en 0,5 m bred og høy ringmur. Ned til vannspeilet er det 1,5 m. En tipp på 120 m³ viser at sjakta er relativt dyp. To mindre grunne gjengrodde groper finnes mellom denne sjakta og Sletne nord som ligger 80 m lengre nord. Pga. de glatte veggene er det ikke mulig å få noe inntrykk av mineraliseringen i sjakta. Amfibolitt, dels silifisert og med disseminasjon av sulfider dominerer i ringmuren. Semi-massiv magnetkis-sinkblende malm med spor av kobberkis i en kvarts-amfibolrik grunnmasse finnes også (prøve .07). |
Photo(s) from the Deposit area: |
|
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
AA0159.07 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Name of Locality: Sletne nord |
(Object Id: 0919,012,04,00) |
|
Location |
County: | Aust-Agder (09) | Municipality: | Froland (0919) |
Map 1:50000: | Nelaug (1612-3) | Map 1:250000: | Arendal |
Coordinate system: | EU89-UTM Zone 32 |
East: | 482740 m. | North: | 6491850 m. |
Longitude: | 8.7032950 | Latitude: | 58.5667580 |
Show on map |
|
Resource |
Resource Type: | Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) | Resource Subtype: | Copper | |
Element(s): | Cu Zn Kis |
Resources and production |
Activity: | Pitting | Reserves: | ||
Operating method: | Historical production: |
Mineralogy |
Relationship | Mineral | Amount | |
Gangue mineral | Feldspar | Major mineral (>10%) | |
Gangue mineral | Quartz | Major mineral (>10%) | |
Gangue mineral | Amphibole | Major mineral (>10%) | |
Ore mineral | Pyrrhotite | Major mineral (>10%) | |
Ore mineral | Sphalerite | Major mineral (>10%) | |
Ore mineral | Chalcopyrite | Major mineral (>10%) | |
Ore mineral | Pyrite | Subordinate mineral (1-10%) |
Lithology: |
Relationship | Rock | Origin | |
Wall rock | Altered amphibolite | Extrusive Original rock :Basalt |
|
Metamorphic facies :Amphibolite |
Structures |
Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
Wall rock | Foliation | Strike/Dip :14 / 55 | Post-mineralisation ;...Effect :Modifies |
Information(s) in free text format |
Free text |
Dette er en 9 m lang, 1-2 m bred og opptil 2 m høy vannfylt, dagskjæring med retning 16º. Den er omgitt av en ringmur og i tillegg finnes en tipp på 60 m³. Kvartsrik glimmergneis med foliasjon 14º/55º er blottet i heng, mens svakt sulfiddisseminert amfibolitt finnes i ligg. Malmsona er ikke blottet. I ringmuren og på tipp finnes massiv magnetkis-sinkblende med spor av kobberkis, mens strenger/aggregater med kobberkis-magnetkis i tilknytning til kvartslinser i amfibolitten er mest vanlig (prøve .06). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | ||||
AA0159.06 | Dump |
|
NB! All analyse values are shown at the end of the printout.: |
Analyse Results |
from |
Deposit Area 919 - 012 Bøylestad |
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# |
AA0159.01 | Dump | 13443 | 4579 | 26 | 258 | 236 | 8.5 | 286.0 |
AA0159.02 | Bedrock | 11438 | 1412 | 81 | 39 | 30 | 5.8 | 70.0 |
AA0159.03 | Dump | 7142 | 17403 | 72 | 343 | 243 | 2.7 | 49.0 |
AA0159.04 | Dump | 952 | 43923 | 32 | 326 | 416 | 1.3 | 21.0 |
AA0159.05 | Dump | 22210 | 5253 | 465 | 90 | 114 | 25.1 | 1986.0 |
AA0159.06 | Dump | 2914 | 160 | 19 | 119 | 292 | 1.8 | 1.0 |
AA0159.07 | Dump | 2386 | 45578 | 413 | 242 | 496 | 2.3 | 11.0 |
------------------ |
Sample No. | Pt# | Pd# | As* | Cd* | Ba* | Mo* | Sb* | Bi* | S% |
AA0159.01 | 4.0 | 14.0 | 346 | 25.8 | 13 | 7.00 | 2 | 35 | 16.10 |
AA0159.02 | 1.0 | 4.0 | 49 | 5.0 | 135 | 4.00 | 5 | 17 | 2.25 |
AA0159.03 | 7.0 | 2.0 | 699 | 56.8 | 81 | 2.00 | 2 | 13 | 17.70 |
AA0159.04 | 1.0 | 1.0 | 27 | 147.1 | 24 | 2.00 | 2 | 2 | 26.30 |
AA0159.05 | 4.0 | 10.0 | 107 | 17.8 | 27 | 3.00 | 2 | 38 | 7.54 |
AA0159.06 | 1.0 | 2.0 | 742 | .9 | 2 | 4.00 | 2 | 4 | 8.19 |
AA0159.07 | 1.0 | 15.0 | 169 | 307.9 | 9 | 4.00 | 2 | 5 | 14.50 |
------------------ |
Sample No. | V* | Cr* | Mn* | Fe% | Th* | U* | W* | Sr* | La* |
AA0159.01 | 13 | 34 | 249 | 23.01 | 1.00 | 10.00 | 1 | 8.0 | 1.00 |
AA0159.02 | 181 | 168 | 616 | 7.47 | 4.00 | 9.00 | 1 | 12.0 | 9.00 |
AA0159.03 | 100 | 132 | 408 | 28.86 | 1.00 | 4.00 | 1 | 9.0 | 5.00 |
AA0159.04 | 9 | 24 | 158 | 35.38 | 1.00 | 4.00 | 1 | 9.0 | 2.00 |
AA0159.05 | 81 | 180 | 420 | 12.09 | 1.00 | 13.00 | 1 | 15.0 | 2.00 |
AA0159.06 | 12 | 40 | 106 | 14.01 | 1.00 | 4.00 | 12 | 1.0 | 1.00 |
AA0159.07 | 91 | 198 | 895 | 31.58 | 1.00 | 4.00 | 1 | 1.0 | 6.00 |
------------------ |
Sample No. | B* | ||||||||
AA0159.01 | 2 | ||||||||
AA0159.02 | 4 | ||||||||
AA0159.03 | 2 | ||||||||
AA0159.04 | 2 | ||||||||
AA0159.05 | 2 | ||||||||
AA0159.06 | 2 | ||||||||
AA0159.07 | 4 |
The fact sheet was created on 01.11.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
Copyright © 2024 Geological Survey of Norway |