Site overview

Bleikvassli Gruber is a former underground zinc-lead mine situated west of Røssvatnet in Hemnes municipality, Nordland county, northern Norway. The ore deposit, a SEDEX-type stratiform massive sulphide body containing zinc, lead, copper, and silver, was first identified in 1916 or 1917. Following investigations in the late 1920s and again during and after the Second World War, trial production began in 1947 and full commercial mining in 1957.

Over approximately four decades of operation, the mine extracted more than five million tonnes of ore grading roughly four percent zinc, two percent lead, and minor copper and silver. Operations ceased in 1997 and 1998 after a combination of terrain subsidence, water ingress, and exhaustion of economically viable ore reserves brought the company to close the mine. Post-closure, heavy metal drainage from the site into the Bleikvasselva river has remained a significant environmental concern, and ground instability events have required the evacuation of nearby residents on at least one occasion.

The former mine occupies a remote valley-side setting west of Røssvatnet, where the industrial remains sit within an open northern landscape still marked by mining disturbance.

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History

The Bleikvassli ore deposit was first discovered in 1916 or 1917 — sources give slightly different dates, with the earliest ore extraction apparently taking place at that time. Formal investigation campaigns were carried out in 1928–1929 and again during the Second World War and its aftermath. A topographic and drilling plan of the site was produced by the Norges geologiske undersøkelse in 1942.

Trial mining began in 1947, and the company Bleikvassli Gruber A/S established full-scale production in 1957. The deposit is a stratiform massive sulphide body classified by geologists as SEDEX-type, hosted by Proterozoic pelitic, quartzo-feldspathic, and amphibolitic rocks of the Uppermost Allochthon of the Scandinavian Caledonides. The orebody forms two connected lenses — a southern and a northern — spanning at least 1,500 metres of strike length, dipping moderately to steeply westward and plunging to the north-east.

The operating mine developed 40 levels and approximately 25 kilometres of drifts, raises, and shafts accessed through a portal and ramp system rather than a surface headframe arrangement. At peak production in the 1980s, the mine extracted approximately 180,000 tonnes of raw ore per year. Production through to the mid-1990s is recorded at around 191,000 tonnes per year, yielding zinc and silver-bearing lead concentrates that were shipped from Andfiskå near Mo i Rana.

Total production over the operating life of the mine reached approximately five million tonnes grading 4.0 percent zinc, 2.0 percent lead, 0.15 percent copper, and 25 grams per tonne silver. In autumn 1997, significant water ingress caused by terrain subsidence and underground falls forced the suspension of regular mining operations. The company board formally resolved to close the mine in August 1998, citing the failure of extensive prospecting to locate further economic ore reserves.

Norwegian Geological Survey estimates prepared at the time of closure indicated residual resources of approximately 720,000 tonnes at elevated zinc, lead, and silver grades, though these figures were not brought to full international reporting standards. After closure, the mine site became a source of heavy metal contamination to the Bleikvasselva watercourse, with research conducted by Norsk institutt for vannforskning in 2009 recording very high concentrations of heavy metals in the upper parts of the catchment attributable primarily to drainage from the former mine area. Regulatory responsibility for remediation remained under discussion between the former operating company, Bergvesenet (the Norwegian Directorate of Mining), and environmental authorities.

In June 2013, a further ground stability incident occurred when an area of approximately seven to eight dekar outside the former mine entrance subsided by 20 to 30 centimetres overnight and a crack propagated through the terrain. Several homes in the immediate vicinity were temporarily evacuated. The mine site and its associated exploration licences were subsequently acquired by EMX Royalty Corp. and then by Norra Metals Corp. (TSX-V: NORA), which conducted technical reviews and three-dimensional geological modelling of the historic data with a view to future exploration but had not resumed mining as of the mid-2020s.

Timeline

1916–1917
Exploration

Discovery of the ore deposit

The Bleikvassli zinc-lead ore deposit was first discovered and some ore initially taken in 1916 or 1917. The deposit is a stratiform massive sulphide body (SEDEX-type) hosted in Proterozoic metamorphic rocks of the Uppermost Allochthon of the Caledonides, situated west of Røssvatnet in Hemnes municipality.
1928–1929
Exploration

First systematic investigation campaign

Norges geologiske undersøkelse and associated interests carried out investigation of the Bleikvassli deposit in 1928–1929, establishing the geological basis for later development.
1942–1946
Exploration

Wartime and post-war investigations; production plan

Further investigation of the deposit took place during and after the Second World War. A detailed topographic and drilling plan was prepared by Norges geologiske undersøkelse in 1942. Planning for production followed these investigations.
1947–1956
Construction

Trial production and mine development

Trial mining commenced in 1947. The company Bleikvassli Gruber A/S developed the underground workings through a portal and ramp system reaching 40 levels with approximately 25 kilometres of drifts, raises, and shafts. Full commercial production was reached in 1957.
1957–1997
Operation

Commercial zinc-lead mining, 1957–1997

Regular production operated from 1957. The ore body yielded zinc-lead-copper-silver massive sulphide ore; the southern and northern ore lenses together spanned over 1,500 metres of strike. Output in the 1980s ran at approximately 180,000 tonnes of raw ore per year, rising to 191,000 tonnes by 1994. Total lifetime production reached over five million tonnes grading approximately 4.0% zinc, 2.0% lead, 0.15% copper, and 25 g/t silver. Zinc concentrate and silver-bearing lead concentrate were shipped from Andfiskå near Mo i Rana.
1997
Closure

Terrain subsidence and water ingress halt operations

In autumn 1997, significant terrain subsidence and underground falls caused major water ingress into the mine workings, forcing the suspension of regular production. The dam site on Bleikvatnet was subsequently moved further into the reservoir as a precautionary measure. This event effectively ended extractive operations.
1998
Closure

Formal closure of Bleikvassli Gruber

The board of Bleikvassli Gruber A/S resolved to close the mine permanently, citing failure to locate further economic ore reserves despite extensive prospecting. The closure was formally announced in August 1998. At closure, the Norwegian Geological Survey estimated residual resources of approximately 720,000 tonnes at grades of 5.17% zinc, 2.72% lead, 0.27% copper, 45 g/t silver, and 0.2 g/t gold.
2009–2010
Heritage

Heavy metal contamination documented in Bleikvasselva

A 2009 survey by Norsk institutt for vannforskning (NIVA) recorded very high concentrations of heavy metals in the upper Bleikvasselva watercourse, attributing the primary source to drainage from the former Bleikvassli mine area. The situation highlighted unresolved regulatory responsibility for remediation between the former operator, Bergvesenet, and environmental authorities.
2013
Heritage

Ground subsidence event; residential evacuation

A terrain subsidence event occurred on 6 June 2013, with an area of approximately seven to eight dekar outside the former mine entrance sinking 20–30 centimetres overnight and a crack extending through the terrain. Three residents were evacuated from five houses adjacent to the former mine site. The area was sealed off pending geological inspection.
2018–2021
Exploration

Acquisition for exploration; geological review

Mineral rights for the former mine and surrounding area were acquired by EMX Royalty Corp. in early 2018 and subsequently transferred to Norra Metals Corp. (TSX-V: NORA). Norra conducted a comprehensive review of historic data from over 650 drill holes, constructing a three-dimensional geological model and identifying priority drill targets. Electrical power remained actively supplied to the former mine site. No mining had resumed as of the early 2020s.

Sources and records

Store norske leksikon article: Bleikvassli Gruber
Wikipedia article (English): List of mines in Norway
NRK Nordland news report: Evakuerer beboere ved nedlagt gruve (6 June 2013)
Nettavisen news report: Beboere evakuert ved nedlagt gruve i Hemnes (June 2013)
Rana Blad news report: Sterk forurensning fra nedlagt gruve (February 2010)
VG news report: Bleikvassli Gruber nedlegges (August 1998)
Mindat.org locality record: Bleikvassli Mine, Bleikvasslia, Hemnes, Nordland
Norra Metals Corp. press release: Norra Metals Prepares for Inaugural Phase I Exploration Programs (October 2020)
Ahead of the Herd (financial press): Norra Metals pursuing high-grade VMS in Norway (2020)
Rosenberg, J.L. and Spry, P.G.: Thermobarometry of the Bleikvassli Zn-Pb-(Cu) deposit, Mineralium Deposita (1998)
Skauli, H. et al.: Lead-isotope study of the sulphide ore and alteration zone, Bleikvassli, Mineralium Deposita (1992)
F.M. Vokes: Geological studies on the Caledonian pyritic zinc-lead orebody at Bleikvassli, Norges geologiske undersøkelse, 1963
NGU-rapport 98.038: Sprekkekartlegging med georadar ved Bleikvassli Gruber (1998)
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