Mo i Rana (South Sámi: Måehvie / Mååfe, Ume Sámi: Muoffie, Lule
Sámi: Måvvå, Northern Sámi: Muoffi) is a town which is an
administration center in Rana municipality on Helgeland in Nordland.
From 1923 to 1964, it was a charging station and a separate urban
municipality.
The municipal council adopted city status in
1997. Mo i Rana is the fourth largest city in northern Norway, after
Tromsø, Bodø and Harstad. It is also the second largest city in
Nordland with 18,898 inhabitants as of 1 January 2020
Prehistory, Early Settlement, and Pre-Industrial Era
Archaeological evidence indicates agriculture began in the Iron Age,
with coastal settlement predating inland areas. The region supported
farming, hunting, fishing, boat-building (notably Nordlandsbåter
traditional boats), fur trading, and early mining/quarrying, including a
significant kleberstein (soapstone) quarry at Alteren on the west side
of Ranfjorden. The original Mo farm, on the site of the modern town
center, served as a focal point.
In the 1720s–1730s, priest and Sami
missionary Thomas von Westen (known as the "Apostle of the Sami")
initiated the construction of Mo Church (completed around 1724, a wooden
structure seating 400 that still stands) as part of efforts to
Christianize and missionize the local Sami population. From 1730 to
1810, a summer Sámi market operated on the church grounds, facilitating
trade in reindeer products, furs, and goods.
Permanent trade
infrastructure emerged in the 1770s. In 1860, wholesale merchant Lars
Aagaard Meyer received royal permission for landhandel (retail trade) at
Moholmen, the oldest district (with some original buildings preserved).
Trade boomed in the late 19th century, exporting fish, grouse, reindeer
meat, skins, and boats (up to ~800 shipments annually by 1880 via
Meyer's company), including routes to Sweden via paths now used for
hiking. The winter road from Mo to Umbukta was completed in 1883
(Swedish side later).
Early 20th Century: Mining Beginnings and
Urban Status
The area's iron ore deposits in the Dunderland Valley
(north of town) were known by the late 18th century. 19th-century
attempts to exploit them were limited until Swedish industrialist
Pehrsson secured land and planned a railway to Gullsmedvik harbor in Mo
i Rana. In 1901, Thomas Edison's Edison Ore Milling Syndicate purchased
rights to apply his magnetic separation patents. The Dunderland Iron Ore
Company (D.I.O.C.) formed in 1902.
Operations started in 1906 at an
open-pit mine near Ørtvann/Storforshei (~27 km north), with a dressing
plant using dry magnetic separation, briquetting, and a coal-powered
facility. The first shipment (250 tonnes of briquettes) went to England
in July 1906, but production halted in 1908 after ~87,200 tonnes due to
quality loss (high dust, reduced iron content) and environmental issues.
A wet-dressing plant at Gullsmedvik operated intermittently pre-WWII,
producing ~500,000 tonnes of high-grade concentrate.
Rana Gruber was
founded in 1937 by A/S Sydvaranger and German Vereinigte Stahlwerke AG.
In 1923, Mo separated as a ladested (market town) municipality from the
larger herred, with a population of ~1,305–1,340 (1930 census). It
gained self-governance over local services until 1964.
WWII Era
(1940–1945)
During the German invasion of Norway (Operation
Weserübung) in April–May 1940, British forces attempted to halt the
German advance toward Narvik. On May 3, 1940, an independent company
from Britain landed as part of Operation Scissors Force; a British
fighter patrolled the coast on May 1. Germans occupied the area,
operating Dunderland mines intermittently from 1941–1943. Austrian
mountain troops (Gebirgsjäger) from the 6th company passed through Mo en
route to Narvik.
Post-liberation in 1945, Operation Asfalt
(1945–1946) sought to exhume and repatriate Soviet POW graves from Mo
Church cemetery, but local protests ("Graveyard War") prevented removals
here—the only such intact Soviet POW burial site preserved in Norway.
Many WWII victims are buried at Mo Church.
Post-WWII Industrial
Boom and Population Explosion
Norway's Parliament approved the
state-owned Norsk Jernverk (Norwegian Ironworks) in 1946 to secure
domestic steel production using local iron ore, hydropower, and post-war
reconstruction needs (including Marshall Plan influences). Construction
began; the integrated steel mill at Mo i Rana produced its first steel
in 1955 after nine years of building. A cokeworks (Norsk Koksverk)
followed in 1964. The Dunderlandsbanen railway and export harbor at
Gullsmedvik supported logistics.
This triggered massive growth: Mo
town population rose from ~1,300–3,150 (1946) to ~7,000 (1955),
~8,600–9,100 (1962–1963), and the broader Rana area reached ~25,000 by
1978, with the mill employing up to 3,200–4,500 at peak. Migrants
arrived from across Norway for jobs; new housing, electricity, water,
and residential blocks were built rapidly. In 1964, Mo municipality
merged with Nord-Rana and parts of Sør-Rana to form larger Rana
Municipality (now Norway's second-largest by area).
Rana Gruber's
mining expanded: state acquisition of D.I.O.C. properties (1947), full
ownership of Rana Gruber (1951 after seizing German shares), pilot
plants (1958–1962), full-scale dressing plant at Gullsmedvik (1962–1964,
operational 1965 with wet autogenous milling, magnetic separation,
spirals, flotation). Mining moved to Ørtfjell (1983); upgrades improved
recovery. Products included iron ore concentrates, later pigments
(COLORANA® black iron oxide from 1990).
Late 20th Century
Decline, Privatization, and Restructuring
Heavy industry dominated
until the 1980s–1990s. Economic pressures led Parliament (1988) to phase
out state ownership of Norsk Jernverk; pig iron production ceased in
1988–1989. ~NOK 1 billion was allocated for transition support. The site
became Mo Industripark (industrial park) with 110–119 companies today,
employing ~1,900–3,000 in steel support, engineering, R&D, IT,
ferroalloys (Elkem, Ferroglobe), and others. Rana Gruber was privatized
(employee/board buyout 1991, later LNS majority 2008); open-pit mining
shifted to underground at Kvannevann (new levels 2012, Lean Mining
2017). Production continues with plans to 2025+.
Mo gained official
town (by) status in 1997.
Modern Era, Culture, and
Diversification
Post-industrial shift emphasized services, education
(Nord University Campus Helgeland opened 2013), state offices, tourism,
and emerging green tech (e.g., FREYR battery initiatives, though scaled
back). Cultural sites include Rana Museum ("MOment" building, 2020,
industrial focus), Nordland Theater (1979), Havmanndagene festival, and
the Havmannen ("The Man from the Sea") sculpture (1995) by Antony
Gormley in the fjord.
Coordinates: approximately 66°18′46″N 14°08′34″E (66.3128°N,
14.1428°E). The town sits at an elevation of about 26 m (85 ft)
above sea level, with the broader mapped area averaging around 178 m
(min near sea level or slightly below, max up to ~630 m in immediate
surroundings).
The city lies at the head (innermost reach) of
Ranfjorden, where the Ranelva (Rana River) empties into the fjord.
It is positioned just south of the Arctic Circle (roughly 30 km or
0.25° latitude south of 66°33'N), on the southern flank of the
Saltfjellet mountains. The town spans about 12.9 km², with suburbs
extending northward (Båsmoen, Ytteren), eastward (Selfors), and
southward (Gruben, Åga, Hauknes, Dalsgrenda). The larger Rana
Municipality covers 4,460 km² (one of Norway's largest), with most
of the ~26,000 residents in or near Mo i Rana.
The terrain is
varied: low-lying, relatively flat deltaic and valley-bottom land at
the fjord head transitions quickly to steep slopes and rugged
mountains. The Saltfjellet range dominates to the north and east,
part of the broader Scandinavian Mountains (Caledonides). The
municipality's highest point is Snøtinden at 1,589 m (5,214 ft);
other notable peaks include Bolna and Nasa. Glacial carving has
produced U-shaped valleys (e.g., Dunderland Valley, Grønnfjelldal),
fjords, and overdeepened basins.
Hydrology is dominated by
Ranfjorden, a major fjord extending westward toward the Norwegian
Sea (about 70 km from the open coast). The Ranelva river, draining a
large upland catchment, flows rapidly (its name derives from Old
Norse for "quick/rapid") into the fjord head at Mo i Rana, forming
an estuary (Engasjyen) rich in birdlife. Numerous smaller rivers,
streams, and lakes dot the lowlands and mountain valleys; the
municipality's water resources historically supported hydropower and
industry.
Glaciers and high mountains include Svartisen, Norway's
second-largest glacier complex (~370 km²), located north/northwest
of Mo i Rana, partly within the municipality and
Saltfjellet–Svartisen National Park. It features multiple outlet
tongues (e.g., Austerdalsisen, Engabreen), accessible via boat and
short hikes from areas near Mo i Rana (e.g., Svartisvatnet or
Holandsfjorden). The glacier's name means "black ice," referring to
its dark appearance under debris or from a distance.
Geologically, the area is underlain by limestone and other rocks of
the Caledonian orogeny (ancient mountain-building event), heavily
modified by repeated Quaternary glaciations that excavated fjords,
valleys, and deposited moraines. Limestone bedrock creates extensive
karst landscapes with numerous caves (e.g., Grønligrotta and
Setergrotta open to the public; Pluragrotta another notable one).
Iron ore deposits (e.g., in Dunderland Valley, ~27 km north) have
been economically important, supporting historical mining (Rana
Gruber, etc.).
Climate is classified as subarctic (Köppen Dfc,
bordering Dsc): long, cold, snowy, windy, overcast winters and
short, cool, wet, mostly cloudy summers. Annual mean temperature
~3.7°C; July daily mean ~14.8–15°C (highs average 19°C, records to
33°C); January daily mean ~-5.9°C (highs ~-3.7°C, lows to -35°C
record). Annual precipitation ~1,430 mm, highest in autumn (e.g.,
Oct 186 mm, Sep 155 mm). Heavy snowfall (peak Jan ~35 inches/90 cm
monthly equivalent), frequent blizzards. Gulf Stream influence
moderates extremes compared to inland Arctic areas, but orographic
lift from mountains increases precip. Extreme photoperiod: midnight
sun briefly (~late June–early July), very long summer days (no true
darkness mid-May–early Aug); short winter days (no full polar
night); aurora borealis frequent in clear winter nights. Winds
stronger in winter (peak ~12 mph Jan).
Vegetation and ecosystems:
Predominantly boreal (taiga) forests, especially spruce-dominated
old-growth stands in reserves like Blakkådalen. Lime-rich
(calcareous) soils in places support richer flora, including
warmer-climate species like elm (Alterhaug nature reserve). Higher
elevations transition to alpine tundra, heath, and bare rock.
Wildlife includes moose, semi-domestic reindeer, various birds (rich
in fjord estuary), fish (salmonids in Ranelva), and typical northern
mammals. Nature reserves protect old-growth forests and bird
habitats.
Human geography ties to the physical setting include
industrial development driven by local iron ore, abundant hydropower
from rivers/glaciers, and the deep-water fjord port. The E6 highway
and rail follow the Ranelva valley northward. The area's caves,
glacier, mountains, and national park support tourism and outdoor
recreation (hiking, caving, glacier walks). Allemannsretten (right
to roam) allows wide public access to the varied landscapes.