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Theme Magazines and Fact Sheets
Download "Geology and Ore no. 11, February 2008" go11.pdf (~7.5 mb)
No. 11 - February 2008
The Nalunaq
Gold Mine
'Nalunaq' the Greenlandic name of
Greenland's first gold mine means the
place that is hard tOFind. It is located
in Kirkespirdalen (Church steeple val-
ley) near the town of Nanortalik.
Since the 1970s a number of signifi-
cant gold occurrences in several places
in Greenland have been found and
described. The Nalunaq deposit is the
result of thorough geological work
that included ten years of exploration
prior to commercial mining. In 2004
the mining company Crew Gold Cor -
poration was granted the final licence
to exploit the gold deposit at Nalu -
naq, of which the operations are car-
ried out by the Nalunaq Gold Mine
A/S. The Nalunaq mine was inaugurat-
ed on 26 August 2004 as the first gold
mine in Greenland.
Greenland's first gold mine means the
place that is hard tOFind. It is located
in Kirkespirdalen (Church steeple val-
ley) near the town of Nanortalik.
Since the 1970s a number of signifi-
cant gold occurrences in several places
in Greenland have been found and
described. The Nalunaq deposit is the
result of thorough geological work
that included ten years of exploration
prior to commercial mining. In 2004
the mining company Crew Gold Cor -
poration was granted the final licence
to exploit the gold deposit at Nalu -
naq, of which the operations are car-
ried out by the Nalunaq Gold Mine
A/S. The Nalunaq mine was inaugurat-
ed on 26 August 2004 as the first gold
mine in Greenland.
Introduction
Gold was early on the list of mineral re -
sources that were desirable for exploitation
in Greenland. Today there are several gold
occurrences known in Greenland. These are
primary in-situ deposits of gold. Secondary
deposits of gold, i.e. placer gold, have not
been found in Greenland.
sources that were desirable for exploitation
in Greenland. Today there are several gold
occurrences known in Greenland. These are
primary in-situ deposits of gold. Secondary
deposits of gold, i.e. placer gold, have not
been found in Greenland.
Over the last three decades a number of
significant gold mineralised areas have been
discovered and described. One of the first
was the Tartoq occurrence in South Green-
land, and subsequently new occurrences
were found in the Disko Bugt area, in the
Godthåbsfjord area and at the Skærgaard
Intrusion in East Greenland. In 1992 the dis-
covery at Kirkespirdalen in the very south of
Greenland was made, which 12 years later
served as the background for the establish-
ment of the first modern gold mine in
Greenland, the Nalunaq Mine. The data
gathered on the gold mineralisation in
Kirkespirdalen led to many finds of other
gold occurrences in the region and now the
area is regarded as a major gold province.
discovered and described. One of the first
was the Tartoq occurrence in South Green-
land, and subsequently new occurrences
were found in the Disko Bugt area, in the
Godthåbsfjord area and at the Skærgaard
Intrusion in East Greenland. In 1992 the dis-
covery at Kirkespirdalen in the very south of
Greenland was made, which 12 years later
served as the background for the establish-
ment of the first modern gold mine in
Greenland, the Nalunaq Mine. The data
gathered on the gold mineralisation in
Kirkespirdalen led to many finds of other
gold occurrences in the region and now the
area is regarded as a major gold province.
Geological setting
The geological setting of the Nalunaq gold
mine is the south Greenland basement,
where it is concluded that the Palaeopro-
terozoic Ketilidian juvenile orogen evolved
during northward subduction of an oceanic
plate under the southern margin of the
Archaean craton. The evolution of the
Ketilidian orogen spans from 1850 Ma to
1725 Ma. The orogen is subdivided into
four domains. The central part of the
Ketilidian orogen is dominated by one large,
multi-phase, continental calc-alkaline
batholith, the Julianehåb batholith, which is
emplaced (18541795 Ma) along the
southern margin of the North Atlantic cra-
ton over a north-dipping subduction zone.
The major phases of the deformation
formed several NNE- or NE-trending, sinis-
tral shear zones through the batholith.
mine is the south Greenland basement,
where it is concluded that the Palaeopro-
terozoic Ketilidian juvenile orogen evolved
during northward subduction of an oceanic
plate under the southern margin of the
Archaean craton. The evolution of the
Ketilidian orogen spans from 1850 Ma to
1725 Ma. The orogen is subdivided into
four domains. The central part of the
Ketilidian orogen is dominated by one large,
multi-phase, continental calc-alkaline
batholith, the Julianehåb batholith, which is
emplaced (18541795 Ma) along the
southern margin of the North Atlantic cra-
ton over a north-dipping subduction zone.
The major phases of the deformation
formed several NNE- or NE-trending, sinis-
tral shear zones through the batholith.
The region north of the batholith is
named the Border Zone and consists of
reworked Archaean basement of the craton
and unconformable overlaying Ketilidian
supracrustal rocks, which become progres-
sively involved in the Ketilidian metamor-
phism and deformation towards the south.
These well-preserved (1800 Ma) Ketilidian
supracrustals are located on Midternæs and
reworked Archaean basement of the craton
and unconformable overlaying Ketilidian
supracrustal rocks, which become progres-
sively involved in the Ketilidian metamor-
phism and deformation towards the south.
These well-preserved (1800 Ma) Ketilidian
supracrustals are located on Midternæs and
in Grænseland within the north-western
Border Zone.
Border Zone.
The region south of the batholith com-
prises extensive areas of supracrustal rocks,
the Psammite and Pelite Zones. The
supracrustal rocks occupy a minimum width
of 100 km and with an estimated pre-ero-
sional thickness of over 15 km. The Psam -
mite Zone rocks include basic volcanic rocks,
variably migmatised pelitic and semi-pelitic
rocks, calcareous metasediments, bedded
massive-pyrrhotite/graphitic-cherts, dole -
rites, syn- to post-kinematic appinite dykes
as well as post-kinematic rapakivi granites.
The psammites are interpreted to represent
intra- and fore-arc sediments, eroded from
the Juliane-håb batholith and deposited in
fluvial and shallow marine environments
between the batholith and an oceanic envi-
ronment to the south. The Pelite Zone at
the southern tip of Greenland comprises
the Psammite and Pelite Zones. The
supracrustal rocks occupy a minimum width
of 100 km and with an estimated pre-ero-
sional thickness of over 15 km. The Psam -
mite Zone rocks include basic volcanic rocks,
variably migmatised pelitic and semi-pelitic
rocks, calcareous metasediments, bedded
massive-pyrrhotite/graphitic-cherts, dole -
rites, syn- to post-kinematic appinite dykes
as well as post-kinematic rapakivi granites.
The psammites are interpreted to represent
intra- and fore-arc sediments, eroded from
the Juliane-håb batholith and deposited in
fluvial and shallow marine environments
between the batholith and an oceanic envi-
ronment to the south. The Pelite Zone at
the southern tip of Greenland comprises
2
Aerial view of the Nalunaq mining camp and the road to the mine adits (2006).
The Nalunaq Gold Mine
View towards the south-west of the valley with
the Nalunaq gold mine (centre right) and the 9
km connecting road to the harbour at the
Saqqa Fjord (centre upper).
the Nalunaq gold mine (centre right) and the 9
km connecting road to the harbour at the
Saqqa Fjord (centre upper).
2
3
3
mainly flat-lying, intensely migmatised
pelitic rocks. The pelitic rocks consist mainly
of turbidite sediments, deposited in deeper
offshore settings compared with the fluvial
and shallow marine environments of the
psammites. The mafic volcanic rocks and
granitoids are gold bearing, as observed at
the Nalunaq mine.
pelitic rocks. The pelitic rocks consist mainly
of turbidite sediments, deposited in deeper
offshore settings compared with the fluvial
and shallow marine environments of the
psammites. The mafic volcanic rocks and
granitoids are gold bearing, as observed at
the Nalunaq mine.
The Nalunaq deposit is a high-grade
gold mineralisation associated with quartz-
veins in a major shear zone. As genetic
type, the deposit is an orogenic-type gold
mineralisation (mesothermal lode gold),
hosted in Palaeoproterozoic amphibolite
facies metavolcanic rocks. Visible gold is
found in sheeted quartz veins which are
located in a large-scale shear structure that
appears to be related to regional thrusting.
veins in a major shear zone. As genetic
type, the deposit is an orogenic-type gold
mineralisation (mesothermal lode gold),
hosted in Palaeoproterozoic amphibolite
facies metavolcanic rocks. Visible gold is
found in sheeted quartz veins which are
located in a large-scale shear structure that
appears to be related to regional thrusting.
The most pronounced structure at Nalunaq
is a narrow zone of ductile shearing sur-
rounded by relatively brittle margins. The
gold carrying quartz veins vary from 0.05 m
to 1.8 m in width and often display pinch
and swell structure. The so-called Main Vein
within the deposit is hosted in a 12 m
wide shear zone with a remarkably constant
orientation.
is a narrow zone of ductile shearing sur-
rounded by relatively brittle margins. The
gold carrying quartz veins vary from 0.05 m
to 1.8 m in width and often display pinch
and swell structure. The so-called Main Vein
within the deposit is hosted in a 12 m
wide shear zone with a remarkably constant
orientation.
Exploration history
The exploration prior to commercial mining
began at the end of the 1980s when geolo-
gists from the exploration company Carl
Nielsen A/S observed small flakes of gold in
the gravel at the coast at the foot of the
mountain named Kirkespiret. The systematic
began at the end of the 1980s when geolo-
gists from the exploration company Carl
Nielsen A/S observed small flakes of gold in
the gravel at the coast at the foot of the
mountain named Kirkespiret. The systematic
geological mapping of the area was carried
out already in the 1960s by the Geological
Survey of Greenland (later GEUS) and thus
provided a good foundation for the explo-
ration work. In 1990 the Greenland-Danish
exploration company Nunaoil A/S was
granted an exploration licenses and the
company's chief geologist pursued the idea
that loose gold at the coast must be due to
in-situ gold in the mountains. In 1992 pri-
mary gold was finally located almost 500 m
above sea level on the slopes of the valley
Kirkespirdalen.
out already in the 1960s by the Geological
Survey of Greenland (later GEUS) and thus
provided a good foundation for the explo-
ration work. In 1990 the Greenland-Danish
exploration company Nunaoil A/S was
granted an exploration licenses and the
company's chief geologist pursued the idea
that loose gold at the coast must be due to
in-situ gold in the mountains. In 1992 pri-
mary gold was finally located almost 500 m
above sea level on the slopes of the valley
Kirkespirdalen.
The gold was visible in outcropping
quartz veins and appeared to occur over an
area of 800 m in length. Later, new players
joined the exploration, carrying out the first
drilling at the location, and in 1998 the first
area of 800 m in length. Later, new players
joined the exploration, carrying out the first
drilling at the location, and in 1998 the first
4
T H E N A L U N A Q G O L D M I N E
Geological map of South Greenland with the location of the Nalunaq Gold Mine.
500 km
60°N
61°N
62°N
Gardar intrusions, basalt and sandstone
Inland Ice, local ice caps and glaciers
Undifferentiated basement
100 km
46° W
48° W
44° W
42° W
Ketilidian orogen
Archaean
Arsuk Ø
Grænseland
Midternæs
Qoornoq
Kobberminebugt
Nørrearm
Lindenow Fjord
Danell Fjord
Napasorsuaq
Fjord
Nanortalik
Qaqortoq
Saarloq
Niaqor-
naarsuk
naarsuk
Søndre Sermilik
Tasermiut
Kap Farvel
Eggers Ø
Prins Christian Sund
Sârdloq
shear zone
shear zone
Kangerluluk
Fore-arc deposits, mainly metagreywacke and granites (Pelite Zone)
Fore-arc deposits, mainly metaarkose (Psammite Zone)
Julianehåb batholith and related intrusions
Rapakivi granite suite and related intrusions
Metasedimentary and metavolcanic rocks (Border Zone)
Sermiligaarsuk
Ivituut
FORELAND
BORDER ZONE
JULIANEHÅB
BATHOLITH
FORE ARC
PSAMMITE
ZONE
PELITE
ZONE
Nalunaq Gold Mine
Nalunaq Gold Mine
4
investigation adit was established. From
here it was possible to obtain enough ore
to carry out pilot production and process-
ing. The UK-based Crew Gold Corporation
took over the majority of the shares in the
gold exploration in 1999, whilst 17.5 per
cent were held by the Greenland company
Nunamin-erals A/S. On 26 August 2004 the
mine was officially opened. In November
2007 Crew Gold Corporation acquired all
shares in the gold mine.
here it was possible to obtain enough ore
to carry out pilot production and process-
ing. The UK-based Crew Gold Corporation
took over the majority of the shares in the
gold exploration in 1999, whilst 17.5 per
cent were held by the Greenland company
Nunamin-erals A/S. On 26 August 2004 the
mine was officially opened. In November
2007 Crew Gold Corporation acquired all
shares in the gold mine.
The terrain surrounding the mine is
alpine with mountain peaks reaching
1,2001,600 m above sea level. The
Nalunaq Mountain is 1,340 m high and is
located in a wide glacial valley reaching
into the Saqqa Fjord about 9 km from
the mine site. Deep fjords allow access for
shipping and the overall climate is sub -
1,2001,600 m above sea level. The
Nalunaq Mountain is 1,340 m high and is
located in a wide glacial valley reaching
into the Saqqa Fjord about 9 km from
the mine site. Deep fjords allow access for
shipping and the overall climate is sub -
arctic allowing full operations around the
year.
year.
Preparing a mine
Crew Gold Corporation was granted the
final licence to exploit the gold deposits at
Nalunaq, which was operated by the
Greenland company Nalunaq Gold Mine
A/S. This licence does not include on-site
extraction of the gold from the ore on-site,
but rather the company will ship the ore to
a processing plant abroad. During the first
two years, the extraction was carried out in
Spain at the plant of Rio Narcea Gold
Mines. Following this, the extraction was
moved to Canada at the Nugget Pond plant
in Newfoundland, which Crew Develop-
ment had acquired in 2006. The harbour
final licence to exploit the gold deposits at
Nalunaq, which was operated by the
Greenland company Nalunaq Gold Mine
A/S. This licence does not include on-site
extraction of the gold from the ore on-site,
but rather the company will ship the ore to
a processing plant abroad. During the first
two years, the extraction was carried out in
Spain at the plant of Rio Narcea Gold
Mines. Following this, the extraction was
moved to Canada at the Nugget Pond plant
in Newfoundland, which Crew Develop-
ment had acquired in 2006. The harbour
5
T H E N A L U N A Q G O L D M I N E
level 350
level 400
level 450
South block
Target block
Mountain block
Mining camp
Fault
Exposed quartz vein
The mining camp at Nalunaq. The wooden bar-
racks and facilities are situated along the river
draining the valley. In the front, one of the 25-
tonne trucks en route to the mine.
racks and facilities are situated along the river
draining the valley. In the front, one of the 25-
tonne trucks en route to the mine.
View of the mining area at Nalunaq.
5
6
T H E N A L U N A Q G O L D M I N E
6
facilities constructed at Nalunaq take advan-
tage of the fact that there is deep water at
the coast enabling large ore vessels to dock
and to be loaded directly from the ore stor-
age facility at the harbour.
tage of the fact that there is deep water at
the coast enabling large ore vessels to dock
and to be loaded directly from the ore stor-
age facility at the harbour.
The Crew Gold Corporation owns 100%
of the Greenland limited liability company,
Nalunaq Gold Mine A/S (NGM). The mining
license, granted by the Governments in
Greenland and Denmark in 2004, has a
duration of 30 years. The license covers an
area of 16 km² around the mine site.
In 2004 the basis for the operation of the
mine, according to Nalunaq Gold Mine A/S,
was estimated to be ore reserves of
400,000 t with a gold grade of 21 grams
per tonne. Furthermore there is indication
of extra resources at 1,670,000 t with an
Nalunaq Gold Mine A/S (NGM). The mining
license, granted by the Governments in
Greenland and Denmark in 2004, has a
duration of 30 years. The license covers an
area of 16 km² around the mine site.
In 2004 the basis for the operation of the
mine, according to Nalunaq Gold Mine A/S,
was estimated to be ore reserves of
400,000 t with a gold grade of 21 grams
per tonne. Furthermore there is indication
of extra resources at 1,670,000 t with an
average gold grade of 18 grams per tonne.
Production in 2006 comprised 108,000 t of
ore with an average grade of gold of 17.9
Production in 2006 comprised 108,000 t of
ore with an average grade of gold of 17.9
grams per tonne. Depending on the pro-
duction rate in the mine, there will probably
be enough ore for an operating period of
duction rate in the mine, there will probably
be enough ore for an operating period of
Underground exploration drilling inside the
Nalunaq mine.
Nalunaq mine.
The study of an underground face of the gold bearing quartz vein in the Nalunaq mine.
7
T H E N A L U N A Q G O L D M I N E
Exploration drilling at the slope of the Nalunaq
mountain on the northern side of
Kirkespirdalen looking towards the north-east.
mountain on the northern side of
Kirkespirdalen looking towards the north-east.
7
between three and ten years. Nalunaq is
equipped with a fully functional assay labo-
ratory, consisting of a preparation lab, a
equipped with a fully functional assay labo-
ratory, consisting of a preparation lab, a
wet chemistry lab and an assay section with
computerized AAS instrumentation.
computerized AAS instrumentation.
Mine operations
The camp accomodate 100 people to man-
age the operation within the mine, in the
camp and harbour. Mining operations and
maintenance are contracted to Procon Mi -
ning and Tunnelling Ltd. of Canada on a
labour hire basis. Mining equipment is
owned by NGM and the Crew Gold Cor -
poration. Locally contractors out of Nanor -
talik are engaged for surface ore haul, on-
site construction work, catering and janitor-
ial work. In total, over 35% of the employ-
ees are locally hired.
age the operation within the mine, in the
camp and harbour. Mining operations and
maintenance are contracted to Procon Mi -
ning and Tunnelling Ltd. of Canada on a
labour hire basis. Mining equipment is
owned by NGM and the Crew Gold Cor -
poration. Locally contractors out of Nanor -
talik are engaged for surface ore haul, on-
site construction work, catering and janitor-
ial work. In total, over 35% of the employ-
ees are locally hired.
On-site, the ore is hauled by 25-tonne
trucks to a 60,000 t capacity stockpile area
at the harbour facility established on the
Saqqaa fjord about 11 km from the mine
site. When there is sufficient ore, a ship is
requested from Western Bulk Carriers with
whom the mine has an annual contract.
Bulk carriers with 2030,000 t capacity are
loaded at the Nalunaq port for delivery to
the Nugget Pond processing facilities.
at the harbour facility established on the
Saqqaa fjord about 11 km from the mine
site. When there is sufficient ore, a ship is
requested from Western Bulk Carriers with
whom the mine has an annual contract.
Bulk carriers with 2030,000 t capacity are
loaded at the Nalunaq port for delivery to
the Nugget Pond processing facilities.
The Nalunaq mine has posed consider-
able challenges due to the geometry of the
Long-hole drilling
Charging long-holes
© Carsten E. Thuesen, GEUS
Access cross-cuts
Sub-level
development
Broken ore
Slot raise
10 m vertical
sub-level interval
Pillar
Mined stopes
8
An underground view of a hanging wall of a mined-out 1.2 m stope.
Schematic 3-D presentation of the mining
method used with demonstration of the long-
hole open stoping system. 3D figure: Carsten E.
Thuesen, GEUS.
method used with demonstration of the long-
hole open stoping system. 3D figure: Carsten E.
Thuesen, GEUS.
T H E N A L U N A Q G O L D M I N E
8
Main Vein. The typical situation in the mine
is a narrow average vein width of 0.7 m,
with a 3040 degree dip. The narrow width
calls for a high degree of drilling and blast-
ing accuracy to prevent dilution, and the
dip both precludes efficient footwall layouts
for mechanised mining and requires addi-
tional rock handling activities to ensure that
the ore is successfully transferred to the
bottom of the stope for later pick-up.
is a narrow average vein width of 0.7 m,
with a 3040 degree dip. The narrow width
calls for a high degree of drilling and blast-
ing accuracy to prevent dilution, and the
dip both precludes efficient footwall layouts
for mechanised mining and requires addi-
tional rock handling activities to ensure that
the ore is successfully transferred to the
bottom of the stope for later pick-up.
The preferred mining method is longhole
open stoping, which comprises develop-
ment of sub-levels horizontally along strike
at 10 m intervals in vertical spacing, result-
ing in ore blocks of about 1416 m length
on dip. The sub-levels are either mined as a
full face or in two cuts separating the ore
and the waste. The block between two sub-
levels is then subdivided into 15 m wide
stopes between 1.5 m rib pillars for stability.
A stope thickness of 1.4 m is endeavoured
and each stope is drilled with blast holes
up-dip using a ring box pattern. Following
stoping and removal of the ore, the stope
has to be cleaned of any residual fine ore,
some of which is high grade. The resulting
stope cavities are unsupported and open to
ment of sub-levels horizontally along strike
at 10 m intervals in vertical spacing, result-
ing in ore blocks of about 1416 m length
on dip. The sub-levels are either mined as a
full face or in two cuts separating the ore
and the waste. The block between two sub-
levels is then subdivided into 15 m wide
stopes between 1.5 m rib pillars for stability.
A stope thickness of 1.4 m is endeavoured
and each stope is drilled with blast holes
up-dip using a ring box pattern. Following
stoping and removal of the ore, the stope
has to be cleaned of any residual fine ore,
some of which is high grade. The resulting
stope cavities are unsupported and open to
the sub-levels above and below. Nalunaq
ore production rate is carried out close to
the planned aim of 500 t per day.
ore production rate is carried out close to
the planned aim of 500 t per day.
To access the sub-levels, from which all
operations are carried out, a ramp and a
number of mine adits have been excavated.
Ore passes are used for transfer of mined
ore.
number of mine adits have been excavated.
Ore passes are used for transfer of mined
ore.
Gold extraction
The amount of gold in the ore is rather
erraticly distributed (nugget effect) with an
average of 18 grams of gold per tonne of
ore, but there are locally very rich parts that
contain as much as four tOFive kg of gold
per tonne of ore. Due to the fact that the
gold occurs in quartz veins, on average only
0.7 m wide, the mining of the ore may
result in a reduction of the gold content as
it is impossible to avoid mixing of bedrock
erraticly distributed (nugget effect) with an
average of 18 grams of gold per tonne of
ore, but there are locally very rich parts that
contain as much as four tOFive kg of gold
per tonne of ore. Due to the fact that the
gold occurs in quartz veins, on average only
0.7 m wide, the mining of the ore may
result in a reduction of the gold content as
it is impossible to avoid mixing of bedrock
9
The layout of the Nalunaq Gold Mine with the
three main levels, drifts and raises in a 3-D
model presentation, November 2005.
three main levels, drifts and raises in a 3-D
model presentation, November 2005.
1
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X
100.00 Y
200.00 Y
300.00 Y
400.00 Y
500.00 Y
600.00 Y
700.00 Y
800.00 Y
300 Level
350 Level
400 Level
450 Level
7/11 2005
Rock sample of quartz vein rich in gold grains.
T H E N A L U N A Q G O L D M I N E
9
T H E N A L U N A Q G O L D M I N E
10
10
with low gold content into the ore. The
minerals in the gold ore are dominated by
metallic gold. Various sulphide minerals in
which gold occurs as impurities account for
less than one per cent. This means that
when the gold is extracted, it 'only' has to
be released from the surrounding silicates
(mostly quartz). In practice this is done by
crushing and subsequent gravity separation
where the high density of gold is utilised
(19.3 g/cm3). This process can achieve a
high recovery rate of close to 100%. Once
the gold has been extracted from the ore, it
is easily melted and cast into ingots for
commercial sale. In practice smelting is car-
minerals in the gold ore are dominated by
metallic gold. Various sulphide minerals in
which gold occurs as impurities account for
less than one per cent. This means that
when the gold is extracted, it 'only' has to
be released from the surrounding silicates
(mostly quartz). In practice this is done by
crushing and subsequent gravity separation
where the high density of gold is utilised
(19.3 g/cm3). This process can achieve a
high recovery rate of close to 100%. Once
the gold has been extracted from the ore, it
is easily melted and cast into ingots for
commercial sale. In practice smelting is car-
ried out in several stages so that the
slag material (from silicate residues)
and impurities of silver, bismuth, anti-
mony and arsenic are removed before
the final commercially tradable pure
gold (bullion) is produced. The smelt-
ing process is carried out outside Greenland
at the smelting plant at Nugget Pond in
Canada.
slag material (from silicate residues)
and impurities of silver, bismuth, anti-
mony and arsenic are removed before
the final commercially tradable pure
gold (bullion) is produced. The smelt-
ing process is carried out outside Greenland
at the smelting plant at Nugget Pond in
Canada.
Concluding remarks
Nalunaq is a high-grade deposit of gold in
quartz veins. The individual quartz veins are
between 0.12.0 m thick, averaging 0.7 m.
The gold-bearing structure has a regional
scale, and it is therefore expected that the
amount of ore is much larger. Production of
gold from Nalunaq is targeted to amount to
four tonnes of gold per year.
quartz veins. The individual quartz veins are
between 0.12.0 m thick, averaging 0.7 m.
The gold-bearing structure has a regional
scale, and it is therefore expected that the
amount of ore is much larger. Production of
gold from Nalunaq is targeted to amount to
four tonnes of gold per year.
In the wake of the successful start of the
mine it has been natural to seek for an
extension of its productive life. In order to
reach the goal of extending ore reserves
exploration activities have been initiated in
both the mine area and in the surrounding
areas with potentially gold-bearing rocks.
Outside the mine area the mining company
mine it has been natural to seek for an
extension of its productive life. In order to
reach the goal of extending ore reserves
exploration activities have been initiated in
both the mine area and in the surrounding
areas with potentially gold-bearing rocks.
Outside the mine area the mining company
T H E N A L U N A Q G O L D M I N E
11
The Saqqa Fjord filled with icebergs. A bulk-carrier preparing for leaving with a full ore
load. To the right the port and in the centre the road to the mining camp in Kirkespir-
dalen. The landmark of the 1590 m high Kirkespiret mountain, is seen in the back-
ground.
load. To the right the port and in the centre the road to the mining camp in Kirkespir-
dalen. The landmark of the 1590 m high Kirkespiret mountain, is seen in the back-
ground.
A working conveyor belt as part of the loading
system for the vessels at the harbour facility.
system for the vessels at the harbour facility.
A docking bulk-carrier at the Nalunaq port. Close to
the pier is the location of the ore storage facility with a
number of ore piles. The road connection to the
Nalunaq mining camp can be followed along the coast
line.
the pier is the location of the ore storage facility with a
number of ore piles. The road connection to the
Nalunaq mining camp can be followed along the coast
line.
11
has been granted additional exploration
licences, which in total covers an area of
around 500 km
licences, which in total covers an area of
around 500 km
2
. At present, activities with-
in the licence area have proven occurrences
of gold mineralisation at a locality 20 km
SW of Nalunaq and on the Niaqornaarsuk
peninsular around 20 km NW of Nalunaq.
Additionally there are various indications of
gold at a number of other sites with corre-
sponding geological environments.
of gold mineralisation at a locality 20 km
SW of Nalunaq and on the Niaqornaarsuk
peninsular around 20 km NW of Nalunaq.
Additionally there are various indications of
gold at a number of other sites with corre-
sponding geological environments.
Garde, A.A., Hamilton M.A., Chadwick B.,
Grocott J., & McCaffrey K.J.W. 2002:
The
Ketilidian orogen of South Greenland: geo -
chronology, tectonics, magmatism, and fore-arc
accretion during Palaeoproterozoic oblique con-
vergence, Canadian Journal of Earth Sciences
39
, 765793.
Gowen, J., Christiansen, O., Grahl-Madsen, L.,
Pedersen, J. L., Petersen, J. S. & Robyn,T.L.
1993:
Discovery of the Nalunaq gold deposit,
Kirkespirdalen, SW Greenland. International
Geology Review
35(11)
, 10011008.
Grammatikopoulos, T. A., Porrit, L., Petersen,
J.S. & Christensen, K. 2004:
Mineralogical char-
acterisation and process mineralogy of gold bear-
ing rocks from the Nalunaq gold deposit,
Greenland. Applied Earth Science
113(3)
, 197203.
Kaltoft, K., Schlatter, D.M. & Kludt, L. 2000:
Geology and genesis of Nalunaq Palaeo
-
proterozoic shear zone-hosted gold deposit,
South Greenland. Applied Earth Science
109
(Section B), B23B33.
Lind, M., Kludt, L. & Ballou, B. 2001:
The Nalunaq
gold prospect, South Greenland: test mining for
feasibility studies. Geology of Greenland Survey
Bulletin
189
, 7075.
Stendal, H. & Secher, K. 2002:
Gold mineralisa-
tion and gold potential in South Greenland.
Geology and Ore
1
, 12 pp.
Stendal, H., Secher, K., Stensgaard, B.M.,
Schønwandt, H.K. & Thorning, L. 2005
:
Greenland geological environments and mineral
resources. Copenhagen, Danmarks og Grønlands
Geologiske Undersøgelse Rapport
2005/8
, 211 pp.
12
Front cover photograph
Underground view of a gold carrying
quartz vein in the Nalunaq mine. Blue
paint is marking the ore to be mined.
Bureau of Minerals and Petroleum
(BMP)
Government of Greenland
P.O. Box 930
DK-3900 Nuuk
Greenland
Tel: (+299) 34 68 00
Fax.: (+299) 32 43 02
E-mail: bmp@gh.gl
Internet: www.bmp.gl
Geological Survey of Denmark
and Greenland (GEUS)
Øster Voldgade 10
DK-1350 Copenhagen K
Denmark
Tel: (+45) 38 14 20 00
Fax.: (+45) 38 14 20 50
E-mail: geus@geus.dk
Internet: www.geus.dk
Authors
K. Secher, H. Stendal & B.M.
Stensgaard
Editor
Karsten Secher, GEUS
Graphic Production
Henrik Klinge Pedersen, GEUS
Photographs
Photos and illustrations: GEUS and
courtesy of the Nalunaq Gold Mine.
Printed
February 2008 © GEUS
Printers
Schultz Grafisk
ISSN
1602-818x
Key literature
An example of the use of Greenland gold: a
couple of 22 K wedding rings with a Polar Bear
mark visible. Artist: Goldsmith Nicolai Appel,
Copenhagen, Denmark.
couple of 22 K wedding rings with a Polar Bear
mark visible. Artist: Goldsmith Nicolai Appel,
Copenhagen, Denmark.
The first output: a 1 kilOFine Gold bullion
(No. A 00001) produced from the Nalunaq
Gold Mine.
(No. A 00001) produced from the Nalunaq
Gold Mine.
12
Last modified: February 14, 2008
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