The

Tasman Region Tasman District () is a local government district in the northwest of the South Island of New Zealand. It borders the Canterbury Region, West Coast Region, Marlborough Region and Nelson City. It is administered by the Tasman District Council, a ...

, and the small adjoining

Nelson Region (Let him, who has earned it, bear the palm) , image_map = Nelson CC.PNG , mapsize = 200px , map_caption = , coordinates = , coor_pinpoint = , coordinates_footnotes = ...

, form one of the more geologically interesting regions of New Zealand. It contains the oldest rocks of anywhere on New Zealand's main islands. It contains all the main terranes that make up New Zealand's basement. These basement rocks include

Ultramafic rock Ultramafic rocks (also referred to as ultrabasic rocks, although the terms are not wholly equivalent) are igneous and meta-igneous rocks with a very low silica content (less than 45%), generally >18% MgO, high FeO, low potassium, and are composed ...

s, such as

Serpentine Serpentine may refer to: Shapes * Serpentine shape, a shape resembling a serpent * Serpentine curve, a mathematical curve * Serpentine, a type of riding figure Science and nature * Serpentine subgroup, a group of minerals * Serpentinite, a ...

and

Dunite Dunite (), also known as olivinite (not to be confused with the mineral olivenite), is an intrusive igneous rock of ultramafic composition and with phaneritic (coarse-grained) texture. The mineral assemblage is greater than 90% olivine, with mi ...

, and valuable minerals, such as

Gold Gold is a chemical element with the symbol Au (from la, aurum) and atomic number 79. This makes it one of the higher atomic number elements that occur naturally. It is a bright, slightly orange-yellow, dense, soft, malleable, and ductile met ...

. The Nelson Region is bordered to the south by the Alpine Fault (usually named the

Wairau Fault The Wairau Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique conv ...

in the Wairau Valley), the main fault forming the boundary between the

Pacific Plate The Pacific Plate is an oceanic tectonic plate that lies beneath the Pacific Ocean. At , it is the largest tectonic plate. The plate first came into existence 190 million years ago, at the triple junction between the Farallon, Phoenix, and Iza ...

and the

Indo-Australian Plate The Indo-Australian Plate is a major tectonic plate that includes the continent of Australia and the surrounding ocean and extends northwest to include the Indian subcontinent and the adjacent waters. It was formed by the fusion of the Indian an ...

, that generated the Southern Alps.

Basement rocks

The terranes that make up New Zealand's basement are divided up into a Western Province, composed of the Buller and Takaka terranes, and an Eastern Province, composed of the Brook Street, Murihiku, Dun Mountain-Maitai, Caples, Torlesse Composite (Rakaia and Pahau), and Waipapa Composite Terranes. The Median Batholith forms the boundary between the two provinces. All these terranes occur within or near the Nelson Region. The Buller Terrane forms the basement rocks to the west of the Anatoki Fault (roughly from Whanganui Inlet to Springs Junction), and throughout the West Coast, west of the Alpine Fault, to Milford Sound. The Greenland Group rocks form the base, and are composed of sandstones and mudstones deposited in a submarine fan environment (Late Cambrian-early Ordovician, 505-470 Ma). They are overlain by the Golden Bay Group rocks, composed of quartz sandstone and shale (Ordovician, 490-443 Ma). The Takaka Terrane forms the basement rocks east of the Anatoki Fault and west of Takaka, the Authur and Matiri Range, south to Springs Junction. The Takaka Terrane is structurally complex, and heavily faulted. The earliest (Middle Cambrian, 518-515 Ma, mostly western) rocks were deposited in an oceanic volcanic arc environment, and represent the oldest rocks in the main islands of New Zealand. Rocks in the Cobb Valley include gabbro and ultramafic rocks that are now largely serpentised. Later (Late Cambrian-Early Devonian, 500-397 Ma, mostly eastern) rocks were deposited in a passive margin environment, and include the Mount Arthur limestone and marble. The Buller and Takaka Terranes are believed to have been amalgamated around Early or Middle Devonian times, about 390 Ma ago. After amalgamation, in Late Devonian times (370-354 Ma), the Karamea Suite granites were intruded into the Buller Terrane. The Karamea Suite granite often has a distinctive pink colour, due to the K-feldspar megacrysts. The Median Batholith forms the rocks between the Western and Eastern Provinces. It is assumed to represent a long lived (Late Devonian-Early Cretaceous, 375-110 Ma) Cordilleran batholith, corresponding to a subduction zone along the margin of eastern Australia, before the formation of the Tasman Sea (83-55 Ma). The Median Batholith includes the Riwaka Complex (~375 Ma) and Separation Point Suite (~110 Ma). The Riwaka Complex intruded rocks on the west of Abel Tasman National Park, south to the Baton River Area. The Separation Point Suite corresponds to the granite rocks from Abel Tasman National Park, south to Springs Junction. The basement rocks between Motueka and Nelson, south to Nelson Lakes, are also part of the Median Batholith, but are mainly hidden by the Moutere Depression. However the Median Batholith outcrops around Peppin Island-Nelson City and Nelson Lakes. The Eastern Province Brook Street, Murihiku, and Dun Mountain-Maitai Central Arc Terranes form narrow successively more easterly strips to the east of the Waimea-Flaxmore Fault System, running from Durville Island in the north, to the Alpine Fault near Nelson Lakes in the south. The Brook Street Terrane corresponds to a Permian (300-250 Ma) oceanic island arc, and contains well-preserved cross sections through volcanic cones. The Murihiku Terrane is composed of Triassic to Jurassic (250-145 Ma), relatively undeformed marine sandstone, derived from a volcanic arc. The

Dun Mountain-Maitai Terrane The Dun Mountain-Maitai Terrane comprises the Dun Mountain Ophiolite Belt (also called the Mineral Belt), Maitai Group and Patuki Mélange. The Dun Mountain Ophiolite is an ophiolite of Permian age located in New Zealand's South Island. Prehistori ...

includes the

Early Permian 01 or '01 may refer to: * The year 2001, or any year ending with 01 * The month of January * 1 (number) Music * '01 (Richard Müller album), 01'' (Richard Müller album), 2001 * 01 (Son of Dave album), ''01'' (Son of Dave album), 2000 * 01 (Urban ...

(290-256 Ma) Dun Mountain Ophiolite Belt, composed of mafic sea floor basalts and ultramafic mantle rocks. The high nickel and magnesium content inhibits the growth of vegetation on Dun Mountain and Red Hills. These are overlain by Early Permian to Triassic (290-206 Ma) Maitai Group breccia, sandstone, siltstone and limestone. The Caples Terrane forms much of the Marlborough Sounds, from east of

D'Urville Island D'Urville Island (), Māori language, Māori name ' ('red heavens look to the south'), is an island in the Marlborough Sounds along the northern coast of the South Island of New Zealand. It was named after the France, French List of explorers, ...

, to west of Charlotte Sound, and southwest to Nelson Lakes and the Alpine Fault (Wairau Valley). The Caples Terrane was formed in Late Permian to Middle Triassic times (256-227 Ma). The rocks are mostly sandstone and argillite, deposited in a submarine fan, adjacent to an island arc, which have been metamorphosed to schist close to the boundary with the Rakaia Terrane in the southeast. The Torlesse (Composite) Terane is composed of the Rakaia and Pahau Terranes. The rocks are mostly marine sandstone and mudstone, with the Pahau Terrane being younger (Late Jurassic to Early Cretaceous, 159-99 Ma) than the Rakaia Terrane (Permian to Late Triassic, 290-206 Ma). The Aspiring Lithologic Association schist, south of the Caples Terrane and north of the Alpine Fault, is regarded as belonging to the Rakaia Terrane. The rocks to the south of the Alpine Fault belong to the Torlesse Composite Terrane (Rakaia to the west of Nelson Lakes, Pahau to the east). The Waipapa (Composite) Terrane is composed of the Hunua and Morrinsville Terranes. The rocks around Picton-Arapawa Island are thought to belong to the Morrinsville Terrane, and are Late Triassic (227-206 Ma) sandstone that has been metamorphosed into schist. The rocks of western Nelson used to be adjacent to those in Fiordland and Central Otago, before the Alpine Fault was activated in the Early Miocene (23 Ma). The terranes in Nelson match those on the other side of the Alpine Fault, in Fiordland and Central Otago.

Coal and limestone

Most of the Nelson area was above sea level from Late Cretaceous to Middle Eocene time. Coal measures developed in swampland around the Whanganui Inlet in the Late Cretaceous. The coal measures were later covered by sandstone, then conglomerate, corresponding to a braided floodplain. Much of the cover rocks have since been eroded. Coal measures also developed in swampland over much of western Nelson in Late Eocene times (40-34 Ma). The coal measures are preserved in the Buller Coalfield, the Heaphy River, Takaka, and Richmond. The land then sank, the sea transgressed, and calcareous sandstone,

mudstone Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology. ...

, and

limestone Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms whe ...

were deposited in Oligocene times (34-24 Ma).

Uplift

The Alpine Fault developed in Early Miocene times (23 Ma), uplift occurred, and deposition changed from limestone to mudstone. Rapid uplift of the Southern Alps occurred in the Late Pliocene (3 Ma). Large quantities of Torlesse derived gravel were generated from the Southern Alps, and are preserved in the Moutere Depression.

Current movement

The Alpine Fault is moving at 3-5mm/year, and the

Awatere Fault The Awatere Fault is an active dextral (right lateral) strike-slip fault in the northeastern part of South Island, New Zealand. It forms part of the Marlborough Fault System, which accommodates the transfer of displacement along the oblique conv ...

at 6-8mm/year. The Waimea-Flaxmore Fault System is also active. The Marlborough Sounds are sinking 1-7mm/year. Nelson itself is relatively stable, and the western coast is rising 0-1mm/year.

Geological resources

Alluvial gold has been obtained in the Anatoki, Takaka, Aorere and Paparoa valleys of Golden Bay. Gold has been mined in the Aorangi Mine (Golden Blocks) area, and Johnston's United Mine area. It has also been mined within the Caples Terrane schist. Chromium and copper have been mined in the Dun Mountain Ophiolite Belt. Asbestos, talc and magnesite have been mined in the Cobb area. Coal has been mined in Collingwood, Takaka, Nelson-Richmond, Baton, Heaphy,

Karamea Karamea is a town on the West Coast of the South Island of New Zealand. It is the northernmost settlement of any real size on the West Coast, and is located northeast by road from Westport. Apart from a narrow coastal strip, the town of Karam ...

and Buller areas. Mount Arthur marble is used for buildings. Tertiary limestone is quarried to make cement. The sea to the northwest of the Nelson region are believed to have the potential for oil and gas.

Geological hazards

The main geological hazard is from earthquakes along the Alpine Fault or related faults. Earthquakes in surrounding areas, such as Murchison, Kaikoura, and Wellington also have the potential for damage.

Geological sites of interest

The Cobb Valley, with mafic and ultramafic rocks, serpentine, talc, and asbestos are of great interest. Abel Tasman National Park is of interest for limestone and marble, Separation Point granite, and the Riwaka Complex diorite and gabbro. From the top of the park, it is possible to see

Harwoods Hole Harwoods Hole is a cave system located in the northwest of the South Island of New Zealand, in the Abel Tasman National Park. At , it is New Zealand's deepest vertical shaft. It was first explored in 1958, long after it was discovered. Format ...

, a large vertical shaft that goes down to the limestone cave system of Takaka Hill. The Arthur Range is a good place to see Mount Arthur marble. The Bryant Range is a good place to see the Central Arc Terranes. Red Hill and Dun Mountain are good places to see the effects of ultramafic rocks on vegetation. A trip on the inter-island ferry provides a good way to see the Marlborough Sounds. The Alpine Fault can be seen in the Wairau Valley, between Blenheim and Nelson Lakes. The effects of glaciation can be seen around Nelson Lakes.

Maps

Geological maps of New Zealand can be obtained from the New Zealand Institute of Geological and Nuclear Science ( GNS Science), a New Zealand Government Research Institute. GNS provides a free Map of New Zealand's Geological Foundations. The main maps are the 1 : 250 000 QMap series, which will be completed as a series of 21 maps and booklets in 2010. Low resolution versions of these maps (without the associated booklet) can be downloaded from the GNS site for free. The map for the Nelson Area was published in 1998. The map for the Wellington Area was published in 2000. The map for the Greymouth Area was published in 2002. The map for the Kaikoura Area was published in 2006.

References

Bibliography

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