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Abel Tasman National Park is located at the
top of the South Island. It is the smallest of all national
parks in New Zealand, with an area of 22,500 hectares (87 square
miles). The land was extensively modified by fire, forest clearing
and introduced plants, before being abandoned and reverting
to wilderness. The creation of the national park in 1942 followed
threats of further exploitation of the remaining native forests.
Abel Tasman National Park is a rough and mountainous area, best
known for its coastline of crescent-shaped bays, golden sand
beaches, clear waters, little islands and granite headlands
sculpted by erosion. Both sea-kayaking and tramping (the Coastal
Track is one of New Zealand's Great Walks) are especially well
suited to discovering and enjoying this coast.
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Specific
references for this page:
Gerald
Cubitt and Les Molloy 1994: Wild
New Zealand. New Holland.
Craig
Potton 1998: National
Parks of New Zealand. Craig Potton Publishing.
A
Park for All Seasons - The Story of Abel Tasman National
Park . Abel Tasman National Park 1985.
New
Zealand National Parks. Collins Nature Heritage Series
1979.
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Geological
setting
The Pikikituna Range is the central mountainous axis of
the park, reaching altitudes of 1156 m (3792') at Mt Evans,
and 1101 m (3612') at Pisgah Hill. The granites (grano-diorites,
quartz diorites and similar) that form most of the coastal cliffs
and outcrops extend inland over the greatest part of the park.
However the western part is made of older (Ordovician) marbles,
limestones, argillites and other rocks, similar to those of
Mt Arthur and Mt Owen in Kahurangi National Park further west.
See also Kahurangi
National Park
The
karst of Takaka Hill and Canaan Downs
These marbles have been intensely subjected to the dissolution
work of water, to produce a type of landform called karst. In
Takaka Hill and Canaan Downs the many karstic features include
caves, sink-holes (dolines), disappearing streams, and karren
(surface dissolution features). This karst includes some of
the deepest caves in New Zealand (Green Link, approximately
360 m/1180') deep, the deepest cave shaft in New Zealand (Harwoods
Hole: 176 m/577' vertical drop), and New Zealand's largest spring:
Waikoropupu Springs, with a discharge averaging 15 m3/second
(35 cu. feet).
Climatic
conditions
With over 2200 hours of sunshine annually the coast of Abel
Tasman National Park is among the sunniest places in New Zealand.
On the coast rainfall, with 1800 mm (71 in.) annually, is fairly
moderate, and is distributed evenly throughout the year. Temperatures
are mild and vary seasonally within a narrow range, from average
daily minimum and maximum of 13.5 C and 24.5 C in January, to
corresponding 4.0 C and 12.5 C in July. Frosts occur on average
25 days in the year, with minima usually within the -1 C to
-2 C range. Thus the park enjoys plenty of mild and sunny weather,
but strong easterlies and westerlies make the coast very windy
through much of the year.
On higher ground clouds and rain are more frequent, rainfall
totalling over 2500 mm (98 in.) annually. Snow may lie on the
ground for short periods.
Vegetation
The original vegetation of the park was extensively cut
down and burnt, but it is regenerating well, with both exotic
and native species. Over three quarters of the park's area is
forested. The uplands are dominated by beech. An interesting
feature of this small park is that all four species of beech
are present, as well as the black beech sub-species of mountain
beech. Hard beech dominates close to the coast, while mountain
and silver beech are more common higher up. Silver beech is
dominant on the poorer soils. Podocarp-broadleaf forests grew
in most valleys below 325 m (1066'), but they were felled for
timber. There are extensive areas of scrubland where the original
vegetation was burnt, as well as exotic pines which cover large
areas. There are also two remarkable naturally non forested
areas in the park. Between Maharau and Torrent Bay only manuka
and kanuka grow on very poor soils developed over the granite
base rock. And Moa Park, near the source of Table Creek on Mt
Evans, is a boggy area where peat has accumulated over impermeable
granite. The vegetation is made of red tussock, sphagnum and
bog pine.
Wildlife
Abel Tasman National Park is home to a wide diversity of birds,
thanks to a range of marine, coastal and forest habitats. Some
of New Zealand's rarest and most endangered birds have disappeared
altogether, in particular kiwi, kokako, kakapo and saddleback.
Others, like kakas, parakeets, New Zealand falcons, and keas
in the uplands, are rare. Little blue penguins, which used to
be common in all the bays, have been decimated by stoats and
now live mainly on the offshore islands. By contrast the population
of wekas has increased again.
The large landsnail Paryphanta is common
in the park. The cave systems are home to several species of
cave wetas and many other insects, such as beetles, spiders,
millipedes, and glow worms.
Among its marine life, the coast of Abel Tasman National Park
has internationally recognised bryozoan 'coral' beds.
Short
and day walks
Starting from each of the three roadends
at Marahau, Totaranui and Canaan Downs, a number of short and
day walks give access to a good range of the natural features
and points of interest of Abel Tasman National Park.
The park is famous for its coastline, and several
walks lead to some of its very attractive golden sand beaches,
bays, clear waters and sculpted rocky headlands. There is a
profusion of wildlife, with many birds and, in places, colonies
of fur seals basking in the sun on the rocks.
These walks also cross a variety of forest and vegetation
types. The native forests are now mainly beech, but some coastal
places are rich in tree ferns and nikau palms, creating a distinctive
tropical character. There are also a few remnants of the original
podocarp forests, with trees such as rimu, kahikatea, and pukatea,
which were extensively milled.
In the western part of the park the Canaan Road
leads to the karst and caves of the marble area. The major attraction
there is Harwoods Hole, the greatest cave shaft in the southern
hemisphere with a vertical drop of 176 m (577').
Tramping
The park offers two major tramping tracks: the Coast
Track, and the Inland Track. The Coast Track is classified as
a walking track, and is one of New Zealand's Great Walks. Its
51 km (32 miles) are usually walked in 3-5 days.
The Inland track is a tramping track that leads
over the highest part of the park, through both regenerating
and undisturbed forest. It is also walked in 3-5 days.
Sea
kayaking
With its dissected coastline of rounded bays, estuaries,
rocky headlands and small islands, Abel Tasman is one of the
most popular places for sea-kayaking in New Zealand.
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