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This alpine wetland is of interest to botanists because "its wide range of plants have adapted to acidic soils at very low temperatures." Sedges, herbs, grasses and mosses make up the ground cover on the floor of the wetland and the
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Over 260 species of higher plant have been recorded in the swamp and
Margaret Bayfield identified several different assemblages within it. The southern margin comprises scrub and shrub/tussockland and is dominated by
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57:. It was formed approximately 3,500 years ago and is of particular interest to botanists. Over 260 species of higher plant have been recorded there. The area of the swamp is approximately 1 km.
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change. The Stony River was considered
Taranaki's best trout fishery until severe erosion and land instability in the river's headwaters from 1997 onwards caused high sediment loads.
77:. This extrusion, which reaches 1,052 metres, lies to the west of the swamp and is known as The Dome. The outlet from the swamp forms the 30-metre-high (98 ft) Bells Falls.
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to the northwest, which reaches 1,400 metres. It was formed about 3,500 years ago when a lava extrusion and a later debris flow blocked the
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The
Pouakai Circuit, a 2–3 day 25 km tramp that has two overnight huts available, passes through "the unique Ahukawakawa Swamp" via a
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A 360° panorama of the
Ahukawakawa Swamp photographed from where the Pouakai Circuit boardwalk footbridge crosses the
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that form in the cool environment and medium fertility wet soils are a feature of the natural environment.
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and sphagnum. Small bodies of open water towards the east end of the swamp contain the pond weed
375:. National Parks Scientific Series Number 5. Science Information Publishing Centre. Wellington.
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The swamp sits at an altitude of 920 metres and lies between the main cone of
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drainage system. Ahukawakawa Swamp is visible to the left of the summit of
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340:"Pouakai Circuit" information sheet. (2014) Department of Conservation.
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287:. Te Ara – The Encyclopedia of New Zealand. Retrieved 6 January 2015.
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304:. Te Ara – The Encyclopedia of New Zealand. Retrieved 6 January 2015.
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244:. Latitude: -39.2518 Longitude: 174.048. Retrieved 7 January 2015.
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is dominant and found along with various sedges including
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373:Vegetation of Egmont National Park New Zealand
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155:. There are abundant mosses, especially
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317:. Taranaki Daily News. 27 November 2010
165:and the New Zealand sub-species of the
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141:are also common. In the "mire proper"
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315:"Erosion Changes face of Mountain"
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218:Tussock grasslands of New Zealand
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131:) although other shrubs such as
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268:. Department of Conservation/
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80:The area is still subject to
33:can also be seen to the west.
285:"Western North Island parks"
272:. Retrieved 6 January 2015.
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29:and the upper canyon of the
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603:Protected areas of Taranaki
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115:to the area. The large red
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570:Ski fields and structures
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358:Clarkson (1986) pp. 45-47
171:Myriophyllum pedunculatum
608:Wetlands of New Zealand
371:Clarkson, B. D. (1986)
223:Wetlands of New Zealand
163:Potamogeton suboblongus
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613:Landforms of Taranaki
349:Clarkson (1986) p. 43
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618:Egmont National Park
450:Mountains and ranges
442:Egmont National Park
158:Dicranoloma robustum
47:Egmont National Park
582:Mount Egmont Branch
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302:"Ahukawakawa Swamp"
259:"Taranaki wetlands"
264:2013-02-23 at the
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577:Manganui Ski Area
529:Waiwhakaiho River
524:Waingongoro River
483:Ahukawakawa Swamp
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561:Te Rere o Kapuni
499:Hangatahua River
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514:Pātea River
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204:Stony River
143:red tussock
139:leatherwood
75:Stony River
55:New Zealand
31:Stony River
23:Mt Taranaki
597:Categories
554:Waterfalls
366:References
153:star sedge
129:filifolium
88:Vegetation
545:Lake Dive
321:6 January
229:Citations
184:boardwalk
388:174°03′E
262:Archived
212:See also
117:tussocks
69:and the
43:sphagnum
385:39°15′S
178:Tourism
167:milfoil
113:endemic
49:in the
45:bog in
492:Rivers
476:Swamps
127:(var.
105:shrub
538:Lakes
125:inaka
323:2015
151:and
137:and
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53:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
