In this section
Inland & alpine
- Basic cliffs, scarps and tors
- Boulderfields of acidic rocks (non-volcanic)
- Boulderfields of calcareous rocks
- Braided riverbeds
- Calcareous cliffs, scarps and tors
- Calcareous screes
Cliffs, scarps and tors of acidic rocks
- Cliffs, scarps and tors of quartzose rocks
- Cloud forests
- Frost hollows
- Granitic gravel fields
- Granitic sand plains
- Inland outwash gravels
- Inland saline (salt pans)
- Inland sand dunes
- Limestone erosion pavements
- Old tephra (>500 years) plains (= frost flats)
- Recent lava flows
- Sandstone erosion pavements
- Screes of acidic rocks
- Strongly leached terraces and plains
- Ultrabasic boulderfields
- Ultrabasic cliffs, scarps and tors
- Ultrabasic hills
- Ultrabasic screes
- Volcanic boulderfields
- Volcanic debris flows or lahars
- Volcanic dunes
- Young tephra plains and hillslopes
Acidic rocks range from soft mudstones to indurated greywacke sandstones, plutonic rocks such as granite, and rhyolite. They are relatively infertile compared with basic and calcareous rocks. Cliffs and scarps are steep faces on hill slopes and ridges and dropping to valleys, whereas tors are steep-sided upstanding outcrops sitting atop other landforms such as ridges. They occur over a wide altitudinal range from the lowlands to the alpine zone. They provide habitats ranging from bare rock holding little moisture in highly exposed situations and colonised only by mosses and lichens, to deeper moist soils in heavily shaded and sheltered habitats supporting taller plants, including trees and shrubs where these can maintain a foothold. Hebes, epacrids and other heath-like shrubs and flax often predominate in the subalpine zone, with specialised herbs at higher altitudes. Native species that have been lost from neighbouring habitats because of animal browse find refuge on cliffs, scarps and tors.
Notable flora and fauna
Compared with more fertile rock types the number of threatened species on these landforms is few, although they are often highly specialised and include nationally critical plants (e.g. Pachycladon stellatum, pink broom (Carmichaelia carmichaeliae), Waitaki broom (C. curta), Canterbury pink broom (C. torulosa), and Kawarau cress (Lepidium sisymbrioides). Cypress hebe (Veronica cupressoides) and Pachycladon cheesemanii are nationally endangered. Many species in these habitats are nationally vulnerable or naturally uncommon, including two species of eidelweiss (Leucogenes neglecta and L. tarahaoa), a Marlborough rock daisy (Pachystegia minor), fierce lancewood (Pseudopanax ferox), and slender coral broom (Carmichaelia crassicaulis subsp. racemosa).
The nationally vulnerable black-eyed gecko (Mokopirirakau kahutarae) occurs on the eastern Marlborough Mountains. The alpine scree weta (Deinacrida connectens) can also be found on cliffs. The rare and nationally endangerd rock wren (Xenicus gilviventris) commonly nests on cliffs as does the endangered kea (Nestor notabilis). Landscapes on the West Coast with these steep features are habitats for several endangered snails (Powelliphanta spp.) although these animals are found on a wider range of slopes.
Not threatened (Holdaway et al. 2012)
Communities on cliffs scarps and tors of acidic rocks at lower altitudes are vulnerable to competition from exotic weeds, especially gorse (Ulex europaeus) and broom (Cytisus scoparius). Cotoneaster spp. are also spreading into these habitats. However, as these are generally infertile, the number of invasive species is limited. Rock climbing can have an impact on some cliffs and outcrops. Browsing impacts from goats, deer, possums and rodents are likely to be present in some sites. Cliffs and outcrops are largely naturally sparse and erosion would have always been part of their landscape dynamics.
Where do they occur?
Cliffs, scarps and tors of acidic rock occur throughout the New Zealand mountains including the volcanic mountains of the central North Island. They are particularly common along the Main Divide in the South Island.
Mark AF 1977. Vegetation of Mount Aspiring National Park, New Zealand. Wellington, National Parks Authority.
Summerville P, Mark AF, Wilson JB 1982. Plant succession on moraines of the upper Dart Valley, southern South Island, New Zealand. New Zealand Journal of Botany 20: 227-244.
Trewick SA 2001. Scree weta phylogeography: Surviving glaciation and implications for Pleistocene biogeography in New Zealand. New Zealand Journal of Zoology 28: 291-298.
Wardle P 1979. Plants and landscape in Westland National Park. National Parks Science Series No. 3. Wellington, Department of Lands and Survey.
Williams PA 1993. The subalpine and alpine vegetation on the Central Sedimentary belt of Paleozoic rocks in north-west Nelson, New Zealand. New Zealand Journal of Botany 31: 65-90.
Wilson HD 1976. Vegetation of Mount Cook National Park, New Zealand. Wellington, Lands and Survey Department.
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