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 screes
- Volcanic boulderfields
- Volcanic debris flows or lahars
- Volcanic dunes
- Young tephra plains and hillslopes
Hills refers here to the slopes, ridges, and summits rising above the surrounding country. Ultrabasic (also known as ultramafic) rocks contain very little quartz or feldspar and are composed essentially of ferromagnesium silicates, metal oxides, and native metals (Anon, 1962). They form soils with low concentrations of major nutrients and high concentrations of toxic metals such as nickel, chromium, and cobalt. These soil conditions result in vegetation that is often characterised by stunted, slow growing, small-leaved trees and shrubs. Plants characteristic of fertile soils can be present, but these sites also support ultrabasic endemics and ecotypes of widespread species. At low altitudes, the ultrabasic influence on vegetation can be obscured because of human burning resulting in manuka-dominated shrublands. These landscapes also have limited areas of ultrabasic boulderfields and ultrabasic screes. While the process is not unique to ultrabasic rocks, the oxidation of the ferromagnesium minerals in these rocks produces the red coloration after which the geographical features are named e.g. Red Hills.
Ultramafic hills, serpentine hills
Notable flora and fauna
Threatened plants include the nationally critical Chaerophyllum basicola, forget-me-nots (Myosotis laeta, Myosotis petiolata var. petiolata), and Notothlaspi (a) 'Red Hills' and the nationally endangered Carex uncifolia and Geranium 'Red Hills'. Naturally uncommon Carex devia, Carex traversii, Celmisia spedenii, Chionochloa defracta, Dracophyllum ophioliticum, Festuca ultramafica, Gentianella stellata, Veronica urvilleana, Leptinella pyrethrifolia var. linearifolia, Myosotis monroi, Pimelea suteri, Trisetum serpentinum, Poa acicularifolia subsp. ophitalis, Pittosporum pimeleoides subsp. majus, Wahlenbergia albomarginata subsp. olivina, Astelia aff. graminea 'Red Hills', Brachyscome aff. humilis 'West Dome', Cardamine 'West Dome', Colobanthus 'Red Hills', Colobanthus aff. wallii 'Serpentine', Craspedia 'Serpentine' and Craspedia ‘Hacket River'.
We have found no information on threatened and rare fauna specific to this ecosystem.
Not threatened (Holdaway et al. 2012)
Ultrabasic soils exclude the majority of species, including exotic weeds, but wilding pines, particularly lodgepole pine (Pinus contorta) and Douglas fir (Pseudotsuga menziesii), are very invasive. Hawkweeds (Hieracium spp.) and briar (Rosa rubiginosa) are of concern on the Red Hills Ridge. Deer and possums are widespread while goats and pigs are locally common in Nelson-Marlborough. Historically, some areas of serpentine were mined (e.g. Cobb Valley asbestos mine) but there are no mines currently in operation. In the 1970s and 1980s proposals to mine asbestos from the Red Hill Range in Southland generated much controversy and eventually led to the incorporation of this area into Mount Aspiring National Park. Ultramafic hills tend to be support open scrubland and grassland, which is susceptible to fire. Many sites have been burnt historically for grazing and are susceptible to further fires, especially in the drier areas of Nelson Marlborough. Ultramafic soils are unsuitable for agriculture but some near Red Hills Ridge have been planted in pines and this has increased the risk of fire.
Where do they occur?
Ultrabasic hills occur in Nelson-Marlborough (Red Hills Ridge on the Richmond Range, Bryant Range, D’Urville Island), South Westland (Red Hills Range) and inland Southland (Eyre and Livingstone Mountains).
Anon 1962. Dictionary of geological terms. National Academy of Sciences for the American Geological Institute, New York, Doubleday.
Dawson JW 1988. Serpentine Vegetation in Forest Vines to Snow Tussocks: The Story of New Zealand Plants. Victoria University Press, Wellington.
Lee WG 1992. New Zealand ultramafics. In: Roberts BA, Proctor J eds The ecology of areas with serpentinized rocks. A world view. The Netherlands, Kluwer. Pp. 375-418.
Wardle P 1991. Vegetation of New Zealand. Cambridge University Press. 672 p.
Wilson JB, Lee WG, Mark AF 1990. Species diversity in relation to ultramafic substrate and to altitude in southwestern New Zealand. Vegetatio 86: 15-20.
Matai Valley, Nelson (The Prow)
Rocks offset along the Alpine Fault (Te Ara Encyclopedia of New Zealand)
Ultramafic rock (Wikipedia)