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
This ecosystem comprises non-volcanic dunes formed inland from river sand. As such, these dunes have never been influenced by coastal processes. Included here are only active or semi-active dunes with raw or recent soils with no well-developed soil horizons. Except for some planted exotic marram grass (Ammophila arenaria), inland dunes support no specialised sand-binders, being colonised by the same species that colonise riverbed sand, such as scabweeds (Raoulia spp.) and silver tussock (Poa cita) (see Fig. 6 in Watt 1979). Volcanic dunes are described separately.
Sand hills, may include sand plains
Notable flora and fauna
Critically endangered (Holdaway et al. 2012)
Most areas in Canterbury and Otago have been converted to agriculture or forestry; in the 1920s these ‘useless sand wastes’ were considered a ‘menace’ to adjacent fertile lands and were deliberately planted for stabilisation. Some locations have been destroyed by or are at risk due to hydro development. Exotic weeds are a major threat; pines (Pinus spp.) have invaded dunes adjacent to Lake Tekapo, while the Cromwell Chafer Beetle Reserve, where rabbit grazing has been severe, is now dominated by sweet vernal (Anthoxanthum odoratum), sheep’s sorrel (Rumex acetosella) and haresfoot trefoil (Trifolium arvense) (Ferreira & McKinlay, 2000). Human modification of the dynamics of braided rivers has also altered the capacity of rivers to supply sediment to adjacent land to form the dunes.
Where do they occur?
Inland sand dunes are best developed in the upper Clutha and upper Waitaki basins of Central and North Otago, and also in the Ashburton, Rakaia, Rangitata, and Waimakariri valleys of Canterbury. The large sand dunes at Mason’s Bay, Stewart Island, may also possibly qualify.
Cockayne L 1911. Report on the dune-areas of New Zealand, their geology, botany and reclamation. Wellington, Department of Lands. 76 p.
Ferreira SM, McKinlay B 2000. Recent vegetation trends at the Cromwell Chafer Beetle Nature Reserve in Central Otago, New Zealand. New Zealand Journal of Botany 38: 235-244.
Leamy ML, Saunders WMH 1967. Soils and land use in the Upper Clutha Valley, Otago. New Zealand Soil Bureau Bulletin 29. 110 p.
Wardle P 1991. Vegetation of New Zealand. Cambridge University Press. Pp. 360-361.
Watt JC 1979. Conservation of the Cromwell Chafer beetle, Prodontria lewisi (Coleoptera: Scarabaeidae). New Zealand Journal of Ecology 2: 22-29.
Inland dunes (Te Ara)