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Kōrero: Landslides

Regolith landslides

Image
Regolith landslides

Regolith landslides, which involve the upper soil layer, occurred during the heavy rainfall that struck the Manawatū in February 2004. As water enters soil particles it increases their weight, and when the ground is fully saturated the water pressure begins to force the particles apart. This makes soil much more likely to slip. Compare the area of steep pasture with the scrub-covered gullies (upper right), where protective vegetation reduced the number of slips.

Te whakamahi i tēnei tūemi

GNS Science

by Graham Hancox

Permission of GNS Science must be obtained before any use of this image.

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Me pēnei te tohu i te whārang

Michael J. Crozier, Landslides – Hill country, regolith and submarine landslides, Te Ara – the Encyclopedia of New Zealand, https://teara.govt.nz/mi/photograph/8794/regolith-landslides (accessed 25 June 2026).

He kōrero nā Michael J. Crozier, i tāngia i te 2 March 2009, updated 19 February 2026.