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Landslide

A landslide is defined as a mass movement of rock, soil and vegetation down a slope.

Landslides occur when the slope strength is overwhelmed by stresses imposed on it. These stresses can be sudden such as an earthquake or a severe weather event, or they can build up over time with the slope gradually weakening until what might seem a relatively insignificant event causes it to fail.

Slope failure

slope failure diagram

1  The steeper the slope, the more unstable it will be. 

2  Plant roots hold the soil in place and the vegetation cover makes the soil surface more resistant to erosion. 

3  Lack of frictional resistance between surfaces that separate one layer of rock from another can cause slop instability. 

4  Earthquakes, hurricanes, volcanic eruptions, the passage of heavy trucks, blasting and other sudden shocks may trigger the rapid movement of soil in slopes. 

5  Cracks in the slope surface, or in the rock layers underneath, are vulnerable to disturbance or degradation. 

6  Different types of soil are more erosion prone than others. 

7  Excessive water and inadequate drainage: when heavy rain has saturated the soi, the earth becomes a lot heavier and prone to movement. 

Landslides in New Zealand

Compared to many other countries, New Zealand has a high number of landslides because:

  • Rocks are often weakened by geological folding and faulting
  • There are frequent earthquakes
  • Much of the land is hill country, formed by rivers cutting into soft clay rocks
  • Many soft and easily erosion prone slopes have been cleared of vegetation as a result of agriculture
  • Slopes can be unstable as a result of weak layers of volcanic ash and other fine windblown sediments.
  • Rainfall can be high and intense.

What does this mean for the Bay of Plenty region?

Bay of Plenty Regional Council has completed a region wide study to map landslide susceptibility for both seismic and extreme rainfall scenarios, particularly focusing on these urban areas:

  • Waihī Beach
  • Katikati
  • Te Puna
  • Paengaroa
  • Te Puke
  • Maketū
  • Kawerau
  • Rotorua
  • Ōpōtiki

This information will be used for natural hazards planning and to identify areas where further assessment will be required for new development. 

Where can I view these maps?

The Bay of Plenty regional landslide susceptibility maps are available on our mapping platform, BayHazards.

What do I do in a landslide?

For information on what to do in the event of a landslide, visit the Bay of Plenty Civil Defence website.