The Waikato region has many active fault lines that increase the chance of earthquakes. About 20 percent of the region’s population live on soils prone to movement during earthquakes. Our map shows where earthquake fault lines are in the Waikato region and which areas are most at risk. More information is available below the map.
Waikato Regional Council's regional Ground Shaking Risk Zones and Active Fault Lines’ map uses information provided by the Institute of Geological and Nuclear Sciences (GNS). It shows active faults in the Waikato region and the extent of the Taupo Volcanic Zone. The information is used in our Waikato region Lifelines Study. You can also download this map in PDF format [PDF, 1.1 MB] below.
Waikato Regional Council has classified and mapped geological materials into four units used to define hazard zones1:
1. Most hazardous
Materials formed less than 10,000 years ago (Holocene), such as :
These have high volcanic ash content, mixed with peat, clay, silt, ash, sand and gravel. They may include layers that are easily saturated with water and are liquefiable. The ground water table is generally very high in these areas.
Materials formed less than 2.5 million years ago (during the Quaternary period), made up of:
These include unsaturated, slightly weathered loose gravel, ash and sand.
Materials formed between 75 and 2.5 million years ago (during the Tertiary period), including:
These materials are weak to moderately strong, containing volcanic rocks of various ages. Gravel is usually dense to very dense. Fine grained rocks are particularly prone to slumping and landsliding, especially if saturated or without vegetation.
Basement rocks (more than 75 million years old) and greywacke (dark, coarse-grained sandstone), with hardened, well bedded, sandstones and siltstones (which are moderately to highly deformed), and minor schist. These materials are weak to very strong.
You can download this map from our PDF file below.
Earthquake Hazard Zones map
(1184 kb, 169 seconds to download, 56k modem)