Waihi Fault Zone

Source: Wikipedia, the free encyclopedia.

Waihi fault zone
Waihi North fault, Waihi South fault
Age
Miocene-Holocene
Volcanic arc/beltTaupō Volcanic Zone
New Zealand geology database (includes faults)

The Waihi Fault Zone is a seismically active area of the central North Island of New Zealand whose earthquakes have been associated with significant loss of life.

Geology

The intra-rift Waihi Fault Zone extends at least 38 kilometres (24 mi) from Little Waihi at Lake Taupō towards

Poutu fault zone to the east, by about 10 kilometres (6.2 mi), is parallel to the Waihi fault.[3] The active Taurewa and Rotopounamu faults that have been separately named by some are now assigned to the two fault zones.[2][4] To the west of the Waihi Fault Zone the National Park Fault is the current western wall fault for the modern Taupo rift.[4]

Risks

Large landslides have occurred in the Hipaua Steaming Cliffs area of the Waihi fault escarpment and it is likely that some the large historical loss of life by New Zealand standards from these landslides has been related to earthquake activity on the fault.[5]

References