Coastal Restoration Trust of New Zealand

Coastal Dune Ecosystem Reference Database

On the vegetation of the Westport district Technical Report

Author
Townson, W.
Year
1906
Volume
39
Pages
380-433
Keywords
Waverley Fault Zone, paleoseismic studies, earthquake hazard, normal faulting, Kawakawa Tephra, Taupo Volcanic Zone, Ngarino Terrace, Rapanui Terrace, Brunswick Terrace
Summary
The Waverley FaultZone, c. 40 km northwest of Wanganui, New Zealand, has clearly defined surface fault scarps trending southwest-northeast for a distance of c. 8 km, from Lake Oturi in the south through to the Brunswick Terrace strandline northeast of Waverley. Paleoseismic studies involving trenching were carried out to determine the timing of past earthquakes, the amount of surface displacement associated with them, and an estimation of associated earthquake magnitudes. The Waverley Fault Zone has been the site of several large, surface-rupturing events in the past. Trench excavations across the fault zone revealed that the zone consists of normal faults dipping 50-80
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