New Zealand Journal of Geology and Geophysics abstracts
Surface rupture of the Poulter Fault in the 1929 March 9 Arthur's Pass
earthquake, and redefinition of the Kakapo Fault, New Zealand
Kelvin Berryman
Pilar Villamor
Institute of Geological & Nuclear Sciences Ltd
P.O. Box 30 368
Lower Hutt, New Zealand
email: k.berryman@gns.cri.nz
Abstract The 1929 March 9 Arthur’s Pass earthquake of
MS 7.1 occurred on a newly mapped fault in the Arthur’s
Pass region, which we name the Poulter Fault. Surface rupture of at least
16 km and possibly as much as 36 km occurred with 4 m of dextral displacement
at one site. The extent of fault rupture coincides very closely with a narrow,
elongate zone of intense landsliding. A best estimate of the dip-slip component
of faulting is 1–2 m (north side up), making the 1929 rupture a dextral to
oblique-dextral fault displacement, in keeping with earthquake first motion
studies. The Poulter Fault is mapped from the South Hurunui River in a WSW
direction to Williams Saddle near the confluence of the Mingha and Edwards
Rivers, a distance of nearly 50 km. The 1929 earthquake was not on the Kakapo
Fault as previously proposed by Yang. No active fault has been found along
the line proposed by Yang, and the Kakapo Fault is here redefined as the
southern element of a rhomboid fault wedge formed with the Hope Fault between
Kakapo Brook and MacKenzie Stream in the upper Hurunui valley.
Keywords earthquake geology; active fault; 1929 Arthur’s
Pass earthquake; Poulter Fault; Kakapo Fault; NZMS 260 toposheets K33, L32,
L33
G03018; Received 27 June 2003; accepted
20 January 2004; online publication date 20 May 2004
New Zealand Journal of Geology & Geophysics, 2004, Vol. 47: 341–351
0028–8306/04/4702–0341 © The Royal Society of New Zealand 2004
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