| 22:50 NZST|
| 7.1 ML|
| 9 March 1929 (1929-03-09)|
South Island New Zealand
1929 Arthur's Pass earthquake Wikipedia
New Zealand lies along the boundary between the Australian and Pacific plates. In the South Island most of the relative displacement between these plates is taken up along a single dextral (right lateral) strike-slip fault with a major reverse component, the Alpine Fault. In the North Island the displacement is mainly taken up along the Kermadec-Tonga subduction zone, although the remaining dextral strike-slip component is accommodated by the North Island Fault System. The Poulter Fault runs for approximately 50 km Northeast from the junction of the Bealey and Mahinga rivers to the valley of the Hurunui River. Between 16 km and 36 km of the fault ruptured, with dextral displacement of up to 4 metres and dip-slip displacement of 1–2 metres (North side up).
Numerous landslides were triggered, damaging the Midland Railway and blocking roads. The highway connecting Canterbury and the West Coast via Arthur's Pass was closed for several months. Many water tanks and chimneys were damaged or toppled. Two years after the earthquake, trampers in the Otahake Valley discovered that a 900m high section of the side of a mountain had collapsed, blocking the valley and sending debris 5 km downstream.
Although (as of 2009) this is one of the ten largest land-based earthquakes to strike New Zealand since European settlement, it was overshadowed by the more deadly 1929 Murchison earthquake a few months later.