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・ 1929 AAA Championship Car season
・ 1929 Aciéries d'Angleur Tournoi
・ 1929 Alabama Crimson Tide football team
・ 1929 All England Badminton Championships
・ 1929 All-Big Six Conference football team
・ 1929 All-Big Ten Conference football team
・ 1929 All-Ireland Minor Hurling Championship
・ 1929 All-Ireland Senior Football Championship
・ 1929 All-Ireland Senior Football Championship Final
・ 1929 All-Ireland Senior Hurling Championship
・ 1929 All-Ireland Senior Hurling Championship Final
・ 1929 All-Pacific Coast football team
・ 1929 Allan Cup
・ 1929 Arkansas Razorbacks football team
・ 1929 Army Cadets football team
1929 Arthur's Pass earthquake
・ 1929 Atlantic hurricane season
・ 1929 Australian Championships
・ 1929 Australian Championships – Men's Singles
・ 1929 Australian Championships – Women's Singles
・ 1929 Australian Grand Prix
・ 1929 Australian timber workers' strike
・ 1929 Bahamas hurricane
・ 1929 Baltic Cup
・ 1929 Barcelona International Exposition
・ 1929 Birthday Honours
・ 1929 Boston Braves season
・ 1929 Boston Bulldogs season
・ 1929 Boston College Eagles football team
・ 1929 Boston Red Sox season


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1929 Arthur's Pass earthquake : ウィキペディア英語版
1929 Arthur's Pass earthquake

The 1929 Arthur's Pass earthquake occurred at on 9 March. The sparsely settled region of the Southern Alps shook for four minutes. Tremors continued almost continuously until midnight and sporadic strong aftershocks were felt for several days.
The earthquake was measured at 7.1 on the Richter Scale and the intensity of shaking in the epicentral region has been assessed from historical records as VIII (''Severe'') on the Modified Mercalli Scale. Intensities of VI (''Strong'') were observed in Christchurch and Westport.〔 The earthquake occurred on the Poulter Fault, which was not identified and mapped until 2001.
==Tectonic setting==
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.〔(Mouslopoulou,V., Nicol,A., Little, T.A. & Walsh, J.J. 2007. Terminations of large strike-slip faults: an alternative model from New Zealand. In: Cunningham, W. D. & Mann, P (eds).Tectonics of Strike-Slip Restraining and Releasing Bends. Geological Society of London, Special Publication, 290; p. 387-415. )〕 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).

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