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1929 Murchison earthquake

1929 Murchison earthquake
1929 Murchison earthquake is located in New Zealand
1929 Murchison earthquake
Date 17 June 1929 (1929-06-17)
Magnitude Ms 7.8
Depth 12km
Epicenter [1]
Areas affected South Island New Zealand
Casualties 17

The 1929 Murchison earthquake occurred at 10:17 AM on 17 June. It struck the Murchison region of the South Island, with an estimated magnitude of 7.8, and was felt throughout New Zealand. There were 17 casualties, mostly as a result of landslides triggered by the earthquake. The rumbling sound of the earthquake was loud enough to be heard at New Plymouth, more than 250 km away.[2]

Contents

  • Tectonic setting 1
  • Damage 2
  • Characteristics 3
  • Aftermath 4
  • See also 5
  • References 6
  • External links 7

Tectonic setting

Major active fault zones of New Zealand showing variation in displacement vector of Pacific Plate relative to Australian Plate along the boundary

New Zealand sits astride the boundary between the

  • Landslide blog about the earthquake by Professor Dave Petley, Durham University, UK

External links

  1. ^ a b c d GeoNet (17 June 1929). "M 7.8, Buller (Murchison),". Archived from the original on 4 June 2010. Retrieved 28 June 2010. 
  2. ^ a b c d e McSaveney, E. (2 March 2009). "The 1929 Arthur’s Pass and Murchison earthquakes". Te Ara - the Encyclopedia of New Zealand. Retrieved 28 June 2010. 
  3. ^ West Coast Regional Council (2002). "Earthquake Hazards". Archived from the original on 25 May 2010. Retrieved 28 June 2010. 

References

See also

The landslides blocked many roads causing food supplies to run out in some areas near the epicenter. This and the risk from aftershocks and flooding from the landslides blocking rivers caused many residents to evacuate the area, mostly on foot. Karamea was completely cut off and received no outside help for two weeks, until a de Havilland Tiger Moth plane landed on the beach. Some of the blocked roads took months to clear.[2]

Aftermath

The earthquake was preceded by several foreshocks before the mainshock, accompanied by booming sounds in the mountains around Murchison.[2] There was a large surface fault rupture visible in the Buller River, indicating about 4.5 m of vertical movement and 2.5 m of lateral movement. The earthquake triggered many landslides and these created 38 new lakes, of which 21 still exist, including Lake Stanley, on Stanley River.[1] The earthquake was accompanied by unusually loud rumbling noises that were heard as far away as New Plymouth. A maximum intensity of X on the Mercalli scale has been estimated for Murchison. Most of the northern part of South Island suffered an intensity of VII or greater.[2]

Characteristics

Although the epicenter was in a sparsely populated area about 65 km north of Murchison, the shaking in the surrounding region was sufficiently intense to cause damage over a wide area. The towns of Nelson, Greymouth and Westport were all affected and roads, buildings and bridges were severely damaged throughout an area estimated at 26,000 km2.[1] The worst damage was caused by landslides triggered by the shaking, destroying several homes and killing 14 out of the 17 that died in the earthquake. Most of the buildings in the Murchison area were built of wood and were warped and moved from their piles, but many brick buildings and chimneys were damaged in Nelson, Greymouth and Westport.[2]

Damage

[1]

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