1901 Cheviot earthquake
Encyclopedia
The 1901 Cheviot earthquake occurred at 07:47 NZT on 16 November 1901 with an estimated magnitude of 6.9 centred near the township of Cheviot
Cheviot, New Zealand
Cheviot is a town in the Hurunui District of north Canterbury, on the east coast of the South Island of New Zealand. It is on the Main North Line railway and State Highway 1 approximately north of Christchurch. It was originally called Mackenzie after politician John McKenzie, who was closely...

 in the Canterbury Region of New Zealand
New Zealand
New Zealand is an island country in the south-western Pacific Ocean comprising two main landmasses and numerous smaller islands. The country is situated some east of Australia across the Tasman Sea, and roughly south of the Pacific island nations of New Caledonia, Fiji, and Tonga...

.

Damage & casualties

A baby was killed when a sod hut collapsed.Other casualties in the Canterbury region are not known.

Damage outside Cheviot

The ChristChurch Cathedral experienced some damage with this earthquake. The top of the spire fell again as a result of the 16 November 1901 Cheviot earthquake. This time, the stone construction was replaced with a more resilient structure of Australian hardwood sheathed with weathered copper sheeting, with an internal mass damper.

Observations of sand blows (sand volcano
Sand volcano
A sand volcano or sand blow is a cone of sand formed by the ejection of sand onto a surface from a central point. The sand builds up as a cone with slopes at the sand's angle of repose. A crater is commonly seen at the summit...

) and lateral spreading, consistent with soil liquefaction
Soil liquefaction
Soil liquefaction describes a phenomenon whereby a saturated soil substantially loses strength and stiffness in response to an applied stress, usually earthquake shaking or other sudden change in stress condition, causing it to behave like a liquid....

 phenomena in the township of Kaiapoi
Kaiapoi
Kaiapoi is a town in the Canterbury region of the South Island of New Zealand, located close to the mouth of the Waimakariri River, and approximately 17 kilometres north of Christchurch....

 were reported in local newspapers in a two to three block area at the eastern end of Charles and Sewell Streets on the north bank of the Kaiapoi River, in addition to similar effects observed on the opposing river bank, and the road to Belfast.

External links

The source of this article is wikipedia, the free encyclopedia.  The text of this article is licensed under the GFDL.
 
x
OK