1848 Marlborough earthquake

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1848 Marlborough New Zealand
1848 Marlborough earthquake is located in New Zealand
1848 Marlborough earthquake
1848 Marlborough earthquake
Date 16 October 1848 (1848-10-16)
Magnitude Mw 7.5
Depth shallow
Epicenter 41°48′S 173°42′E / 41.800°S 173.700°E / -41.800; 173.700Coordinates: 41°48′S 173°42′E / 41.800°S 173.700°E / -41.800; 173.700
Areas affected New Zealand, Marlborough, South Island
Casualties 3 deaths

The 1848 Marlborough earthquake is the name associated with a severe earthquake which occurred at 1:40 a.m. on 16 October 1848 and whose epicenter was in the Marlborough region of the South Island of New Zealand.

In Wellington the shaking lasted for about two minutes and caused widespread damage, especially to brick- or stone- built structures. Most of the buildings damaged in the earthquake were rebuilt in wood and this contributed to the relatively low level of damage and loss of life in the more powerful Wairarapa earthquake that hit Wellington seven years later.[1]

Tectonic setting[edit]

Map of the Marlborough Fault System showing location of the Awatere Fault

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 subduction zone, although the remaining dextral strike-slip component of the relative plate motion is accommodated by the North Island Fault System (NIFS).[2] A group of dextral strike-slip structures, known as the Marlborough Fault System, transfer displacement between the mainly transform and convergent type plate boundaries in a complex zone at the northern end of South Island.[3] The earthquake occurred on the Awatere Fault which is part of the Marlborough Fault System.[4]

Earthquake characteristics[edit]

The earthquake was associated with the rupturing of a minimum of 105 km of the Awatere Fault.[4] A horizontal displacement of about 6 metres was accompanied by smaller vertical movements of varying sense. A shallow epicentral depth is inferred from the large number of felt aftershocks[5] A moment magnitude of about 7.5 has been estimated from the rupture length and measured displacements.[4][6]

Damage[edit]

In Wellington, almost all buildings of brick or stone construction were damaged, including homes, churches, the jail, and the colonial hospital.[7] Most wooden buildings were undamaged, although many lost their brick chimneys. In the Marlborough region itself, a number of homesteads were badly damaged. Several buildings damaged in the main shock were destroyed during strong aftershocks over the next few days. The only fatalities from the earthquake occurred when a damaged building collapsed during one of the aftershocks.[1]

See also[edit]

References[edit]

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