The 1835 Auckland earthquake was a magnitude 6.5 earthquake that occurred sometime during 1835 in the Auckland region of New Zealand.[1] The earthquake was caused by movement along the Wairoa North Fault, which runs through the area.[4][5] At the time, the settlement of Auckland was still quite small, and there are limited records of the specific damage caused by the earthquake. However, historical accounts suggest that the earthquake caused significant shaking and rumbling in the area, and it is possible that some buildings or structures may have been damaged or collapsed. Despite this, there are no records of major damage or casualties resulting from the earthquake. The 1835 Auckland earthquake remains an important event in the region's history, particularly as it highlights the seismic activity that can occur in the area due to the presence of faults such as the Wairoa North Fault.[6]
^ abc"GeoNet Quake – Magnitude 6.5, Thu Jan 1 1835 11:39 AM". GNS Science. Retrieved 14 April 2023.
^"GeoNet Technical – Magnitude 6.5, Thu Jan 1 1835 11:39 AM". GNS Science. Retrieved 14 April 2023.
^Eiby, G.A. (1968). "A descriptive catalogue of New Zealand earthquakes: Part I—Shocks Felt before the end of 1845". New Zealand Journal of Geology and Geophysics. 11 (1). Bibcode:1968NZJGG..11...16E. doi:10.1080/00288306.1968.10423671.
^Daly, Michael (26 December 2020). "Auckland, Hamilton, Tauranga vulnerable to earthquakes in Hunua Ranges, Hauraki Plains". Stuff. Retrieved 14 April 2023.
^Fellows, D.L. (September 1996). "Preliminary Paleoseismic Assessment of the Wairoa North fault". ARC Environment. ISSN 1172-6415. Retrieved 14 April 2023 – via Auckland Engineering Lifelines Group.
^Hull, A.G.; Mansergh, G.D.; Townsend, T.D.; Stagpoole, V (March 1995). "Earthquake hazards in the Auckland region". Institute of Geological and Nuclear Sciences. Retrieved 14 April 2023 – via Auckland Engineering Lifelines Group.
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