Quake activity not 'unusual'
Articles, TV3
The chance of a magnitude 5 earthquake in Christchurch in the next year is just over 50 percent, according to a new forecast.
The chance of a magnitude 5 earthquake in Christchurch in the next year is just over 50 percent, according to a new forecast.
A report covering the effects of seismic activity upon inaka (whitebait) spawning grounds on city rivers.
An update on trout spawning in the Avon River and notes on the effects of seismic activity on physical habitat
It is midday on the busy intersection of Manchester, High and Lichfield Streets when this photograph was taken from the corner of Bedford Row c. 1904. The street is full of activity as shoppers mak…
Cobb & Co.’s booking office on the corner of Cashel and High Streets was a hub of activity. Here the proprietor, W. R. Mitchell took charge of the bookings and service on this site since…
As archaeologists we almost exclusively describe and interpret the physical evidence of past human activity in visual terms, through maps, photos, and descriptions of what the archaeological features or artefacts look like. Although this makes perfect sense, lately I’ve come … Continue read...
A Gap Filler submission to the Christchurch City Council Draft City Plan requesting the permission to be heard at the public hearing with regards to changes to temporary activities and buildings.
This report provides information on the locations and character of active geological faults and folds in Ashburton District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of permanent fault movement at the ground surface, and where more detailed investigations should be done if development is proposed in that area (depending on the potential activity of the fault and the type of development proposed). See Object Overview for background and usage information. Most of the faults and folds identified at the ground surface in Ashburton District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region.
This report provides information on the locations and character of active geological faults and folds in Mackenzie District. The faults are mapped at a district scale and the information is intended to highlight areas where there is a risk of fault movement, and where more detailed investigations should be done if development is proposed in that area(depending on the potential activity of the fault and the type of development proposed). Most of the faults and folds identified at the ground surface in Mackenzie District are in rural or very sparsely populated areas. In addition, most of the faults have relatively long recurrence intervals (long-term average time between fault movements) in the order of several thousand years. Following the Ministry for the Environment Active Fault Guidelines, normal residential development would be allowed on or near faults with recurrence intervals this long. There are no recommendations associated with this report. The information in the report will be reviewed as required, after the remaining district reports are completed in the region. See Object Overview for background and usage information.