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The oldest of these strata are the Eocene coal measures of the Waikato region. Upper Cretaceous strata, mainly mudstones, are the most widespread of the younger rocks of North Auckland. Young volcanic rocks are widespread in the North Island. This is one of the largest and youngest accumulations of acid volcanic rocks in the world.
Most of it has been erupted in late Pliocene and Pleistocene times. The belt of most recent activity in the Central Volcanic District is known as the Taupo Volcanic Zone; it contains all this country's active volcanoes, many inactive ones, and all the geysers and boiling springs. Mount Egmont is a huge, conical, andesite volcano, with the remnants of two other volcanic cones nearby; all are of Pleistocene age. In the Waikato there are eroded Pleistocene cones of approximately basic andesite composition. The largest is Pirongia, some 3, ft high. Auckland city and the area immediately to the south has been the scene of many eruptions of basalt lava and scoria in late Pleistocene and Holocene times; and many small scoria cones can be seen in the locality.
Late Tertiary and Quaternary basaltic eruptions in North Auckland have built lava plateaus and many young cones.
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New Zealand Geological Survey Bulletin 66, The Geological Map of New Zealand, ,, , is a lengthier summary with a more detailed geological map and cross sections. Such disturbed regions, of which New Zealand is one, are evidently the site of some kind of development affecting the outer shell of the Earth.
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Little is yet known about the internal processes that give rise to these geophysical disturbances, nor are the relations connecting them fully understood. Formerly earthquakes were believed to be caused by volcanic activity, but it is now recognised that volcanic earthquakes are restricted to small shocks in the immediate vicinity of the volcanism.
In New Zealand, tremors of this kind are experienced in the zone of active volcanism that extends from Mount Ruapehu to White Island. In some places geological faulting at the surface gives visible evidence that a major earth movement has occurred. Occasionally movement on a fault has been observed to occur simultaneously with an earthquake in the same vicinity. New Zealand provided one of the earliest examples of this to become generally known, when movement took place on the Wairarapa Fault at the time of the great Wellington earthquake of Such events as this have led to the idea that earthquakes in general are caused by fault movements, but it has proved difficult to find convincing evidence in support of this theory.
It is noteworthy that there seems to be little earthquake activity along much of the Alpine Fault, which has been traced for miles from Milford Sound to Lake Rotoiti and is classed by geologists as one of the largest and most active faults in the world. The nature of the connection between earthquakes and faulting is still somewhat obscure.
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The great majority of the world's earthquakes occur at depths of less than 40 miles, and in many earthquake zones there are no shocks at any greater depth. A moderate number of New Zealand earthquakes are classed as intermediate in depth, i. The two deepest New Zealand earthquakes recorded so far occurred four and a half minutes apart on 23 March , with a common focus miles deep under North Taranaki, about 80 miles shallower than the deepest earthquake known.
It is difficult to compare the degree of earthquake activity in New Zealand with that in other regions because of the many differences that arise in earthquake type and mode of occurrence. New Zealand and California are often regarded as roughly similar, with an activity very much less than, for example, Japan or Chile. Regional Distribution —There are two separate regions of earthquake activity in New Zealand.
It thus includes the northern half of the South Island, and all the North Island apart from the North Auckland peninsula; but the area from Kaipara Harbour to the lower Waikato River should be excluded. Earthquakes have only occasionally been located in the parts of New Zealand lying outside these two regions.
Within the active regions the occurrence of shallow earthquakes is widely scattered. There has been a tendency, however, for the larger shallow earthquakes to lie towards the Pacific side of the northern active region and towards the Tasman side of the southern active region. Earthquakes with deeper foci are mostly confined to a narrow belt in the northern region, extending from the Bay of Plenty south-westwards to Tasman Bay. The historical record is too brief to support a quantitative assessment of the frequency with which one might expect earthquakes to be felt at a given intensity in various parts of New Zealand.
Considering the distances to which major earthquakes can be effective, in relation to the size of New Zealand, it would be imprudent to regard any part of the country as permanently exempt from the possibility of earthquake damage. Outside the active regions there are many areas, however, where no damaging intensity has actually been experienced in historical times. Moreover, since the major shallow earthquakes on record have been rather widely distributed within the active regions, there appears to be no particular area of markedly intense seismicity.
The Hawke's Bay earthquake of 3 February resulted directly or indirectly in deaths. The total of deaths that have been recorded as due to other earthquakes since is 32, of which three resulted from the Inangahua earthquake of The installations at the following stations include instruments for recording distant earthquakes: Afiamalu, Rarotonga, Wellington, Roxburgh and Scott Base. At the Pacific and Antarctic stations preliminary readings are made locally and notified by radiogram. The analysis of records from all stations is carried out at the Observatory in Wellington.
The analysis involves using observations from stations in other countries as well as those from the local network, and the Observatory likewise contributes data to the international seismological agencies about distant earthquakes as well as large local ones. Details of tremors felt in New Zealand are supplied to the public and the press. Earthquake data are used by the Observatory for studying the fundamental characteristics of the Earth's crust in New Zealand, Antarctica and the neighbouring oceanic regions, and also for contributing to geophysical knowledge of the Earth's interior.
Earthquakes during —Earthquakes did not cause any appreciable damage in The most noteworthy event was the swarm of small earthquakes, centred near Puru in the Coromandel Peninsula, that began in August and persisted for more than a month. There were several hundred shocks, many of which were felt in the immediate vicinity of the epicentres, and were responsible for minor damage to goods and a few weak structures.
A magnitude 5. Other shocks of magnitude 5 or more occurred near Pahiatua on February 14, and in Fiordland on 15 September.
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On 23 November small shocks were reported from Timaru and Oamaru. By arrangement with the administrations concerned the Service performs similar functions for British territories in the Pacific. Weather reports for use in forecasting are made at about places within New Zealand and 50 in Pacific islands and collected by telegraph and radio, along with measurements of winds at upper levels made at nine radio wind stations and of temperatures made at eight radiosonde stations.
Daily observations are made for climatological purposes at about places in New Zealand and 80 in the islands. Rainfall measurements are made at a total of about 2, places within New Zealand and outside the country. The weather pattern from day to day is dominated by a succession of anticyclones, separated by troughs of low pressure, which pass more or less regularly from west to east across the Australia - Tasman Sea - New Zealand area and beyond. In this region there is no semi-permanent anti-cyclone such as those found in similar latitudes over the Indian Ocean and eastern Pacific Ocean respectively.
The troughs normally have a northwest to southwest orientation and are associated with deep depressions centred far to the south.