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Valentine's Day Wellington Speed Dating 40 Plus - Wellington - Eventfinda
Was quick and easy and I was provided with a recommendation for the best plan and option for me. The website also has a filter so you can narrow down your choices to what you want. Highly recommended! Gillian perfectly matched our riding abilities to her horses, the trek involved a road ride down to the beach.
Beach Front & Sea Views - InterVille
The horses are safe and quiet and used to this, the drivers very polite and reducing their speed. You'll pass some cute beach houses as you get near, once on the beach there is a stunning view of Kapiti Island.
We were lucky to be there during the late afternoon during low tide, Gillian took some fantastic photos which she sahres on Facebook's. As a rider with some experience I was given the opportunity to go faster, and was able to have a gallop on along the shoreline.
Would definitely recommend to visitors and locals, lots of fun and beautiful scenery ….
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Read more. Date of experience: July Gillian H wrote a review Oct New Zealand 9 contributions. Best horses. The horses are so calm and safe and the trekking is stunning with ocean and mountain views to die for.
Date of experience: October Helpful Share. The discovery in that the beds of numerous rivers in the South Island contained extensive deposits of alluvial gold was of considerable importance in the economic development of the country. Not only did it lead to an increase in population and in wealth, but, through the following of the numerous streams to their sources, it also led to the rapid exploration of large tracts of remote country. The exploitation of these deposits has been carried on with varying degrees of success up to the present time by both manual and mechanical means.
A further factor in connection with the rivers is that, owing to the very successful acclimatization of fresh-water fish, notably trout, many of them now provide exceptionally fine fishing. Surrounded by extremely rugged country the larger lakes of the South Island are distinguished by the grandeur of their alpine settings, while those of the North Island, situated on a volcanic plateau, are of interest by reason of the neighbouring thermal activity. Owing to the excellence of their fishing, the North Island lakes possess an added tourist attraction.
In both Islands the larger lakes are situated at high altitudes, and their consequent remoteness renders them unsuitable as a means of communication. In their functions as reservoirs the lakes of both Islands are of vital importance for the maintenance of the streams draining them and as a means of flood-prevention. More especially is this the case where hydro-electric schemes are involved.
Tekapo, Wanaka, Hawea, and Wakatipu in the South Island, being of particular significance in this respect. An article on the lakes of New Zealand will be found in the Year-Book. Some particulars of the more important are given in the following table.
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Henderson, M. The information given below has been supplied by Mr. Hayes, Director of the Seismological Observatory. Seismicity and Earthquake Distribution. However, this is due to the occurrence of a large number of earthquakes of the semi-destructive type R. During the period —, 73 destructive earthquakes are known to have occurred in New Zealand, 53 of which were of the semi-destructive type not exceeding intensity R.
Of the remainder, 14 were of intensity 9, and 6 of intensity The total number of earthquakes of all intensities, and the maximum intensity, reported felt in New Zealand in each of the years to were as follows: —. The abnormally large number of earthquakes reported in the year was due to the swarm of local shocks in the Taupo region in the latter half of that year. Abnormally large numbers of shocks also occurred in —30, due to aftershocks of the Buller earthquake of 17th June, Summary of Seismic Activity in New Zealand in The largest disturbance occurred on 23rd May in the Hanmer-Waiau region when intensity M.
VIII was reached in the strongest shock. Some buildings in the epicentral region suffered structural damage. Minor activity continued at intervals for some months. Other strong shocks occurred on 15th January off the Manawatu coast, on 19th June off the west coast of the South Island, and in July in the Monowai region. The first two of these shocks were; widely felt. There was some concentration of minor activity in the Taupo region early in the year and occasionally in the Wanganui region. On 26th January a slight shock was felt at some localities around the Kaipara Harbour.
There were earthquakes reported felt during the year, 81 being in the North Island, 53 in the South island, and 7 in both Islands. The maximum intensities reported were M. VI in the North Island and M. The highest intensities in this shock affected the Taihape-Wanganui area. It was perceptible from Tolaga Bay to South Canterbury. Although thy remainder of the year was comparatively quiet, a shock of intensity M.
A certain amount of activity persisted in the latter region throughout the year. Intensity M. V was experienced at Karamea on 23rd December. On 27th June a shock in the White Island region occurred at a depth of km. This depth is second only to that of a shock in the same region on 27th June, , at a depth of km.
Outside the main seismic zone, minor activity occurred in the following regions—Great Barrier Island, Ruawai Northland , Paeroa, and Raglan. Shocks located in unusual regions occurred on 14th April and 27th May from to miles east of Christchurch, and on 16th September, west of Cape Egmont. In all, 97 shocks were reported felt during the year, 71 in the North Island, 34 in the South Island, and 8 in both Islands. The maximum intensity reported in both Islands was M. Regional Distribution. By combining early earthquake records with the more precise data of recent years it is possible to divide the country roughly into four seismic regions.
These regions are classified below, in order of seismicity.