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HISTORY |
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THE RESERVE In the late 19th Century, people in the Rotorua community, Maori and European, became increasingly concerned at the loss of native forest on Mount Ngongotaha. In the early 1900s, the Scenery Preservation Commission recommended the acquisition of a large area of bush as reserve. After much discussion, a reserve of 480 acres around the summit was created in 1916.
In 1918, the Rotorua Chamber of Commerce wrote to the Government advising that “The Rotorua Chamber of Commerce, having heard that Mr. Stead is negotiating for the sale of his property on Mount Ngongotaha, deems it their duty to urge upon the Government the absolute necessity of acquiring the land as a scenic reserve.” As a result, 250 acres was added to the reserve. Various pieces of land were later acquired by negotiation or exchange and added to the reserves. The total area of the Mount Ngongotaha Scenic Reserve is now 524 hectares. (SEE MAP BELOW) |
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JUBILEE TRACK
Prior to 1890, local residents had
been asking the government for foot and horse access to the top of
the mountain to enjoy the view. Eventually, locals took matters
into their own hands and with “axes, tomahawks and billhooks”
completed a “very respectable” track in about 4 hours. The following
is from the Bay Of Plenty Times of 3 Feb 1890. “On this Day (Jubilee Day, 29 January 1890) a number of our stalwart members of society, horny handed sons of the soil, formed themselves into a working bee and cut a track to the top of Ngongotaha.” The Jubilee Track today follows much the same route as the original except for changes of access and some minor diversions that make it less steep. |
GEOLOGY Mount Ngongotaha, at 757 m asl (450 m from base to summit), is the largest of several rhyolitic dome volcanoes in the Rotorua volcanic centre. Others are Mokoia Island, Kawaha and Hinemoa Points, and Pukeroa , or “Hospital Hill”. The main feature of this centre is the Rotorua caldera (or Rotorua basin), a 15 km-wide crater occupied by the present lake. Formerly thought to be the result of a single titanic outburst, the basin is now considered to be the result of several eruptions, the earliest of which occurred in the vicinity of Mount Ngongotaha. There has not always been a lake in the basin. Indeed, for most of its history it has been a dry valley, with a small pool (draining underground) towards its centre. On the other hand, on at least six occasions the lake level has been over 50 m above its present level, including a period about 180,000 years ago when it was about 150 m above its present level, making Mount Ngongotaha an island. During the last Ice Age from 25,000 to 28,000 years ago, the harsh weather conditions completely stripped the summit of Mount Ngongotaha above 500 m of all loose soil.
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