On 30 November 2007 Bob realised an ambition and visited White Island on a field trip following the New Zealand Geological Society Conference in Tauranga.
White Island is regarded as the most active volcano in New Zealand and was continuously active between 1975 and 2000. At present activity is largely restricted to fumaroles and emission of volcanic gases
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| The colours and textures are striking with no sign of any life. The main outflow stream from the fumaroles and springs is chlorine rich and with a very low pH. Hence the rocks and soils rapidly corrode away creating an artists palette of colours | ||
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| Fresh magmatic bombs, lapilli and ash mantle the crater floor. The most recent of these date back to a Strombolian eruption in July 2000. Other deposits include bedded ash and scoria and mounds from a landslide (Lahar?) that occurred in 1914 | ||
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| At a smaller scale the colours and textures show the diversity that exists inside an active volcanic crater | ||
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| The current activity consists of fumaroles discharging steam and volcanic gases which include CO2, SO2 and H2S. The gases sting the eyes and and affect breathing requiring gas masks to be worn when the steam drifts towards you. The gases originate from a relatively shallow magma chamber under the crater floor. | ||
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| A crater lake occupies the site of the craters which were responsible for the latest eruption. The lake was rising steadily until increasing temperature in the last year saw much of the lake evaporate away. If the lake rise again it presents a particular hazard as it could overtop and rapidly erode the loose deposits in Donald Duck Crater (bottom right) unleashing a lahar down the crater floor | ||
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| The long history of the volcano can be read in the crater walls where horizontally bedded former crater deposits are interspersed with scoria and ash horizons. Lava flows are relatively rare in the recent history of the volcano | ||
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| Crater Bay is the site of a former Sulphur mining operation that continued in to the early years of the 20th century. In September 1914 a landslide in the crater wall produced a mudflow that overwhelmed workers in the crater floor. The eleven miners were never found. The current ruins relate to later attempts to mine the sulphur. | ||
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The old Sulphur factory is the site of one the Geonet Web Cams used to monitor the volcano activity. One of the worlds most famous dinosaurs, Dino is always in view in the foreground |
| The Island is not totally devoid of life. Pohutukawa forest clings to parts of the outer cone and Gannets and Red Billed gulls nest on the Island | ||
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In short it was a thoroughly enjoyable experience enjoyed by all (especially myself, right) and ably lead by by Brad Scott (below) and Mike Rosenberg | ![]() |
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