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Champagne Pool

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Journal Article
Published: 01 March 2005
Journal of the Geological Society (2005) 162 (2): 323–331.
...Vernon R. Phoenix; Robin W. Renaut; Brian Jones; F. Grant Ferris Abstract Siliceous sinter, loose sediments, and suspended flocs in Champagne Pool, an anoxic hot (75 °C) spring at Waiotapu, New Zealand, are composed of opaline silica and metal-rich sulphides that contain many well-preserved...
FIGURES | View All (9)
Journal Article
Published: 01 November 2001
Journal of the Geological Society (2001) 158 (6): 895–911.
...BRIAN JONES; ROBIN W. RENAUT; MICHAEL R. ROSEN Abstract Champagne Pool, a large hot spring at Waiotapu in North Island, New Zealand, is rimmed by a subaerial sinter dam and a shallow subaqueous shelf that is composed of orange sinter rich in metallic sulphides. Orange siliceous flocs, also rich...
FIGURES | View All (11)
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Macroscopic features of <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>, Waiotapu. (A) Western <span class="search-highlight">pool</span> margin s...
Published: 26 November 2003
Fig. 5. Macroscopic features of Champagne Pool, Waiotapu. (A) Western pool margin showing raised ledge (∼ 30 cm above water surface) overhanging pool edge (L). At the current water level there is extensive growth of spicular microstromatolites (S). The orange sinter shelf (Sh) is visible below
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Oblique aerial view to the south-southeast over the <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span> area of ...
Published: 01 May 2022
Fig. 12. Oblique aerial view to the south-southeast over the Champagne Pool area of the Waiotapu geothermal system, New Zealand (Google Earth image, August 22, 2010). Champagne Pool discharges at ~72°–75°C from a 900- to 700-yr-old hydrothermal eruption crater; surface discharge cools from ~160°C
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( A ) <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span> and Artist’s Palette, Waiotapu geothermal system (New ...
Published: 01 December 2020
Figure 4. ( A ) Champagne Pool and Artist’s Palette, Waiotapu geothermal system (New Zealand). The distinctive orange sulfur precipitates contain high concentrations of heavy metals, including As, Sb (giving the characteristic orange colour), Au, Ag, Hg, and Tl (Mountain et al. 2003). P hoto : M
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Photograph of Waiotapu, looking SE. <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>, a hydrothermal eruption...
Published: 22 August 2019
Fig. 5. Photograph of Waiotapu, looking SE. Champagne Pool, a hydrothermal eruption vent formed 900 years ago, is in the centre, with a surrounding sinter sheet extending left and collapse craters induced by hydrothermal alteration in the right foreground. The steaming pool ( c . 260°C) is c
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<span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>, New Zealand. The colourful colloids of S, As and Sb serve t...
Published: 01 April 2014
Figure 3.2 Champagne Pool, New Zealand. The colourful colloids of S, As and Sb serve to demonstrate that, although much of the geothermal water originated as local rainfall, the high concentrations of many other elements require a magmatic origin.
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Location and setting of <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>. ( a ) Location of Taupo Volcanic Zo...
Published: 01 March 2005
Fig. 1.  Location and setting of Champagne Pool. ( a ) Location of Taupo Volcanic Zone (inset) and Waiotapu, North Island, New Zealand. ( b ) Sketch plan of Champagne Pool showing sampling sites A and B. ( c ) Cross-section through sinter rim and shelf around margin of Champagne Pool (after
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Sinter shelf around <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>. ( a ) Shallow, orange, subaqueous sinte...
Published: 01 March 2005
Fig. 2.  Sinter shelf around Champagne Pool. ( a ) Shallow, orange, subaqueous sinter shelf showing stromatolites (St), loose sediment (S), and grey subaerial sinter rim. (Site A in Fig. 1b. ) ( b ) Silica stromatolites rich in As–Sb sulphides on subaqueous sinter shelf. Loose sediment (S
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( a ) Speciation plot of dissolved arsenic species in <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span> genera...
Published: 01 March 2005
Fig. 9.  ( a ) Speciation plot of dissolved arsenic species in Champagne Pool generated using GWB React code and the data in Table 1 . The domination of neutral or negatively charged thio-, oxide and hydroxide complexes should be noted. Arrow indicates f O of spring water. The species H 2 AsO 4
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Experimental sinter growths on glass slides from <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>. (A) After ...
Published: 26 November 2003
Fig. 6. Experimental sinter growths on glass slides from Champagne Pool. (A) After 30 days, small spicules (∼ 1 mm) have developed on the top edges of the slides (shown magnified). Plastic holder is covered with growth of filamentous material covered in orange sulfur. (B) After 4 months, spicule
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( a ) General view of <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span> (CP) and Artist’s Palette (AP) looking...
Published: 01 November 2001
Fig. 2. ( a ) General view of Champagne Pool (CP) and Artist’s Palette (AP) looking to the west. ( b ) Northern margin of Champagne Pool showing sinter rim and subaqueous shelf. Arrows indicates shelf edge. ( c ) Subaqueous shelf covered with stromatolites that are formed of orange siliceous
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Stromatolitic sinters from shelf around <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>. Lightest laminae ha...
Published: 01 November 2001
Fig. 4. Stromatolitic sinters from shelf around Champagne Pool. Lightest laminae have deepest yellowish-orange colour. ( a ) Thinly laminated stromatolitic sinter. ( b ) Digitate stromatolites that nucleated on old sinter mass (arrows). ( c ) Coniform stromatolites.
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Microbes from stromatolites on subaqueous shelf around <span class="search-highlight">Champagne</span> <span class="search-highlight">Pool</span>. ( a ...
Published: 01 November 2001
Fig. 5. Microbes from stromatolites on subaqueous shelf around Champagne Pool. ( a ) Filamentous microbes on outer surface of stromatolite. Note variance in size of filaments. ( b ) Stromatolite surface showing large diameter, collapsed, non-mineralized filamentous microbes overlying masses
Journal Article
Journal: Economic Geology
Published: 01 June 2005
Economic Geology (2005) 100 (4): 677–687.
... concentrations are elevated within Champagne Pool and in precipitates surrounding this spring. Therefore, it is likely that the reservoir fluid that feeds springs at Waiotapu also contains dissolved gold. Champagne Pool has the highest gold concentration measured in this study, 109 ngL –1 dissolved and 362 ngL...
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Journal Article
Journal: PALAIOS
Published: 01 June 1997
PALAIOS (1997) 12 (3): 220–236.
...Brian Jones; Robin W. Renaut; Michael R. Rosen Abstract Clusters of microstromatolites, up to 10 mm high with a basal diameter of 4 mm, grow on twigs and small islands in shallow hot-spring waters around Champagne Pool and on Primrose Terrace at Waiotapu, New Zealand. Similar microstromatolites...
Journal Article
Journal: Economic Geology
Published: 01 October 1985
Economic Geology (1985) 80 (6): 1640–1668.
..., including the Champagne Pool which was formed 900 years ago, continue to discharge chloride water directly from the deeper hydrothermal reservoir. Precipitates formed within this pool are enriched in arsenic, antimony, thallium, and mercury and are ore grade with respect to gold and silver. Two chemical...
Journal Article
Published: 01 February 1999
Journal of the Geological Society (1999) 156 (1): 89–103.
...BRIAN JONES; ROBIN W. RENAUT; MICHAEL R. ROSEN Abstract Oncoids that are actively growing in some of the shallow-water pools around Champagne Pool, Waiotapu, New Zealand, are formed of amorphous silica (opal-A) with minor amounts of native sulphur. The growth of these oncoids is being mediated...
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2020
DOI: 10.5382/SP.23.38
EISBN: 9781629496429
... precipitates containing up to 6 wt.% Au from a hydrothermal solution containing a few ppb Au. Sorption on to As-Sb-S colloids produces precipitates containing tens to hundreds of ppm Au in the Champagne Pool hot spring. Sorption on to As-rich pyrite also leads to anomalous endowments of Au of up to 1 ppm...
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Journal Article
Published: 22 August 2019
Geochemistry: Exploration, Environment, Analysis (2020) 20 (3): 299–314.
...Fig. 5. Photograph of Waiotapu, looking SE. Champagne Pool, a hydrothermal eruption vent formed 900 years ago, is in the centre, with a surrounding sinter sheet extending left and collapse craters induced by hydrothermal alteration in the right foreground. The steaming pool ( c . 260°C) is c...
FIGURES | View All (18)