Fig. 3. Model of heat transfer mechanism under Crater Lake. The scale of the volcanic vent is highly exaggerated for pictorial purposes. Within the main part of the vent, a heat pipe consisting of counter flows of vapour (upwards) and condensed liquid (downwards) transfers heat from a magmatic source at depth to the vicinity of the lake. Beneath the lake a liquid sulphur layer regulates heating and cooling of the lake. (Courtesy of DSIR Geology and Geophysics).
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Ruapehu Bulletin, Volume 9, Issue 420, 21 January 1992, Page 12
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77Fig. 3. Model of heat transfer mechanism under Crater Lake. The scale of the volcanic vent is highly exaggerated for pictorial purposes. Within the main part of the vent, a heat pipe consisting of counter flows of vapour (upwards) and condensed liquid (downwards) transfers heat from a magmatic source at depth to the vicinity of the lake. Beneath the lake a liquid sulphur layer regulates heating and cooling of the lake. (Courtesy of DSIR Geology and Geophysics). Ruapehu Bulletin, Volume 9, Issue 420, 21 January 1992, Page 12
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