From Geoscience Australia

Investigation of hot gas emissions from Koranga volcano, Papua New Guinea, in 1967

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Created 13/01/2025

Updated 13/01/2025

Hot emissions of mainly sulphur dioxide and carbon dioxide took place from a mound in Koranga open cut, near Wau, following a landslide at the end of May, 1967. Rocks of the Holocene volcano, Koranga, are exposed in the open cut. The emissions lasted about three months, and ceased on 13 August after another landslide removed the active mound. During the period of activity, recorded temperatures ranged up to 680°C; no anomalous seismic or tilt phenomena were recorded. The cause of the activity is not known, but it is thought that the high temperatures and gases may have been the result of the spontaneous combustion of reactive sulphides and carbonaceous material present in the altered rocks of Koranga volcano.

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Title Investigation of hot gas emissions from Koranga volcano, Papua New Guinea, in 1967
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/5f257872-fdb2-4ef7-9fe8-2bfe6153aab1
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[146.4, -7.5], [146.9, -7.5], [146.9, -7.0], [146.4, -7.0], [146.4, -7.5]]]}
Data Portal data.gov.au

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This dataset was originally found on data.gov.au "Investigation of hot gas emissions from Koranga volcano, Papua New Guinea, in 1967". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/investigation-of-hot-gas-emissions-from-koranga-volcano-papua-new-guinea-in-1967