TEMPERATURE MEASUREMENTS IN THE CRATER OF MOUNT EREBUS, ROSS ISLAND, ANTARCTICA (2)
Surface temperature distribution in the crater of Mount Erebus, Ross Island, Antarctica was surveyed during the 1989-1990 field season using an infrared radiation thermometer. A convecting lava lake with the diameter of about 20 to 30m was observed in the inner crater of the main crater. The maximum...
Main Authors: | , , , , |
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Format: | Report |
Language: | English |
Published: |
Shimabara Earthquake and Volcano Observatory, Kyushu University
1991
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Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2687 http://id.nii.ac.jp/1291/00002687/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2687&item_no=1&attribute_id=18&file_no=1 |
Summary: | Surface temperature distribution in the crater of Mount Erebus, Ross Island, Antarctica was surveyed during the 1989-1990 field season using an infrared radiation thermometer. A convecting lava lake with the diameter of about 20 to 30m was observed in the inner crater of the main crater. The maximum surface temperature of the inner crater was 118℃. |
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