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...

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Bibliographic Details
Main Authors: シミズ ヒロシ, カミヌマ カツタダ /, Hiroshi SHIMIZU, Katsutada KAMINUMA, Raymond R. DIBBLE
Format: Report
Language:English
Published: Shimabara Earthquake and Volcano Observatory, Kyushu University 1991
Subjects:
Ross Island
Lava Lake
Mount Erebus
Main Crater
Inner Crater
Antarc*
Antarctica
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
Description
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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