Please use this identifier to cite or link to this item: http://hdl.handle.net/123456789/1636
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dc.contributor.authorElvaene Jamesen_US
dc.contributor.authorHennie Fitria W. Soehady Erfenen_US
dc.contributor.authorAzman A. Ghanien_US
dc.contributor.authorAngela Vidda Chuwat4en_US
dc.contributor.authorGerald Eko Ejigaen_US
dc.date.accessioned2021-05-06T03:12:50Z-
dc.date.available2021-05-06T03:12:50Z-
dc.date.issued2020-
dc.identifier.isbn01265539-
dc.identifier.urihttp://hdl.handle.net/123456789/1636-
dc.descriptionOthersen_US
dc.description.abstractThe occurrence of columnar jointing is commonly associated with volcanic rocks and a rapid cooling environment. We recently discovered well-preserved columnar dacite on the road cutting slope in the eastern part of Tawau town, Sabah. This paper briefly describes the occurrences and morphology of columnar dacite in the study area. Columnar dacite exhibits entablature feature since it has thinner and chaotic columns. The hexagon side dominates the columnar joints with minor pentagons to heptagon sides. Columns for dacite are much smaller compared with columnar basalt Tawau. The formation of columnar joints was influenced mainly by external fluid where the water flow on top of the cooling lavas makes it cool rapidly.en_US
dc.language.isoenen_US
dc.publisherThe Geological Society of Malaysiaen_US
dc.relation.ispartofGeological Notesen_US
dc.subjectcolumnar dacite, entablature, Tawau, rapid coolingen_US
dc.titleThe characteristics and morphology of columnar dacite in Tawau, Sabahen_US
dc.typeNationalen_US
dc.identifier.doihttps://doi.org/10.7186/wg462202002-
dc.description.page45 - 51en_US
dc.volume46(2)en_US
dc.description.typeArticleen_US
item.languageiso639-1en-
item.grantfulltextopen-
item.openairetypeNational-
item.fulltextWith Fulltext-
crisitem.author.deptUniversity Malaysia Kelantan, Malaysia-
Appears in Collections:Faculty of Earth Science - Other Publication
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