Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan

Karst of Sangkulirang Mangkalihat is one of the greatest karst areas in Indonesia and has hundreds of caves. Some of those caves are located at Suaran Block, one of the main karst block at this karst. This paper aims to study the speleogenesis process, as the fundamental process on karst landscape a...

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Main Authors: Reinhart Hilary, Labib Mohammad Ainul, Haryono Eko
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/60/e3sconf_icst2020_06011.pdf
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spelling doaj-e48114d8bef34f0eb2a64e2cb327b2c02021-04-02T18:11:27ZengEDP SciencesE3S Web of Conferences2267-12422020-01-012000601110.1051/e3sconf/202020006011e3sconf_icst2020_06011Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East KalimantanReinhart HilaryLabib Mohammad AinulHaryono EkoKarst of Sangkulirang Mangkalihat is one of the greatest karst areas in Indonesia and has hundreds of caves. Some of those caves are located at Suaran Block, one of the main karst block at this karst. This paper aims to study the speleogenesis process, as the fundamental process on karst landscape and cave development in that area. Speleogenetic process can be examined from the shape of the cave passage using uniformitarianism approach. That principle creates speleomorphology as the study of cave passage form and the factors that affect it. The examination of the cave passages uses cave maps to see the form and direction of them. As the result, caves at Suaran Block are formed mainly driven by geological structures such as fault – fissures and bedding plane which is indicated by linear form of the cave passage and water flow which shows sinusoidal form of the cave passage. Some caves are shaped by the combination of geological structure and water flows make them have mixed-induced speleogenesis.https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/60/e3sconf_icst2020_06011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Reinhart Hilary
Labib Mohammad Ainul
Haryono Eko
spellingShingle Reinhart Hilary
Labib Mohammad Ainul
Haryono Eko
Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
E3S Web of Conferences
author_facet Reinhart Hilary
Labib Mohammad Ainul
Haryono Eko
author_sort Reinhart Hilary
title Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
title_short Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
title_full Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
title_fullStr Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
title_full_unstemmed Speleogenetic process of Suaran Block, karst of Sangkulirang–Mangkalihat, East Kalimantan
title_sort speleogenetic process of suaran block, karst of sangkulirang–mangkalihat, east kalimantan
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2020-01-01
description Karst of Sangkulirang Mangkalihat is one of the greatest karst areas in Indonesia and has hundreds of caves. Some of those caves are located at Suaran Block, one of the main karst block at this karst. This paper aims to study the speleogenesis process, as the fundamental process on karst landscape and cave development in that area. Speleogenetic process can be examined from the shape of the cave passage using uniformitarianism approach. That principle creates speleomorphology as the study of cave passage form and the factors that affect it. The examination of the cave passages uses cave maps to see the form and direction of them. As the result, caves at Suaran Block are formed mainly driven by geological structures such as fault – fissures and bedding plane which is indicated by linear form of the cave passage and water flow which shows sinusoidal form of the cave passage. Some caves are shaped by the combination of geological structure and water flows make them have mixed-induced speleogenesis.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2020/60/e3sconf_icst2020_06011.pdf
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