Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak
Debris flows have always been a major issue in hilly environments. This paper concerns about the debris flow event along Sungai Mandi, Santubong which caused damage to property, buildings and roads at the river mouth. The main objective of this study is to determine the root cause of the debris flow...
Saved in:
Main Authors: | , , , , , , , , , |
---|---|
Other Authors: | |
Format: | Book chapter |
Published: |
Springer Science and Business Media Deutschland GmbH
2024
|
Subjects: | |
Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
Institution: | Universiti Tenaga Nasional |
id |
my.uniten.dspace-34416 |
---|---|
record_format |
dspace |
spelling |
my.uniten.dspace-344162024-10-14T11:19:38Z Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak Zarime N.A. Bachat J. Solemon B. Omar R.C. Wahab W.A. Taher T.M. Jaapar A.R. Roslan R. Aripin F.S. Isa A.A.M. 56593247000 57192005245 24832320000 35753735300 56040257700 57195257852 57361879800 57159693200 58906157800 58074943900 Abandoned channel Boulder deposits Debris flow Debris flow anatomy zones Debris flow risk map Energy Santubong Debris flows have always been a major issue in hilly environments. This paper concerns about the debris flow event along Sungai Mandi, Santubong which caused damage to property, buildings and roads at the river mouth. The main objective of this study is to determine the root cause of the debris flow event and to provide a better understanding on the debris flow mechanism and structures at risk at Santubong, Sarawak. A comprehensive assessment on geological, geomorphological, topographical, hydrological conditions and rainfall assessment concerns was conducted, where debris flow hazard factors were identified and assessed. Such hazard factors included the presence of boulder deposits, colluvium, relic landslide, riverbank erosion, boulders accumulated or trapped along river valley that created the temporary natural dams, which can contribute to further debris flow event in future. In addition, kinematic failure analysis was conducted to determine the rockfall failure potential as well as aerial photo interpretation on lineament and relic landslide. The interpretations and assessment would allow the results to be used to produce the debris flow risk map (buffer and danger zones) and debris flow anatomy zones. Furthermore, these assessments are critical for making judgements when evaluating the debris flow mechanism that could affect the tourism activities at Santubong Peninsula. � The Author(s), under exclusive license to Springer Nature Singapore Pte Ltd. 2023. Final 2024-10-14T03:19:38Z 2024-10-14T03:19:38Z 2023 Book chapter 10.1007/978-981-99-3708-0_71 2-s2.0-85185929990 https://www.scopus.com/inward/record.uri?eid=2-s2.0-85185929990&doi=10.1007%2f978-981-99-3708-0_71&partnerID=40&md5=5b52af0f4a85268475da400fcf714fc6 https://irepository.uniten.edu.my/handle/123456789/34416 Part F2265 1005 1015 Springer Science and Business Media Deutschland GmbH Scopus |
institution |
Universiti Tenaga Nasional |
building |
UNITEN Library |
collection |
Institutional Repository |
continent |
Asia |
country |
Malaysia |
content_provider |
Universiti Tenaga Nasional |
content_source |
UNITEN Institutional Repository |
url_provider |
http://dspace.uniten.edu.my/ |
topic |
Abandoned channel Boulder deposits Debris flow Debris flow anatomy zones Debris flow risk map Energy Santubong |
spellingShingle |
Abandoned channel Boulder deposits Debris flow Debris flow anatomy zones Debris flow risk map Energy Santubong Zarime N.A. Bachat J. Solemon B. Omar R.C. Wahab W.A. Taher T.M. Jaapar A.R. Roslan R. Aripin F.S. Isa A.A.M. Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
description |
Debris flows have always been a major issue in hilly environments. This paper concerns about the debris flow event along Sungai Mandi, Santubong which caused damage to property, buildings and roads at the river mouth. The main objective of this study is to determine the root cause of the debris flow event and to provide a better understanding on the debris flow mechanism and structures at risk at Santubong, Sarawak. A comprehensive assessment on geological, geomorphological, topographical, hydrological conditions and rainfall assessment concerns was conducted, where debris flow hazard factors were identified and assessed. Such hazard factors included the presence of boulder deposits, colluvium, relic landslide, riverbank erosion, boulders accumulated or trapped along river valley that created the temporary natural dams, which can contribute to further debris flow event in future. In addition, kinematic failure analysis was conducted to determine the rockfall failure potential as well as aerial photo interpretation on lineament and relic landslide. The interpretations and assessment would allow the results to be used to produce the debris flow risk map (buffer and danger zones) and debris flow anatomy zones. Furthermore, these assessments are critical for making judgements when evaluating the debris flow mechanism that could affect the tourism activities at Santubong Peninsula. � The Author(s), under exclusive license to Springer Nature Singapore Pte Ltd. 2023. |
author2 |
56593247000 |
author_facet |
56593247000 Zarime N.A. Bachat J. Solemon B. Omar R.C. Wahab W.A. Taher T.M. Jaapar A.R. Roslan R. Aripin F.S. Isa A.A.M. |
format |
Book chapter |
author |
Zarime N.A. Bachat J. Solemon B. Omar R.C. Wahab W.A. Taher T.M. Jaapar A.R. Roslan R. Aripin F.S. Isa A.A.M. |
author_sort |
Zarime N.A. |
title |
Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
title_short |
Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
title_full |
Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
title_fullStr |
Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
title_full_unstemmed |
Debris Flow Mapping at Sungai Mandi, Santubong, Sarawak |
title_sort |
debris flow mapping at sungai mandi, santubong, sarawak |
publisher |
Springer Science and Business Media Deutschland GmbH |
publishDate |
2024 |
_version_ |
1814061179403763712 |