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Active Tectonics in Sabah – Seismicity and Active Faults Felix Tongkul
Bulletin of the Geological Society of Malaysia, Volume 64, December 2017, pp. 27 – 36 Active tectonics in Sabah – seismicity and active faults Felix Tongkul Natural Disaster Research Centre (NDRC), Universiti Malaysia Sabah, 88400, Kota Kinabalu, Sabah Email address: [email protected] Abstract: The location of Sabah near the boundaries of three major tectonic plates, the Eurasian, India-Australia and Philippine-Pacific plates, makes it prone to seismic activities. Sabah is currently under a WNW-ESE compressive stress regime due to the effect of plate movements as the Philippine-Pacific plate move westward at the rate of about 10 cm/ year against the southeast moving Eurasian plate at the rate of about 5 cm/year. The WNW-ESE compression is being accommodated by NE-SW trending active thrust faults and NW-SE trending active strike-slip faults present all over Sabah. Evidence of active faults based on geomorphological features, such as linear structures associated with triangular facets, stream offsets, mud volcanoes and hot springs are widespread in Sabah.The WNW-ESE compression resulted in regional folding or warping of the upper crust to produce an uplifted belt trending NE-SW in Western Sabah, currently occupied by the Crocker-Trusmadi Range. The warping and uplift of the upper crust is thought to be driving extensional tectonics, marked by the presence of NE-SW trending active normal faults along the crest and flanks of the Crocker- Trusmadi Range anticlinorium. At least six elongate Quaternary graben-like basins (Tenom, Keningau, Tambunan, Ranau, Timbua and Marak-Parak) occur along the crest of the anticlinorium. -
Sabah REDD+ Roadmap Is a Guidance to Press Forward the REDD+ Implementation in the State, in Line with the National Development
Study on Economics of River Basin Management for Sustainable Development on Biodiversity and Ecosystems Conservation in Sabah (SDBEC) Final Report Contents P The roject for Develop for roject Chapter 1 Introduction ............................................................................................................. 1 1.1 Background of the Study .............................................................................................. 1 1.2 Objectives of the Study ................................................................................................ 1 1.3 Detailed Work Plan ...................................................................................................... 1 ing 1.4 Implementation Schedule ............................................................................................. 3 Inclusive 1.5 Expected Outputs ......................................................................................................... 4 Government for for Government Chapter 2 Rural Development and poverty in Sabah ........................................................... 5 2.1 Poverty in Sabah and Malaysia .................................................................................... 5 2.2 Policy and Institution for Rural Development and Poverty Eradication in Sabah ............................................................................................................................ 7 2.3 Issues in the Rural Development and Poverty Alleviation from Perspective of Bangladesh in Corporation City Biodiversity -
Journal of TROPICAL BIOLOGY & CONSERVATION a Journal of the Institute for Tropical Biology and Conservation, Universiti Malaysia Sabah
Journal of TROPICAL BIOLOGY & CONSERVATION A journal of the Institute for Tropical Biology and Conservation, Universiti Malaysia Sabah Editor-in-chief Dr. Charles S. Vairappan (Prof., Universiti Malaysia Sabah, Malaysia) Managing Editor Dr. Liew Thor Seng (Universiti Malaysia Sabah, Malaysia) Editorial Assistant Julia George Kunai (Universiti Malaysia Sabah, Malaysia) Editorial Board Dr. Mohd. Tajuddin Abdullah (Prof., Universiti Malaysia Terengganu, Malaysia) Dr. Abdul Hamid Ahmad (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) Dr. Henry Bernard (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) Dr. Shigeki Matsunaga (Prof., the University of Tokyo, Japan) Dr. Homathevi Rahman (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) Dr. Menno Schilthuizen (Prof., Leiden University, the Netherlands) Dr. Monica Suleiman (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) Dr. Holger Thus (Natural History Museum, London) Reviewers Dr. Abdul Hamid Ahmad Dr. Menno Schilthuizen (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) (Prof., Leiden University, the Netherlands) Dr. Alexender Kiew Sayok Dr. Moh Pak Yan (Universiti Malaysia Sarawak, Malaysia) (Universiti Malaysia Sabah, Malaysia) Anthony Lamb Dr. Monica Suleiman (Kota Kinabalu, Sabah, Malaysia) (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) Dr. Awangku Hassanal Bahar Bin Pengiran Bagul Dr. Niels Jacobsen (Universiti Malaysia Sabah, Malaysia) (Prof., Universiti of Conpenhagen, Denmark) Dr. Arthur Y.C. Chung Dr. Norela Sulaiman (Forest Research Centre, Sabah, Malaysia) (Assoc. Prof., Universiti Kebangsaan Malaysia) Dr. Arzyana Sunkar Pelf-Nyok Chen (Bogor Agricultural University, Indonesia) (Turtle Conservation Society of Malaysia, Malaysia) Dr. Colin Ruzelion Maycock Dr. Pratap Kumar Panda (Assoc. Prof., Universiti Malaysia Sabah, Malaysia) (Atal Behari College, Basudevpur, India ) Effi Helmy Bin Ariffin Dr. Sahana Harun (Universiti Malaysia Terengganu, Malaysia) (Universiti Malaysia Sabah, Malaysia) Dr. Henry Bernard Dr. -
Day 1: KOTA KINABALU –APIN-APIN, KENINGAU- PAGANDADAN
Standard Itinerary Day 1: KOTA KINABALU –APIN-APIN, KENINGAU- PAGANDADAN RANGERS (Dinner) Meet your driver in the designated hotel and then will transfer to Kapayan Recreation Resources(KRR) where all climbers will gather before proceed to the starting point in Apin- Apin, Keningau. Upon arrival to Apin-Apin Keningau, continue to register and double check the climbing permit and attend to a short safety briefing before start heading to the starting point base camp lead by the mountain guide. Estimated time taken shall be around 3- 4 hours depends on your pace. Along the way, stop by at the captivating Trusmadi Waterfall. Dinner will be served at the camp site and later overnight stay at the camp. After dinner, join in with a short night walk in search of nocturnal animal before proceed to rest in the tent provided. (Timing and places all depend on your schedule of arrival) Day 2: CAMPSITE – WATERFALL VISIT (Breakfast, Lunch, Dinner) Wake up around 06:00 hrs to prepare for a trek to the Kalawot Waterfall. The trek shall takes around 1 hour to 1 hour 30 minutes to arrive. Upon arrival, relax and enjoy the water. Later on, trek back to the base camp and proceed for lunch upon arrival to the camp site. Listen to a short briefing before heading to bed from the Leader Guide. Rest early for the night as you will be require to wake up early for the climb to the summit later on. Day 3: BASE CAMP - SUMMIT- PAGANDADAN RANGERS- KOTA KINABALU (Breakfast, Lunch) Wake up as early as 00:00 hrs to get ready for another 4-5 hours track. -
Internalization and Anti Littering Campaign Implementation
Available online at www.sciencedirect.com ScienceDirect Procedia - Social and Behavioral Sciences 85 ( 2013 ) 544 – 553 AcE-Bs 2013 Hanoi ASEAN Conference on Environment-Behaviour Studies Hanoi Architectural University, Hanoi, Vietnam, 19-22 March 2013 "Cultural Sustainability in the Built and Natural Environment" Internalization and Anti Littering Campaign Implementation Haijon Gunggut*, Chua Kim Hing, Dg Siti Noor Saufidah Ag Mohd Saufi Universiti Teknologi MARA, Locked Bag 71, 88997 Kota Kinabalu, Malaysia Abstract This paper seeks to account for the variations in implementation progress of the Anti-litterbugs Campaign in Sabah. A total of nine local authorities were studied. Data was mainly obtained from interviews, observations and written sources. The variation in the Campaign implementation progress can be explained in term of campaign internalization among local authority top leadership. Internalization is reflected in the understanding of the campaign and priority of local government top leaderships observed in their actions, choice of words and activities. In addition, the structure of the local authority also influenced implementation progress. © 2013 The Authors. Published by Elsevier Ltd. ©Selection 2013 andPublished peer-review by Elsevierunder responsibility Ltd. Selection of Centre and for peer-review Environment-Behaviour under responsibility Studies (cE-Bs), of the Faculty Centre of Architecture, for Environment- BehPlanningaviour & Surveying,Studies (cE-Bs), Universiti Faculty Teknologi of Architecture,MARA, Malaysia Planning & Surveying, Universiti Teknologi MARA, Malaysia. Keyword: Anti-litterbugs campaign; programme internalization; local government structure; policy implementation 1. Introduction Sabah is one the top biodiversity hotspots in the world and an estimated 2.93 million tourists visited the state in 2012 (Bangkuai, 2012). Unfortunately visitors were often turned off by the presence of litters everywhere. -
Mantle Structure and Tectonic History of SE Asia
Nature and Demise of the Proto-South China Sea ROBERT HALL, H. TIM BREITFELD SE Asia Research Group, Department of Earth Sciences, Royal Holloway University of London, Egham, Surrey, TW20 0EX, United Kingdom Abstract: The term Proto-South China Sea has been used in a number of different ways. It was originally introduced to describe oceanic crust that formerly occupied the region north of Borneo where the modern South China Sea is situated. This oceanic crust was inferred to have been Mesozoic, and to have been eliminated by subduction beneath Borneo. Subduction was interpreted to have begun in Early Cenozoic and terminated in the Miocene. Subsequently the term was also used for inferred oceanic crust, now disappeared, of quite different age, notably that interpreted to have been subducted during the Late Cretaceous below Sarawak. More recently, some authors have considered that southeast-directed subduction continued until much later in the Neogene than originally proposed, based on the supposition that the NW Borneo Trough and Palawan Trough are, or were recently, sites of subduction. Others have challenged the existence of the Proto-South China Sea completely, or suggested it was much smaller than envisaged when the term was introduced. We review the different usage of the term and the evidence for subduction, particularly under Sabah. We suggest that the term Proto-South China Sea should be used only for the slab subducted beneath Sabah and Cagayan between the Eocene and Early Miocene. Oceanic crust subducted during earlier episodes of subduction in other areas should be named differently and we use the term Paleo- Pacific Ocean for lithosphere subducted under Borneo in the Cretaceous. -
Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey
Downloaded from orbit.dtu.dk on: Oct 05, 2021 Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey Fauzi Nordin, Ahmad; Jamil, Hassan; Noor Isa, Mohd; Mohamed, Azhari; Hj. Tahir, Sanudin; Musta, Baba ; Forsberg, René; Olesen, Arne Vestergaard; Nielsen, Jens Emil; Majid A. Kadir, Abd Total number of authors: 13 Published in: Borneo Science, The Journal of Science and Technology Publication date: 2016 Document Version Publisher's PDF, also known as Version of record Link back to DTU Orbit Citation (APA): Fauzi Nordin, A., Jamil, H., Noor Isa, M., Mohamed, A., Hj. Tahir, S., Musta, B., Forsberg, R., Olesen, A. V., Nielsen, J. E., Majid A. Kadir, A., Fahmi Abd Majid, A., Talib, K., & Aman Sulaiman, S. (2016). Geological Mapping of Sabah, Malaysia, Using Airborne Gravity Survey. Borneo Science, The Journal of Science and Technology, 37(2), 14-27. General rights Copyright and moral rights for the publications made accessible in the public portal are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. Users may download and print one copy of any publication from the public portal for the purpose of private study or research. You may not further distribute the material or use it for any profit-making activity or commercial gain You may freely distribute the URL identifying the publication in the public portal If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. -
M.V. Solita's Passage Notes
M.V. SOLITA’S PASSAGE NOTES SABAH BORNEO, MALAYSIA Updated August 2014 1 CONTENTS General comments Visas 4 Access to overseas funds 4 Phone and Internet 4 Weather 5 Navigation 5 Geographical Observations 6 Flags 10 Town information Kota Kinabalu 11 Sandakan 22 Tawau 25 Kudat 27 Labuan 31 Sabah Rivers Kinabatangan 34 Klias 37 Tadian 39 Pura Pura 40 Maraup 41 Anchorages 42 2 Sabah is one of the 13 Malaysian states and with Sarawak, lies on the northern side of the island of Borneo, between the Sulu and South China Seas. Sabah and Sarawak cover the northern coast of the island. The lower two‐thirds of Borneo is Kalimantan, which belongs to Indonesia. The area has a fascinating history, and probably because it is on one of the main trade routes through South East Asia, Borneo has had many masters. Sabah and Sarawak were incorporated into the Federation of Malaysia in 1963 and Malaysia is now regarded a safe and orderly Islamic country. Sabah has a diverse ethnic population of just over 3 million people with 32 recognised ethnic groups. The largest of these is the Malays (these include the many different cultural groups that originally existed in their own homeland within Sabah), Chinese and “non‐official immigrants” (mainly Filipino and Indonesian). In recent centuries piracy was common here, but it is now generally considered relatively safe for cruising. However, the nearby islands of Southern Philippines have had some problems with militant fundamentalist Muslim groups – there have been riots and violence on Mindanao and the Tawi Tawi Islands and isolated episodes of kidnapping of people from Sabah in the past 10 years or so. -
Sabah 90000 Tabika Kemas Kg
Bil Nama Alamat Daerah Dun Parlimen Bil. Kelas LOT 45 BATU 7 LORONG BELIANTAMAN RIMBA 1 KOMPLEKS TABIKA KEMAS TAMAN RIMBAWAN Sandakan Sungai SiBuga Libaran 11 JALAN LABUKSANDAKAN SABAH 90000 TABIKA KEMAS KG. KOBUSAKKAMPUNG KOBUSAK 2 TABIKA KEMAS KOBUSAK Penampang Kapayan Penampang 2 89507 PENAMPANG 3 TABIKA KEMAS KG AMAN JAYA (NKRA) KG AMAN JAYA 91308 SEMPORNA Semporna Senallang Semporna 1 TABIKA KEMAS KG. AMBOI WDT 09 89909 4 TABIKA KEMAS KG. AMBOI Tenom Kemabong Tenom 1 TENOM SABAH 89909 TENOM TABIKA KEMAS KAMPUNG PULAU GAYA 88000 Putatan 5 TABIKA KEMAS KG. PULAU GAYA ( NKRA ) Tanjong Aru Putatan 2 KOTA KINABALU (Daerah Kecil) KAMPUNG KERITAN ULU PETI SURAT 1894 89008 6 TABIKA KEMAS ( NKRA ) KG KERITAN ULU Keningau Liawan Keningau 1 KENINGAU 7 TABIKA KEMAS ( NKRA ) KG MELIDANG TABIKA KEMAS KG MELIDANG 89008 KENINGAU Keningau Bingkor Keningau 1 8 TABIKA KEMAS (NKRA) KG KUANGOH TABIKA KEMAS KG KUANGOH 89008 KENINGAU Keningau Bingkor Keningau 1 9 TABIKA KEMAS (NKRA) KG MONGITOM JALAN APIN-APIN 89008 KENINGAU Keningau Bingkor Keningau 1 TABIKA KEMAS KG. SINDUNGON WDT 09 89909 10 TABIKA KEMAS (NKRA) KG. SINDUNGON Tenom Kemabong Tenom 1 TENOM SABAH 89909 TENOM TAMAN MUHIBBAH LORONG 3 LOT 75. 89008 11 TABIKA KEMAS (NKRA) TAMAN MUHIBBAH Keningau Liawan Keningau 1 KENINGAU 12 TABIKA KEMAS ABQORI KG TANJUNG BATU DARAT 91000 Tawau Tawau Tanjong Batu Kalabakan 1 FASA1.NO41 JALAN 1/2 PPMS AGROPOLITAN Banggi (Daerah 13 TABIKA KEMAS AGROPOLITAN Banggi Kudat 1 BANGGIPETI SURAT 89050 KUDAT SABAH 89050 Kecil) 14 TABIKA KEMAS APARTMENT INDAH JAYA BATU 4 TAMAN INDAH JAYA 90000 SANDAKAN Sandakan Elopura Sandakan 2 TABIKA KEMAS ARS LAGUD SEBRANG WDT 09 15 TABIKA KEMAS ARS (A) LAGUD SEBERANG Tenom Melalap Tenom 3 89909 TENOM SABAH 89909 TENOM TABIKA KEMAS KG. -
On Slopes Along the Penampang to Tambunan Road, Sabah, Malaysia
Malaysian Journal of Geoscien ces 2(1) (2018) 0 9-17 Malaysian Journal of Geosciences (MJG) DOI : https://doi.org/10.26480/mjg.01.2018.0 .1 9 7 ISSN: 2521-0920 (Print) ISSN: 2521-0602 (Online) CODEN : MJGAAN ENGINEERING GEOLOGICAL ASSESSMENT (EGA) ON SLOPES ALONG THE PENAMPANG TO TAMBUNAN ROAD, SABAH, MALAYSIA Rodeano Roslee1,2*, Felix Tongkul 1,2 1 Natural Disaster Research Centre (NDRC), Universiti Malaysia Sabah 2 Faculty of Science and Natural Resources, Universiti Malaysia Sabah *Corresponding Author Email: [email protected] This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ARTICLE DETAILS ABSTRACT Article History: This study focused on the engineering geological investigation of slope failures along Penampang to Tambunan road, approximately 12th km to 101th km from Kota Kinabalu city, Sabah, Malaysia. The area is underlain by the Crocker Received 12 November 2017 Formation (Late Eocene to Early Miocene age) and the Quaternary Deposits (Recent age). These rock units show Accepted 12 December 2017 Available online 1 January 2018 numerous lineaments with complex structural styles developed during several regional Tertiary tectonic activities. The tectonic complexities influenced the physical and mechanical properties of the rocks, resulting in a high degree of weathering and instability. The weathered materials are unstable and may experience sliding due to by high pore pressure and intensively geomorphological processes. In this study, a total of 31 selected critical slope failures were studied and classified into two main groups: rock slope and soil slope. -
South-East Asia Second Edition CHARLES S
Geological Evolution of South-East Asia Second Edition CHARLES S. HUTCHISON Geological Society of Malaysia 2007 Geological Evolution of South-east Asia Second edition CHARLES S. HUTCHISON Professor emeritus, Department of geology University of Malaya Geological Society of Malaysia 2007 Geological Society of Malaysia Department of Geology University of Malaya 50603 Kuala Lumpur Malaysia All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior permission of the Geological Society of Malaysia ©Charles S. Hutchison 1989 First published by Oxford University Press 1989 This edition published with the permission of Oxford University Press 1996 ISBN 978-983-99102-5-4 Printed in Malaysia by Art Printing Works Sdn. Bhd. This book is dedicated to the former professors at the University of Malaya. It is my privilege to have collabo rated with Professors C. S. Pichamuthu, T. H. F. Klompe, N. S. Haile, K. F. G. Hosking and P. H. Stauffer. Their teaching and publications laid the foundations for our present understanding of the geology of this complex region. I also salute D. ]. Gobbett for having the foresight to establish the Geological Society of Malaysia and Professor Robert Hall for his ongoing fascination with this region. Preface to this edition The original edition of this book was published by known throughout the region of South-east Asia. Oxford University Press in 1989 as number 13 of the Unfortunately the stock has become depleted in 2007. Oxford monographs on geology and geophysics. -
Uhm Ma 3222 R.Pdf
Ui\i1VEi~.'3!TY OF HA\/VAI'I LIBRARY PLANNING KADAZANDUSUN (SABAH, MALAYSIA): LABELS, IDENTITY, AND LANGUAGE A THESIS SUBMITTED TO THE GRADUATE DIVISION OF THE UNIVERSITY OF HAWAI'I IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN LINGUISTICS MAY 2005 By Trixie M. Tangit Thesis Committee: AndrewD. W. Wong, Chairperson Kenneth L. Rehg Michael L. Fonnan © 2005, Trixie M. Tangit 111 For the Kadazandusun community in Sabah, Malaysia and for the beloved mother tongue IV ACKNOWLEDGEMENTS I wish to take this opportunity to record my gratitude and heartfelt thanks to all those who have helped. me to accomplish my study goals throughout the M.A. program. Firstly, my thanks and appreciation to the participants who have contributed to this study on the Kadazandusun language: In particular, I thank Dr. Benedict Topin (from the Kadazan Dusun Cultural Association (KDCA», Ms. Evelyn Annol (from the Jabatan Pendidikan Negeri Sabab/ Sabah state education department (JPNS», and Ms. Rita Lasimbang (from the Kadazandusun Language Foundation (KLF». I also take this opportunity to thank Mr. Joe Kinajil, ex-JPNS coordinator (retired) ofthe Kadazandusun language program in schools, for sharing his experiences in the early planning days ofthe Kadazandusun language and for checking language data. I also wish to record my sincere thanks to Ms. Pamela Petrus Purser and Mr. Wendell Gingging for their kind assistance in checking the language data in this thesis. Next, my sincere thanks and appreciation to the academic community at the Department ofLinguistics, University ofHawai'i at Manoa: In particular, mahalo nui loa to my thesis committee for their feedback, support, and advice.