Status of Spiny Lobster Resources in Sabah, Malaysia1
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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 -
Plate Tectonics and Seismic Activities in Sabah Area
Plate Tectonics and Seismic Activities in Sabah Area Kuei-hsiang CHENG* Kao Yuan University, 1821 Zhongshan Road, Luzhu District, Kaohsiung, Taiwan. *Corresponding author: [email protected]; Tel: 886-7-6077750; Fax: 886-7-6077762 A b s t r a c t Received: 27 November 2015 Ever since the Pliocene which was 1.6 million years ago, the structural Revised: 25 December 2015 geology of Sabah is already formed; it is mainly influenced by the early Accepted: 7 January 2016 South China Sea Plate, which is subducted into the Sunda Plate. However, In press: 8 January 2016 since the Cenozoic, the Sunda Plate is mainly influenced by the western and Online: 1 April 2016 southern of the Sunda-Java Arc and Trench system, and the eastern side of Luzon Arc and Trench system which has an overall impact on the tectonic Keywords: and seismic activity of Sunda plate. Despite the increasing tectonic activities Arc and Trench System, of Sunda-Java Arc and Trench System, and of Luzon Arc and Trench Tectonic earthquake, Seismic System since the Quaternary, which cause many large and frequent zoning, GM(1,1)model, earthquakes. One particular big earthquake is the M9.0 one in Indian Ocean Seismic potential assessment in 2004, leading to more than two hundred and ninety thousand deaths or missing by the tsunami caused by the earthquake. As for Borneo island which is located in residual arc, the impact of tectonic earthquake is trivial; on the other hand, the Celebes Sea which belongs to the back-arc basin is influenced by the collision of small plates, North Sulawesi, which leads to two M≧7 earthquakes (1996 M7.9 and 1999 M7.1) in the 20th century. -
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. -
Tourist Satisfaction Towards Kota Kinabalu, Sabah Using Importance-Performance Analysis (IPA) As a Tool to Determine Urban Ecotourism Potential
Journal of Tropical Biology and Conservation 17: 187–202, 2020 ISSN 1823-3902 E-ISSN 2550-1909 Research Article Tourist Satisfaction towards Kota Kinabalu, Sabah Using Importance-Performance Analysis (IPA) As a Tool to Determine Urban Ecotourism Potential Nattana Simon¹, Fiffy Hanisdah Saikim¹*, Awangku Hassanal Bahar Pengiran Bagul², Nor Akmar Abdul Aziz3 ¹Institute for Tropical Biology & Conservation, Universiti Malaysia Sabah, Jalan UMS, 88400 Kota Kinabalu, Sabah, Malaysia ²Faculty of Business, Economy and Accounting, Universiti Malaysia Sabah, Jalan UMS, 88400, Kota Kinabalu, Sabah, Malaysia 3Department of Nature Parks and Recreation, Faculty of Forestry and Environment, Universiti Putra Malaysia, 43400 Serdang, Malaysia *Corresponding author: [email protected] Abstract The Importance-Performance Analysis (IPA) is widely used in many fields of study as it produces simple and straightforward results. However, it is rarely used by managers of ecotourism and urban green spaces. Importance-Performance Analysis (IPA) was adopted from a destination perspective to understand industry demand. This study explores the visitors’ satisfaction level on ecotourism attributes i.e. attraction, urban green spaces and accessibility that affect tourist satisfaction towards Kota Kinabalu, Sabah, Malaysia using IPA scheme. A total of 384 tourists to Kota Kinabalu were provided with a list of environmental features and asked to rate the importance of and satisfaction with each attribute. IPA was performed to compare mean scores and identify areas of concern. The analysis identified eight (8) attributes which were applauded with excellent performance on highly important features and should maintain its competitiveness as a tourist destination. Six (6) attributes resulted under the poor performance on an extremely important category; indicates the areas that should be given improvement interventions, while four (4) attributes were identified as possible overkill that implies divergences of resources elsewhere are needed. -
25 the Land Capability Classification of Sabah Volume 1 the Tawau Residency
25 The land capability classification of Sabah Volume 1 The Tawau Residency OdEXäxo] ßte©@x>a?®^ ®(^ Scanned from original by ISRIC - World Soil Information, as ICSU World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued information available for consultation, following Fair Use Guidelines. Every effort is taken to respect Copyright of the materials within the archives where the identification of the Copyright holder is clear and, where feasible, to contact the originators. For questions please contact [email protected] indicating the item reference number concerned. The land capability classification of Sabah Volume 1 The Tawau Residency T-i2>S Land Resources Division The land capability classification of Sabah Volume 1 The Tawau Residency (with an Introduction and Summary for Volumes 1—4) P Thomas, F K C Lo and A J Hepburn Land Resource Study 25 Land Resources Division, Ministry of Overseas Development Tolworth Tower, Surbiton, Surrey, England KT6 7DY 1976 THE LAND RESOURCES DIVISION The Land Resources Division of the Ministry of Overseas Development assists develop ing countries in mapping, investigating and assessing land resources, and makes recommendations on the use of these resources for the development of agriculture, livestock husbandry and forestry; it also gives advice on related subjects to overseas governments and organisations, makes scientific personnel available for appointment abroad and provides lectures and training courses in the basic techniques of resource appraisal. The Division works in close cooperation with government departments, research institutes, universities and international organisations concerned with land resource assessment and development planning. -
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. -
A Gravity High in Darvel Bay
Ceol. Soc. MaLaYJia, BulLetill 59, July 1996,. pp. 1lJ-122 A gravity high in Darvel Bay PATRICK J.e. RYALL! AND DWAYNE BEATTIE2 1 Department of Geology Dalhousie University Halifax, Nova Scotia Canada B3H 3J5 2Geoterrex Ltd. 2060 Walkley Road Ottawa, Ontario Canada K1 G 3P5 Abstract: A gravity survey was carried out along the coastlines of Darvel Bay and many of the islands (e.g. Sakar, Tabauwan, Silumpat) in the Bay. In addition stations were located along the road from Kunak to Lahad Datu. The resulting Bouguer anomaly map shows a broad gravity high of at least 60 mgal which strikes west northwest with its maximum on the southern coast of Pulau Sakar. The anomaly narrows and decreases where it comes ashore and may continue along the Silam-Beeston Complex. This large positive anomaly suggests that there is an extensive ultramafic body beneath Darvel Bay. The gravity anomaly can best be modelled as a 3 to 5 km thick slab of ultramafic rock under the Bay with amphibolites on its northern and southern edges dipping away from the Bay. This model is consistent with a folded structure which brings upper mantle rocks to the surface. It is unlikely that there is a significant thickness of Chert-Spilite Formation beneath Darvel Bay, although the gravity data w.ould permit a thickness of up to a few hundred metres. INTRODUCTION Hutchison (1968,1975) considers the ophiolitic rocks of Darvel Bay as part of a strongly arcuate Borneo line which runs from the Sulu Archipelago in the northeast, through Darvel Bay and northwestern The island of Borneo is located in a complex Sabah and along Palawan (Fig. -
Coral Reefs in the Coastal Waters of the South China Sea MALAYSIA
United Nations UNEP/GEF South China Sea Global Environment Environment Programme Project Facility NATIONAL REPORT on Coral Reefs in the Coastal Waters of the South China Sea MALAYSIA Mr. Abdul Rahim Bin Gor Yaman Focal Point for Coral Reefs Marine Park Section, Ministry of Natural Resources and Environment Level 11, Lot 4G3, Precinct 4, Federal Government Administrative Centre 62574 Putrajaya, Selangor, Malaysia NATIONAL REPORT ON CORAL REEF IN THE SOUTH CHINA SEA – MALAYSIA 37 MALAYSIA Zahaitun Mahani Zakariah, Ainul Raihan Ahmad, Tan Kim Hooi, Mohd Nisam Barison and Nor Azlan Yusoff Maritime Institute of Malaysia INTRODUCTION Malaysia’s coral reefs extend from the renowned “Coral Triangle” connecting it with Indonesia, Philippines, Papua New Guinea, and Australia. Coral reef types in Malaysia are mostly shallow fringing reefs adjacent to the offshore islands. The rest are small patch reefs, atolls and barrier reefs. The United Nations Environment Programme’s World Atlas of Coral Reefs prepared by the Coral Reef Unit, estimated the size of Malaysia’s coral reef area at 3,600sq. km which is 1.27 percent of world total coverage (Spalding et al., 2001). Coral reefs support an abundance of economically important coral fishes including groupers, parrotfishes, rabbit fishes, snappers and fusiliers. Coral fish species from Serranidae, Lutjanidae and Lethrinidae contributed between 10 to 30 percent of marine catch in Malaysia (Wan Portiah, 1990). In Sabah, coral reefs support artisanal fisheries but are adversely affected by unsustainable fishing practices, including bombing and cyanide fishing. Almost 30 percent of Sabah’s marine fish catch comes from coral reef areas (Department of Fisheries Sabah, 1997). -
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. -
Curriculum Vite
BIODATA Ejria Binti Saleh Senior Lecturer, Borneo Marine Research Institute, Universiti Malaysia Sabah, Malaysia BIO SUMMARY - LIM AI YIM - MALAYSIA CURRICULUM VITE PERSONAL INFORMATION Name Name of Current Employer: Borneo Marine Research Institute Ejria Binti Saleh Universiti Malaysia Sabah Corresponding Address: E-mail: Borneo Marine Research Institute, [email protected]/[email protected] Universiti Malaysia Sabah, 88999 Kota Kinabalu, Sabah Malaysia Tel: 6088-320000 ext: 2594 Fax: 6088-320261 NRIC: 710201-12-5042 Nationality: Malaysian Date of Birth: 01 January 1971 Sex: Female ACADEMIC QUALIFICATION Diploma/Degree Name of University Year Major Doctor of Philosophy Universiti Malaysia 2007 Physical Oceanography Sabah, Malaysia. Master Science University of Liverpool, 1997 Recent Environmental United Kingdom. Change Bachelor of Fisheries Universiti Putra 1996 Marine science Sc. (Marine Sciences) Malaysia, Malaysia. 1 Diploma in Fisheries Universiti Putra 1993 Fisheries Malaysia, Malaysia. RESEARCH PROJECTS Project Project Title Role Year Funder Status No. B-08-0- Tidal effects on salinity Co- 2002-2003 FRGS Completed 12ER intrusion and suspended Researcher sediment discharged in Manggatal River Estuary, Sabah SCF0019- Study of the factors regulating Co- 2006 -2009 Science Completed AGR-2006 the bloom mechanisms of Researcher Fund harmful algal species in Sabah SCF0015- Coastal processes and Co- 2006 -2009 Science Completed ENV-2006 geomorphologic Researcher Fund characteristics of major coastal towns in East Sabah for assessment