25 the Land Capability Classification of Sabah Volume 2 the Sandakan Residency
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09 Lim Index.Indd 142 5/16/08 3:10:49 PM Index 143
INDEX 1982 Federal election, 82 Anwar Ibrahim, 66, 69, 109 1994 Sabah State elections, 81 Anti-Corruption Agency, 62 Asek bin Pintar, 96 A Assistant Residents, 21 ABC system, 84–86, 99–100, 120 Association for the Relief of A. G. Sahari, Datuk Haji, 106 Calamity, 36 Abell, Anthony (Sir), 57 Abdilah Hassan, 80 B Abdul Rahman (Tunku), see Tunku Bajau, 16 Abdul Rahman hostility with Kadazan-Dusun Abdul Razak (Tun), see Tun Abdul communities, 18 Razak Bank Islam Malaysia, 69 Aceh, 12 Bank Kerjasama Rakyat, 62 Adat rituals, 113 Banten, 12 Administration of Muslim Law Barisan Nasional, 1, 6, 53 Enactment, 109 constitutional amendments, 54 Advisory Council for Native Affairs expulsion of USNO from, 77–78 (ACNA), 31 Basel Church, 30 membership, 32, 34 BERJAYA administration, 63, 68 Affendi Stephen, Haji, 80 developmentalist approach to Ahmad Raffae, Pangiran Haji, 50 Islamization, 122 Alcock, Rutherford (Sir), 20, 39 economic transformation under, Aliuddin, A.K., 63 82–86 Amanah Saham Nasional, 120 failing to live up to multiracial Amanah Saham Rakyat Sabah, 89, pledges, 122 99 financial allocation for Islamic Amanah Saham Rakyat, 89 activities, 107 Amanah Saham Tun Hj Datu Islamization drive, 120 Mustapha, 88 political economy, 84–86 Angkatan Belia Islam (ABIM), 69 setting up of training courses, 94 142 09 Lim Index.indd 142 5/16/08 3:10:49 PM Index 143 BERJAYA Corporate Governance C institutional expansion of, Chartered Company Territory, 39 87–89 China BERJAYA party, 7, 56 education curriculum, 30 1981 State Elections, 78 China Borneo Company, -
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 -
Landslide Factors and Susceptibility Mapping on Natural and Artificial
Sains Malaysiana 46(9)(2017): 1531–1540 http://dx.doi.org/10.17576/jsm-2017-4609-23 Landslide Factors and Susceptibility Mapping on Natural and Artificial Slopes in Kundasang, Sabah (Faktor Tanah Runtuh dan Pemetaan Kerentanan ke atas Cerun Semula Jadi dan Buatan di Kundasang, Sabah) KAMILIA SHARIR, RODEANO ROSLEE, LEE KHAI ERN & NORBERT SIMON* ABSTRACT This study was carried out on the hilly topographic area in Kundasang, Sabah. This area is known to be extremely prone to landslides that occurred either naturally or by human interference to natural slopes. Aerial photographs interpretation was conducted in order to identify landslide distributions across three assessment years (2012, 2009 and 1984). These datasets were classified into two landslides groups based on their occurrences; natural and artificial. A total of 362 naturally occurring landslides were identified and another 133 are artificial slope landslides. Physical parameters which include lithology, slope angle, slope aspect and soil series were analyzed with each landslide group to examine the different influence of these parameters on each of the group. From the analysis, the landslide density for the natural landslide group shows that more than 35° slope angle and slope aspect facing east and southwest are prone to landslides. In terms of geological materials, high landslide density is recorded in the phyllite, shale, siltstone and sandstone lithologies group and the Pinosuk, Kepayan and Trusmadi soil series. In contrast, for the artificial slope landslide, high landslide density is observed in the 25°-35° slope angle and similar density in every slope aspect classes. The geological materials however have similar landslide density across their factors’ classes. -
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. -
The Importance of Orangutans in Small Fragments for Maintaining Metapopulation Dynamics
bioRxiv preprint doi: https://doi.org/10.1101/2020.05.17.100842; this version posted May 19, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. Version 1 (18 March 2020): this manuscript is a non-peer reviewed preprint shared via the BiorXiv server while being considered for publication in a peer-reviewed academic journal. Please refer to the permanent digital object identifier (https://doi.org/XXXX). Under the Creative Commons license (CC-By Attribution-Non Commercial-No Derivatives 4.0 International) you are free to share the material as long as the authors are credited, you link to the license, and indicate if any changes have been made. You may not share the work in any way that suggests the licensor endorses you or your use. You cannot change the work in any way or use it commercially. The importance of orangutans in small fragments for maintaining metapopulation dynamics Marc Ancrenaz1,2,3*, Felicity Oram3, Nardiyono4, Muhammad Silmi5, Marcie E. M. Jopony6, Maria Voigt7,8, Dave J.I. Seaman7, Julie Sherman9, Isabelle Lackman1, Carl Traeholt10, Serge Wich11,12, Matthew J. Struebig7, Truly Santika7,13,14, Erik Meijaard2,7,13 1HUTAN, Sandakan, Sabah, Malaysia 2Borneo Futures, Brunei Darussalam 3Pongo Alliance, Kuala Lumpur, Malaysia 4PT Austindo Nusantara Jaya Tbk., Jakarta 12950, Indonesia 5United Plantations berhad / PT Surya Sawit Sejati, -
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. -
Borneo Highlights
Borneo Highlights 12 Day Tour to Kota Kinabalu, Sandakan, Sepilok, Sukau Kinabatangan & Danum Valley Day 1 Arrival Kota Kinabalu Meal: Nil Welcome to Kota Kinabalu, Malaysia! Kota Kinabalu is the capital of the East Malaysian state of Sabah. Upon your arrival at Kota Kinabalu International Airport, you will be met and greet by our representative and chauffeured to your hotel. You are free at own leisure after check-in. Day 2 Kota Kinabalu Meal: B This morning is at leisure 1345hrs: Heritage Village and City Highlights: Visit the Heritage Village and Museum for a closer view of Sabah’s ethnic diversity highlighted by the unique local architectural styles of homes in North Borneo and the colourful costumes display. Then, proceed for a city drive by major landmarks such as the State & City Mosque, Tg. Aru Beach & Tun Mustapha Tower and the highest building the Sabah State Administration Centre. Mingle with the local people at the Handicraft Market before stopping by a typical water village to capture the essence of life in Kota Kinabalu. Day 3 Kota Kinabalu – Crocker Range Meal: B/L/D 0530hrs: The start of a two day trip which across the Crocker Range. Drive about 2 hours overland to Beaufort which lies on the coast to the South of Kota Kinabalu. Board Borneo's last remaining commercial train for the three hour journey to Tenom via the scenic Padas Gorge, passing tropical lowland rainforest, rubber plantations and native villages. Lunch at Tenom before visiting the Agricultural Park (closed on Mondays) at Lagud Sebrang, showcasing gardens, tropical fruits, beverage plants (e.g. -
Wong A. B. H., Chaw V. V., Fikri A. H., 2020 Land Use Effects On
Land use effects on Ephemeroptera, Plecoptera, and Trichoptera (EPT) communities in Ranau- Beluran District, Sabah, Malaysia 1Andrew B. H. Wong, 1Vi V. Chaw, 1,2Arman H. Fikri 1 Institute for Tropical Biology and Conservation, Universiti Malaysia Sabah, Sabah, Malaysia; 2 Water Research Unit, Universiti Malaysia Sabah, Sabah, Malaysia. Corresponding author: A. H. Fikri, [email protected] Abstract. Ephemeroptera, Plecoptera, and Trichoptera (EPT) are particularly sensitive and well suited as bioindicators for monitoring stream health. This study aims to investigate the EPT communities between disturbed and undisturbed areas of Ranau-Beluran District. Based on National Water Quality Standards of Malaysia, the sampled streams were categorized as Class I and II of water classes. Nonparametric Mann- Whitney test showed that only canopy cover was significantly different between disturbed and undisturbed sites. The sampled insects were dominated by Ephemeroptera (80.42%), followed by Plecoptera (14%) and Trichoptera order (5.58%). The Leptophlebiid family was the most abundant (44.82%). Family richness, the Simpson’s and Shannon-Weiner diversity indices all showed similar trends, EPT diversity being lower in disturbed sites. The diversity of EPT was strongly related to canopy cover. Key Words: benthic macroinvertebrates, bioassessment, Borneo, EPT, land uses. Introduction. For centuries, humans had relied on the resources near the aquatic environments for settlements, transportation, and water supply for domestic and agricultural use (Fang & -
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. -
8Th Euroseas Conference Vienna, 11–14 August 2015
book of abstracts 8th EuroSEAS Conference Vienna, 11–14 August 2015 http://www.euroseas2015.org contents keynotes 3 round tables 4 film programme 5 panels I. Southeast Asian Studies Past and Present 9 II. Early And (Post)Colonial Histories 11 III. (Trans)Regional Politics 27 IV. Democratization, Local Politics and Ethnicity 38 V. Mobilities, Migration and Translocal Networking 51 VI. (New) Media and Modernities 65 VII. Gender, Youth and the Body 76 VIII. Societal Challenges, Inequality and Conflicts 87 IX. Urban, Rural and Border Dynamics 102 X. Religions in Focus 123 XI. Art, Literature and Music 138 XII. Cultural Heritage and Museum Representations 149 XIII. Natural Resources, the Environment and Costumary Governance 167 XIV. Mixed Panels 189 euroseas 2015 . book of abstracts 3 keynotes Alarms of an Old Alarmist Benedict Anderson Have students of SE Asia become too timid? For example, do young researchers avoid studying the power of the Catholic Hierarchy in the Philippines, the military in Indonesia, and in Bangkok monarchy? Do sociologists and anthropologists fail to write studies of the rising ‘middle classes’ out of boredom or disgust? Who is eager to research the very dangerous drug mafias all over the place? How many track the spread of Western European, Russian, and American arms of all types into SE Asia and the consequences thereof? On the other side, is timidity a part of the decay of European and American universities? Bureaucratic intervention to bind students to work on what their state think is central (Terrorism/Islam)?