No 1 2 3 Cameron Highlands 4 5 6 7 8 9 10 11 12 13 14 15 16 NEGERI

Total Page:16

File Type:pdf, Size:1020Kb

No 1 2 3 Cameron Highlands 4 5 6 7 8 9 10 11 12 13 14 15 16 NEGERI NEGERI PAHANG SENARAI TAPAK BEROPERASI : 16 TAPAK Tahap Tapak No Kawasan PBT Nama Tapak Alamat Tapak (Operasi) 1 Bentong TP Padang Sertik Padang Sertik Bukan Sanitari 2 Bera TP Kg Chuat Kg Chuat, 28300 Kerayong Bukan Sanitari Jalan Cameron Highlands- 3 Cameron Highlands TP Blue Valley Bukan Sanitari Simpang Pulai 4 Jerantut TP Kuala Tahan, Tmn Negara Tmn Negara Kuala Tahan Bukan Sanitari Persimpangan Jabor - Jerangau, 5 Kuantan TP Jabor Jerangau Kuantan By-Pass, Gebeng, Bukan Sanitari Kuantan Lembaga 6 Pembangunan TP Kg Tekek TP Kg. Tekek, Pulau Tioman Bukan Sanitari Tioman (LPT) 7 Lipis TP Jln Lipis KM 8, Jln Lipis - Padang Tengku Bukan Sanitari Batu 55, Jalan Jerantut, 26500 8 Maran TP Maran, Batu 55 Bukan Sanitari Maran 9 Maran TP Jengka 10 26400 Bandar Jengka, Pahang Bukan Sanitari KM 9, Permatang Keledang, Jln 10 Pekan TP Keledang Bukan Sanitari Nenasi-Pekan 11 Pekan TP Kawasan Chini Jalan Chini - Ibam Bukan Sanitari Km 12, Jalan Cheroh, Raub, 12 Raub TP Cheroh Bukan Sanitari Pahang KM 5, Kg. Feri, 26800 Kuala 13 Rompin TP Kg Feri Bukan Sanitari Rompin, Pahang Jalan Segamat Kuantan, 14 Rompin TP Perwira Jaya Bukan Sanitari berhampiran Balai Pejabat Hutan 15 Rompin TP Muadzam Shah Jalan Muadzam Shah - Bukit Iban Bukan Sanitari Simpang masuk Bandar Tun 16 Rompin TP Bdr Tun Razak Bukan Sanitari Razak NEGERI PAHANG SENARAI TAPAK TIDAK BEROPERASI : 16 TAPAK Tahap Tapak No Kawasan PBT Nama Tapak Alamat Tapak (Operasi) 1 Bentong TP Sg Sematut Sungai Sematut, Bentong Bukan Sanitari 2 Bentong TP Kg Lebak Kg Lebak, Chamang, Bentong Bukan Sanitari Bt. 34 3/4, Jalan Tapah - 3 Cameron Highlands TP MDCH Bukan Sanitari Cameron Highlands Batu 58, Jalan Kuantan, 27000 4 Jerantut TP Batu 57 Bukan Sanitari Jerantut 5 Jerantut TP Kg Sg Lekok Kg Sg Lekok, Jerantut Bukan Sanitari Batu 1, Kampung Mat Kilau, 6 Jerantut TP Kg Mat Kilau Bukan Sanitari 27000 Jerantut 7 Kuantan TP Tmn Bandar Taman Bandar, Kuantan, Pahang Bukan Sanitari KM 35, Jln. Besar, Kuantan 8 Kuantan TP Gambang Bukan Sanitari Termeloh Indera Mahkota, Jalan Gebeng, 9 Kuantan TP Indera Mahkota Bukan Sanitari Kuantan 10 Kuantan TP Atabara Km 8, Jalan Sungai Lembing Bukan Sanitari 11 Lipis TP Mela Jln. Kampung Jani, Mela Bukan Sanitari Merapoh, Mukim Batu Yon, Kuala 12 Lipis TP Merapoh Bukan Sanitari Lipis 3 KM Dari Kawasan Perindustrian 13 Lipis TP Sisa Industri Kayu Kechau Bukan Sanitari Kechau Tui 14 Lipis TP Mukim Ulu Jelai Jalan Lama Sungai Koyan - Betau Bukan Sanitari Lot 9815 dan 6016, Kg. Ruan, 15 Raub TP Sg Ruan Bukan Sanitari Raub Jalan By-Pass Temerloh, 16 Temerloh TP Ulu Tualang Bukan Sanitari Mentakab.
Recommended publications
  • MALAYSIA the Kampung Kuantan Firefly Reserve Jamil Bin
    MALAYSIA The Kampung Kuantan Firefly Reserve Jamil bin Hamzah and Suzana Mohkeri Wetlands International-Asia Pacific INTRODUCTION Malaysia is comprised of 13 federal states with Kuala Lumpur as the federal capital situated in the Federal Territory. Eleven states are in West Malaysia (also known as Peninsular Malaysia) and two states are situated in Borneo Island. Selangor is one of the most highly developed and urbanized states in Malaysia. However, there are still large areas of forested lands scattered throughout the state either under forest reserves, owned by the state, private companies or private landowners. Since the beginning of civilization rivers have been the most important source of food, water resources and transportation. In Malaysia, human settlement always related or concentrated along the rivers. Sungai Selangor (Selangor River), is one of the main rivers in the state of Selangor. The headwater of Sungai Selangor originates from the highland area of the Titiwangsa Range, which is part of the Main Range, the backbone of Peninsular Malaysia. It is an important source of water supply for domestic and agriculture use and fishing industries for people living along the riverbanks. Sungai Selangor flows mainly through oil palm estates and small villages and it does not pass through any major towns. Thus the riparian vegetation along the riverbanks is still intact. According to a report prepared by the Department of Environment, Sungai Selangor river basin is listed as one of the two cleanest rivers in Selangor (Environmental Quality Report, 1996). This river is highlighted here not because of its important food and water resources but of its ecotourism factor.
    [Show full text]
  • FH 2019 10 Ir.Pdf
    PHYSICAL IMPACT INDICATORS FOR MOUNTAIN TRAILS AT GUNUNG TAHAN TRAIL, MALAYSIA SAM SHOR NAHAR BIN YAAKOB FH 2019 10 PHYSICAL IMPACT INDICATORS FOR MOUNTAIN TRAILS AT GUNUNG TAHAN TRAIL, MALAYSIA UPM By SAM SHOR NAHAR BIN YAAKOB COPYRIGHT Thesis Submitted to the School of Graduate Studies, Universiti Putra Malaysia, in Fulfillment of Requirements for the Degree of Doctor of © Philosophy March 2019 All material contained within the thesis, including without limitation text, logos, icons, photographs and all other artwork, is copyright material of Universiti Putra Malaysia unless otherwise stated. Use may be made of any material contained within the thesis for non-commercial purposes from the copyright holder. Commercial use of material may only be made with the express, prior, written permission of Universiti Putra Malaysia. Copyright © Universiti Putra Malaysia UPM COPYRIGHT © Abstract of thesis presented to the Senate of Universiti Putra Malaysia in fulfillment of the requirements for the degree of Doctor of Philosophy ABSTRACT PHYSICAL IMPACT INDICATORS FOR MOUNTAIN TRAILS AT GUNUNG TAHAN TRAIL, MALAYSIA By SAM SHOR NAHAR BIN YAAKOB March 2019 UPM Chairman: Associate Professor Azlizam bin Aziz, PhD Faculty: Forestry Mountain trekking in Malaysia has been growing in popularity as evident from the increasing number of trekkers to popular mountain tops in the country. Mountain trails are usually the most practical access to these mountain tops. These trails are usually subjected to various physical impacts as they are extensively used by the trekkers. Thus, indicators are needed if physical impacts at the mountain trails are to be managed. This study was conducted to determine suitable physical impact indicators for mountain trails in Malaysia.
    [Show full text]
  • 6 Existing Environment
    Environmental Impact Assessment: Proposed Onsite Secure Landfill (Prescribed Premise) for the Storage of NUF Solids within the Existing LAMP Site located on PT 17212, Gebeng Industrial Estate, Kuantan, Pahang 6 EXISTING ENVIRONMENT 6.1 INTRODUCTION This section provides a description of the physical, chemical, biological and social aspects of the environment within the Zone of Impact (ZOI) of the proposed secure landfill Project. It highlights the components of environmental concerns of the Project site and its surroundings. The term ZOI is used to describe the area most likely to be impacted by the Project. The ZOI represents the surrounding area within a 5 km radius from the boundary of the LAMP site. The information provided within this chapter forms the basis of the impact assessment in Chapter 7. The description provided in this chapter is based on site visits and environmental monitoring data at the LAMP site, undertaken by Permulab (M) Sdn. Bhd., a laboratory accredited by the Department of Standards, Malaysia under the Skim Akreditasi Makmal Malaysia (SAMM), Malaysian Meteorological Department and publications by DOE, Kuantan Municipal Council, Pihak Berkuasa Perancang Tempatan (PBPT) Daerah Kuantan. Data from past studies, including the “Preliminary EIA and Quantitative Risk Assessment of the Proposed Advanced Materials Plant in Gebeng Industrial Area, Kuantan, Pahang, by Enviro Sdn Bhd, 2007” was also referenced. 6.2 TOPOGRAPHY Regionally, the GIE is located in the Kemajuan Tanah Merah area where Bukit Tanah Merah was flattened to construct the industrial estate. The GIE is located within the low-lying and predominantly swampy Sungai Balok catchment area with an average land elevation of 7m above mean sea level.
    [Show full text]
  • Sedimentary Sequence in the Subsurface of the Pekan Coastal Plain, Pahang
    Geological Society of Malaysia Annual Geological Conference 2002 May 26 - 27, Kota Bharu, Kelantan, Malaysia Sedimentary sequence in the subsurface of the Pekan coastal plain, Pahang CHE AzIzALI Program Geologi, Fakulti Sains dan Teknologi Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor Abstract: The Pekan coastal plain in which the Pahang river delta is located is made up of a thick sequence of unconsolidated sedimentary sequence of an unnamed formation. Drilling programmes carried out in the area show that the unconsolidated sequence was deposited during two major periods of sedimentation that took place in two different setting. The lower sequence which has been interpreted to have been deposited during the Pleistocene period consists of entirely continental sediment. The continental sequence can be devided into several packages according to their depositional trends and the boundary of each package is marked by an apparent depositional break. The sea-level rise during the early Holocene period have resulted in deposition of a series of marinel marine-influenc~d sediments at the top of the sequence. Abstrak: Dataran pantai Pekan yang di dalamnya terletak delta Sungai Pahang dibentuk oleh satu jujukan sedimen takterkonsolidasi yang tebal yang setakat ini tidak begitu jelas nama formasinya. Program penggerudian yang dilakukan di kawasan tersebut menunjukkan bahawa sedimen takterkonsolidasi tersebut telah dimendapkan pada period yang berlainan dan berlaku di dalam setting yang berbeza. Jujukan bawah yang telah ditafsirkan· telah dimendapkan semasa Pleistosen terdiri daripada sedimen daratan. Jujukan sedimen daratan tersebut boleh dibahagikan kepada dua pakej pemendapan yang setiap satunya di pisahkan dari pada yang lain oleh rumpang pemendapan. Peningkatan paras laut semasa awal Holosen telah mengakibatkan pemendapan satu siri sedimen lautanldipengaruhi lautan di abahagian atas jujukan.
    [Show full text]
  • CBD Sixth National Report
    SIXTH NATIONAL REPORT OF MALAYSIA to the Convention on Biological Diversity (CBD) December 2019 i Contents List of Figures ............................................................................................................................................... iv List of Tables ................................................................................................................................................ vi List of Acronyms ........................................................................................................................................... vi Foreword ..................................................................................................................................................... vii Preamble ....................................................................................................................................................... 1 EXECUTIVE SUMMARY .................................................................................................................................. 3 CHAPTER 1: UPDATED COUNTRY BIODIVERSITY PROFILE AND COUNTRY CONTEXT ................................... 1 1.1 Malaysia as a Megadiverse Country .................................................................................................... 2 1.2 Major pressures and factors to biodiversity loss ................................................................................. 3 1.3 Implementation of the National Policy on Biological Diversity 2016-2025 ........................................
    [Show full text]
  • Geology of the Rompin–Endau Area, Pahang Darul Makmur–Johor Darul
    144 GEOLOGICAL SOCIETY OF MALA YSIA -ANNUAL GEOLOGICALCONFERENCE 1991 Geology of the Rompin-Endau area, Pahang Darul Makmur-Johor Darul Takzim M.B. MUNAWIRI, M.B. IDRIS2 & N.B. NORAZLAM2 lDepartment of Geology, University of Malaya, 59100 Kuala Lumpur 2Sarawak Shell Berhad, Lutong, Miri Sarawak Three main rock types are found in the Rompin-Endau area. These are volcanics, igneous intrusives and sedimentary sequences. Metamorphic rocks occur only at Gunung Lesong. The votcanic rocks are referred to as the Jasin volcanics and represent the oldest rocks of the area, probably of Mid-Permian to Triassic age. Some of these rhyolites are also mylonitised. A granite batholith found on the western flank of the area can be termed a biotite-adamellite granite. This granite pluton which has intruded the volcanic rocks, is similar to those found in other parts of the Ulu Endau area and has been dated to be of Late Triassic Age. On the eastern plateau, sedimentary sequences of sandstone, shale, siltstone and mudstone overly the volcanics. A similar sequence of sediment is seen capping the granite hill 1448 on the western side, forming a mesa. These sediments are referred to as the Tebak Formation which is of continental origin and exhibits subhorizontal dips. Plant fossils were recorded from light grey mudstone beds in the tributaries of Sungai Telentang, and a boulder of silicified wood was found in Sungai Anak Seladang on the western flank of Sungai Kinchin. The plant fossil has been identified as Frenelopsis malaine Ko' ono, which is a foliage of a conifer plant, giving an age of Upper Jurassic - Lower Cretaceous.
    [Show full text]
  • TITLE Fulbright-Hays Seminars Abroad Program: Malaysia 1995
    DOCUMENT RESUME ED 405 265 SO 026 916 TITLE Fulbright-Hays Seminars Abroad Program: Malaysia 1995. Participants' Reports. INSTITUTION Center for International Education (ED), Washington, DC.; Malaysian-American Commission on Educational Exchange, Kuala Lumpur. PUB DATE 95 NOTE 321p.; Some images will not reproduce clearly. PUB TYPE Guides Non-Classroom Use (055) Reports Descriptive (141) Collected Works General (020) EDRS PRICE MFO1 /PC13 Plus Postage. DESCRIPTORS Area Studies; *Asian History; *Asian Studies; Cultural Background; Culture; Elementary Secondary Education; Foreign Countries; Foreign Culture; *Global Education; Human Geography; Instructional Materials; *Non Western Civilization; Social Studies; *World Geography; *World History IDENTIFIERS Fulbright Hays Seminars Abroad Program; *Malaysia ABSTRACT These reports and lesson plans were developed by teachers and coordinators who traveled to Malaysia during the summer of 1995 as part of the U.S. Department of Education's Fulbright-Hays Seminars Abroad Program. Sections of the report include:(1) "Gender and Economics: Malaysia" (Mary C. Furlong);(2) "Malaysia: An Integrated, Interdisciplinary Social Studies Unit for Middle School/High School Students" (Nancy K. Hof);(3) "Malaysian Adventure: The Cultural Diversity of Malaysia" (Genevieve M. Homiller);(4) "Celebrating Cultural Diversity: The Traditional Malay Marriage Ritual" (Dorene H. James);(5) "An Introduction of Malaysia: A Mini-unit for Sixth Graders" (John F. Kennedy); (6) "Malaysia: An Interdisciplinary Unit in English Literature and Social Studies" (Carol M. Krause);(7) "Malaysia and the Challenge of Development by the Year 2020" (Neale McGoldrick);(8) "The Iban: From Sea Pirates to Dwellers of the Rain Forest" (Margaret E. Oriol);(9) "Vision 2020" (Louis R. Price);(10) "Sarawak for Sale: A Simulation of Environmental Decision Making in Malaysia" (Kathleen L.
    [Show full text]
  • Persatuan Geologi Malaysia
    KDN 0560/82 ISSN 0126/5539 PERSATUAN GEOLOGI MALAYSIA NEWSLETTER OF THE GEOLOGICAL SOCIETY OF MALA VSIA Jil. 8, No.6 (Vol. 8, No.6) Nov- Dis 1982 KANDUNGAN (CONTENTS) CATATAN GEOLOGI (GEOLOGICAL NOTES) G .B. Ong & P.H. Stauffer: A large prehistoric landslide near Raub, Pahang, Peninsular Malaysia 253 H.D. Tjia: Disharmonic folds at Tanjung Mat Amin, Trengganu 258 Perbincangan (Discussion) C.S. Hutchison: A chromium-nickel laterite in Bukit Punggor, Malacca, Peninsular Malaysia-A Discussion 260 B.K. Tan: A chromium-nickel laterite in Bukit Punggor, Malacca, Peninsular Malaysia-A Reply 263 PERHUBUNGAN LAIN (OTHER COMMUNICATIONS) S.K. Yong: Peninsular Malaysia Place-names 264 PERTEMUAN PERSATUAN (MEETINGS OF THE SOCIETY) C.R. Jones: Geological and mineral exploration of the Kalahari, SW Africa 268 ROCKCON Training Course and Symposium-Report & Abstracts 268 Petroleum Geology Seminar '82-Report & Abstracts 287 BERITA PERSATUAN (NEWS OF THE SOCIETY) GEOSEA V-First Circular 299 Forthcoming GSM Bulletins 302 GSM 2-year Councillors 1983/84-election results 303 Keahlian (Membership) 303 Pertukaran Alamat (Change of Address) 303 BERIT A-BERIT A LAIN (OTHER NEWS) Universiti Sains Malaysia M.Sc. Theses 304 Universiti Teknologi Malaysia B.Sc. Theses 1981 /82 304 Carigali and Carigali-BP strike oil in Malaysia 304 Overseas Research Students ORS Awards 1983 307 XVIII General Assembly of IUGG 308 10th International Geochemical Exploration Symposium 310 Coastal Evolution in the Holocene- International Symposium 310 Techniques for Hydrologic Investigation 311 Kursus-kursus Latihan (Training Courses) 314 Kalendar (Calendar) 316 DIKELUARKAN DWIBULANAN ISSUED BIMONTHLY ;' PERSATUAN GEOLOGI MALAYSIA (GEOLOGICAL SOCIETY OF MALAYSIA) Majlis (Council) 1982/83 Pegawai-pegawai (Officers) Presiden Khoo Teng Tiong, Jabatan Geologi, (President) Universiti Malaya, Kuala Lumpur Naib Presiden Leong Khee Meng, Carigali-BP, (Vice-President) P.O.
    [Show full text]
  • 20Th December 2006
    REPORT ON HEAVY RAINFALL THAT CAUSED FLOODS IN JOHOR, MELAKA, NEGERI SEMBILAN AND PAHANG DURING THE PERIOD th th 17 – 20 DECEMBER 2006 PREPARED BY: RESEARCH DIVISION MALAYSIAN METEOROLOGICAL DEPARTMENT MINISTRY OF SCIENCE, TECHNOLOGY AND INNOVASION 21st DECEMBER 2006 1. Introduction Cold surges emanating from high-pressure system over Siberia was the main factor of the intensification in northeasterly wind speed over the South China Sea on 16th December 2006. This enhanced the cyclonic wind shear over our region, mainly over the southern Peninsular Malaysia from the 17th until 20th December 2006. This caused Johor, Pahang, Negeri Sembilan and Malacca to experience heavy rainfall. 2. Analysis of rainfall from the 16th until the 20th of December 2006 Table 1: Daily Rainfall (mm) from the 16th until the 20th of December 2006 Saturday Sunday Monday Tuesday Wednesday State Station Total 16/12/06 17/12/06 18/12/06 19/12/06 20/12/2006 Batu Pahang Embun 15.0 8.8 7.0 30.6 40.0 101.4 Kuantan 28.0 80.0 84.2 79.2 189.0 460.4 Muadzam Shah 21.6 35.8 173.8 211.6 125.0 567.8 Temerloh 9.0 4.6 21.4 10.8 21.0 66.8 Johor Batu Pahat 0.8 10.8 93.4 71.6 2.0 178.6 Senai 46.4 94.6 128.0 236.0 40.0 545.0 Kluang T 53.2 126.8 266.0 18.0 464.0 Mersing 0.8 1.8 7.4 133.6 6.0 149.6 Melaka Melaka 1.6 17.2 63.2 89.8 10.0 181.8 Table 2: December Accumulated Rainfall (1/12/2006-20/12/2006) in comparison with the Monthly Accumulated Mean.
    [Show full text]
  • Satellite Rainfall (TRMM 3B42-V7) Performance Assessment and Adjustment Over Pahang River Basin, Malaysia
    remote sensing Article Satellite Rainfall (TRMM 3B42-V7) Performance Assessment and Adjustment over Pahang River Basin, Malaysia Siti Najja Mohd Zad 1, Zed Zulkafli 1,* ID and Farrah Melissa Muharram 2 ID 1 Department of Civil Engineering, Faculty of Engineering, Universiti Putra Malaysia, 43400 Serdang, Malaysia; [email protected] 2 Department of Agriculture Technology, Faculty of Agriculture, Universiti Putra Malaysia, 43400 Serdang, Malaysia; [email protected] * Correspondence: [email protected] Received: 26 December 2017; Accepted: 23 February 2018; Published: 2 March 2018 Abstract: The Tropical Rainfall Measuring Mission (TRMM) was the first Earth Science mission dedicated to studying tropical and subtropical rainfall. Up until now, there is still limited knowledge on the accuracy of the version 7 research product TRMM 3B42-V7 despite having the advantage of a high temporal resolution and large spatial coverage over oceans and land. This is particularly the case in tropical regions in Asia. The objective of this study is therefore to analyze the performance of rainfall estimation from TRMM 3B42-V7 (henceforth TRMM) using rain gauge data in Malaysia, specifically from the Pahang river basin as a case study, and using a set of performance indicators/scores. The results suggest that the altitude of the region affects the performances of the scores. Root Mean Squared Error (RMSE) is lower mostly at a higher altitude and mid-altitude. The correlation coefficient (CC) generally shows a positive but weak relationship between the rain gauge measurements and TRMM (0 < CC < 0.4), while the Nash-Sutcliffe Efficiency (NSE) scores are low (NSE < 0.1).
    [Show full text]
  • Malaya Annual Conference Methodist Episcopal Church Held in Singapore, January 1938
    , • oS ......; I ",", 0, Al J.. -I r, C~1 MINUTES OF THE MALAYA ANNUAL CONFERENCE METHODIST EPISCOPAL CHURCH HELD IN SINGAPORE, JANUARY 1938 WESLEY CHUR C H, SINGAPORE TABLE OF CONTENTS I. OFFICERS OF TEE ANNUAL CONFERENCE S II. BOARDS, COMMISSIONS AND COMMITTEES 4 Special Committees , .. 6 III. DAILY PROCEEDINGS 7 IV. DISCIPLINARY QUESTIONS 18 Certificate of Ordination 25 V. APPOINTMENTS 26 Special Appointments 34 Secretary's Certi1lcate 34 VI. REPORTS: (a) District Superintendents Singapore District-R. L. Archer 3!S Sibu District-Lee Hock Hiang 38 Central lI[alaya District-Abel Eklund 40 Central Tamil District-P. L. Peach 43 &erik! District-Wong King Hwo 46 Southern Tamil District-S. S. Pakianathan 47 Penang-Ipoh District-I Dodsworth 49 (b) Standing Committees and Boards Committee on Public Morals 55 Committee on Evangelism 55 Committee on Resolutions 56 Committee on the State of the Church 57 Committee on Home ][issions 57 Conference Board of Stewards 60 STATISTICS Summary of Kalaya Annual Conference and Malaysia Chinese Mission Conference Statistics 64 Statistical Beport of Malaya Annual Conference Inserted Statistics for Educational Institutions Inserted Statistician's Recapitulation Report Inserted Conference Treasurer's Report 66 VII. lIlISCELLANEOUS Recommendations of Committee on Christian Literature 67 General Report on Girls' Schools 67 Report of the Malaysia Commission on Beligious Education for 1937 69 VIII. ROLL OF THE DEAD 73 Memoirs 74 IX. HISTORICAL Conference Sessions 77 Chronol~gical Boll 78 Retired Ministers 79 .MINUTES OF THE FOR TY -SIXTH SESSION MALAYA ANNUAL CONFERENCE .METHODIST EPISCOPAL CHURCH HELD IN WESLEY CHURCH SINGAPORE, STRAITS SETTLEMENTS, MALAYA JANUARY 6, TO 12, I938 PUBLISHED BY SECRETARY, MALAYA ANNUAL CONFERENCE FIVE, FORT CANNING ROAD -.
    [Show full text]
  • Conglomerate from Setia Jasa Near Temerloh, Pahang, Peninsular Malaysia: Its Stratigraphic Position and Depositional Environment
    Geological Society of Malaysia Annual Geological Conference 2001 June 2-3 2001, Pangkor island, Perak Darul Ridzuan, Malaysia Conglomerate from Setia Jasa near Temerloh, Pahang, Peninsular Malaysia: Its stratigraphic position and depositional environment MoHo SHAFEEA LEMAN1 AND MASATOSHI SoNE2·* 1Geology Programme, School of Environmental Science and Natural Resources, Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor, Malaysia 2lnstitute for Environment and Development (LESTARI), Universiti Kebangsaan Malaysia, 43600 Bangi, Selangor, Malaysia 'Present address: Asia Centre, University of New England, Armidale, NSW 2351, Australia Abstract: A thick sequence of conglomerate, tuffaceous sandstone and shale/mudstone largely exposed at the Setia Jasa area is described. The matrix-supported conglomerate of very well rounded clasts conformably overlies pebbly mudstone and shows a gradual change in matrix grain size from clay to sand. An Anisian (early Middle Triassic) age is indicated for a whole sequence by the presence of an ammonoid Paraceratites sp. found in a lower shale bed. Sedimentological features suggest that the conglomerate and underlying sandstone/shale sequences were possibly deposited in a relatively deep marine environment, and probably belong to the Semantan Formation. Abstrak: Satu jujukan tebal konglomerat, batu pasir bertuf dan syallbatu lumpur yang tersingkap di kawasan Setia Jasa diperihalkan di sini. Konglomerat sokongan matriks dengan klasta sangat bulat didapati menindih batu lumpur berpebel dan menunjukkan perubahan berterusan matriks dari saiz lumpur ke saiz pasir. Keseluruhan jujukan ditafsirkan berusia Anisian (Trias Tengah) berdasarkan kehadiran fosil amonoid Paraceratites sp. yang ditemui dalam syal di bawahnya. Bukti-bukti sedimentologi mencadangkan bahawa jujukan konglomerat dan jujukan batu pasir-syal di bawahnya mungkin diendapkan di sekitaran laut yang agak dalam dan mungkin merupakan sebahagian daripada Formasi Semantan.
    [Show full text]