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Rainfall Forecasting with Time Series Model in Alor Setar, Kedah
Universiti Malaysia Terengganu Journal of Undergraduate Research eISSN: 2637-1138 Volume 3 Number 1, January 2021: 37-44 © Penerbit UMT RAINFALL FORECASTING WITH TIME SERIES MODEL IN ALOR SETAR, KEDAH FAIQAH MOHAMAD FUDZI*, ZAHAYU MD YUSOF AND MASNITA MISIRAN School of Quantitative Sciences, Universiti Utara Malaysia, 06010 UUM Sintok, Kedah, Malaysiaa Institute of Strategic Industrial Decision Modelling, School of Quantitative Sciences, Universiti Utara Malaysia, 06010 UUM Sintok Kedah, Malaysiab Centre for Testing, Measurement and Appraisal, Universiti Utara Malaysia, 06010 UUM Sintok, Kedah, Malaysiac * Corresponding author: [email protected] http://doi.org/10.46754/umtjur.2021.01.005 Abstract: The prediction of rainfall on monthly and seasonal time scales is not only scientifically challenging but is also important for planning and devising agricultural strategies. In this paper, the study is conducted to examine the pattern of monthly rainfall in Alor Setar, Kedah within ten years which is from 2008 to 2018. This paper considered a model based on real data that obtained from Department of Meteorology Malaysia. This study indicates that the monthly rainfall in Alor Setar has a seasonal and trend pattern based on yt vs t plotting, autocorrelation function and Kruskal Wallis Test for seasonality. The examined rainfall time-series modelling approaches include Naïve Model, Decomposition Method, Holt-Winter’s and Box-Jenkins ARIMA. Multiplicative Decomposition Method was identified as the best model to forecast rainfall for the year of 2019 by analysing the previous ten-year’s data (2008-2018). As a result from the forecast of 2019, October is the wettest month with highest forecasted rainfall of 276.15mm while the driest month is in February with lowest forecasted rainfall of 50.55mm. -
S813219 Abstract.Pdf
ASPEK PERANCANGAN BANDAR YANG MEMPENGARUHI REBRANDING BANDARAYA ALOR SETAR DALAM KONTEKS PELANCONGAN MOHD YUSRI BIN MD DAUD SARJANA SAINS (PENGAJIAN STRATEGIK) UNIVERSITI UTARA MALAYSIA 06010 SINTOK, KEDAH DARUL AMAN MEI 2014 ASPEK PERANCANGAN BANDAR YANG MEMPENGARUHI REBRANDING BANDARAYA ALOR SETAR DALAM KONTEKS PELANCONGAN MOHD YUSRI BIN MD DAUD Tesis ini dihantar ke Pusat Pengajian Siswazah, Universiti Utara Malaysia (UUM) bagi memenuhi syarat memperolehi Sarjana Sains (Pengajian Strategik) ii PERAKUAN HAKCIPTA Hakcipta terpelihara. Tidak dibenarkan mengeluarkan ulang dan atau membuat salinan mana-mana bahagian, bab, ilustrasi atau isi kandungan ilmiah ini dalam apa jua bentuk dan dengan cara apa jua pun sama ada secara elektronik, fotokopi, makanika, rakaman atau cara lain sebelum mendapat kebenaran bertulis daripada Kolej Undang-Undang, Kerajaan dan Pengajian Antarabangsa. iii PERAKUAN PELAJAR Dengan ini, saya Mohd Yusri Bin Md Daud (813219), mengakui bahawa kajian ini adalah hasil nukilan saya sendiri kecuali petikan, huraian dan ringkasan yang terdapat di dalamnya yang telah dinyatakan sumbernya. Tarikh : ________________ ________________________ Tandatangan Pelajar iv KEBENARAN MERUJUK TESIS Kajian ini dikemukakan sebagai memenuhi syarat pengijazahan Sarjana Sains (Pengajian Strategik), Universiti Utara Malaysia. Saya bersetuju memberi kebenaran kepada pihak perpustakaan university ini untuk mempamerkannya sebagai rujukan. Saya juga bersetuju bahawa sebarang salinan sama ada secara keseluruhan atau sebahagian daripada kajian ini untuk tujuan akademik adalah dibolehkan dengan kebenaran penyelia tesis atau Dekan Pusat Pengajian Siswazah, Kolej Undang-undang, Kerajaan dan Pengajian Antarabangsa (COLGIS). Sebarang bentuk salinan dan cetakan bagi tujuan komersil dan membuat keuntungan adalah dilarang sama sekali tanpa kebenaran bertulis daripada penyelidik. Pernyataan rujukan kepada penulis dan Universiti Utara Malaysia perlulah dinyatakan jika sebarang bentuk dibuat ke atas kajian ini. -
518 [LOG 23] LEVEL of GAS EMISSIONS by HEAVY-DUTY TRUCKS at CROSS BORDER CHECKPOINTS BUKIT KAYU HITAM, KEDAH Kamal Imran Mohd Sh
[LOG 23] LEVEL OF GAS EMISSIONS BY HEAVY-DUTY TRUCKS AT CROSS BORDER CHECKPOINTS BUKIT KAYU HITAM, KEDAH Kamal Imran Mohd Sharif1, Nik Nurul Ain Nik Ya2, Fatimatuzzahrah Azmil3 & Raidah Mohd Shah4 1-4School of Technology Management and Logistics, College of Business, Universiti Utara Malaysia, 06010 UUM Sintok, Kedah [email protected], [email protected], [email protected], [email protected] ABSTRACT Transportation has become an integral part of the economy and a vital as a daily activities which means it is also an essential things towards source of greenhouse gas emissions. This research seek to investigate about level of gas emissions by heavy-duty trucks at Cross Border Checkpoints, Bukit Kayu Hitam, Kedah Darul Aman, Malaysia. Basically, the gas emissions that produces by heavy-duty trucks is increasing until contribute into environmental and physical impacts. For this purpose, the study objective is to calculate the level of gas emissions rate by interpreting in three types of chemical component. It includes of carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O). In the present work, the calculation and estimation of chemical component defined by grams per mile (g/mi). The data collected from Cross Border Checkpoints, Bukit Kayu Hitam, Kedah, Malaysia that will be obtained to shows in the result. In that part, a strategies and recommendations has been made to solve the gas emissions by heavy-duty trucks problems from being erupted. This paper can be used as a platform for future research in area of sustainability in green transportation. Keywords: level of gas emissions, chemical component, physical impacts, environmental, sustainability, green transportation BACKGROUND OF STUDY Cross Border Checkpoints, Bukit Kayu Hitam is stated in Kedah’s which is as a main border of Malaysia and Thailand. -
A Gravity Survey of Perlis, Kedah and Penang
Geol. Soc. Malaysia, Bulletin 26, April 1990; pp. 13 - 20 A gravity survey of Perlis, Kedah and Penang ALAN J. BURLEY AND JAMALUDIN OTHMAN Geological Survey of Malaysia, P.O. Box 1015, 30820 Ipoh. Abstract: The results of a gravity survey of northwest Peninsular Malaysia are pre sented, forming the fIrst stage of a survey of the whole Peninsula. The aim is to obtain as uniform a coverage as possible, initially using 4WD vehicles and boats for transport. At a later stage it is anticipated that areas not otherwise accessible will be reached using a helicopter. The results can be largely explained in terms of the confIguration of granitic rocks. A steep gravity gradient follows approximately the boundary of the Main Range granite in a series ofen echelon northwest and northeast trending sections. The extent and steepness of the gradient along some sections implies steeply dipping contacts between granite and sediments extending to depths of a few kilometres. It is steepest along the section coinciding with the Bok Bak fault, for which there is some indication of a possible extension northwestwards into Perlis: here it could have influenced the deposition ofthe Tertiary Bukit Arang coal beds, which show a signifIcant gravity response. If there has been major lateral movement along this fault and/or faults parallel to it, a net sinistral displacement of about 30 kilometres is suggested by the gravity results. The Gunung J erai granite is shown to be much more extensive underground than at outcrop, and the results show that the Pulau Pinang, Kulim and Main Range granites are all connected at relatively shallow levels. -
ALAMAT PEJABAT JAWATAN DAN NAMA TELEFON/E-MEL
LEMBAGA HASIL DALAM NEGERI MALAYSIA DIREKTORI LHDNM ALAMAT PEJABAT JAWATAN DAN NAMA TELEFON/e-MEL KEDAH / PERLIS PEJABAT PENGARAH NEGERI PENGARAH T.T.: 04-7344100 SAMB.: 140000 LEVEL 6 & 7, MENARA BDB AMNAH BT. TAWIL e-mel: [email protected] 88, LEBUHRAYA DARULAMAN 05100 ALOR SETAR SETIAUSAHA SAMB.: 140001 KEDAH DARUL AMAN RUHAINAH BT. MUHAMAD TEL. AM : 04-7334100 PEGAWAI PERHUBUNGAN AWAM SAMB.: 140026 FAKS : 04-7334101 BALKHIS BT. ROSLI e-mel: [email protected] CAWANGAN ALOR SETAR PENGARAH T.T.: 04-7400280 SAMB.: 140111 WISMA HASIL, ROSIDE B. JANSI e-mel: [email protected] KOMPLEKS PENTADBIRAN KERAJAAN PERSEKUTUAN, BANDAR MUADZAM SHAH, SETIAUSAHA SAMB.: 140444 06550 ANAK BUKIT, AZLIZA BT. ZAINOL KEDAH DARUL AMAN TEL. AM : 04-7400100 TIMBALAN PENGARAH SAMB.: 140333 FAKS : 04-7329481 HAFSAH BT. MOHD NOOR e-mel: [email protected] PEGAWAI PERHUBUNGAN AWAM T.T.: 04-7400250 SAMB.: 140131 NURAZURA BT. MOHD YUSOF e-mel: [email protected] CAWANGAN SUNGAI PETANI PENGARAH T.T.: 04-4449720 SAMB.: 140600 MENARA HASIL NORAZIAH BT. AHMAD e-mel: [email protected] JALAN LENCONGAN TIMUR BANDAR AMAN JAYA 08000 SUNGAI PETANI, KEDAH SETIAUSAHA SAMB.: 140601 MASLINDA BT. MUKHTAR TEL. AM : 04-4456000 TIMBALAN PENGARAH T.T.: 04-4449730 SAMB.: 140673 WAN NOOR MAZUIN BT. WAN ARIS PEGAWAI PERHUBUNGAN AWAM T.T.: 04-4449772 SAMB.: 140726 NOOR FAZLLYZA BT. ZAKARIA e-mel: [email protected] [email protected] CAWANGAN SIASATAN ALOR SETAR PENGARAH T.T.: 04-7303987 SAMB.: 140501 ARAS 3, WISMA PERKESO MD. FAHMI BIN MD. SAID e-mel: [email protected] BANGUNAN MENARA ZAKAT JALAN TELOK WANJAH 05200 ALOR SETAR SETIAUSAHA SAMB.: 140504 KEDAH NORHAYATI BT. -
Malaysia Singapore & Brunei
© Lonely Planet 207 Kedah & Perlis Tucked into Malaysia’s northwest corner are two states that fairly drip with greenness and fertility: Kedah and Perlis. If Kuala Lumpur is Malaysia at its most frenetically developed, and Borneo the nation at its wildest and ruggedest, this is the country’s, well, country: not paved, not jungled over, but cultivated, cared for and landscaped into a horizon of looping emerald ridges. Limestone pillars thrust up through this paddyscape and peasants dot it, the latter contributing to the harvest of over half of Malaysia’s domestic rice supply. Not that many foreigners see all this. While it may be one of the most touristed states in Malaysia, most travellers would draw a blank if you asked them anything about ‘Kedah.’ That’s because almost everyone knows it by its biggest island and Malaysia’s number one holiday destination: Pulau Langkawi. One of those postcard places where life is a cruise ship commercial starring you, Langkawi is also a living island where there’s a fair bit to explore beyond the beach, although no one will fault you for losing a few days (Weeks? Months? Langkawi has that effect…) on the sand. Langkawi’s duty-free status also makes it popular with a certain kind of shopper, and it’s not uncommon to see folks leaving the island with tanned arms busting with cartons of Marlboros. Perlis is the smallest state in Malaysia; physically and culturally it borders Kedah. It’s also proximate to Thailand, and most travellers rush through here on their way to that kingdom. -
Turkish Online Journal of Distance Education-TOJDE October 2007 ISSN 1302-6488 Volume: 8 Number: 4
Turkish Online Journal of Distance Education-TOJDE January 2013 ISSN 1302-6488 Volume: 14 Number: 1 Article 10 EFFECTIVE LEARNING INTERACTION AS A PREREQUISITE TO SUCCESSFUL OPEN DISTANCE LEARNING (ODL): A Case study of Learners in the Northern State of Kedah and Perlis, Malaysia Hisham DZAKIRIA, PhD Azilah KASIM, PhD Abdul Halim MOHAMED, PhD Anne Althea CHRISTOPHER, PhD Universiti Utara Malaysia, MALAYSIA ABSTRACT The provision of ODL is now largely available in most part of the world, and is just a matter of choice for working adults to pursue. With the competing priorities of work, home, and school, adult learners everywhere desire a high degree of flexibility and accessibility. The structure of ODL provides learners with the greatest flexibility. It provides control over time, place and pace of education; however, learning at a distance is not without problems. Loss of student motivation due to lack of face-to-face (f2f) contact with tutors, peers and content; high startup costs, and lack of support are all barriers to the success of ODL. One important element of success factor for students attending ODL program is the level of interactivity within the student-tutor-content dyads. This paper looks at the issue of interactivity as reported in this research on students’ perspectives and experiences of ODL programs in the northern part of Malaysia. The study supported the widely held belief that a high level of interaction is desirable in ODL environment (Dzakiria, 2008, Dzakiria & Idrus, 2003; Rumble, 2000; Walker, 2002)) and positively affects the learning experiences. Recent technological advancements, allowing an increasing level of interaction between the interactivity dyads have implicated how teaching and learning should be in an ODL environment. -
2 Geology of Peninsular Malaysia
2 GEOLOGY OF PENINSULAR MALAYSIA 2.1 INTRODUCTION Peninsular Malaysia has traditionLlly been subdivided into NNW-SSE longitudinal belts on the basis of stratigraphy, mineralisation, geological structure, geological history and tectonic evolution . Scrivenor (19:;8) subdivided the Peninsula into three elongate belts on the basis of mineralisation: a western tin belt, a central gold belt and an eastern tin belt. Hutchison (1977) divided the Peni isula into four major tectonic subdivisions on the basis of different tectonic histories; the '1Vestern Stable Shelf, the Main Range Belt, the Central graben, and the Eastern Belt. Fo ) (1983) divided the Peninsula into four zones on the basis of differences in stratign phy. Khoo and Tan (1983) proposed a threefold subdivision; a Western Belt, Central Belt and an Eastern Belt on the basis of differences in stratigraphy and geological histoi y within Peninsular Malaysia. Within this threefold subdivision, Khoo and Tan (1983' further divided the Western Belt into two regions: a northwest sector and a Kinta-Ma acca sector. Tjia and Harun (1985) recognised four structural domains within the Peninsula. They defined Northwest, West, Central and Eastern structural domains. Within all the above subdivision schemes, the boundary between the eastern and central "belts" is taken as the Lebir Fault 2 one, and the boundary between the central and western "belts" is the Bentong-Raub line of Hutchison (1975). As previously stated (Chapter 1.5.2), Metcalfe (1988) proposed that Peninsular Malaysia consisted of two continental terra les, a western Gondwanan affinity continental terrane (Sibumasu) and an eastern Cathaysian affinity continental terrane (Indochina/East Malaya) Chapter 2: Geology of Peninsular Malaysia (Fig. -
(UUM) Ialah Universiti Keenam Malaysia Yang Secara Rasminya Ditubuhkan Pada 16 Februari 1984, Di Bawah Perintah Universiti Utara Malaysia 1984 (P.U
BAB II GAMBARAN UMUM UNIVERSITY UTARA MALAYSIA 2.1 Sejarah University Utara Malaysia Universiti Utara Malaysia (UUM) ialah universiti keenam Malaysia yang secara rasminya ditubuhkan pada 16 Februari 1984, di bawah Perintah Universiti Utara Malaysia 1984 (P.U. (A) 47/1984). UUM juga satu-satunya universiti yang ditetapkan supaya mengkhusus kepada bidang pengurusan sejak awal penubuhannya. UUM mengandungi dua kampus; kampus utama, yang dibina di Sintok, Kedah pada 15 September 1990 dan dibuka secara rasmi pada 17 Februari 2004, dan kampus kedua (kampus bukan kediaman), yang dibina di Kuala Lumpur, Wilayah Persekutuan Kuala Lumpur. UUM menduduki tempat ke-131 di dalam QS Asia Universiti Rankings 2018[7], menduduki antara tempat ke-101 ke tempat ke-150 di dalam QS Top 50 Under 50 2019[8], dan juga menduduki antara tempat ke-601 ke tempat ke-650 di dalam QS World University Rankings® 2019. Perancangan pembinaan Universiti Utara Malaysia bermula apabila Kementerian Pendidikan Malaysia merancang untuk menubuhkan universiti ini dalam bulan Ogos 1983. Pada 19 Oktober 1983, Jemaah Menteri telah memberi kelulusan rasmi ke atas projek yang pada waktu itu dinamakan “Projek Universiti Keenam”, di Kedah. Beberapa bulan kemudian, pejabat sementara universiti keenam yang diberi nama Universiti Utara Malaysia dibuka secara rasminya pada 15 Februari 1984 di Jitra. Empat bulan kemudian, UUM berpindah ke kampusnya yang pertama – Kampus Darul Aman di Jitra – pada bulan Jun 1984 apabila fasa pertama projek berkenaan siap. Perpindahan itu dilakukan bagi menyambut ketibaan sekumpulan 4 pelajar sulung universiti menjelang kemasukan mereka pada awal bulan Julai 1984. Kampus tersebut didirikan di atas satu kawasan seluas 62 ekar di Bandar Darulaman, iaitu 18 km ke utara Alor Setar dan 4.8 km dari Jitra. -
Complex Lada: a Remarkable Achievement
21 OCT 1996 Complex-Opening COMPLEX LADA: A REMARKABLE ACHIEVEMENT LANGKAWI, Oct 21 (Bernama) -- The new Langkawi Development Authority Complex (Lada), to be opened by Prime Minister Datuk Seri Dr Mahathir Mohamad on Wednesday, can be considered a remarkable achievement for Lada in its short life of only six years. Lada, which is under the Finance Ministry, had within this short space of time shown extraordinary performance for a government agency. The 10-storey complex had solved the problem of shortage of office space on this duty-free island. Built at a cost of RM30 million, the complex situated about one kilometre from Kuah Jetty and Kuah town would house all government departments, both state and Federal under one roof. This would facilitate dealings with the public because before this state and Federal government departments were scattered all over Kuah town and some were even operating in housing estates. Apart from office space, the complex also has an auditorium, which can seat 300 people and kiosks to sell foodstuffs and dry items. The grand colourful opening ceremony would begin at 8pm, Lada Public Relations Officer Mohd Hatta Said said. Simultaneously, Dr Mahathir would also open the Lang Square and the Langkawi Legend in the Park located some 500 metres from the Lada Complex. These two latest attractions in Langkawi were also built by Lada, with the square costing RM14 million and the legend project costing RM30 million. Like its name, the main attraction at Lang Square is a giant replica of an eagle meauring about 12 metres in height while visitors to the Langkawi Legend in the Park could know about the history of the island through giant carvings on its past. -
Urusetia & Bilik Pengurusan Banjir Lpp Negeri Kedah
URUSETIA & BILIK PENGURUSAN BANJIR LPP NEGERI KEDAH NAMA LPP / PPN / PPK NAMA URUSETIA NO.TELEFON BILIK PENGURUSAN BENCANA BANJIR LPP KEDAH / PPN JASNIZAN BIN AHMAD 012-3445584 / BILIK MESYUARAT LPP NEGERI KEDAH 04-7333792 ARAS 7, BANGUNAN KWSP-PELADANG, JALAN SULTAN BADLISHAH,BADLISHAH,PETIPETI SURAT 137, 05710 ALOR SSETAR,ETAR,KEDAH. KEDAH. PPK LANGKAWI / PPNJ AGUS SALIM BIN AWANG 019-5610025 / BILIK GERAKAN PPK LANGKAWI LANGKAWI 04-9551205 PADANG MAT SIRAT, 07100 LANGKAWI, KEDAH. PPK CHANGLUN SAKAWI BIN HAMID 019-5656430 / BILIK GERAKAN PPK CHANGLUN, 04-92412769241276 06010 CHANGLUN, KEDAH.KEDAH. PPK ASUN / PPNJ ASUN MOHD NOOR BIN HASSAN 013-5092577 / BILIK GERAKAN PPK ASUN, 04-9171315 0600600000 JITRA,JITRA,KEDAH KEDAH PPK LUBUK BATU NORIZAH BT NORDIN 019-4241000 / BILIK GERAKAN PPK LUBUK BATU, 04-9170601 KAMPUNGKAMPUNG LUBUK BATU, MUKIM PELUBANG, 06000 JITRA, KKEDAHEDAH PPK POKOK SENA BUKHARI BIN SHUIB 019-4506910 / BILIK GERAKAN PPK POKOK SENA, 04-7821282 NO. 111, BATU 12, 06400 POKOK SENA, KEDAH PPK KUALA NERANG HJ. YUNUS BIN LAUPE 019-8732474 / BILIK GERAKANGERAKAN PPK KUALA NERANG, 04-7866245 NO. 40,41,42 JLN SEMELIANSEMELIANG,G, 06300 KUALA NERANG, KEDAH PPK NAKA RAMLI BIN CHIK 012-5793117 / BILIK GERAKAN PPK NAKA, 04-7851219 06350 PADANG TERAP, KEDAH PPK KUBUR PANJANG HJH ANISAH BT MAN 012-4063963 / BILIK GERAKAN PPK KUBUR PANJANG, 04-7849366 06760 ALOR SETAR, KEDAH NAMA LPP / PPN / PPK NAMA URUSETIA NO.TELEFON BILIK PENGURUSAN BENCANA BANJIR PPK PENDANG SELATAN / SAIFUL ANUAR BIN IBRAHIM 012-2848500 / BILIK GERAKAN PPK PENDANG SELATAN, PPNJ PENDANG 04-7596058 962, MUKIM PADANG PUSING, KG. SAWA KECIL, 06700 PENDANG, KEDAH. -
Geologi Kedah Utara Dan Perlis
STAG2022 Stratigrafi Malaysia Stratigrafi Semenanjung Malaysia Geologi Kedah Utara - Perlis Stratigrafi Nama unit Usia Alluvium Resen-Pleistosen Lapisan Arang Bukit Arang Tertiar (?Miosen) Lapisan Saiong Jura-Kapur ? Formasi Chuping (Formasi Kodiang) Perm Tengah – Trias Awal Formasi Semanggol Formasi Kubang Pasu Devon, Karbon & Perm Awal (mungkin sampai Trias di Kedah Utara) Formasi Setul Ordovisi-Devon Awal Formasi Machinchang Kambrias Akhir FORMASI SETUL Pengenalan Formasi Setul merupakan formasi batuan karbonat yang tertua di Semenanjung Malaysia. Formasi batuan yang berusia Ordovisi hingga Devoni Awal ni terdiri daripada batu kapur tidak tulen yang bercampur dengan lumpur dalam amaun yang agak tinggi, batu kapur berdolomit dan dua ahli gersik yang terdiri daripada perlapisan syal, batu lumpur kaya silika, batu lodak dan sedikit rijang. Pemendapan sedimen telah berlaku di dalam sekitaran pelantar laut cetek di dalam keadaan iklim yang lebih dingin daripada sekarang yang ditunjukkan oleh kehadiran fosil-fosil yang mirip kepada fauna beriklim sedemikian. FORMASI KUBANG PASU Pengenalan Formasi Kubang Pasu tersingkap di kawasan Kedah, dan terdiri daripada selang lapis batuan syal, batu lodak dan juga batu pasir. Selain itu terdapat juga sedikit lapisan rijang yang berpelapisan nipis, terutamanya di bahagian bawah jujukan. Bahagian atas jujukan formasi ini terdapat suatu fasies perantaraan yang terdiri daripada lapisan klastik dan lapisan berkapur (termasuk batu kapur nipis). Formasi Kubang Pasu adalah setara dengan Formasi Singa yang tersingkap di Kepulauan Langkawi. Perlapisan batu pasir yang dominan dan terdiri daripada batu pasir kuarza dan batu pasir kaya feldsfar yang terdapat dalam Formasi Kubang Pasu merupakan perbezaan yang agak nyata antara Formasi Kubang Pasu dengan Formasi Singa. FORMASI KUBANG PASU Taburan FORMASI KUBANG PASU Litologi Formasi Kubang Pasu terdiri daripada syal, batu lodak dan batu pasir.