Water Resources Modelling of the Worfe River Catchment and Perak State Using Remote Sensing and GIS
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The Perak Development Experience: the Way Forward
International Journal of Academic Research in Business and Social Sciences December 2013, Vol. 3, No. 12 ISSN: 2222-6990 The Perak Development Experience: The Way Forward Azham Md. Ali Department of Accounting and Finance, Faculty of Management and Economics Universiti Pendidikan Sultan Idris DOI: 10.6007/IJARBSS/v3-i12/437 URL: http://dx.doi.org/10.6007/IJARBSS/v3-i12/437 Speech for the Menteri Besar of Perak the Right Honourable Dato’ Seri DiRaja Dr Zambry bin Abd Kadir to be delivered on the occasion of Pangkor International Development Dialogue (PIDD) 2012 I9-21 November 2012 at Impiana Hotel, Ipoh Perak Darul Ridzuan Brothers and Sisters, Allow me to briefly mention to you some of the more important stuff that we have implemented in the last couple of years before we move on to others areas including the one on “The Way Forward” which I think that you are most interested to hear about. Under the so called Perak Amanjaya Development Plan, some of the things that we have tried to do are the same things that I believe many others here are concerned about: first, balanced development and economic distribution between the urban and rural areas by focusing on developing small towns; second, poverty eradication regardless of race or religion so that no one remains on the fringes of society or is left behind economically; and, third, youth empowerment. Under the first one, the state identifies viable small- and medium-size companies which can operate from small towns. These companies are to be working closely with the state government to boost the economy of the respective areas. -
Land North West of Stableford Hall Stableford Bridgnorth Shropshire
Committee and date South Planning Committee 13 January 2015 Development Management Report Responsible Officer: Tim Rogers email: [email protected] Tel: 01743 258773 Fax: 01743 252619 Summary of Application Application Number: 14/04387/FUL Parish: Worfield Proposal : Application under Section 73a of the Town and Country Planning Act 1990 for the erection of an agricultural building and formation of an agricultural access track (part retrospective) Site Address : Land North West Of Stableford Hall Stableford Bridgnorth Shropshire Applicant : Mr B Higginson Case Officer : Thomas Cannaby email : [email protected] Grid Ref: 375735 - 298714 Land North West of Stableford Hall, South Planning Committee – 13 January 2015 Bridgnorth © Crown Copyright. All rights reserved. Shropshire Council 100049049. 2011 For reference purposes only. No further copies may be made. Contact: Tim Rogers (01743) 258773 Land North West of Stableford Hall, South Planning Committee – 13 January 2015 Bridgnorth Recommendation:- Grant Permission,subject to confirmation that the building would be sited outside of flood zones 2 and 3, and to the conditions set out in Appendix 1. REPORT 1.0 THE PROPOSAL 1.1 The application is for the erection of an agricultural building and the formation of an access track on land adjacent to the River Worfe, near Stableford. The application is in part retrospective, with the access track already under construction and this application resulting from an investigation of an enforcement complaint against the works. 1.2 The proposed building would be of steel portal framed construction, with part block walls and part timber weather board cladding, and with a fibre cement sheet roof. -
Higher-Resolution Biostratigraphy for the Kinta Limestone and an Implication for Continuous Sedimentation in the Paleo-Tethys, Western Belt of Peninsular Malaysia
Turkish Journal of Earth Sciences Turkish J Earth Sci (2017) 26: 377-394 http://journals.tubitak.gov.tr/earth/ © TÜBİTAK Research Article doi:10.3906/yer-1612-29 Higher-resolution biostratigraphy for the Kinta Limestone and an implication for continuous sedimentation in the Paleo-Tethys, Western Belt of Peninsular Malaysia 1,2, 2 3 4 2 5 Haylay TSEGAB *, Chow Weng SUM , Gatovsky A. YURIY , Aaron W. HUNTER , Jasmi AB TALIB , Solomon KASSA 1 South-East Asia Carbonate Research Laboratory (SEACaRL), Department of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS, Bandar Seri Iskandar, Perak Darul Ridzuan, Malaysia 2 Department of Geosciences, Faculty of Geosciences and Petroleum Engineering, Universiti Teknologi PETRONAS, Bandar Seri Iskandar, Perak Darul Ridzuan, Malaysia 3 Lomonosov Moscow State University, Moscow, Russian Federation 4 Department of Applied Geology, Western Australian School of Mines, Curtin University, Perth, Australia 5 Department of Applied Geology, School of Applied Natural Sciences, Adama Sciences and Technology University, Adama, Ethiopia Received: 29.12.2016 Accepted/Published Online: 21.09.2017 Final Version: 13.11.2017 Abstract: The paleogeography of the juxtaposed Southeast Asian terranes, derived from the northeastern margins of Gondwana during the Carboniferous to Triassic, resulted in complex basin evolution with massive carbonate deposition on the margins of the Paleo- Tethys. Due to the inherited structural and tectonothermal complexities, discovery of diagnostic microfossils from these carbonates has been problematic. This is particularly the case for the Kinta Limestone, a massive Paleozoic carbonate succession that covers most of the Kinta Valley in the central part of the Western Belt of Peninsular Malaysia. -
Upper Kinta Basin Environmental Assessment Report
UPPER KINTA BASIN ENVIRONMENTAL ASSESSMENT REPORT PREPARED BY: IN COORPERATION WITH: Upper Kinta Baseline Environmental Assessment Report TABLE OF CONTENTS ii Page Table of Contents iii List of Tables v List of Figures vii List of Annexes x Global Environment Centre Nov 2018 Upper Kinta Baseline Environmental Assessment Report TABLE OF CONTENTS iii Page CHAPTER 1: INTRODUCTION 1.1 BACKGROUND 1-1 1.2 OBJECTIVES 1-2 1.2.1 Target beneficiaries 1-3 1.3 BASELINE STUDY 1-4 1.3.1 Format of this report 1-5 CHAPTER 2: UPPER KINTA BASIN 2.1 PROJECT AREA 2-1 2.2 METHODOLOGY 2-2 2.3 SECONDARY DATA ANALYSIS 2-3 2.3.1 Climate 2-3 2.3.2 Geology and Soil Type 2-3 2.3.3 Water Supply 2-4 2.3.4 Demography 2-6 2.3.5 Land Use Assessment 2-9 2.4 LAND USE WITHIN UKB 2-10 2.4.1 Forest 2-11 2.4.2 Agriculture 2-12 2.4.3 Residential and Transportation Facility 2-12 2.4.4 Industries 2-13 2.4.5 Waterbody 2-15 2.4.6 Others 2-16 2.5 LAND USE AND WATER BODIES 2-17 CHAPTER 3: POLLUTION SOURCE RAPID INVENTORY 3.1 INTRODUCTION 3-1 3.2 METHODOLOGY 3-2 3.2.1 Pollution Source Inventory 3-2 3.2.2 Water Quality Study 3-2 3.2.2.1 Secondary Data Collection 3-2 3.2.2.2 Sampling by GEC Team 3-4 3.2.3 Biological Water Quality Study 3-7 3.3 RESULTS & DISCUSSIONS 3-8 3.3.1 Pollution Source Inventory 3-8 3.3.2 Water Quality Status 3-31 3.3.2.1 Water Quality Monitoring by Agencies 3-31 3.3.2.2 Overall UKB Water Quality Status 3-32 3.3.2.3 Impact of Development Activities 3-38 3.3.2.4 Water Quality Status before Dam 3-39 3.3.3 Biological Water Quality Status 3-40 3.3.3.1 Distribution -
Advisory Visit River Worfe March 2011
Advisory Visit River Worfe March 2011 1.0 Introduction This report is the output of a site visit undertaken by Tim Jacklin of the Wild Trout Trust to the River Worfe, Shropshire on 7th March, 2011. Comments in this report are based on observations on the day of the site visit and discussions with Tony Bostock of Severn Rivers Trust and Simon Cumming of the Environment Agency. Normal convention is applied throughout the report with respect to bank identification, i.e. the banks are designated left hand bank (LHB) or right hand bank (RHB) whilst looking downstream. 2.0 Catchment / Fishery Overview The River Worfe rises to the east of Telford and flows south near Ryton, Badger and Worfield where it turns west to join the River Severn just north of Bridgnorth. The river flows off the mid-Severn sandstone plateau and the underlying geology is largely Triassic sandstone, with superficial deposits of till or river terrace material. The three areas of the river inspected during this visit were to the south of Davenport House (SO752950), upstream of Worfield (SO759961) and downstream of Broad Bridge (SO761981) near Stableford. The lower section of the river from Rindleford down to the Severn was seen from a car. The river is fished by Salopian Fly Fishers (www.salopianflyfishers.co.uk) although some beats have recently been relinquished. Tony Bostock has fished the River Worfe for 37 years and reports a decline in the trout fishery in recent years based on personal experience and historic records. A full- time river keeper was employed by the Apley Estate in the 1930s and he kept written records regarding the river. -
Changing Trends of Rainfall and Sediment Fluxes in the Kinta River Catchment, Malaysia
doi:10.5194/piahs-367-340-2015 340 Sediment Dynamics from the Summit to the Sea (Proceedings of a symposium held in New Orleans, Louisiana, USA, 11–14 December 2014) (IAHS Publ. 367, 2014). Changing trends of rainfall and sediment fluxes in the Kinta River catchment, Malaysia WAN RUSLAN ISMAIL1 & MOHMADISA HASHIM2 1 HydroGeomorphology Research Group, Geography Section, School of Humanities, Universiti Sains Malaysia, 11800 Minden, Pulau Pinang, Malaysia [email protected] 2 Department of Geography and Environment, Faculty of Human Sciences, Universiti Pendidikan Sultan Idris, 35900 Tanjong Malim, Perak, Malaysia Abstract The Kinta River, draining an area of 2566 km2, originates in the Korbu Mountain in Perak, Malaysia, and flows through heterogeneous, mixed land uses ranging from extensive forests to mining, rubber and oil palm plantations, and urban development. A land use change analysis of the Kinta River catchment was carried out together with assessment of the long-term trend in rainfall and sediment fluxes. The Mann-Kendall test was used to examine and assess the long-term trends in rainfall and its relationship with the sediment discharge trend. The land use analysis shows that forests, water bodies and mining land declined whilst built and agricultural land use increased significantly. This has influenced the sediment flux of the catchment. However, most of the rainfall stations and river gauging stations are experiencing an increasing trends, except at Kinta river at Tg. Rambutan. Sediment flux shows a net erosion for the period from 1961 to 1969. The total annual sediment discharge in the Kinta River catchment was low with an average rate of 1,757 t/km2/year. -
The Role of Authenticity in Food Tourism Development in Two Historic Cities in Malaysia a Comparative Case Study Between George Town, Penang and Ipoh, Perak
THE ROLE OF AUTHENTICITY IN FOOD TOURISM DEVELOPMENT IN TWO HISTORIC CITIES IN MALAYSIA A COMPARATIVE CASE STUDY BETWEEN GEORGE TOWN, PENANG AND IPOH, PERAK MASTER THESIS BY ANNE PLADDET 2 Master thesis for the Master Leisure, Tourism and Environment Thesis code: GEO-80436 Author: Johanne Marrigje Pladdet Student number: 900307654090 Contact: [email protected] Supervisor: dr. Arjaan Pellis Examiner: Prof. dr. René van der Duim Wageningen University and Research Department of Environmental Sciences Cultural Geography Chair Group August 2019 Disclaimer: This thesis is a student report produced as part of the Master Program Leisure, Tourism and Environment. It is not an official publication and the content does not represent an official position of Wageningen University and Research. 3 ACKNOWLEDGEMENTS The journey of this master thesis started a long time ago, to be precise in March 2015. It has been a journey that I have enjoyed and hated at the same time, but after all I’m grateful for the whole journey because it taught me a lot about academics, food tourism in Malaysia and myself. Due to various reasons it has taken me a long time to finalize this thesis, therefore I’m really happy to be able to finally end this journey and see what is next for me after graduating from the master Leisure, Tourism and Environment at Wageningen University and Research. I would like to thank a few people who played a major role in finalizing this thesis. First, I would like to thank my two supervisors. In 2015 I started this project with dr. Meghann Ormond as my supervisor. -
The Shropshire Landscape Typology
The Shropshire Landscape Typology September 2006 Contents Part I – Setting the Scene 1 Introduction 2 The Shropshire Character Framework 5 Assessing Landscape Character 6 Part II – The Typology 11 Defining landscape types 12 High Open Moorland 14 High Enclosed Plateau 16 High Volcanic Hills and Slopes 18 Upland Smallholdings 20 Upstanding Enclosed Commons 22 Pasture Hills 24 Principal Wooded Hills 26 Wooded River Gorge 28 Wooded Hills and Farmlands 30 Wooded Hills and Estatelands 32 Sandstone Hills 34 Sandstone Estatelands 36 Incised Sandstone Valleys 38 Wooded Forest 40 Forest Smallholdings 42 Timbered Plateau Farmlands 44 Principal Timbered Farmlands 46 Timbered Pastures 48 Wooded Estatelands 50 Estate Farmlands 52 Settled Pastoral Farmlands 54 Principal Settled Farmlands 56 i Contents Part II – The Typology continued Enclosed Lowland Heaths 58 Lowland Moors 60 Riverside Meadows 62 Lowland Moss 64 Coalfields 66 Glossary 68 Further Information 73 ii Part I Setting the Scene “For the personality of a man reacting upon the spirit of a place produces something which is neither man nor the place, but fiercer and more beautiful than either” Mary Webb. The Golden Arrow © Gordon Dickens 1 Introduction Shropshire possesses one of the richest and most varied landscapes of any of the English counties. It offers a diverse range of scenery: from the lakes and rolling pasturelands around Ellesmere in the north, to the gaunt moorlands of the Clee Hills, with their stark industrial ruins, in the south; the densely wooded scarps of Wenlock Edge; or the straight, sandy lanes of the north-eastern heathlands, with their large arable fields and ‘big skys’. -
Global-Report-2 Sided 1 Column
Telford & Wrekin Council Scoping Water Cycle Study Final Report Hyder Consulting (UK) Limited 2212959 5th Floor The Pithay All Saints Street Bristol BS1 2NL United Kingdom Tel: +44 (0)117 372 1200 Fax: +44 (0)117 37 www.hyderconsulting.com Telford & Wrekin Council Scoping Water Cycle Study Final Report Author Heather Taylor Checker Liam Foster / Aimee Hart Approver Heather Taylor Report No 1 Date 5th September 2012 This report has been prepared for Telford & Wrekin Council in accordance with the terms and conditions of appointment for Final Report dated 3rd March 2012. Hyder Consulting (UK) Limited (2212959) cannot accept any responsibility for any use of or reliance on the contents of this report by any third party. Scoping Water Cycle Study—Final Report Hyder Consulting (UK) Limited-2212959 k:\uaprojects\ua004156 telford & wrekin\i- issued\5001-ua004156-telford wrekin scoping wcs-r-bm-final issue september 2012.docx CONTENTS 1 Executive Summary .............................................................................. 1 2 Introduction ........................................................................................... 3 2.1 Background to Study ............................................................................ 3 2.2 What is a Water Cycle Study (WCS)? .................................................. 4 2.3 Study area ............................................................................................ 6 2.4 The Water Cycle .................................................................................. -
Regulation 19: Pre-Submission Draft of the Shropshire Local Plan 2016 to 2038
Shropshire Council Regulation 19: Pre-Submission Draft of the Shropshire Local Plan 2016 to 2038 December 2020 Regulation 19: Pre-Submission Draft of the Shropshire Local Plan Page 0 1. Contents 2. Introduction ...................................................................................... 6 Shropshire’s Character ................................................................................... 6 National Planning Policy Framework (NPPF) ................................................ 8 The Shropshire Local Plan 2016 to 2038 ....................................................... 8 Cross Boundary Issues and the Duty to Cooperate ................................... 10 Infrastructure ................................................................................................. 10 Neighbourhood Plans and Community Led Plans ...................................... 10 3. Strategic Policies ........................................................................... 12 SP1. The Shropshire Test ......................................................................... 12 SP2. Strategic Approach ........................................................................... 13 SP3. Climate Change ................................................................................. 22 SP4. Sustainable Development................................................................. 25 SP5. High-Quality Design .......................................................................... 26 SP6. Health and Wellbeing ....................................................................... -
Changing Trends of Rainfall and Sediment Fluxes in the Kinta River Catchment, Malaysia
340 Sediment Dynamics from the Summit to the Sea (Proceedings of a symposium held in New Orleans, Louisiana, USA, 11–14 December 2014) (IAHS Publ. 367, 2014). Changing trends of rainfall and sediment fluxes in the Kinta River catchment, Malaysia WAN RUSLAN ISMAIL1 & MOHMADISA HASHIM2 1 HydroGeomorphology Research Group, Geography Section, School of Humanities, Universiti Sains Malaysia, 11800 Minden, Pulau Pinang, Malaysia [email protected] 2 Department of Geography and Environment, Faculty of Human Sciences, Universiti Pendidikan Sultan Idris, 35900 Tanjong Malim, Perak, Malaysia Abstract The Kinta River, draining an area of 2566 km2, originates in the Korbu Mountain in Perak, Malaysia, and flows through heterogeneous, mixed land uses ranging from extensive forests to mining, rubber and oil palm plantations, and urban development. A land use change analysis of the Kinta River catchment was carried out together with assessment of the long-term trend in rainfall and sediment fluxes. The Mann-Kendall test was used to examine and assess the long-term trends in rainfall and its relationship with the sediment discharge trend. The land use analysis shows that forests, water bodies and mining land declined whilst built and agricultural land use increased significantly. This has influenced the sediment flux of the catchment. However, most of the rainfall stations and river gauging stations are experiencing an increasing trends, except at Kinta river at Tg. Rambutan. Sediment flux shows a net erosion for the period from 1961 to 1969. The total annual sediment discharge in the Kinta River catchment was low with an average rate of 1,757 t/km2/year. -
Bridgnorth and Surrounding Area Place Plan This Version Published 2019/20
Bridgnorth and Surrounding Area Place Plan This version published 2019/20 1 Contents Context What is a Place Plan? 3 Section 1 List of Projects 5 1.1 Data and information review 1.2 Prioritisation of projects 1.3 Projects for Bridgnorth and Surrounding Area Place Plan 1.4 Potential Projects Section 2 Planning in Shropshire 26 2.1 County-wide planning processes 2.2 This Place Plan area in the county-wide plan Section 3 More about this area 29 3.1 Place Plan boundaries 3.2 Pen picture of the area 3.3 List of Parishes and Elected Members 3.4 Other local plans Section 4 Reviewing the Place Plan 33 4.1 Previous reviews 4.2 Future reviews Annexe 1 Supporting information 35 2 Context: what is a Place Plan? Shropshire Council is working to make Shropshire a great place to live, learn, work, and visit – we want to innovate to thrive. To make that ambition a reality, we need to understand what our towns and communities need in order to make them better places for all. Our Place Plans – of which there are 18 across the county – paint a picture of each local area and help all of us to shape and improve our communities. Place Plans are documents which bring together information about a defined area. The information that they contain is focussed on infrastructure needs, such as roads, transport facilities, flood defences, schools and educational facilities, medical facilities, sporting and recreational facilities, and open spaces. They also include other information which can help us to understand local needs and to make decisions.