Irrigation and Field Patterns in the Indus Delta. Mushtaq-Ur Rahman Louisiana State University and Agricultural & Mechanical College
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Introduction: Honour Violence, Law and Power in Upper Sindh
Introduction HONOUR VIOLENCE, LAW AND POWER IN UPPER SINDH n The story that I am to narrate here begins in the 1990s, when as a reporter in a local magazine called Newsline, I wrote a comprehensive news story on karo kari,1 (literally ‘black man and black woman’), a vernacular honour- based practice in the Upper Sindh region of present-day Pakistan. Known popularly as a rasam, a ‘custom’ that sanctioned men and women accused of sexual transgressions with death,2 karo kari has since become a leading story of the national media in Pakistan, a major human rights issue and a problem that both lawmakers and civil society are concerned about. My report was the first comprehensive exposé of the existence and preva- lence of this practice in the region of Upper Sindh.3 This report disclosed the violence committed through karo kari, whose perpetrators were defend- ing what was considered a timeless, natural and therefore unquestionable ideology of honour called ghairat, a moral sanction enforced by each indi- vidual, and more specifically each man, but with social approval. In the report, I described the punishment of ‘black’ men and women as retributive justice for men whose honour had been damaged when a female relative was accused of engaging in sexual relations with another man. Husbands, fathers, brothers and sons could accuse their wives, daughters, sisters or mothers of being black, and the action taken against women could be either expulsion from the community or death. If found with the woman, the co- accused man could be killed or subsequently hunted down. -
Rivers, Canals, and Distributaries in Punjab, Pakistan
Socio#Hydrology of Channel Flows in Complex River Basins: Rivers, Canals, and Distributaries in Punjab, Pakistan The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Wescoat, James L., Jr. et al. "Socio-Hydrology of Channel Flows in Complex River Basins: Rivers, Canals, and Distributaries in Punjab, Pakistan." Water Resources Research 54, 1 (January 2018): 464-479 © 2018 The Authors As Published http://dx.doi.org/10.1002/2017wr021486 Publisher American Geophysical Union (AGU) Version Final published version Citable link https://hdl.handle.net/1721.1/122058 Terms of Use Creative Commons Attribution-NonCommercial-NoDerivs License Detailed Terms http://creativecommons.org/licenses/by-nc-nd/4.0/ PUBLICATIONS Water Resources Research RESEARCH ARTICLE Socio-Hydrology of Channel Flows in Complex River Basins: 10.1002/2017WR021486 Rivers, Canals, and Distributaries in Punjab, Pakistan Special Section: James L. Wescoat Jr.1 , Afreen Siddiqi2 , and Abubakr Muhammad3 Socio-hydrology: Spatial and Temporal Dynamics of 1School of Architecture and Planning, Massachusetts Institute of Technology, Cambridge, MA, USA, 2Institute of Data, Coupled Human-Water Systems, and Society, Massachusetts Institute of Technology, Cambridge, MA, USA, 3Lahore University of Management Systems Sciences, Lahore, Pakistan Key Points: This paper presents a socio-hydrologic analysis of channel flows in Punjab province of the Coupling historical geographic and Abstract statistical analysis makes an Indus River basin in Pakistan. The Indus has undergone profound transformations, from large-scale canal irri- important contribution to the theory gation in the mid-nineteenth century to partition and development of the international river basin in the and methods of socio-hydrology mid-twentieth century, systems modeling in the late-twentieth century, and new technologies for discharge Comparing channel flow entitlements with deliveries sheds measurement and data analytics in the early twenty-first century. -
Dayton Valley Development Guidelines Final Draft
FINAL DRAFT Dayton Valley Development Guidelines Supplement to the Dayton Valley Area Drainage Master Plan prepared for August Lyon County | Storey County | 2019 Carson Water Subconservancy District i FINAL DRAFT Table of Contents 1 Introduction .......................................................................................................................................... 1 1.1 Background and Rationale ............................................................................................................ 3 1.1.1 More Frequent Flooding ....................................................................................................... 3 1.1.2 Larger Flood Peaks ................................................................................................................ 3 1.1.3 Scour and Erosion ................................................................................................................. 3 1.1.4 Flow Diversion ....................................................................................................................... 3 1.1.5 Flow Concentration ............................................................................................................... 3 1.1.6 Expanded Floodplains ........................................................................................................... 3 1.1.7 Reduced Surface Storage ...................................................................................................... 3 1.1.8 Decreased Ground Water Recharge .................................................................................... -
The Geographic, Geological and Oceanographic Setting of the Indus River
16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan. -
Irrigation of World Agricultural Lands: Evolution Through the Millennia
water Review Irrigation of World Agricultural Lands: Evolution through the Millennia Andreas N. Angelakιs 1 , Daniele Zaccaria 2,*, Jens Krasilnikoff 3, Miquel Salgot 4, Mohamed Bazza 5, Paolo Roccaro 6, Blanca Jimenez 7, Arun Kumar 8 , Wang Yinghua 9, Alper Baba 10, Jessica Anne Harrison 11, Andrea Garduno-Jimenez 12 and Elias Fereres 13 1 HAO-Demeter, Agricultural Research Institution of Crete, 71300 Iraklion and Union of Hellenic Water Supply and Sewerage Operators, 41222 Larissa, Greece; [email protected] 2 Department of Land, Air, and Water Resources, University of California, California, CA 95064, USA 3 School of Culture and Society, Department of History and Classical Studies, Aarhus University, 8000 Aarhus, Denmark; [email protected] 4 Soil Science Unit, Facultat de Farmàcia, Universitat de Barcelona, 08007 Barcelona, Spain; [email protected] 5 Formerly at Land and Water Division, Food and Agriculture Organization of the United Nations-FAO, 00153 Rome, Italy; [email protected] 6 Department of Civil and Environmental Engineering, University of Catania, 2 I-95131 Catania, Italy; [email protected] 7 The Comisión Nacional del Agua in Mexico City, Del. Coyoacán, México 04340, Mexico; [email protected] 8 Department of Civil Engineering, Indian Institute of Technology, Delhi 110016, India; [email protected] 9 Department of Water Conservancy History, China Institute of Water Resources and Hydropower Research, Beijing 100048, China; [email protected] 10 Izmir Institute of Technology, Engineering Faculty, Department of Civil -
“Major World Deltas: a Perspective from Space
“MAJOR WORLD DELTAS: A PERSPECTIVE FROM SPACE” James M. Coleman Oscar K. Huh Coastal Studies Institute Louisiana State University Baton Rouge, LA TABLE OF CONTENTS Page INTRODUCTION……………………………………………………………………4 Major River Systems and their Subsystem Components……………………..4 Drainage Basin………………………………………………………..7 Alluvial Valley………………………………………………………15 Receiving Basin……………………………………………………..15 Delta Plain…………………………………………………………...22 Deltaic Process-Form Variability: A Brief Summary……………………….29 The Drainage Basin and The Discharge Regime…………………....29 Nearshore Marine Energy Climate And Discharge Effectiveness…..29 River-Mouth Process-Form Variability……………………………..36 DELTA DESCRIPTIONS…………………………………………………………..37 Amu Darya River System………………………………………………...…45 Baram River System………………………………………………………...49 Burdekin River System……………………………………………………...53 Chao Phraya River System……………………………………….…………57 Colville River System………………………………………………….……62 Danube River System…………………………………………………….…66 Dneiper River System………………………………………………….……74 Ebro River System……………………………………………………..……77 Fly River System………………………………………………………...…..79 Ganges-Brahmaputra River System…………………………………………83 Girjalva River System…………………………………………………….…91 Krishna-Godavari River System…………………………………………… 94 Huang He River System………………………………………………..……99 Indus River System…………………………………………………………105 Irrawaddy River System……………………………………………………113 Klang River System……………………………………………………...…117 Lena River System……………………………………………………….…121 MacKenzie River System………………………………………………..…126 Magdelena River System……………………………………………..….…130 -
The Thick-Splay Depositional Style of the Crevasse Canyon Formation, Cretaceous of West-Central New Mexico Steven J
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/34 The thick-splay depositional style of the Crevasse Canyon Formation, Cretaceous of west-central New Mexico Steven J. Johansen, 1983, pp. 173-178 in: Socorro Region II, Chapin, C. E.; Callender, J. F.; [eds.], New Mexico Geological Society 34th Annual Fall Field Conference Guidebook, 344 p. This is one of many related papers that were included in the 1983 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Egyptian and Greek Water Cultures and Hydro-Technologies in Ancient Times
sustainability Review Egyptian and Greek Water Cultures and Hydro-Technologies in Ancient Times Abdelkader T. Ahmed 1,2,* , Fatma El Gohary 3, Vasileios A. Tzanakakis 4 and Andreas N. Angelakis 5,6 1 Civil Engineering Department, Faculty of Engineering, Aswan University, Aswan 81542, Egypt 2 Civil Engineering Department, Faculty of Engineering, Islamic University, Madinah 42351, Saudi Arabia 3 Water Pollution Research Department, National Research Centre, Cairo 12622, Egypt; [email protected] 4 Department of Agriculture, School of Agricultural Science, Hellenic Mediterranean University, Iraklion, 71410 Crete, Greece; [email protected] 5 HAO-Demeter, Agricultural Research Institution of Crete, 71300 Iraklion, Greece; [email protected] 6 Union of Water Supply and Sewerage Enterprises, 41222 Larissa, Greece * Correspondence: [email protected] Received: 2 October 2020; Accepted: 19 November 2020; Published: 23 November 2020 Abstract: Egyptian and Greek ancient civilizations prevailed in eastern Mediterranean since prehistoric times. The Egyptian civilization is thought to have been begun in about 3150 BC until 31 BC. For the ancient Greek civilization, it started in the period of Minoan (ca. 3200 BC) up to the ending of the Hellenistic era. There are various parallels and dissimilarities between both civilizations. They co-existed during a certain timeframe (from ca. 2000 to ca. 146 BC); however, they were in two different geographic areas. Both civilizations were massive traders, subsequently, they deeply influenced the regional civilizations which have developed in that region. Various scientific and technological principles were established by both civilizations through their long histories. Water management was one of these major technologies. Accordingly, they have significantly influenced the ancient world’s hydro-technologies. -
Early Hydraulic Civilization in Egypt Oi.Uchicago.Edu
oi.uchicago.edu Early Hydraulic Civilization in Egypt oi.uchicago.edu PREHISTORIC ARCHEOLOGY AND ECOLOGY A Series Edited by Karl W. Butzer and Leslie G. Freeman oi.uchicago.edu Karl W.Butzer Early Hydraulic Civilization in Egypt A Study in Cultural Ecology Internet publication of this work was made possible with the generous support of Misty and Lewis Gruber The University of Chicago Press Chicago and London oi.uchicago.edu Karl Butzer is professor of anthropology and geography at the University of Chicago. He is a member of Chicago's Committee on African Studies and Committee on Evolutionary Biology. He also is editor of the Prehistoric Archeology and Ecology series and the author of numerous publications, including Environment and Archeology, Quaternary Stratigraphy and Climate in the Near East, Desert and River in Nubia, and Geomorphology from the Earth. The University of Chicago Press, Chicago 60637 The University of Chicago Press, Ltd., London ® 1976 by The University of Chicago All rights reserved. Published 1976 Printed in the United States of America 80 79 78 77 76 987654321 Library of Congress Cataloging in Publication Data Butzer, Karl W. Early hydraulic civilization in Egypt. (Prehistoric archeology and ecology) Bibliography: p. 1. Egypt--Civilization--To 332 B. C. 2. Human ecology--Egypt. 3. Irrigation=-Egypt--History. I. Title. II. Series. DT61.B97 333.9'13'0932 75-36398 ISBN 0-226-08634-8 ISBN 0-226-08635-6 pbk. iv oi.uchicago.edu For INA oi.uchicago.edu oi.uchicago.edu CONTENTS List of Illustrations Viii List of Tables ix Foreword xi Preface xiii 1. -
Hydropower Energy
Hydropower Associate Professor Mazen Abualtayef Environmental Engineering Department Islamic University of Gaza, Palestine Adapted from a presentation by S. Lawrence Leeds School of Business, Environmental Studies University of Colorado, Boulder, CO, USA 1 Course Outline Renewable Sustainable Solar Power Hydrogen & Fuel Cells Hydro Power Nuclear Wind Energy Fossil Fuel Innovation Oceanic Energy Exotic Technologies Geothermal Integration Biomass Distributed Generation 2 Hydro Energy Video 1 Video 2 Video 3 3 Hydrologic Cycle 4 http://www1.eere.energy.gov/windandhydro/hydro_how.html Hydropower to Electric Power Electrical Potential Energy Energy Electricity Kinetic Energy Mechanical Energy 5 Hydropower in Context 6 Sources of Electric Power - world In the USA 7 Renewable Energy Sources 8 World Trends in Hydropower 9 Boyle, Renewable Energy, 2nd edition, Oxford University Press, 2003 World hydro production 10 IEA.org Major Hydropower Producers 11 World’s Largest Dams Max Annual Name Country Year Generation Production Three Gorges China 2009 18,200 MW Itaipú Brazil/Paraguay 1983 12,600 MW 93.4 TW-hrs Guri Venezuela 1986 10,200 MW 46 TW-hrs Grand Coulee United States 1942/80 6,809 MW 22.6 TW-hrs Sayano Shushenskaya Russia 1983 6,400 MW Robert-Bourassa Canada 1981 5,616 MW Churchill Falls Canada 1971 5,429 MW 35 TW-hrs Iron Gates Romania/Serbia 1970 2,280 MW 11.3 TW-hrs Aswan Dam Egypt 1950 2,100 MW Ranked by maximum power. The Electricity production from hydroelectric sources in Egypt was 12.863 (TWh) in 2009, according to a -
Powered by TCPDF (
Powered by TCPDF (www.tcpdf.org) TUGAS AKHIR – DP 141558 PERANCANGAN BUKU ENSIKLOPEDIA PENEMUAN BESAR UMAT ISLAM BAGI DUNIA UNTUK ANAK USIA 9-12 TAHUN Andini Oktarani Tria Rahma NRP. 3413100121 Dosen Pembimbing Sayatman, S. Sn, M. Si NIP. 19740614 200112 1 003 Bidang Studi Desain Komunikasi Visual Departemen Desain Produk Fakultas Arsitektur, Desain, dan Perencanaan Institut Teknologi Sepuluh Nopember 2018 i FINAL PROJECT – DP 141558 ENCYCLOPEDIA BOOK OF MUSLIM INVENTIONS AND ITS CONTRIBUTION TO THE WORLD FOR CHILDREN AGED 9-12 YEARS Andini Oktarani Tria Rahma NRP. 3413100121 Supervisor Sayatman, S. Sn, M. Si NIP. 19740614 200112 1 003 Visual Communication Design Department of Product Design Faculty of Architecture, Design and Planning Institut Teknologi Sepuluh Nopember 2018 ii KATA PENGANTAR Puji syukur penulis panjatkan ke hadirat Allah Subhanahuwataala, sebagai dzat yang Maha pemberi petunjuk, serta Maha pemberi rahmat serta karunia sehingga penulis dapat menyelesaikan laporan ini. Karya Tulis yang berjudul “Buku Ensiklopedia Visual Penemuan Besar Umat Isam bagi Dunia untuk Anak 9-12 Tahun” ini, disusun sebagai prasyarat mata kuliah, yang yang merupakan gabungan antara analisis dan solusi kreatif berbasis jurusan Desain Komunikasi Visual di Fakultas Arsitektur, Desain, dan Perancangan ITS. Bagaimanapun, kelancaran dan keberhasilan penulis tidak lepas dari bantuan berbagai pihak. Untuk itu, penulis ingin mengucapkan terimakasih kepada: 1. Bapak yang telah memberikan support; 2. Ibu dan keluarga yang terus mempercayai saya bisa menyelesaikan laporan ini; 4. Dosen pembimbing, dan dosen penguji yang memberikan kritik dan saran yang membangun. 5. Rahayuning Putri (Rara) yang telah banyak membantu, mendukung, dan menemani saya dalam proses; 6. Teman-teman kontrakan yang penuh semangat memberikan saya dukungan. -
Architectural Features of the Early Harappan Forts
Ancient Punjab – Volume 8, 2020 103 ARCHITECTURAL FEATURES OF THE EARLY HARAPPAN FORTS Umesh Kumar Singh ABSTRACT What is generally called the Indus or the Harappan Civilization or Culture and used as interchangeable terms for the fifth millennium BCE Bronze Age Indian Civilization. Cunningham (1924: 242) referred vaguely to the remains of the walled town of Harappa and Masson (1842, I: 452) had camped in front of the village and ruinous brick castle. Wheeler (1947: 61) mentions it would appear from the context of Cunningham and Masson intended merely to distinguish the high mounds of the site from the vestiges of occupation on the lower ground round about and the latter doubt less the small Moghul fort which now encloses the police station on the eastern flank of the site. Burnes, about 1831, has referred to a ruined citadel on the river towards the northern side (Burnes 1834: 137). Marshall (1931) and Mackay (1938) also suspected of identifying Burnes citadel and Mackay (1938) had to suspend his excavations whilst in the act of examining a substantial structure which he was inclined to think was a part of city wall. Wheeler had discovered a limited number of pottery fragments from the pre- defense levels at Harappa in 1946 but the evidence was too meager to provoke serious discussion. The problem of origin and epi-centre of the Harappa Culture has confronted scholars since its discovery and in this context the most startling archaeological discoveries made and reported by Rafique Mughal (1990) is very significant and is a matter of further research work.