Relevant Abstract of Central Water Commission in 1981
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LIST of INDIAN CITIES on RIVERS (India)
List of important cities on river (India) The following is a list of the cities in India through which major rivers flow. S.No. City River State 1 Gangakhed Godavari Maharashtra 2 Agra Yamuna Uttar Pradesh 3 Ahmedabad Sabarmati Gujarat 4 At the confluence of Ganga, Yamuna and Allahabad Uttar Pradesh Saraswati 5 Ayodhya Sarayu Uttar Pradesh 6 Badrinath Alaknanda Uttarakhand 7 Banki Mahanadi Odisha 8 Cuttack Mahanadi Odisha 9 Baranagar Ganges West Bengal 10 Brahmapur Rushikulya Odisha 11 Chhatrapur Rushikulya Odisha 12 Bhagalpur Ganges Bihar 13 Kolkata Hooghly West Bengal 14 Cuttack Mahanadi Odisha 15 New Delhi Yamuna Delhi 16 Dibrugarh Brahmaputra Assam 17 Deesa Banas Gujarat 18 Ferozpur Sutlej Punjab 19 Guwahati Brahmaputra Assam 20 Haridwar Ganges Uttarakhand 21 Hyderabad Musi Telangana 22 Jabalpur Narmada Madhya Pradesh 23 Kanpur Ganges Uttar Pradesh 24 Kota Chambal Rajasthan 25 Jammu Tawi Jammu & Kashmir 26 Jaunpur Gomti Uttar Pradesh 27 Patna Ganges Bihar 28 Rajahmundry Godavari Andhra Pradesh 29 Srinagar Jhelum Jammu & Kashmir 30 Surat Tapi Gujarat 31 Varanasi Ganges Uttar Pradesh 32 Vijayawada Krishna Andhra Pradesh 33 Vadodara Vishwamitri Gujarat 1 Source – Wikipedia S.No. City River State 34 Mathura Yamuna Uttar Pradesh 35 Modasa Mazum Gujarat 36 Mirzapur Ganga Uttar Pradesh 37 Morbi Machchu Gujarat 38 Auraiya Yamuna Uttar Pradesh 39 Etawah Yamuna Uttar Pradesh 40 Bangalore Vrishabhavathi Karnataka 41 Farrukhabad Ganges Uttar Pradesh 42 Rangpo Teesta Sikkim 43 Rajkot Aji Gujarat 44 Gaya Falgu (Neeranjana) Bihar 45 Fatehgarh Ganges -
1 Indus River System River Origin Tributries/Meets with Remarks
Indus River System River Origin Tributries/Meets with Remarks Indus Chemayungdung Jhelum, Ravi, Beas, Satluj, 2880 Kms Glacier near Chenab Drains in Arabian sea Mansarovar Lake Zaskar,Syang,Shigar & east of Karachi Gilgit Shyok,Kabul,Kurram,Gomal Jhelum Sheshnag lake, near Navigable b/w Beninag in Pirpanjal Anantnag and range Baramulla in Kashmir vally Ravi Rohtang Pass, Kangra Distt. Beas Beaskund, Near origin Tributary of Satluj, meets of Ravi near Kapurthala Satluj Lake Rakas, Near Enters HP near Shipki Mansarovar lake La Pass Indus Water Treaty, 1960 :-> India can use 20 % of the Indus, Satluj & Jhelum & 80% of Chenab Ravi & Beas 5 Rivers of Punjab :-> Satluj, Ravi, Chenab, Beas & Jhelum ( All these as a combined stream meets Indus at Mithankot) Chenab in HP is known as Chandrabhanga because Chenab originate in form of two streams: Chandra & Bhanga on both the sides of the Bada Laccha La pass in HP. Ganga River System Ganga Tributary Origin Meeting Point Remarks Yamuna Yamunotri Glaciar Allahbad (Prayag) Tributaries: Tons, Hindon, Sharda, Kunta, Gir, Rishiganga, Hanuman Ganga, Chambal, Betwa, Ken, Sindh Son (aka ‘Savan’) Amarkantak (MP), Comes straight from peninsular plateau near origin of Narmada Damodar Chandawa, Palamau Hoogli, South of Carries water of Chotanagpur plateau distt. On Chota Kolkata Nagpur plateau (Jharkhand) Ramganga: Doodhatoli ranges, Ibrahimpur (UP) Pauri Gharwal, Uttrakhand 1 Gandak Nhubine Himal Glacier, Sonepur, Bihar It originates as ‘Kali Gandak’ Tibet-Mustang border Called ‘Narayani’ in Nepal nepal Bhuri Gandak Bisambharpur, West Khagaria, Bihar Champaran district Bhagmati Where three headwater streams converge at Bāghdwār above the southern edge of the Shivapuri Hills about 15 km northeast of Kathmandu Kosi near Kursela in the Formed by three main streams: the Katihar district Tamur Koshi originating from Mt. -
Final Technical Report on the Results of the UNESCO/Korean Funds-In
UNESCO/Republic of Korea Funds-in-Trust Final Technical Report on the results of the UNESCO/Korean Funds-in-Trust Project: Support for the Preparation for the World Heritage Serial Nomination of the Silk Roads in South Asia, 2013- 2016 2016 Final Technical Report on the results of the UNESCO/Korean Funds-in-Trust project: Support for the Preparation for the World Heritage Serial Nomination of the Silk Roads in South Asia, 2013-2016 Executing Agency: • UNESCO World Heritage Centre, in collaboration with UNESCO Field Offices in Kathmandu and New Delhi Implementing partners: • National Commissions for UNESCO of Bhutan, China, India, and Nepal • Department of Archaeology of Nepal (DoA) • Archaeological Survey of India (ASI) • Division for Conservation of Heritage Sites, Department of Culture, Ministry of Home and Cultural Affairs, Royal Government of Bhutan • State Administration of Cultural Heritage of China • ICOMOS International • ICOMOS International Conservation Centre – Xi’an (IICC-X) • University College London, UK Written & compiled by: Tim Williams (Institute of Archaeology, University College London) Edited by: Tim Williams, Roland Lin Chih-Hung (Asia and the Pacific Unit, World Heritage Centre, UNESCO) and Gai Jorayev (Institute of Archaeology, University College London) Prepared for publication by Gai Jorayev at the Institute of Archaeology, University College London www.ucl.ac.uk/archaeology ISBN: 978-0-9956132-0-1 Creative commons licence: Attribution-NonCommercial-NoDerivatives 4.0 International. Share, copy and redistribute this publication in any medium or format under the following terms: Attribution — You must give appropriate credit and indicate if changes were made. NonCommercial — You may not use the material for commercial purposes. -
"MAGIC BOOK" GK PDF in English
www.gradeup.co www.gradeup.co Content 1. Bihar Specific General Knowledge: • History of Bihar • Geography of Bihar • Tourism in Bihar • Mineral & Energy Resources in Bihar • Industries in Bihar • Vegetation in Bihar • National Park & Wildlife Sanctuaries in Bihar • First in Bihar • Important Tribal Revolt in Bihar • Bihar Budget 2020-21 2. Indian History: • Ancient India • Medieval India • Modern India 3. Geography: 4. Environment: 5. Indian Polity & Constitution: 6. Indian Economy: 7. Physics: 8. Chemistry: 9. Biology: www.gradeup.co HISTORY OF BIHAR • The capital of Vajji was located at Vaishali. • It was considered the world’s first republic. Ancient History of Bihar Licchavi Clan STONE AGE SITES • It was the most powerful clan among the • Palaeolithic sites have been discovered in Vajji confederacy. Munger and Nalanda. • It was situated on the Northern Banks of • Mesolithic sites have been discovered from Ganga and Nepal Hazaribagh, Ranchi, Singhbhum and Santhal • Its capital was located at Vaishali. Pargana (all in Jharkhand) • Lord Mahavira was born at Kundagram in • Neolithic(2500 - 1500 B.C.) artefacts have Vaishali. His mother was a Licchavi princess been discovered from Chirand(Saran) and (sister of King Chetaka). Chechar(Vaishali) • They were later absorbed into the Magadh • Chalcolithic Age items have been discovered Empire by Ajatshatru of Haryanka dynasty. from Chirand(Saran), Chechar(Vaishali), • Later Gupta emperor Chandragupta married Champa(Bhagalpur) and Taradih(Gaya) Licchavi princess Kumaradevi. MAHAJANAPADAS Jnatrika Clan • In the Later Vedic Age, a number of small • Lord Mahavira belonged to this clan. His kingdoms emerged. 16 monarchies and father was the head of this clan. republics known as Mahajanapadas stretched Videha Clan across Indo-Gangetic plains. -
Report on the Flora and Fauna of the Kanchenjunga Region
I 1- I I Report Series, # 13 I r Report on the Flora and Fauna of the Kanchenjunga Region Chris Carpenter (Ph.D.) Suresh Ghimire (M.Sc.) Taylor Brown (M.A.) '\Vildlands Study Program, San Francisco State University -n-an 100.;1 Autu.I.....LI. .... ~.//"'T PREFACE The \\'orid Wildlife Fund Nepal Program is pleased to present this series of research reports. Though VrWF has been active in Nepal since 1967. there has been a gap in the public's knowledge of \V\VF' s \vorks. These reports help bridge that gap by offering the conscn'ation community access to works funded andior executed by \V\VF. The report series attests to the din:rsity and complexity of the conservation challenges facing Nepal. Some reports feature scientific research that will enable ecologically sound conservation management of protected areas and endangered species. Other reports represent research in areas that are relatively less known or studied (e.g. the proposed Kanchenjunga Conservation Area or the impact of pesticides in Nepal). The \Vildlands Studies Program. San Francisco State University, has conducted ecological surveys of vegetation and \vildlife in eastern Nepal for the past 5 years. These reports detail the community structure of forests and alpine zones in the Kanchenjunga area. Tree, wildlife. and bird species observed are given with altitudinal and habitat distribution. The report augments \VWF's feasibility study of the proposed Kanchenjunga Conservation Area by providing up-to-date data on this unique and under-studied ecosystem. WWF thanks the Wildlands Studies Program, Dr. Chris Carpenter and his students for their contributions. -
Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys
Louisiana State University LSU Digital Commons LSU Historical Dissertations and Theses Graduate School 1955 Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys. S. Ali ibne hamid Rizvi Louisiana State University and Agricultural & Mechanical College Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_disstheses Recommended Citation Rizvi, S. Ali ibne hamid, "Comparative Physiography of the Lower Ganges and Lower Mississippi Valleys." (1955). LSU Historical Dissertations and Theses. 109. https://digitalcommons.lsu.edu/gradschool_disstheses/109 This Dissertation is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Historical Dissertations and Theses by an authorized administrator of LSU Digital Commons. For more information, please contact [email protected]. COMPARATIVE PHYSIOGRAPHY OF THE LOWER GANGES AND LOWER MISSISSIPPI VALLEYS A Dissertation Submitted to the Graduate Faculty of the Louisiana State University and Agricultural and Mechanical College in partial fulfillment of the requirements for the degree of Doctor of Philosophy in The Department of Geography ^ by 9. Ali IJt**Hr Rizvi B*. A., Muslim University, l9Mf M. A*, Muslim University, 191*6 M. A., Muslim University, 191*6 May, 1955 EXAMINATION AND THESIS REPORT Candidate: ^ A li X. H. R iz v i Major Field: G eography Title of Thesis: Comparison Between Lower Mississippi and Lower Ganges* Brahmaputra Valleys Approved: Major Prj for And Chairman Dean of Gri ualc School EXAMINING COMMITTEE: 2m ----------- - m t o R ^ / q Date of Examination: ACKNOWLEDGMENT The author wishes to tender his sincere gratitude to Dr. Richard J. Russell for his direction and supervision of the work at every stage; to Dr. -
FLOOD FREQUENCY ANALYSIS for KOSI RIVER at ITS BARRAGE SITE Radha Krishan1 and L.B
J. Indian Water Resour. Soc., Vol 36, No. 1, January, 2016 FLOOD FREQUENCY ANALYSIS FOR KOSI RIVER AT ITS BARRAGE SITE Radha Krishan1 and L.B. Roy2 ABSTRACT Floods are natural events that have always been an integral part of the geologic history of earth. Human settlements and coactivity have always tended to use flood plains. The Kosi river in north Bihar plains of Eastern India presents a challenge in terms of long and recurring flood hazard. Despite a long history of flood control management in the basin for more than five decades, the river continues to bring a lot of misery through extensive flooding. In the present paper the Log-Pearson Type III distribution, a statistical technique for fitting frequency distribution, has been used to predict the design flood for the river at its barrage site for the discharge data from 1964 to 2008 obtained from WRD, Govt. of Bihar. Apart from this the morphology of the River and the Kosi project have also been described and discussed. Keywords: Floods, Kosi river, frequency distribution methods INTRODUCTION Flood and drainage are the two vital interrelated problems of Bihar, a poverty stricken state particularly in North Bihar. The North Bihar plains are drained by some Himalayan rivers and the Ganga being the trunk drain. These rivers are perennial as these are rain as well as snow fed. Important rivers of North Bihar include the Kosi, Gandak, Baghmati, Burhi Gandak, Kamla, Kamla-Balan Mahananda, Kareh and few others. All these rivers have relatively youthful topography and are engaged in channel deepening. They move parallel to the Ganga in the South-east direction and then drain into it. -
Hydrology and Water Resources Development in Nepal
HYDROLOGY AND WATER RESOURCES DEVELOPMENT IN NEPAL Prepared by the United States Geological Survey in cooperation with the Nepalese Department of Hydrology and Meteorology under the auspices of the United States Agency for 1!1ternational Development Hyih"ology and Water Resources Development in Nepal by W. W. Evett U. S. Geological Survey Open File Report Contents Page Abstract------------------------------------------------ 1 Introduction--------------------------------------------- 4 Puysical Features---------------------------------------- 11 Topography------------------------------------------ 11 Climate---------------------------------------------- 17 Water and History of Nepal------------------------------ 20 Dnportance of Water in Nepal's Development---------------------------------------- 22 Hydrologic Investigations---------------------------- 23 Surface Water----------------------------------- 24 Ground Water------------------------------------ 28 Meteorology------------------------------------- 30 Quality of Water------------------------------- 31 Publication of Hydrologic Data------------------ 36 River Basins of Nepal------------------------------------ 38 Major R~ver Basins----------------------------------- 38 Sapt Kosi-------------------------------------- 39 Narayani River--------------------------------- 42 Karnali River---------------------------------- 48 Sardi River------------------------------------- 51 Minor River Basins----------------------------------- 53 Kankai Mai------------------------------------- -
Policy and Institutions in Adaptation to Climate Change Case Study on Flood Mitigation Infrastructure in India and Nepal
ICIMOD Working Paper 2013/4 Policy and Institutions in Adaptation to Climate Change Case study on flood mitigation infrastructure in India and Nepal 1 About ICIMOD The International Centre for Integrated Mountain Development, ICIMOD, is a regional knowledge development and learning centre serving the eight regional member countries of the Hindu Kush Himalayas – Afghanistan, Bangladesh, Bhutan, China, India, Myanmar, Nepal, and Pakistan – and based in Kathmandu, Nepal. Globalization and climate change have an increasing influence on the stability of fragile mountain ecosystems and the livelihoods of mountain people. ICIMOD aims to assist mountain people to understand these changes, adapt to them, and make the most of new opportunities, while addressing upstream-downstream issues. We support regional transboundary programmes through partnership with regional partner institutions, facilitate the exchange of experience, and serve as a regional knowledge hub. We strengthen networking among regional and global centres of excellence. Overall, we are working to develop an economically and environmentally sound mountain ecosystem to improve the living standards of mountain populations and to sustain vital ecosystem services for the billions of people living downstream – now, and for the future. ICIMOD would like to acknowledge the Swedish International Development Cooperation Agency (Sida) for funding this project. ICIMOD gratefully acknowledges the support of its core donors: the Governments of Afghanistan, Austria, Bangladesh, Bhutan, China, -
Cold Water Fisheries in the Trans-Himalayan Countries
ISSN 0429-9345 FAO Cold water fisheries in the FISHERIES TECHNICAL trans-Himalayan countries PAPER 431 FAO Cold water fisheries in the FISHERIES TECHNICAL trans-Himalayan countries PAPER 431 Edited by T. Petr Toowoomba, Queensland Australia and S.B. Swar Directorate of Fisheries Development Balaju, Kathmandu Nepal FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2002 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. ISBN 92-5-104807-X All rights reserved. Reproduction and dissemination of material in this information product for educational or other non-commercial purposes are authorized without any prior written permission from the copyright holders provided the source is fully acknowledged. Reproduction of material in this information product for resale or other commercial purposes is prohibited without written permission of the copyright holders. Applications for such permission should be addressed to the Chief, Publishing Management Service, Information Division, FAO, Viale delle Terme di Caracalla, 00100 Rome, Italy or by e-mail to [email protected] © FAO 2002 iii PREPARATION OF THIS DOCUMENT This volume contains contributions presented at the Symposium on Cold Water Fishes of the Trans-Himalayan Region, which was held on the 10-13 July 2001 in Kathmandu, Nepal. The objectives were to share information on the status of indigenous fish species and fisheries in the Trans-Himalayan region, improve understanding of their importance in peoples’ livelihoods and assess the potential for further development. -
GS PAPER-1 (History, Art & Culture, Social Issues & Geography)
1 2 GS PAPER-1 (History, Art & Culture, Social Issues & Geography) Kharg: Iran's largest warship (Topic- GS Paper I –Geography, Source- Indian Express) Why in the news? • Recently, Kharg the largest warship in the Iranian navy caught fire and later sank in the Gulf of Oman under unclear circumstances. About the Gulf of Oman 3 • The Gulf of Oman or Sea of Oman is a gulf that connects the Arabian Sea with the Strait of Hormuz, which then runs to the Persian Gulf. • It borders Iran and Pakistan on the north, Oman on the south, and the United Arab Emirates on the west. • The Gulf of Oman offers the only entrance from the Arabian Sea and the Indian Ocean into the Persian Gulf. • The world’s major oil exporters and importers have a joint interest in its security. Indian Ocean Dipole monsoon (Topic- GS Paper I –Geography, Source- The Hindu) Why in the news? • Recently the India Meteorological Department has said that monsoon rains will likely be 101% of the Long Period Average (LPA) of 88 cm. Reasons for this LPA • It is due the ‘negative’ IOD (Indian Ocean Dipole) conditions over the Indian Ocean during the monsoon season along with the another climate factors are, as of now, unlikely to have a significant influence over the prevailing monsoon. • In 2020, it was 109% of the LPA and in 2019, 110%. More on the news • The forecast 101% LPA is short of the rainfall received in these years and still within the range of what the IMD considers ‘normal’ rainfall, it is positive news because the current forecast is ‘above normal’ rainfall in the core agricultural zone. -
The Failure of Kosi River (Bihar, India) Embankments and Its Effect on Land Use and Land Cover: a Remote Sensing and GIS Based Approach
Journal of Environment and Earth Science www.iiste.org ISSN 2224-3216 (Paper) ISSN 2225-0948 (Online) Vol.5, No.17, 2015 The failure of Kosi River (Bihar, India) embankments and its effect on land use and land cover: a Remote sensing and GIS based approach Avijit mahala Centre for the study of Regional Development, Jawaharlal Nehru University, New Delhi-110067. Abstract The kosi is an important river system in the north Bihar of India. The kosi is important in terms of its Geological settings, Basin characteristics, Flow characteristics, and its dynamic characteristics. The large upper catchment area, the high number of first and second order stream, large Himalayan glaciers makes the river high flood prone. Kosi originates from upper Himalayas and flows through the shiwaliks, Nepal foothills where river makes large alluvial fan, and finally it joins ganga in plain where large bending are seen. In august, 2008, kosi experience its embankment’s change and devastating flood. The main idea of the paper is to analyzed the morphometric, geological, and anthropogenic causes of such river embankment’s failure with the use of Dem and satellite imagery, how this changes have effect local landuse and land cover characteristics. Key words: River system, Geological settings, Basin characteristics, Alluvial fan, Embankment, Morphometric characteristics. Introduction The eastern state of Bihar in India is a flood-prone fluvial plain, with maximum havoc being caused by the Kosi River and its feeder channels. The recent floods of the Kosi basin by abrupt migration of the master stream eastwards by 110 kilometers have impacted upon the geography of this densely inhabited region.