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Antecedence of the Yarlung–Siang–Brahmaputra River, Eastern Himalaya ∗ Karl A
Earth and Planetary Science Letters 397 (2014) 145–158 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl Antecedence of the Yarlung–Siang–Brahmaputra River, eastern Himalaya ∗ Karl A. Lang , Katharine W. Huntington Department of Earth and Space Sciences and Quaternary Research Center, Johnson Hall, Rm. 070, Box 351310, University of Washington, Box 351310, Seattle, WA 98195, USA article info abstract Article history: At the eastern terminus of the Himalayan orogen, distortion and capture of southeast Asian drainage Received 17 January 2014 basins reflects regional patterns of crustal strain due to the indentation of the Indian Plate into Eurasia. Received in revised form 11 April 2014 After flowing eastward >1000 km along the southern margin of Tibet, the Yarlung–Siang–Brahmaputra Accepted 12 April 2014 River turns abruptly southward through the eastern Himalayan syntaxis rapidly exhuming a crustal scale Available online 13 May 2014 antiform in an impressive >2 km knickpoint. This conspicuous drainage pattern and coincidence of Editor: T.M. Harrison focused fluvial incision and rapid rock exhumation has been explained by the capture of an ancestral, Keywords: high-elevation Yarlung River by headward erosion of a Himalayan tributary. However, recent observation Detrital zircon U–Pb geochronology of Tibetan detritus in Neogene foreland basin units complicates this explanation, requiring a connection River capture from Tibet to the foreland prior to the estimated onset of rapid rock exhumation. We constrain the Arunachal Pradesh Himalaya sedimentary provenance of foreland basin units deposited near the Brahmaputra River confluence in the Siwalik Group eastern Himalayan foreland basin using detrital zircon U–Pb geochronology. -
2017 Global Retirement Index 1
2017 GLOBAL RETIREMENT INDEX 1 Table of Contents Introduction ....................................................................................................................................................... 3 Background ........................................................................................................................................................ 6 Executive summary ............................................................................................................................................ 7 The Global Retirement Index 2017 ................................................................................................................... 8 Framework ......................................................................................................................................................... 9 The Best Performers ........................................................................................................................................ 10 Regional Perspective ....................................................................................................................................... 12 The Top 25: Year-on-Year Trends .................................................................................................................... 14 BRICs trail North America and Western Europe .............................................................................................. 41 Health ............................................................................................................................................................... -
Perennial and Non-Perennial River- River Originating from Mountains, They Get Water Throughout the Year, That River Consider As Perennial River
Perennial and Non-Perennial river- River originating from mountains, they get water throughout the year, that river consider as Perennial river. on the other hand river originating from plateau region called Non-Perennial river. these river do not have enough water for the whole year. Peninsular river- They have a large seasonal fluctuation in volume as they are solely fed from rainfall. These river flow in valley with steep gradients. the river which end in the Bay of Bengal are called 'East flowing' river, If the river empties into the Arabian sea, it is called ' West flowing' river. Inland drainage river- The river which does not empty itself into any sea, and end with any lake or any other water body is known as Inland Drainage river. Classification Indus River Originated from Bokharchu Glacier , near Mansarover. Rivers in India Total length of about 2897 km, it fall into the Arabian sea. Enter in India through Ladakh, flow only in J&K. Ganga River It flow between the Ladakh range and the Zaskar range at Leh. Brahmaputra River Originates as the Bhagirathi from the Gangotri glacier. Originates from Mansaravar Lake. Alaknanda unites with Bhagirathi at Devprayag, Uttarakhand, henceafter know as Ganga. Total length of about 3848 km. It fall into Bay of Bengal. At Bangladesh, Ganga merge with Brahmaputra, mixture known as Padma river. Enter India in Arunachal Pradesh. most of its course lies outside India. Total length of about 2510 km, It fall into the Bay of Bengal. It flow parallel to the Himalayas in the eastward direction. Originate from the Yamunotri glacier, at the Bandarpoonch peak in Uttarakhand. -
Psilorhynchus Kamengensis, a New Species of Fish (Teleostei: Psilorhynchidae) from Northeast India
70 (2): 101 – 110 © Senckenberg Gesellschaft für Naturforschung, 2020. 2020 Psilorhynchus kamengensis, a new species of fish (Teleostei: Psilorhynchidae) from northeast India Abhinit Dey 1, Hrishikesh Choudhury 1, Abhishek Mazumder 1, Ratul Ch. Bharali 2, Sarbojit Thaosen 3 & Dandadhar Sarma 1, * 1 Department of Zoology, Gauhati University, Guwahati 781014, Assam (India) — 2 Department of Zoology, Udalguri College, Udalguri (BTAD) 784509, Assam (India) — 3 Department of Zoology, Haflong Govt. College, Haflong 788819, Assam (India) — *Corresponding Author: [email protected] Submitted January 21, 2020. Accepted February 19, 2020. Published online at www.senckenberg.de/vertebrate-zoology on April 1, 2020. Published in print Q2/2020. Editor in charge: Ralf Britz Abstract Psilorhynchus kamengensis, new species, is described from a stream of the Kameng River, a northern tributary to the Brahmaputra drain- age, Arunachal Pradesh, northeast India. The new species belongs to the P. balitora species group and can be distinguished from all other members of this group by the presence of a longer post-epiphyseal fontanelle, 3 unbranched anal-fn rays, 9 + 8 caudal-fn rays, 35 vertebrae and fn coloration. The validity of the species is also corroborated by molecular phylogenetic analysis based on the mitochondrial cyt b gene. Key words Torrent minnow, Kameng, morphology, cyt b, phylogeny. Introduction Cypriniform fshes of the genus Psilorhynchus McClel- The Kameng River is the major drainage in East and land, 1838 are characterized by having an arched dor- West Kameng districts of Arunachal Pradesh, northeast sum with fattened ventral surface, horizontally-placed India. The Kameng originates from the Greater Himala- paired fns, a naked breast and an inferior mouth devoid yas, at an elevation of more than 7000 m, and descends of barbels (RAINBOTH, 1983). -
2014 Global Retirement Index
2014 Global Retirement Index As an ESOMAR member, CoreData Research complies with the ICC/ESOMAR International Code of Marketing and Social Research Practice. Disclaimer This paper was compiled from primary research and other information available at the time of writing. The information is believed to be accurate however no representation or warranty express or implied is made as to its completeness and CoreData Research does not make any warranty to correct any information subseQuently found to be inaccurate. This paper does not constitute investment advice or a business recommendation. This paper may contain the personal views, standards and opinions of the researchers and third party contributors. The inclusion of this material is not an endorsement by CoreData Research. In all cases, people reading this material should attain appropriate professional advice in evaluating its accuracy, currency, completeness and relevance for their purposes. CoreData Research disclaims any direct or indirect liability or costs arising from any reliance on the information contained within this publication. LONDON | BOSTON | SYDNEY | BEIJING | MANILA | SAO PAULO | CAPE TOWN 2 LONDON | BOSTON | SYDNEY | BEIJING | MANILA | SAO PAULO | CAPE TOWN 3 Contents Background .................................................................................................................................................................... 5 Executive Summary ...................................................................................................................................................... -
West Kameng District, Arunachal Pradesh
Technical Report Series: D No: Ground Water Information Booklet West Kameng District, Arunachal Pradesh Central Ground Water Board North Eastern Region Ministry of Water Resources Guwahati September 2013 WEST KAMENG DISTRICT AT A GLANCE Sl.No. ITEMS STATISTICS 1 GENERAL INFORMATION i) Geographical area (sq.km.) 7422 ii) Administrative Divisions (As on 31st March, 01 sub-divisions 2011) Number of Tehsils/Block 04 Number of Panchayat/villages/Circles 212 villages, 10circles iii) Population (As per 2011 census) 87013 iv) Average Annual Rainfall (mm) 1607 2 GEOMORPHOLOGY Denudo structural hills, Structural hills, valley fills Major physiographic units High Mountainous peaks Irregular land forms Major Drainages Kameng river and its tributaries viz. Tenga, Bichom and Dirang 3 LAND USE a) Forest area (reserved forest) 708.35hac b) Net area sown 5303 hac c) Gross cropped area 5386 hac 4 MAJOR SOIL TYPES Alluvial and residual soils 5 AREA UNDER PRINCIPAL CROPS (As on 2010-11), in Rice, Wheat and Maize sq.km.) 6 IRRIGATION BY DIFFERENT SOURCES (Areas and numbers of Structures) Dug wells Nil Tube wells Nil Tanks/ponds Nil Canals 26 Nos. 53 Hectares Other sources (Hand pumps) Nil Net irrigated area 191.66 Hectares Gross irrigated area 191.66 hectares 7 NUMBER OF GROUND WATER MONITORING WELLS OF CGWB (As on 31.3.2013) No. of Dug wells No. of Piezometers Nil 8 PREDOMINENT GEOLOGICAL FORMATIONS Bomdilla Group, Tenga Formation 9 HYDROGEOLOGY Older alluvium and River Terraces, Siwalik Group, Gondwana Formations 10 GROUND WATER EXPLORATION BY CGWB (as -
The Status of Glaciers in the Hindu Kush-Himalayan Region
The Status of Glaciers in the Hindu Kush-Himalayan Region The Status of Glaciers in the Hindu Kush-Himalayan Region Editors Samjwal Ratna Bajracharya Basanta Shrestha International Centre for Integrated Mountain Development, Kathmandu, Nepal, November 2011 Published by International Centre for Integrated Mountain Development GPO Box 3226, Kathmandu, Nepal Copyright © 2011 International Centre for Integrated Mountain Development (ICIMOD) All rights reserved. Published 2011 ISBN 978 92 9115 215 5 (printed) 978 92 9115 217 9 (electronic) LCCN 2011-312013 Printed and bound in Nepal by Sewa Printing Press, Kathmandu, Nepal Production team A Beatrice Murray (Consultant editor) Andrea Perlis (Senior editor) Dharma R Maharjan (Layout and design) Asha Kaji Thaku (Editorial assistant) Note This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. ICIMOD would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or for any other commercial purpose whatsoever without prior permission in writing from ICIMOD. The views and interpretations in this publication are those of the author(s). They are not attribuTable to ICIMOD and do not imply the expression of any opinion concerning the legal status of any country, territory, city or area of its authorities, or concerning the delimitation of its frontiers or boundaries, or the endorsement of any product. This publication is available in electronic form at www.icimod.org/publications Citation: Bajracharya, SR; Shrestha, B (eds) (2011) The status of glaciers in the Hindu Kush-Himalayan region. -
IRBM for Brahmaputra Sub-Basin Water Governance, Environmental Security and Human Well-Being
IRBM for Brahmaputra Sub-basin Water Governance, Environmental Security and Human Well-being Jayanta Bandyopadhyay Nilanjan Ghosh Chandan Mahanta IRBM for Brahmaputra Sub-basin Water Governance, Environmental Security and Human Well-being Jayanta Bandyopadhyay Nilanjan Ghosh Chandan Mahanta i Observer Research Foundation 20, Rouse Avenue Institutional Area, New Delhi - 110 002, INDIA Ph. : +91-11-43520020, 30220020 Fax : +91-11-43520003, 23210773 E-mail: [email protected] ©2016 Copyright: Observer Research Foundation ISBN: 978-81-86818-22-0 ALL RIGHTS RESERVED. No part of this book shall be reproduced, stored in a retrieval system, or transmitted by any means, electronic, mechanical, photocopying, recording, or otherwise, without the prior written permission of the copyright holder (s) and/or the publisher. Typeset by Vinset Advt., Delhi Printed and bound in India Cover: Vaibhav Todi via Flickr. ii IRBM for Brahmaputra Sub-basin: Water Governance, Environmental Security and Human Well-being Table of Contents About the Authors v Acknowledgements vi Foreword vii Preface ix I The Brahmaputra River Sub-basin 1 II Integrated Management of Trans-boundary Water Regimes: A Conceptual Framework in the Context of Brahmaputra Sub-basin 19 III The Brahmaputra Sub-basin in the DPSIR Framework 43 IV Management Challenges Facing Human Well-being and Environmental Security in the Brahmaputra Sub-basin 49 V Institutional Response: A Regional Organisation for the Lower Brahmaputra Sub-basin 61 References 73 iii IRBM for Brahmaputra Sub-basin: Water Governance, Environmental Security and Human Well-being About the Authors Jayanta Bandyopadhyay is a retired Professor from IIM Calcutta. He obtained his PhD in Engineering from IIT Kanpur, and after completing his doctoral work, shifted his research interests to the Himalaya and, in particular, the challenges in sustaining the region's rivers. -
District Census Handbook, Kameng, Part X, Series-24, Arunachal Pradesh
CENSUS OF INDIA- 1971 Series No. 24 ARUNACHAL PRAI)ESH PART X DISTRICT CENSUS HANDBOOK KAMENG DISTRICT Part A: TOWN & VILLAGE--DIREGTORY Part B : ,URBAN BbOCK I VILLAGEWISE PRIMARY CENSUS ABSTRACT J. K. Barthakur, of tke Indian Frontier Administratwe Service~ Director of Census Operat~ ~unoohal-prau~--- , Shillong-3 ·A'P.(u. ~ Statements made. views expressed or con clusions drawn in this report are wholly the responsibil ity of the author alone in his perso nal capacity and do not necessarily represent the views of the Government. Arunachai ~ad* is til thinly pbpuitilted hiIiy tract lying touah1v be'" ween the latitudes ~ and 29"3O'N and the longitudes 91.°3O'E and,97°30'E on the north east extremity of India, compi-ising roughly of 83,578 kilometre squares of area. bordering the international boundaries of Bhutan. Tibet, China and Burma. The Pradesh is known to be rich in flora. fauna, power and mine ral potentia1. When the 1971 Census was taken in Arunachal Pradesh, the area was known as the North East Frontier Agency (NEFA in short) which was consti tutionally a part of ~e State of AsSam. At that time NEFA was directly_ ad ministered by the President of India through the Governor of Assam as his agent, who was assisted by an adviser. The office_ of the Adviser to the Gover· nor of AssQUl was situated at Shillong, t~e capital of the Assam. State. On the 21st -JanUary, 1972, NEFA haa been ttlade into a Union Territory under the provision of the North-Eastern Areas (Reorganisation) Act. -
C. Arunachal Pradesh – Sulung 121
c. arunachal pradesh – sulung 121 SULUNG Overview Assam. We talked about local problems, like trans- port. Sulung (also known as Puroik) settlements are small, Officially there was a bus service from Seppa once with typically five to ten houses and no systematic a week, but sometimes the bus didn’t come at all. plan. They are often located on isolated spurs near Supply of diesel was also a problem because the areas where sago palms grow. Houses are simple and lorry hadn’t come, and so the generator couldn’t work of a rectangular type on a raised platform, accom- and there was no electricity. And for some time the modating a nuclear family. In case of more wives or high tension cable from Seppa had been out of action. families, each wife has her own room and hearth. Mr Doley thought the diesel wouldn’t arrive for a long Houses in interior areas, however, are said to be much time. larger, up to 5 × 24 metres. We talked about the Sulungs. He explained that The sections of the house are: front veranda with they were poor and still dependent on Bangnis and ritual space; a central room with one fireplace; a nar- Nyishis. In fact, slavery had not really disappeared. row corridor-like side room for storage and toilet; He agreed with what the Additional Deputy Com- rear veranda for storage. A notched log leads to both missioner in Seppa had told us yesterday about the verandas. Granaries are built at some distance from government project to buy the Sulungs’ liberty: the the houses. -
Kameng River Arunachal Pradesh Signature Trip of Himalayan River Runners
Estd. 1988 Himalayan River Runners (India) Pvt. Ltd C1, Basement, Community Centre, Safdarjung Development Area, New Delhi -10016, India Tel:01126968169, 26852602 E- mail:[email protected] Website: www.hrrindia.com ‘New Frontier’ Kameng River Arunachal Pradesh Signature trip of Himalayan River Runners The tribal State of Arunachal Pradesh on the north eastern extremity of India bordering Tibet remains lesser known and explored. It is perhaps the richest State in India in terms of bio diversity, tribal culture, abundant riverine systems and luxuriant rain forests. Himalayan River Runners pioneered several of these rivers like the Subansiri and Lohit in the early 90’s while training the Indian Army. Recently we added another feather to our cap - opening the Kameng River for whitewater adventure and exploration in the hitherto closed East Kameng District. Our 9 day journey to this unexplored wilderness offers world class whitewater, close interaction with the local tribals of the region - the Nishis, and a chance to learn about the vast bio-diversity of the region from the locals themselves. Day 1: Fly Delhi - Guwahati - Kingfisher Flt IT 3357 departing 0845hrs. Arv 1120 hrs. Drive onto the Eco Camp Nameri near the banks of the Kameng River, a six hour 220 km drive from Guwahati. Overnight Eco Camp. Day 2: Explore the environs around the Eco Camp, within the Nameri National Park, a biodiversity hotspot and home to several endangered avian and animal species of the region. Overnight at the Eco Camp. Day 3: Depart Eco Camp after an early breakfast. Drive along the Kameng River thru verdant Arunachal countryside. -
2016 Natixis Global Retirement Index
PERSONAL RESPONSIBILITY. PUBLIC TRUST. 2016 Natixis Global Retirement Index 2016 GLOBAL RETIREMENT INDEX 1 2016 GLOBAL RETIREMENT INDEX 3 ABOUT THE GLOBAL RETIREMENT INDEX 5 PERSONAL RESPONSIBILITY. PUBLIC TRUST. 8 LEARNING FROM THE LEADERS 11 THE TOOLS FOR BUILDING PUBLIC TRUST 15 MEETING TRUST WITH PERSONAL AND PUBLIC MEASURES 17 THE GLOBAL RETIREMENT INDEX 2016 43 THE EMERGING ECONOMIES: LACKLUSTER PERFORMANCE 51 HEALTH INDEX 53 FINANCES IN RETIREMENT INDEX 55 QUALITY OF LIFE/NATURAL ENVIRONMENT INDEX 57 MATERIAL WELLBEING INDEX 59 REFERENCES 60 APPENDIX A: METHODOLOGY 66 APPENDIX B: FULL RANKINGS 2 2016 GLOBAL RETIREMENT INDEX About the Global Retirement Index The Global Retirement Index (GRI) is a multi-dimensional index developed by Natixis Global Asset Management and CoreData Research to examine the factors that drive retirement security and to provide a comparison tool for best practices in retirement policy. The index incorporates 18 performance indicators, grouped into four thematic sub-indices, which have been calculated on the basis of reliable data from a range of international organizations and academic sources. It takes into account the particular characteristics of the older demographic retiree group in order to assess and compare the level of retirement security in different countries around the world. The four thematic indices cover key aspects for welfare in retirement: the material means to live comfortably in retirement; access to quality financial services to help preserve savings value and maximize income; access to quality health services; and a clean and safe environment. The sub-indices provide insight into which particular characteristics are driving an improvement or worsening each country’s position.