Date: 06.11.2017 Time Activities Hall Name
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
Komandorsky Zapovednik: Strengthening Community Reserve Relations on the Commander Islands
No. 36 Summer 2004 Special issue: Russia’s Marine Protected Areas PROMOTING BIODIVERSITY CONSERVATION IN RUSSIA AND THROUGHOUT NORTHERN EURASIA CONTENTS CONTENTS Voice from the Wild (A letter from the editors)......................................1 Komandorsky Zapovednik: Strengthening Community Reserve Relations on the Commander Islands......................................24 AN INTRODUCTION TO MARINE Lazovsky Zapovednik: PROTECTED AREAS Working to Create a Marine Buffer Zone...................................................28 MPAs: An Important Tool in Marine Conservation......…………………...2 Kurshskaya Kosa National Park: Tides of Change: Tracing the Development Preserving World Heritage on the Baltic Sea ..........................................30 of Marine Protected Areas in Russia .................................................................4 Dalnevostochny Morskoi Zapovednik: How Effective Are Our MPAs? Looking for Answers An Important Role to Play.........................................................................................6 with Russia’s First Marine Protected Area..................................................32 The Challenges that Lie Ahead.....................………………………………………………8 Russia’s Marine Biosphere Reserves......………………………………………………10 MPA Workshop Offers Opportunities for Dialogue..........................13 THE FUTURE Plans for the Future: Developing a Network of Marine Protected Areas .....................................................……....………………...35 CASE STUDIES An Introduction .............................................................................……....………………...14 -
Status and Protection of Globally Threatened Species in the Caucasus
STATUS AND PROTECTION OF GLOBALLY THREATENED SPECIES IN THE CAUCASUS CEPF Biodiversity Investments in the Caucasus Hotspot 2004-2009 Edited by Nugzar Zazanashvili and David Mallon Tbilisi 2009 The contents of this book do not necessarily reflect the views or policies of CEPF, WWF, or their sponsoring organizations. Neither the CEPF, WWF nor any other entities thereof, assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, product or process disclosed in this book. Citation: Zazanashvili, N. and Mallon, D. (Editors) 2009. Status and Protection of Globally Threatened Species in the Caucasus. Tbilisi: CEPF, WWF. Contour Ltd., 232 pp. ISBN 978-9941-0-2203-6 Design and printing Contour Ltd. 8, Kargareteli st., 0164 Tbilisi, Georgia December 2009 The Critical Ecosystem Partnership Fund (CEPF) is a joint initiative of l’Agence Française de Développement, Conservation International, the Global Environment Facility, the Government of Japan, the MacArthur Foundation and the World Bank. This book shows the effort of the Caucasus NGOs, experts, scientific institutions and governmental agencies for conserving globally threatened species in the Caucasus: CEPF investments in the region made it possible for the first time to carry out simultaneous assessments of species’ populations at national and regional scales, setting up strategies and developing action plans for their survival, as well as implementation of some urgent conservation measures. Contents Foreword 7 Acknowledgments 8 Introduction CEPF Investment in the Caucasus Hotspot A. W. Tordoff, N. Zazanashvili, M. Bitsadze, K. Manvelyan, E. Askerov, V. Krever, S. Kalem, B. Avcioglu, S. Galstyan and R. Mnatsekanov 9 The Caucasus Hotspot N. -
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). -
New Records of Megachilid Bees (Hymenoptera, Megachilidae) from the North Caucasus and Neighboring Regions of Russia1 A
ISSN 0013-8738, Entomological Review, 2018, Vol. 98, No. 9, pp. 1165–1174. © Pleiades Publishing, Inc., 2018. New Records of Megachilid Bees (Hymenoptera, Megachilidae) from the North Caucasus and Neighboring 1 Regions of Russia A. V. Faterygaa*, M. Yu. Proshchalykinb**, Yu. V. Astafurovac***, and I. B. Popovd**** aT.I. Vyazemsky Karadag Scientific Station—Nature Reserve of the Russian Academy of Sciences, Feodosiya, 298188 Russia *e-mail: [email protected] bFederal Scientific Center of the East Asia Terrestrial Biodiversity, Far Eastern Branch, Russian Academy of Sciences, Vladivostok-22, 690022 Russia **e-mail: [email protected] cZoological Institute, Russian Academy of Sciences, St. Petersburg, 199034 Russia ***e-mail: [email protected] dI.T. Trubilin Kuban State Agrarian University, Krasnodar, 350044 Russia ****e-mail: [email protected] Received February 14, 2019 Revised February 18, 2019 Accepted February 18, 2019 Abstract—New data on the distribution of 37 species are reported. Eleven species are new to Russia: Lithurgus tibialis Morawitz, 1875, Anthidium spiniventre Friese, 1899, Icteranthidium ferrugineum (Fabricius, 1787), Hoplitis carinata (Stanek, 1969), Coelioxys acanthura (Illiger, 1806), C. decipiens (Spinola, 1838), Megachile al- bonotata Radoszkowski, 1886, M. pyrenaica (Lepeletier de Saint-Fargeau, 1841), M. burdigalensis Benoist, 1940, M. flavipes Spinola, 1838, and M. tecta Radoszkowski, 1888. Twenty species are new to the North Caucasus, five species are new to the south of the European part of Russia, and one species, Megachile leucomalla Gerstäcker, 1869, is new to the North Caucasus and south of the European part of Russia; the latter species is also reported for the first time from Iran. Hoplitis ravouxi (Pérez, 1902) is excluded from the list of the Russian fauna. -
Ground Water Scenario of Himalaya Region, India
Hkkjr ds fgeky;h {ks=k dk Hkwty ifjn`'; Ground Water Scenario of Himalayan Region, India laiknu@Edited By: lq'khy xqIrk v/;{k Sushil Gupta Chairman Central Ground Water Board dsanzh; Hkwfe tycksMZ Ministry of Water Resources ty lalk/ku ea=kky; Government of India Hkkjr ljdkj 2014 Hkkjr ds fgeky;h {ks=k dk Hkwty ifjn`'; vuqØef.kdk dk;Zdkjh lkjka'k i`"B 1- ifjp; 1 2- ty ekSle foKku 23 3- Hkw&vkd`fr foKku 34 4- ty foKku vkSj lrgh ty mi;kst~;rk 50 5- HkwfoKku vkSj foorZfudh 58 6- Hkwty foKku 73 7- ty jlk;u foKku 116 8- Hkwty lalk/ku laHkko~;rk 152 9- Hkkjr ds fgeky;h {ks=k esa Hkwty fodkl ds laca/k esa vfHktkr fo"k; vkSj leL;k,a 161 10- Hkkjr ds fgeky;h {ks=k ds Hkwty fodkl gsrq dk;Zuhfr 164 lanHkZ lwph 179 Ground Water Scenario of Himalayan Region of India CONTENTS Executive Summary i Pages 1. Introduction 1 2. Hydrometeorology 23 3. Geomorphology 34 4. Hydrology and Surface Water Utilisation 50 5. Geology and Tectonics 58 6. Hydrogeology 73 7. Hydrochemistry 116 8. Ground Water Resource Potential 152 9. Issues and problems identified in respect of Ground Water Development 161 in Himalayan Region of India 10. Strategies and plan for Ground Water Development in Himalayan Region of India 164 Bibliography 179 ifêdkvks dh lwph I. iz'kklfud ekufp=k II. Hkw vkd`fr ekufp=k III. HkwoSKkfud ekufp=k d- fgeky; ds mRrjh vkSj if'peh [kaM [k- fgeky; ds iwohZ vkSj mRrj iwohZ [kaM rFkk iwoksZRrj jkT; IV. -
Erosion–Deposition and Land Use/Land Cover of the Brahmaputra River in Assam, India
J. Earth Syst. Sci. (2019) 128:211 Ó Indian Academy of Sciences https://doi.org/10.1007/s12040-019-1233-3 (0123456789().,-vol.:V)( 0123456789().,-vol.:V) Erosion–deposition and land use/land cover of the Brahmaputra river in Assam, India 1, 2 3 LALIT SAIKIA * ,CHANDAN MAHANTA ,ABHIJIT MUKHERJEE 4 and SURANJANA BHASWATI BORAH 1 Department of Earth Science, University of Science and Technology Meghalaya, 9th Mile, Meghalaya, India. 2 Department of Civil Engineering, Indian Institute of Technology Guwahati, Guwahati, India. 3 Department of Geology and Geophysics, Indian Institute of Technology Kharagpur, Kharagpur, India. 4 Department of Environmental Science, Tezpur University, Tezpur, India. *Corresponding author. e-mail: [email protected] [email protected] MS received 16 August 2018; revised 17 May 2019; accepted 24 May 2019 The Brahmaputra is a unique dynamic river in the world with intense braiding and critical bank erosion. Both erosion and deposition are continuous processes in the river in an attempt to reach a new equi- librium in channel geometry and morphology by the ever dynamic nature of flow. Erosion and deposition of the river have link to land use and land cover (LULC) as the land cover is under constant change in a dynamic landscape constantly shaped by continuous erosion and deposition. The objective of the present work is to evaluate the extent of erosion and deposition along the Brahmaputra river and change in the LULC of the Brahmaputra river in Assam, India. Remote sensing and geographic information system (GIS) techniques were utilised to extract information from Landsat images. Total area of erosion and deposition during 1973–2014 was 1557 and 204 km2, respectively. -
DHI Report UK
Preparation of Two Stage Detailed Project Report (DPR) of Proposed Cluster 2 Inland Waterways Feasibility Report for NW-31 Dhansiri/Chathe River September 2016 Inland Waterways Authority of India Feasibility Report September 2016 Preparation of Two Stage Detailed Project Report (DPR) of Proposed Cluster 2 Inland Waterways Feasibility Report for NW-31 Dhansiri/Chathe River Final September 2016 Prepared for Inland Waterways Authority of India Represented by Hydrographic Chief Dr. Ruchi Kalra, Bibekananda Padhy, Arjun S, Dr. B. Sakthivel, Swarup Dutta, Dr. Mohd. Authors Fahimuddin Quality supervisor Dr. Flemming Jakobsen, Team Leader Project number 63800891 Approval date 21.09.2016 Revision 1 Classification Confidential DHI (India) Water & Environment Pvt Ltd•NSIC Bhawan, IIIrd Floor, NSIC - STP Complex•Okhla Industrial Estate•IN- 11 00 20New Delhi• India Telephone: +91 11 4703 4500 • Telefax: +91 11 4703 4501 • • www.dhigroup.com This report has been prepared under the DHI Business Management System certified by Bureau Veritas to comply with ISO 9001 (Quality Management) Approved by Dr. Flemming Jakobsen Managing Director DHI (India) Water & Environment Pvt Ltd•NSIC Bhawan, IIIrd Floor, NSIC - STP Complex•Okhla Industrial Estate•IN- 11 00 20New Delhi• India Telephone: +91 11 4703 4500 • Telefax: +91 11 4703 4501 • • www.dhigroup.com Contents List of Abbreviations .................................................................................................................... iv Category – II Waterways: Stage – I Feasibility Report Salient -
Russia) 265-280 © Entomofauna Ansfelden/Austria; Download Unter
ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Entomofauna Jahr/Year: 2016 Band/Volume: 0037 Autor(en)/Author(s): Poltawski Alexander N., Ilyina Elena V. Artikel/Article: New records of some rare Noctuoidea and Pyraloidea in Daghestan Republic (Russia) 265-280 © Entomofauna Ansfelden/Austria; download unter www.zobodat.at Entomofauna ZEITSCHRIFT FÜR ENTOMOLOGIE Band 37, Heft 16: 265-280 ISSN 0250-4413 Ansfelden, 4. Januar 2016 New records of some rare Noctuoidea and Pyraloidea in Daghestan Republic (Russia) Alexander N. POLTAVSKY & Elena V. ILYINA Abstract New and rare Lepidoptera species in Daghestan republic in the period 2013–2014 are reported. Among them the first records for Russia: Aglossa asiatica (ERSCHOFF, 1872) and Ecpyrrhorrhoe diffusalis (GUENÉE, 1854) (Pyraloidea), Agrotis lasserrei (OBER THÜR, 1881) and Arcyophora dentula (LEDERER, 1870) (Noctuoidea); the first records for Daghestan: Stiphrometasia monialis (ERSCHOFF, 1872), Achyra nudalis (HÜBNER, 1796), Paratalanta cultralis (STAUDINGER, 1867), Udea austriacalis (HERRICH-SCHÄFFER, 1851), Agrotera nemoralis (SCOPOLI, 1763), Loxostege aeruginalis (HÜBNER, 1796) and Ephelis cruentalis (GEYER, 1832) (Pyraloidea), Photedes morrisii (DALE, 1837) (Noctuoidea). Key words: Noctuoidea, Pyraloidea, republic of Daghestan, North-East Caucasus, Russia, first records. 265 Heft 16- 265-280 Poltavsky-New records of some rare Noctuoidea_Z2.indd 265 23.11.15 20:29 © Entomofauna Ansfelden/Austria; -
June 2019 - March 2020
Geography (PRE-Cure) June 2019 - March 2020 Visit our website www.sleepyclasses.com or our YouTube channel for entire GS Course FREE of cost Also Available: Prelims Crash Course || Prelims Test Series Table of Contents 1. Quadilateral Meet ......................................1 34. National Freight Index: By Rivigo Logistics 2. Organisation Of Islamic Corporation ...1 12 3. New START (Strategic Arms Reduction 35. Kaladan Multimodal Project ...................13 Treaty) ...........................................................1 36. Summer Solstice 2019 .............................13 4. Siachen Glacier ...........................................2 37. Unique Flood Hazard Atlas: Odisha ......13 5. Mount Etna ..................................................2 38. G20 Summit 2019 ....................................13 6. NASA (Insight) Mission .............................3 39. Fortified Rice ...............................................15 7. Air Traffic Management ............................3 40. Space Activities Bill, 2017 .......................15 8. International Renewable Energy Agency 41. Outer Space Treaty ....................................16 (IRENA) .........................................................4 42. Falcon Heavy ...............................................16 9. Pacific Ring Of Fire .....................................4 43. Solar-Powered Sail .....................................17 10. G20 ................................................................5 44. Deep Space Atomic Clock ........................17 11. -
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