Ichthyofaunal Diversity in Bachan Gad and Kakda Streams of the Mid-Himalayan Ganga River System of Garhwal in Relation to Stream Gradient and Distance
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The Alaknanda Basin (Uttarakhand Himalaya): a Study on Enhancing and Diversifying Livelihood Options in an Ecologically Fragile Mountain Terrain”
Enhancing and Diversifying Livelihood Options ICSSR PDF A Final Report On “The Alaknanda Basin (Uttarakhand Himalaya): A Study on Enhancing and Diversifying Livelihood Options in an Ecologically Fragile Mountain Terrain” Under the Scheme of General Fellowship Submitted to Indian Council of Social Science Research Aruna Asaf Ali Marg JNU Institutional Area New Delhi By Vishwambhar Prasad Sati, Ph. D. General Fellow, ICSSR, New Delhi Department of Geography HNB Garhwal University Srinagar Garhwal, Uttarakhand E-mail: [email protected] Vishwambhar Prasad Sati 1 Enhancing and Diversifying Livelihood Options ICSSR PDF ABBREVIATIONS • AEZ- Agri Export Zones • APEDA- Agriculture and Processed food products Development Authority • ARB- Alaknanda River Basin • BDF- Bhararisen Dairy Farm • CDPCUL- Chamoli District Dairy Production Cooperative Union Limited • FAO- Food and Agricultural Organization • FDA- Forest Development Agency • GBPIHED- Govind Ballabh Pant Institute of Himalayan Environment and Development • H and MP- Herbs and Medicinal Plants • HAPPRC- High Altitude Plant Physiology Center • HDR- Human Development Report • HDRI- Herbal Research and Development Institute • HMS- Himalayan Mountain System • ICAR- Indian Council of Agricultural Research • ICIMOD- International Center of Integrated Mountain and Development • ICSSR- Indian Council of Social Science Research LSI- Livelihood Sustainability Index • IDD- Iodine Deficiency Disorder • IMDP- Intensive Mini Dairy Project • JMS- Journal of Mountain Science • MPCA- Medicinal Plant -
How Do They Add to the Disaster Potential in Uttarakhand?
South Asia Network on Dams, Rivers and People Uttarakhand: Existing, under construction and proposed Hydropower Projects: How do they add to the disaster potential in Uttarakhand? As Uttarakhand faced unprecedented flood disaster and as the issue of contribution of hydropower projects in this disaster was debated, one question for which there was no clear answer is, how many hydropower projects are there in various river basins of Uttarakhand? How many of them are operating hydropower projects, how many are under construction and how many more are planned? How projects are large (over 25 MW installed capacity), small (1-25 MW) and mini-mirco (less than 1 MW installed capacity) in various basins at various stages. This document tries to give a picture of the status of various hydropower projects in various sub basins in Uttarakhand, giving a break up of projects at various stages. River Basins in Uttarakhand Entire Uttarakhand is Uttarakhand has 98 operating hydropower part of larger Ganga basin. The Ganga River is a projects (all sizes) with combined capacity trans-boundary river of India and Bangladesh. The close to 3600 MW. However, out of this 2,525 km long river rises in the western Himalayas capacity, about 1800 MW is in central sector in the Indian state of Uttarakhand, and flows south and 503 MW in private sector, making it and east through the Gangetic Plain of North India into Bangladesh, where it empties into the Bay of uncertain how much power from these Bengal. The Ganga begins at the confluence of the projects the state will get. -
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 -
Adaptive Modification of Lip and Its Associated Structures of Hill- Stream Fish Schizothorax Richardsonii (Cypriniformes: Cyprinidae)
IOSR Journal of Pharmacy and Biological Sciences (IOSR-JPBS) e-ISSN: 2278-3008. Volume 5, Issue 4 (Mar. – Apr. 2013), PP 59-65 www.iosrjournals.org Adaptive modification of lip and its associated structures of Hill- stream fish Schizothorax richardsonii (Cypriniformes: Cyprinidae). Hoshiyar Singh1, S.C. Joshi2, Ila Bisht1 and S.K. Agarwal1 1. Department of Zoology, S.S.J. Campus Almora, Kumaun University Nainital, 263601, India. 2. Department of Zoology, Surajmal Agarwal Girls, P.G. College Kichha, K.U. Nainital, 263145. Abstract: The lips and associated structures, in different groups of fishes, are greatly modified in relation to the characteristic mode of feeding, food preference and the mode of life exhibited by the fish. The successful maintenance of fish populations in challenging environments requires responsive adjustments in their behaviour, morphology and physiology and these have been reflected by modifications at the level of their organ systems, organs and tissues. The lips are no exception to this. The importance of food in daily life of a fish is obvious and is reflected in the form of the mouth, lips, jaw and so on. These structures present more diverse modifications than any other organ of the body. The functional aspects of the lips and associated structures in family Gobiidae, Cobitidae, Belontiidae and few species of Cyprinidae show considerable variation and exhibit unique morphological modifications associated with their lips and other structures around the mouth regarding information on the level of surface architecture as seen under SEM in relation to various food and feeding habits and ecological niches. Key words: Cyprinidae, fishes, lip and morphology. -
Kedarnath Flash Floods: a Hydrological and Hydraulic Simulation Study
RESEARCH COMMUNICATIONS Kedarnath flash floods: a hydrological nami3,4. Experts say that it is another alarm regarding the impact of rapid climate change on the environment3,5. and hydraulic simulation study Unprecedented destruction by the rainfall witnessed in Uttarakhand was attributed to a unique meteorological K. H. V. Durga Rao*, V. Venkateshwar Rao, event by environmentalists due to unscientific develop- V. K. Dadhwal and P. G. Diwakar mental activities undertaken in recent decades contribut- National Remote Sensing Centre, Indian Space Research Organisation, ing to loss of lives and property. The satellite imageries Balanagar, Hyderabad 500 037, India show that massive landslides occurred in the upstream northeast region of the Kedarnath valley due to high- The recent floods in the Kedarnath area, Uttarakhand intensity rainfall6. In the present work, hydrological and are a classic example of flash floods in the Mandakini hydraulic simulation study was carried out on the Man- River that devastated the country by killing thousands dakini River to understand the events which took place in of people besides livestock. Though the duration of the the Kedarnath valley during 10–18 June 2013. The disas- event was small compared to other flood disasters in the country, it resulted in severe damage to property ter was due to an integrated effect of heavy rainfall inten- and life. Post-disaster satellite images depict that the sity, sudden outburst of a lake (Chorabari), and very steep river banks were eroded completely along the Kedar- topographic conditions. The complete scenario was simu- nath valley due to the flash floods and few new chan- lated in the Geographic Information System (GIS) envi- nels were visible. -
SCIENCE CHINA Phylogenetic Relationships and Estimation Of
SCIENCE CHINA Life Sciences • RESEARCH PAPER • April 2012 Vol.55 No.4: 312–320 doi: 10.1007/s11427-012-4305-z Phylogenetic relationships and estimation of divergence times among Sisoridae catfishes YU MeiLing1,2* & HE ShunPing1* 1Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 400732, China; 2Graduate University of Chinese Academy of Sciences, Beijing 100049, China Received December 10, 2011; accepted March 9, 2012 Nineteen taxa representing 10 genera of Sisoridae were subjected to phylogenetic analyses of sequence data for the nuclear genes Plagl2 and ADNP and the mitochondrial gene cytochrome b. The three data sets were analyzed separately and combined into a single data set to reconstruct phylogenetic relationships among Chinese sisorids. Both Chinese Sisoridae as a whole and the glyptosternoid taxa formed monophyletic groups. The genus Pseudecheneis is likely to be the earliest diverging extant ge- nus among the Chinese Sisoridae. The four Pareuchiloglanis species included in the study formed a monophyletic group. Glaridoglanis was indicated to be earliest diverging glyptosternoid, followed by Glyptosternon maculatum and Exostoma labi- atum. Our data supported the conclusion that Oreoglanis and Pseudexostoma both formed a monophyletic group. On the basis of the fossil record and the results of a molecular dating analysis, we estimated that the Sisoridae diverged in the late Miocene about 12.2 Mya. The glyptosternoid clade was indicated to have diverged, also in the late Miocene, about 10.7 Mya, and the more specialized glyptosternoid genera, such as Pareuchiloglanis, originated in the Pleistocene (within 1.9 Mya). The specia- tion of glyptosternoid fishes is hypothesized to be closely related with the uplift of the Qinghai-Tibet Plateau. -
6. Mandakini River Retaining Wall
6. MANDAKINI RIVER RETAINING WALL KEDARNATH REDEVELOPMENT/RESTORATION PROJECT DRAFT MEMORANDUM OF INFORMATION PACKAGE AN INITIATIVE BY JSW, PREPARED FOR CSR CAUSE & FUNDING OF THE PROJECT Prepared for Prepared by 12th January, 2018 KEDAR VALLEY PROJECTS: 1. Maun Gufa / Meditation Caves along the Tirth yatra route (5 nos.) 2. Smriti-van Memorial at foothills 3. Road widening and Construction of Rambara to Garudchatti (5.25km Long - 1.9km Existing , 3.9km New) 4. Road widening and Construction of GarudChatti to Kedartown (3.6 km) 5. Saraswati Ghats & Retaining wall (JSW funded Project ) 6. Mandakini Ghats & Retaining Wall (Government Funded Project) 7. Kedarpuri Central Approach Street widening & Grading (ONGC Funded Project) 8. Shri Shankaracharya Samadhi/Virtual Museum (JSW funded Project) 9. Guest Houses (8 nos.) on Saraswati & Mandakini River-banks 10. Kedarpuri Infrastructure Project : Storm Water, Solid Waste Management, Water Supply, Electrification, Lane Cabling & other Sustainable Solutions. 11. Balance 70 Houses for Tirth Purohits in Kedarpuri 12. Laser/Light and Sound show on mountain slopes Background BARKOT KEDARNATH KEDARNATH 54 km RAMBARA KEDARNATH State: Uttarakhand GAURIKUND District: Rudraprayag PHATA 14 km 27 km UKHIMATH Tehsil: Ukhimath 41 km Location: 217 km from Rishikesh, 14 km from Gaurikund 30 km GAURIKUND 78 km 46 km RUDRAPRAYAG River: Mandakini 15 km 34 km Glacier: Chorabari 31km KARNAPRAYAG SRINAGAR PHATA Height: 3583m/ 11755ft from sea level RISHIKESH 19 km 105 km 27 km 24 km Mountain: Kedar Dome (6831m/22411ft -
Global Catfish Biodiversity 17
American Fisheries Society Symposium 77:15–37, 2011 © 2011 by the American Fisheries Society Global Catfi sh Biodiversity JONATHAN W. ARMBRUSTER* Department of Biological Sciences, Auburn University 331 Funchess, Auburn University, Alabama 36849, USA Abstract.—Catfi shes are a broadly distributed order of freshwater fi shes with 3,407 cur- rently valid species. In this paper, I review the different clades of catfi shes, all catfi sh fami- lies, and provide information on some of the more interesting aspects of catfi sh biology that express the great diversity that is present in the order. I also discuss the results of the widely successful All Catfi sh Species Inventory Project. Introduction proximately 10.8% of all fi shes and 5.5% of all ver- tebrates are catfi shes. Renowned herpetologist and ecologist Archie Carr’s But would every one be able to identify the 1941 parody of dichotomous keys, A Subjective Key loricariid catfi sh Pseudancistrus pectegenitor as a to the Fishes of Alachua County, Florida, begins catfi sh (Figure 2A)? It does not have scales, but it with “Any damn fool knows a catfi sh.” Carr is right does have bony plates. It is very fl at, and its mouth but only in part. Catfi shes (the Siluriformes) occur has long jaws but could not be called large. There is on every continent (even fossils are known from a barbel, but you might not recognize it as one as it Antarctica; Figure 1); and the order is extremely is just a small extension of the lip. There are spines well supported by numerous complex synapomor- at the front of the dorsal and pectoral fi ns, but they phies (shared, derived characteristics; Fink and are not sharp like in the typical catfi sh. -
Modeling the Efficacy of the Ganga Action Plan's Restoration of The
Modeling the Efficacy of the Ganga Action Plan’s Restoration of the Ganga River, India By Shaw Lacy A thesis submitted In partial fulfillment of the requirements For the degree of Master of Science Natural Resources and Environment at The University of Michigan August 2006 Thesis Committee: Professor Michael Wiley Professor Jonathan Bulkley Abstract. To combat rising levels of water pollution in the Ganges River, the Indian gov- ernment initiated the Ganga Action Plan (GAP) in 1984. After twenty years, it is a com- mon perception that the GAP has failed to achieve the goals of a cleaner river. Using available government data on pollution levels and hydrology, I undertook an of the GAP efficacy for fifteen pollution parameters across 52 water quality sampling points moni- tored by India’s Central Pollution Control Board (CPCB) within the Ganga Basin. Dis- solved oxygen, BOD, and COD showed a significant improvement of water quality after twenty years. In addition, fecal and total coliform levels, as well as concentrations of cal- cium, magnesium, and TDS all showed a significant decline. Building on this analysis, a GIS analysis was used to create a spatial model of the majority of the Ganga River net- work using a reach-based ecological classification approach. Using recent GAP monitor- ing data, a multiple linear regression model of expected pollutant loads within each reach (VSEC unit) was created. This model was then used to inventory water quality across the entire basin, based on CPCB criteria. My analysis showed 208 river km were class A, 1,142 river km were class B, 684 river km were class C, 1,614 river km were class D, and 10,403 river km were class E. -
Archeological and Historical Database on Earthquakes
Archeological and Historical Database on earthquakes. We are not aware of any studies on the seismic the Medieval Earthquakes of the Central performance of the temples in the Garhwal Himalaya, but Himalaya: Ambiguities and Inferences models of the performance of similar multistoried structures in Nepal show a fundamental time period less than 0.6 s (Jaishi by C. P. Rajendran, Kusala Rajendran, Jaishri et al., 2003). Because this is within the range of natural period of a wide variety of soils, there is a high probability for such Sanwal, and Mike Sandiford structures to approach a state of partial resonance during large earthquakes. The spatial distribution of damage, response of specific structures, and models based on their structural elements INTRODUCTION could lead to the location and magnitude of pre-twentieth cen- tury earthquakes. The architectural style showed only minor variations be- Global Positioning System-based convergence rate between In- 20 3mm=yr tween different clans and their rulers, and the constructions dia and southern Tibet is estimated as (Larson generally consist of a common plan, which used large and heavy et al., 1999). Despite this fast convergence, the seismicity rate ∼50% rock units arranged on top of each other, without mortar of the Himalaya has been remarkably low, as only of (Fig. 2). As a society whose social milieu revolved around this plate boundary has ruptured during the last 200 years. the temples for ages (>1000 years), the temple archives carried This long-lived deficit in seismic productivity has led many through generations serve as an important and often the only to believe that the region holds potential for more than one magnitude ≥8:0 source of information on its history including the impact of earthquake (Ambraseys and Jackson, 2003). -
Environmental Assessment & Management Plan
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized E1050 v3 rev m Theun 2 Hydroelectric Project Na & Management Plan Environmental Assessment March 2005 annexes List of Annexes List of Annexes Annex A: References ........................................................................................A1-6 Annex B: Contributors to the EAMP ....................................................................B1-2 Annex C: Project Key Technical Data ..................................................................C1-4 Annex D: Technical Drawings of Project Infrastructure ......................................D1-18 Annex E: Hydrological Data ............................................................................. E1-10 Annex F: Simulated Dam Operations ................................................................ F1-10 Annex G: Water Quality Modelling Assumptions and Results ................................G1-4 Annex H: Forest & Vegetation Types ..................................................................H1-4 Annex I: Mammal & Bird Species of the NNT Area .............................................I1-20 Annex J: Fish Species & Migration ..................................................................... J1-8 Annex K: Head Construction Contractor’s Environmental Requirements .............. K1-18 Annex L: Pest Management Plan ..................................................................... L1-18 Annex M: Public Consultation and Disclosure Events ......................................... -
Proceedings of National Workshop on "Uttarakhand Disaster 2013
National Workshop on UTTARAKHAND DISASTER 2013: LESSONS LEARNT Monday, August 19, 2013 PROCEEDINGS Organized by National Institute of Disaster Management (Ministry of Home Affairs, Government of India) 5B, I.P. Estate, Mahatma Gandhi Marg , New Delhi‐110002 www.nidm.gov.in Proceedings of the National Workshop on Uttarakhand Disaster 2013: Lessons Learnt BACKGROUND Uttarakhand, one of the hill states of Northern India, was severely hit by heavy rain induced flash floods and landslides in the 3rd week of June, 2013. This abnormally high amount of rainfall has been attributed to the fusion of Westerlies with the Indian monsoonal cloud system (Fig. 3). This has resulted into huge loss to lives and properties and specially disrupting the peak seasonal activities to Char Dham Pilgrimmage. The melting of Chorabari Glacier and eruption of the Mandakini River has led to floods near Kedarnath Shrine area, Rambara, Agostyamuni, Tilwara, Guptkashi in Rudraprayag district. There were torrential rainfall in Himachal Pradesh and Western Nepal, and in other nearby regions of Delhi, Haryana, Uttar Pradesh and some parts of Tibet. Pilgrimage centres in the region, including Gangotri, Yamunotri, Kedarnath and Badrinath, are visited by thousands of devotees, especially during May to September. Over a lakh people were stuck in various regions because of damaged roads, landslides and flash flood induced debris. People in other important locations such as the Valley of Flowers, Roopkund and the Sikh Pilgrimage Centre Hemkund were stranded for days together. Fig. 1 &2: The Kedarnath Shrine in Rudraprayag District, before and after June 2013 Flash flood 2 Proceedings of the National Workshop on Uttarakhand Disaster 2013: Lessons Learnt The scale and magnitude of the extreme event was such that more than 580 persons are confirmed to have lost their lives.