Krishna Wildlife Sanctuary  Sri Lankamalleswara Wildlife Sanctuary  Pulicat Lake Bird Sanctuary  Koundinya Wildlife Sanctuary

Total Page:16

File Type:pdf, Size:1020Kb

Krishna Wildlife Sanctuary  Sri Lankamalleswara Wildlife Sanctuary  Pulicat Lake Bird Sanctuary  Koundinya Wildlife Sanctuary KNOW YOUR STATE ANDHRA PRADESH WHEN AND HOW WAS IT FORMED? • It was formed on 1st NOV 1956. • It was the first state in India to be made on linguistic basis. GEOGRAPHY Size – 160 X 205 Sq. Km. Capital – Amravati Official Language - Telugu 7th largest state 13 Administrative districts. Other important cities – Vijayawada Chittoor Visakhapatnam It has the second largest coastline (974KM) after Gujrat. It is 10th largest state of India in terms of population (4.97 Crore). STATE SYMBOLS State Animal – Black Buck State Bird – Rose ringed State Tree - Neem State Flower - Jasmine Parakeet The state physiography of Andhra Pradesh is : Coastal Regions, Plateau, Plains. Major Rivers in Andhra Pradesh are Godavari, Krishna and Penna. Amravati is situated on the banks of Krishna River. Major Dams in Andhra Pradesh Nagarjun Sagar Dam – Krishna River Srisailam Dam – Krishna River Tatipudi Dam – Gosthani River Dowleswaram Barrage – Godavari River National Parks and Wild Life Sanctuaries: Sri Venkateswara National Park Nagarjunasagar Srisailam Papikonda Wildlife Sanctuary Coringa Wildlife Sanctuary Kolleru Bird Sanctuary Krishna Wildlife Sanctuary Sri Lankamalleswara Wildlife Sanctuary Pulicat Lake Bird Sanctuary Koundinya Wildlife Sanctuary IMPORTANT GI TAGS Kondapalli Bommallu Srikalahasti Kalamkari Budiiti Bell and Brass Craft Machilipatnam Kalamkari IMPORTANT HISTORICAL SITES Bugga Ramalingeswara Swamy Sri Venkateswara Swamy Temple Golconda Fort Kanipakam temple Major Minerals Found Natural Gas Manganese Iron ore Gold Diamond Graphite More than India’s 33% of Limestone reserve. FAMOUS FESTIVALS Tirupati Brahmotsavam Ugadi Rama Navami Maha Sivarathri MAJOR DANCE FORMS Lambadi Dance Kuchipudi Dance Burra Katha Dance Veeranatyam NUMBER OF SEATS Number of Seats in Legislative assembly – 175 Number of Seats in Legislative council - 58 Seats in Rajya Sabha – 11 Seats in Lok Sabha - 25 IMPORTANT POLITICAL PERSONLATIES GOVERNOR Chief Minister Biswabhusan Harichandan YS Jagan Mohan Reddy YSR Congress Party .
Recommended publications
  • Major Points About Andhra Pradesh - Know Your State in PDF for SSC, Bank Exams
    Major Points about Andhra Pradesh - Know Your State in PDF for SSC, Bank exams If you look at the question papers of exams like SSC CHSL, SSC CGL, SSC MTS, IBPS PO, IBPS Clerk, IBPS SO, IPPB Sc. I, LIC AAO, etc. you will find a lot of questions related to India and its states. Questions based on various states of India form a large part of the General Awareness section of many government and bank exams. In fact, if are thinking of appearing for state govt. exams, it becomes all the more important for you to know your state. Our latest GK Notes series - 'Know All your States', will help you learn major facts, global importance and culture of every state. This particular article will help you learn everything about Andhra Pradesh in one glance. Read the complete article to find out the history, economy, geographical significance, flora & fauna, important sites, tourist attractions, etc. about Andhra Pradesh. You can also download this article as PDF to keep it handy. Important Points about Andhra Pradesh in PDF Situated at the south-eastern coast of India, Andhra Pradesh is a state rich in culture, heritage and potential. Here's more for you to read about Andhra Pradesh: Andhra Pradesh - Hyderabad Capital & - Visakhapatnam, Tirupati, Vijayawada, Imp Cities Nellore, Chittoor, Anantapur, Secunderabad 1 | P a g e - Carved out of Madras state on 1st October Date of 1953 Formation - Reorganized (Telangana excluded) on 2nd June 2014 Districts 13 - Telugu (Official language) Language - Urdu - Egg bowl of Asia Known as/for - Kohinoor of India - State with 2nd longest coastline (972 km) - Consists of coastal regions, plateau, and plains.
    [Show full text]
  • Sedimentological Characterization of Nagavali-Vamsadhra Estuarine System, East Coast of India, Andhra Pradesh
    Studia Rosenthaliana (Journal for the Study of Research) ISSN NO: 1781-7838 Sedimentological Characterization of Nagavali-Vamsadhra Estuarine System, East Coast of India, Andhra Pradesh Gara Raja Rao1, Yamala Vinay Kumar2, Vaggela Asha3, Sanapala Harikrishna3, Mokka Jagannadha Rao4 1 Assistant Professor, Department of Geology, Andhra University, Visakhapatnam. 2,3 Research Scholar, Department of Geology, Andhra University, Visakhapatnam. 4 Professor, Department of Geology, Andhra University, Visakhapatnam. Abstract: The importance of textural characteristics of estuarine sediments in the present study is useful in understanding the intensity of sediment transportation in the fluvial systems. The importance of grain size parameters of the sediments is well recognized in sedimentology and has been well established. The present study illustrates the detailed textural characterization of Nagavali and Vamsadhara estuarine sediments of East Coast of India, Srikakulam, Tamil Nadu. The textural studies reflect that the sediments have significant fractions of fine to medium sand, silt and clay, where fine sand is predominant in both the estuaries. The statistical sedimentary analysis for the samples say mean size, standard deviation, skewness and kurtosis is carried out. The sediment is dominantly fine sand with moderately sorted, nearly skewed in Nagavali estuary whereas the sand is very well sorted and nearly symmetrical in Vamsadhara estuarine sediments. The sediments of both are similar in size and show low variance. The present study suggests that the sediments were deposited in low energy conditions. The Nagavali estuary samples shows nearly symmetrical skewness and the Vamsadhara estuary samples shows nearly symmetrical to positive skewness. Negative Skewness was being correlated with high energy and winnowing action and positive Skewness with lower energy levels.
    [Show full text]
  • Problems of Salination of Land in Coastal Areas of India and Suitable Protection Measures
    Government of India Ministry of Water Resources, River Development & Ganga Rejuvenation A report on Problems of Salination of Land in Coastal Areas of India and Suitable Protection Measures Hydrological Studies Organization Central Water Commission New Delhi July, 2017 'qffif ~ "1~~ cg'il'( ~ \jf"(>f 3mft1T Narendra Kumar \jf"(>f -«mur~' ;:rcft fctq;m 3tR 1'j1n WefOT q?II cl<l 3re2iM q;a:m ~0 315 ('G),~ '1cA ~ ~ tf~q, 1{ffit tf'(Chl '( 3TR. cfi. ~. ~ ~-110066 Chairman Government of India Central Water Commission & Ex-Officio Secretary to the Govt. of India Ministry of Water Resources, River Development and Ganga Rejuvenation Room No. 315 (S), Sewa Bhawan R. K. Puram, New Delhi-110066 FOREWORD Salinity is a significant challenge and poses risks to sustainable development of Coastal regions of India. If left unmanaged, salinity has serious implications for water quality, biodiversity, agricultural productivity, supply of water for critical human needs and industry and the longevity of infrastructure. The Coastal Salinity has become a persistent problem due to ingress of the sea water inland. This is the most significant environmental and economical challenge and needs immediate attention. The coastal areas are more susceptible as these are pockets of development in the country. Most of the trade happens in the coastal areas which lead to extensive migration in the coastal areas. This led to the depletion of the coastal fresh water resources. Digging more and more deeper wells has led to the ingress of sea water into the fresh water aquifers turning them saline. The rainfall patterns, water resources, geology/hydro-geology vary from region to region along the coastal belt.
    [Show full text]
  • GRMB Annual Report 2017-18
    Government of India Ministry of Water Resources, RD & GR Godavari River Management Board ANNUAL REPORT 2017-18 GODAVARI BASIN – Dakshina Ganga Origin Brahmagiri near Trimbakeshwar, Nasik Dist., Maharashtra Geographical Area 9.50 % of Total GA of India Area & Location Latitude - 16°19’ to 22°34’ North Longitude – 73°24’ to 83° 4’ East Boundaries West: Western Ghats North: Satmala hills, the Ajanta range and the Mahadeo hills East: Eastern Ghats & the Bay of Bengal South: Balaghat & Mahadeo ranges stretching forth from eastern flank of the Western Ghats & the Anantgiri and other ranges of the hills and ridges separate the Gadavari basin from the Krishna basin. Catchment Area 3,12,812 Sq.km Length of the River 1465 km States Maharashtra (48.6%), Telangana (18.8%), Andhra Pradesh (4.5%), Chhattisgarh (10.9%), Madhya Pradesh (10.0%), Odisha (5.7%), Karnataka (1.4%) and Puducherry (Yanam) and emptying into Bay of Bengal Length in AP & TS 772 km Major Tributaries Pravara, Manjira, Manair – Right side of River Purna, Pranhita, Indravati, Sabari – Left side of River Sub- basins Twelve (G1- G12) Dams Gangapur Dam, Jayakwadi dam, Vishnupuri barrage, Ghatghar Dam, Upper Vaitarna reservoir, Sriram Sagar Dam, Dowleswaram Barrage. Hydro power stations Upper Indravati 600 MW Machkund 120 MW Balimela 510 MW Upper Sileru 240 MW Lower Sileru 460 MW Upper Kolab 320 MW Pench 160 MW Ghatghar pumped storage 250 MW Polavaram (under 960 MW construction) ANNUAL REPORT 2017-18 GODAVARI RIVER MANAGEMENT BOARD 5th Floor, Jalasoudha, Errum Manzil, Hyderabad- 500082 FROM CHAIRMAN’S DESK It gives me immense pleasure to present the Annual Report of Godavari River Management Board (GRMB) for the year 2017-18.
    [Show full text]
  • MAP:East Godavari(Andhra Pradesh)
    81°0'0"E 81°10'0"E 81°20'0"E 81°30'0"E 81°40'0"E 81°50'0"E 82°0'0"E 82°10'0"E 82°20'0"E 82°30'0"E EAST GODAVARI DISTRICT GEOGRAPHICAL AREA (ANDHRA PRADESH) 47 MALKANGIRI SH Towards Sileru 18°0'0"N 18°0'0"N IR (EXCLUDING: AREA ALREADY AUTHORISED) ERVO I RES AY AR NK DO MALKANGIRI V IS H KEY MAP A K H A P A T N A M M Towards Polluru CA-02 A CA-01 M M ± A CA-07 H CA-35 CA-34 K V CA-60 I CA-03 CA-57 CA-58 S CA-33 CA-59 H CA-04 CA-57 CA-37 CA-36 AKH 17°50'0"N CA-32 CA-56 17°50'0"N CA-31 CA-55 CA-05 CA-38 CA-55 CA-39 AP CA-06 CA-30 CA-53 CA-54 CA-40 CA-39 A CA-07 CA-29 CA-41 CA-51 T CA-08 CA-41 T NAM CA-07 CA-28 CA-51 oward CA-42 CA-52 CA-27 CA-51 CA-09 CA-26 CA-44 CA-44 CA-25 s Tu T CA-10 CA-11 CA-43 CA-45 CA-46 o L lasipaka w W CA-24 A ar E CA-12 CA-23 S NG T CA-13 E d G CA-47 CA-22 B s O CA-48 D CA-21 F K A CA-14 CA-50 O V CA-20 o A R CA-49 Y.
    [Show full text]
  • The Pulicat Lake, Adjoining the Bay of Bengal Is a Shallow Water Body, Bordering the East Coast of India and Located 40 Km North of Chennai
    ENVIRONMENTAL GEOCHEMISTRY OF THE PULICAT LAKE, SOUTH INDIA PURANIK GAYATRI RANGANATH JUNE-2000 ABSTRACT The Pulicat lake, adjoining the Bay of Bengal is a shallow water body, bordering the east coast of India and located 40 km north of Chennai. The lake is one of the largest salt-water lake in India that supports a wide range of socioeconomic and cultural activities. The primary aim of this study is to understand the biogeochemical processes of the Pulicat lake ecosystem in order to preserve the ecological and environmental characteristics of this fragile ecosystem. Seasonal samples of water, bed, suspended and core sediments were collected over a one-year period in three zones (southern-channel, central and northern regions) of the Pulicat lake. The lake receives fresh water discharge only during monsoon, from two seasonal rivers, the Arani discharging into the southern region of the lake (zone I) and the Kalangi discharging into the northwestern region of the lake (zone III). The Buckingham canal, running parallel to the coastline discharges sewage contaminated water and industrial effluents into the Pulicat lake. Due to the limited freshwater supply and tidal action, the mouth of the lake gets silted up and closed during the dry season. Understanding the spatial and seasonal variations in the water chemistry was one of the primary aspects of this study. The chemical composition of the surface water indicates a strong influence by seawater during the summer and diluted by river water during the monsoon season. The results obtained indicate that the dominant cations and anions of the surface water are in the order of Cl>Na>S04>K>Mg>HC03>Ca.
    [Show full text]
  • International Journal of Academic Research ISSN: 2348-7666; Vol.3, Issue-4(2), April, 2016 Impact Factor: 3.075; Email: [email protected]
    International Journal of Academic Research ISSN: 2348-7666; Vol.3, Issue-4(2), April, 2016 Impact Factor: 3.075; Email: [email protected] , Assistant Professor, Dept. of Civil Engineering, Sri. Indu College of Engineering and Technology, Seriguda , Ibrahim patnam (M) R.R District. Telangana State. , Lecturer in Dept. of Economics, Govt. (UG &PG) College, Anantapur, Andhra Pradesh , Post-Doctoral Fellow , Dept. of Economics , S.K. University , S.V. Puram , Anantapur , District, Andhra Pradesh. Floods are the most devastating natural calamities by their nature since time immemorial. Flooding is mainly caused by over spilling of river banks Severity increases where there is obstruction like encroachment in water ways in urban areas etc. The present paper analysed flood management. The main objectives are (i) To describe the river system, Rainfall, forecasting system and affected areas, (ii) To identify the causes vulnerability, impacts, losses, strategies, controlling measures of floods affected areas. The paper discuss the river basin wise flood situations rainfall , forecasting systems sites cause , losses, risk reduction measures strategies and flood management of the study area. flood management, calamities, forecasting, river basin catchment, vulnerability, strategies. Flood waters are simply going as a waste Floods are one of the most devastating in to seas and oceans. To control the natural calamities, by their nature and floods and utilize the waters for irrigation since time immemorial. It is most and other purposes, Interlinking of rivers commonly observed during monsoon can be a substantial solution. A variety of season and severe floods occurring every mitigation measures can be identified and year in one part or the throughout the implemented measures include flood country which has been causing forecasting and warning, adopting proper recurrent tremendous extensive damage land-use planning, flood-prone area to Agriculture, life and property besides zoning, and management.
    [Show full text]
  • Urban and Landscape Design Strategies for Flood Resilience In
    QATAR UNIVERSITY COLLEGE OF ENGINEERING URBAN AND LANDSCAPE DESIGN STRATEGIES FOR FLOOD RESILIENCE IN CHENNAI CITY BY ALIFA MUNEERUDEEN A Thesis Submitted to the Faculty of the College of Engineering in Partial Fulfillment of the Requirements for the Degree of Masters of Science in Urban Planning and Design June 2017 © 2017 Alifa Muneerudeen. All Rights Reserved. COMMITTEE PAGE The members of the Committee approve the Thesis of Alifa Muneerudeen defended on 24/05/2017. Dr. Anna Grichting Solder Thesis Supervisor Qatar University Kwi-Gon Kim Examining Committee Member Seoul National University Dr. M. Salim Ferwati Examining Committee Member Qatar University Mohamed Arselene Ayari Examining Committee Member Qatar University Approved: Khalifa Al-Khalifa, Dean, College of Engineering ii ABSTRACT Muneerudeen, Alifa, Masters: June, 2017, Masters of Science in Urban Planning & Design Title: Urban and Landscape Design Strategies for Flood Resilience in Chennai City Supervisor of Thesis: Dr. Anna Grichting Solder. Chennai, the capital city of Tamil Nadu is located in the South East of India and lies at a mere 6.7m above mean sea level. Chennai is in a vulnerable location due to storm surges as well as tropical cyclones that bring about heavy rains and yearly floods. The 2004 Tsunami greatly affected the coast, and rapid urbanization, accompanied by the reduction in the natural drain capacity of the ground caused by encroachments on marshes, wetlands and other ecologically sensitive and permeable areas has contributed to repeat flood events in the city. Channelized rivers and canals contaminated through the presence of informal settlements and garbage has exasperated the situation. Natural and man-made water infrastructures that include, monsoon water harvesting and storage systems such as the Temple tanks and reservoirs have been polluted, and have fallen into disuse.
    [Show full text]
  • Silting and Ancient Sea-Ports of the Tamil Country
    Indian Journal of History of Science, 47.2 (2012) 261-269 SILTING AND ANCIENT SEA-PORTS OF THE TAMIL COUNTRY JEAN DELOCHE* (Received 19 September 2008) The progressive and irreversible process of sedimentation on the Tamil coast has brought about the decline of the ancient sea ports which could not escape ruin when lagoons and river mouths were filled up. Conditions were much favourable for earlier navigation, since lagoons and deltaic tributaries were better suited for maritime settlements, with sufficient water depth and safe shelter. Owing to the sand bars thrown by the action of the waves across their openings into the Bay of Bengal, their access, as found in ancient documents, must have always been difficult, but the coastal sailing vessels could put up with it. Their history can be reconstructed by geologists who study fossil pollen grains preserved in sediments in the coastal area. The result of these investigations can thus be used by historians to know, with a relative precision, the water depth of a lagoon at a given period and thus trace the stages of maritime activities in the settlements situated at their outlets. Key words: Coastal barrier, Geomorphological, Navigation, Neolithic, Palynology, Sedimentation INTRODUCTION In a research article (Deloche 1983, pp. 439-448), it had been shown that it is very difficult to provide a complete account of the ancient sea-ports of India. The factors responsible for the evolution of the littoral forms, or the varied causes explaining the shifting of the shores, the encroaching of the sea on land, or its receding are but little known.
    [Show full text]
  • Performance of Sweet Pepper Under Protective Structure
    INTERNATIONAL JOURNAL OF ENVIRONMENT Volume-3, Issue-2, Mar-May 2014 ISSN 2091-2854 Received:13 April Revised:1 May Accepted:16 May ENVIRONMENTAL CONDITIONS OF BORRA CAVE, VISAKHAPATTANAM, INDIA Haraprasad Bairagya Department of Geography, Visva-Bharati University, Santiniketan, West Bengal, India, 731235 Email: hbairagya7@ gmail.com Abstract Caving is an art which can be best experienced in the mystic Borra of Eastern Ghats and ranked as the second largest cave of India just after Belum Caves situated in the same state Andhrapradesh, India. This Cave is fast becoming a hot tourist‟s destination offering great adventurous opportunity to the tourists in the Eastern Ghats. The cave is located in the Ananthagiri hills of the Eastern Ghats region near Visakhapattanam and is made of limestone. The emotion of thrill heightens after entering the cave. The entrance has a narrow vertical opening and is well lit. Due to its location in the sub-equatorial region, dripping of water from the cave roofs occurs almost throughout the year. The formation of stalactites and stalagmites create wonderful phenomena specially found in this cave. The conspicuous pillars formed due to the joining of the roof and the floors are an awe-inspiring creativity of the creator of this world. Various viruses and bacteria are in the cave interior along with different other creatures. The Borra cave helps the Govt. of Andhra Pradesh, India, to earn huge economic benefits for the sake of tourism industry. Keywords: Cave, stalactite, stalagmite, virus, bacteria Introduction Caves have always hunted the imagination of mankind already from the start of human history; these natural formations provided shelter to early man and were sought after earnestly, to provide a „safe home‟.
    [Show full text]
  • District Survey Report - 2018
    District Survey Report - 2018 4 DEPARTMENT OF MINES AND GEOLOGY Government of Andhra Pradesh DISTRICT SURVEY REPORT - KRISHNA DISTRICT Prepared by ANDHRA PRADESH SPACE APPLICATIONS CENTRE (APSAC) ITE & C Department, Govt. of Andhra Pradesh 2018 i District Survey Report - 2018 ACKNOWLEDGEMENTS APSAC wishes to place on record its sincere thanks to Sri. B.Sreedhar IAS, Secretary to Government (Mines) and the Director, Department of Mines and Geology, Govt. of Andhra Pradesh for entrusting the work for preparation of District Survey Reports of Andhra Pradesh. The team gratefully acknowledge the help of the Commissioner, Horticulture Department, Govt. of Andhra Pradesh and the Director, Directorate of Economics and Statistics, Planning Department, Govt. of Andhra Pradesh for providing valuable statistical data and literature. The project team is also thankful to all the Joint Directors, Deputy Directors, Assistant Directors and the staff of Mines and Geology Department for their overall support and guidance during the execution of this work. Also sincere thanks are due to the scientific staff of APSAC who has generated all the thematic maps. VICE CHAIRMAN APSAC ii District Survey Report - 2018 Contents Page Acknowledgements List of Figures List of Tables 1 Salient Features of Krishna District 1 1.1 Administrative Setup 1 1.2 Drainage 2 1.2a Kolleru Lake- A eco-sensitive zone 4 1.3 Climate and Rainfall 4 1.4 Transport and Communications 9 1.5 Population and Literacy 10 1.6 Important Places 11 1.6a Places of Tourist Interest 11 1.6b Places of
    [Show full text]
  • Are You Suprised ?
    Chapter 2 Physical features 2.1 Geographical Disposition The Pennar (Somasila) – Palar - Cauvery (Grand Anicut) link canal off takes from the existing Somasila reservoir located across the Pennar River near Somasila village in Nellore district of Andhra Pradesh state. The link canal is proposed to pass through the Kaluvaya, Rapur, Dakkili, Venkatagiri mandals of Nellore district; Srikalahasti, Thottambedu, Pitchattur and Nagari mandals of Chittoor district of Andhra Pradesh state, Tiruttani taluk of Tiruvallur district; Arakonam taluk of Vellore district; Cheyyar and Vandavasi taluks of Tiruvannamalai district; Kancheepuram, Uthiramerur taluks of Kancheepuram district; Tindivanam, Gingee, Villupuram, Tirukoilur taluks of Villupuram district; Ulundurpettai, Vridhachalam, Tittagudi taluks of Cuddalore district; Udaiyarpalayam, Ariyalur taluk of Perambalur district; and Lalgudi taluk of Tiruchchirappalli district of Tamil Nadu state.The link canal alignment passes through Pennar basin, Streams between Pennar and Palar basins, Palar basin and streams between Palar and Cauvery basins. The link canal takes off from the right flank of Somasila dam with a full supply level of 95.420 m. and runs parallel on right side of the Kandaleru flood flow canal, upto RD 10 km. The canal generally runs in south direction till it out-falls into Grand Anicut across Cauvery River at RD 529.190 km. The major rivers that would be crossed by the canal are Swarnamukhi, Arani Ar, Nagari, Palar, Cheyyar, Ponnaiyar, and Vellar. The districts that would be benefited by the link canal through enroute irrigation are Nellore, Chittoor of Andhra Pradesh state and Tiruvallur, Kancheepuram, Vellore, Tiruvannamalai, Villupuram, Cuddalore districts of Tamil Nadu state and Pondicherry (U.T).
    [Show full text]