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Thiruchirappal Disaster Managem Iruchirappalli
Tiruchirappalli District Disaster Management Plan – 2020 THIRUCHIRAPPALLI DISTRICT DISASTER MANAGEMENT PLAN-2020 Tiruchirappalli District Disaster Management Plan – 2020 INDEX S. Particulars Page No. No. 1. Introduction 1 2. District Profile 2-4 3. Disaster Management Goals (2017-2030) 5-11 4. Hazard, Risk and Vulnerability Analysis with Maps 12-49 (District map, Division maps, Taluk maps & list of Vulnerable area) 5. Institutional Mechanism 50-52 6. Preparedness Measures 53-56 7. Prevention and Mitigation measures (2015 – 2030) 57-58 8. Response Plan 59 9. Recovery and Reconstruction Plan 60-61 10. Mainstreaming Disaster Management in Development Plans 62-63 11. Community and other Stake holder participation 64-65 12. Linkages / Co-ordination with other agencies for Disaster Management 66 13. Budget and Other Financial allocation – Outlays of major schemes 67 14. Monitoring and Evaluation 68 15. Risk Communication Strategies 69-70 16. Important Contact Numbers and provision for link to detailed information 71-108 (All Line Department, BDO, EO, VAO’s) 17. Dos and Don’ts during all possible Hazards 109-115 18. Important Government Orders 116-117 19. Linkages with Indian Disaster Resource Network 118 20 Vulnerable Groups details 118 21. Mock Drill Schedules 119 22. Date of approval of DDMP by DDMA 120 23. Annexure 1 – 14 120-148 Tiruchirappalli District Disaster Management Plan – 2020 LIST OF ABBREVIATIONS S. Abbreviation Explanation No. 1. AO Agriculture Officer 2 AF Armed Forces 3 BDO Block Development Officers 4 DDMA District Disaster Management Authority 5 DDMP District Disaster Management Plan 6 DEOC District Emergency Operations Center 7 DRR Disaster Risk Reduction 8 DERAC District Emergency Relief Advisory Committee. -
Geoinformatics for Concentration of Crime Against Women in Tiruchirappalli City, Tamil Nadu
Journal of Information and Computational Science ISSN: 1548-7741 GEOINFORMATICS FOR CONCENTRATION OF CRIME AGAINST WOMEN IN TIRUCHIRAPPALLI CITY, TAMIL NADU. P. Mary Santhi1, S. Balaselvakumar2 K. Kumaraswamy3 1Research Scholar 2Assistant Professor & 3Emeritus Professor 1&2 Department of Geography, Periyar E.V.R. College (Autonomous), Tiruchirappalli – 620 023 3Department of Geography, Bharathidasan University, Tiruchirappalli – 620 024 Affiliated to Bharathidasan University, Tiruchirappalli – 620 024 Abstract This paper is an attempt to mapping and analysing the concentration of crimes against women in Tiruchirappalli city for the years 2012 to 2017. The concentration score of crimes against women (rape, dowry death, molestation, kidnapping, cruelty by husband, dowry Prohibition Act 1961 and POCSO Act, 2012) recorded in each of All Women Police Station (AWPS) has been calculated and it reveals that the high concentration of crime rape was recorded in AWPS Golden rock with 1.4%, dowry death in AWPS Srirangam with 3.4%, molestation in AWPS Cantonment with 0.6%, cruelty by husband in AWPS Srirangam with 1.4%, dowry Prohibition Act 1961 cases in AWPS Fort with 1.7% and POCSO Act, 2012 cases in AWPS Golden rock with 1.4%. The low concentration of crime rape and cruelty by husband was recorded in AWPS Srirangam and Golden rock with 0.9% and molestation and kidnapping in AWPS Fort and Cantonment with 0.1 %. Among all four AWPS, the AWPS Golden rock and Srirangam had recorded the maximum concentration of crimes against women when the total crimes in a particular police station were compared to the total crimes in the study area. -
Archaeologically Excavated Sites in Tiruchirapplli
The International journal of analytical and experimental modal analysis ISSN NO: 0886-9367 M.SATHYA Roll No.25599/Ph.D2 Ph.D. Research Scholar Department of History Govt. Arts College for Women(A), Pudukkottai & Dr.S.Neelavathi M.A.,M.Phil.Ph.D Assistant Professor, Department of History Govt. Arts College for Women(A), Pudukkottai ARCHAEOLOGICALLY EXCAVATED SITES IN TIRUCHIRAPPLLI Tiruchirappalli is reputed for the antiquity of its civilization and situated on the riverbanks of Cauvery. It has been the centre of many empires and battlefields, besides being an important strategic place. It is also chiefly attractive for its remarkable Rock and the group of temples clustered on and around it. Tiruchirappalli was a part of Uraiyur till the close of the 14th century and had no separate identity. In the writings of early Greek travelers, Uraiyur is figured frequently. The Anthor of the Periplus of the Erythraean Sea mentioned Argaru (Uraiyur) as the centre of trade1. It is also referred as Koliyur in the Sangam literature2. „It would appear that, up to Viswanatha‟s reign Uraiyur was the capital of the country, and that the he found Tiruthirappalli at all events, fortified and greatly enlarged it.‟3 Antiquity of Tiruthirappalli To analyse the antiquity of Tiruthirappalli, one has to study thoroughly the geological factors which shaped the destiny of Tiruthirappalli. The present Volume XI, Issue IX, September/2019 Page No:3603 The International journal of analytical and experimental modal analysis ISSN NO: 0886-9367 geographical features, perhaps may give some scope to the study of per-history. Though hereditary and environmental factors to a large extent shaped the life of the people in the per-historic and historic periods, it was not so in the geological age. -
Annual Report 2018-19 National Institute of Technology Tiruchirappalli
ANNUAL REPORT 2018-19 NATIONAL INSTITUTE OF TECHNOLOGY TIRUCHIRAPPALLI ANNUAL REPORT 2018-19 NATIONAL INSTITUTE OF TECHNOLOGY TIRUCHIRAPPALLI CONTENTS S. No. Title Page No. DIRECTOR’S FOREWORD 1 1 CITY SCAPE 4 2 NIT, TIRUCHIRAPPALLI – AN OVERVIEW 5 2. 1 BRIEF INFORMATION ABOUT THE INSTITUTE 5 2. 2 VISION, MISSION AND CORE VALUES 5 2. 2. 1 Preamble 5 2. 2. 2 Vision 6 2. 2. 3 Mission 6 2. 2. 4 Core Values 6 3 ADMINISTRATION 7 3. 1 BOARD OF GOVERNORS 7 3. 2 COMMITTEES AT NITT 8 3. 2. 1 Finance Committee 8 3. 2. 2 Building and Works Committee 8 3. 2. 3 The Senate 9 3. 2. 4 Staff Selection Committee 10 3. 2. 5 Selection Committee for Technical / Administrative / Ministerial Staff 10 3. 3 STAFF POSITION 11 3. 4 FINANCE AND ACCOUNTS 12 4 STRATEGIC PLANNING GROUP 13 5 ACADEMIC PROGRAMMES AND AWARD OF DEGREES 14 5. 1 PROGRAMMES OF STUDY 14 5. 1. 1 Undergraduate Programmes 14 5. 1. 2 Postgraduate Programmes 14 5. 2 ADMISSIONS 2018-19 15 5. 2. 1 Fresh Admission 2018-19 15 5. 3 STUDENTS / SCHOLARS ON ROLL IN VARIOUS PROGRAMMES 16 5. 3. 1 SC/ST students on roll 17 5. 3. 2 B. Tech. / B.Arch. students on roll 17 5. 3. 3 M. Arch. & M.Tech. students on roll 18 5. 3. 4 MBA Students on Roll 18 5. 3. 5 MCA Students on Roll 18 5. 3. 6 M.Sc. Students on Roll 19 5. 3. 7 M.S. (by research) Students on Roll 19 National Institute of Technology, Tiruchirappalli – 620 015 i Annual Report 2018 – 2019 5. -
Upper Cretaceous) of the Anaipadi–Saradamangalam Region of the Cauvery Basin, South-East India
Acta Geologica Polonica, Vol. 68 (2018), No. 4, pp. 663–687 DOI: 10.1515/agp-2018-0036 Inoceramids and associated ammonite faunas from the uppermost Turonian−lower Coniacian (Upper Cretaceous) of the Anaipadi–Saradamangalam region of the Cauvery Basin, south-east India IRENEUSZ WALASZCZYK1, WILLIAM JAMES KENNEDY2 and AMRUTA R. PARANJAPE3 1 Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, PL-02-089 Warszawa, Poland. E-mail: [email protected] 2 Oxford University Museum of Natural History, Parks Road, Oxford OX1 3PW and Department of Earth Sciences, South Parks Road, Oxford OX1 3AN, United Kingdom. 3 Sinhgad College of Science, Ambegaon (Bk.), Pune 411041, India. ABSTRACT: Walaszczyk, I., Kennedy, W.J. and Paranjape, A.R. 2018. Inoceramids and associated ammonite faunas from the uppermost Turonian–lower Coniacian (Upper Cretaceous) of the Anaipadi–Saradamangalam region of the Cauvery Basin, south-east India. Acta Geologica Polonica, 68 (4), 663–687. Warszawa. The lower (but not lowermost) part of the Upper Cretaceous Anaipadi Formation of the Trichinopoly Group in the area between Kulatur, Saradamangalam and Anaipadi, in the south-western part of the Cauvery Basin in south- east India yielded rich inoceramid and ammonite faunas. The ammonites: Mesopuzosia gaudama (Forbes, 1846), Damesites sugata (Forbes, 1846), Onitschoceras sp., Kossmaticeras (Kossmaticeras) theobal dianum (Stoliczka, 1865), Lewesiceras jimboi (Kossmat, 1898), Placenticeras kaffrarium Etheridge, 1904, and Pseudoxybeloceras (Schlueterella) sp., are characteristic of the Kossmaticeras theobaldianum Zone. The absence of Peroniceras (P.) dravidicum (Kossmat, 1895) indicates the presence of only lower part of this zone, referred to the nominative Kossmaticeras theobaldianum Subzone at the localities studied. -
CYCLONE GAJA I-JENA IMMEDIATE JOINT EMERGENCY NEEDS ASSESSMEN November 2018
INTER AGENCY GROUP TAMIL NADU CYCLONE GAJA I-JENA IMMEDIATE JOINT EMERGENCY NEEDS ASSESSMEN November 2018 ©Inter-Agency Group, Tamil Nadu November 2018 Inter Agency Group, TN Cyclone Gaja Assessment Report Page 1 of 42 Table of Contents i. Acknowledgements ........................................................................................................... 3 ii. Affirmation ........................................................................................................................... 3 1. Executive summary ................................................................................................................... 4 2. Introduction/background ......................................................................................................... 6 3. Methodology and Process ....................................................................................................... 7 3.1 Sampling............................................................................................................................... 8 3.2 Tools ...................................................................................................................................... 8 3.3 Research teams/training .................................................................................................. 8 3.4 Data analysis ....................................................................................................................... 8 4. Findings ....................................................................................................................................... -
Research Article
z Available online at http://www.journalcra.com INTERNATIONAL JOURNAL OF CURRENT RESEARCH International Journal of Current Research Vol. 8, Issue, 04, pp.30018-30022, April, 2016 ISSN: 0975-833X RESEARCH ARTICLE INTER-CONECTIONS BETWEEN NARMADA AND CAUVERY BASINS DURING TURONIAN (LATE CRETACEOUS) TIME *Susheel Kumar Department of Geology, Banaras Hindu University, Varanasi 22100, India ARTICLE INFO ABSTRACT Article History: During the Late Cretaceous times the Narmada Basin in the Central India and Cauvery Basin in South rd India received a thick pile of marine sediments as a result of the global Cenomanian marine Received 23 January, 2016 Received in revised form Transgression. It is believed that Tethyan sea became narrower facilitating the formation of Indian 15th February, 2016 ocean as a result the large part of the Indian Plate especially Kachchh, Narmada and Cauvery basin Accepted 27th March, 2016 inundated. The Late Cretaceous sediments of Narmada Basin is popularly known as Bagh Beds which Published online 26th April, 2016 ranges in age from Cenomanian to Coniacian. In the Cauvery Basin Late Cretaceous sediments are known as Trichinopoly Beds and range in age from Middle Aptian to Maastrichtian. The Turonian Key words: sediments of Narmada Basin is grouped as Nodular Limestone Formation and in Trichinopoly region Lithostratigraphy of Both Basins, Maruvattar and Paravay formations. Both of these have more or less similar history, although affected Common bivalve, by fluctuating sea levels, rate of local subsidence and rate of sedimentation resulting in different Turonian. lithological framework. An attempt has been made to use Turonian bivalves of the two sub-basin to give further ascertain of the views of the faunal synochronisation in these parts of Narmada and Cauvery basins. -
Geochemical Characteristics of Sandstones from Cretaceous Garudamangalam Area of Ariyalur, Tamilnadu, India: Implications of Provenance and Tectonic Setting
J. Earth Syst. Sci. (2017) 126: 45 c Indian Academy of Sciences DOI 10.1007/s12040-017-0821-3 Geochemical characteristics of sandstones from Cretaceous Garudamangalam area of Ariyalur, Tamilnadu, India: Implications of provenance and tectonic setting Babu K Department of Civil Engineering, Bannari Amman Institute of Technology, Sathyamangalam, Erode 638 401, India. e-mail: [email protected] The Trichinopoly Group (later redesignated as Garudamangalam) has unconformable relationship with underlying Uttatur Group and is divided into lower Kulakanattam Formation and upper Anaipadi For- mation. These calcareous sandstones are analysed major, trace and rare earth elements (REEs) to find out CIA, CIW, provenance and tectonic setting. The silica content of fossiliferous calcareous sandstone show wide variation ranging from 12.93 to 42.56%. Alumina content ranged from 3.49 to 8.47%. Higher values of Fe2O3 (2.29–22.02%) and low MgO content (0.75–2.44%) are observed in the Garudamangalam Formation. CaO (23.53–45.90) is high in these sandstones due to the presence of calcite as cement- ing material. Major element geochemistry of clastic rocks (Al2O3 vs. Na2O) plot and trace elemental ratio (Th/U) reveal the moderate to intense weathering of the source rocks. The Cr/Zr ratio of clas- tic rocks reveal with an average of 1.74 suggesting of felsic provenance. In clastic rocks, high ratios of LREE/ HREE, La/Sc, Th/Sc, Th/Co, La/Co and low ratios of Cr/Zr, and positive Eu anomaly ranges from (Eu/Eu* = 1.87–5.30) reveal felsic nature of the source rocks. 1. -
Stratigraphy of India
BGYCT-137 STRATIGRAPHY AND Indira Gandhi National Open University PALAEONTOLOGY School of Sciences Block STRATIGRAPHY OF INDIA UNIT 4 Precambrian of India 85 UNIT 5 Palaeozoic of India 115 UNIT 6 Mesozoic of India 133 UNIT 7 Gondwana Supergroup and Deccan Traps 149 UNIT 8 Cenozoic of Himalaya 167 GLOSSARY 181 79 Course Design Committee Prof. Vijayshri Prof. M. A. Malik (Retd.) Prof. K. R. Hari Former Director Department of Geology School of Studies in Geology & School of Sciences University of Jammu Water Resources Management IGNOU, New Delhi Jammu, Pt. Ravishankar Shukla University Prof. V. K. Verma (Retd.) Prof. D. C. Srivastava Raipur, Chhattisgarh Department of Geology Department of Earth Science Prof. S.J. Sangode University of Delhi, Indian Institute of Technology Department of Geology Delhi Roorkee Savitribai Phule Pune University Late Prof. Pramendra Dev Roorkee, Uttarkhand Pune, Maharashtra School of Studies in Earth Sciences Prof. L. S. Chamyal Dr. K. Anbarasu Vikram University Department of Geology Department of Geology Ujjain, MP M.S.University of Baroda National College Prof. P. Madhusudhana Reddy Vadodara, Gujarat Tiruchirapalli, Tamilnadu Department of Geology Prof. H. B. Srivastava Faculty of Geology Discipline Dr. B.R. Ambedkar Open University Centre of Advanced Study in School of Sciences, IGNOU Hyderabad Geology Banaras Hindu University Prof. Meenal Mishra Late Prof. G. Vallinayagam Varanasi, UP Prof. Benidhar Deshmukh Department of Geology Prof. Arun Kumar Kurukshetra University Department of Earth Sciences Dr. M. Prashanth Kurukshetra, Haryana Manipur University Dr. Kakoli Gogoi Imphal, Manipur Prof. J. P. Shrivastava (Retd.) Dr. Omkar Verma Centre of Advanced Study in Prof. (Mrs.) Madhumita Das Geology Department of Geology University of Delhi, Delhi Utkal University Bhubaneshwar, Odisha Block Preparation Team Course Contributors Dr. -
Tranche 4: Dharmapuri, Trichy and Kanyakumari Initial Environmental
Initial Environmental Examination Document Stage: Project Number: 40648-037 February 2018 IND: Infrastructure Development Investment Program for Tourism (IDIPT) Tranche 4 — Improvement at Tourist Guest House and Information Centre at Hogenakkal in Dharmapuri District, Construction of Banquet Hall & Tourist Hostel in District Town of Trichy and Renovation of Heritage Tourist Centre in Kanyakumari District Package No. IDIPT/TN/T4/NCB/07/2017 Prepared by the Department of Tourism and Culture Government of Tamil Nadu for the Asian Development Bank. This initial environmental examination report is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. CURRENCY EQUIVALENTS (as of 15 December 2017) Currency unit – indian rupee (₹) ₹1.00 = $0.015 $1.00 = ₹65.50 ABBREVIATIONS ADB - Asian Development Bank CAC - common air contaminants CFE - consent for establishment CFO - Consent for operation CRZ - Coastal Regulation Zone DOT - Department of Tourism PMSC - Project Management and Supervision Consultant EIA - Environmental Impact Assessment EMP - Environmental Management Plan GoI - Government of India IEE - Initial Environmental Examination NGO - non-government organization NOC - No Objection Certificate PIU - Project Implementation Unit PMSC - Project Management Consultant PMU - Project Management Unit RCC - Reinforced Cement Concrete ROW - right-of-way SPS - Safeguard Policy Statement NOTE In this report, "$" refers to US dollars. -
Folio Id Name 1 Add 1 Add 2 Add 3 City Pin Net Div
UNCLAIMED DIVIDEND FOLIO_ID NAME_1 ADD_1 ADD_2 ADD_3 CITY PIN NET_DIV WAR_NO 100 ACHANTA LAKSHMI 34-97 BOMMALA ST TANUKU WEST GODAVARI A P 534211 800.00 1951 10000 THIRUVENKATAM P 24,IQBAL COLONY TRICHY TAMIL NADU 620020 200.00 8233 10006 THOMAS M V NO 7 NEW KODAMBAKKAM ROAD MADRAS-600 029 600029 4000.00 11918 10009 THRESIA JOSE NO 301 MARS-A WING VASANT GALAXY BANGUR NAGAR GOREGAON[W] MUMBAI 400090 1000.00 8621 1001 BASANTH KUMAR SUBUDHI AT /PO BINKA BOLANGIR DIST BOLANGIR DIST ORRISA 767019 200.00 9367 10012 THRINADHA RAO DUNNA INCOMETAX OFFICE 9-15-10 C B M COMPOUND VISAKHAPATNAM AP 0 200.00 11462 10014 THRIPURA BALU N 3/82 AMMAVARISALA STREET RAJAMPET 516 115 CUDDAPAH 516115 400.00 5820 10015 THRIPURAMBA T PARTHA APARTMENTS 12/6 VEMBULI AMMAN KOIL STREET VIRUGAMBAKKAM WEST K K NAGAR MADRAS 600 078 600078 400.00 3936 10016 THUKARAM REDDY P PAIMAGHAM ARAGONDA CHITTOOR DT A P 517129 400.00 1121 10023 THUMALAPALLI SESHAGIRI RAO 10-2-289/59 SHANTHI NAGAR COLONY HYDERABAD ANDHRA PRADESH 500028 200.00 378 10025 TIKAM CHAND JAIN SUREKHA CLOTH MERCHANTS POST DORNAKAL DIST WARANGAL ANDHRA PRADESH 506381 200.00 5756 10029 TIRUPATHY SWAMY GUDALA 5-16-34 SARWABATLA VARI STREET KAVALI-524 201 524201 400.00 1414 1003 BASAVA P BELLARY TQ DT SHRIDARAGADDA POST KARNATAKA 583103 400.00 6781 10030 TIRUPATI VYANKATRAMANAMDEO JOSHI C/O SHRI N V JOSHI 354 SOMWAR KARAD 415 110 415110 400.00 9037 10042 TRIBHOOVANPAL GOVERDHANDAS S DUGAR BROTHERS & CO. 1116 DALAMAL TOWER 211 NARIMAN POINT BOMBAY 400 021 400021 400.00 4559 10043 TRICHINOPOLY RAMACHANDRAN L NO -
A Study on Violent Crimes in Tiruchirappalli City, Tamil Nadu
Science, Technology and Development ISSN : 0950-0707 A STUDY ON VIOLENT CRIMES IN TIRUCHIRAPPALLI CITY, TAMIL NADU P. Mary Santhi* *Research Scholar, Department of Geography Periyar E.V.R. College (Autonomous), Tiruchirappalli – 620 023 S. Balaselvakumar* *Assistant Professor, Department of Geography Periyar E.V.R. College (Autonomous), Tiruchirappalli – 620 023 Affiliated to Bharathidasan University, Tiruchirappalli – 620 024 K. Kumaraswamy** **ICSSR Senior Fellow - Emeritus Professor **Department of Geography, Bharathidasan University, Tiruchirappalli – 620 024 ABSTRACT This research is an attempt to examine the violent crimes in Tiruchirappalli city. It reveals that the highest percentage of Cruelty by husband 36%. The year 2012 had recorded the highest percentage of violent crimes i.e. about 21%. Srirangam range had suffered maximum violent crimes with 31% and violent crimes were mostly reported in Woraiyur and Srirangam police stations of Srirangam range. Watching and observing the behaviours and actions of criminals in the month of July, April and May, first week of Fridays and Sundays and during the peak hours of 2.00 a.m. to 11.00 a.m. and guiding the youth and training the students through education and various awareness programmes, intensified patrolling, security and other law enforcement activities will bring down the violent crimes in the city. KEYWORDS: violent crimes, year-wise, range-wise, police station-wise, hotspot INTRODUCTION Crime can take place anywhere and everywhere and anytime with anyone. Violent crimes can happen in public spaces such as in the street, clubs and pubs, as well as at home or in the workplace, and often the victims know the person who attacks them.