Stratigraphy of India
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List of Colleges in Mahabubnagar District
LIST OF COLLEGES IN MAHABUBNAGAR DISTRICT YEAR OF COLLEGE S NO COLLEGE NAME & ADDRESS STARTING FIRST YEAR STRENGTH DURING THE ACADEMIC YEARS CODE 2009-10 2010-11 2011-12 2012-13 17 MAHABUBNAGAR Government 1 17002 GOVT JR COLLEGE FOR GIRLS, MAHABUBNAGAR 1982-1983 808 777 899 745 2 17003 GOVT M V S JR COLLEGE, MAHABOOBNAGAR 1973-1974 197 169 182 220 3 17018 GOVT JR COLLEGE FOR BOYS MAHABUBNAGAR 1978-1979 533 410 465 389 4 17027 GOVT JUNIOR COLLEGE, BHOOTHPUR 2004-2005 178 202 224 200 5 17039 GOVT JR COLLEGE KOTHAKOTA 1981-1982 83 69 92 98 6 17045 GOVT JR COLLEGE, KOILAKONDA 2009-2010 32 151 139 186 7 17052 GOVT JR COLLEGE, YANAMANAGANDLA 1989-1990 266 345 380 257 8 17063 GOVT JR COLLEGE GADWAL 1982-1983 298 339 270 301 9 17075 GOVT JR COLLEGE FOR GIRLS,GADWAL(V&M) 2013-2014 10 17079 GOVT JR COLLEGE FOR BOYS JADCHERLA 1982-1983 119 145 148 141 11 17081 GOVT JR COLL FOR GIRLS JADCHERLA 1982-1983 216 195 260 231 12 17083 GOVT JR COLLEGE, TIMMAJIPET 1999-2000 119 142 148 144 13 17093 GOVT JR COLLEGE, KOTHAPET 2008-2009 41 65 62 80 14 17096 GOVT JR COLLEGE, SHADNAGAR 1970-1971 162 194 236 172 15 17101 GOVT JUNIOR COLLEGE, BALANAGAR 2001-2002 142 142 159 167 16 17113 GOVT JR COLLEGE MOGILIGIDDA 1999-2000 145 184 199 170 17 17126 GOVT JR COLLEGE KALWAKURTHY 1970-1971 167 172 155 144 18 17140 GOVT JR COLLEGE (BOYS), KOLLAPUR 1970-1971 189 153 123 66 19 17141 GOVT JR COLLEGE FOR GIRLS KOLLAPUR 1999-2000 195 162 190 62 LIST OF COLLEGES IN MAHABUBNAGAR DISTRICT YEAR OF COLLEGE S NO COLLEGE NAME & ADDRESS STARTING FIRST YEAR STRENGTH DURING THE ACADEMIC -
Mobile No PASARE SANDEEP (71286) TELANGANA (Adilabad)
Volunteer Name with Reg No State (District) (Block) Mobile no PASARE SANDEEP (71286) TELANGANA (Adilabad) (Indravelli - Narnoor) 8333058240 KUMBOJI VENKATESH (73448) TELANGANA (Adilabad) (Adilabad Rural - Adilkabad) 9652885810 ANNELA ANIL KUMAR (71285) TELANGANA (Adilabad) (Boath - Mavala) 9989298564 CHOUDHARY PARASHURAM (64601) TELANGANA (Adilabad) (Bhela - Jainath) 8500151773 KOLA NAGESH (64600) TELANGANA (Adilabad) (Neradigonda - Gudihathnoor) 6305633892 RAMAGIRI SAI CHARAN (64598) TELANGANA (Adilabad) (Bajarhathnoor - Utnoor) 9000669687 SUNKA RAMULU (64488) TELANGANA (Adilabad) (Talamadugu) 9676479656 THUKKAREDDY RAJENDHAR TELANGANA (Adilabad) (Ichoda - Srikonda) 7993779502 REDDY (64487) BOJANAM VANITHA (64258) TELANGANA (Adilabad) (Adilabad Rural - Adilkabad) 8333958398 KOKKULA MALLIKARJUN (61007) TELANGANA (Adilabad) (Adilabad Rural - Adilkabad) 9640155109 ARGULA JAIPAL (72523) TELANGANA (Adilabad) (Adilabad Rural - Adilkabad) 8500465732 JANA RAJASRI (63026) TELANGANA (Nizamabad) (Velpoor - Bheemgal) 8897974188 BENDU NAVEEN (70971) TELANGANA (Nizamabad) (Mendora - Erragatla) 6305672227 RAJASHEKAR ENUGANTI (63088) TELANGANA (Nizamabad) (Armoor - Jakaranpally) 9059848340 BHUCHHALI SAI PRIYA (68731) TELANGANA (Nizamabad) (Nizamabad North South) 9177234014 PALTHYA PREMDAS (71113) TELANGANA (Nizamabad) (Rudrur - Varni - Kotagiri) 8121557589 M SAI BABU (63018) TELANGANA (Nizamabad) (Indalwai - Dichpally) 9989021890 GUNDLA RANJITH KUMAR (61437) TELANGANA (Nizamabad) (Sirikonda - Dharpally) 8500663134 BOTHAMALA NARESH (63035) TELANGANA -
Sources of Maratha History: Indian Sources
1 SOURCES OF MARATHA HISTORY: INDIAN SOURCES Unit Structure : 1.0 Objectives 1.1 Introduction 1.2 Maratha Sources 1.3 Sanskrit Sources 1.4 Hindi Sources 1.5 Persian Sources 1.6 Summary 1.7 Additional Readings 1.8 Questions 1.0 OBJECTIVES After the completion of study of this unit the student will be able to:- 1. Understand the Marathi sources of the history of Marathas. 2. Explain the matter written in all Bakhars ranging from Sabhasad Bakhar to Tanjore Bakhar. 3. Know Shakavalies as a source of Maratha history. 4. Comprehend official files and diaries as source of Maratha history. 5. Understand the Sanskrit sources of the Maratha history. 6. Explain the Hindi sources of Maratha history. 7. Know the Persian sources of Maratha history. 1.1 INTRODUCTION The history of Marathas can be best studied with the help of first hand source material like Bakhars, State papers, court Histories, Chronicles and accounts of contemporary travelers, who came to India and made observations of Maharashtra during the period of Marathas. The Maratha scholars and historians had worked hard to construct the history of the land and people of Maharashtra. Among such scholars people like Kashinath Sane, Rajwade, Khare and Parasnis were well known luminaries in this field of history writing of Maratha. Kashinath Sane published a mass of original material like Bakhars, Sanads, letters and other state papers in his journal Kavyetihas Samgraha for more eleven years during the nineteenth century. There is much more them contribution of the Bharat Itihas Sanshodhan Mandal, Pune to this regard. -
Beware, 'They' Create Clashes CM KCR Alerts Police
Follow us on: @TheDailyPioneer facebook.com/dailypioneer RNI No. TELENG/2018/76469 Established 1864 ANALYSIS 7 MONEY 8 PAGE 12 Published From HYDERABAD DELHI LUCKNOW A CASE FOR ‘INDIA'S DECISION TO BLOCK 43 MORE CHOWMAHALLA PALACE: BHOPAL RAIPUR CHANDIGARH NATURAL GAS CHINESE APPS VIOLATES WTO RULES’ CASTLE IN THE AIR BHUBANESWAR RANCHI DEHRADUN VIJAYAWADA *LATE CITY VOL. 3 ISSUE 40 HYDERABAD, THURSDAY NOVEMBER 26, 2020; PAGES 12 `3 *Air Surcharge Extra if Applicable TRS working president KTR with The Pioneer www.dailypioneer.com More reports in page 4 KTR: BJP is Beware, ‘they’ create clashes anti-Telangana RS working president KT Rama Rao on TWednesday skewered CM KCR alerts police the BJP-led Union govern- ment, giving the expansion of 'BJP' as 'Build-up Jumla CM asks police to tackle them with iron hand to maintain law and order Party' and characterizing the Centre as patently 'anti- PNS n HYDERABAD attempts by these elements to Telangana'. disturb peace and harmony The Narendra Modi gov- As a way to ensure that the TS should be dealt with firmly. ernment's actions and Police do not let their guard The anti-social elements approach towards Telangana ‘Our rival is MIM, not BJP’ down amidst a politically Without naming should be crushed with an iron over the past six years had turbo-charged but highly viti- the forces, the hand, he declared. The Chief proved beyond doubt that ated atmosphere, Chief Minister made it clear that the BJP was 'anti-Telangana', n TRS will hit a century this time in GHMC polls Minister K Chandrashekhar CM said that the police had been given a free KTR averred in an interview Rao on Wednesday instructed government hand to deal with anti-social to The Pioneer, while decry- n the police brass to take stern had 'definite elements. -
Upper Jurassicelower Cretaceous Stratigraphy in South-Eastern Tibet: a Comparison with the Western Himalayas
Author's personal copy Cretaceous Research 29 (2008) 301e315 www.elsevier.com/locate/CretRes Upper JurassiceLower Cretaceous stratigraphy in south-eastern Tibet: a comparison with the western Himalayas Xiumian Hu a,*, Luba Jansa b, Chengshan Wang c a State Key Laboratory of Mineral Deposits Research, Department of Earth Sciences, Nanjing University, Nanjing 210093, China b Department of Earth Sciences, Dalhousie University, Halifax B3H 3J5, Canada c Geological Centre for Tibetan Plateau, China University of Geosciences, Beijing 100083, P.R. China Received 24 January 2007; accepted in revised form 14 May 2007 Available online 28 November 2007 Abstract Lithostratigraphic studies of the Upper JurassiceLower Cretaceous sedimentary successions exposed in the TingrieGyangze area, south- eastern Tibet resulted in the establishment of a revised stratigraphic framework. A major crustal fault separates the southern Tibetan sedimentary successions into a Southern Zone and a Northern Zone. The Upper JurassiceLower Cretaceous strata of the Southern Zone are subdivided into the Menkadun Formation (Oxfordian, Kimmeridgian, up to lower Upper Tithonian), the Gucuo Formation (Upper Tithonian to Lower Albian) and the overlying Dongshan Formation (Upper Albian). The Gucuo Formation is further subdivided into a quartz arenite unit, which is overlain by a shale unit, in turn overlain by a volcaniclastic sandstone unit. The youngest cluster of detrital zircon absolute age data (127.7 Æ 1.8 Ma) from the lower part of the volcaniclastic unit of the Gucuo Formation place the volcanic event before the Late Barremian. In the Northern Zone, the Upper JurassiceLower Cretaceous strata have been subdivided into four formations: the Zhera Formation (Upper Jurassic), the Weimei Formation (Tithonian), the Rilang Formation (?Berriasian) and the Gyabula Formation (? post-Valanginian). -
Title: Need to Sanction a New Railway Line Between Gadwal and Macherla in Andhra Pradesh. DR. MANDA JAGANNATH (NAGARKURNOOL): A
> Title: Need to sanction a new railway line between Gadwal and Macherla in Andhra Pradesh. DR. MANDA JAGANNATH (NAGARKURNOOL): A new railway line between Macherla in Andhra Pradesh to Raichur via Gadwal was proposed and as a part of it Gadwal - Raichur is completed and is ready for the inauguration. However, remaining part of the new line between Gadwal and Macherla is pending for sanction. When the matter was raised under Rule 377 the then Railway Minister Hon'ble Mamata Benerjee replied that the line between Gadwal and Macherla would be taken up after the completion of the new line between Gadwal and Raichur. In the recent past, Govt. of Andhra Pradesh proposed the line between Gadwal and Macherla on cost sharing basis. Survey was also completed two years back and sent to the Railway Board. Though two years have lapsed since the updated survey had been completed no action is forthcoming from the Railway Ministry. The line between Gadwal - Macherla is very important because it cuts short the distance between coastal Andhra and Mumbai considerably. This line passes through Nalgonda district, Mahaboobnagar in Andhra Pradesh and Raichur of Karnataka, which are very backward. There is a lot of scope of development of this area employment wise, and farmers can take up cultivation of commercial crops which will change their economic capacity. I request the Railway Ministry to take necessary steps to sanction the Gadwal - Macherla new line immediately. . -
Sample Test Paper
DIRECTION 1. Consider the following in regards to 3. The most plausible explanation of the Thar desert ; location of the Thar desert in Western 1. The region ,of moving sand and low India is ; rainfall is called Marusthali (a) The obstruction caused by the Aravallis 2. During Mesozoic era it was under the to the rainbearing wind that proceeds sea to the Ganga Valley 3. Upliftment took place during (b) The Prevalance of comparative high Pleistocene pressure 4. Only flow luni has fresh upper course (c) The absence of mountains to the north and salty lower course of Rajasthan to cause orographic Which of the statements given above rainfall is/are correct ? (d) That the moisture carried by the south- (a) 1 and 4 (b) 1,3, 4 west monsoon is driven away by the dry (c) 1, 2,3, 4 (d) 2,3, 4 upper air current. 4. Consider the location of mounts in India 2. Match List-I with List-II and select the which one of the following is in right correct answer : sequence from South to North. List- I List- II a) Kalsubai,Mahabaleshwar,Salher, (Peaks) ( Ranges) Kudremukh A. Dodabetta 1. Nilgiri Hills b) Salher,Kalsubai,Mahabaleshwar, B. Nanda Devi 2.Himalaya Mountains Kudermukh C. Amar Kantak 3. Aravalli Range c) Kudremukh ,Mahabaleshwar,Kalsubai, D. Guru Sikhar 4. Maikal Range Salher Code d) Kudremukh,Kalsubai,Mahabaleshwar, ABCD Salher (a)2134 (b)3214 5. Which one of the following states does (c)1243 not form part of the Narmada basin? (d)4123 IAS Test Series Programme 2019 ( 1 ) Test - 1 DIRECTION (a) Madhya Pradesh(b) Rajasthan 8. -
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. -
Callovian to Oxfordian Benthic Foraminifera from Ler Dome, Kutch Basin (Gujarat, India): Systematic, Ecostratigraphy and Palaeoenvironmental Reconstruction
Rivista Italiana di Paleontologia e Stratigrafia (Research in Paleontology and Stratigraphy) vol. 126(2): 315-362. July 2020 CALLOVIAN TO OXFORDIAN BENTHIC FORAMINIFERA FROM LER DOME, KUTCH BASIN (GUJARAT, INDIA): SYSTEMATIC, ECOSTRATIGRAPHY AND PALAEOENVIRONMENTAL RECONSTRUCTION SYED MD. WASIM1, MATIAS REOLID2*, ABU TALIB1 & SHABBER HABIB ALVI1 1Department of Geology, Aligarh Muslim University, 200 002 Aligarh, Uttar Pradesh, India. E-mail: [email protected] 2Department of Geology, University of Jaén, Campus Las Lagunillas sn 23071 Jaén, Spain. E-mail: [email protected] *Corresponding author. To cite this article: Wasim S. Md., Reolid M., Talib A. & Alvi S.H. (2020) - Callovian to Oxfordian benthic foraminifera from Ler Dome, Kutch Basin (Gujarat, India): Systematic, ecostratigraphy and palaeoenvironmental reconstruction. Riv. It. Paleontol. Strat., 126(2): 315-362. Keywords: Foraminifera; Systematics; Ecostratigraphy; Transgressive-regressive cycles; Kutch Basin. Abstract. Analysis of the foraminiferal assemblages of the Chari Formation (Middle-Upper Jurassic transi- tion) exposed at Ler Dome, Kutch Basin (India) allows one to interpret the incidence of different environmental parameters, especially the effect of sea-level changes in this group of microorganisms. The overall deposition of the Chari Formation took place in an open marine environment in the middle to outer shelf, having normal salinity and well-oxygenated bottom waters according to the lithofacies and the composition of the foraminiferal and macroin- vertebrate assemblages. Changes in the diversity, abundance of foraminifera, and proportion of specialist forms were associated mainly with the availability of labile organic matter on the sea floor. The changes in trophic resources were associated with fluctuations in the type of sedimentation, which ranges from carbonates to siltstones and sandstones. -
Buceros Vol-9 No-3 Year-2004
Buceros Vol. 9, No. 3 (2004) A bibliography of the Anatidae of south Asia Aasheesh Pittie 8-2-545 Road No. 7, Banjara Hills, Hyderabad 500034, India. Email: [email protected] INTRODUCTION This bibliography has been extracted from my larger a distribution pattern of the Anatidae.Accuracy in bibliographic database (Pittie 2005) and covers the transcribing is a basic tenet of bibliography and though political boundaries of the following south Asian great care has been taken to ensure it, mistakes may countries: Afghanistan, Bangladesh, Bhutan, India, the have crept in and pertinent papers, notes, reports, books, Maldives, Myanmar (Burma), Nepal, Pakistan, and Sri etc., may have been inadvertently left out.This is the Lanka. Tibet is also covered. It comprises papers, popular more likely in that I have not seen all the entries listed articles, books, published and un-published reports, and below in the original, but have freely taken them second chapters, in which members of the avian family, Anatidae hand from the ‘References’ or ‘Further Reading’ sections (ducks, geese, swans), find mention. It covers a period of papers and books. of over two and a half centuries, from 1750 up to 2004. Authors have been arranged alphabetically and their Of the 49 genera and 158 species that comprise the work chronologically. Multi-author papers have been family Anatidae worldwide (Dickinson 2003), 19 genera listed under the name of the senior author(i.e., the first and 46 species are found in south Asia. Of these, the author, not the oldest). Separate entries have not been Pink-headed Duck Rhodonessa caryophyllacea is made for co-authors. -
Environments and Faunal Patterns in the Kachchh Rift Basin
Rivista Italiana di Paleontologia e Stratigrafia volunre I i 0 no. I pp.181-190 April 2004 ENVIRONMENTS AND FAUNAL PATTERNS IN THE KACHCHH RIFT BASIN. \TESTERN INDIA, DURING THE JURASSIC FRANZ THEODOR FURSICH', JOHN H. CALLOMON" DHIRENDRA K. PANDEY.E{ ANAND K. TAITLY* Recit,ed September 19, 2002: accepted July 13,2003 Key-zoords: Jurassic, taphonomy, palaeoecology, cycles, Kach- dominata dai bivalvi, seguiti da brachiopodi, gasteropodi, coralli, ser- chh, India. pulidi e spugne. Lanalisi di 370 campioni statistici ed oltre 27000 esem- plari h;r prodotto più di a0 associazioni e rrggruppamenti bentonici. Abstract. Marine Jurassic sediments (Bajocian-Tithonian) of the Essi mostrano una relazione con molti parametri ambientali, due dei Kachchh Basin were deposited in a ramp setting. Except during the quali, salinità e clima, vengono brevemente discussi. Viene delineata la Middle and Late Bathonian, when a carbonate reginre became estab- distribuzione areale delle facies e dei biota per due porzioni temporali, lished, the fill of the basin consists predominantly of siliciclastics. The rispettivamente il Bathoniano ed il Calloviano-Oxfordiano. sediments represent environnrents that range from coastal plains (riv- ers and associated flood plains with caliche nodules), deltas, brackish water lagoons, nearshore sand and iron-oolite bars of the inner rlmp, generally situated above fair-weather wave-base, to the middle ramp in- Introduction fluenced by stornr-waves and by storm-generated currents, and finally to the outer ramp which is characterised by lor. energy, fine-grained The rift basin of Kachchh originated at the west- sediments. Changes in relative sea level produced a cyclic sedimenta- ern margin of the Indian Plate in the Triassic (e.g.