Council of States 1953
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National Compilation on Dynamic Ground Water Resources of India, 2017
National Compilation on Dynamic Ground Water Resources of India, 2017 Government of India Ministry of Jal Shakti Department of Water Resources, RD & GR Central Ground Water Board Faridabad July 2019 भारत सरकार K C Naik केीय भूिम जल बोड Chairman जल श मंालय जल संसाधन , नदी िवकास और गंगा संर ण िवभाग Government of India Central Ground Water Board Ministry of Jal Shakti Department of Water Resources, River Development and Ganga Rejuvenation FOREWORD Water is crucial to life on Earth, however, its availability in space and time is not uniform. The near utilization of surface water resources has made the public and Government to look towards groundwater resources to supplement the water supply. The ever- increasing demand has resulted in the greater dependence on groundwater and consequently resulting in depletion of groundwater resources in many parts of the country. In the era of climate change, groundwater may act as a buffering resource in the time of drought and it needs to be managed more intensively to enhance its sustainability. The change in groundwater extraction and rainfall pattern necessitate periodic revision of groundwater resources assessment. The report 'National Compilation on Dynamic Groundwater Resources of India, 2017' is a compilation of State-wise assessment carried out jointly by CGWB and State Groundwater Departments at periodical intervals under the supervision of State level Committee of the respective States/UTs and under overall guidance of Central Level Expert Group. The groundwater resources of India are assessed following Groundwater Estimation Methodology, 2015, which takes care of all the relevant parameters contributing to the net annual ground water recharge and extractions for various uses. -
Sr. No. College Name University Name Taluka District JD Region
Non-Aided College List Sr. College Name University Name Taluka District JD Region Correspondence College No. Address Type 1 Shri. KGM Newaskar Sarvajanik Savitribai Phule Ahmednag Ahmednag Pune Pandit neheru Hindi Non-Aided Trust's K.G. College of Arts & Pune University, ar ar vidalaya campus,Near Commerece, Ahmednagar Pune LIC office,Kings Road Ahmednagrcampus,Near LIC office,Kings 2 Masumiya College of Education Savitribai Phule Ahmednag Ahmednag Pune wable Non-Aided Pune University, ar ar colony,Mukundnagar,Ah Pune mednagar.414001 3 Janata Arts & Science Collge Savitribai Phule Ahmednag Ahmednag Pune A/P:- Ruichhattishi ,Tal:- Non-Aided Pune University, ar ar Nagar, Dist;- Pune Ahmednagarpin;-414002 4 Gramin Vikas Shikshan Sanstha,Sant Savitribai Phule Ahmednag Ahmednag Pune At Post Akolner Tal Non-Aided Dasganu Arts, Commerce and Science Pune University, ar ar Nagar Dist Ahmednagar College,Akolenagar, Ahmednagar Pune 414005 5 Dr.N.J.Paulbudhe Arts, Commerce & Savitribai Phule Ahmednag Ahmednag Pune shaneshwar nagarvasant Non-Aided Science Women`s College, Pune University, ar ar tekadi savedi Ahmednagar Pune 6 Xavier Institute of Natural Resource Savitribai Phule Ahmednag Ahmednag Pune Behind Market Yard, Non-Aided Management, Ahmednagar Pune University, ar ar Social Centre, Pune Ahmednagar. 7 Shivajirao Kardile Arts, Commerce & Savitribai Phule Ahmednag Ahmednag Pune Jambjamb Non-Aided Science College, Jamb Kaudagav, Pune University, ar ar Ahmednagar-414002 Pune 8 A.J.M.V.P.S., Institute Of Hotel Savitribai Phule Ahmednag Ahmednag -
Factors Controlling Detrital Mineralogy of the Sandstone of the Lameta Formation (Cretaceous), Jabalpur Area, Madhya Pradesh, India
FactorsProc Indian Controlling Natn Sci Acad Detrital 74 No.2 Mineralogy pp. 51-56 (2008)of the Sandstone of the Lameta Formation 51 Research Paper Factors Controlling Detrital Mineralogy of the Sandstone of the Lameta Formation (Cretaceous), Jabalpur Area, Madhya Pradesh, India AHM AHMAD ANSARI*, SM SAYEED** and AF KHAN*** Department of Geology, Aligarh Muslim University, Aligarh 202 002 (UP) (Received 7 February 2008; Accepted 6 May 2008) Cretaceous (Maastrichtian) deposits of the Lameta Formation crop out along the eastern part of Jabalpur basin on isolated hills and along the banks of Narmada River near Jabalpur city. The quartzarenite composition with little amounts of feldspar, mica, rock fragments and heavy minerals, are medium to fine grained, moderately sorted to poorly sorted and subangular to subrounded. The study suggests that palaeoclimate, distance of transport and source rock composition influenced the detrital mineralogy of the sandstone. By using Suttner and Dutta diagram, the mean values of the ratio were plotted and that indicate a humid Paleoclimate in this area. The plate tectonic setting and provenance of the sandstone were interpreted using the Dickinson’s method of detrital modes and Qt-F-L, Qm-F-Lt, Qp-Lv-Ls and Qm-P-K triangular diagrams. The petrofacies analysis of the Lameta Formation suggest mainly craton interior in a rifted continental margin basin setting. The plot of various quartz types on diamond diagram after [17] reflects Plutonic terrain. The probable provenance of these sandstones is Mahakoshal and Jabalpur Groups. Key Words: Cretaceous; Lameta Formation; Jabalpur; Mineralogy; Madhya Pradesh; India 1. Introduction Table 1. Stratigraphy of Lameta Formation, Jabalpur area (Madhya Pradesh); Tandon et al. -
Indigenous Knowledge of Local Communities of Malwa Region on Soil and Water Conservation
Int.J.Curr.Microbiol.App.Sci (2016) 5(2): 830-835 International Journal of Current Microbiology and Applied Sciences ISSN: 2319-7706 Volume 5 Number 2(2016) pp. 830-835 Journal homepage: http://www.ijcmas.com Original Research Article doi: http://dx.doi.org/10.20546/ijcmas.2016.502.094 Indigenous Knowledge of Local Communities of Malwa Region on Soil and Water Conservation Manohar Pawar1*, Nitesh Bhargava2, Amit Kumar Uday3 and Munesh Meena3 Society for Advocacy & Reforms, 32 Shivkripa, SBI Colony, Dewas Road Ujjain, India *Corresponding author ABSTRACT After half a century of failed soil and water conservation projects in tropical K e yw or ds developing countries, technical specialists and policy makers are Malwa, reconsidering their strategy. It is increasingly recognised in Malwa region Indigenous, that the land users have valuable environmental knowledge themselves. This Soil and Water review explores two hypotheses: first, that much can be learned from Conservation previously ignored indigenous soil and water conservation practices; second, Article Info that can habitually act as a suitable starting point for the development of technologies and programmes. However, information on ISWC (Indigenous Accepted: 10 January 2016 Soil and Water Conservation) is patchy and scattered. Total 14 indigenous Available Online: Soil and water Conservation practises have been identified in the area. 10 February 2016 Result showed that these techniques were more suitable accord to geographic location. Introduction Soil and water are the basic resources and their interactions are major factors affecting these must be conserved as carefully as erosion-sedimentation processes. possible. The pressure of increasing population neutralizes all efforts to raise the The semi–arid regions with few intense standard of living, while loss of fertility in rainfall events and poor soil cover condition the soil itself nullifies the value of any produce more sediment per unit area. -
Early Cretaceous Alkaline/Ultra-Alkaline
300 Article 300 by Rajesh K. Srivastava Early Cretaceous alkaline/ultra-alkaline silicate and carbonatite magmatism in the Indian Shield – a review: implications for a possible remnant of the Greater Kerguelen Large Igneous Province Department of Geology, Centre of Advanced Study, Institute of Science, Banaras Hindu University, Varanasi 221005, India; Email: [email protected] (Received : 12/01/2019; Revised accepted : 24/07/2019) https://doi.org/10.18814/epiiugs/2020/020017 ABSTRACT alkaline/ultra-alkaline silicate rocks is directly related to the nature The early Cretaceous (ca. 118-100 Ma) alkaline/ultra- and source of melts and their crystallization history. The origin of carbonated silicate melts through liquid-immiscibility or fractional alkaline silicate and carbonatite magmatism, exclusively crystallization suggest genetic connection between carbonate and recorded in the Chhotanagpur Gneissic Complex and silicate derivatives, whereas direct genetic connection between these the Shillong Plateau-Mikir Hills in the eastern/north- two rocks is uncertain if derived directly from low-degree partial eastern regions of the Indian Shield, have been reviewed melts of carbonated mantle peridotite at deeper level (cf. Bell et al., to understand their genetic aspects. These are thought 1998; Gittins and Harmer, 2003; Srivastava et al., 2005; Mitchell, 2005; Melluso et al., 2010; Beccaluva et al., 2017). Furthermore, the to be associated to the Kerguelen hot spot, active in this spatial and temporal connections between carbonatites and Large region during ca. 118-100 Ma. The existing geochemical, Igneous Provinces (LIPs), and ultimately to plume tectonics, are also geochronological and isotopic data do not support any well established (e.g. Simonetti et al., 1998; Bell and Tilton, 2001; definite emplacement order for these diverse groups of Campbell, 2005; Ernst, 2014; Bryan and Ernst, 2008; Ernst and Bell, magmatic suites. -
I:\Mood for Change\Mood For
MOOD FOR CHANGE Madhya Pradesh - 2018 by Dr. Sajjan Kumar MOOD OF THE STATE - MADHYA PRADESH MOOD FOR CHANGE (MADHYA PRADESH 2018) METHODOLOGY Peoples Pulse, a Hyderabad-based Research Organization specializing in fieldwork based political and electoral research undertook a month long ground study in poll bound Madhya Pradesh. The field study was led and coordinated by Peoples Senior Associate Dr. Sajjan Kumar, a Ph.D from CPS, JNU. Peoples Pulse research scholars travelled over 6000 kilometres across Madhya Pradesh covering all the six sub-regions of the state, Gwalior, Bundelkhand, Baghelkhand, Mahakoshal, Malwa and Bhopal to understand the mood of the people at the ground level. This was done from 28th May to 27th June, 2018, about six months before the schedule for Madhya Pradesh Assembly elections. Peoples Pulse research scholars covered 44 out of 51 districts of the state, with 7 districts, namely, Bhind in the Gwalior region, Sagar in Bundelkhand region, Singrauli and Murwara in Baghelkhand region, Narsimhapur and Burhanpur in Mahakoshal region and Neemuch in Malwa region could not be covered. 2 MOOD OF THE STATE - MADHYA PRADESH This study was undertaken to ascertain the people’s opinions and perceptions on the current political scenario as well as their future choices. As part of the study and as a background to people’s opinion, their economic, social and political status as well as perceived problems were also collected. The study was based on open-ended free-wheeling conversations with respondents to elicit their views on a host of issues interspersed with the question related to the specific study. -
Nizam's Rule and Muslims
Broadsheet on Contemporary Politics Nizam’s Rule and Muslims Truth and Fairy Tales about Hyderabad’s Liberation Volume 1, No 1 (Quarterly) Bilingual (English and Telugu) November 2010 Donation : Rs. 10/- Contents • Editorial • Silences and History M.A. Moid • A Muslim perspective about Hyderabad Hasanuddin Ahmed • Celebration on my coffin M.A. Majid • Do not hurt self-respect Rafath Seema & Kaneez Fathima • Half-truths, misconceptions! Divi Kumar • Granted Nizam’s despotism, what about ARASAM’s? Jilukara Srinivas • How the Nizam treated Scheduled Castes Ashala Srinivas • Two connotations of ‘Nizam’ R. Srivatsan H.E.H. Mir Osman Ali Khan Editorial Group: M A Moid, A Suneetha, R Srivatsan Nizam of Hyderabad Translation Team: Kaneez Fathima, M.A. Moid, R. Srivatsan (English) A. Srinivas, A. Suneetha (Telugu) Advisory Board: Sheela Prasad, Aisha Farooqi, Rama Melkote, K. Sajaya, P. Madhavi, B. Syamasundari, Susie Tharu, Veena Shatrugna, D. Vasanta, K. Lalita, N. Vasudha, Gogu Shyamala, V. Usha Production: A. Srinivas, T. Sreelakshmi Published by : Anveshi Research Centre for Women’s Studies, 2-2-18/49, D.D. Colony, Amberpet, Hyderabad 500013. sheet since many positions express themselves EditorialEditorial with intensity. Readers of Telugu media are generally not aware about the discussion in Urdu and vice versa. We have therefore decided to cover this controversy by selecting e welcome our readers to this location. In this forum, we will try to go some pieces from the Telugu and Urdu print inaugural issue of Anveshi’s beyond this familiar split between high theory media. One article, M.A. Moid’s “Silences and WBroadsheet on Contemporary Politics. -
Political Economy of Irrigation Development in Vidarbha
Political Economy Of Irrigation Development In Vidarbha SJ Phansalkar I. Introduction: • Vidarbha comprises ofthe (now) eleven Eastern districts in Maharashtra. As per the 1991 Census Over 17 million people live in some 13300 villages and nearly 100 small and big towns in Vidarbha, covering a total of 94400 sq km at a population density of 184 persons per sq km. Thirty four percent ofthese people belong to the SC/ST. While a large majority of the people speak Marathi or its dialects as their mother tongue, there is a strong influence ofHindi in all public fora. A strong sense of being discriminated against is perpetuated among the people of Vidarbha. Its origin perhaps lies in the fact that the city ofNagpur (which is the hub of all events in Vidarbha) and hence the elite living in it suffered a major diminution in importance in the country. It was the capital ofthe Central Provinces and Berar till 1956 and hence enjoyed a considerable say in public matters. The decision making hub shifted to Mumbai in 1956. Vidarbha elite have now got to compete for power with the more resourceful and crafty elite from Western Maharashtra. While largely an issue with the political elite, yet this sense of having been and still being wronged is significantly reinforced by the fact of relatively lower development of this region vis a vis other areaS in Maharashtra. For instance the CMIE Development indexes shown below indicate significantly lower level ofdevelopment for the Vidarbha area. .. Levels ofDevelopment in different districts ofVidarbha SN District Relative Index of Development as per 'CMIE 1 Akola 65 2 Amrawati 74 3 Bhandara 73 4 Buldana 59 - 5 Chandrapur 72 6 Gadchiroli 64 7 Nagpur 109 8 Wardha 99 9 Yavatmal 64 Maharashtra . -
Page 400-454
400 4. Policy of the Agitators : The leaders of the movement are not believers in the policy of non-violence for achieving their objects. In order to terrorise the State Government and its Muslim officials, some Hindus of Poona, such as Dr. Gore residing in Rasta Peth, G. M. Nalavade, Khadivle, Vaidya and others, are considering plans to prepare bombs and send them to Hyderabad for use in the agitation. At the beginning of February this year, while speaking at a meeting of the Hindu Maha Sabha Working Committee in Delhi, Barrister Savarkar, the President, was reported to have allowed full and unrestricted discretion to individual workers to pursue any plan in furtherance of the struggle without even making any fetish of non-violence. Savarkar was said to he contemplating the launching of secret subversive propaganda amongst the State subjects and spreading the cult of terrorism. In connection with the Hyderabad agitation meeting were held at Nagpur, Amraoti, Akola and Yeotmal districts of the C. P., and speeches were made stating that the launching of the satyagraha amounted to a declaration of war which could not be carried on through non-violence. The processionists were armed with lathis, a huge knife was displayed in the meeting, and the conduct of the Arvi Hindus in the riot of 1925 was praised. 401 On February 11 th 1939, at a meeting at Nasik, B. V. Devre of Poona said that without armed opposition the Hindus could not possibly obtain their rights in a State like Hyderabad. On March 29th, at a meeting at Poona to give farewell to a jatha of volunteers bound for Hyderabad, B. -
Portrait of Population Madhya Pradesh
CENSUS OF INDIA, 1981 A PORTRAIT OF POPULATION MADHYA PRADESH Draft by M. L. SHARMA Deputy Director and M. G. MOHRIL .A ssistant Director DIRECTORATE OF CENSUS OPERATIONS MADHYA PRADESH BHOPAL (iii) ,,' 7f ,,' eI MADHYA PRADESH ADMINISTRATIVE DIVISIONS 1981 . " ,,' ..! DiStRICT HEAOI)UART~RS 'AHSILH(,I,OQUAATERS. t,Whlllll1t MI'IIt Gl dlltrict or tahilidillirl fr'Om tht n~lI\tm d~ ~rag~uQrtm or 1M tahiti IltQdqulrter, It hal bun ~ho\l'rt . wll~,ft bracklls thU1 (BASTAR) (Gira) 0 ..Z ~ ri e , ltuttr ~fiI " 114+16r 4ltlrid $ o",Arta klolotl to Cttio talilil 01 0Il1/t 'Utrltk II J .. Arft klo"ll• .!ttlJQiltlll' t'~lil, I I 3 so· I MADHYA PRADESH COMMUNICATIONS . , . " ,t ,f ~ , A\ \ ~ IOUNDm,SUTE ;8 OISHICI H~~ll SUTE miTAl .. UILVAY, iMAOGAU.f • IIEHEmU. NHMWmH. lOAD, NATlml~I;IIWAY .. STAlE Hr,HvAY KI[OMEHfS 32 0 32 64 96 121160 .Shontr; t~III1I.1 ~Illior dhlii(t. I LJ .iOL:J;o;;;oi . ArlO \,Io~ .. t. {)QIIQ \Qhsil Qt OI\iQ dil\ri,t, " Auo biron" 10 ~O~~oI9~r tQ~,11 (v) J(b)-364 R.G. Illllia/NDl 88 (vii) '''l i .f' z ~ % i til .'\' III 0 4 ...c ti: a:: ..::> G. • 4 ~ ... ~ % c cI 0 I-e 2 4 1&1 S; "/.,I&. k 0 0 0 c c 0 0 0 0 0 $ S $ 4 en ... 8 ~ ... ,.. ~ .. - :J IX ~ ... ... N ~ (J\ .. - . (000100 ~I ) I. Z ~e 0 - :~~ , ~ ""..J ..... 4 ~ ~ A- S 0 ..• a. :> I t ~ '> ~ I -0 Z .... :; -.. ;.~ ...0 ~~~ 0 0 0 0 0 0 0 0 c 0 0 0 0 0 0 0 0 CD S 0 CD ID 04 0 ~ ~ N N N ~ ~ .. -
Regional Imbalance in the Indian State of Andhra Pradesh with Special Reference to Telengana
REGIONAL IMBALANCE IN THE INDIAN STATE OF ANDHRA PRADESH WITH SPECIAL REFERENCE TO TELENGANA A Dissertation submitted to the Tilak Maharashtra University Towards the Fulfillment of the Requirements for the Degree of MASTER OF PHILOSOPHY IN POLITICAL SCIENCE Submitted by: Supervised by: Robinson. Undrasi (Rg. No: 2207012987) Dr. Manik Sonawane Principal, (SDA) Head, Dept.of Political science, Mumbai Central. T.M.V. Sadashiv Peth, Pune DEPARTMENT OF POLITICAL SCIENCE TILAK MAHARASHTRA UNIVERSITY SADASHIV PETH, PUNE 411031 JANUARY 2013 DECLARATION BY THE CANDIDATE I, Robinson Undrasi declare on oath that the references and literature which are quoted in my dissertation entitle “Regional imbalance in the Indian state of Andhra Pradesh with special reference to Telangana” are from original sources and are acknowledged at the appropriate place in the dissertation. I declare further that I have not used this information for any purpose other than my research. Place : Mumbai Date : January, 2013 (Robinson Undrasi) Dr. Manik D. Sonawane Post-Graduate Dept. of Political M.A., M.Phil, Ph.d. Science and Public Administration, Head of the Department Tilak Maharashtra Vidya Peeth Sadashiv Peth, Pune. 411030 Ph. 020-24454866 ==================================================== CERTIFICATE BY GUIDE This is Certified that the work incorporated in his ‘M.Phil’ dissertation “Regional imbalance in the Indian state of Andhra Pradesh with special reference to Telangana” submitted by Robinson Undrasi was carried out under my supervision. Such material as obtained from other sources has been duly acknowledged in the dissertation. Date: / / Dr. Manik D. Sonawane ACKNOWLEDGEMENT I express my sincere gratitude to my guide Dr. Manik Sonawane, Head of Department of Political Science Tilak Maharashtra Vidyapeth for his valuable guidance, critical comments, encourage and constent inspiration throughout this course of investigation. -
Petrological and Geochemical Characteristics of Paleoproterozoic Ultramafic Lamprophyres and Carbonatites from the Chitrangi
Petrological and geochemical characteristics of Paleoproterozoic ultramafic lamprophyres and carbonatites from the Chitrangi region, Mahakoshal supracrustal belt, central India Rajesh K Srivastava Centre of Advanced Study, Department of Geology, Banaras Hindu University, Varanasi 221 005, India. e-mail: [email protected] A number of ENE–WSW trending Paleoproterozoic dykes and plugs of mafic, ultramafic, alkaline and carbonatite rocks intrude Mahakoshal supracrustal belt (MSB), which is a part of the Central Indian Tectonic Zone (CITZ). Best exposures of these intrusions are found in the eastern parts of the MSB, particularly in and around Chitrangi area. Many of these intrusions have greenschist facies mineral composition and show sharp contact with supracrustal rocks. However, igneous textures, such as por- phyritic/glomeroporphyritic, are still preserved in the form of partly pseudomorphed olivines, phlogo- pites and pyroxenes. Striking feature observed in some ultramafic samples is the presence of melanite garnet and rounded or elliptical carbonate ocelli. The petrographic characteristics suggest occurrence of carbonate-rich ultramafic lamprophyres; close to aillikite composition. Coarse-grained carbonatites show hypidiomorphic texture and mostly composed of calcite with appreciable amount of silicate miner- als like clinopyroxene, phlogopite and olivine (often pseudomorphed by calcite, amphibole and chlorite). It is difficult to establish any direct genetic relationship between carbonatite and ultramafic lampro- phyre samples on the basis of their chemistry; they were likely derived from distinct parental melts. High Mg# (up to ∼78), and high Ni and Cr contents (up to ∼1700 and ∼1100, respectively) and low HREE concentration in few ultramafic lamprophyre samples apparently suggest their derivation from a near-primary mantle-derived melts originated at great depths.