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Ancient Hindu Rock Monuments
ISSN: 2455-2631 © November 2020 IJSDR | Volume 5, Issue 11 ANCIENT HINDU ROCK MONUMENTS, CONFIGURATION AND ARCHITECTURAL FEATURES OF AHILYA DEVI FORT OF HOLKAR DYNASTY, MAHISMATI REGION, MAHESHWAR, NARMADA VALLEY, CENTRAL INDIA Dr. H.D. DIWAN*, APARAJITA SHARMA**, Dr. S.S. BHADAURIA***, Dr. PRAVEEN KADWE***, Dr. D. SANYAL****, Dr. JYOTSANA SHARMA***** *Pt. Ravishankar Shukla University Raipur C.G. India. **Gurukul Mahila Mahavidyalaya Raipur, Pt. R.S.U. Raipur C.G. ***Govt. NPG College of Science, Raipur C.G. ****Architectural Dept., NIT, Raipur C.G. *****Gov. J. Yoganandam Chhattisgarh College, Raipur C.G. Abstract: Holkar Dynasty was established by Malhar Rao on 29th July 1732. Holkar belonging to Maratha clan of Dhangar origin. The Maheshwar lies in the North bank of Narmada river valley and well known Ancient town of Mahismati region. It had been capital of Maratha State. The fort was built by Great Maratha Queen Rajmata Ahilya Devi Holkar and her named in 1767 AD. Rani Ahliya Devi was a prolific builder and patron of Hindu Temple, monuments, Palaces in Maheshwar and Indore and throughout the Indian territory pilgrimages. Ahliya Devi Holkar ruled on the Indore State of Malwa Region, and changed the capital to Maheshwar in Narmada river bank. The study indicates that the Narmada river flows from East to west in a straight course through / lineament zone. The Fort had been constructed on the right bank (North Wards) of River. Geologically, the region is occupied by Basaltic Deccan lava flow rocks of multiple layers, belonging to Cretaceous in age. The river Narmada flows between Northwards Vindhyan hillocks and southwards Satpura hills. -
Resettlement in Narmada River Basin Evolution of Resettlement Policy in India
Resettlement in Narmada River Basin Evolution of Resettlement Policy in India Uday Shelat Professor, Department of Architecture and Planning The Maharaja Sayajirao University of Baroda, India Abstract The present paper examines the problems of resettlement of people affected by a large-scale water resource development project in India. At present there is no resettlement policy at the national level, but the Government of Gujarat has evolved resettlement policies for the Saradar Sarovar Project on the river Narmada. The attempt has been made to look into the policies, strategies and implementation process i.e., efforts made by the state government to resettle the project-affected people in the new habitats. Finally, the paper depicts recommendations and suggestions to strengthen the resettlement process. Introduction India after independence embarked on an ambitious programme of economic development. Nation faced twin problems of unemployment and poverty to begin with. The land was rich with diverse natural resources but was unharnessed. The crucial task was to channelize these resources- land, water, minerals, forests, and sea wealth so as to transform them into productive wealth for the people. India has unique geographic situation where arable land is spread out stretching from Kutch to Brahmputra valley and from Deccan trap to plains of Punjab, while bulk of surface water sources are concentrated in about dozen river basins; and 80% of surface water is available only in monsoon months which flows down the sea if not impounded. Therefore neither water nor land is utilised optimally, depriving the country of their full benefits. The Saradar Sarovar Project (SSP) on river Narmada was conceived keeping these potentials. -
Some Major Fairs of Tribal Population in Gujarat State
RESEARCH PAPER Statistics Volume : 6 | Issue : 1 | JANUARY 2016 | ISSN - 2249-555X Some Major Fairs of Tribal Population in Gujarat State KEYWORDS Bharti D.Singh Research assistant Statistics Branch District Panchayat Dahod. Introduction of Gujarat. Every year, this fair is held at Ahwa, the most Gujarat ranks highest in the country in terms of number significant town of The Dangs District. The Dangs is one of fairs held every year. Annually around 3500 fairs are of the picturesque districts of Gujarat situated at the held here mostly by the tribal population with great fes- backdrop of Saputara Hills. These hills were originally the tive fervour, splendour and pomp. These fairs, in addition abode of the tribal people, the adivasis. Therefore this fair to reflecting the rich cultural heritage of the place, also re- reflects the tribal culture perfectly, as every year, there are flect the lifestyles and deep rooted traditions of the tribal millions of tribal people who come to this place, heavily population of the state. These fairs which have religious decked up, playing the Shehnai while rhythmically beat- and mythological basis have various social, religious and ing their drums. Cultural performances like dance, drama cultural implications. Good number of foreign tourists vis- and folk songs are performed by them in this festival. The its these fairs as they are attracted by the culture, tradition name Darbar came into existence, because, in the earlier and customs of the large tribal population which partici- days, the British Darbar consisting of Rajas and Naiks were pates in these fairs. conducted in close vicinity to the Ahwa town. -
DDMP-Kheda Part-1
Ò<,F VF5l¿ jIJ:YF5G IMHGF DISTRICT DISASTER MANAGEMENT PLAN Message Gujarat State has faced a cocktail of disasters such as Flood of 1978, Cyclone of 1998, Earthquake of 2001 and Flood of 2005-06. Government of Gujarat has set up a nodal agency Gujarat State Disaster Management Authority to manage disasters in the State. Kheda District is vulnerable to natural disasters like earthquake, flood, cyclone and man-made disasters like road & rail accidents, fire, epidemics, riots. Many a time it is not possible to prevent disasters but awareness & sensitization of people regarding preparedness and mitigation of various disasters gives positive results. Collectorate-Kheda have tried to include the district related information, risks and preparedness against risks, responses at the time of disasters as well as disaster management and strategy during the disaster etc. for Kheda District. This is updated periodically and also we are improving it through our draw, errors and learn new lessons. District Disaster Management Plan (DDMP) is in two parts. Part-1 includes District profile of various disasters, action plans including IRS (Incident Response System). And Part-2 includes detalied version of DDMP as per the guidelines provided by GSDMA. Kheda - Nadiad Shri.Sudhir.B.Patel IAS May - 2019 Collector Kheda District Disaster Management Plan- 2019-20 i Preface: Gujarat State is prone to various types of natural hazards and grave disasters. Gujarat has faced a cocktail of disasters namely Flood of 1978, Cyclone of 1998, Earthquake of 2001 and Flood of 2005-06. After the Kutch earthquake in the year 2001, it was badly felt to create the permanent arrangements for long term disaster preparedness and mitigation. -
Morphotectonic of Sabarmati-Cambay Basin, Gujarat, Western India V.21, No.5, Pp: 371-383
J. Ind. Geophys. Union ( September 2017 ) Morphotectonic of Sabarmati-Cambay basin, Gujarat, Western India v.21, no.5, pp: 371-383 Morphotectonic of Sabarmati-Cambay basin, Gujarat, Western India Vasu Pancholi*1, Girish Ch Kothyari1, Siddharth Prizomwala1, Prabhin Sukumaran2, R. D. Shah3, N. Y. Bhatt3 Mukesh Chauhan1 and Raj Sunil Kandregula1 1Institute of Seismological Research, Raisan Gandhinagar, Gujarat 2Charotar University of Science and Technology (CHARUSAT), Vallabh Vidhyanagar, Gujarat 3Department of Geology, MG. Science College Ahmedabad, Gujarat *Corresponding Author: [email protected] ABSTracT The study area is a part of the peri-cratonic Sabarmati-Cambay rift basin of western Peninsular India, which has experienced in the historical past four earthquakes of about six magnitude located at Mt. Abu, Paliyad, Tarapur and Gogha. Earthquakes occurred not only along the two major rift boundary faults but also on the smaller longitudinal as well as transverse faults. Active tectonics is the major controlling factor of landform development, and it has been significantly affected by the fluvial system in the Sabarmati- Cambay basin. Using the valley morphology and longitudinal river profile of the Sabarmati River and adjoining trunk streams, the study area is divided into two broad tectono-morphic zones, namely Zone-1 and Zone-2. We computed stream length gradient index (SL) and steepness index (Ks) to validate these zones. The study suggests that the above mentioned structures exert significant influence on the evolution of fluvial landforms, thus suggesting tectonically active nature of the terrain. Based on integration of the morphometry and geomorphic expressions of tectonic instability, it is suggested that Zone-2 is tectonically more active as compared to Zone-1. -
Perennial and Non-Perennial River- River Originating from Mountains, They Get Water Throughout the Year, That River Consider As Perennial River
Perennial and Non-Perennial river- River originating from mountains, they get water throughout the year, that river consider as Perennial river. on the other hand river originating from plateau region called Non-Perennial river. these river do not have enough water for the whole year. Peninsular river- They have a large seasonal fluctuation in volume as they are solely fed from rainfall. These river flow in valley with steep gradients. the river which end in the Bay of Bengal are called 'East flowing' river, If the river empties into the Arabian sea, it is called ' West flowing' river. Inland drainage river- The river which does not empty itself into any sea, and end with any lake or any other water body is known as Inland Drainage river. Classification Indus River Originated from Bokharchu Glacier , near Mansarover. Rivers in India Total length of about 2897 km, it fall into the Arabian sea. Enter in India through Ladakh, flow only in J&K. Ganga River It flow between the Ladakh range and the Zaskar range at Leh. Brahmaputra River Originates as the Bhagirathi from the Gangotri glacier. Originates from Mansaravar Lake. Alaknanda unites with Bhagirathi at Devprayag, Uttarakhand, henceafter know as Ganga. Total length of about 3848 km. It fall into Bay of Bengal. At Bangladesh, Ganga merge with Brahmaputra, mixture known as Padma river. Enter India in Arunachal Pradesh. most of its course lies outside India. Total length of about 2510 km, It fall into the Bay of Bengal. It flow parallel to the Himalayas in the eastward direction. Originate from the Yamunotri glacier, at the Bandarpoonch peak in Uttarakhand. -
Flood Forecasting Appraisal Report 2013
kovala kayaa--laya p`yaaoga hotu For official use only Baart sarkar kond`Iya jala Aayaaoga maahI maMDla,gaaMQaInagar GOVERNMENT OF INDIA CENTRAL WATER COMMISSION MAHI DIVISION , GANDHI NAGAR baaZ pUvaa--naumaana eop`a[--jala irpaoT-- vaYa-- 2013 maahI,saabarmait evaM banaasa baoisana FLOOD FORECASTING APPRISAL REPORT 2013 MAHI,SABARMATI AND BANAS BASIN Wanakbori Weir nama--da evaM tapI baoisana saMgazna,gaaMQaInagar jala vaO&anaIya p`oxaNa pirmaMDla,gaaMQaInagar maahI maMNDla ,gaaMQaInagar NARMADA & TAPI BASIN ORGANISATION, GANDHINAGAR HYDROLOGICAL OBSERVATION CIRCLE , GANDHINAGAR MAHI DIVISION, GANDHINAGAR janavarI 2014 JANUARY 2014 BaUimaka kond`Iya jala Aayaaoga doSa maoM baaZ pUvaa-naumaana tqaa baaZ inayaM~Na piryaaojanaaAaoM kI yaaojanaa, AiBaklp tqaa kayaa- nvayana maoM mah%vapUNa- BaUimaka inaBaa rha hO. kond`Iya jala Aayaaoga nao Baart maoM baaZ inayaM~Na ka naoTvak- saBaI mah%vapUNa- AMtra-jyaIya nadI baoisana maoM ivakisat kr rKa hO ijasakI sahayata sao kond`Iya jala Aayaaoga ja$rt pDÊnao pr AMtvaa- h³[nFlaao´ tqaa str³ laovala ´, baaZ pUvaa-naumaana kao saUicat krta hO. maahI maMDla, kond`Iya jala Aayaaoga , gaaMQaInagar Wara maahI,saabarmatI tqaa banaasa baoisana maoM kDanaa³maahI baoisana´, Qarao[-³saabarmatI baoisana´ tqaa daMtIvaaDa³ banaasa baoisana´ baaMQaao ko ilae AMtvaa-h baaZ pUvaa-naumaana ka kaya- ikyaa jaata hO.[sako Alaavaa baanakbaaorI vaoyar ³maahI nadI´ tqaa sauBaaYa iba`ja Ahmadabaad ³saabarmatI nadI´ pr jala str pUvaa-naumaana ka kama BaI maahI maMDla Wara ikyaa jaata hO. Pa`stut p`itvaodna ³irpaoT-´ maoM, maahI, saabarmatI tqaa banaasa baoisana maoM dixaNa piScama maanasaUna 2013 ko daOrana ]plabQa jalaIya maaOsamaIya pirisqaityaaoM ka ica~Na ikyaa gayaa hO tqaa saaqa maoM baaZ pUvaa-naumaana sao sambainQat maahI maMDla kI gaitivaiQayaaoM ka ivavarNa idyaa gayaa hO. -
“A Visit to Sardar Sarovar Dam”
“A VISIT TO SARDAR SAROVAR DAM” 23rd September 2017 Coordinator ORGANIZED BY J. S. Makadiya CIVIL DEPARTMENT S. M.DOBARIYA PREPARED BY D R SOLANKI J S MAKADIYA K.P.BARAD 1 CONTENT (1) Acknowledgement 03 (2) General Information 04 (3) Purpose of Visit 05 (4) Learning Point 06 (5) Conclusion 13 2 ACKNOWLEDGEMENT We are gladly thankful to Head of the Department Civil Engg. for providing such great opportunities to learn something new and innovative and our faculties who gave us a great guidance regarding training and instructed us the importance of training in civil field. So we decided to take visit in Sardar Sarovar Narmada dam, near Navagam. 3 GENERAL INFORMATION Narmada Dam & sardar sarovar are one of the largest water resources of India covering four major states - Maharashtra, Madhya Pradesh, Gujarat and Rajasthan. Dam's spillway discharging capacity is 30.7 lakhs cusecs. Narmada Main Canal' s length is 532 km and it is the largest irrigation canal in the world with 1133 cumecs (40000 cusecs) capacity at the head regulator. It is the largest dam and part of the Narmada Valley Project, a large hydraulic engineering project involving the construction of a series of large irrigation and hydroelectric multi-purpose dams on the Narmada river. 4 PURPOSE OF VISIT Our main purpose for this visit is to be familiar with industrial environment and to get practical knowledge of Hydraulic structure of dam and Hydro power plant in dam. Also in 5th semester subject like Irrigation engineering requires knowledge about how components of dam and hydro power plant are constructed, so it is very much convenient to see all the practical and components in real time work environment. -
Quantitative Assessment of Coastal Changes Between
International Journal of Geology, Earth & Environmental Sciences ISSN: 2277-2081 (Online) An Online International Journal Available at http://www.cibtech.org/jgee.htm 2013 Vol.3 (3) September-December, pp.89-95/Janak et al. Research Article QUANTITATIVE ASSESSMENT OF COASTAL CHANGES BETWEEN NARMADA AND KIM RIVER OF SOUTH GUJARAT, INDIA Janak P Joshi1, Sumit Dabral2 and *Bindu Bhatt2 1Department of Geography, the Maharaja Sayajirao University of Baroda 2NHPC Ltd., Tawang Hydro-Electric Project Stage I, Nehru Market, District: Tawang – 790104, Arunachal Pradesh, India *Author for Correspondence ABSTRACT Coastal areas are very important for human beings since the beginning of time. Change detection is the process of identifying differences in the state of an object or phenomenon by observing it at different times. Coastal changes are attracting more focus since they are important environmental indicators that directly impact coastal economic development and land management. Both natural and anthropogenic processes along the coast control the erosion, and accretion activities of the coastal zones The study quantifies the changes along the Coast between Narmada and Kim River of South Gujarat, India by using geospatial techniques. The analysis of the multi-temporal remote sensing data shows that the coast is subject to important changes during years between 1978-2011 time interval including erosion and accretion. The study also demonstrates the applicability and efficacy of geospatial technique for quantitative assessment and monitoring of the coastal environment. Key Words: Quantitative, Erosion, Accretion, Coastal Region, Geospatial INTRODUCTION Coastal zone is the transition area between land and ocean Aidy et al., (2007) and is an area of complex, dynamic and delicate environment. -
The Sardar Sarovar Dam Project: Selected Documents Level
Chapter 1 The Sardar Sarovar Dam Project: An Overview Philippe Cullet The Sardar Sarovar Project (SSP) is part of a gigantic scheme seeking to build more than 3,000 dams, including 30 big dams, on the river Narmada, a 1,312 km river flowing westwards from Amarkantak in Madhya Pradesh, touching Maharashtra and ending its course in Gujarat. The SSP is a multi-purpose dam and canal system whose primary rationale is to provide irrigation and drinking water. Power generation is another expected benefit. It is the second biggest of the proposed dams on the Narmada, and its canal network is projected to be the largest in the world. The dam is situated in the state of Gujarat, which will derive most of the benefits of the project, but the submergence – 37,533 hectares in total – is primarily affecting the state of MP (55 per cent) and to a much lesser extent the state of Maharashtra. The SSP has been one of the most debated development projects of the past several decades in India and at the international level. It is only one of many similar big projects in the Narmada valley and in India generally but it has acquired a symbolic status in development debates. This is due in part to the complexity of such multi-purpose projects and the multiple positive and negative impacts associated with big dams. This is also due to the specificities of this project, which was first proposed nearly 60 years ago. Firstly, the fact that this project involves four states – Gujarat, MP, Maharashtra and Rajasthan – with the state of Gujarat receiving most of the benefits of the project has repeatedly led to disagreements among the concerned states. -
Rural Rajasthan and Tribal Gujarat November 8-29, 2021
, 38 Villa Avenue, San Rafael, CA 94901 Phone: 415-381-5861 ◆ Fax: 415-367-3081 [email protected] ◆ www.originalworld.com CST Permit #2057026-40 Rural Rajasthan and Tribal Gujarat Includes Three Festivals: Pushkar Fair, Kartik Purnima/Shamlaji Fair and Vautha Tribal/Spiritual Fair November 8-29, 2021 After you have seen the Taj and visited the “Golden Triangle;” after the forts and castles of the glorious Maharaja period; maybe even after you have visited beautiful South India - return to India to see the traditional rural lifestyles of the people. This tour ventures away from the chaos and congestion that India’s cities are known for and we step into the vast heartland of the fascinating states of Rajasthan and Gujarat. On this tour we attend the well-known Pushkar Fair as it is near the village of Kishangarh; the Kartik Purnima/Shamlaji Fair and Vautha tribal fairs. We shall stay in wonderful restored heritage properties with character and charm. Many are hosted by descendants of the royal families. There will be ample opportunities to interact with the local people. Nov 8 DAY 1, Day 1: Delhi Arrive Delhi, meet & transfer to hotel. Nov 9, Day 2: Delhi – Alwar (160 km) /Hilltop Kesroli Fort / (B,L) Enjoy a leisurely morning to relax after the long flight. We start our journey into Rajasthan with a drive to Alwar. Nestled in the Aravalli Hills, Alwar is one of the oldest cities in Rajasthan. Viratnagar and areas around Alwar have footprints of Stone Age men who lived in caves and drew sketches of animals on the walls. -
Hoshangabad District Madhya Pradesh
HOSHANGABAD DISTRICT MADHYA PRADESH Ministry of Water Resources Central Ground Water Board North Central Region Government of India 2013 HOSHANGABAD DISTRICT AT A GLANCE S. ITEMS Statistics No. 1. GENERAL INFORMATION i) Geographical area 6704 Sq.Km. ii) Administrative Divisions (As on 2013) Number of Tehsils 8 (Babai, Bankhedi, Hoshangabad, Itarsi, Pipria, Seonimalwa, Dolaria and Sohagpur) Number of Blocks 7 (Babai, Bankhedi, Hoshangabad, Kesla, Pipria, Seonimalwa and Sohagpur Number of Panchayats 391 Village Panchayats, 07 Block Panchayats and 14 Revenue Zonal Panchayats. Number of Villages 975 iii)Population (As per 2011 census) 1,240,975 iv)Nornal Rainfall (mm) 1225.9 mm 2. GEOMORPHOLOGY i) Major Physiographic Units (1) Satpura range in the south, (2) Alluvial plain in the middle and (3) Badland topography zone confined to the vicinity of Narmada river Narmada river and its tributaries, ii) Major Drainage namely, Tawa river, Denwa river, Morand river, Banjal river, Ajnal river, Ganjal river and Keolari, Hather and Indra Nadi. 3. LAND USE (Sq. Km.) i) Forest area: 2561 ii) Net area sown: 3009 iii) Cultivable area: 3150 4. MAJOR SOIL TYPES Soil Type Black soils and ferruginous red lateritic soils, Sandy clay loam, sandy loam and clay loam (area lying west of Ganjal river). Taxonomy (Ustocherpts/ Ustorthents/ Haplustalfs/Haplusterts as per pedological taxonomy) 5. PRINCIPAL CROPS 1.Wheat 2.Soyabean 3.Gram 4.Paddy 5.Tuar 6. IRRIGATION BY DIFFERENT SOURCES Number Area (Sq. Km.) Dugwells 23495 535 Tube wells/Bore wells 4853 523 Tanks/Ponds 9 11 Canals (Tawa Canal Command) 6 1474 Other Sources 163 Net Irrigated Area 2703 7.