Part I Chapter

Total Page:16

File Type:pdf, Size:1020Kb

Part I Chapter PART I CHAPTER - I INTRODUCTION CHAPTER I Introduction Climatology is a science that seeks to describe and explain the nature of climate, why it differs from place to place and how it is related to the other elements of natural environment. Climatology involves the collection and interpretation of observed weather data for developing generalization and also for testing theories. It necessitates instrumental and statistical techniques and hence is regarded as a study of causal system based on mathematical structure. The 'geographical climatology1, as the name suggests is the combination of climatology as physical science and geography as the field science with special reference to biotic life in relation to space and time. Climatology in its investigation of spatial relationship makes abundant use of tools of geography and mathematical models. However, these mathematical models, when applied to large area may not explain completely all the observed facts of climate. It is the function of the geographical climatology to describe and interpret the actual facts of climate (Stringer, 1972). The usual method of presenting these facts is in the form of maps or verbal 2 statements or in the form of statistical tables from which the maps or verbal statements are derived. Geographical climatology considers atmosphere as an entity with its movement and momentum as are affected by geographic factors such as latitude, altitude, topography and distribution of land and i/ater. It has been a long felt need for the geographers and the students of climatology in getting coherent information about the spatial and temporal behaviour of climatic elements for the state of Maharashtra. The geographical disposition of Maharashtra in India has a great bearing on the climatological studies of the entire sub-continent. The burst of monsoon over the Konkan coast, is of great significance to the people of Deccan plateau, Central India and over northern India as a whole; rather than the initiation of monsoon arrival, along the Kerala coast. Geographical climatology, as it primarily deals with the regional distribution of climatic elements, has been restricted in this present study to the two distinct geographical units of Maharashtra, the coast (Konkan) and the plateau (Desh). The study of geographical climatology offers a helpful approach In planning the agricultural operations, developing resort centers and for planning and executing various irrigation projects etc. Objectives of the Present study : The primary aim of the study is to map, describe and interpret the various climatic elements in relation to the climate of Maharashtra with a geographical background. Rainfall analysis has been emphasised amongst all the climatic elements. The rainfall data is analysed with an altogether different Astro-climatological approach. Astro- cliiaatology deals with the spatial and temporal distribution of primary and derived climatic element* in correlation with the occurrence of the various astronomical phenomena viz. the a. transit of the sun into the signs of zodiac, solar transits in the various fixed star constellations (Nakshatras) the conduction of the inner planets mercury and Venus with the sun and their setting durations phases of the moon etc. An investigation of the climatic appliances related t water budget, the moisture indices has been stressed in greater length;as these aspects find a very little place in the work done so far, in relation to Maharashtra, In additic some aspects of applied climatology, especially the comfort 4 zones and architectural layout for some stations in Maharashtra have been dealt with. previous work done and the present need s Most of the published work in the subject, namely the distribution of climatic elements, climatic classification based on Koppen and Thornthwaite systems, is related to India as a whole. The climatological investigations with special reference to Maharashtra are rare; mention may, however, be made to a few studies in which some attention has been paid to this theme and region. Prominent amongst these are the papers by Raghavendra and by C.R.V. Raman. Raghavendra has studied the trends and periodicities of rainfall in Maharashtra and applied various fcfcc statistical parameters to rainfall analysis; while C.V. Raman's investigations are related to the dates of commencement of sowing rains in Maharashtra. The publication in the series "State Climatological Summaries"; the "Climate of Maharashtra State" is of formative type and concerns mainly with the facts and information about the climatic elements. A detailed study, on the climatological aspects of Maharashtra with special emphasis to astro- -climatology has been a neglected topic in the existing 5 literature on climatology. Although the statistical information about precipita­ tion data is available on daily basis over a large number of years at various Taluka places there is comparatively paucity of data on temperature which is available for some district places, and that too for a comparative short period. This has always resulted in confining the climatologlcal studies, especially dealing with climatic classification to district places only. Constraints of similar nature have limited the scope of deliberations related to applied climatology. The computation of daily rainfall data on Naks hatr awls e basis In this study therefore has been restricted primarily at the district level. The present approach of the Nakshatrawise analysis of the,rainfall will, in future, create a new opening for the estimation and evaluation of the minor regional variations in the precipitation characteristics at Taluka level. The basic climatic data used in this work consists of the monthly and yearly rainfall figures for the various district places over a period of 70 years from 1901 to 1970 and the temperature and humidity data available for the limited G number of years during this period. This data was supplied by Indian Meterological Department, Pune; while the old issues of Gazetteer part III from 1948 to 1970,were the main source of the daily rainfall data. Proposed outline of the work : The study of geographical climatology has been organized into three sections x (i) Physical setting (ii) Spatial distribution of various cJ-imatic elements , and (ill) Climates of Maharashtra and some aspects of applied climatology. The first section describes briefly the physical setting, soil types and natural vegetation. The second part on basic climatic elements is mostly devoted to spatial and temporal variations in the distribution of climatic elements. The Chapter three in this section mainly concerns with the distribution of primary climatic elements such as temperature, pressure, relative humidity and cloud amount. These elements in the original and in derived forms are illustrated by graphs and maps. In addition to 7 Isothermal maps for different seasons the hysteresis curves of relative temperature have been dram for various places, in order to bring out the influence of continentallty on the yearly march of the seasons. The average pressure conditions for various seasons and the distribution of relative humidity at 8.30 and 17.30 hours during the four seasons of the year are discussed with the help of maps. Seasonal and diurnal variations in the wind direction influencing the local weather condition are studied \d.th the illustrations from the wind ros e maps. This is followed by the investigations of the main rainfall characteristics and the temporal variations of the dry and wet years during the last 70 ye£.rs. An attempt is also made to examine the drought and excessive rainfall years and to find out the probability of occurrence of droughts in the state. The next chapter of this section has been specially devoted to ITakshatrawise rainfall analysis, in Indian farmer is mostly habituated to plan his agricultural activities with the rainfall incidents in various Hakshutras. The division of a solar yetr into the various Nakshatra periods has a special astronomical connotation and therefore an attempt in search of 8 the Interrelationship between the rainfall amounts and various Nakshatras is made. Rainfall distribution in the fourteen Nakshatras from Kruttika to Vishakha according to the Hindu Calender forms the basis of the present study on the rainfall analysis. This analysis of rainfall data is relevant to 28 parts in all of the fourteen Nakshatras? as a Nakshatra period is further divided each into two parts I and II. Rainfall averages and variability have bean calculated Nskshatrawise and represented by means of naps. A matrix of simple eorrelatlonfl between the 28 input variables Tor each of the 26 district places has been evaluated by using the eomptttorf st 2.I.F.R. Bombay, and Regional Computer Centre, Puna. This matrix has been used to investigate the correlation between the various distinct grou^3 of variables which are significant at different levels of Ji^iiricance. This analysis further concentrates for a search of those BTakshatra groups which will be useful from the point of long range forcasting of rainfall. The third section focust&* on climates of the State and some aspects of Applied Climatology. The chapter six is mainly devoted to climatic classification and it deals with a critical account of the application of the various schemes putforth by Koppan, Lang, de-Mortonne, Miller and Thomthwaite 3 for dassifing the climates. Considering further the importance of heat and moisture factors in eco-climatic studies, an attempt is made to examplify how the Thomthwaite's scheme based on the concept of the potential evapotranspiration meets the full ecological requirements of climatic classification with reference to Maharashtra. Water balance charts for 26 district places have been used to delimit the areas of water surplus and deficit in the State. Deliberations related to 'discomfort indices' are confined to the last chapter in this section. The analysis of discomfort indices, both for morning as well as for evening is made in order to recognize suitability of climates for human comfort. In this very chapter, the architectural layout in relation to the varied climatic conditions for the four selected stations in the state has been studied.
Recommended publications
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • C6431029320.Pdf
    International Journal of Engineering and Advanced Technology (IJEAT) ISSN: 2249 – 8958, Volume-9 Issue-3, February, 2020 Estimation of Water Balance Components of Watersheds in the Manjira River Basin using SWAT Model and GIS Akshata Mestry, Raju Narwade, Karthik Nagarajan Abstract: This study mainly focus on hydrological behavior of The study area includes two watersheds from Manar stream watersheds in The Manjira River basin using soil and water (watershed code-MNJR008 and MNJR011) [19]. These assessment tool (SWAT) and Geographical information system watersheds come under Manjira river which is the tributary (GIS). The water balance components for watersheds in the of India’s second largest river Godavari and flows through Manjira River were determined by using SWAT model and GIS. some parts of Marathwada region. The various GIS data Determination of these water balance components helps to study direct and indirect factors affecting characteristics of selected such as soil data, LU/LC, DEM used as inputs in SWAT to watersheds. Manjira River contains total 28 watersheds among determine water balance components of study area. The them 2 were selected having watershed code as MNJR008 and water balancing components helps in water budgeting, gives MNJR011 specified by the Central Ground Water Board. The brief idea about watershed characteristics, this further can be SWAT input data such as Digital elevation model (DEM), land used to predict the availability of water and so can help in use and land cover (LU/LC), Soil classification, slope and water resource management.[14] weather data was collected. Using these inputs in SWAT the different water balancing components such as rainfall, baseflow, II.
    [Show full text]
  • Chapm I INTRODUCTION I Geographical Aspects of Ichandesh
    C H A P m I INTRODUCTION I Geographical aspects of IChandesh Khandesh, lying between 20* 8' and 22* 7* north latitude and 75* 42' and 76* 28' longitude with a total area of 20,099 sQuare Km formed the 'most northern district' of the terri­ tories under tne control of the sole Conunissioner of Deccan in 1818 Ad J Stretching nearly 256 Kin along the Tapi and varying in breadth from 92 to 144 iOn, Khaiidesh forms an upland basin, the most northerly section of the Deccan table-laiid. Captain John Briggs, the then Political Agent of Khandesh (1818-1823) described Khandesh as 'bounded on the south by the range of Hills in v/hich the forts of Kunhur, Uhkye and Chandoor lie; on tue north by the Satpoora Mountains; on the east by the districts of Aseer, Zeinabad, Edlabad, Badur, sind Jamner, 2 and on the west by the Hills and forests of Baglana', Prom the north-east corner, as far as the Sindwa pass on the Agra roaa, the hiil coimtry belonged to Holkar, Purther »i/est, in Sahada, the Khandesh bounaary skirts, the base of the hills; then, including the Akrani territory, it moved north, right into the heart of the hills, to where, in a deep narrow channel, the Narmada forces its way through the Satpuda. Prom this to its north-west centre, the Narmada remained the northern boundary of the district* On the east ana south-east, a row of pillars and some conveiiient streams without any marked natiiral boimdary, separated Khandesh 1‘rom the central Provinces and Berar, To the south of the Ajanta, Satmala or Chandor marked the line between Khandesh and the Mizam’s territory.
    [Show full text]
  • Geomorphic Characteristics, Fortification and Archtectural Elements of Ancient Hindu Military Check Post, Shivneri Hill Fort, Junnar, M.H
    © 2020 JETIR October 2020, Volume 7, Issue 10 www.jetir.org (ISSN-2349-5162) GEOLOGIC -GEOMORPHIC CHARACTERISTICS, FORTIFICATION AND ARCHTECTURAL ELEMENTS OF ANCIENT HINDU MILITARY CHECK POST, SHIVNERI HILL FORT, JUNNAR, M.H. INIDIA. Dr. H.D. DIWAN*, Dr. S.S. BHADAURIA**, Dr. PRAVEEN KADWE***, Dr. D.SANYAL**** *Alumni, Dept. of Applied Geology, Dept. of Civil Engineering, NIT, Raipur, C.G. **Head, Dept of Geology, Govt. NPG College of Science, Raipur, C.G. *** Head, Dept. of Defence Studies, Govt. NPG College of Science, Raipur, C.G. ****Head, Dept of Architecture, NIT, Raipur, C.G. ABSTRACT The triangular Hill Fort Shivneri had been used by Yadvas of Ancient Devagiri Kingdom as guard / check post and old trading route from Desh ( interior country ) to the Arabian Sea Port City of Kalyan . The Junnar city was an important trade centre in the 1st century AD during Satvahana Kingdom reign in the region. The military fortification was made by the Maratha Cheifs in 17th century (1630 AD) . The great Hindu Maratha worrier Chhattrapati Shivaji was born at the Fort on 19th February 1630 AD and his name was dedicated to GodessShivai Devi of fort. The rigid and highly stable grounds of Shivneri Hill provide the intact super structure of ShivneriFort . The horizontal flat topped plateaue table lands are rigid and compact in nature, belonging to the trappean basaltic rocks of Cretaceaous ages. The fort was under possession of Maratha Chief (Bhonsale) from 1595 AD till the Anglo – Maratha war of 1820 AD . In this study, the lithologic and geomorphic characteristics of Shivneri Hill region and suitability of fortification under existing physical domain of the territory has been interpreted and analysed using saterllite imagery data of the terrain.
    [Show full text]
  • Western Ghats
    Western Ghats From Wikipedia, the free encyclopedia "Sahyadri" redirects here. For other uses, see Sahyadri (disambiguation). Western Ghats Sahyadri सहहदररद Western Ghats as seen from Gobichettipalayam, Tamil Nadu Highest point Peak Anamudi (Eravikulam National Park) Elevation 2,695 m (8,842 ft) Coordinates 10°10′N 77°04′E Coordinates: 10°10′N 77°04′E Dimensions Length 1,600 km (990 mi) N–S Width 100 km (62 mi) E–W Area 160,000 km2 (62,000 sq mi) Geography The Western Ghats lie roughly parallel to the west coast of India Country India States List[show] Settlements List[show] Biome Tropical and subtropical moist broadleaf forests Geology Period Cenozoic Type of rock Basalt and Laterite UNESCO World Heritage Site Official name: Natural Properties - Western Ghats (India) Type Natural Criteria ix, x Designated 2012 (36th session) Reference no. 1342 State Party India Region Indian subcontinent The Western Ghats are a mountain range that runs almost parallel to the western coast of the Indian peninsula, located entirely in India. It is a UNESCO World Heritage Site and is one of the eight "hottest hotspots" of biological diversity in the world.[1][2] It is sometimes called the Great Escarpment of India.[3] The range runs north to south along the western edge of the Deccan Plateau, and separates the plateau from a narrow coastal plain, called Konkan, along the Arabian Sea. A total of thirty nine properties including national parks, wildlife sanctuaries and reserve forests were designated as world heritage sites - twenty in Kerala, ten in Karnataka, five in Tamil Nadu and four in Maharashtra.[4][5] The range starts near the border of Gujarat and Maharashtra, south of the Tapti river, and runs approximately 1,600 km (990 mi) through the states of Maharashtra, Goa, Karnataka, Kerala and Tamil Nadu ending at Kanyakumari, at the southern tip of India.
    [Show full text]
  • Insta Revision Tests 3.0 Test 13 to 16 Questions
    INSIGHTSIAS SIMPLYFYING IAS EXAM PREPARATION OFFLINE Centres at BENGALURU | DELHI | HYDERABAD INSTA Revision Plan 3.0 - 2020 INSTA Tests DAYS 13 to 16 QUESTIONS For more visit: www.INSIGHTSONINDIA.com Copyright © by Insights IAS All rights are reserved. No part of this document may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without prior permission of Insights IAS. INSIGHTSIAS SIMPLYFYING IAS EXAM PREPARATION DAY – 13 Which of the statements given above is/are correct? (a) 1 and 3 only 1. Arrange the following hills from East to West (b) 3 only 1. Rajmahal hills (c) 2 and 3 only (d) 1 and 2 only 2. Ramgarh hills 3. Ajanta hills 4. Consider the following statements 4. Satmala range Select the correct answer using the 1. The Thal Ghat is located on code given below: Mumbai–Nashik route. (a) 2 4 1 3 2. Pal Ghat joins the Madurai city in (b) 2 3 1 4 Tamil Nadu with Kottayam (c) 1 2 4 3 district in Kerala. (d) 1 2 3 4 Which of the statements given above is/are correct? 2. Which of the following passes (a) 1 only connects with China? (b) 2 only 1. Shipki La (c) Both 1 and 2 2. Lipu Lekh (d) Neither 1 nor 2 3. Nathu la Pass Select the correct answer using the 5. Which of the following parameters code given below: is/are considered to rank institutions across India under National Institute (a) 1 and 2 only ranking framework (NIRF)? (b) 1 and 3 only 1.
    [Show full text]
  • District Survey Report, Osmanabad
    District Survey Report, Osmanabad (Draft) (2018) Mining Section-Collectorate, Osmanabad 1 PREFACE District Survey Report has been prepared for sand mining or river bed mining as per the guidelines of the Gazette of India Notification No. S.O.141 (E) New Delhi, Dated 15th January 2016 of Ministry of Environment, Forest and Climate mentioned in Appendix-X. District Environment Impact Assessment Authority (DEIAA) and District Environment Assessment Committee (DEAC) have been constituted to scrutinize and sanction the environmental clearance for mining of minor minerals of lease area less than five hectares. The draft of District Survey Report, Osmanabad is being placed on the website of the NIC Osmanabad for inviting comments/suggestions from the general public, persons, firms and concerned entities. The last date for receipts of the comments/suggestion is twenty one day from the publication of the Report. Any correspondence in this regard may kindly be sent in MS- Office word file and should be emailed to [email protected] or may be sent by post to Member Secretary District level Expert Appraisal Committee Mining Section Collectorate Osmanabad 413 501 2 INDEX Contents Page No. 1. Introduction 4 2. Overview of Mining Activity in the District 7 3. The List of Mining Leases in the District with location, area and period of validity 9 4. Details of Royalty or Revenue received in last three years 10 5. Detail of Production of Sand or Bajari or minor mineral in last three years 10 6. Process of Deposition of Sediments in the rivers of the District 11 7. General Profile of the District 11 8.
    [Show full text]
  • Agroclimatic Features of the Study Region
    CHAPTER AGROCLIMATIC FEATURES OF THE STUDY REGION 2.1 Introduction Agroclimatic potential of any region depends upon its natural and human resources as well as level of technology and investment of capital. However, the present study is concerned with the analysis of the natural resources and that too with regard to climate. The natural resources mainly include, Climatic factors - temperature, moisture, wind, sunlight etc.; Physiographic factors - rock type, topography, altitude, and Edaphic factors - soil texture, structure and chemical composition. The most crucial among these is climate interacting with soil which is manifested through water availability to a crop. The present chapter, therefore, discusses the agroclimatic features such as topography, climate, soil, landuse etc. of the study region. 18 2.2 Background of the study region 2.2 Background of the study region 2.2.1 Physiography Dry Farming Tract, as mentioned earlier, includes the area where the annual rainfall ranges from 40 to 100 cm (Swaminathan, 1970). Of the total geographical area (307609 sq.km) of Maharashtra state, the DFT covers approximately 12300 sq.km area. Lying on the east of Sahyadris it coincides almost with the Maharashtra Plateau excluding the Vidarbha (Fig.2.1). The entire region can be resolved into a number of smaller plateaus and river valley plains. The altitude declines towards the eastern and northern periphery of the DFT. The Tapi-Purna valley an east-west furrow in the Deccan tableland lies in the northern part of the region. The study region is mainly drained by Godavari. Bhima and Krishna rivers and their tributaries. The broad valleys of these rivers bounded by 600 meter contour are separated by flat-topped divides which project eastward from the Sahyadri range.
    [Show full text]
  • UNIT – I PHYSIOGRAPHIC DIVISIONS of INDIA Geological Structure
    UNIT – I PHYSIOGRAPHIC DIVISIONS OF INDIA Geological Structure 1. THE ARCHAEAN FORMATIONS (PRE-CAMBRIAN) The Archaean Era is also known as the Precambrian Period. The division of geologic time scale from the formation of the Earth (about 4.6 billion years ago) to the beginning of the Cambrian Period of the Paleozoic Era (about 570 million years ago}. The Precambrian time constitutes about 86.7% of the Earth's history. The term 'Archaean', introduced by J.D. Dana in 1782, refers to the oldest rocks of the Earth's crust. The oldest known rocks of the Earth, the evolutionary atmosphere, the first chemosynthesis, the first photosynthesis, the life-supporting atmosphere and the Earth's modem atmosphere, were developed during the Precambrian Era (Archaean and Protozoic). Rocks of the Archaean System are devoid of any form of life. The Archaean rocks are all azoic or non fossiliferous. They are thoroughly crystalline, extremely contorted and faulted, and practically devoid of any sediment. They are largely intruded by plutonic intrusions and generally have a well-defined foliated structure. These rocks are known as the basement complex or fundamental gneisses. Cover two-thirds of Peninsular India. In the Peninsular region, the Archaean rocks are known to be of three well-defined types: a) The Bengal Gneiss occurs in the Eastern Ghats, Orissa (known as Khodoliles after Khond tribes in Koraput and Bolangir districts), stretching over Manbhum and Hazaribagh districts of Jharkhand, Nellore district of Andhra Pradesh and Salem district of Tamil Nadu. Occur in the Son Valley, Meghalaya Plateau and Mikir HiUs. Thinly foliated.
    [Show full text]
  • Salher Fo : the Highest Fo in Maharashtra
    Salher Fo: The highest fo in Maharashtra About This Experience At an astounding 1567 meters high, the Salher peak is the second highest in all of Maharashtra. Upon it stands the highest fo in the state - the Salher fo. It is one of the most prominent fos of the Maratha regime and was held by Shivaji Maharaj in the year 1671. This August, trek with us to the highest fo in Maharashtra and the twin fo of Salota. What we can promise is an exhilarating experience as you navigate your way through rock cut steps to the top of the fo, stay the night in caves and explore the ruins of the fo. Trek Diculty: Moderate Team Size: 15 only Salher Height: 5141 Salota Height: 4986 헖헢헩헜헗-ퟭퟵ 헣헥험헖헔헨헧헜헢헡헦 We understand that safety of our campers, instructors, as well as the local people are of utmost impoance. We are making sure that things are handled with great care and vigilance before, during, and aer our camps. Check Our Preparations Duration : 1N/2D Experiences : Local Treks Events In Hyderabad Meeting Point : begumpet railway station, Uma Nagar, From INR 3500 /- per person Begumpet, Hyderabad, Telangana, India Destination : Manmad, Maharashtra, India PLAN IN A NUTSHELL Day 1 Board the Ajanta Express from Secunderabad to Train Stay Not Applicable Meals Not Included Manmad Day 2 Travel to Salherwadi. Trek to Salher Fo Trek Tents All Meals Caves Day 3 Trek from Salher to Salota. Descent via Waghambe. Train Train Stay Not Applicable All Meals from Manmad to Hyderabad INCLUSIONS AND EXCLUSIONS INCLUSIONS EXCLUSIONS - Non AC train from Hyderabad to Manmad - All meals not mentioned above including and back meals in train - Local transpo from Manmad to - Personal expenses and tips Salherwadi **Note: For last minute bookings Tatkal - Local transpo from Waghambe to charges will be added to the event cost.
    [Show full text]
  • The Study of Quaternary Sediments of Manjra River,Near Chousala, Dist. Beed
    The study of Quaternary sediments of Manjra River,Near Chousala, Dist. Beed P. B. Zamarkar* A.D. Fuladi** Assistant Professor, Department of Geology, S.S.E.S.A’s Science College, Congress Nagar, Nagpur, M.S., India. Email: [email protected] Corresponding Author: A. D. Fuladi ABSTRACT The study is based on Quaternary sediments of Manjra River, Near Chousala, District Beed. The field work is carried out near Chausala. The main objective of the field work was to observe the lithology, depositional features of sediments. Deccan trap is observed at the base of the soil and Quaternary sediments. During the fieldwork samples were collected and brought to the laboratory for investigations. The laboratory study includes, pH, sieve analysis, clay mineral analysis, and Granulometric study. The study reveals that the nature of sediments suggests the flow regime is turbulent and it is a mixture of different size sediments. But at places it shows that the flow regime is much turbulent and suddenly changed to stagnancy and represented by fine sediments. The overall observation reveals that sediments are river transported. Keywords: Quaternary sediments, Manjara River, clay minerals. I INTRODUCTION The various studies on geographical, lithological and structural mapping of a limited area and Quaternary sediments have been carried out from the upper and lower Godavari sediments by a handful of workers. This prompted the author to take up the similar studies in Manjara River. Hence, the area near Chausala was selected for the present studies. Sediment supplies from continental sources to adjoining rivers are gently influenced by climatic and tectonic variables at various spatio – temporal scales (Milliman and Meade, 1983; Vaithyanathan, et.
    [Show full text]