PHYSIOGRAPHIC DIVISIONS of INDIA By
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Kutch Basin Forms the North-Western Part of the Western Continental
Basin Introduction :. Kutch basin forms the north-western part of the western continental margin of India and is situated at the southern edge of the Indus shelf at right angles to the southern Indus fossil rift (Zaigham and Mallick, 2000). It is bounded by the Nagar- Parkar fault in the North, Radhanpur-Barmer arch in the east and North Kathiawar fault towards the south. The basin extents between Latitude 22° 30' and 24° 30' N and Longitudes 68° and 72° E covering entire Kutch district and western part of Banaskantha (Santalpur Taluka) districts of Gujarat state. It is an east-west oriented pericratonic embayment opening and deepening towards the sea in the west towards the Arabian Sea. The total area of the basin is about 71,000 sq. km of which onland area is 43,000 sq.km and offshore area is 28,000 sq.km. upto 200 bathymetry. The basin is filled up with 1550 to 2500m of Mesozoic sediments and 550m of Tertiary sediments in onland region and upto 4500m of Tertiary sediments in offshore region (Well GKH-1). The sediment fill thickens from less than 500m in the north to over 4500m in the south and from 200m in the east to over 14,000m in the deep sea region towards western part of the basin indicating a palaeo-slope in the south-west. The western continental shelf of India, with average shelf break at about 200 m depth, is about 300 km wide off Mumbai coast and gradually narrows down to 160 km off Kutch in the north. -
Volume9 Issue9(2)
Volume 9, Issue 9(2), September 2020 International Journal of Multidisciplinary Educational Research Published by Sucharitha Publications Visakhapatnam Andhra Pradesh – India Email: [email protected] Website: www.ijmer.in Editorial Board Editor-in-Chief Dr.K. Victor Babu Associate Professor, Institute of Education Mettu University, Metu, Ethiopia EDITORIAL BOARD MEMBERS Prof. S. Mahendra Dev Prof. Igor Kondrashin Vice Chancellor The Member of The Russian Philosophical Indira Gandhi Institute of Development Society Research, Mumbai The Russian Humanist Society and Expert of The UNESCO, Moscow, Russia Prof.Y.C. Simhadri Vice Chancellor, Patna University Dr. Zoran Vujisiæ Former Director Rector Institute of Constitutional and Parliamentary St. Gregory Nazianzen Orthodox Institute Studies, New Delhi & Universidad Rural de Guatemala, GT, U.S.A Formerly Vice Chancellor of Benaras Hindu University, Andhra University Nagarjuna University, Patna University Prof.U.Shameem Department of Zoology Prof. (Dr.) Sohan Raj Tater Andhra University Visakhapatnam Former Vice Chancellor Singhania University, Rajasthan Dr. N.V.S.Suryanarayana Dept. of Education, A.U. Campus Prof.R.Siva Prasadh Vizianagaram IASE Andhra University - Visakhapatnam Dr. Kameswara Sharma YVR Asst. Professor Dr.V.Venkateswarlu Dept. of Zoology Assistant Professor Sri.Venkateswara College, Delhi University, Dept. of Sociology & Social Work Delhi Acharya Nagarjuna University, Guntur I Ketut Donder Prof. P.D.Satya Paul Depasar State Institute of Hindu Dharma Department of Anthropology Indonesia Andhra University – Visakhapatnam Prof. Roger Wiemers Prof. Josef HÖCHTL Professor of Education Department of Political Economy Lipscomb University, Nashville, USA University of Vienna, Vienna & Ex. Member of the Austrian Parliament Dr.Kattagani Ravinder Austria Lecturer in Political Science Govt. Degree College Prof. -
Herein After Termed As Gulf) Occupying an Area of 7300 Km2 Is Biologically One of the Most Productive and Diversified Habitats Along the West Coast of India
6. SUMMARY Gulf of Katchchh (herein after termed as Gulf) occupying an area of 7300 Km2 is biologically one of the most productive and diversified habitats along the west coast of India. The southern shore has numerous Islands and inlets which harbour vast areas of mangroves and coral reefs with living corals. The northern shore with numerous shoals and creeks also sustains large stretches of mangroves. A variety of marine wealth existing in the Gulf includes algae, mangroves, corals, sponges, molluscs, prawns, fishes, reptiles, birds and mammals. Industrial and other developments along the Gulf have accelerated in recent years and many industries make use of the Gulf either directly or indirectly. Hence, it is necessary that the existing and proposed developments are planned in an ecofriendly manner to maintain the high productivity and biodiversity of the Gulf region. In this context, Department of Ocean Development, Government of India is planning a strategy for management of the Gulf adopting the framework of Integrated Coastal and Marine Area Management (ICMAM) which is the most appropriate way to achieve the balance between the environment and development. The work has been awarded to National Institute of Oceanography (NIO), Goa. NIO engaged Vijayalakshmi R. Nair as a Consultant to compile and submit a report on the status of flora and fauna of the Gulf based on secondary data. The objective of this compilation is to (a) evolve baseline for marine flora and fauna of the Gulf based on secondary data (b) establish the prevailing biological characteristics for different segments of the Gulf at macrolevel and (c) assess the present biotic status of the Gulf. -
Smart Border Management: Indian Coastal and Maritime Security
Contents Foreword p2/ Preface p3/ Overview p4/ Current initiatives p12/ Challenges and way forward p25/ International examples p28/Sources p32/ Glossary p36/ FICCI Security Department p38 Smart border management: Indian coastal and maritime security September 2017 www.pwc.in Dr Sanjaya Baru Secretary General Foreword 1 FICCI India’s long coastline presents a variety of security challenges including illegal landing of arms and explosives at isolated spots on the coast, infiltration/ex-filtration of anti-national elements, use of the sea and off shore islands for criminal activities, and smuggling of consumer and intermediate goods through sea routes. Absence of physical barriers on the coast and presence of vital industrial and defence installations near the coast also enhance the vulnerability of the coasts to illegal cross-border activities. In addition, the Indian Ocean Region is of strategic importance to India’s security. A substantial part of India’s external trade and energy supplies pass through this region. The security of India’s island territories, in particular, the Andaman and Nicobar Islands, remains an important priority. Drug trafficking, sea-piracy and other clandestine activities such as gun running are emerging as new challenges to security management in the Indian Ocean region. FICCI believes that industry has the technological capability to implement border management solutions. The government could consider exploring integrated solutions provided by industry for strengthening coastal security of the country. The FICCI-PwC report on ‘Smart border management: Indian coastal and maritime security’ highlights the initiatives being taken by the Central and state governments to strengthen coastal security measures in the country. -
The Geographic, Geological and Oceanographic Setting of the Indus River
16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan. -
Sir Creek: the Origin and Development of the Dispute Between Pakistan and India
IPRI Journal 1 SIR CREEK: THE ORIGIN AND DEVELOPMENT OF THE DISPUTE BETWEEN PAKISTAN AND INDIA Dr Rashid Ahmad Khan∗ ir Creek is one of the eight long-standing bilateral disputes between Pakistan and India that the two countries are trying to resolve under S the ongoing composite dialogue process. It is a dispute over a 96 km (60 miles) long strip of water in the Rann of Kutch marshlands of the River Indus, along the border between the Sindh province of southern part of Pakistan and the state of Rajasthan in India. For the last about 40 years, the two countries have been trying to resolve this row through talks. Although, like other bilateral issues between Pakistan and India, the row over Sir Creek, too, awaits a final solution, this is the only area where the two countries have moved much closer to the resolution of the dispute. Following a meeting between the foreign ministers of Pakistan and India on the sidelines of 14th SAARC Summit in New Delhi, an Indian official announced that the two countries had agreed on a common map of Sir Creek, after the completion of joint survey agreed last year. “W e have one common map of the area, from which we will now work and try and see how far we can take this issue to a resolution, hopefully,” declared the Indian Foreign Secretary Shivshankar Menon after Foreign Minister of Pakistan, Mr. Khurshid Mahmud Kasuri, met his Indian counterpart, Mr. Pranab Mukherji in New Delhi on 2 April 2007.1 W hile discussing the prospects of the resolution of this issue in the light of past negotiations between the two countries, this paper aims to examine the implications of the resolution of this issue for the ongoing peace process between Pakistan and India. -
Yoga in the Himalayan Foothills to Rishikesh
Yoga in the Himalayan Foothills to Rishikesh Prices start from : £ 1,879 Travel between : 01 Oct 18 and 09 Dec 18 Rating : 4 Star Icon Board Basis : As per Itinerary Duration : 9 nights Book by : 31 Aug 18 Includes : Flights from London with Virgin Atlantic Airport taxes 2 nights accommodation on Bed & Breakfast basis in Delhi 7 nights accommodation on Full Board at Dewa Retreat in a Deluxe room with a private balcony Transfer in Delhi & Rishikesh Attend special Ganage Aarti (Lamp Prayer Ceremony) on the Ganges One Complimentary Herbal Massage Per Person in our SPA during you stay Free use of Swimming Pool Library Lounge Train fare for the sector Delhi/Haridwar/Delhi by airconditioned chair car Escorted Himalayan Village Trip: Hike of 2 hrs one way to the Himalayan village, see village life, farming, herbal & organic plantations and also interact with village folk Daily Yoga, Meditation, Pranayama, Power & Restorative Yoga Sessions by a Professional & Experienced Yoga Teacher Detailed Itinerary : Bonus offer: Daily Yoga Sessions Highlights: Delhi - Rishikesh Alternate travel dates: 15 Jan 19 - 20 Feb 19 15 Mar 19 - 15 Apr 19 Hotels: Delhi - The Park Hotel 4* Rishikesh - Dewa Retreat - A Himalayan Boutique Hotel 4* Itinerary: Day 0: London Heathrow to Delhi Day 1: Delhi - 11:40 Hrs: Arrive Delhi airport. - Upon arrival at the airport, you will be met and transferred to your hotel. Day 2: Delhi to Haridwar by train Shatabadi express: 06:45 - 11:45 hrs - Transfer from hotel to New Delhi railway station in time to board train for Haridwar. Local snacks, tea / coffee and breakfast will be served on board - 11:45 Hrs: Arrive Haridwar railway station. -
Mountain Ranges in India for Banking & SSC Exam
Mountain Ranges in India for Banking & SSC Exam - GK Notes in PDF Every year 11th December is observed as the 'International Mountain Day.' A theme is set for this day to mark a purpose and to create awareness. This year's theme is “#MountainsMatter.” It will highlight the importance of mountains and their need for youth, water, disaster risk reduction, food, indigenous peoples and biodiversity. Mountains play a pivotal role in our life by altering the weather pattern and climatic conditions. They are also rich in endemic species and has great impact on Natural Ecosystem of the country. Thus, the knowledge of Mountain Ranges is very important from the point of view of various Banking, SSC and other Government Exams. To help you prepare this topic, here's the account of the major Mountain Ranges in India. A Mountain Range is a sequential chain or series of mountains or hills with similarity in form, structure and alignment that have arisen from the same cause, usually an orogeny. List of the prominent Mountain Ranges in India ⇒ The Himalaya Range • Himalaya is the highest mountain ranges in India • The word Himalaya literally translates to "abode of snow" from Sanskrit. • The Himalayan Mountain range is the youngest mountain range of India and new fold mountain is formed by the collision of two tectonic plates. • Himalayan Mountain Range has almost every highest peak of the world. • On an average they have more than 100 peaks with height more than 7200 m. 1 | P a g e • Nanga Parbat and Namcha Barwa are considered as the western and eastern points of the Himalaya. -
Avalanche Protection and Control in the Himalayas
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Defence Science Journal Def Sci J, Vol 35, No 2, April 1985, pp 255-266 Avalanche Protection and Control in the Himalayas N. MOHANRAO Snow & Avalanche Study Establishment, Manali Abstract. The problems of snow avalanches, their prediction and control in the Himalayas have assumed great relevance and importance not only for the Army but also for the progress of the Himalayan States of Jammu & Kashmir. Himachal Pradesh and Uttar Pradesh, whose upper reaches remain snowbound for nearly six months in a year. The paper discusses br~eflythe gravity of the problem and presents a broad outline of a case-study of avalanche control for Badrinath Temple and Township in Uttar Pradesh undertaken by the Snow & Avalanche Study Establishment (SASE), Manali. This and many other studies undertaken by the SASE illustrate the contribution of Defellce Science to the solution of this major problem affecting communications, tourism and hill development, as a spin-off from Defence Research. The Pirpanjals and the Great Himalayas, besides other ranges, experience heavy snow during the winter months particularly from January to March. The total snowfall is as much as 1500 cm in some years in the Western Himalayas. Storms lasting for several days bringing down at times more than 200 cm of snow in one spell lasting from 3 to 7 days are not uncommon. The problem is further accentuated when high intensities of 8 to 10 cm/hr prevail. The result is a heavy avalanche activity affecting Army posts and movements, communications, villages and winter tourism. -
Are You Suprised ?
Chapter 2 Physical features 2.1 Geographical Disposition The Pennar (Somasila) – Palar - Cauvery (Grand Anicut) link canal off takes from the existing Somasila reservoir located across the Pennar River near Somasila village in Nellore district of Andhra Pradesh state. The link canal is proposed to pass through the Kaluvaya, Rapur, Dakkili, Venkatagiri mandals of Nellore district; Srikalahasti, Thottambedu, Pitchattur and Nagari mandals of Chittoor district of Andhra Pradesh state, Tiruttani taluk of Tiruvallur district; Arakonam taluk of Vellore district; Cheyyar and Vandavasi taluks of Tiruvannamalai district; Kancheepuram, Uthiramerur taluks of Kancheepuram district; Tindivanam, Gingee, Villupuram, Tirukoilur taluks of Villupuram district; Ulundurpettai, Vridhachalam, Tittagudi taluks of Cuddalore district; Udaiyarpalayam, Ariyalur taluk of Perambalur district; and Lalgudi taluk of Tiruchchirappalli district of Tamil Nadu state.The link canal alignment passes through Pennar basin, Streams between Pennar and Palar basins, Palar basin and streams between Palar and Cauvery basins. The link canal takes off from the right flank of Somasila dam with a full supply level of 95.420 m. and runs parallel on right side of the Kandaleru flood flow canal, upto RD 10 km. The canal generally runs in south direction till it out-falls into Grand Anicut across Cauvery River at RD 529.190 km. The major rivers that would be crossed by the canal are Swarnamukhi, Arani Ar, Nagari, Palar, Cheyyar, Ponnaiyar, and Vellar. The districts that would be benefited by the link canal through enroute irrigation are Nellore, Chittoor of Andhra Pradesh state and Tiruvallur, Kancheepuram, Vellore, Tiruvannamalai, Villupuram, Cuddalore districts of Tamil Nadu state and Pondicherry (U.T). -
Unit 23 Central and Eastern India
.UNIT 23 CENTRAL AND EASTERN INDIA Objectives Introduction Malwa Jaunpur Bengal Assam 23.5.1 Kamata-Kamrup 23.5.2 The Ahoms Orissa Let Us sum UP Answers to Check Your Progress Exercises 4 23.0 OBJECTIVES In the present Unit, we will study about regional states in Central and Eastern India during the 13-15th centuries. After reading this Unit, you would learn about: the emergence of regional states in Central and Eastern India, territorial expansion of these regional kingdoms, their relations with their neighbours and other regional states, and 1 their relations with the Delhi Sultanate. 23.4 INTRODUCTION You have already read (in Block 5, Unit 18) that regional kingdoms posed severe threat to the already weakened Delhi Sultanate and with their emergence began the process of the physical disintegration of the Sultanate. In this Unit, our focus would be on the emergence of regional states in Central and Eastern India viz., Malwa, Jaunpur, Bengal, Assam and Orissa. We will study the polity-establishment, expansion and disintegration-of the above kingdoms. You would know how they emerged and succeeded in establishing their hegemony. During the 13th-15th centuries in Central and Eastern India, there emerged two types of kingdoms: a) those whose rise and development was independent of the Sultanate (for example : the kingdoms of Assam and Orissa) and b) Bengal, Malwa and Jaunpur who owed tHeir existencr ru the Sultanate. All these kingdoms were constantlyat war with each other. The nobles, ci,' ;s or rajas and local aristocracy played crucial roles in these confrontations. 23.2 MALWA The decline of the Sultanate paved the way for the emergence bf the independent kingdom of Malwa. -
GEOGRAPHY)] Born with the Vision of “Enabling a Person Located at the Most Remote Destination a Chance at Cracking AIR 1 in IAS”
IASBABA.COM 2018 IASBABA [IASBABA’S 60 DAYS PLAN-COMPILATION (GEOGRAPHY)] Born with the vision of “Enabling a person located at the most remote destination a chance at cracking AIR 1 in IAS”. IASbaba’s 60 Days Plan – (Geography Compilation) 2018 Q.1) Consider the following. 1. Himalayas 2. Peninsular Plateau 3. North Indian Plains Arrange the following in chronological order of their formations. a) 1-3-2 b) 2-1-3 c) 2-3-1 d) 3-2-1 Q.1) Solution (b) The oldest landmass, (the Peninsula part), was a part of the Gondwana land. The Gondwana land included India, Australia, South Africa, South America and Antarctica as one single land mass. The northward drift of Peninsular India resulted in the collision of the plate with the much larger Eurasian Plate. Due to this collision, the sedimentary rocks which were accumulated in the geosyncline known as the Tethys were folded to form the mountain system of western Asia and Himalayas. The Himalayan uplift out of the Tethys Sea and subsidence of the northern flank of the peninsular plateau resulted in the formation of a large basin. In due course of time this depression, gradually got filled with deposition of sediments by the rivers flowing from the mountains in the north and the peninsular plateau in the south. A flat land of extensive alluvial deposits led to the formation of the northern plains of India. Do you know? Geologically, the Peninsular Plateau constitutes one of the ancient landmasses on the earth’s surface. It was supposed to be one of the most stable land blocks.