Wednesday, December 1, 2010
Wednesday, June 9, 2010
Jharkhand minerals
(A)Iron
(B)Uranium
(C)Aluminum
Jharkhand mines and minerals seem to be synonymous with the territory of Jharkhand. Jharkhand possesses a large reserve of mineral wealth within the territory: coal, iron ore, copper ore, bauxite, mica, graphite, kyanite, sillimanite, limestone, etc. form an integral part of mining industry in Jharkhand.
An estimate of the major mines and minerals of Jharkhand are as follows:
| District | Important Minerals in Jharkhand | Other Minerals |
|---|---|---|
| Deoghar, Dhanbad. | Coal | Fire Clay,Silver. |
| Garwa. | Coal | Dolomite. |
| Bokaro. | Coal | - |
| Godda. | Coal | - |
| Hazaribagh. | Coal | Fire-Clay, Feldspar, Mica, Lime stone, Stone-chips. |
| Dumka. | Coal | - |
| Sahibganj. | - | Silica Sand, Kaolin, Stone chips. |
| Giridih. | Coal | Mica. |
| Latehar, Lohardaga. | Bauxite | - |
| Gumla. | Bauxite | - |
| Palamau. | Iron Ore | Fire Clay, Graphite, Dolomite, Feldspar, Limestone, Manganese. |
| Ranchi. | - | Lime stone, Kaolin |
| Jamtara, Kodarma. | - | Mica, Stone-chips. |
| East Singhbhum. | Uranium, Copper | Quartzite, Kaolin, Gold, Silver, Fire Clay, Steatite. |
| West Singhbhum. | Iron Ore | Dolomite, Limestone, Manganese, Kyanite. |
| Sarikela Kharswan, Simdega. | - | Stone chips. |
| Pakur. | - | Stone-chips. |
Saturday, May 29, 2010
Current Status Of Radars Network in IMD
Recently we read in the newspapers that Indian Meteorological Department is modernizing its observational network by replacing its old and conventional radar by the state of art S-band Doppler Weather Radar (DWR) in a phased manner at different locations all over the country. A Doppler Weather Radar (DWR) would provide short-range accurate weather prediction in a radius of __500kms_____
Friday, December 25, 2009
Image via Wikipedia
PHYSIOGRAPHIC DIVISION OF INDIA
| Mountains | |
| The Peninsular Mountains : classified as follows | |
| the western Ghats | run along the west coast from south of the Tapti river valley to Kanyakumari; Deccan trap constitutes the northern portion of the Ghats; Southern part : composed of Archean gneisses, Schists and Charnockites Anai Muddi in the Anaimalai Hills 2,695 m (8,842 ft) in Kerala is the highest peak in the Western Ghats. |
| the Eastern Ghats | irregular hill ranges stretches from northern Orissa to the Kerala and Tamil Nadu across coastal Andhra; Highest Peak at 1680m in Vishakhapatnam dist( Andhra) |
| The meeting point of the western and Eastern Ghats in the Nilgiri Hills has the highest point at Doda Betta Peak. | |
| The Vindhya Range | Running from Sasaram(Bihar) in the east to Jobat(Gujarat) in the west separates northern India from the southern mainland They are believed to have been formed by the wastes created by the weathering of the ancient Aravali mountains.[ |
| The Satpura range | extends from Narmada valley(N) to the Tapti valley (S) ; It is triangular in shape, with its apex at Ratnapur highest point : Dhupgarh near Pachmarhi(M.P.) |
| The Aravalis | the oldest mountain range in India; most ancient fold mountain ranges ; separates the semi desert and fertile regions of Rajasthan highest point: Gurushikhar peak of Abu hills |
| The Northern Mountains : stretches across northern India from Jammu and Kashmir to Arunachal Pradesh( abt 2400km); the world’s youngest fold mountain ,achieve greatest heights in eastern Nepal | |
| the outer Himalayas ( the siwaliks ) | composed of tertiary sediments; emerged as most recent phase in Himalaya OROGENY |
| the outer Himalayas ARE SEPERATED FROM THE LESSER Himalayas by Duns ( valleys resulting from draining away of the temporary lakes formed by ridges when these obstructed the course of rivers | |
| the lesser/outer Himalayas ( the himachal) | the ranges include the 400km Pir Panjal range, the longest range of the Himalayas |
| the greater Himalayas ( the himadri) | the innermost Himalayan Range is the world’s highest and most continuous of Himalayan ranges ; Himadri’s highest peak include world’s highest peak- Mt Everest |
| the trans Himalayan zone | include imp ranges such as Zaskar Range and the Great Karakoram Range :extends 2wards south-east to form the Kailash Range; highest peak K2 longest glacier : Siachen ( Nubra Valley – 72 km ) |
| the Peninsular Plateau : largest and oldest of all the physiographic division ; north- east limit: Aravali Range ‘ northern extreme – Bundelkhand and western and eastern ends : Western Ghats and Eastern Ghats resp. | |
| the central plateaus | the upland of Central India with river Ganga (N) , Vindhya and Satpura ranges (S)Kaimur-Maikal Range (E) and Aravalis and Kutch to (W) comprise Mewar,Malwa(in M.P. formed of lava ) and Vindhya Plateaus |
| the eastern Plateaus | diversified to topography ; low lying Mahanandi basin to undulating plateatus of the Bhaghelkhand , Chhota Nagpur and Dandakaranya Meghalaya Plateau : beyond lava ridden Rajhmahal Hills |
| The Kathiawar and Kutch Plateaus | joined to the Peninsular Plateaus by Gujrat’s plain; Deccan lava make up this region while Kutch – tertiary rocks |
| The Deccan plateaus | occupy land between the Western and Eastern Ghats and south of Mahadeo ,Maikal and Satpura ranges ; comprise the Maharashtra Plateau(basalt) ‘Karnataka and Telangana plateaus ( Archaean gneisses) India’s largest plateaus |
| the great plains : lies between the Himalayas and the peninsular Plateau , alluvial in nature | |
| the Punjab Haryana plains | Comprise the Bist Doab (betn Sutlej &Beas Rivers); Upper Bari Doab ( betn Beas and Ravi Rivers) and south- east Malwa Plain. |
| the Rajasthan plains | comprise the marusthali of Thar and nearly Bagar areas Luni river : flowing 2wards south-east ,only river in region Rajasthan desert : sloping 2wards 2 direction – Indus valley in Pak ( W-wards ) and Ran of Kutch (S-wards) |
| the Ganga Plains | spreading across the states of Uttar Pradesh ,West Bengal &Bihar divided into : Ganga –Yamuna Doab , Rohilkhand Plain ,Avadh plain ( U.P.),Bihar Plain and Bengal Plain Ganga Delta : constitutes the Ben gal basin , covered with tidal forests ( the Sunderbans) |
| the Brahmaputra Plains | formed by deposit carried by Brahmaputra River , moist soil conditions |
| the Coastal plains : 4500 –km long coastline , Arabian Sea (W) , the Bay of Bengal (E)&Indian ocean (S) runs from Rann of Kutch (W) to the delta of the Ganga- Brahmaputra (E) | |
| the east coastal plains | extend betn the source of Subarnarekha and Kanyakumari ; contain deltas of almost all rivers ( except Tapti and Narmada ) ; include Tamil Nadu plains, Andhra Plain and Utkal Plain |
| the West coastal plains | run from Rann of Kutch to Kanyakumari; sandy plains |
| Islands : has a no. of islands (247) ; Bay of Bengal ( 204) & Arabian Sea (43) The Andaman and Nicobar Islands: in the Bay of Bengal, represent elevated potions of submarine mountains. Mount Harriet (460m): in South Andaman Islands is the highest point. The Nicobar group contains 19 Islands. The Great Nicobar – largest island in group Islands in Arabian Sea : coral origin & surrounded by fringing reefs e.g. Lakshadweep islands Author--Nisha Dolas | |
Sunday, November 15, 2009
Nepanagar
आगरा
Agra (English pronunciation: /ˈɑːɡrə/; Hindi: आगरा, Urdu: آ گرہ) is a city on the banks of the Yamuna River in the northern state of Uttar Pradesh, India. It finds mention in the epic Mahābhārata where it was called Agrevaṇa (अग्रेवण), or 'the border of the forest'.[1] Legend ascribes the founding of the city to Rājā Badal Singh (around 1475), whose fort, Badalgarh, stood on or near the site of the present Fort. However, the 11th century Persian poet Mas'ūd Sa'd Salmān writes of a desperate assault on the fortress of Agra, then held by the Shāhī King Jayapala, by Sultan Mahmud of Ghazni.[2] Sultan Sikandar Lodī was the first to move his capital from Delhi to Agra in the year 1506; he died in 1517 and his son Ibrāhīm Lodī remained in power there for nine more years, finally being defeated at the Battle of Panipat in 1526.[3] It achieved fame as the capital of the Mughal emperors from 1526 to 1658 and remains a major tourist destination because of its many splendid Mughal-era buildings, most notably the Tāj Mahal, Agra Fort and Fatehpūr Sikrī, all three of which are UNESCO World Heritage Sites.