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Karbi-Meghalaya Plateau
Karbi-Meghalaya plateau is, in fact, an extension of the main Indian peninsular plateau and are originally two different plateaus - Karbi Anglong Plateau and Meghalaya plateau. ThMeghalaya plateauis traditionally divided into Garo, Khasi and Jaintia Hills. The region from the river Dhansiri in the east to the Singimari River on the west is about 400 km long with an average width of about 40 km, covering about 35, 291 km2. Karbi Plateau is pear-shaped and has an area of about 7000 km2. Its link with the Meghalaya plateau proper is towards the south through a patch of highly denuded and subdued senile terrain. Details It is believed that due to the force exerted by the northeastward movement of the Indian plate at the time of the Himalayan origin, a huge fault was created between the Rajmahal hills The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are tod ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of India
India is situated north of the equator between 8°4' north (the mainland) to 37°6' north latitude and 68°7' east to 97°25' east longitude. India Yearbook, p. 1 It is the seventh-largest country in the world, with a total area of . Total area excludes disputed territories not under Indian control. India measures from north to south and from east to west. It has a land frontier of and a coastline of . On the south, India projects into and is bounded by the Indian Ocean—in particular, by the Arabian Sea on the west, the Lakshadweep Sea to the southwest, the Bay of Bengal on the east, and the Indian Ocean proper to the south. The Palk Strait and Gulf of Mannar separate India from Sri Lanka to its immediate southeast, and the Maldives are some to the south of India's Lakshadweep Islands across the Eight Degree Channel. India's Andaman and Nicobar Islands, some southeast of the mainland, share maritime borders with Myanmar, Thailand and Indonesia. The southernmost tip ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karbi Anglong Plateau
Karbi Anglong plateau is an extension of the Indian peninsular plateau in the Assam, North Eastern state of India. This area receives maximum rainfall from the Southwest summer Monsoon from June through September. Geography Average height of the plateau varies from to . Karbi Anglong Plateau is pear-shaped. It has an area of about 7000 km2. https://www.northeastindiainfo.com/2020/05/karbianglong-plateau.html Karbi ANglong Plateau It link with Meghalaya Plateau towards the south through a patch of low uneven terrain. See also * Mikir Hills Mikir Hills are a group of hills located to the south of the Kaziranga National Park, Assam. The easternmost Meghalaya comprising the detached Mikir Hills is partly isolated being surrounded by three sidesKarbi plateauor Mikir Hills is known oldes ... References Karbi Anglong district Plateaus of India Landforms of Assam {{Assam-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shillong Plateau
The Shillong Plateau is a plateau in eastern Meghalaya state, northeastern India. The plateau's southern, northern and western ridges form the Garo, Khasi and Jaintia Hills respectively. The plateau shows numerous fracture lineaments in satellite images and has been subjected to extensive and compressive forces in the N-S and E-W direction respectively. Several deep earthquakes point to tectonic activity in the mantle, such as from the 1897 Assam earthquake along the blind Oldham Fault. See also *Karbi-Meghalaya plateau. *1897 Assam earthquake *Dauki fault The Dauki fault is a major fault along the southern boundary of the Shillong Plateau that may be a source of destructive seismic hazards for the adjoining areas, including northeastern Bangladesh. The fault, inferred to go through the southern ma ... References External links INIST-CNRSEncyclopædia Britannica {{Plateaus of india Geology of India Landforms of Meghalaya Plateaus of India ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meghalaya
Meghalaya (, or , meaning "abode of clouds"; from Sanskrit , "cloud" + , "abode") is a states and union territories of India, state in northeastern India. Meghalaya was formed on 21 January 1972 by carving out two districts from the state of Assam: (a) the United Khasi Hills and Jaintia Hills and (b) the Garo Hills.History of Meghalaya State Government of India Meghalaya was previously part of Assam, but on 21 January 1972, the districts of Khasi, Garo and Jaintia Hills became the new state of Meghalaya. The population of Meghalaya as of 2014 is estimated to be 3,211,474. Meghalaya covers an area of approximately 22,430 square kilometres, with a length-to-breadth ratio of about 3:1.Meghal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rajmahal Hills
The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are today inhabited by the Sauria Paharia people whilst its valleys are dominated by the Santhal people. The hills span over an area of . Volcanic activity during the Jurassic resulted in the formation of the Rajmahal Traps. The hills are approximately located at . The Rajmahal hills are named after the town of Rajmahal which lies in the eastern Jharkhand. The hills trend north-south with an average elevation of , from the Sahibganj district to the Dumka district. The River Ganges wanders around the hills changing the direction of flow from east to south. Francis Buchanan-Hamilton travelled through the Rajmahal hills in the early 19th century. He described the hills that seemed impenetrable in a zone where few travellers had been. He wrote that everywhere people were hostile, apprehensive of officials and unwil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateaus Of India
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
