Satpura Range | india geography in hindi | Guide 2021

 The Satpura Range is a range of hills in crucial India. It begins in Japanese Gujarat near the Arabian Sea coast, then runs east through Maharashtra, Madhya Pradesh, and ends inside the country of Chhattisgarh. It extends for a distance of 900 km with a lot of its peaks growing above one thousand m (three,300 toes). It is angular in form, with its vertex at Ratnapura and the two aspects being parallel to the Tapti and Narmada rivers. It runs parallel to the Vindhya Range, which lies to the north, and those east-west tiers divide the Indo-Gangetic simple of northern India from the Deccan Plateau mendacity in the south. The Narmada runs within the melancholy among the Satpura and Vindhya degrees, and drains the northern slope of the Satpura range, strolling west in the direction of the Arabian Sea.

 The northern end of the variety continues as remoted hills and rocky ridges into Haryana, ending near Delhi. The highest height is Mount Abu, growing to one,722 m (five,653 toes), mendacity close to the southwestern extremity of the variety, close to the border with Gujarat. The town of Ajmer with its lake lies at the southern slope of the variety in Rajasthan. The Aravalli Range is the eroded stub of a historical folded mountain device that changed as soon as it snow-capped. The variety rose in a Precambrian occasion called the Aravalli-Delhi orogen. The range joins of the ancient segments that make up the Indian craton, the Marwar section to the northwest of the range, and the Bundelkhand segment to the southeast. The present Aravalli variety is simplest a remnant of the colossal device that existed in prehistoric instances with numerous of its summits growing above the snow line and nourishing glaciers of stupendous importance which in turn fed many fantastic rivers.

The Western Gats  | Satpura

The Western Ghats or Sahyadri mountains run along the western fringe of India's Deccan Plateau and separate the Deccan plateau from a slender coastal undeniable along the Arabian Sea. The variety starts south of the Tapti River close to the border of Gujarat and Maharashtra, and runs about 1,600 km (1,000 miles) thru the states of Maharashtra, Goa, Karnataka, Kerala, and Tamil Nadu, nearly to the southern tip of the Indian peninsula. The common elevation is around 1,000 m with the better peaks occurring in the southern section in Nilgiris and in Kerala. The Anai Mudi in the Cardamom Hills at 2,695 m (eight,841 ft) in Kerala is the best peak inside the Western Ghats.

The Eastern Ghats are a discontinuous range of mountains, which have been eroded and cut via by using the 4 predominant rivers of southern India, the Godavari, Mahanadi, Krishna, and Kaveri. These mountain stages make it bigger from West Bengal within the north, via Orissa and Andhra Pradesh to Tamil Nadu inside the south. They run parallel to the Bay of Bengal and are not as tall as the Western Ghats, although a number of its peaks are over 1000 m in peak.

The Eastern and Western Ghats meet on the Nilgiri or Malay knot in Tamil Nadu. The Anai Mudi within the Cardamom Hills at 2,695 m (eight,841 feet) in Kerala is the highest top in the Western Ghats. The Nilgiris are taken into consideration to be part of the Western Ghats.

the Indo Plain 

The Indo-Gangetic plains are huge floodplains of the Indus and the Ganga- Brahmaputra river structures. They run parallel to the Himalaya mountains, from Jammu and Kashmir inside the west to Assam in the east, draining the states of Punjab, Haryana, Japanese Rajasthan, Uttar Pradesh, Bihar, Jharkhand, and West Bengal. The plains encompass an area of seven-hundred,000 km² (270,000 mile²) and vary in width via their period by using several hundred kilometers. Major rivers that form part of this machine are the Ganga (Ganges) and Indus River at the side of their tributaries; Beas, Yamuna, Gomti, Ravi, Chambal, Sutlej, and Chenab.

The Indo-Gangetic belt is the arena's maximum vast expanse of uninterrupted alluvium shaped with the aid of the deposition of silt by means of several rivers. The plains are flat and by and large treeless, making it conducive for irrigation through canals. The location is also wealthy in groundwater sources.

The plains are one of the global's maximum intensely farmed regions. Crops grown on the Indo-Gangetic Plain are commonly rice and wheat, grown in rotation. Other crops encompass maize, sugarcane, and cotton. Also known as the Great Plains, the Indo-Gangetic plains rank the various world's maximum densely populated areas. Water our bodies of India are Indian ocean, Arabian Sea, Bay of Bengal.

The Thar Desert Facts In India Geography facts 

The Thar Desert (also known as the Great Indian Desert) is a hot wasteland that paperwork a big part of western India. Spread over 4 states in India – Punjab, Haryana, Rajasthan, and Gujarat it covers an area of 208,110 km² (eighty,350 mile²). The wasteland continues into Pakistan as the Cholistan Desert. Most of the Thar Desert is located in Rajasthan, covering 61% of its geographic region. Most of the desolate tract is rocky, with a small part of the acute west of the wilderness being sandy.

The starting place of the Thar Desert is unsure. Some geologists take into account it to be four,000 to 10,000 years vintage, whereas others country that aridity commenced on this area plenty earlier. The place is characterized by way of intense temperatures of above forty-five ° C (113 ° F) in the summer season to below freezing in winters. Rainfall is precarious and erratic, starting from below a hundred and twenty mm (four.72 in) in the extreme west to 375 mm (14.75 in) eastward. The lack of rainfall is especially because of the precise role of the desert with respect to the Aravalli range. The wasteland lies inside the rain shadow region of the Bay of Bengal arm of the southwest monsoon. The parallel nature of the variety to the Arabian Sea arm additionally method that the wasteland does no longer acquire tons rainfall.

The barren region may be divided into areas, the Great Desert and the little wasteland. The first-rate Desert extends northwards from the threshold of the Rann of the Kutch region of Gujarat. The little wilderness extends from the River Luni among the cities of Jodhpur and Jaisalmer, as much as the northern regions. The soils of the arid area are normally sandy to sandy-loam in texture. The consistency and intensity vary in keeping with the topographical functions. The low-lying loams are heavier and may have a tough pan of clay, calcium carbonate, or gypsum. Due to the low population density, the effect of the populace on the environment is distinctly less in comparison to the relaxation of India.

The High Lands | Gk in Hindi 

The Central Highlands are composed of 3 main plateaus – the Malwa Plateau within the west, the Deccan Plateau in the south, (protecting most of the Indian peninsula); and the Chota Nagpur Plateau in Jharkhand in the direction of the east.

Satellite photo of the Deccan area of southern India

The Deccan plateau is a huge triangular plateau, bounded by the Vindhyas to the north and flanked by means of the Eastern and Western Ghats. The Deccan covers a complete area of one. Nine million km² (735,000 mile²). It is mostly flat, with elevations starting from three hundred to six hundred m (1,000 to 2,000 ft).

The name Deccan comes from the Sanskrit word Dakshina, because of this "the south". The plateau slopes lightly from west to east and give upward thrust to several peninsular rivers which include the Godavari, the Krishna, the Kaveri, and the Narmada. This area is commonly semi-arid because it lies on the leeward side of each Ghats. Much of the Deccan is included by using thorn scrub woodland scattered with small areas of the deciduous broadleaf wooded area. The climate ranges from hot summers to moderate winters.

The Chota Nagpur Plateau is a plateau in jap India, which covers plenty of Jharkhand state as well as adjacent parts of Orissa, Bihar, and Chhattisgarh. The overall vicinity of Chota Nagpur Plateau is approximately 65,000 km² (25,000 mile²). The Chota Nagpur Plateau is made from three smaller plateaus, the Ranchi, Hazaribagh, and Kodarma plateaus. The Ranchi plateau is the most important of the plateaus, with a median elevation of 700 m (2, three hundred feet). Much of the plateau is forested, included by means of the Chota Nagpur dry deciduous forests. The plateau is well-known for its full-size reserves of ores and coal.

Besides the Great Indian peninsula, the Kathiawar Peninsula in Gujarat is every other large peninsula of India.

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