Deccan Plateau

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Deccan Plateau
The Deccan Plateau covers parts of south-west India.
Highest point
Coordinates 17°N77°E / 17°N 77°E / 17; 77

The Deccan Plateau [1] is a large plateau in western and southern India. It rises to 100 metres (330 ft) in the north, and to more than 1,000 metres (3,300 ft) in the south, forming a raised triangle within the South-pointing triangle of the Indian subcontinent's coastline. [2]

Plateau An area of a highland, usually of relatively flat terrain

In geology and physical geography, a plateau, also called a high plain or a tableland, is an area of a highland, usually consisting of relatively flat terrain, that is raised significantly above the surrounding area, often with one or more sides with steep slopes. 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.

India Country in South Asia

India, also known as the Republic of India, is a country in South Asia. It is the seventh-largest country by area, the second-most populous country, and the most populous democracy in the world. Bounded by the Indian Ocean on the south, the Arabian Sea on the southwest, and the Bay of Bengal on the southeast, it shares land borders with Pakistan to the west; China, Nepal, and Bhutan to the northeast; and Bangladesh and Myanmar to the east. In the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives; its Andaman and Nicobar Islands share a maritime border with Thailand and Indonesia.

Indian subcontinent Peninsular region in south-central Asia south of the Himalayas

The Indian subcontinent, is a southern region and peninsula of Asia, mostly situated on the Indian Plate and projecting southwards into the Indian Ocean from the Himalayas. Geologically, the Indian subcontinent is related to the land mass that rifted from Gondwana and merged with the Eurasian plate nearly 55 million years ago. Geographically, it is the peninsular region in south-central Asia delineated by the Himalayas in the north, the Hindu Kush in the west, and the Arakanese in the east. Politically, the Indian subcontinent includes Bangladesh, Bhutan, India, Maldives, Nepal, Pakistan and Sri Lanka.


It extends over eight Indian states and encompasses a wide range of habitats, covering significant parts of Telangana, Maharashtra, Karnataka and Andhra Pradesh. [3]

Habitat ecological or environmental area inhabited by a particular species; natural environment in which an organism lives, or the physical environment that surrounds a species population

In ecology, a habitat is the type of natural environment in which a particular species of organism lives. It is characterized by both physical and biological features. A species' habitat is those places where it can find food, shelter, protection and mates for reproduction.

Maharashtra State in western India

Maharashtra is a state in the western peninsular region of India occupying a substantial portion of the Deccan plateau. It is the second-most populous state and third-largest state by area in India. Spread over 307,713 km2 (118,809 sq mi), it is bordered by the Arabian Sea to the west, the Indian states of Karnataka and Goa to the south, Telangana and Chhattisgarh to the east, Gujarat and Madhya Pradesh to the north, and the Indian union territory of Dadra and Nagar Haveli to the north west. It is also the world's second-most populous subnational entity.

Karnataka State in southern India

Karnataka is a state in the south western region of India. It was formed on 1 November 1956, with the passage of the States Reorganisation Act. Originally known as the State of Mysore, it was renamed Karnataka in 1973. The state corresponds to the Carnatic region. The capital and largest city is Bangalore.

The plateau is located between two mountain ranges, the Western Ghats and the Eastern Ghats, each of which rises from its respective nearby coastal plain, and almost converge at the southern tip of India. It is separated from the Gangetic plain to the north by the Satpura and Vindhya Ranges, which form its northern boundary. The Deccan produced some of the major dynasties in Indian history including Pallavas, Satavahana, Vakataka, Chalukya, and Rashtrakuta dynasties, the Western Chalukya, the Kadamba Dynasty, Kakatiya Empire, Vijayanagara and Maratha empires and the Muslim Bahmani Sultanate, Deccan Sultanate, and the Nizam of Hyderabad.

Western Ghats mountain range running parallel to the western coast of India

The Western Ghats, also known as Sahyadri, are a mountain range that covers an area of 140,000 square kilometres (54,000 sq mi) in a stretch of 1,600 kilometres (990 mi) parallel to the western coast of the Indian peninsula, traversing the states of Kerala, Tamil Nadu, Karnataka, Goa, Maharashtra and Gujarat. It is a UNESCO World Heritage Site and is one of the eight "hottest hot-spots" of biological diversity in the world. It is sometimes called the Great Escarpment of India. It contains a large proportion of the country's flora and fauna, many of which are only found in India and nowhere else in the world. According to UNESCO, the Western Ghats are older than the Himalayas. They influence Indian monsoon weather patterns by intercepting the rain-laden monsoon winds that sweep in from the south-west during late summer. 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 areas in the Western Ghats, including national parks, wildlife sanctuaries and reserve forests, were designated as world heritage sites in 2012 – twenty in Kerala, ten in Karnataka, five in Tamil Nadu and four in Maharashtra.

Eastern Ghats mountain range

The Eastern Ghats are a discontinuous range of mountains along India's eastern coast. The Eastern Ghats run from the northern Odisha through Andhra Pradesh to Tamil Nadu in the south passing some parts of Karnataka and in the Wayanad district of Kerala. They are eroded and cut through by four major rivers of peninsular India, viz. Godavari, Mahanadi, Krishna, and Kaveri.

Satpura Range mountain range

The Satpura Range is a range of hills in central India. The range rises in eastern Gujarat state running east through the border of Maharashtra and Madhya Pradesh to the east till Chhattisgarh. The range parallels the Vindhya Range to the north, and these two east-west ranges divide Indian Subcontinent into the Indo-Gangetic plain of northern India and the Deccan Plateau of the south. The Narmada River originates from north-eastern end of Satpura and runs in the depression between the Satpura and Vindhya ranges, draining the northern slope of the Satpura range, running west towards the Arabian Sea. The Tapti River originates in the eastern-central part of Satpura, crossing the range in the center and running west at the range's southern slopes before meeting the Arabian Sea at Surat, draining the central and southern slopes of the range. The Godavari River and its tributaries drain the Deccan plateau, which lies south of the range, and the Mahanadi River drains the easternmost portion of the range. The Godavari and Mahanadi rivers flow into the Bay of Bengal. At its eastern end, the Satpura range meets the hills of the Chotanagpur Plateau. The Satpura Range is a horst mountain and is flanked by Narmada Graben in the north and much smaller but parallel Tapi Graben in the south.


Deccan plateau, Hyderabad, India Deccan Views (31349872275).jpg
Deccan plateau, Hyderabad, India

The name Deccan is an anglicised form of the Prakrit word dakkhin or dakkhaṇa, itself derived from the Sanskrit word dákṣiṇa (meaning "southern"), as the Deccan Plateau is located in the southern part of the subcontinent. [4] [5]

Sanskrit language of ancient India

Sanskrit is a language of ancient India with a 3,500 year history, and is the oldest Indo-European language still spoken. Vedic Sanskrit is believed to be the closest to the Proto-Indo-European language. It is the primary liturgical language of Hinduism and the predominant language of most works of Hindu philosophy as well as some of the principal texts of Buddhism and Jainism. Sanskrit, in its variants and numerous dialects, was the lingua franca of ancient and medieval India. In the early 1st millennium CE, along with Buddhism and Hinduism, Sanskrit migrated to Southeast Asia, parts of East Asia and Central Asia, emerging as a language of high culture and of local ruling elites in these regions.


The Deccan region has historically lacked an enduring geo-political centre, and has been defined in various ways. Geographers have attempted to define it using indices such as rainfall, vegetation, soil type or physical features. When considering physical features, it is taken to be the area bounded on North by the Narmada River, in East by the Eastern Ghats and on West by the Western Ghats. The 16th-century historian Firishta defined Deccan as the territory inhabited by the native speakers of Kannada, Marathi, and Telugu languages. Richard M. Eaton (2005) also settled on this linguistic definition. [6]

North one of the four cardinal directions

North is one of the four compass points or cardinal directions. It is the opposite of south and is perpendicular to east and west. North is a noun, adjective, or adverb indicating direction or geography.

Narmada River A river of central India in a rift valley

The Narmada River, also called the Rewa and previously also known as Nerbudda, is a river in central India after the Godavari, and the Krishna. It is also known as "Life Line of Gujarat and Madhya Pradesh" for its huge contribution to the state of Gujarat and Madhya Pradesh in many ways. Narmada rises from Amarkantak Plateau near Anuppur district. It forms the traditional boundary between North India and South India and flows westwards over a length of 1,312 km (815.2 mi) before draining through the Gulf of Khambhat into the Arabian Sea, 30 km (18.6 mi) west of Bharuch city of Gujarat.

Firishta or Ferishta, full name Muhammad Qasim Hindu Shah, was Mughal historian of Persian origin, he was born in 1560 and died in 1620. The name Firishta means angel or one who is sent in Persian.


Topographic map of the Deccan peninsula showing the locations of major cities and towns. Map of the Cities and Towns in the Deccan Plateau, India.png
Topographic map of the Deccan peninsula showing the locations of major cities and towns.
Hogenakal Falls, Tamil Nadu Hogenakkal Falls Close.jpg
Hogenakal Falls, Tamil Nadu
Near Hampi, Karnataka Hampi Fluss Haupttempel.jpg
Near Hampi, Karnataka
Rock formations at Hyderabad, Telangana Hills of granite boulders are a common feature of the landscape on the Deccan plateau. Hyd Rock Formations1.jpg
Rock formations at Hyderabad, Telangana Hills of granite boulders are a common feature of the landscape on the Deccan plateau.
Deccan Traps in Maharashtra Deccan Traps Matheran.jpg
Deccan Traps in Maharashtra

The Deccan plateau is a topographically variegated region located south of the Gangetic plains-the portion lying between the Arabian Sea and the Bay of Bengal-and includes a substantial area to the north of the Satpura Range, which has popularly been regarded as the divide between northern India and the Deccan. The plateau is bounded on the east and west by the Ghats, while its northern extremity is the Vindhya Range. The Deccan's average elevation is about 2,000 feet (600 m), sloping generally eastward; its principal rivers, the Godavari, Krishna, and Kaveri, flow from the Western Ghats eastward to the Bay of Bengal.

Vindhya Range mountain range

The Vindhya Range is a complex, discontinuous chain of mountain ridges, hill ranges, highlands and plateau escarpments in west-central India.

The Western Ghats mountain range is very tall and blocks the moisture from the southwest monsoon from reaching the Deccan Plateau, so the region receives very little rainfall. [7] [8] The eastern Deccan Plateau is at a lower elevation spanning the southeastern coast of India. Its forests are also relatively dry but serve to retain the rain to form streams that feed into rivers that flow into basins and then into the Bay of Bengal. [2] [9]

Most Deccan plateau rivers flow south. Most of the northern part of the plateau is drained by the Godavari River and its tributaries, including the Indravati River, starting from the Western Ghats and flowing east towards the Bay of Bengal. Most of the central plateau is drained by the Tungabhadra River, Krishna River and its tributaries, including the Bhima River, which also run east. The southernmost part of the plateau is drained by the Kaveri River, which rises in the Western Ghats of Karnataka and bends south to break through the Nilgiri Hills at the island town of Shivanasamudra and then falls into Tamil Nadu at Hogenakal Falls before flowing into the Stanley Reservoir and the Mettur Dam that created the reservoir, and finally emptying into the Bay of Bengal. [10]

On the western edge of the plateau lie the Sahyadri, the Nilgiri, the Anaimalai and the Elamalai Hills, commonly known as Western Ghats. The average height of the Western Ghats, which run along the Arabian Sea, goes on increasing towards the south. Anaimudi Peak in Kerala, with a height of 2,695 m above sea level, is the highest peak of peninsular India. In the Nilgiris lie Ootacamund, the well-known hill station of southern India. The western coastal plain is uneven and swift rivers flow through it that forms beautiful lagoons and backwaters, examples of which can be found in the state of Kerala. The east coast is wide with deltas formed by the rivers Godavari, Mahanadi and Kaveri. Flanking the Indian peninsula on the western side are the Lakshadweep Islands in the Arabian Sea and on the eastern side lies the Andaman and Nicobar Islands in the Bay of Bengal.

The eastern Deccan plateau, called Telangana and Rayalaseema, is made of vast sheets of massive granite rock, which effectively traps rainwater. Under the thin surface layer of soil is the impervious gray granite bedrock. It rains here only during some months.

Comprising the northeastern part of the Deccan Plateau, the Telangana Plateau has an area of about 148,000 km2, a north-south length of about 770 km, and an east-west width of about 515 km.

The plateau is drained by the Godavari River taking a southeasterly course; by the Krishna River, which divides the peneplain into two regions; and by the Pennai Aaru River flowing in a northerly direction. The plateau's forests are moist deciduous, dry deciduous, and tropical thorn.

Most of the population of the region is engaged in agriculture; cereals, oilseeds, cotton, and pulses (legumes) are the major crops. There are multipurpose irrigation and hydroelectric-power projects, including the Pochampad, Bhaira Vanitippa, and Upper Pennai Aaru. Industries (located in Hyderabad, Warangal, and Kurnool) produce cotton textiles, sugar, foodstuffs, tobacco, paper, machine tools, and pharmaceuticals. Cottage industries are forest-based (timber, firewood, charcoal, bamboo products) and mineral-based (asbestos, coal, chromite, iron ore, mica, and kyanite).

Having once constituted a segment of the ancient continent of Gondwanaland, this land is the oldest and most stable in India. The Deccan plateau consists of dry tropical forests that experience only seasonal rainfall.


The climate of the region varies from semi-arid in the north to tropical in most of the region with distinct wet and dry seasons. Rain falls during the monsoon season from about June to October. March to June can be very dry and hot, with temperatures regularly exceeding 40 °C. The plateau's climate is drier than that on the coasts and is arid in places. Although sometimes used to mean all of India south of the Narmada River, the word Deccan relates more specifically to that area of rich volcanic soils and lava-covered plateaus in the northern part of the peninsula between the Narmada and Krishna rivers.

The Deccan Traps

The northwestern part of the plateau is made up of lava flows or igneous rocks known as the Deccan Traps. The rocks are spread over the whole of Maharashtra and parts of Gujarat and Madhya Pradesh, thereby making it one of the largest volcanic provinces in the world. It consists of more than 2,000 metres (6,600 ft) of flat-lying basalt lava flows and covers an area of nearly 500,000 square kilometres (190,000 sq mi) in west-central India. Estimates of the original area covered by the lava flows are as high as 1,500,000 square kilometres (580,000 sq mi). The volume of basalt is estimated to be 511,000 cubic km. The thick dark soil (called silt) found here is suitable for cotton cultivation.


The volcanic basalt beds of the Deccan were laid down in the massive Deccan Traps eruption, which occurred towards the end of the Cretaceous period between 67 and 66 million years ago. Some paleontologists speculate that this eruption may have accelerated the extinction of the dinosaurs. Layer after layer was formed by the volcanic activity that lasted many thousands of years, and when the volcanoes became extinct, they left a region of highlands with typically vast stretches of flat areas on top like a table. The volcanic hotspot that produced the Deccan traps is hypothesized to lie under the present day island of Réunion in the Indian Ocean. [11]

Typically the Deccan Plateau is made up of basalt extending up to Bhor Ghat near Karjat. This is an extrusive igneous rock. Also in certain sections of the region, we can find granite, which is an intrusive igneous rock. The difference between these two rock types is: basalt rock forms on eruption of lava, that is, on the surface (either out of a volcano, or through massive fissures—as in the Deccan basalts—in the ground), while granite forms deep within the Earth. Granite is a felsic rock, meaning it is rich in potassium feldspar and quartz. This composition is continental in origin (meaning it is the primary composition of the continental crust). Since it cooled relatively slowly, it has large visible crystals. Basalt, on the other hand, is mafic in composition—meaning it is rich in pyroxene and, in some cases, olivine, both of which are Mg-Fe rich minerals. Basalt is similar in composition to mantle rocks, indicating that it came from the mantle and did not mix with continental rocks. Basalt forms in areas that are spreading, whereas granite forms mostly in areas that are colliding. Since both rocks are found in the Deccan Plateau, it indicates two different environments of formation.

The Deccan is rich in minerals. Primary mineral ores found in this region are mica and iron ore in the Chhota Nagpur region, and diamonds, gold and other metals in the Golconda region.


The large areas of remaining forest on the plateau are still home to a variety of grazing animals from the four-horned antelope (Tetracerus quadricornis), [10] chinkara (Gazella bennettii), [10] and blackbuck (Antilope cervicapra) to the large gaur and wild water buffalo (Bubalus arena).


The Deccan is home to many languages and people. Bhil and Gond people live in the hills along the northern and northeastern edges of the plateau, and speak various languages that belong to both the Indo-Aryan and Dravidian families of languages. Marathi, an Indo-Aryan language, is the main language of the north-western Deccan in the state of Maharashtra. Speakers of Telugu and Kannada, the predominant languages of Andhra Pradesh, and Karnataka respectively, occupy those states' portions of the plateau. The city of Hyderabad is an important center of the Urdu language in the Deccan; its surrounding areas also host a notable population of Urdu speakers. The Urdu dialect spoken in this region is also known as Dakhini or as Deccani, named after the region itself. Northeastern parts of the Deccan are in the state of Odisha. Odia, another Indo-Aryan language, is spoken in this part of Deccan.

The chief crop is cotton; also common are sugarcane, rice, and other crops.

Apart from the states already mentioned, the state of Chhattisgarh is found in the northeast corner of the plateau. The large cities in the Deccan are Hyderabad, the capital of Andhra Pradesh and Telangana, Bangalore, the capital of Karnataka, Pune, the cultural hub of Maharashtra and Nagpur, the winter capital of Maharashtra . Other major cities include Mysore, Gulbarga and Bellary in Karnataka; Satara, Amravati, Akola, Kolhapur, Latur, Nanded, Sangli, and Aurangabad in Maharashtra; Amaravati, Visakhapatnam, Kurnool, Anantapur, Rajahmundry, Eluru, in Andhra Pradesh; and Warangal, Karimnagar, Ramagundam, Nizamabad, Siddipet, Jammikunta, Mahbubnagar in present Telangana.


The Deccan produced some of the most significant dynasties in Indian History like the Chola dynasty, Pallavas, The Tondaiman, Satavahana dynasty, Vakataka dynasty, Kadamba dynasty, Chalukya dynasty, Rashtrakuta dynasty, Western Chalukya Empire, Vijayanagara Empire and Maratha Empire. Of the early history, the main facts established are the growth of the Mauryan empire (300 BC) and after that the Deccan was ruled by the Satavahana dynasty which protected the Deccan against the Scythian invaders, the Western Satraps. [12] Prominent dynasties of this time include the Cholas (3rd century BC to 12th century AD), Chalukyas (6th to 12th centuries), Rashtrakutas (753–982), Hoysalas (10th to 14th centuries), Kakatiya (1083 to 1323 AD) and Vijayanagara Empire (1336–1646). Ahir Kings once ruled over the Deccan. A cave inscription at Nasik refers to the reign of an Abhira prince named Ishwarsena, son of Shivadatta. [13] After the collapse of the Satavahana dynasty the Deccan was ruled by the Vakataka dynasty from the 3rd century to 5th century.

From the 6th to 8th century the Deccan was ruled by the Chalukya dynasty which produced great rulers like Pulakesi II who defeated the north India Emperor Harsha or Vikramaditya II whose general defeated the Arab invaders in the 8th century. From the 8th to 10th century the Rashtrakuta dynasty ruled this region. It led successful military campaigns into northern India and was described by Arab scholars as one of the four great empires of the world. [14] In the 10th century the Western Chalukya Empire was established which produced scholars like the social reformer Basava, Vijñāneśvara, the mathematician Bhāskara II and Someshwara III who wrote the text Manasollasa. From the early 11th century to the 12th century the Deccan Plateau was dominated by the Western Chalukya Empire and the Chola dynasty. [15] Several battles were fought between the Western Chalukya Empire and the Chola dynasty in the Deccan Plateau during the reigns of Raja Raja Chola I, Rajendra Chola I, Jayasimha II, Someshvara I and Vikramaditya VI and Kulottunga I. [16]

In 1294, Alauddin Khalji, emperor of Delhi, invaded the Deccan, stormed Devagiri, and reduced the Yadava rajas of Maharashtra to the position of tributary princes (see Daulatabad), then proceeding southward to conquer the Andhra, Carnatic. In 1307, a fresh series of Muslim incursions led by Malik Kafur began in response to unpaid tributes, resulting in the final ruin of the Yadava power; and in 1338 the conquest of the Deccan was completed by Sultan Muhammad bin Tughluq. The imperial hegemony was brief, as soon Andhra and Karnataka reverted to their former masters. These defections by the Hindu states was soon followed by a general revolt of the Muslim governors, resulting in the establishment in 1347 of the independent Muslim dynasty of Bahmani. [17] The power of the Delhi sultanate evaporated south of the Narmada River. The southern Deccan came under the rule of the famous Vijayanagara Empire which reached its zenith during the reign of Emperor Krishnadevaraya. [18]

In the power struggles which ensued, the Hindu kingdom of Karnataka fell bit by bit to the Bahamani dynasty, who advanced their frontier to Golkonda in 1373, to Warangal in 1421, and to the Bay of Bengal in 1472. Krishnadevaraya of the Vijayanagara Empire defeated the last remnant of Bahmani Sultanate power after which the Bahmani Sultanate collapsed. [19] When the Bahmani empire dissolved in 1518, its dominions were distributed into the five Muslim states of Golkonda, Bijapur, Ahmednagar, Bidar and Berar, giving rise to the Deccan sultanates. [17] South of these, the Hindu state of Carnatic or Vijayanagar still survived; but this, too, was defeated, at the Battle of Talikota (1565) by a league of the Muslim powers. Berar had already been annexed by Ahmednagar in 1572, and Bidar was absorbed by Bijapur in 1619. Mughal interest in the Deccan also rose at this time. Partially incorporated into the Empire in 1598, Ahmadnagar was fully annexed in 1636; Bijapur in 1686, and Golkonda in 1687.

In 1645, Shivaji laid the foundation of the Maratha Empire. The Marathas under Shivaji directly challenged the Bijapur Sultanate and ultimately the mighty Mughal empire. Once the Bijapur Sultanate stopped being a threat to the Maratha Empire, Marathas became much more aggressive and began to frequently raid Mughal territory. These raids however angered the Mughal Emperor Aurangzeb and by 1680 he moved his capital from Delhi to Aurangabad in Deccan to conquer maratha held territories. After Shivaji died, his son Sambhaji defended the Maratha empire from the Mughal onslaught but he was captured by the Mughals and executed. By 1698 the last Maratha stronghold at Jinji fell and Mughals now controlling all maratha held territories.

In 1707, Emperor Aurangzeb died of sickness at the age of 89 and this allowed Marathas to reacquired their lost territories and established their authority in much of modern Maharashtra. After the death of Chhatrapati Shahu, the Peshwas became the de facto leaders of the Empire from 1749 to 1761, while Shivaji's successors continued as nominal rulers from their base in Satara. The Marathas kept the British at bay during the 18th century. By 1760, with the defeat of the Nizam in the Deccan, Maratha power had reached its zenith. However, dissension between the Peshwa and their sardars (army commanders) saw a gradual downfall of the Empire leading to its eventual annexation by the British East India Company in 1818 after the three Anglo-Maratha wars.

A few years later, Aurangzeb's viceroy in Ahmednagar, Nizam-ul-Mulk, established the seat of an independent government at Hyderabad in 1724. Mysore was ruled by Hyder Ali. During the contests for power which ensued from about the middle of the 18th century between the powers on the plateau, the French and British took opposite sides. After a brief course of triumph, the interests of France declined, and a new empire in India was established by the British. Mysore formed one of their earliest conquests in the Deccan. Tanjore and the Carnatic were soon annexed to their dominions, followed by the Peshwa territories in 1818.

In British India, the plateau was largely divided between the presidencies of Bombay and Madras. The two largest native states at that time were Hyderabad and Mysore; many smaller states existed at the time, including Kolhapur, and Sawantwari.

After independence in 1947, almost all native states were incorporated into the Republic of India. The Indian Army occupied Hyderabad in Operation Polo in 1948 when it refused to join. [20] In 1956, the States Reorganisation Act reorganized states along linguistic lines, leading to the states currently found on the plateau.


The Deccan plateau is very rich in minerals and precious stones. [21] The plateau’s mineral wealth led many lowland rulers, including those of the Mauryan (4th–2nd century BCE) and Gupta (4th–6th century CE) dynasties, to fight over it. [22] Major minerals found here include coal, iron ore, asbestos, chromite, mica, and kyanite. Since March 2011, large deposits of uranium have been discovered in the Tummalapalle belt and in the Bhima basin at Gogi in Karnataka. The Tummalapalle belt uranium reserve promises to be one of the top 20 uranium reserve discoveries of the world. [23] [24] [25]

Low rainfall made farming difficult until the introduction of irrigation. Currently, the area under cultivation is quite low, ranging from 60% in Maharashtra to about 10% in Western Ghats. [26] Except in developed areas of certain river valleys, double-cropping is rare. Rice is the predominant crop in high-rainfall areas and sorghum in low-rainfall areas. Other crops of significance include cotton, tobacco, oilseeds, and sugar cane. Coffee, tea, coconuts, areca, pepper, rubber, cashew nuts, tapioca, and cardamom are widely grown on plantations in the Nilgiri Hills and on the western slopes of the Western Ghats. Cultivation of Jatropha has recently received more attention due to the Jatropha incentives in India.


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  6. Richard M. Eaton 2005, p. 2.
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  10. 1 2 3 Wikisource-logo.svg Chisholm, Hugh, ed. (1911). "India"  . Encyclopædia Britannica . 14 (11th ed.). Cambridge University Press. pp. 375–421.
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  18. Richard M. Eaton 2005, p. 83.
  19. Richard M. Eaton 2005, p. 88.
  20. Benichou, Lucien D. (2000). From Autocracy to Integration: Political Developments in Hyderabad State (1938—1948), p. 232. Chennai: Orient Longman Limited.
  21. Ottens, Berthold (1 January 2003). "Minerals of the Deccan Traps, India". HighBeam Research. Archived from the original on 11 September 2016. Retrieved 8 August 2016.
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  23. Subramanian, T. S. (20 March 2011). "Massive uranium deposits found in Andhra Pradesh". news. Chennai, India: The Hindu. Retrieved 8 August 2016.
  24. Thakur, Monami (19 July 2011). "Massive uranium deposits found in Andhra Pradesh". International Business Times. USA.
  25. Bedi, Rahul (19 July 2011). "Largest uranium reserves found in India". The Telegraph. New Delhi, India.
  26. "Peninsular India". ita. September 1995. Retrieved 8 August 2016.

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Gulbarga City in Karnataka, India

Gulbarga, also known as Kalaburagi, is a city in the Indian state of Karnataka, India. It is the administrative headquarters of the Gulbarga district and a major city of the North Karnataka region. Gulbarga is 623 km north of the state capital city of Bangalore and 220 km from Hyderabad. Previously it was part of Hyderabad State and incorporated into a newly formed Mysore State through the States Reorganisation Act in 1956.

Beginning in the 13th century, several Islamic states were established in the Indian subcontinent in the course of a gradual Muslim conquest in the Indian subcontinent. This process culminated in the Mughal Empire, which ruled most of India during the mid-16th to early-18th centuries. The Islamic rule gradually declined due to the dominance of Maratha Empire, Kshatriya's and several other rebellions. The eventual end of the period of Islamic rule of India is marked by the two main events Indian Rebellion of 1857 and the beginning of British rule, although Islamic rule persisted in Hyderabad State and other minor princely states until Union of India in 1948. However, most Islamic rules had started to wane in the 17th and 18th century before that.

Dakhini or Dakkhani, also spelled Dakkani, Dakhni and Deccani (dec-ca-ni), is an Indo-Aryan language spoken in southern India. It arose as a language of the Deccan sultanates ca. 1300 AD in ways similar to Urdu. It is similar to Urdu in its influence from Arabic and Persian with a Prakrit base, but differs because of the strong influence of Marathi, Telugu and Kannada spoken in the states of Maharashtra, Telangana, Andhra Pradesh, Karnataka and a few muslims in Tamil Nadu. This dialect has a rich and extensive literary heritage. The dialect is today only spoken in Deccan. Dakhini is the native language of the Dakhini Muslims.

Carnatic region

The Carnatic region is the region of peninsular South India lying between the Eastern Ghats and the Western Ghats, in the modern Indian states of Karnataka, Tamil Nadu and southern Andhra Pradesh.

History of South India

The history of South India covers a span of over four thousand years during which the region saw the rise and fall of a number of dynasties and empires. The period of known history of the region begins with the Iron age period until the 14th century CE. Dynasties of Satavahana, Chola, Chera, Pandyan, Chalukya, Pallava, Rashtrakuta, Kakatiya, Seuna (Yadava) dynasty and Hoysala were at their peak during various periods of history. These Dynasties constantly fought amongst each other and against external forces when Muslim armies invaded south India. Vijayanagara empire rose in response to the Muslim intervention and covered the most of south India and acted as a bulwark against Mughal expansion into the south. When the European powers arrived during the 16th century CE, the southern kingdoms resisted the new threats, and many parts eventually succumbed to British occupation. The British created the Madras Presidency which covered most of south India directly administered by the British Raj, and divided the rest into a number of dependent princely states. After Indian independence South India was linguistically divided into the states of Andhra Pradesh, Karnataka, Kerala and Tamil Nadu.

The Raichur Doab is a Doab, in this case the triangular region of land in the southern Indian states of Telangana and Karnataka lying between the Krishna River and its tributary, the Tungabhadra River. The doab is named for the town of Raichur in the Raichur District. The Raichur Doab is considered to be very fertile because of the sediments carried by Krishna & Tungabhadra rivers. The doab includes Raichur district and Koppal district in Karnataka, and Gadwal district in Telangana. Some areas of Raichur doab also called as Nadigadda region became a part of Telangana during Andhra Pradesh Reorganisation Act in 2014.Those areas are Gadwal, Alampur and Maganoor. Gadwal is one of the 31 districts of Telangana State.

Raichur district District in Karnataka, India

Raichur District is an administrative district in the Indian state of Karnataka. It is located in the northeast part of the state and is bounded by Yadgir district in the north, Bijapur and Bagalkot district in the northwest, Koppal district in the west, Bellary district in the south, Mahabubnagar district of Telangana and Kurnool district of Andhra Pradesh in the east.

Medieval India refers to a long period of the history of the Indian subcontinent between the "ancient period" and "modern period". Definitions of the period itself vary widely, and partly for this reason, many historians now prefer to avoid the term completely.

North Karnataka Place in Karnataka, India

North Karnataka officially known as Uttara Karnataka is a geographical region consisting of mostly semi-arid plateau from 300 to 730 metres elevation that constitutes the northern part of the South Indian state of Karnataka. It is drained by the Krishna River and its tributaries the Bhima, Ghataprabha, Malaprabha, and Tungabhadra. North Karnataka lies within the Deccan thorn scrub forests ecoregion, which extends north into eastern Maharashtra.

History of Karnataka

The recorded history of Karnataka goes back more than two millennia. Several great empires and dynasties have ruled over Karnataka and have contributed greatly to the history, culture and development of Karnataka

History of Andhra Pradesh

Andhra Pradesh is one of the 29 states of India whose recorded history begins in the Vedic period. It is mentioned in Sanskrit epics such as Aitareya Brahmana. The Assaka Mahajanapada was an ancient kingdom located between the Godavari and Krishna Rivers in southeastern India. Accounts that people in the region are descended from the sage Viswamitra are found in the Ramayana, the Mahabharata and the Puranas.

Political history of medieval Karnataka

The political history of medieval Karnataka spans the 4th to the 16th centuries, when the empires that evolved in the Karnataka region of India made a lasting impact on the subcontinent. Before this, alien empires held sway over the region, and the nucleus of power was outside modern Karnataka. The medieval era can be broadly divided into several periods: The earliest native kingdoms and imperialism; the successful domination of the Gangetic plains in northern India and rivalry with the empires of Tamilakam over the Vengi region; and the domination of the southern Deccan and consolidation against Muslim invasion. The origins of the rise of the Karnataka region as an independent power date back to the fourth-century birth of the Kadamba Dynasty of Banavasi, the earliest of the native rulers to conduct administration in the native language of Kannada in addition to the official Sanskrit. This is the historical starting point in studying the development of the region as an enduring geopolitical entity and of Kannada as an important regional language.

Srinivas Saradagi is a village in the southern state of Karnataka, India. It is located in the Gulbarga taluk of Gulbarga district in Karnataka.


Prabalgad is located between Matheran and Panvel and comes under the Raigad District in the state of Maharashtra, India.

Belgaum Fort

Belagavi Fort or Belgaum Fort is in the city of Belagavi, in the Belagavi district, in Karnataka state, India. It was begun by Jaya Raya, also called Bichi Raja, an ally of the Ratta Dynasty, in the year 1204 AD. It has undergone several renovations over the centuries under dynastic rulers of the region.

Gulbarga Fort

The Gulbarga Fort is located in Gulbarga City in the Gulbarga district of North Karnataka. It was subsequently significantly enlarged in 1347 by Al-ud-din Hasan Bahmani of the Bahmani Dynasty after he cut off his ties with the Delhi Sultanate; Islamic monuments such as mosques, palaces, tombs, and other structures were also built later within the refurbished fort. The Jama Masjid built later, within the fort, in 1367, is a unique structure built in Persian architectural style, fully enclosed, with elegant domes and arched columns, which is unlike any other mosque in India. It was built to commemorate the establishment of the dynastic rule of the Bahmani kingdom at Gulbarga fort between 1327 and 1424. It remained the capital of the Bahmani Kingdom till 1424 where after the capital was shifted to Bidar Fort, as Bidar had better climatic conditions.

Maharashtra is a state in the western region of India and is India's second-most populous state and third-largest state by area. Although the present day state in India was only formed in 1960,the region that comprises the state has a long history dating back to the 4th century BCE.

History of Hyderabad

Hyderabad is the capital of the Indian state of Telangana. It is a historic city noted for its many monuments, temples, mosques and bazaars. A multitude of influences has shaped the character of the city in the last 400 years.

Bidar is a historic place located in the north-eastern part of the South Indian state of Karnataka. Bidar enjoys a picturesque situation, having been situated and built on the brink of a plateau, and thus commanding lovely views of the lowlands (talghat) towards the north and the east. Its latitude is 17°55'N., its longitude 77°32' E., and the height above the sea-level 2,330 feet (710 m). The climate is bracing and the temperature in the hottest season does not usually rise above 105 °F (41 °C). The Bidar plateau is an irregular oblong, 22 miles (35 km) in length and 12 miles (19 km) in extreme breadth.


Coordinates: 17°N77°E / 17°N 77°E / 17; 77