Clockwise from top: Curzon Gate, Nava Kailash temple at Kalna, Sita-Rama Temple in Ukhra, Damodar River, Radhamadhab Temple in Khandra, 108 Shiva Temple at Nababhat
Historians link the name of the district to the 24th and last Jaintirthankara, Mahavira Vardhamana, who came to preach in the area. A Jain image is in the collection of Vidyasagar Mandir in the Midnapur town. A Jaina brass plaque has been found from a place very close to Katwa (Burdwan district). Jaina figures of rare artistic quality have been discovered in the place.[5]
Quite a large number of the mutilated sculptures representing Jaina Tirthankara were noticed within the enclosure of the brick temple of Satdeulia in Burdwan district.[6]
History
During the period of Jahangir this place was named Badh-e-dewan (district capital). The city owes its historical importance to being the headquarters of the Maharajas of Burdwan, the premier noblemen of lower Bengal, whose rent-roll was upwards of 300,000. Archaeological excavations/ findings at Pandu Rajar Dhibi and Birbhanpur have indicated settlements in the Ajay and Damodar valleys in the Mesolithic age, around 5,000 BC. Not much is known about the early settlements and the period that followed till around 700 BC in ancient times when the area was referred to as Bardhamanbhukti, which was a part of the Rarh region. It was one of the sixteen janapad (In ancient times, districts were called Janapadas ) of ancient India. Large and powerful empires such as the Magadhas, Mauryas, Kushanas and Guptas held sway over the area and beyond it. In the 7th century AD, the area was part of the Gauda Kingdom, then ruled by Shashanka. It was subsequently ruled by the Palas and Senas, till Bakhtiyar Khilji captured it in 1199 AD.[7][8]
The early Muslim rulers ruled over major parts of Bengal from Gauda or Lakhnauti. In the Mughal period Bardhaman is mentioned as a mahal or pargana of Sarcar Sharifabad. Some western parts of Bardhaman was Gopbhum, ruled for many years by the Sadgope kings. The Gopbhum area later became part of the Shergarh and Senpahari parganas.[7][8]
In 1606, Sher Afghan, the jagirdar of Bardhaman, was killed just outside Bardhaman. After Sher Afghan's death, his wife, Meher-un-Nissa, was taken by Jahangir as his consort, and named Nur Jahan. It was one of the most romantic chapters of Mughal history. In 1622, when Jahangir's son, Khurram, who later became Shah Jahan, rebelled against his father, he captured the fort of Bardhaman.[8][7]
In 1689, Raja Krishnaram Roy, of the Bardhaman Raj family, obtained a farman (royal decree) from Aurangzeb by which he was made the zamindar (landlord) of Bardhaman, and since then the Raj family's history became identical with that of the district. During the reign of Krishnaram Rai, Subha Singh, zamindar of Chitua and Barda, then part of Bardhaman, raised the standard of revolt in 1696. He was killed by Rajkumari Satyabati, when he tried to outrage her. Kirti Chandra Rai added the parganas of Chitua, Bhurshut, Barda and Manoharshahsi to his territories. He also seized the estates of the Raja of Belghara and attacked and defeated the powerful Raja of Bishnupur. Chitra Sen Ray was conferred the title of Raja by the Mughal emperor in 1740. He was succeeded by Tilakchand Ray, who was also conferred the title of Raja by the Mughal emperor. It was during his rule that East India Company acquired Bardhaman and other areas of Bengal.[7][8]
After the death of Aurangzeb, the Mughal Empire became weak and Murshid Quli Khan became the Nawab of Bengal, owning only nominal allegiance to the Mughal emperor. At that time Bardhaman was referred to as chakla, a change from the earlier pargana. Subsequently, during the reign of Alivardi Khan, the Bargis attacked and plundered Bardhaman.[7][8]
After the victory of the British in the Battle of Plassey in 1757, the fertile district of Bardhaman, along with Medinipur and Chittagong, was ceded to the East India Company. In 1857, the British Crown took over the administration of the country from the East India Company.[7][8]
In 1765, when East India Company acquired the diwani of Bardhaman, it was composed of Bardhaman, Bankura, Hooghly and a third of Birbhum. Hooghly was separated in 1820, Bankura and Birbhum in 1837. In 1765, Tilakchand Ray was the zamindar of Bardhaman. He controlled 75 parganas and also looked after the law and order. At the time of the Permanent Settlement of Lord Cornwallis in 1793, the chaklas were reduced in size, in order to make them more manageable, and districts were created. Six subdivisions were created in Bardhaman district – Bud Bud in 1846, Katwa, Raniganj, Jahanabad (later named Arambagh), and Bardhaman Sadar in 1847 and Kalna in 1850. The parganas were converted to thanas (police stations). At that time there were 22 thanas in Bardhaman district. Later, Jahanabad was transferred out of Bardhaman. Some minor changes went on taking place.[7][8]
The Permanent Settlement ultimately led to the dismemberment of the Bardhaman estate. As the rajas often failed to pay the rent demands, some parts of the estate were auctioned off. However, there were bright spots. Mahatabchand was appointed additional member of the Viceroy’s Executive Council and in 1877 was allowed to use the title of His Highness before his name. Bijoy Chand Mahatab was conferred the title of Maharajadhiraj by Lord Minto in 1908. Uday Chand Mahtab took over in 1941 and served till abolition of the zamindary system in 1954, after independence of the country.[7][8]
Burdwan district with its varied tectonic elements and riverine features, is a transitional zone between the Jharkhand plateau which constitutes a portion of peninsular shield in the west and Ganga-Brahmaputra alluvial plain in the north and east. In general the Jharkhand plateau consists of the metasedimentary rocks of precambrian age, Gondwana sedimentary rocks, Rajmahal basalts and upper tertiary sediments. Laterite has developed on these older rocks as well as on early Quaternary sediments. To the south, the alluvial plain merges with Damodar-kasain-Subarnarekha deltaic plains. The western half of the district resembles a promontory jutting out from the hill ranges of Chotonagpur plateau and consists of barren, rocky and rolling country with a laterite soil rising into rocky hillocks, the highest being 227 m. These diversify the otherwise monotonous landscape and lend a special charm to the skyline around Asansol subdivision. Ajoy-barakar divide is a convex plateau, the average altitude being 150 m. The gradient is westerly to the west and to the east it is northerly toward
Ajay and southerly toward Damodar below the latitude. The Ajoy-Damodar inter-stream tract is made up of several stows consisting of vales and low convex spurs which run in almost all directions except northeast and thus lends a very complicated character to local relief.[12]
Rivers
The river system in Burdwan includes the Bhagirathi-Hooghly in the east, the Ajoy and its tributaries in the north, and the Dwarakeswar, the Damodar and its branches in the southwest. Besides, there are innumerable Khals and old riverbeds all over the area. The notable rivers and khals are Damodar, Bhagirathi, Barakar, Ajay, Dwarakeswar, Nonia, Singaram, Tamla, Kukua, Kunur, Tumuni, Khari, Banka, Chanda-kanki nala, Behula, Gangur, Brahmani, Khandesvari, Karulia nala, Dwaraka or Babla, Koiya nala, Kandarkahal, Kanadamodar, Kananadi, Ghea, Kakinadi etc.[12]
Soil
Different types of soil are encountered in topographical biological, hydrological, and geological conditions in the Burdwan district. In the west, coarse gritty soil blended with rock fragments is formed from the weathering of pegmatite, quartz veins and conglomeratic sandstones, where as sandy soil characteristic of granite rocks and sandstones. This soil is reddish, medium to coarse in texture, acidic in reaction, low in nitrogen, calcium, phosphate and other plant nutrients. Water holding capacity of this soil increases with depth as well as with the increase of clay portions. Towards the east alluvial soil attains an enormous thickness in the low level plains to the east. These soils are sandy, well drained and slightly acidic.[12]
Minerals
Burdwan was one of the premier districts in India in value of minerals. The Raniganj coalfield was the birthplace of the Indian coal industry. Besides coal, important minerals found in the district are iron ores, calcium carbonate, abrasives, silica bricks and moulding sands, glass sands, building materials, manganese, bauxite, laterite etc.[12]
Water resources
There are many ponds, wells, canals, marshes and burrows all over the district. In the Damodar Valley region, there are around 17000 tanks. The
Durgapur barrage and Mithon dam have formed two large reservoirs at the
southwestern and western periphery of the district.[12]
Forest
The forest areas of the district are chiefly in the lateritic and red soil highlands in the Aushgram PS of Sadar subdivision and in the Asansol subdivision.[12]
The district experiences a climate which is transitional between CWg and AW types, where 'C' stands for 'warm temperate rainy climates with mild winter', 'W' for 'dry winter not compensated for by total rain in the rest of the year', 'g ' for 'eastern Ganges type of temperature trend' and 'AW' for 'tropical savanna climates'. Average temperature in hot season is 30 C while at the cold season is 20 C. Average rainfall is 1496 mm. The cold season starts from about the middle of November and continues till the end of February. March to May is dry summerintervened by tropical cyclones and storms. June to September is wet summer while October and November is autumn.[12]
Demographics
Historical population
Year
Pop.
±% p.a.
1901
1,528,283
—
1911
1,533,868
+0.04%
1921
1,434,766
−0.67%
1931
1,575,694
+0.94%
1941
1,890,726
+1.84%
1951
2,191,660
+1.49%
1961
3,082,617
+3.47%
1971
3,916,174
+2.42%
1981
4,835,388
+2.13%
1991
6,050,605
+2.27%
2001
6,895,514
+1.32%
2011
7,717,563
+1.13%
Note: After 2011, the Bardhaman district was bifurcated into two separate districts namely Purba Bardhaman and Paschim Bardhaman. The census data is addition of two splitted districts. Source: Census of India[13]
^Lalavānī, Gaṇeśa (1997). Jainism in India. Prakrit Bharati Academy.
^ abcdefghChattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), (in Bengali), Vol I, pp 261-370, Radical Impression. ISBN81-85459-36-3
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