1826 and 1829. In 1837, Bhuj is said to have had a population of 30,000, including 6,000 Muslims. After independence of India in 1947, Kutch State acceded unto the dominion of India and was constituted an independent commissionaire, Kutch State. In 1956, Kutch State was merged with Bombay state, which in 1960 was divided into the new linguistic states of Gujarat and Maharashtra, with Kutch becoming part of Gujarat state as Kutch district. Bhuj is the district headquarters of Kutch District, the largest district in India. On 21 July 1956 as well as on 26 January 2001, the city suffered great losses of life and property due to earthquakes. Many parts of Bhuj were demolished due to the extensive damage, whilst others were repaired. There has been great progress in rebuilding the City since the 2001 earthquake, with considerable improvements to roads, transportation, and infrastructure. Bhuj is home to one of the first Swaminarayan Sampraday temples, built in 1822. Bhuj temple is one of the six original temples built during the earthly presence of the Lord Swaminarayan. The devotees living in Bhuj including Gangaram Mull, Sundarji Suthar and Hirji Suthar requested Lord to construct a temple at Bhuj. Lord instructed Vaishnavanand Swami to construct the temple, and Lord himself installed the murti of Lord NarNarayan Dev in Bhuj on VS 1879 on the 5th day of the bright half of the month of Vaishakh (Friday 15 May 1823 AD). Geography Bhuj has an average elevation of 110 metres (360 feet). On the eastern side of the city is a hill known as Bhujia Hill, on which there is a Bhujia Fort, that separates Bhuj city and Madhapar town ( considered one of the richest villages in Asia ). It has two lakes namely Hamirsar and Deshadsar (દેેેશળસર). Climate Bhuj has a borderline hot desert climate (Köppen BWh) just short of a hot semi-desert climate (BSh). Although annual rainfall "averages" around the variability is among the highest in the world with coefficient of variation of around sixty per cent – among the few comparably variable climates in the world being the Line Islands of Kiribati, the Pilbara coast of Western Australia, the sertão of Northeastern Brazil, and the Cape Verde islands. Recorded annual rainfall has been as low as in 1899 – yet in 1926 a total of fell and in the incomplete year of 1959 rainfall exceeded , of which