Editing Meghalaya

'''Meghalaya''', alongside neighbouring Indian states, has been of archaeological interest. People have lived in Meghalaya since the Neolithic period. Neolithic sites discovered so far are located in areas of high elevation in Khasi Hills, Garo Hills and in neighbouring states, where Neolithic style jhum or shifting cultivation is practiced even today. The highland plateaus fed by abundant rains provided safety from floods and a rich soil.The importance of Meghalaya is its possible role in human history via domestication of rice. One of the competing theories for the origin of rice comes from Ian Glover, who states, "India is the center of greatest diversity of domesticated rice with over 20,000 identified species and Northeast India is the most favorable single area of the origin of domesticated rice." The limited archaeology done in the hills of Meghalaya suggest human settlement since ancient times.

After the Conquest of Taraf in 1304, Shah Arifin Rafiuddin, a disciple of Shah Jalal, migrated and settled in the Khasi and Jaintia Hills where he preached Islamic monotheism to the local people. His khanqah remains in Sarping / Laurergarh on the Bangladeshi border but the part containing his mazar is in Meghalaya on top of Laur Hill. Bhaitbari is an archaeological site first discovered and excavated by A. K. Sharma in 1993, a fortification of burnt brick with mud core was discovered at Meghalaya - Assam border and is dated to 4th-8th century AD, the city has been speculated to have been one of the capital cities of Kamarupa.

The Khasi, Garo, and Jaintia tribes had their own kingdoms until they came under British administration in the 19th century. Later, the British incorporated Meghalaya into Assam in 1835.The region enjoyed semi-independent status by virtue of a treaty relationship with the British Crown. When Bengal was partitioned on 16 October 1905 by Lord Curzon, Meghalaya became a part of the new province of Eastern Bengal and Assam. When the partition was reversed in 1912, Meghalaya became a part of the province of Assam. On 3 January 1921 in pursuance of Section 52A of the Government of India Act of 1919, the governor-general-in-council declared the areas now in Meghalaya, other than the Khasi states, as "backward tracts." Subsequently, the British administration enacted the Government of India Act 1935, which regrouped the backward tracts into two categories: "excluded" and "partially excluded" areas.Meghalaya is one of the Seven Sister States of northeast India. The state of Meghalaya is mountainous, with stretches of valley and highland plateaus, and it is geologically rich. It consists mainly of Archean rock formations. These rock formations contain rich deposits of valuable minerals like coal, limestone, uranium and sillimanite. The name Meghalaya was given by Shiba P. Chatterjee, a geography professor at Kolkata University.

Meghalaya has many rivers. Most of these are rainfed and seasonal. The important rivers in the Garo Hills region are Ganol, Daring, Sanda, Bandra, Bugai, Dareng, Simsang, Nitai and the Bhupai. In the central and eastern sections of the plateau, the important rivers are Khri, Umtrew, Digaru, Umiam or Barapani, Kynshi (Jadukata), Umngi, Mawpa, Umiam Khwan, Umngot, Umkhen, Myntdu and Myntang. In the southern Khasi Hills region, these rivers have created deep gorges and several waterfalls.