Vindhya Range in the context of "Sagar, Madhya Pradesh"

Western India is a loosely defined region of India consisting of western states of Republic of India. The Ministry of Home Affairs in its Western Zonal Council Administrative division includes the states of Goa, Gujarat, and Maharashtra along with the Union territory of Dadra and Nagar Haveli and Daman and Diu, while the Ministry of Culture and some historians also include the state of Rajasthan. The Geological Survey of India includes Maharashtra but excludes Rajasthan whereas Ministry of Minority Affairs includes Karnataka but excludes Rajasthan.

Madhya Pradesh is also often included and Haryana, western Uttar Pradesh and southern Punjab are sometimes included. Western India may also refer to the western half of India, i.e. all the states west of Delhi and Chennai, thus also including Punjab, Kerala and surrounding states. The region is highly industrialised, with a large urban population. Roughly, Western India is bounded by the Thar Desert in the north, the Vindhya Range in the east and north and the Arabian Sea in the west. A major portion of Western India shares the Thar Desert with North India and Pakistan and the Deccan Plateau with South and Central India.

The Deccan Plateau (/ˈdɛkən/ DEK-ən ) is a geographic formation that extends over an area of 422,000 km (163,000 sq mi) on the southern part of the Indian peninsula. It stretches from the Satpura and Vindhya Ranges in the north to the northern fringes of Tamil Nadu in the south. It is bound by the mountain ranges of the Western Ghats and the Eastern Ghats on the sides, which separate the region from the Western and Eastern Coastal Plains respectively. It covers most of the Indian States of Maharashtra, Karnataka, Telangana and Andhra Pradesh excluding the coastal regions, and minor portions of Tamil Nadu and Kerala.

The plateau is marked by rocky terrain with an average elevation of about 600 m (2,000 ft). It is subdivided into Maharashtra Plateau, Karnataka Plateau, and Rayalaseema and Telangana Plateau. The Deccan Traps in the northwest were formed by multiple layers of igneous rock deposited by basaltic lava flows following a massive volcanic eruption occurred at the end of the Cretaceous period (66 mya). The underlying bed consists of granite and sedimentary rocks formed during the Precambrian era and the formation of Gondwana.

Malwa (IPA: [maːlʋaː]) is a historical region of west-central India occupying a plateau of volcanic origin. Geologically, the Malwa Plateau generally refers to the volcanic upland north of the Vindhya Range. Politically and administratively, it is also synonymous with the former state of Madhya Bharat which was later merged with Madhya Pradesh. At present the historical Malwa region includes districts of western Madhya Pradesh and parts of south-eastern Rajasthan. Sometimes the definition of Malwa is extended to include the Nimar region south of the Vindhyas.

The Malwa region had been a separate political unit from the time of the ancient Malava Kingdom, and has been ruled by several kingdoms and dynasties. Malwa continued to be an administrative division until 1947, when the Malwa Agency of British India was merged into Madhya Bharat (also known as Malwa Union) state of independent India.

The Deccan sultanates is a historiographical term referring to five late medieval to early modern Persianate Muslim kingdoms on the Deccan Plateau between the Krishna River and the Vindhya Range. They emerged after the disintegration of the Bahmani Sultanate and were ruled by various dynasties: Ahmadnagar, Berar, Bidar, Bijapur, and Golconda. Ahmadnagar was the first to declare independence, in 1490; followed by Bijapur and Berar in the same year. Bidar became independent in c. 1492, and Golconda in 1512.

Although the five sultanates were all ruled by Muslims, their founders were of diverse origins: the Nizam Shahi dynasty, the ruling family of the Ahmadnagar Sultanate, was founded by Malik Hasan Bahri, a Marathi Muslim of Brahmin origin; the Berar Sultanate by a Kannadiga Muslim of Brahmin origin; the Bidar Sultanate by a Georgian slave; the Bijapur Sultanate by a foreigner who may have been a Georgian slave purchased by Mahmud Gawan; and the Golconda Sultanate by a slave of Iranian Turkmen origin.

Amarkantak (NLK Amarakaṇṭaka) is a pilgrim town and a Nagar Panchayat in Anuppur, Madhya Pradesh, India. The Amarkantak region is a unique natural heritage area. It is the meeting point of the Vindhya and the Satpura Ranges, with the Maikal Hills being the fulcrum. This is where the Narmada River, the Son River and Johilla River (tributary of Son) originate.

15th-century Indian mystic and poet Kabir is said to have meditated in Amarkantak, and the place is now known as Kabir Chabutra.

The Satpura Range (IPA: [sət̪pʊɽaː]), formerly also known as the Seeonee Hills, is a range of hills in central India. The range rises in eastern Gujarat running east through the border of Maharashtra and Madhya Pradesh and ends in Chhattisgarh. The range parallels the Vindhya Range to the north, and these two east–west ranges divide the Indian subcontinent into the Indo-Gangetic Plain of northern India and the Deccan Plateau of the south. The Narmada River originates from the north-eastern end of Satpura in Amarkantak, 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. Multai, the place of Tapti river origin is located about 465 kilometer far, south-westerly to Amarkantak, separated across by the hill 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 the much smaller but parallel Tapi Graben in the south.