The Sarasvati River is a mythologized and deified ancient river first mentioned in the Rigveda and later in Vedic and post-Vedic texts. It played an important role in the Vedic religion, appearing in all but the fourth book of the Rigveda.
The Yamuna is the second-largest tributary river of the Ganges by discharge and the longest tributary in India. Originating from the Yamunotri Glacier at a height of about 4,500 m (14,800 ft) on the southwestern slopes of Bandarpunch peaks of the Lower Himalaya in Uttarakhand, it travels 1,376 kilometres (855 mi) and has a drainage system of 366,223 square kilometres (141,399 sq mi), 40.2% of the entire Ganges Basin. It merges with the Ganges at Triveni Sangam, Prayagraj, which is a site of the Kumbh Mela, a Hindu festival held every 12 years.
The Aravalli Range is a mountain range in Northern-Western India, running approximately 670 km (420 mi) in a south-west direction, starting near Delhi, passing through southern Haryana, Rajasthan, and ending in Ahmedabad Gujarat. The highest peak is Guru Shikhar on Mount Abu at 1,722 m (5,650 ft). The Aravalli Range is one of the oldest geological feature on Earth, having its origin in the Proterozoic era.
The Sutlej River is the longest of the five rivers that flow through the historic crossroads region of Punjab in northern India and Pakistan. The Sutlej River is also known as Satadru. It is the easternmost tributary of the Indus River. The Bhakra Dam is built around the river Sutlej to provide irrigation and other facilities to the states of Punjab, Rajasthan and Haryana.
The Chambal River is a tributary of the Yamuna River in Central and Northern India, and thus forms part of the drainage system of the Ganges. The river flows north-northeast through Madhya Pradesh, running for a time through Rajasthan, then forming the boundary between Rajasthan and Madhya Pradesh before turning southeast to join the Yamuna in Uttar Pradesh state.
Mewar or Mewad is a region in the south-central part of Rajasthan state of India. It includes the present-day districts of Bhilwara, Chittorgarh, Pratapgarh, Rajsamand, Udaipur, Pirawa Tehsil of Jhalawar District of Rajasthan, Neemuch and Mandsaur of Madhya Pradesh and some parts of Gujarat.
The Banas is a river which lies entirely within the state of Rajasthan in western India. It is a tributary of the Chambal River, itself a tributary of the Yamuna, which in turn merges into the Ganga. The Banas is approximately 512 kilometres in length.
The Berach River, a tributary of the Banas River, is a river of Rajasthan state in western India. The river belongs to the Ganga River basin. The Berach originates in the hills of Udaipur district, northeast of Udaipur, and has a length of 157 km and basin area of 7,502 km2. It flows northeast through Udaipur, Chittorgarh and Bhilwara districts, joining the Banas near Bigod village of Bhilwara district.
The Ghaggar-Hakra River is an intermittent river in India and Pakistan that flows only during the monsoon season. The river is known as Ghaggar before the Ottu barrage at 29.4875°N 74.8925°E, and as Hakra downstream of the barrage in the Thar Desert. In pre-Harappan times the Ghaggar was a tributary of the Sutlej. It is still connected to this paleochannel of the Sutlej, and possibly the Yamuna, which ended in the Nara River, presently a delta channel of the Indus River joining the sea via Sir Creek.
Udaipur is a city in the north-western Indian state of Rajasthan. It serves as the administrative headquarters of Udaipur district. It is the historic capital of the kingdom of Mewar in the former Rajputana Agency. It was founded in 1559 by Udai Singh II of the Sisodia clan of Rajputs, when he shifted his capital from the city of Chittorgarh to Udaipur after Chittorgarh was besieged by Akbar. It remained as the capital city till 1818 when it became a British princely state, and thereafter the Mewar province became a part of Rajasthan when India gained independence in 1947. It is also known as the City of Lakes, as it is surrounded by five major artificial lakes.
Pottery in the Indian subcontinent has an ancient history and is one of the most tangible and iconic elements of Indian art. Evidence of pottery has been found in the early settlements of Lahuradewa and later the Indus Valley Civilisation. Today, it is a cultural art that is still practiced extensively in the subcontinent. Until recent times all Indian pottery has been earthenware, including terracotta.
The Ahar culture, also known as the Banas culture is a Chalcolithic archaeological culture on the banks of the Ahar River of southeastern Rajasthan state in India, lasting from c. 3000 to 1500 BCE, contemporary and adjacent to the Indus Valley civilization. Situated along the Banas and Berach Rivers, as well as the Ahar River, the Ahar–Banas people were exploiting the copper ores of the Aravalli Range to make axes and other artefacts. They were sustained on a number of crops, including wheat and barley.
Gilund is a village and an archaeological site located in Rajsamand district of Rajasthan state in western India. It is one of five ancient sites excavated in the Ahar-Banas Complex which also includes the sites of Ahar, Ojiyana, Marmi, and Balathal. Out of the 111 reported sites found in the Ahar-Banas Complex, Gilund is the largest. The archaeological site was named after the present-day village, Gilund, and is locally known as Modiya Magari which means "bald habitation mound".
Balathal is an archaeological site located in Vallabhnagar tehsil of Udaipur district of Rajasthan state in western India. It is one of the ninety Ahar-Banas culture sites located in the Basins of the Banas river and its tributaries.
The Sahibi river, also called the Sabi River, is an ephemeral, rain-fed river flowing through Rajasthan, Haryana and Delhi states in India. It originates in the eastern slopes of the Saiwar Protected Forest (PF) hills in Sikar District, enters Jaipur district near the foot of these hills, and after initially flowing southeast and east turns northeastwards near Shahpura and continues further till it exits Rajasthan to enter Haryana and further drains into Yamuna in Delhi, where its channeled course is also called the Najafgarh drain, which also serves as Najafgarh drain bird sanctuary. It flows for 300 km of which 157 km is in Rajasthan 100 km is in Haryana and 40 km in Delhi.
The Krishnavati river, also called Kasaunti, is a rain-fed river originates from Aravalli Range near Dariba copper mines in Rajsamand district of Rajasthan, and flows through Patan in Dausa district and Mothooka in Alwar district and then disappears in Mahendragarh district in Haryana where it used to be a tributary of Sahibi River, which in turn still is a tributary of Yamuna. Several Ochre Coloured Pottery culture sites have been found along the banks of Krishnavati, Sahibi river, Dohan river and Sota River. The drainage pattern for all these rivers is dendritic.
The Dohan river, is a rain-fed river that originates at Mandholi village near Neem Ka Thana in Sikar district of Rajasthan and then disappears in Mahendragarh district in Haryana where it used to be a tributary of Sahibi River, which in turn is a still flowing tributary of Yamuna. Its canalised portion in one of its paleochannel in Haryana is called the "Outfall Drain No 8".
Ahar is a former town of historical significance, located on the north bank of the Ahar River in the present-day city of Udaipur, Rajasthan, in India.
