Tag: mineral resources in rajasthan

Godavari, India's second longest river after the river Ganga and is one among the peninsular rivers. The river Godavari is often referred to as Vridha Ganga because of its large size and extent among the peninsular rivers.

Ranjit Sagar Dam is hydroelectric project on river Ravi. It is shared by Punjab and Jammu and Kashmir. Its height is 160m and it is used for both irrigation as well as power generation.

Black soil, also known as Regur soil, is primarily formed by the weathering of basaltic rocks found in the Deccan Plateau region. Other soil types like alluvial or red soil have different parent materials and formation processes.

The Chambal River is a tributary of the Yamuna River in central India, and thus forms part of the greater Gangetic drainage system. 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.

There are many Rajasthan rivers, which flow across the state. Most of these rivers are seasonal. Ghaggar is the intermittent stream, which flows through Rajasthan and disappears at the heart of the Thar Desert. Some of the other important Rajasthan Rivers are Kali, Banas, Banganga, Parvati, Gambhiri, Mahi, Kakni, Jokham, Sabarmati, Katli, Sabi and Mantha.

The Sabarmati river is one of the major rivers in the western India. It originates in Dhebar lake in Aravalli Range of the Udaipur District of Rajasthan and meets the Gulf of Cambay of Arabian Sea after travelling 371 km in a south-westerly direction across Gujarat. The river flows through Gujarat except initial 9.5 km.

Bay of Bengal lies on eastern side of India. All the rivers that flow into this Sea forms Bay of Bengal Drainage system. The rivers that constitute Bay of Bengal Drainage system are Parvati, Banas, Bedach and their tributaries. These originate from eastern side of Aravalli Mountains. Among the given options Mahi does not fall under Bay of Bengal Drainage system.

The Internal Drainage Basin is described by rivers/streams draining into a group of inland water bodies (lakes) that are located around the north-central part of the country. The system, mainly of troughs and faults runs southward from lake Natron at the border with Kenya to central Tanzania in the Bahi depression and varies in width from 30-90 km.

The basin extends over large areas in Rajasthan and Gujarat and covers whole of Diu having an area of 321,851 Sq.km with maximum length and width of 865 km and 445 km. The basin is bounded by Aravalli range and Gujarat plains on the east, by Rajasthan desert on north, and by the Arabian Sea on the south and the west. Luni is the major river system of the basin and it originates from western slopes of the Aravalli ranges at an elevation of 772 m in Ajmer district of Rajasthan. The total length of the river is 511 km and it drains a total area of 32,879 Sq.km. The river flows up to Rann of Kutch forming a delta where the water spreads out and does not contribute any runoff. The main tributaries of Luni joining from left are the Lilri, the Guhiya, the Bandi (Hemawas), the Sukri, the Jawai, the Khari Bandi, the Sukri Bandi and the Sagi whereas the Jojri joins it from right.