Q- What is the north east extension of Deccan Plateau called?
Answer- The north east extension of Deccan Plateau is commonly known as Anglong Plateau, North ‘Cachar hills’, Meghalaya as well as Karbi.
The answer given above is small but is enough to tell you about what is the northeast extension of deccan plateau called. If it might be helpful for you so tell us your more questions in comment box. If you are interested in reading more about Deccan plateau so the paragraphs given below are only for you. You should read them carefully.
The word Deccan Plateau is of a prakrit word dakkhana or dakkhin that etymologically in sandskrit refers to dakshin that means the south direction. As Deccan Plateau is a very huge plateau that lies in the southern region of India. It lies in the middle of two major ghats that are Western ghats and Eastern ghats. The deccan plateau are more drier as compared to other coastal region near it in southern region of India. In the North this plateau is bounded by the Vindhya ranges and Satpura. Several geographers did dead study on deccan plateau ad found several amazing facts of it. They also prepared a new definition of Deccan plateau that is based on their researches and observations. They defined Deccan plateau as a peninsular tableland that lies on the southern region of Tropic of Cancer. The area of Deccan plateau is sub divided into two categories physiologic-geographical regions. These are noted below one by one:
1. Plateau with fertile black soil that is totally formed of igneous rock.
2. A Hilly region with red soil that is composed of gneiss peneplain
The average elevation of deccan plateau is about 2000 feet or 600 m. As the deccan plateau lies in the center of eastern ghat and western ghats so because of high mountain ranges of western ghats the monsoon winds get blocked from reaching deccan plateau. So, this leads to very less rainfall in that region. Most of the rivers in deccan plateau falls in southern region of India, whereas the majority of the northern portion of deccan plateau is drained by River Godavari and its tributaries.
When we talk about the climatic condition of deccan plateau. So, the climate in deccan plateau is such that some region of it is semi-arid in the northern part and tropical in other region. The two most dried region of this plateau are Vidarbha and Rayalaseema. The mid of March and June moth the climate remains hot and dry but in the mid of June-October month rainfall occurs.
However we had talked a lot about Deccan plateau in detail. And we hope that you get all the points clearly that we told you in above paragraphs. Now, we are going to talk about a very important term ‘Deccan Trap’ that is also related to deccan plateau.
Deccan Trap are large igneous province of central-west India. These are the largest or one of the largest volcanic features in the World. The deccan traps are composed of several or multiple layers of solidified flood basalt that are about 2000 metres in thickness.
From the ancient time the Deccan plateau leads to origination and survival or several major dynasties in Indian history:
- Satavahana
- Chalukya
- Pallavas
- Vakataka
- Western Chalukya
- Rashtrakuta
- Kadamba dynasty
- The Nizam of Hydrabad
- Bahmani Sultanate
- Deccan Sultanate
- Maratha Empire
- Vijayanagara
- Musunuri Nayakas
- Kakatiya Empire
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