For Admissions Contact @ 9133527733

Menu

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

  • Krishna Piedmont

Krishna Piedmont

hhKrishna Piedmonthhhhhhhh

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

Krishna Piedmont

  • This region extends over an arca about 14,240 Sq Km in Telangana state.
  • This is mainly spread in Narayanpet, Mahabubnagar, Jogulamba Gadwal, Nagarkurnool , Nalgonda , Devarakonda, Miryalaguda and Huzurnagar and areas of Suryapet district.
  • The terrain in this region is uneven. It is mainly an exposed rocky surface.

Geologically it is composed of Archean and Precambrian rocks. Soil in this region facilitates cultivation

Describe the major physiographic features of Telangana.

 

Introduction Telangana is distinguished by its diverse and complex physiography. It exhibits a variety of physical features shaped by ancient geological formations and ongoing geomorphological processes.
Body The interplay of endogenic and exogenic forces has given rise to three distinct geological regions within Telangana: the Godavari Basin, the Telangana Plateau, and the Krishna Piedmont. Each of these regions possesses unique topographical characteristics that influence the state’s climate, agriculture, and socio-economic dynamics.

Godavari Basin Region

Geological Composition:

  • Predominantly consists of Carboniferous rocks, Archean Gneisses, and Gondwana rocks.

Key Features:

  • Plains: The region encompasses fertile plains such as Karimnagar Peddapalli plain, Metpalli-Jagitial plain, Parkal plain, and Khammam-Madira-Kalluru-Kothagudem plain, which are highly conducive for agriculture.
  • Hills: Features prominent hills including Rekapallo Hills, Hasnaparthi Hills, Chandragiri Hills, Papikondalu, Raki Guttalu, Ramagiri Guttalu, and Kandikal Guttalu.
  • Flooding: The region is flood-prone due to major rivers like Godavari, Sabari, Munneru, Palair, Wira, and Akheru.
  • Districts Covered: Jagitial, Rajanna Sirisilla, Karimnagar, Peddapalli, Warangal, Khammam, and Hanmakonda.

Telangana Plateau

Geological Composition:

  • Comprised of Archean Gneisses, Hornblende, and Biotite rocks.

Key Features:

  • Topography: The plateau is higher in the West and Southwest, gradually sloping down towards the East and Northeast, merging with the Eastern Ghats.
  • Hill Tracts and Plateaus: Includes Satmala Hill Tract, Nirmal Hill Tract, Bhainsa Nirmal Plateau, Bheemgal Plain, Narayankhed-Andole Plain, Kodangal-Koilkonda Upland, and Devarakonda Plateau.
  • Hills: Significant hills include Sirnapalli Ranges, Rachakonda Hills (Hyderabad), Shabad Hill, and Koil Hills (Mahabubnagar).
  • Rivers: The region is drained by rivers such as Musi and Manjira.
  • Districts Covered: Adilabad, Nizamabad, Medak, Hyderabad, Rangareddy, and Mahabubnagar.

Krishna Piedmont

Geological Composition:

  • Dominated by Archean Gneisses and Granites, with basaltic lava forming the peneplain.

Key Features:

  • Soil Types: The region features deep black soil, red sandy soil, and laterites, making it ideal for agriculture.
  • Forests: Home to dry deciduous scrub forests.
  • Hill Tracts and Plateaus: Includes Krishna Dindi Forest Tract, Nalgonda-Miryalaguda Plateau, and Bhongir Ramannapet Plateau.
  • Hills: Notable hills include Nandagiri Hills (Nalgonda) and Ramagiri Hills (Yadadri).
  • Districts Covered: Nalgonda, Suryapet, Yadadri, Miryalaguda, Devarakonda, and Wanaparthy.
Conclusion Telangana’s physical features are a testament to its rich geological history and diverse geomorphological processes. The state’s physiography, characterized by the Godavari Basin, Telangana Plateau, and Krishna Piedmont, plays a crucial role in shaping its climate, agriculture, and socio-economic development.
Scroll to Top