Soru

Zorluk: OrtaPhysiography and Relief Features of India

Match the regional physiographic features of India listed in Column I with their corresponding geological or geomorphological descriptions in Column II.

  • PatlandsHigh flat-topped, basalt-capped tablelands characteristic of the Chota Nagpur Plateau
  • ChosEphemeral seasonal torrents causing severe gully erosion in the Siwalik foothills
  • BarchansCrescent-shaped mobile sand dunes formed by wind action in the Thar Desert
  • DuarsFoothill alluvial floodplains serving as natural gateways to the Eastern Himalayas

Cevap

Patlands match with high flat-topped basaltic tablelands in the Chota Nagpur Plateau; Chos match with ephemeral seasonal torrents causing severe gully erosion in the Siwalik foothills; Barchans match with crescent-shaped mobile sand dunes formed by wind action in the Thar Desert; Duars match with foothill alluvial floodplains serving as natural gateways to the Eastern Himalayas.
Each physiographic feature is paired accurately with its unique geographic description: Patlands correspond to high basaltic plateaus in Chota Nagpur, Chos to gullied seasonal streams in the Siwaliks, Barchans to crescent sand dunes in Rajasthan, and Duars to the alluvial foothill gateways of the Eastern Himalayas.

Adım Adım Çözüm

1
Analyze the landforms of the Peninsular Plateau and Northern Mountains.
Patlands represent elevated plateau remnants in the Chota Nagpur region, while Duars are foothill alluvial plains in North Bengal.
Regional physiographic terminology specifies distinct structural origins across Indian relief zones.
2
Analyze the erosional and depositional features of the Desert and Sub-Himalayan zones.
Barchans are aeolian sand features of the Thar Desert, whereas Chos are water-eroded gulley systems in the Siwaliks.
Evaluating geomorphic processes distinguishes wind-driven arid landforms from fluvial sub-Himalayan torrents.

Anahtar Kavram

Regional Physiographic Landforms and Micro-Relief Features of India
Bu soruyu puanla