• Gulam Sabri Ahmed
• M K Bhatnagar

The southern and eastern piece of Pench-Kanhan Tawa valley is lopsided and harsh with thick woods cover however the western. North-western parts are generally level. Pench-Kanhan Tawa stream gushing westward and south is controlling the waste of Tawa repository. Scarcely any occasional nallahs (Latiya Nala, Dagdaga Nala and so forth) starting from Kilandev Pahad, Bagdev Pahad, Shri Phar and other raised locales release in to Pench-Kanhan Tawa Waterway which streams in westerly course. Satpura dam has been worked across Tawa Stream to store water for nuclear energy Plant at Sarni as well as to manage the progression of water in the downstream of Tawa Stream. Pench-Kanhan region shows a rough geography covered with Deccan Trap. The territory contains many slopes and valleys-primary slopes, covered by Gondwanas, are found in northern part; denudational slopes in southern part and took apart Deccan level in eastern and northeastern parts. The region is depleted by two significant waterways - Pench and Kanhan stream (streaming towards south east) and their feeders to be specific Gonur, Magrahi, Ghatamai, Sukri stream, Bor Nala, Rakhi Nala, Tambiya Nadi, Bardhar Nadi and so on. The new alluvium stores are found at places along these waterways.

"A review on vegetation of Pench-Kanhan-Tawa and Satpura valley Coalfield", International Journal of Emerging Technologies and Innovative Research (www.jetir.org), ISSN:2349-5162, Vol.10, Issue 2, page no.e387-e398, February-2023, Available :http://www.jetir.org/papers/JETIR2302442.pdf

"A review on vegetation of Pench-Kanhan-Tawa and Satpura valley Coalfield", International Journal of Emerging Technologies and Innovative Research (www.jetir.org | UGC and issn Approved), ISSN:2349-5162, Vol.10, Issue 2, page no. ppe387-e398, February-2023, Available at : http://www.jetir.org/papers/JETIR2302442.pdf