By Pramod Pagare
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Extra info for Applied Plant Geography
Bhainsdehi-Khamala Plateau : The south-western part of the study area comes under Bhainsdehi-Khamala plateau. Its northern boundary is marked by the Tapti and southern boundary is formed by the Gawaligarh hills. It forms a narrow belt bordered by the ravines of the Wardha and its Tributaries (Maru) to the east which separates the plateau from Multai plateau. The general elevation of the plateau is about 640 metres. In the eastern part it is about 701 metres in the west with large area rising above 762 metres.
The beds comprise of purple clays and are accumulation of volcanic agglomerate mixed with a little sand. The clay is composed of numerous angular quartz grains. They are exposed near Taramkhera and along the road east of Pat (Tableland). In lameta formation teak is invasive in the clear fellings of the mixed forests. The Deccan Trap The Deccan traps are the one major geological formation occurring in the area under study. More than half part of the plateau is covered by this formation. The extensive trap formations are found in the Betul-Multai plateau, Bhainsdehi and Morand plateau.
The seven months (November to May) are xeric, so the water balance remains unfavourable for the vegetation. The formula proposed by Miller (1951), T/R is tried to determine the index of vegetation climate where T is mean annual temperature in OF and R is mean annual rainfall in inches. 62 in the study area which represents humid vegetation climate. It is conducive to good growth of plants. 7). No. Station TlR Index Type Description 1. 61 Humid (i) 2. 67 Humid 3. 68 Humid 4. 75 Humid 5. 90 Humid 6.
Applied Plant Geography by Pramod Pagare