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By Pramod Pagare

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The summer heat on the plateau is mitigated by the altitude, which also ensures a cold winter. Temperature varies according to altitude, aspects and configuration of the ground. Thus, it is more equitable in plateau than in valleys. March of Temperature 1. 3°C) due to low humidity resulted from vernilization of leaves. 1 157 167 Temp. 3. to reach it, thus causes an increase in humidity. In other way, we can say that the daily temperature is influenced by vegetation indirectly. An increase in' both mean daily minimum and daily maximum temperature alarms the plants to their preparation for scanty supply of moisture because of more evaporation.

In the study area one interesting feature of the impact of geology on the distribution of vegetation is seen in Gondwana sandstone area. The sandstone consists of massive, soft sand stones, gravel beds, clays, etc. The mixed forests are predominating over this formation. The underlying rocks of the Gondwana sandstones give birth to infertile soil which is occupied by dry miscellaneous forests. Some of the Talchir and Barakar soil are more clayey and give a slightly better forest crop of moist miscellaneous species.

37 Source: Climatological Table of Observatories in India (1931-1961), Government of India, p. 397. 4. The summer heat on the plateau is mitigated by the altitude, which also ensures a cold winter. Temperature varies according to altitude, aspects and configuration of the ground. Thus, it is more equitable in plateau than in valleys. March of Temperature 1. 3°C) due to low humidity resulted from vernilization of leaves. 1 157 167 Temp. 3. to reach it, thus causes an increase in humidity. In other way, we can say that the daily temperature is influenced by vegetation indirectly.

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