Geology, Rock and Soil
The foot hill plains of Nilgiri hills abutting smaller hill ranges along with the main chain of Nilgiri Mountain range bordering Bandipur Tiger Reserve comprises of Achaean metamorphic rock which include Charnockite, Biotitic, Magnetite, Quartzite, Hornblende, Granulite, Pegmatite, and Dolerite and Quartz veins. Intensive bands of Charnockite forms bulk of the rock units in bordering Mudumalai Tiger Reserve area, extending in to the Bandipur Tiger Reserve. This hypersthenes-bearing bluish grey rock forms the basement in high-grade metamorphic terrain. The Charnockite has granolithic texture and contains quartz, feldspar, hypersthenes garnet and hornblende, Biotite, apatite and zircon as accessory minerals. Hornblende Granulite is found along the areas bordering Wayanad, extending into the Bandipur Tiger Reserve.
The underlying rocks belong mainly to the metamorphic formations of which Gneiss, Quartzite, Mica, Hornblende and Schists are found generally all over. The Igneous rocks, Granite and Charnockite are found intruding through the metamorphic rocks appear as out crops at higher levels and in the beds of water course. Quartz is a major component of the rock formations in the south east extreme of the Reserve in Kaniyanapura Block-II and III, Moyar Area and the fissile character of the Granite near Yelchatti is largely due to the banding of Quartz veins. A variety of Pinkish Grey Granite is seen in the beds of Heballa, Honnurhatti and Arekadu halla (Dr. Kadambi).
Two Principal types of Soil are –
The soils are shallow on the hill tops and deep in valleys. The substratum of clayey soils is generally a variety of white, soft, easily disintegrating rock in which feldspar predominates. The clayey soils are confined to low lying localities in patches. The substratum of loamy soils consists generally of metamorphic formations which are highly ferruginous. The reddish loam soils are the product of the process of weathering of these underlying ferruginous rocks. The best forest growth is found on deep well drained loamy soils. There are patches of shale mixed with powdered quartz containing some minerals and salts which form the Natural Salt Licks for the Wild Animals. The one at Upneerhalla and some on Chammanalla road are good examples of this type.Hydrology and Water Sources
Three seasons are markedly noticed in the Reserve, the dry, the wet and the cold. The cold season starts in November and lasts up to mid February; later on the hot season commences and lasts up to middle of June. The coldest months are December and January and the hottest are March and April. The wet season starts in the middle of June with heavy pre-monsoon showers in April and May. The wet season lasts up to September. The North-East Monsoon starts from the mid of October lasting up to the mid November. The climate is generally hot and dry in summer; with occasional pre-monsoon showers. The climate, on the whole, is generally healthy except in the South-Western portions of Beerambadi, Ainurmarigudi and Begur area.
Principal Forest Types- The forests of the Tiger Reserve are varied and rich. To the eastern most portions lie the scrub forests of Moyar. While the vegetation in the central portion of the Tiger Reserve viz., Kaniyanapura, Bandipur part of Beerambadi is dry deciduous, the vegetation in the western part of the reserve viz., Ainurmarigudi, Begur and Beerambadi is moist deciduous. The vegetation, therefore, changes from scrub type to moist deciduous type from east to west. These forests are classified as under: