The Bundelkhand plateau is formed in Pe-
Cambrian era in the form of rocks Bundelkhand gneiss,
over time which have been converted into igneous and
metamorphic rocks as a result of the intercalation process.
Most of the Bundelkhand Plateau is a flat plain,
surrounded by the Vindhyan Scrap Land. The tributaries
of Yamuna, which flows towards the northeast in the
Bundelkhand Plateau are Dhasan, Ken, Betwa which form
narrow valleys. waterfalls. verges and ravines.

Central India Plateau faces the problem of
soil erosion (also called Gully erosion) in M.P. The
northern region of Central India Plateau has mostly
suffered from the problem of soil erosion due to largest
deforestation. As a result, this area has been transformed
into the largest rugged area in India.

Central High Land covers two-third of M.P.
The Central High Lands are formed by rocks of Archean,
Dharwar, Deccan Trap and Vindhyan Series. Geometrically,
the shape of Central Highland is triangular, forming two-
thirds of the area of M.P. The extension of Central
Highland is in the northern part of the Narmada-Son valley.

Bhander Series of Vindhyan Rocks is
extended in Western part of Vindhyan Mountain Range
in M.P. i.e. Sagar, Satna and Damoh dists. of M.P. The
sandstones are divided into Lower Bhander and Upper
Bhander stages with shales known as the Sirbu Shales in
between them. Deposits of limestone, sandstone and shale
are found from the rocks of the Bhander Series.