Indian plate consists of several microplates, in the plate tectonic process they merged and disintegrated. The stable part of India i.e., Southern India, consists of several microplates, including the Eastern Dharwad and Western Dharwad in between lies the Chitradurga Schist belt. It has even the primordial rocks and rich in minerals. It was a pleasure to see the oldest rocks and understand all the structural changes happened in the history. This structural and geological study gives a glimpse into one of the oldest parts on earth. I am thankful to Prof. K. V. Subba Rao, a very well known Geologist of India for introducing me to this field area.