Memoirs of the Geological Survey of India

This gneiss forms all the lower hills around the base of the Chunderpur Pits of which the plateau on the right (south) of the profile is a continuation (about 8 500 feet) situated near the village of Chunderpur. [...] In general outline of has; as well as in Ethological character of the rock the granite of this ridge is identical with the rocks of the southern areLitman% Tourmaline granites prevail and form the main mass of the eastern extension of the ridge sending out long spurs into the neighbouring schists. [...] inclination of the strata the face of the cliff is actually overhanging the rocks splitting off along the joints which are mostly normal to the of bedding. [...] VI I have given the profile of the eastern escarpment of the Reimkola plateau in which the Mahadevas (1) are seen to slope to the north-west with the trap (2) forming the intrusive sheet beneath the strata of the landetone. [...] The narrow strip of trap north of Nimadhfika (5 miles north-west of Maiapur) at the foot of the Salhota hill is probably part of the intrusive sheet which is hidden` by the Mahadeva sandstone of the ^ Churipat hills.