This paper presents the Recently geological study; Stratigraphy, regional geology, geology of the Basin, sedimentary formation and basaltic lavas flow of the Shivna River Basin in the Deccan Basaltic Province north Western region of Madhya Pradesh, India. The geological setting of area is characterized by development of rocks of different ages, ranging from Neo Proterozoic to Recent. The presence of the Binota shale, Jiran Sandstone Kharip/ Semri Group of Vindhyan Super Group (Neo Proterozoic), and Deccan Traps (Upper Cretaceous to Lower Eocene) developed under a capping of the Laterite and Alluvium (Pleistocene to Holocene). Binota Shale is conformably overlain by grey and pink Jiran Sandstone. The ridges of sandstone are developed in North–West sector of the Basin. Deccan Traps comprise to Basaltic flows which have been grouped into Kalisindh and Kankariya – Pirukhedi Formations. The flows have a vesicular type and sparsely to moderately porphyritic. Laterite occurs as a cover of basaltic lava flow and Alluvium deposit occurs as narrow linear belt along the River.