plateau with typical topography. There is a continuous chain of hills throughout the entire region. The height of the region varies between 450 and 530 meters above the mean sea level. The surface height decreases towards the north. Since it is an upland area, a number of seasonal streams originate from this zone and drain mostly towards the east. Lakundar and Ahu are the main streams flowing from south to north in this region. The streams that join the Lakundar river on its left bank, originate from this hill tract. The Ahu river drains along the western border of the region. The hilly terrain is covered with forest. Kali Sindh basin The Kali Sindh basin stretches between the southern and northern limits of the district. It occupies the major parts of Susner and Shajapur tehsils and a very small part of Agar tehsil. The southern part of the region is hilly whereas the northern part is plain. The hills gradually decrease in height from south to north. There are a few scattered hillocks in the central and northern parts also. The altitude of the region varies between 450 and 528 meters above the mean sea level. Numerous streams originate from the hilly area and dissect the surface. Kali Sindh is the main river, which traverses through the hills and further flows on the eastern border of the district. Lakundar is the main rivulets of Kali Sindh that flows northwards. Geologically the entire region is a part of the Deccan Trap of the Cretaceous Eocene period. Its main helping river is kanthal that is the major source of water in Soyat Kalan. Shajapur upland This region extends over the eastern part of the district covering the entire Shujalpur tehsil and a small segment of Shajapur tehsil. Being a part of the Malwa plateau, it presents a dissected topography. A hill range enters this region from the north and extends towards the south. The southern part of the region is an upland area and northern part is relatively low lying. In the south, the hills are scattered and are eroded by various streams. The height at the region varies between 435 and 507 meters above the main sea level. The 450 meters contour encircles the area along the Newaj river where the small hills are spread, and the Newaj dissects these hills. The eastern part of the region is a low and