Shajapur district

Shajapur District is a of   of. The town of is the district headquarters.

Shajapur District is part of the Plateau. The district is situated in the northwestern part of the state and lies between latitudes 32"06' and 24" 19' North and longitude 75" 41' and 77" 02' East. The district is bounded by to the west,  and  to the south,  to the east, and  of  to the north. Shajapur District is part of.

History
The district was formerly a district of. When Gwalior acceded to the after Indian Independence in, Shajapur District, along with the rest of Gwalior State, became part of  state. Madhya Bharat was merged into Madhya Pradesh on,.

Geography
The entire district is a part of the s of - age. of recent period is, however, found along the river in a narrow strip. The district has deep black and shallow black brown and alluvial soils of the northern region. The physical geography of the district can be sub-divided into the following:

Agar-Malwa(Baijnath Dham)
This is the western part of the district covering the major areas of. There is a hill tract in the west of town showing scattered hillocks in a north-south direction. The presence of hills in the center has affected the drainage pattern. The height of this tract varies between 500 and 545 meters above the mean sea level and it slopes towards the north. and are the main streams in the west, originating from the hill tract and draining towards the west. , which is the main perennial stream of the region, flows northwards on the western border of the region. agar is too good city.

Shajapur forested upland
The region stretches from north to south in the middle of the district covering considerable portions of and  tehsils and a small part of  tehsil. It is a part of Malwa plateau with typical topography. There is a continuous chain of hills in 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. and 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 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 form 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 form 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  period.

Shajapur upland
This region extends over the eastern part of the district covering the entire 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 river where the small hills are spread, and the Newaj dissects these hills. The eastern part of the region is a low and water dividing line of the western part can be decided by the tributaries of Newaj. The river Newaj and Parbati drains the region. The river Parbati flows northwards on the eastern border of the region while river Newaj flows in the middle of the region. Both the rivers are perennial.

External link

 * Shajapur District web site