The document summarizes the key geomorphological features of the Bharveli area in Madhya Pradesh, India. It describes that two-thirds of the study area consists of planar surfaces covered by clayey soil. Undulating ground surfaces formed by denudation processes are also present. Infilled valleys confined along river streams are depositional landforms used for agriculture. Denudational hills composed of granite and gneiss formed from weathering and erosion processes are located near Agarwara. Residual hills, pediments, and pediplains resulting from pediplanation are also observed near Bharveli, Jarera, and Manjhara respectively. Structural hills and linear ridges developed due to tectonic

1. GEOMORPHOLOGY OF THE AREA
AROUND, BHARVELI.(M.P.)
Dr.ANIL KUMAR NEMA
GUEST LECTURER
GEOLOGY
Govt.J.S.T.P.G.College Balaghat

2. GEOMORPHOLOGY
• Almost two-third part of the study area is covered
by the planar surface. These planar surfaces are
covered by deep, moderately well drained clayey
soil.
• These undulating ground surfaces with remnant
low relief are formed by dynamic wheels of
denudation processes.

3. • DEPOSITIONAL LANDFORMS
• Infilled Valleys confined along the course of
river streams and streamlets.
• The land use pattern of these valley fills are
Agricultural.

4. Geomorphological map of the study area

5. • DENUDATIONAL LANDFORMS
• These hills are the remnants of natural
dynamic processes of denudation and
weathering added by the fluvial action.
• In the study area Denudational hills are
located near Agarwara; and are made up of
hard and resistant granite and granite gneiss.

6. RESIDUAL HILL
Residual Hills are the end product of
the process of pediplanation, which
reduces the original mountain into a
series of scattered knolls standing as
no pediplains.
It is located near Bharveli

7. PEDIMENT
The pediment is nearly a flat or
strongly concave erosional surface of
the bedrock.
Pediments are located near Jarera

8. PEDIPLAIN
Term generally used to describe a series
of coalescing pediments.
Pediplains are located near Manjhara

9. • STRUTCTURAL LANDFORMS
• These landforms are developed due to effect
of tectonic movements later modified by
erosion.
• In the present study area, structural
landforms are observed as structural hills, and
linear ridges

10. THANKS