Page 1 of 11

Journal for Studies in Management and Planning

Available at http://edupediapublications.org/journals/index.php/JSMaP/

e‐ISSN: 2395‐0463

Volume 01 Issue 10

November 2015

Available online: http://edupediapublications.org/journals/index.php/JSMaP/ Page | 249

Delineation of watershed in Amravati tehsil using geomorphological

investigations through Remote Sensing and GIS techniques

Khadri S.F.R*, Sachin Thakare and Pooja Surkar

Department of Geology, Sant Gadge Baba Amravati University, Amravati-44602 (MS)

*Email: khadrisfr@rediffmail.com

Abstract:

In this study an attempt has been

made to understand various

geomorphological factors controlling the

various landforms which in turn helpful in the

delineation of watershed in Amravati tehsil

through remote sensing and GIS techniques.

The study area exposes part of Pedhi River

and Kholad River which is a part of Wardha

Watershed. The present investigations have

helped to understand the groundwater

potential as well as nature of the watershed

with the help of detailed geomorphological

investigations. Satellite remote sensing data

as well as topographic data has been widely

utilised in this study to identify the watershed

and groundwater potential zones with the

help of latest available techniques.

The results of the present study

demonstrate the presence of various hydro

geomorphological zones showing their

groundwater potentialities which vary from

excellent to poor. The study area covering

Pedhi watershed shows excellent to good

ground water quality whereas the Kholad and

Kapasi watersheds show moderate to poor

ground water quality. Overall, the present

study demonstrates the useful ness of remote

sensing and GIS techniques in the delineation

of potential aquifers in the region which plays

a major role in the sustainable management

of water resources in the Amravati region.

Key Words: Remote Sensing, GIS,

Geomorphology, Watershed, Satellite,

Topography.

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Introduction:

A watershed can be defined as the

area of land that drains to a particular point

along a stream. Each stream has its own

watershed. Topography is the key element

affecting this area of land. The boundary of a

watershed is defined by the highest elevations

surrounding the stream. A drop of water falling

outside of the boundary will drain to another

watershed (Sewickley Creek Watershed

Conservation Plan, 2003). From a planning

standpoint, watershed is considered the most

ideal unit for analysis and management of

natural resources. For optimal use of

environmental resources in a region, integrated

watershed development approach is still

viewed by many to be the most ideal as it helps

in maintaining the ecological basis of resources

utilization (Sahai 1988). Geomorphology is

defined as the science of landforms with an

emphasis on their origin, evolution, form, and

distribution across the physical landscape. The

science that deals with surface features of the

earth, their forms, nature, their origin and

development is termed as geomorphology.

DAVIS (1912) first projected the concept of

Page 2 of 11

Journal for Studies in Management and Planning

Available at http://edupediapublications.org/journals/index.php/JSMaP/

e‐ISSN: 2395‐0463

Volume 01 Issue 10

November 2015

Available online: http://edupediapublications.org/journals/index.php/JSMaP/ Page | 250

geomorphic cycle. According to bauling

(1950), the role of factors that are important the

geomorphology are lithology, stratigraphy,

climatic variation and the regional basis for the

development of landforms. The use of remote

sensing technology for Geomorphological

studies has definitely increased its Importance

due to the establishment of its direct

relationship with allied disciplines, such as

geology, soils, vegetation/Land use &

hydrology.

Geomorphological mapping involves

the identification and characterization of

various landforms and structural features. The

various landforms can influence a conservation

area in many ways like slope gradient,

elevation and aspect, affect the quantity of solar

energy, water, nutrients and other materials,

while the slope affect the flow of materials.

Slope is also the deciding factors of intensity of

disturbance, such as fire and wind, which are

strongly influenced by the pressure of

vegetation (Swanson et al 1988).

Study Area:

Amravati Tehsil basically part of

Amravati city and the villages around it lying

between 220 45” N to 210 20” N and 770 32” E

to 780

02” E. Amravati is District place and

major city in Vidharbha region. Amravati

names comes from Hindu goddess

“Ambadevi”, in Mahabharata epic Amravati is

a capital of Vidarbha Naresh, and it is a part of

Varhad (Berar).

Geography:

Amravati Tehsil is bordered with

Achalpur tehsil as well as Murtizapur Tehsil in

North direction and Chandur Bazar Tehsil

touches the boundary in east and west

direction. Wardha River is naturally separate

Amravati District from Wardha District.

Wardha River is a major River of Vidarbha

region which is join Painganga River in the

boundary of Marathwada. Pohra Malkhed is

protected forest area in Amravati. The average

elevation is 543m from MSL.

Climate:

Climate of Amravati Tehsil is hot and

dry, April to June Month having extremely heat

and temperature goes to 450 C as well as winter

season temp goes down 110

C which shows

temperature variation, Rainy season start from

end of June Month to September in an average.

Soil:

There are three main types of soil present

in Amravati Tehsil which is- a) Deep Black Soil b) Medium

Black Soil c) Shallow black Soil

Crop pattern:

Amravati Tehsil is having different

types of Crop Pattern such as Cotton, Sorghum

(Jawar), Green Gram (Moong), Soybean etc.

but Amravati tehsil as well as whole District is

famous for Orange (Citrus Spp.)

Rail/Road:

In Amravati tehsil Badnera is Major

Railway Station of Central Railway. National

Highway 6 is passed through the Amravati

Tehsil.Fig.1 shows the location of Amravati

Tehsil.

Page 3 of 11

Journal for Studies in Management and Planning

Available at http://edupediapublications.org/journals/index.php/JSMaP/

e‐ISSN: 2395‐0463

Volume 01 Issue 10

November 2015

Available online: http://edupediapublications.org/journals/index.php/JSMaP/ Page | 251

Fig. 1 Location Map of Study Area

Materials and Method:

Data Used

a) Toposheet Approved by Survey of India Having 1:50000 scale

b) Satellite Imagery LISS data having 23.5m resolution

c) ERDAS Imagine Remote sensing Software

d) ARC GIS Software

Methodology

Fig.2: Flowchart showing the methodology used for Watershed