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THE EFFECT OF MINING ON GEOMORPHOLOGY
(Detection of changes by using Remote Sensing techniques)
Author name: FALAK NAWAZ ‘ faalak@àvahoo.com
Co-author: PROF. DR. HAMIDULLAH " hamidu&
übrain.net.pk
ARSHAD FAYAZ'" sajeelarshad&hotmail.com
Affiliation & Official Address:
*&*
* ; TA : = ; . 3 ;
National Centre of Excellence in Geology, University of Peshawar, Pakistan.
* kx . ~ . +
Geological Survey of Pakistan, Islamabad, Pakistan
KEY WORDS
Geology, Geomorphology, Geographical Information
System, Remote Sensing, monitoring, change detection,
3-dimensional
ABSTRACT
The study focuses on the use of Remote Sensing
techniques for the detection of changes and effects of
mining on Geomorphology, especially the use of
sequential images allow us to detect changes taken place
from time to time. Nowadays, GIS and Remote Sensing
are emerging as powerful techniques widely applicable in
natural resource management and development. These
techniques, not only enable a manageable storage and
prompt access to large volumes of data, but also provide
efficient tools to extract information/knowledge for
logical decision making. Recent developments in Remote
Sensing, Aerial Photography and GIS make it possible to
detect changes and devise strategies based on these
changes.
For this purpose, the Margalla hills range are
selected where the aerial photograph of 1953, 1986 and
1999 are available. This area lies at a distance of 30 km
from the Capital City; Islamabad. From the last 30 years
when the Capital city came into being, after that time, the
Margalla hills remained the main supplier of limestone
for the construction of buildings, roads and bridges to the
Islamabad and surrounding areas. Geologically, the rocks
in the area range in age from Jurassic to Paleocene and
are of sedimentary origin. It mainly comprises of
sandstone and shale, which is very suitable for
construction of building and bridges. That is the reason
that the beautiful and green Margalla hills are being eaten
up by limestone mining and crushing activities which in
addition to the destruction of the natural landscape is
causing large scale environmental degradation and air
pollution. The site is exposed on the main Grand Trunk
Road, which connects Islamabad with rest of the Punjab
and North West Frontier Provinces of Pakistan. The
available aerial photographs shows the situation before
mining, during the mid of mining and now the latest
situation. Visual and digital image interpretation of the
available images together with GIS techniques will lead
1301
us to conclude and recommend certain concrete steps to
stop mining and propose certain other sites suitable for
the mining.
INTRODUCTION
The study area lies at the border of Islamabad (the Capital
of Pakistan) and Rawalpindi Districts. Geographically, it
stretches from 33?, 42/ to 33% 44’ north latitude and 72°
46' to 72°, 52/ east longitude (Figure 1). Margalla hill
range starts from this point and further run north-west
direction which ultimately joins the Murree mountain
series. Lslamabad, the Capital City; is located in the
southern foothills of Margalla hill range. This area lies at
a distance of about 30 km from Islamabad. From the last
30-35 years, when the Capital city came into being, after
that time, the Margalla hills remained the main supplier
of limestone for the construction of buildings, roads and
bridges to the Islamabad and surrounding areas.
Geologically, the rocks in the area range in age from
Jurassic to Paleocene and are of sedimentary origin. It
mainly comprises of sandstone and shale, which is very
suitable for the construction of building and bridges. That
is the reason that the beautiful and green Margalla hills
are being eaten up by limestone mining and crushing
activities (Figure 2), which in addition to the destruction
of the natural landscape is causing large scale
environmental degradation and air pollution. The site is
exposed on the main Grand Trunk Road, which connects
Islamabad with rest of the Punjab and North West
Frontier Provinces of Pakistan. The available aerial
photographs shows the situation before mining, during
the mid of mining and now the latest situation. Figure 3a,
b & c show the gradual depletion of the Margalla hill
range. Aerial Photograph of 1953 (Figure 3a) shows the
situation before the start of the mining activities, where
the beautiful Margalla hill is standing proudly and
increases the beauty of nature. While Figure 3b & 3c,
which have been taken during 1986 and 1999
respectively, show that the beautiful Margalla are being
eaten up by the mining activities. Plate 1 to 4 also
clarifies the situation, where the crusher machines are
eaten up the Margalla very hungrily.
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Figure 1: Location Map of Margalla Hill Range