JOURNEYING THROUGH GEOLOGY
Ms Shilpa Khandolkar is a ‘Geoscientist
at the Geological Survey Of India’. She graduated from Dhempe College of Arts
& Science in 2008 and obtained a masters degree from Goa University in
2010. She subsequently joined the teaching profession and worked at Dhempe
College of Arts & Science and later at Parvatibai Chowgule of Arts &
Science.
In December 2013, she joined the
training office as a Trainee Geologist.After completing eleven months at various
training Institutes all over India, she was posted at Kolkata in 2014. She spent two years
in Geochemical Mapping in the State of Orissa and is currently working for Geoinformatics.
Interviewer:
How was your experience in Chowgule and Dempo, when as lecturer?
Interviewee:
Enjoyed teaching, loved Chowgule, good environment
and cooperative staff.
.
Interviewer:
Do you miss your job?
Interviewee:
Yes a lot
Interviewer:
How was the department during your time?
Interviewee:
Very nice, I still remember those days.Students were very much interested in
Geology. The staff and students were very cooperative.
Interviewer:
How did you get into GSI?
Interviewee:
I answered the UPSC exam for geologists. It is held every year.
Interviewer:
Tell us something about GSI?
Interviewee:
It’s basically to find coal and mineral resources.
There are currently 5 missions,
1- Ground
and Marine.
2- Mineral
Resource Assessment
3- Geoinformatics
4- Geotectonics
and Geohazards.
5- Training
and Capacity Building.
The beginning of
geological investigation in India was in the early part of the nineteenth
century. A few amateur geologists associated with the Survey of India and Army
initiated geological studies in the country. H.W. Voysey (1818-1823) of the
Great Trigonometric Survey made the first Geological Map of Hyderabad region
along with a detailed report. A committee for “The Investigation of Coal and
Mineral Resources” was set up in 1837. The Secretary of the Committee John
McClelland made the appointment of the first professional geologist. D. H.
Williams was the first Geological Surveyor appointed by the East India Company
in 1846. John McClelland for the first time used the term Geological Survey of
India in his report in 1848. He designated himself as officiating Surveyor,
Geological Survey till 1st April 1850. The Geological Survey of India (GSI) was
set up in 1851 primarily to find coal deposits for the Railways. The arrival of
Sir Thomas Oldham, Professor of Geology at Trinity College Dublin and the Chief
of Irish Geological Survey at Calcutta on 4th March 1851, marked the beginning
of the continuous period of the Geological Survey of India. Over the years, it
has not only grown into a repository of geo-science information required in
various fields in the country, but has also attained the status of a
geo-scientific organisation of international repute. The main functions of GSI
relate to creation and updation of national geoscientific information and
mineral resource assessment. These objectives are achieved through ground
surveys, air-borne and marine surveys, mineral prospecting and investigations,
multi-disciplinary geoscientific, geo-technical, geo-environmental and natural
hazards studies, glaciology, seismotectonic study, and carrying out fundamental
research. Outcome of work of GSI has immense societal value. Functioning and
annual programmes of GSI assume significance in the national perspective.
GSI, headquartered at Kolkata, has six Regional offices located at Lucknow, Jaipur, Nagpur, Hyderabad, Shillong and Kolkata and State Unit offices in almost all States of the country. Presently, Geological Survey of India is an attached office to the Ministry of Mines.
GSI, headquartered at Kolkata, has six Regional offices located at Lucknow, Jaipur, Nagpur, Hyderabad, Shillong and Kolkata and State Unit offices in almost all States of the country. Presently, Geological Survey of India is an attached office to the Ministry of Mines.
Interviewer:
Is GSI in contact with other countries with respect to research?
Interviewee:
Yes, British University is in collaboration with respect to natural hazards.
Interviewer:
What does GSI mostly focus on?
Interviewee: GSI
also focuses on Landslides Hazards and its Consequences
Protection of life and properties from
landslide disaster is indispensable in creating a safe environment for the
society. The national imperative towards safety due to landslide initiation is
increasing in view of the higher rate of human settlement in the mountain slope
across the country. Landslides are significant amongst those hazards that can
easily be disastrous to human life and property. It is estimated that economic
loss due to landslides may reach between 1-2% of the gross national product in
many developing countries. Evaluating and mitigating the landslide hazard and
risk is a major challenge for the technocrats and decision makers in the
developing world as 80% of the reported fatalities due to landslide is within
the developing countries.
In India, about 0.42 million sq. km or 12.6% of land area, excluding snow covered area, is prone to landslide hazard. Out of this, 0.18 million sq. km falls in North East Himalaya, including Darjeeling and Sikkim Himalaya; 0.14 million sq. km falls in North West Himalaya (Uttarakhand, Himachal Pradesh and Jammu & Kashmir); 0.09 million sq. km in Western Ghats and Konkan hills (Tamil Nadu, Kerala, Karnataka, Goa and Maharashtra) and 0.01 million sq. km in Eastern Ghats of Aruku area in Andhra Pradesh. The landslide-prone Himalayan terrain falls in the maximum earthquake-prone zones (Zone-IV and V; BIS 2002) where earthquakes of Modified Mercalli intensity VIII to IX can occur, and thus, are also prone to earthquake-triggered landslides. The most recent example is the aftermath of 18 September 2011 Sikkim Earthquake in the Sikkim-Darjeeling Himalayas.
In India, about 0.42 million sq. km or 12.6% of land area, excluding snow covered area, is prone to landslide hazard. Out of this, 0.18 million sq. km falls in North East Himalaya, including Darjeeling and Sikkim Himalaya; 0.14 million sq. km falls in North West Himalaya (Uttarakhand, Himachal Pradesh and Jammu & Kashmir); 0.09 million sq. km in Western Ghats and Konkan hills (Tamil Nadu, Kerala, Karnataka, Goa and Maharashtra) and 0.01 million sq. km in Eastern Ghats of Aruku area in Andhra Pradesh. The landslide-prone Himalayan terrain falls in the maximum earthquake-prone zones (Zone-IV and V; BIS 2002) where earthquakes of Modified Mercalli intensity VIII to IX can occur, and thus, are also prone to earthquake-triggered landslides. The most recent example is the aftermath of 18 September 2011 Sikkim Earthquake in the Sikkim-Darjeeling Himalayas.
Compiled by Vidiksha Fernandes and
Evania Dias.
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