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What’s
more life-threatening, ravines or dacoits? You’ll be surprised
in Bhind and Morena, says
Mukul
Sharma.
THIS
is a cancer that affects whole villages. Like the cancerous
cells in the human body, this one too spreads fast, but unlike
the deadly disease, is not being checked. No chemotherapy
to zap the bad cells here. Ravines are gobbling up whole villages
and communities in Bhind and Morena districts in Madhya Pradesh,
destroying their houses and wasting away the soil.
It’s
estimated that ravines have affected 948 villages in Bhind
and Morena districts. Mrigpura village in Morena is being
gobbled up by the ravines so rapidly that all the land around
it has turned into deep pits. Devdutta, who shared one of
the patches along with 15 families, says, ‘‘We have no place
to stay any more. People have settled on whichever patch of
land they found. The village as we knew it is now divided
into 18 parts. What could be the life of any person when his
place is divided into so many parts, when there is no land
to till, no pastures and no work?’’
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Ravines
were blamed for shielding the dreaded dacoits of Chambal.
But when hundreds of them surrendered in 1972, the government
didn’t feel the need to reclaim ravines any more
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Lack
of vegetation helps rainwater sweep away the upper portion
of the land. The fast-flowing water creates nallahs, big cracks
and fissures which develop slowly or quickly, depending on
the rainwater, and become ravines. Once even a small ravine
is formed, every rainfall makes it bigger by creating holes
in the front as well as the corners. Scientists explain that
in the specific context of Bhind and Morena districts, the
light and alluvial kind of soil, coupled with deforestation,
increasing population pressure, faulty irrigation projects
and short-term developmental schemes seemed to have fuelled
the formation of ravines.
Chursalai
village is 17 kilometres away from Amba, but has to be covered
by foot or camel. Since the last two years, the ravines have
been steadily gobbling up and destroying village land. Ramjee
Lal says nobody in the village, which numbers 50 houses, has
agricultural land now. The villagers either do some cultivation
on the riverbank or cut forest trees to sell to the cities’
markets. Be it farming, employment, schools, roads, electricity
or hospitals, the place has nothing to offer except the bare
minimum vestiges of human survival.
Though it’s situated near the Chambal river, there is a shortage
of drinking water. The village now has only a single well
that provides water for a maximum of an hour a day. Villagers
have to go to Chambal river and get water on the camels’ back.
Fifty
kilometres away, the ravines have carved up Rudawali village,
with a population of 5,000, into three segments. Almost half
the village, comprising houses, schools and streets, has been
turned into ravines. In the middle of the village, 50-60 feet
deep ravines are present.
Virendra
Kumar’s house is partly breached and can be eroded any time.
‘‘Where else do we go?’’ he asks, ‘‘Those who could afford
safer places have left the village. But the Dalits have no
other residential place and no money to buy one.’’ Not a single
hand-pump is working, and groundwater levels have dipped so
much the water level of wells has sunk to 200 feet.
In Porsha
block of Morena district, Ratanbasai village has split into
eight new segments. The streets and roads have been destroyed
and it takes a tough walk across three kilometres to cover
all segments of the old village. The ravines are eating into
the social life of the villages. A villager narrates how it’s
now a problem to get their children married.
Nayakpura,
Rubara, Ajitpura, Khadoli, Jaghona, Rithona, Mahuwa, Sarsani,
Gaushpur are among the innumerable ravine-affected villages
in this region. The Chambal Division Commissioner’s Office
at Gwalior estimates that in Chambal Division, which has an
area of 16.14 lakh hectares, around 20 per cent of the division,
i.e. around 3.107 lakh hectares are ravines. The ravines have
spread along the main rivers of the region, which include
Chambal, Quari, Lasan, Seep, Vaishali, Kuno, Parvati, Sanka
and Sindh. The worst ravines are in the vicinity of Chambal
river and are expanding faster than ever before.
Ravines
are by no means a recent problem — thousands of hectares of
fertile land along the banks of rivers like Yamuna, Chambal,
Mahi and their tributaries have been ruined by ravine formation
in Uttar Pradesh, Madhya Pradesh, Rajasthan and Gujarat. But
the rapid spread of ravines is a recent phenomenon, more so
in Chambal.
And with
no definitive survey being carried out in the last 20-25 years,
governmental and non-governmental organisations posit differing
estimates. The Science Centre at Gwalior, which started an
awareness campaign on this issue, could only quote the study
done by the Centre for Science and Environment, Delhi: ‘‘In
the last 30 years, ravines have increased by 36 per cent in
Bhind and Morena districts. Between 1943-1950, every year
800-hectare area became ravines in these districts. Between
1950-1975, ravine formation increased, at the rate of 5,000
hectares area every year. Its main reason was large-scale
deforestation. Only 20.58 per cent land has forest cover in
these districts.’’
The absence
of accurate data has fuelled dire predictions. Dr. K. S. Senger
of Government Girls College, Morena, says by 2050, additional
52,000-hectares agricultural land in this region would turn
into ravines. Around 1,500 villages would be ravine-affected
and the per capita land availability would come down from
the present 0.33 hectare to a mere 0.124 hectare.
The ravines
have been spreading despite various government programmes.
In 1970-71, the ‘ravine agriculture scheme’ was launched with
the purpose of restoring shallow ravines for cultivation.
Until 1990, only 1,175 hectares of land had been restored,
but the total expenditure was more than one crore. A central
scheme to last over 28 years was also launched in 1971 by
the Ministry of Home Affairs, with an estimated expenditure
of a whopping Rs 1,224 crore. But in 1972, the scheme was
terminated in its first phase itself.
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