| Voice of Rajveer Bharadwaj
: Rajveer Bharadwaj

JindDistrict
Area, Population & Sex Ratio
Geographical Area : 2702.0 Km2
Population in Jind (Census 2011)
Total Population
Total : 1332042
Male : 712254
Female : 619788
Disabled population
Total disabled population : 31107
In seeing : 15205
In speech : 1425
In hearing : 1683
In movement : 10019
Mental : 2775
Rank ( VoiceOfBharat.org Analysis
)
Backwardness : 436
Sex Ratio Rank : 46
(Rank one is least sex ratio - Cenus 2001)
HIV Category District : C
(HIV Sentinel Surveillance 2004 -2006)
Disability : 297 (Census 2001)
Literacy Ratio : 333 (Census 2001)
Minority : Does not figure in MCD
Water : Flouride in Groundwater above permissible limits

Brief About Jind District
ORIGIN AND NAME OF THE DISTRICT
The district derives its name from its headquarters town Jind that
is said to be a corruption of Jaintapuri. It is also said that this
town had been founded at the time of Mahabharta. According to an
old saying the Pandavas built a temple in honour of Jainti Devi
(the goddess of victory), offered prayers for success, and then
launched the battle with the Kauravas. The town grew up around the
temple and was named Jaintapuri (Abode of Jainti Devi) which later
on came to be known as Jind.
Location, Boundaries
And Area Of The District
Location
The district lies in the North
of Haryana between 29.03’ and 29.51’ North latitude & 75.53’
and 76.47’ East longitude. On its East and North-East lie the districts
of Panipat, Karnal and Kaithal respectively. Its boundary line on
the North forms the inter-state Haryana- Punjab border with Patiala
and Sangurar districts of Punjab. In the West and South-West it
has a common boundary with district Hisar & Fatehabad and in
its South and South-East lies the district of Rohtak and Sonipat
respectively.
Area
The area of the district
is 3,606 square kilometers.
Sub-Division &
Tahsils The district is divided into three Sub-Divisionns,
Jind Safidon and Narwana. The Jind Sub-Division comprises two tahsils,
viz. Jind and Julana. While the Narwana, Safidon Sub-Divisions comprises
the Narwana & Safidon tahsil respectively .
PHYSIOGRAPHY
The district of Jind
stretching in the northwest to southeast direction occupies the
north-central part of the Haryana. Physiographically, it constitutes
a part of the Punjab-Haryana plain, which is largely flat and featureless
and is formed of Pleistocene and sub-recent alluvial deposits of
the Indo-Gangetic system. Wind action in the past and man’s role
in recent times have played a prominent part in shaping the relief
of the district which is
located in a transitional zone between the sub-humid districts Kaithal, Panipat and Karnal in the
east and the semi-arid district
Hisar in the west.
Broadly speaking,
the district is a flat, monotonous upland plain. It is evident from
the fact that the general elevation of the district ranges between
218 meters and 239 meters above sea level. As the spot-heights are
examined more closely, one discovers that there is no general and
consistent trend in the slope of the area. However, the northern
part of Narwana tahsil presents a saucer like shape having the highest
elevation of 239 meters in the extreme north near Sanghan village. As one moves south-westward, the
ground level gradually declines reaching its lowest of 226 meters
near the town of Narwana from where it again starts rising until
it reaches 232 meters near Durjanpur village almost on the district’s
border. The southern half of the district, consisting of Jind and Safion tahsils on the other
hand offers a fradual east-to-west slope. The highest point in this
part of the district is reached near village Bahri (232 meters)
and the lowest elevation of 218 meters is met near Rajpura village
in the west along the district border with Hisar district.
There are minor undulations
in the general physiographic formation of the district. These undulations
characterise the area having been subject to wind action in the
past and owe their existence to the presence of sand dunes, sand
ridges and depressions at places. The sand dunes/ridges are now
stable generally having a local relief of 2 to 6 meters.
The largest and the highest sand dune of the district lying north-west
of Kakrod village (Narwana tahsil) on Hisar-Jind border is 2 Kilometers
long and quarter a kilometer wide and has a local relief of 6 meters.
This is the area where large sand ridges occur the most, particularly to the south-west
of Kakrod village. Other areas where sanddunnes occur frequently
are (i) the area along Hisar border between Sulhera village in the
north and Danauda Khurd village in the south where the local relief
ranges between 2 to
5 meters; (ii) the area in the vicinity of village Ashrafgarh, especially
south-west and south of the village where the sand dunes rise from
2 to 4 meters above the local relief (iii) the small area lying
to south of Julani village (west of Jind town); and (iv) the area
in the proximity of Jai Jai Wanti village in
Jind tahsil which
has wide undulations but where the local relief variations do not
exceed 4 meters.
These sand ridges
apart, one also comes
across thee depressions at places. The largest of such depressions
lies south of Bhambewa village in Safidon tahsil just on the district
border with sonipat district. This depression extends over 1.5 kilometers
of length and about one kilometers of width and is about 5 metres
deep. Another depression occurs north of village Bithmara (Narwana
tahsil ) which extends over 1 kilometer in length and about half
a kilometer in
width. The third lies to south of Safidon near village Bahaderpur
and it extends over one kilometer in length and kilometer in width.
In brief, the district
does not offer much physiographic diversity. It is
flat, featureless, alluvial upland plain dotted only sporadically
with sand dunes and depressions, yielding a local relief of not
more than 6 metres either way.
Drainage :
With regard to the drainage pattern, the complete absence
of major or minor rivers/streams defies any detailed discussion
on drainage. However, it is necessary to mention the entry and termination
of Chautang river into the district near the village Mundh and its
termination near village Bosini into Karnal district after covering
about a distance of ten kilometers in Jind district
GEOLOGY
The district, by
and large, is underlain by the quaternary alluvium, comprising chiefly
clays, sand of various grades, kankar and occasionally gravel and
pebbles. It has been observed that the clayey material generally
constitutes between 31 and 81 percent of the caustic sediments down
to a maximum drilled depth of about 151 meters from the ground level.
Granular material comprising chiefly fine to coarse grained sand
with occasional pebbles appear
to be ventricular in
shape with their longer axes generally running in the north-south
direction.
CLIMATE
The climate of this
district is on the whole dry, hot in summer and cold in winter.
The year may be divided into four seasons. The cold season from
november to march is followed by hot season which lasts till the
onset of the south-west monsoon. The monsoon withdraws by 15 September
and is followed by the Post-monsoon or the transition period.
Rainfall
The average rainfall
over the district as a whole is 55 cm. It generally increases from
south or south-west to east or north-east. Over 70 per cent of the
annual rainfall is received during the monsoon months of July to
September. July and August are the rainiest months, together accounting
for over 50 per cent of the annual rainfall. Per-monsoon rainfall
in June constitutes just about 10 per cent of the annual normal.
Some precipitation, constituting about 10 per cent of the annual
rainfall, is also received during the winter months of December
to Februrary in association with western disturbances which pass
across the district or its neighborhood from west to east, affecting
the weather over the district in this season. The variation in annual
rainfall from year to year is large. In 48 years during 1901 to
1948, Jind which is the only station in the district with a long
period of rainfall record, had 220 per cent of the annual normal
rain in 1933 and only 29 per cent in 1939. Considering the rainfall
in individual years during 48 years, it was less than 80 per cent of
the annual normal in
15 years, including one spell of consecutive 5 years and one of
consecutive two years.
The average number of rainy days for the district is only
25 out of which 18 days are confined to the months of
June to September and 4 days to the winter months of December
to March. This shows that rainfall occurs mainly as showers.
The heaviest rainfall
recorded in the district in 24 hours was 225.5 mm at Jind on 11th
July 1953.
Temperature
There is no meteorological
observatory in the district, On the basis of records
of the observatories in the neighboring districts where similar
climatic conditions prevail, it is stated that from the beginning
of March, temperature increases rapidly till June which is generally
the warmest month. The mean daily maximum temperature during June
is around 41C and the mean daily minimum around 27C. The heat in
summer in intense. On individual days, the day temperature may occasionally
exceed 47 or 48 C. Scorching dust laden winds which blow during
the hot season render the weather very tiring. Afternoon thunder
showers which occur on some days bring some relief although only
temporarily. With the onset of the monsoon by the end of June or
beginning of July there is a drop
in the day temperature but the nights are nearly as warm
as in June. Due to the increase humidity in the air, the weather
is oppressive between the rains. After the withdrawal of the monsoon
by about the middle of September there is a decrease in temperature,
the fall in the night temperature being more rapid. After October
both day and night temperature decreases rapidly. January is usually
the coldest month with the mean daily maximum temperature at about
21 C , and the mean daily minimum at about 6 C in the cold season.
Particularly in January and February, cold winds in the wake of
passing western disturbances affect the district and the minimum
temperature occasionally drops down to below the freezing point
of water.
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