The
Gomti
River
The river Gomti originates from about 3 km east of Pilibhit town of the same district at an
height of 200 meters. The river drains the area lying between river Ramganga and Sharda in
the upper reaches and Ganga
and Ghaghra at the lower reaches. After flowing southwards through the districts of Lucknow,
Barabhanki, Sultanpur, Faizabad and Jaunpur, it confluences with River Ganga.
This river is the chief drainage line of the district and is in fact the only stream of
any importance. In pargana Jagdishpur it winds along the whole of the northern boundary,
separating this district from Barabanki and Faizabad, and receiving all the drainage
of the northern portion of the pargana by various natural water resourses. Along
the upper reaches down to Sathin the banks are high and sometimes precipitous, and the bed
is well marked. South of Sathin the river opens out, the high banks recede, and from Mau
Atwara onwards the low lands are
subject
to damage from flooding. South-eastwards from Jagdishpur the river separates the two
parganas of Isauli on the north and and Musafirkhana on the south. Here, again, the there
is fair extent of lowland, and the river seems to have altered its course in the past, and
looks as if it once ran in a fairly direct line from Fatehpur. At present, however, it
winds along in a fairly well defined bed between stretches of lowlying grounds on either
side. On the north the high cliff are scored with deep ravines, and on either bank there
is much irregular broken ground. Proceeding
in
the same direction, the Gomti separates pargana Miranpur on the south-west from Baraunsa
on the north-east. Here, too, it ordinarily runs between well defined banks, although in
the west of Baraunsa there are some lowlying riparian strips of cultivation. The banks on
the south side in pargana Miranpur are generally of a similar nature, but in places they
sink and the soil is crumbly, considerable damage being done in years of heavy rainfall.
In the east of this pargana the scour from the uplands is considerable, and large ravines
have formed, while here and there the constant erosion has caused much land to be thrown
out of cultivation. The river in these two parganas passes by Chandaur
and Sultanpur. Thence it passes on towards the south-east and separates Aldemau from
Chanda, passing Paparghat, Dera, Dhopap, Aldemau, Kadipur and Dwarka. In this part of the
district the course of the river is tortuous and irregular. In Aldemau the ground in the
vicinity as far as the village
of Katwari
is much cut up by ravines, passing through a block of high light land, which easily lends
itself to erosion. In Chanda the banks are similar, being high and in places precipitous.
In the north of the pargana where the ground along the river is light and highlying
,
ravines have frequently been formed and some land has gone out of cultivation in
consequence. The drainage of the land in its neighbourhood is carried down to the river by
numerous natural channels.
Except in years
of
abnormal rainfall, the Gomti gives no trouble, yet damage is frequently caused by floods
and their consequent effects.
|
It is not possible to construct bridges over it at all the possible end and suitable
points for transportation of people living on both sides. Therefore, the Zila Parishad
auctions various ghats
to
different contractors for making arrangements of ferries for transport purposes. There are
about fifty nine such
ghats
which
are as follows :- Mudwa, Sarriya, Sakhauli, Millenda, Agniholipur, Dipra, Rajghat,
Kurwar, Mansukhpur, Mithenepur, Khadari, Benipur, Lutia, Agai, Hayatnagar,
Bhandara, Nirsaiya, Katawa, Ameliya, Saifullaganj, Gudra, Siwara, Fathepur Dwarika,
Hinduabad, Panhi, Shikaripur, Bhawangawan, Reachghat, Madhuban, Bilehari, Semer,
Payerghat, Phunrwa, Madhusoon, Nanemau, Nari, Gajanpun, Duwaria, Kotwa, Paigupur,
Pakerpur, Katsari, Patana, Pali, Gopinathpur, Sakipur, Umremau, Bhakaripur, Kisuni,
Bhakara, Sathin, Piyari, Kalimeet, Rangawa, Hajiganj, Chndokalarapur,
Bhaddaur, Isauli and Aamghat. |
|