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Imperial Gazetteer of India, v. 6, p. 165.


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of Moradabad city. Population (1901), 7,452. According to tradition,
it was founded in the time of Prithwi Raj. The town contains several
mosques and a temple. It is administered under Act XX of I856, with
an income of about Rs. 1,300. A primary school has 78 pupils.
Backergunge (Bdkarganj, 'Mart of Agha Bakar').-Southern-
most District of the Dacca Division, Eastern Bengal and Assam, lying
between 2I° 49' and 23° 5' N. and 89° 52' and 9I° 2' E., with an area
of 4,542 square miles. It is bounded on the north by Faridpur; on
the east by the Meghna and Shahbazpur rivers, which separate it from
Noakhali; on the south by the Bay of Bengal; and on the west by
the Baleswar river and its estuary the Haringhata, which divide it from
Khulna.
Backergunge is a typical part of the alluvial delta formed by the three
great river systems of Eastern Bengal. The District consists partly of
mainland and partly of islands in the estuary of the
Meghna, the largest being DAKHIN SHAHBXZPUR, and aspects.
forms an unbroken plain intersected by a network of
sluggish and muddy tidal rivers and channels, with a slight decline from
the east towards the west and north-west. Along the coast-line of the
Bay lie the SUNDARBANS, a group of half-reclaimed islands separated by
tidal creeks, which cover an area in this District of 897 square miles.
The MEGHNA estuary, here some 8 miles in breadth, sweeps past the
east of the District, and is divided by the Dakhin Shahbazpur island
into an eastern branch called the Shahbazpur, and a western known as
the Tetulia river. The Arial Khan is a branch of the Ganges; it crosses
the north-east corner of the District, and joins the Meghna through the
Mashkata and Kalinga channels. The river system consists of offshoots
from the Meghna estuary and the tributaries and distributaries of the
Arial Khan and Baleswar (as the MADHUMATI is called in its lower
reaches), which ramify into channels intersecting the District in every
direction. A perplexing multiplicity of names extends even to the
smaller watercourses, which are often known by different names to
villagers living on opposite banks, while the Meghna estuary itself is
known in different parts of its course as the Satbaria, the Ilsa, the
Tetulia, and the Shahbazpur. Most of the rivers and water-channels
are navigable throughout the year and are subject to tidal action, which
however is powerless during the freshes of the rainy season to arrest the
seaward flow of the immense volume of rain-water pouring down the
big rivers. Alluvion and diluvion are constantly taking place, especially
towards the east, where the District is washed by the Meghna. On the
north and east of the island of Dakhin Shahbazpur, the land is being
rapidly cut away, while on its western shore a corresponding formation
is taking place and large alluvial accretions are being thrown up in the
estuary, the names of which indicate their recent origin. There is a very



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