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Download - foreverindus.org - WWF - Pakistan

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Final Report of Vegetation Assessment<br />

2.1 Brief History of Keti Bundar<br />

Keti Bundar is located at a distance of about 200 km SE of Karachi in Thatta district of Sindh<br />

province. It is a Taluka (Tehsil) of Thatta district and consists of a total of 42 dehs (cluster of<br />

villages) that spread over a total area of 60,969 hectare. It is believed that the sea has<br />

engulfed 28 dehs and the total affected area in Keti Bundar is around 46,137 hectare (<strong>WWF</strong><br />

2004). Hoekstra et al. (1997) mentioned that Keti Bundar Tehsil includes a total of 19 Dehs<br />

and 29 villages while total human population is around 12000.<br />

Historically Keti Bundar was a port city before the construction of any dams and barrages on<br />

Indus river. At that time river was navigable up to Thatta and even upwards.<br />

At present, it is one of the major towns along the <strong>Pakistan</strong> coastline that is facing<br />

environmental degradation and loss of livelihood opportunities for the locals. Local elders<br />

mention that the location of Keti Bundar town has changed thrice during the past 70 years due<br />

to progressive intrusion of the seawater. There are four major creeks in the area viz. Chann,<br />

Hajamro, Khobar and Kangri with innumerable small creeks. For sweet water (drinking and<br />

farming), Keti Bundar and other coastal region depend entirely on Indus River and its<br />

distributaries.<br />

Keti Bundar is located in Indus Delta experiencing warm monsoon climatic regime. Mild<br />

winters extend from November to February while summer season extends from March to<br />

October. Most of the annual precipitation falls during monsoon, which is erratic in distribution.<br />

Mean annual rainfall is 220 mm. January is the coolest month with minimum temperature of<br />

9.5 o C while in June – July minimum and maximum temperatures range from 23 o C – 26 o C<br />

and from 30 o C - 36 o C, respectively. Humidity is generally higher in the morning than in the<br />

afternoon. It also varies from place to place depending upon the proximity to the sea. Wind is<br />

another important feature of coastal zone. It is variable and is faster during summer (7.4 to<br />

20.5 km/h) than winter (Qureshi 1985).<br />

Before construction of upstream barrages, river water used to reach the tail end during low<br />

tides round the year. However, upstream dams and barrages have considerably reduced the<br />

river flow to the extent that Kharo Chan and Shah Bundar area that had good agrarian<br />

economy in the past and produced plenty of high quality red rice, are now facing acute water<br />

shortage. During aabkalani (flood season), water is stored in ponds for subsequent human<br />

and livestock use. The agriculture has now deteriorated due to water logging and salinity of<br />

lands. During off season (May to<br />

August), local people were dependent<br />

on agriculture practices in the past<br />

and fish during other months of the<br />

year (Qureshi 1985). Scarcity of fresh<br />

water in the area from the Indus and<br />

seawater intrusion into the land has<br />

been degrading the area.<br />

Communities in and around main<br />

creeks in Keti Bundar area have<br />

cattle, buffaloes and camels. Camels<br />

have popularly supposed to have<br />

aversion to water and not to thrive in<br />

damp areas but in Delta region,<br />

camels feed on mangrove foliage,<br />

wading in the mud and swim in the<br />

creeks (Hoekstra et al. 1997). Faqirani Jat community in Keti Bundar kept majority of the<br />

camels. During monsoon season, camels of inland communities are also grazed in creeks<br />

Indus For All Programme Page 14 of 131

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