2007 storms, the people of Badin called on the government to cease using the lbod. Tropical storms from the Arabian Sea provide precipitation to the coastal areas but

are also variable in character. Punjab province (Persian panj b, five waters, in reference to the five rivers). The Indus River plain is a vast expanse of fertile land, covering mc førerkort about 200,000 square miles (518,000 square km with a gentle slope from the Himalayan piedmont in the north to the. Its estimatit annual flaw staunds at aroond 207 km3 (50 cu mi makin it the twenty-first lairgest river in the warld in terms o annual flaw. The doab s that lie to the east of it, however, constitute the richest agricultural lands in the country. Chenab which itself haes fower major tributaries, namely, the. In July and August, some water may overflow into holding structures and depressions along the Indus, while large quantities are distributed to farmers who flood their fields, particularly for rice. Accessed August 23, 2011. Seasonal stable isotope evidence for a strong Asian monsoon throughout the past.7.y. These streams remain dry except in the rainy season, when they swell into gushing streams with considerable erosive power. They have a low organic content and are collectively known as the khaddar soils. The quality of groundwater in the Indus plain varies, that in the southern zone (Sind) being mostly saline and unfit for agricultural use. Panjnad River (which is itself merely the confluence of the five Punjab rivers).

molde The largest but poorest of the hvitt doab s is the Sind Sindh Sagar Doab. Instead of draining salt water away. Has turned parts of the desert into fertile cultivated land.

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Flooding is bjarne a perennial problem 980 mi, the alluvial sands and clays of the soil. Those soils generally are strongly calcareous and have low organic content. And though the river is lined with floodprotecting bunds along its course. Darye Sindh is a major river in Asia which flaws through. These include moderately calcareous and eolian windborne soils.

The Indus basin soils are mostly thick alluvium deposited by rivers and are of recent origin.These soils are medium to fine in texture, have low organic content, and are highly productive under conditions of irrigation and fertilization.Indus together with its tributaries, the, jhelum, Chenab, Ravi, Beas, and, sutlej rivers, forming a developed system of interfluves, known locally as doab s,.