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TheImprovement ofTropical and Subtropical Rangelands

TheImprovement ofTropical and Subtropical Rangelands

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THE MARRl BALUOH OF PAKISTAN 289<br />

valley, the main trend of the ridges is east-west. Valley bottoms <strong>and</strong><br />

plateaus in the main Marri tribal area vary from 800 to 1,000 m in<br />

elevation, while hill elevations gradually increase from 1,000 m in the<br />

south to over 3,000 m in the Pathan districts to the north. Passes<br />

are few <strong>and</strong> widely scattered <strong>and</strong> paaage from one valley to the next<br />

is often a problem. The result is a confused drainage pattern, the<br />

east slopes of the Sulaiman mountains draining directly to the Indus,<br />

whereas the remainder of the surface runoff is discharged toward the<br />

southwest into the plains around Sibi.<br />

Most of these streams flow during no more than two months of<br />

the year (July <strong>and</strong> August), <strong>and</strong> the seasonal nature of the stream<br />

flow is directly related to the paucity of the region's precipitation.<br />

Rainfall totals are low, averaging 75-125 mm in the lowl<strong>and</strong>s, while<br />

totals as high as 300 mm have been recorded under orographic conditions<br />

in the northern mountains. 6 Although rain occasionally falls<br />

in winter-the result of very infrequent cyclonic storms of low mois.­<br />

ture content that drift in from the eastern Mediterranean-the main<br />

rainfall occurs in July, August, <strong>and</strong> early September. Coming at the<br />

end of the summer monsoon, this rain, sporadic in distribution <strong>and</strong><br />

violent in character, falls in the form of torrential thunder showers<br />

that give rise to heavyflooding. Although streams flow only during<br />

part of the year, subsurface water in streambeds is usually available<br />

with only a small amount of digging.<br />

Not only is rainfall sporadic in distribution <strong>and</strong> sparse in quantity,<br />

but it also occurs during the hottest part of the year, thus<br />

lessening its efFectivenese. Temperatures in excese of SOOC are not<br />

uncommon in the Sibi plains during the summer. Highl<strong>and</strong> temperatures<br />

tend to be cool in summer <strong>and</strong> cold in winter, 80 that a marked<br />

daily <strong>and</strong> seasonal temperature range is characteristic. The combination<br />

of high temperatures <strong>and</strong> low rainfall totals produces a scanty<br />

vegetation cover, <strong>and</strong> vegetation, like temperature conditions, tends<br />

to be distributed altitudinally.e On the higher elevations are found<br />

IlCattered st<strong>and</strong>s of juniper, pistachio, ash, <strong>and</strong> wild almond, while<br />

acacias (AcGciG niloticG, A. modutG), olives, <strong>and</strong> occasional poplar<br />

(Populu euphrGticG),T blue gum (Et&cGI"tu), <strong>and</strong> willow trees are<br />

found in the lower hills. In the valleys, dwarf palm (NGnno"hop.<br />

ritchieGnG), tamarisk (TGmGriz indicG), Zi.,phu nummulGriG, <strong>and</strong><br />

occasional myrtle groves are common. Annual grasses <strong>and</strong> herbs are<br />

IlCattered everywhere, <strong>and</strong> it is their fluorescence in late spring <strong>and</strong><br />

continued presence in summer, together with that of the trees <strong>and</strong><br />

shrubs, that give the area its best pastures.'

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