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SANDOWAY

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Originally appearing in Volume V24, Page 140 of the 1911 Encyclopedia Britannica.
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SANDOWAY , a See also:

town and See also:district in the See also:Arakan See also:division of See also:Lower See also:Burma. The town (pop. 1901, 12,845) is very See also:ancient, and is said to have been at one See also:time the See also:capital of Arakan. The district has an See also:area of 3784 sq. m.; pop. (1901) 90,927, showing an increase of 16 % in the See also:decade. The See also:country is mountainous, the Arakan range sending out spurs which reach the See also:coast. Some of the peaks in the N. attain 4000 and more ft. The streams are only See also:mountain torrents to within a few See also:miles of the coast; the mouth of the Khwa forms a See also:good anchorage for vessels of from 9 to 10 ft. See also:draught. The rocks in the Arakan range and its spurs are metamorphic, and comprise See also:clay, slates, ironstone and indurated See also:sandstone; towards the S., ironstone, See also:trap and rocks of basaltic See also:character are See also:common; See also:veins of steatite and See also:white fibrous See also:quartz are also found. The rainfall in 1905 was 230'49 in. Except a few acres of See also:tobacco, all the cultivation is See also:rice. Sandoway was ceded to the See also:British, with the See also:rest of Arakan, by the treaty of Yandabo in 1826.

End of Article: SANDOWAY

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