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An Embassy to the Court of the Teshoo Lama in Tibet - Prajna Quest

An Embassy to the Court of the Teshoo Lama in Tibet - Prajna Quest

An Embassy to the Court of the Teshoo Lama in Tibet - Prajna Quest

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;206 TIBET.At <strong>the</strong> end <strong>of</strong> <strong>the</strong> next day's journey, we came <strong>to</strong><strong>the</strong> source <strong>of</strong> ariver, which ran <strong>to</strong>wards <strong>the</strong> north, near which we travelled all <strong>the</strong> way<strong>to</strong> its confluence with <strong>the</strong> Berhampooter, a little beyond <strong>Teshoo</strong> Loomboo.The Berhampooter <strong>the</strong>re flows <strong>in</strong> a very widely extended bed, andpasses on^ shap<strong>in</strong>g its course <strong>to</strong> <strong>the</strong> south <strong>of</strong> Lassa; it afterwards takesa vast circuit through <strong>the</strong> mounta<strong>in</strong>s on <strong>the</strong> borders<strong>of</strong> <strong>Tibet</strong>, beforeitenters <strong>the</strong> k<strong>in</strong>gdom <strong>of</strong> Assam, and f<strong>in</strong>ally jo<strong>in</strong>s <strong>the</strong> Ganges, <strong>in</strong> Bengal.These great rivers, when united, take <strong>to</strong>ge<strong>the</strong>r <strong>the</strong> name <strong>of</strong> Megna,and flow but a short distance, before <strong>the</strong>y divide <strong>in</strong><strong>to</strong> <strong>in</strong>numerablestreams, that <strong>in</strong>tersect <strong>the</strong> terri<strong>to</strong>ry, which is called <strong>the</strong> Sunderbunds,<strong>in</strong> a most <strong>in</strong>tricate labyr<strong>in</strong>th, and <strong>the</strong>n f<strong>in</strong>ally mix <strong>the</strong>ir waters with <strong>the</strong>sea.The prodigious difl'erence <strong>of</strong> climate affords, also, strong testimony<strong>to</strong> <strong>the</strong> truth <strong>of</strong> my assertion, respect<strong>in</strong>g <strong>the</strong> height <strong>of</strong> this part <strong>of</strong><strong>Tibet</strong>. Perpetual w<strong>in</strong>ter may be said <strong>to</strong> reign at Phari ; Chumulareeis for ever clo<strong>the</strong>d with snow; and this mounta<strong>in</strong>, from its remarkableform, leaves no room <strong>to</strong> doubt its be<strong>in</strong>g <strong>the</strong> same, which I haveheard described as occasionally visible from Purnea and Rajemahland wliich I once saw, before 1 set out from Rungpore upon my presentjourney. I had not <strong>the</strong> means <strong>to</strong> ascerta<strong>in</strong> its elevation; but some <strong>in</strong>ferencemay, perhaps, be drawn from analogy.We hear, that on MountLebanon <strong>in</strong> Syria, snow does not rema<strong>in</strong> through <strong>the</strong> whole year, except<strong>in</strong> <strong>the</strong> highest cavities. Now it is well known that snow, under <strong>the</strong>secircumstances, <strong>in</strong> that latitude (34° 30' north), requires an elevation <strong>of</strong>1500 or 160 fathoms above <strong>the</strong> level <strong>of</strong> <strong>the</strong> sea. The l<strong>of</strong>tiest <strong>of</strong> <strong>the</strong>Alps, which is Mount Blanc, is estimated at 2,400;<strong>the</strong> Peak <strong>of</strong> Ossian,<strong>in</strong> <strong>the</strong> Pyrenees, is said <strong>to</strong> be 1900 fathoms above <strong>the</strong> level <strong>of</strong> <strong>the</strong> sea;

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