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The universal geography : earth and its inhabitants

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TOrOGRAl'UY OF MAri'.l'.KI.KLAND. 271Further auriferous depos<strong>its</strong> wore brought to light by Mr. F. C. Selous duriugan ex2)loriug expedition to the Mashoua country, from which he returned inJanuary, 1888. A considerable tract of alluvial gold-fields was discovered, besidesa very remarkable excavation in solid rock, which Mr. Selous believes to be amine of very ancient date. On this subject he writes :" At Sinoia, near the riverAngwa (a tributary of the Mauyame), there is an immense circular hole about aliundred feet or more in depth <strong>and</strong> sixty feet or more in diameter, at the bottom ofwhich is a pool of water which extends some hundred <strong>and</strong> eight}- feet into a vastcavern in the rock. <strong>The</strong> water is of the most wonderful colour—a deep cobaltblue—<strong>and</strong> very clear, as pebbles are visible al a great depth on the bottom.<strong>The</strong>reis a slanting shaft or tunnel running at an angle of about forty-five degrees from apoint about a hundred yards distant from the top of tlie hole, a\ Inch strikes thebottom of the latter just at the edge of the water. "\Ve are inclined to think thatall these excavation.s are the result of old gold-workings, <strong>and</strong> that a vein of quartzlias been worked out down the tunnel, <strong>and</strong> that eventually a spring was tapped,tlie water of which, welling up from below, has formed the subterranean lake.the whole thing is the work of man, a truly extraordinary amount of labour musthave been expended in this place. <strong>The</strong> natives have built a stockaded town roundthe old gold mine, or whatever it is, <strong>and</strong> go down the tunnel to draw water. Webathed in it <strong>and</strong> swam up the cavern to the other end of the pool ; the water wasquite warm. <strong>The</strong> rock on each side is covered with innumerable scorings, whichlook as if they had been done with some kind of iron instrument." *Senna, or Sffo-J/r/rr^^/, the " moribimd," which lies on the right bank of theZambese, at the foot of a high bluff, <strong>and</strong> over against the navigable Ziu-Ziu branchcommunicating with the Shire, is even a more decayed place than Tetc. It hasoften had to pay tribute to <strong>its</strong> Umgoni (Angoui Zulu) neighbours, <strong>and</strong> even tobarricade <strong>its</strong>elf at night against the lions. <strong>The</strong> climate also is imhealthy, theatmosphere being charged with malarious vapours rising from the stagnant watersleft by the river, which is here gradually shitting <strong>its</strong> bed in the direction of thenorth. Hence it has been pro2JOsed to remove the town to the left or north sideof the Zambese, which is swept by the current, without leaving any lagoons orsluggish backwaters.IfiMr.vmxAMS OF the Nv.\.ss.v <strong>and</strong> Siiikk Basi.n~.South of the Zambese the military empires of Gazal<strong>and</strong> <strong>and</strong> Matebelelaud \wrcfounded by warlike Zidu conquerors, advancing from the south. North of theriver vast territories have also been occupied by invaders of the same martialrace. But being here di^-ided into independent b<strong>and</strong>s, without any nationalcohesion, they have been unable to found any powerful states. <strong>The</strong>se Kafirs,variously known as Mavitis (^la-Viti) <strong>and</strong> Ma/itus (Ma-Zitu), are the Munhacs ofGamitto, <strong>and</strong> are also called ilangoncs (Ma-Xgone'l, a name almost identical withthat of the Umgoni invaders <strong>and</strong> conquerors of the region comprised between the• r,ocee,i,iigs of the Roijal Gfog,-apl„cal .W.'./y, ir;iivli, ISSS, p. 101.

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