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The Malay archipelago : the land of the orang-utan ... - Wallace Online

The Malay archipelago : the land of the orang-utan ... - Wallace Online

The Malay archipelago : the land of the orang-utan ... - Wallace Online

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220 THE MALAY ARCHIPELAGO. [chap.<strong>the</strong> little town, with its neat red-tiled white houses and <strong>the</strong>thatched cottages <strong>of</strong> <strong>the</strong> natives, bounded on one side by <strong>the</strong> oldPortuguese fort. Beyond, about half a mile distant, lies <strong>the</strong>larger is<strong>land</strong> in <strong>the</strong> shape <strong>of</strong> a horseshoe, formed <strong>of</strong> a range <strong>of</strong>abrupt hills covered Avith fine forest and nutmeg gardens ; whileclose opjDosite <strong>the</strong> town is <strong>the</strong> volcano, forming a nearly perfectcone, <strong>the</strong> lower part only covered with a light green bushyvegetation. On its north side <strong>the</strong> outline is more uneven, and<strong>the</strong>re is a slight hollow or chasm about one-fifth <strong>of</strong> <strong>the</strong> waydown, from which constantly issue two columns <strong>of</strong> Smoke, whichalso rises less abundantly from <strong>the</strong> rugged surface around andfrom some spots nearer <strong>the</strong> summit. A white efilorescence,probably sulphur, is thickly spread over <strong>the</strong> upper part <strong>of</strong> <strong>the</strong>mountain, marked by <strong>the</strong> narrow black vertical lines <strong>of</strong> watergullies. <strong>The</strong> smoke unites as it rises, and forms a dense cloud,which in calm damp wea<strong>the</strong>r spreads out into a wide canopyhiding <strong>the</strong> toj) <strong>of</strong> <strong>the</strong> mountain. At night and early morning it<strong>of</strong>ten rises up straight and leaves <strong>the</strong> whole outline cleai'.It is only when actually gazing on an active volcano that onecan fully realize its awfulness and grandeur. Whence comesthat inexhaustible fire whose dense and sulphureous smoke forever issues from this bare and desolate peak? Whence <strong>the</strong>mighty forces that produced that peak, and still from time totime exhibit <strong>the</strong>mselves in <strong>the</strong> earthquakes that always occur in<strong>the</strong> \dcinity <strong>of</strong> volcanic vents ? <strong>The</strong> knowledge from childhood,<strong>of</strong> tlie fact that volcanoes and earthquakes exist, lias taken awaysomewhat <strong>of</strong> <strong>the</strong> strange and exceptional character that reallybelongs to <strong>the</strong>m. Tlie inhabitant <strong>of</strong> most parts <strong>of</strong> nor<strong>the</strong>rnEurope sees in <strong>the</strong> earth <strong>the</strong> emblem <strong>of</strong> stability and repose.His whole life-experience, and that <strong>of</strong> all his age and generation,teaches him that <strong>the</strong> earth is solid and firm, that its massiverocks may contain water in abundance but never fire ; and<strong>the</strong>se essential characteristics <strong>of</strong> <strong>the</strong> earth are manifest in everymountain his country contains. A volcano is a fact opposed toall this mass <strong>of</strong> experience, a fact <strong>of</strong> so awful a character that,if it were <strong>the</strong> rule instead <strong>of</strong> <strong>the</strong> exception, it would make <strong>the</strong>eartli uninhabitable ; a fact so strange and unaccountable thatwe may be sure it would not be believed on any human testimony,if presented to us now for <strong>the</strong> first time, as a naturalphenomenon happening in a distant country.<strong>The</strong> summit <strong>of</strong> <strong>the</strong> small is<strong>land</strong> is composed <strong>of</strong> a highly crystallinebasalt ; lower down I found a hard stratified slaty sandstone,wliile on <strong>the</strong> beach are huge blocks <strong>of</strong> lava, and scattered masses<strong>of</strong> white coralline limestone. <strong>The</strong> larger is<strong>land</strong> has coral rock toa height <strong>of</strong> three or four hundred feet, while above is lava andbasalt. It seems probable, <strong>the</strong>refore, that this little group <strong>of</strong>four is<strong>land</strong>s is <strong>the</strong> fragment <strong>of</strong> a larger district which was perhapsonce connected with Ceram, but which was separated andbroken up by <strong>the</strong> same forces which formed <strong>the</strong> volcanic cone.When I \'isited <strong>the</strong> larger is<strong>land</strong> on ano<strong>the</strong>r occasion, I saw a

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