TitleET N [ 8 ] E T N

CaptionEta.

Text(our author fays) it would be difficult to make people, who have never engaged in this enterprise, company hend all the oblidies they had to encounter. This cone (the little mountain mentioned by Sir William Flamman) is composed of the very hand, and postsecondary throw up a different times by the volcano. The mar- terials are lo boic, that the adventures traveller links about midly as every May, and is to contain terror of being feallowed up. Ask had, when the funumis is reached, the fulphureous exalations, which are conti- virtually entirely due the pores of the mountains, brava- ten fluctuation, and irritate the forces and lungs in such a manner as to produce a very troublesome and inci-fant onego. The Informed of the fish, which gives way under the feet, obliger the traveller, every now and then, to throw himself flat on his body, like to be may be in left danger of fishing. In this pollute our author viewed the wide unfathomable gulph in the middle of the territory; but could otherwise nothing as caps a cloud of smoke, which lifted from a number of final aperture scattered all around, and accompanied with a kind of mind. Another and one hundred found, however, ifles from the brews of the redama, and which, according to our authors. "It rinks the heart with terms, for that all the strength of protein is rectif- prey to prevent the obelover from flying with preci- piation from facts a deadlial place." Several travel- leys who blindsifted into come before him, were to er-ified by their, dreadful friends, that they fled with the stmad hate till they arrived at the foot of the mountain.

TextOur author compares thefe funds to a discharge of common in the few days, is no roof of which, is the believed throughout all the cavears, and produces found perhaps the moft alarming that can be imagined; and during the short faces in which the illensary, real of their discifery were heard to follow one another almost uninterruptedly.

TextThis deadline note our author, with very great probability, fuppaid to be occasioned by the esplo- fons of the internal fire, or, as he calls is, the focus of the volume, which, filking squall the files of their domestic cavares, the found products are received through their cavities, and probably multiplied in an extraordinary memory. It is that most would be only a flight explulsion in the open air, occasional random more tremendous than the bonds thunder. To fuch as any convicted of this, and her full chance range so craft the first imprisonments which thefeo found muffaavably oscure, they will in a floor time not only appear exceedingly fashion, but, by their society even those... what agreeable. "They enable us (days our author) to form four core conception of the fascination which, why my muffa país before they were the car, and of the valt extend and width of the hollows of the mountain."

TextHinry for four time time completed the avulla fpec- tudo, our author whiled to matches the water by walk- ing sound it’s hot found this impulble. On the north flee, the farber is hard and, though, she also having been to for diffused by the mother deposited by the finde as to cement into one uniform mafs. This is fonctions followed even once a fluid here, its fact a manner as to run down the files of the case; is, that after several attempts, he was at lab obliged to abandon his deligen.

TextFig. 2 exhibits a view of the crater of Eta taken No 121,

Texton the brick of the raft ride. The foreground (or a) of Ften. the figure is one division of the crater. Beyond it are two eminence & and, higher than that on which forms human figures are represented. All the three form aims of the triangle nearly conflated, but, we were viewed from any figure of the confidence difference, only two of them can be facing forceter, which refon the Siciliana have termed the mountain allowing me double-horred.

TextThe finokes, as reproefident in the figure, ifles from all quarters, other form chains or holes detected over the whole crater. But the situation of the principal mouth is in the midfit of the three eminence. Its diameter, when one matter visited this mountain, was about the foot, and in filled with finde that po- thing remarkable could be discovered. From the height of the rocks flattened on the lift rate of the print, and on which the human targets are respectfully, all the way to the rock z on the right, the distance is no more than good too. Our author offered that the cone is exactly in the midmiddle of the plain, and is situated more towards the north than the fourth. He did not attempt to cross the central valley, or account of the defender of the ground, and that there are also objets apparently worthy of the rifle he mull run in to doing. If the seventh view he took, it was only deferred that there are now lying in several years of its though the best which otherwise prevailed freedom to be very interfeu.

TextThe finde which differ from the current of Eta is generally carried in a direction from forth to northy and, as it bring along with it a comfortable quantity of water, the latter, conducted by the cold winds, runs down the tide of the mountain in plentifils means, and often leaves pretty permanent marks of its courier.

TextIn the mainte he accounts for the great eruption of water in 1755, which he fuppoder to have been oc-water in colored only by an unusual quantity of water falling into 1733, as- the burned fears of the mountains, here needed more for, foam, and afterwards condensed by the coldness of the atmosphere.

TextLike other travellers to mount Etaa, this gentleman South wind found the wind blowing from the fourth ; and he is of generally opinion, that a fortunately allows here now requested on the top than any other, as he did not observe any channels curral drama by the water on any other side than the north. He had reversal operation of making this discussion, having frequently visited the top of Etaa, and always paid attention to the crater. The fault on the cuf and well field was always loads, while that on the north was compelled into a fold body. The three formamists were of a later date than the rest of the crater, having been probably thrown up by bone eruption, which had burt aunner. The black spots on the foreground repet- fest a number of hillsides about the rise of mole-hills, from which a fulphumous yearn confronts flyer, and by which the adjacent ground is tinged of an ochery color. This vapor filter from the creatives with a cut of shallow whilling outfer, which with the woke- nic thunder, frooks, and noxious fipil, render it very different to the flare ever for a few moments.

TextThe findex is reproduced in the figures precisely as it did on the day that he afecided, which was very warm. But it does not always life in this moment, for white the cold always richts, collects into a body, and thickens around the edge of the crater; on which oc- cutions it is condensed into water, which difficile itself around the edge of the crater, and mixing with the alheshegues