Short Fiction by Edgar Allan Poe (good books for 7th graders .TXT) ๐
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Edgar Allan Poe is one of the primary figures of American nineteenth-century literature. His writing was heavily influenced by Romanticism ideals of emotion and feeling, and although mostly known for his Gothic-tinged horror, his tales jump between many different genres, including science-fiction, satire, humor, mystery, and even early detective fiction.
Poe mostly wrote short stories and poems, published in magazines and periodicals like the Southern Literary Messenger and Grahamโs Magazine, although he also turned his hand to essays and novels (including The Narrative of Arthur Gordon Pym of Nantucket). He was one of the first American writers to pursue writing as a career, but was better received in France than in his native country. He struggled to make ends meet and resorted to work as a literary critic. His reputation suffered a further blow after his unfortunately early death in 1849 at the age of 40, when a rival not only wrote an extremely unflattering obituary, but bought the rights to his work and published a compilation with a hit piece for an introduction. This undeserved reputation took many decades to fade, but didnโt hinder praise from other notable authors including Arthur Conan Doyle and H. P. Lovecraft.
Collected here are all of Poeโs short fiction stories, in order of their original magazine publication. Notable stories include โThe Gold-Bug,โ โThe Black Cat,โ โThe Fall of the House of Usher,โ โThe Masque of the Red Death,โ โThe Pit and the Pendulum,โ โThe Murders in the Rue Morgue,โ and many more.
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- Author: Edgar Allan Poe
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โThe next point to be regarded was a matter of far greater importance. From indications afforded by the barometer, we find that, in ascensions from the surface of the earth we have, at the height of 1,000 feet, left below us about one-thirtieth of the entire mass of atmospheric air, that at 10,600 we have ascended through nearly one-third; and that at 18,000, which is not far from the elevation of Cotopaxi, we have surmounted one-half the material, or, at all events, one-half the ponderable, body of air incumbent upon our globe. It is also calculated that at an altitude not exceeding the hundredth part of the earthโs diameterโ โthat is, not exceeding eighty milesโ โthe rarefaction would be so excessive that animal life could in no manner be sustained, and, moreover, that the most delicate means we possess of ascertaining the presence of the atmosphere would be inadequate to assure us of its existence. But I did not fail to perceive that these latter calculations are founded altogether on our experimental knowledge of the properties of air, and the mechanical laws regulating its dilation and compression, in what may be called, comparatively speaking, the immediate vicinity of the earth itself; and, at the same time, it is taken for granted that animal life is and must be essentially incapable of modification at any given unattainable distance from the surface. Now, all such reasoning and from such data must, of course, be simply analogical. The greatest height ever reached by man was that of 25,000 feet, attained in the aeronautic expedition of Messieurs Gay-Lussac and Biot. This is a moderate altitude, even when compared with the eighty miles in question; and I could not help thinking that the subject admitted room for doubt and great latitude for speculation.
โBut, in point of fact, an ascension being made to any given altitude, the ponderable quantity of air surmounted in any farther ascension is by no means in proportion to the additional height ascended (as may be plainly seen from what has been stated before), but in a ratio constantly decreasing. It is therefore evident that, ascend as high as we may, we cannot, literally speaking, arrive at a limit beyond which no atmosphere is to be found. It must exist, I argued; although it may exist in a state of infinite rarefaction.
โOn the other hand, I was aware that arguments have not been wanting to prove the existence of a real and definite limit to the atmosphere, beyond which there is absolutely no air whatsoever. But a circumstance which has been left out of view by those who contend for such a limit seemed to me, although no positive refutation of their creed, still a point worthy very serious investigation. On comparing the intervals between the successive arrivals of Enckeโs comet at its perihelion, after giving credit, in the most exact manner, for all the disturbances due to the attractions of the planets, it appears that the periods are gradually diminishing; that is to say, the major axis of the cometโs ellipse is growing shorter, in a slow but perfectly regular decrease. Now, this is precisely what ought to be the case, if we suppose a resistance experienced from the comet from an extremely rare ethereal medium pervading the regions of its orbit. For it is evident that such a medium must, in retarding the cometโs velocity, increase its centripetal, by weakening its centrifugal force. In other words, the sunโs attraction would be constantly attaining greater power, and the comet would be drawn nearer at every revolution. Indeed, there is no other way of accounting for the variation in question. But again:โ โThe real diameter of the same cometโs nebulosity is observed to contract rapidly as it approaches the sun, and dilate with equal rapidity in its departure towards its aphelion. Was I not justifiable in supposing with M. Valz, that this apparent condensation of volume has its origin in the compression of the same ethereal medium I have spoken of before, and which is dense in proportion to its vicinity to the sun? The lenticular-shaped phenomenon, also called the zodiacal light, was a matter worthy of attention. This radiance, so apparent in the tropics, and which cannot be mistaken for any meteoric lustre, extends from the horizon obliquely upward, and follows generally the direction of the sunโs equator. It appeared to me evidently in the nature of a rare atmosphere extending from the sun outward, beyond the orbit of Venus at least, and I believed indefinitely farther.10 Indeed, this medium I could not suppose confined to the path of the cometโs ellipse, or to the immediate neighborhood of the sun. It was easy, on the contrary, to imagine it pervading the entire regions of our planetary system, condensed into what we call atmosphere at the planets themselves, and perhaps at some of them modified by considerations, so to speak, purely geological; that is to say, modified, or varied in its proportions (or absolute nature) by matters volatilized from the respective orbs.
โHaving adopted this view of the subject, I had little further hesitation. Granting that on my passage I should meet with atmosphere essentially the same as at the surface of the earth, I conceived that, by means of the very ingenious apparatus of M. Grimm, I should readily be enabled to condense it in sufficient quantity for the purposes of respiration. This would remove the chief obstacle in a journey to the moon. I had indeed spent some money and great labor in adapting the apparatus to the object intended, and confidently looked forward to
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