WORST IN WO Comprehensive History of Volcanoes in the Past. WASTE OF LIFE AND PROPERTY Account of the Greatest Disaster of' Recorded Time?A Little World Is Blotted off the /lap. Volcanoes and earthquakes have al >aye been the most dreaded by humanity of all calamities that could befall a community. The causes producing the two geological disturbances so prolific of fear and terrible havoc are practically the same. They result from the fact that the interior of th's globe is still intensely hot, radiating heat into space and consequently contracting in bulk. Portions of molten rock are from time to time ejected and sudden seismic disturbances occur which cause destruction like that at St. Pierre from?volcanic erup- < tions, or the earthquakes which have recently Kinea nunareus 01 peopie m several of the Central American countries. During the existence of this world many important geographical changes have been made throughout this natural phenomena. Scientists have found traces of this la many quarters of the globe where there have been no heavy earthquakes or volcanic eruptions for ages and ages. Volcanoes range in size from a diminutive cone to a huge mountain. In x both cases they are formed from material which has been belched forth from the earth's interior. They can break through any kind of geological formation, and have come through granite of immense depths, and also through Silurian rock, such instances of their awful power being demostrated by extinct volcanoes that have been discovered in France and j r? ? ixuuuiu. Those known as Etna and Vesuvius emerged from beneath soft marine 6trata. They are generally classed as active, dormant and extinct. In many cases, however, it is impossible to distinguish the latter two, and many that have remained quiescent for hundreds of centuries have been known to suddenly break forth in the most violent manner. Such a one was Sornena, which after being domant almost beyond time ira, memorial, became active in the frst century of the Christian era and ultimately produced Vesuvius. The latter in 79 A. D. vomited i forth lava and deadly gases in such gigantic volume and so rapidly that tue inhabitants of the city of Pompeii and several other adjacent towns were destroyed as were the people of St.. Pierre. But Pelee, the volcano which so quickly ended St. Piere and its people, was another one which was always considered extinct. Mt. Epomeo, on the island of Iscbia, finishes another illustration of the ' ' uncertainties of these dread creatures of the earth's hidden mysteries. It remained dormant for about seventeen centuries and then, in 1802, burst forth with the utmost violence. In operation a volcano emits gases, ! vapors, ashes, boulders and lava. .Sometimes the acids are as destruc- ' tlve to life as is the lava and ashes. J The erator of Idjen, a volcano in Ja 'a, I turned loose a huge lake of acid water, which rushed down the mountain side, t and the poisonous proportions of the j liquid caused widespread destruction 1 among human beings, cattle and birds. The ashes sent form by a volcano are ' will nnno. 1 peiierauy so uuc mai mcj f trate a house through the smallest ; creeks and crevices. They are generally so hot that the Inhalation of the smallest amount will cause death. Ashes have been known to fall over a country covering a radiU6 within 160 miles of the volcano from which they were discharged. That occurred when ' Vesuvius broke loose in 1822. On another occasion, when the Cose- 1 f llfp sin^A Pnmneil was buried until St. Pierre was destoryed. The explosion buried the island and about 20,000 inhabitants at the bottom of the sea in the course of a few minutes. The vibratory effects were felt around the world. It caused a tidal wave which reached San Francisco and wiped out many villages on the Island of Sumatra, while it was on the way. The noise of the explosion was heard in India, it was heard in Australia and it was heard in the Island of Roderiquez, 2,968 miles distant. The seismic wave of sea was seen at Cape Horn, 7,500 miles from the scene of the calamity, and at a point in Sumatra it carried the Dutch mar?-of-War Benow two miles inland and left the vessel high and dry thirty feet above the level of the sea. An air wave was created by the explosion which travelled three times around the world before it became dissipated. While erupt.ons of volcanoes always cause the most dread, the earthquakes cause the greater loss of life and property by an overwhelming amount. It is estimated that the destruction of human beings through this medium is greater than any other agency but riiaoaso From first to last during human occupancy of this planet it has been figured that 13,000,000 people have become moribund as a result of earthquake disasters. On this continent they have been tuost disastrous on the Pacific coast, in Mexico and the countries south of it. Below is a list of the great disasters from this cause during a period covered by mediaeval and subsequent history: Year. Number. Catania 1137 15,000 Cilioia 1268 60,000 Naples 1456 40,000 Lisbon 1531 30,000 Lisbon 1755 60000 Naples 1623 70.000 Schanaiki, Russia 1667 80,000 Sicily 1633 iuo.uuo Jcddo, Japan 1703 200,000 Abruzzi, Italy 1706 15.000 Algiers 1716 20,000 China 1731 100,000 Lima, Peru 1746 18,000 Grand Cairo 1752 40.000 Kasehan, Persia 1755 40,000 Syria 1759 20,000 South Italy 1S51 14,000 Peru 1868 25,000 Java 1882 170,000 China and Japan 1891 30,000 Thousands have lost their lives from the same cause in Mexico and other South African countries during the past few months. j ERUPTIONS OF iMT. PELEE. The volcano of Mont Pelee was la3t i in eruption during the month of Auj gust, 1851. Previous to that, in 1767, about 1.C00 people were killed by an earthquake in Martiniqi e. In 1S39, the then capital, Fort Royal, now Fore de I France, was visited by an earthquake which destroyed about half the town, caused great damage throughout the island and killed about seven hundred persons. Mont Pelee is the loftiest mountain on Martinique and is 4,450 feet high. When it was in eruption in 1851 flames | and volumes of black smoke and fine aslies burst suddenly from the crater , and threw the people of St. Pierre into j a panic. They fled from the place, ; many taking refuge on the ships in the roadstead. The eruption on this occas! ion was not serious only covering some hundreds of acres with sulphurous debris, but it was enough to show that Mont Pelee was not dead, but sleeping. The terrible volcanic storm in which : ages ago Mont Pelee was uplifted j crumpled her summit and rent and Assured her sides, and sent her foothills sprawling all over the northern end of i the island of Martinique, less, perhaps, ' by her enormous bulk than by her , pyramid summetry of her outlines. ; nrp^a Dolrl Mmin4nSn '' r Vin tt? o o PolloH iuc uaiu muuuiaiu, n?o , but never was adjective so misapplied, for La Pelee was fully clothed from the edge of the sea to the very summit in the most extravagant luxuriance of tropical vegetation. Within twenty years the great mountain has sounded its warning?rumb- ' i ling and growling and muttering like some uneasy giant in his sleep?but ' the gay people merely shrugged their shoulders and laughed at the menace, for they knew that the crater had been turned into a lake by the rains and that it had been many years?hardly ' within the memory of the oldest inha! bitant?since the volcano did anything ; but threaten. The presence of the lake ! in the crater they accepted as proof I positive that the fires had been drowned out, never to be lighted again. 1 Interesting Facts About St. Pierre. The part of St. Pierre on the slope i was known as the "upper town" and n.-aB rUoan and well hllilt. The lower town situated along the roadstead front was dirty and unhealthy. The town was divided into two parts by a small river over which there was a handsome bridge. Five newspapers were published In St Pierre. They were Las Antilles, founded in 1842; Les Colonies, founded in 1878; La Defense, founded in 1881; Le Propagateur, founded in 1852 and L'Unlon, founded in 1891. The principal commerce of St Plerr9 was the exportation of sugar, rum, soffee and cocoa. Remarkably fine cologne water was manufactured in St. Pierre and exported to France. France took most of the exportations. The im portations of St. Pierre were textile fabrics, grain, flour, wine, oil and meef cattle. The climate has been described as very fine and healthful, resembling tnat 01 Lower Lanioraia iu a rcmaiaable degree. An abundance of clear, sparkling water from the mcuntalus helped keep the town in a fine sanitary condition. One traveller, writing of St. Pierre, said : 'The visitor to the island is reminded on every corner that the Empress ! Josephine was born in Martinique, at | Trois Islets, enar Fort de France. 1 i went to see both her birthplace and | the statue which Napoleon III. erected ! to her memory in the public square In Fort de France; but it is no reminder I of Josephine that is uppermost when I i think of Martinique. It is one of the i most beautiful and quiet spots in the I world that presents Itself. "Just to *.he southward of St. Pierre I is a point of rocks, half way up of j j which a large white cross has been I erected. Beyond the point of rocks the ; sea sweeps inward in a gTeat semiciri cle, making a bay, with another point I - i nut- - * iLt- L... in a distance. ine snore ui inia uay i is a broad yellow beach, smooth as a | carpet. Where the beach ends and the | grass begins a thousand cocoanut palms, all giants, stretch around the semicircle. Under thw palms nestle a score of little stone houses with red: tiled roofs. In the back yards of these houses, a hundred feet back from the water, the mountain begins, and goe3 up, almost straight up. till its summit Is lost in the clouds. Such a beautiful ! nook I fear I shall never see again." Some Idea of the formation of the island of Martinique may be obtained I from the fact that, although It is not i quite forty-five miles loig and only I about nineten miles wide, it has 404 ' mountains, at least six of which, including Mont Pelee, are volcanoes. 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