Natural Hazards: Causes and Effects - Disaster Management Center ...
Natural Hazards: Causes and Effects - Disaster Management Center ... Natural Hazards: Causes and Effects - Disaster Management Center ...
The first symptoms of unrest in the volcano were evident in April 1901. Earthquakes were severe enough that people living on the western slope of La Soufriere became alarmed. Some considered leaving the area, but the shocks ceased and the people resumed their normal activities until in April 1902, when the shocks were again felt. By the first of May the inhabitants on the leeward side of the volcano north of Chateaubelair had sought refuge elsewhere. If this had not happened, the death toll of the eruption would have been much higher. Those living on the windward side were not particularly disturbed and continued their activities as usual. It was felt that in the event of an eruption the ash and gases would be carried towards the west by the prevailing winds. When the great eruption occurred on May 7, few people were killed on the leeward side (one report says only one) while 1,350 were killed in the windward side (other estimates place the loss of life as high as 1,600). The hot blast overturned trees, scorching them on the side facing the volcano, destroyed houses, and set fire to inflammable objects. The hot ash, which fell in great quantities, killed all vegetation and devastated an area comprising about one-third of the island. Red-hot stones up to 15 centimeters (six inches) in diameter fell in Georgetown, nine kilometers (5.5 miles) from the crater. The orientation of trees blown down revealed that the blast swept outward in all directions from the crater. At the end of the eruption La Soufriere still showed no signs of “dome” development and was therefore considered capable of further destructive eruptions. 3 A minor eruption occurred in 1971, but St. Vincent Island was shaken by a violent eruption again on April 14, 1979. This eruption sent stones raining down on parts of the island while a cloud of smoke and ash blocked out the sun after the eruption just before noon. The state-run radio reported that lava was coming from one side of the volcano’s crater. People in the northern half of the island were told to head for the beaches where boats could take them to safety. The eruption hurled ashes and smoke 6,100 meters (20,000 feet) into the air, showering Barbados, 160 kilometers (100 miles) to the east, with volcanic dust. Rumblings could be heard as far away as Kingstown, more than 20 kilometers (12 miles) to the south. Seven small explosions shook the volcano again on April 18. The explosions, at intervals of only a few minutes, threw a small amount of ash and steam into the air north of the Larikai Valley, where lava had poured down the volcano’s sides the day before following the eighth violent eruption in five days. On April 22 the volcano erupted intermittently for three hours, sending a column of ash more than 11 kilometers (seven miles) into the air and shaking the earth with tremors. The government evacuated the northern two-thirds of the island and cared for the 17,000 refugees until the volcano was declared quiet. 4 Jorullo, Mexico, 1759 The volcano Jorullo was born on September 29, 1759, in the midst of an area that was being cultivated at the time. It is one of the best known volcanoes born during historic times. Jorullo is located in western Mexico in the state of Michoacan, about 240 kilometers (150 miles) west of Mexico City. The general elevation is about 750 meters (2,460 feet), and the climate is tropical. The region is relatively inaccessible but can be reached by a truck road. At the time of the eruption the Hacienda de Jorullo was one of three farms operated in the general area for the
production of sugar and cattle. Because of the fertility of the soil and the tropical climate, the area was known as Jorullo, which in the language of the Tarascan Indians means “Paradise.” Near the end of June 1759, the people living at the Hacienda de Jorullo were alarmed by subterranean noises that, accompanied by mild earthquakes, continued until September 17. At this time the noises became much louder, being compared to cannonfire, and the earthquakes were strong enough to seriously damage the chapel. The frightened people fled to the surrounding hills for safety. At 3:00 A.M. on September 29, about a kilometer to the southeast of the Hacienda in a ravine known as Cuitinga Creek, a very dark and dense steam cloud rose, accompanied by sharp earth tremors and loud explosions, and soon flames burst through the cloud, which was becoming thicker and denser. For two days the volcano threw out masses of “sand [cinders], fire and thunder without one minute cessation.” On October 1 a mass of “sand so hot it set fire to whatever it fell upon” rose from the outlet of the volcano, which was little more than a cleft, and flowed for a kilometer down Cuitinga Creek. Violent eruptions continued until February 1760, and with decreasing intensity until about 1775, making the total life of Jorullo’s activity about 15 years. The outpouring of lava consisted of at least four separate flows, forming a great wasteland that covered nine square kilometers to depths up to a hundred meters. The flows are believed to have appeared in 1764, considered to be the year of maximum activity. The first three flows are covered with ash and cinders, indicating that these materials were still being ejected after the outpourings of lava. However, the last flow, which issued from a breach on the north rim of the crater and flowed as a great cascade down the north side of the cone, is free of any ash or cinder cover. This “frozen” cascade of black lava is still quite “new” and “fresh” looking and is one of the striking features of Jorullo. It seems likely that this was the end of the explosive activity of the volcano and that thereafter it was in a venting or fumarolic state. Jorullo is presently 1,330 meters (4,360 feet) high. The crater is an oval-shaped depression with a diameter at the rim of 400 meters by 500 meters (1,300 feet by 1,640 feet). Its depth is 150 meters (500 feet) below the highest point. The bottom of the crater appears to have collapsed since its last eruptive activity, and the bottom is filled with rubble that has fallen from the sides. At a depth of less than a meter below the rubble the heat is too intense for the hand but not sufficient to brown a piece of paper or to make water “hiss.” However, the fact that Jorullo is continuing after 200 years to give off heat as well as gases indicates the life of volcanoes. 5 Geographical Distribution of Volcanoes About 500 volcanoes around the world can be considered active, in that they have erupted during historic times. Many more can be described as dormant: they are not known to have erupted for thousands of years but could return to activity at any time. For example, Mount Lamington, in New Guinea, erupted violently in 1951 when it had been thought to be inactive. Volcanoes are described as extinct when there is no chance of renewed eruption. This is usually only when a change in the geological environment has effectively defused a once-active volcano. Over the millions of years of geological history volcanoes have existed in almost every part of the world and have formed enormous volumes of rock. The entire landmass of Iceland has been thrown up out of a continuous series of volcanoes. Today volcanoes are generally found in restricted belts around the world. 6
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The first symptoms of unrest in the volcano were evident in April 1901. Earthquakes were<br />
severe enough that people living on the western slope of La Soufriere became alarmed. Some<br />
considered leaving the area, but the shocks ceased <strong>and</strong> the people resumed their normal<br />
activities until in April 1902, when the shocks were again felt. By the first of May the inhabitants<br />
on the leeward side of the volcano north of Chateaubelair had sought refuge elsewhere. If this<br />
had not happened, the death toll of the eruption would have been much higher. Those living on<br />
the windward side were not particularly disturbed <strong>and</strong> continued their activities as usual. It was<br />
felt that in the event of an eruption the ash <strong>and</strong> gases would be carried towards the west by the<br />
prevailing winds. When the great eruption occurred on May 7, few people were killed on the<br />
leeward side (one report says only one) while 1,350 were killed in the windward side (other<br />
estimates place the loss of life as high as 1,600).<br />
The hot blast overturned trees, scorching them on the side facing the volcano, destroyed<br />
houses, <strong>and</strong> set fire to inflammable objects. The hot ash, which fell in great quantities, killed all<br />
vegetation <strong>and</strong> devastated an area comprising about one-third of the isl<strong>and</strong>. Red-hot stones up<br />
to 15 centimeters (six inches) in diameter fell in Georgetown, nine kilometers (5.5 miles) from<br />
the crater. The orientation of trees blown down revealed that the blast swept outward in all<br />
directions from the crater.<br />
At the end of the eruption La Soufriere still showed no signs of “dome” development <strong>and</strong> was<br />
therefore considered capable of further destructive eruptions. 3<br />
A minor eruption occurred in 1971, but St. Vincent Isl<strong>and</strong> was shaken by a violent eruption<br />
again on April 14, 1979. This eruption sent stones raining down on parts of the isl<strong>and</strong> while a<br />
cloud of smoke <strong>and</strong> ash blocked out the sun after the eruption just before noon. The state-run<br />
radio reported that lava was coming from one side of the volcano’s crater. People in the<br />
northern half of the isl<strong>and</strong> were told to head for the beaches where boats could take them to<br />
safety. The eruption hurled ashes <strong>and</strong> smoke 6,100 meters (20,000 feet) into the air, showering<br />
Barbados, 160 kilometers (100 miles) to the east, with volcanic dust. Rumblings could be heard<br />
as far away as Kingstown, more than 20 kilometers (12 miles) to the south.<br />
Seven small explosions shook the volcano again on April 18. The explosions, at intervals of<br />
only a few minutes, threw a small amount of ash <strong>and</strong> steam into the air north of the Larikai<br />
Valley, where lava had poured down the volcano’s sides the day before following the eighth<br />
violent eruption in five days.<br />
On April 22 the volcano erupted intermittently for three hours, sending a column of ash more<br />
than 11 kilometers (seven miles) into the air <strong>and</strong> shaking the earth with tremors.<br />
The government evacuated the northern two-thirds of the isl<strong>and</strong> <strong>and</strong> cared for the 17,000<br />
refugees until the volcano was declared quiet. 4<br />
Jorullo, Mexico, 1759<br />
The volcano Jorullo was born on September 29, 1759, in the midst of an area that was being<br />
cultivated at the time. It is one of the best known volcanoes born during historic times.<br />
Jorullo is located in western Mexico in the state of Michoacan, about 240 kilometers (150 miles)<br />
west of Mexico City. The general elevation is about 750 meters (2,460 feet), <strong>and</strong> the climate is<br />
tropical. The region is relatively inaccessible but can be reached by a truck road. At the time of<br />
the eruption the Hacienda de Jorullo was one of three farms operated in the general area for the