Kamis, 23 Desember 2010

Natural Disaster

Eruption of Mount Merapi

Eruption of Mount Merapi have eruption in the year 2010. Eruptions that are ekspolif October 26 experienced a pause, but starting on Wednesday (3 / 11) eruptions occur continuously until Saturday (6/5/11).
Eruptions that without ceasing is caused by magma supply from the bag in the belly of the earth is still high. Magma bag closest to the peak of Merapi are in 3 kilometers from the summit, while in the magma pocket located at position 100 kilometers from the peak of Merapi.
Based on field observation, pyroclastic deposits currently reached a distance of 12 kilometers in Kali Boyong with a thickness of up to 10 meters. Based on reports from BPPTK, up at 06.00 AM thunderous eruption can still be heard from a distance of 20 kilometers from the mountain top.
Similarities Merapi eruption was in 2010 with the 1872 eruption in 1872 produced the crater with a diameter of between 480-600 meters. While the current eruption that formed the crater was predicted to reach 400 square meters.
According to data BPPTK, 1872 eruption lasted for five days and is classified in class D. Cracking noise sounded to Falkirk, Madura and Bawean. Pyroclastic flows through almost all existing river at the peak of Merapi, namely Kali Apu, Trising Kali, Kali Senowo, Kali Blongkeng, Batang Kali, Kali Woro, and Kali Gendol. However, the 1872 eruption did not mention the number of casualties.

Eruption of Mount Merapi

Rabu, 29 September 2010

26 dec 2004

2004 Tsunami Video

2004 Boxing Day Tsunami

Natural Disaster




Tsunami

A tsunami is a series of ocean waves. They are one of the biggest disasters in the world which mainly damage the cities that or close to the ocean or harbors. Tsunamis are generated by a sudden displacement on the ocean floor, landslides, earthquakes, or volcanic activities. A tsunami is formed because the waves slow down when it reaches the shore which makes the water become compressed which causes it to rise and fall down on land. Most of the tsunamis waves are high because they have not lost a lot of energy because of friction or spreading. Many of them can travel 500 miles per hour and slows down to 20 to 30 miles per hour when it reaches shallow waters or the shore. In less than 24 hours a tsunami can travel across the pacific ocean.

A tsunami is capable of demolishing a whole city within minutes. It can also destruct the entire pacific basin and kill thousands people, if it is strong. If a person is caught in middle of Tsunami it is very difficult for him to survive. He'll either drown in the water or get crushed in debris. A tsunami can have waves over three hundred miles wide and can reach a height of about hundred feet.

In the deep ocean tsunami is barely noticeable but when it approaches land it becomes a hazard. The tsunami is named from the Japanese words tsu which mean harbor and nami which means waves. The impact of a tsunami can be much less if people are prepared and warned on timely basis. A tsunami hit southeast Asia on December 26, 2004. It was the deadliest disaster in modern history killing over 240,000 people. Hawaii in US gets the most Tsunamis than any other state and has a risk of getting onother one.


Selasa, 25 Mei 2010