Additional notes on management of volcanic hazards
... Ozone depletion following release of huge amounts of sulphur dioxide ...
... Ozone depletion following release of huge amounts of sulphur dioxide ...
Unit test review - hrsbstaff.ednet.ns.ca
... Distribution of volcanoes Geologic formations (pillow basalt, columnar jointing, plateau basalt) What comes out of a volcano? How does it affect surrounding areas? Effects of ash fall? Viscosity of lava: Aa, pahoehoe, what changes it’s viscosity Pysroclastic flow: how is it formed Volcanic dome Erup ...
... Distribution of volcanoes Geologic formations (pillow basalt, columnar jointing, plateau basalt) What comes out of a volcano? How does it affect surrounding areas? Effects of ash fall? Viscosity of lava: Aa, pahoehoe, what changes it’s viscosity Pysroclastic flow: how is it formed Volcanic dome Erup ...
Mount Pinatubo
Mount Pinatubo (Filipino: Bundok Pinatubo) is an active stratovolcano in the Cabusilan Mountains on the island of Luzon, near the tripoint of the Philippine provinces of Zambales, Tarlac, and Pampanga. Before the volcanic activities of 1991, its eruptive history was unknown to most people. It was heavily eroded, inconspicuous and obscured from view. It was covered with dense forest which supported a population of several thousand indigenous people, the Aetas, who fled to the mountains during the Spanish conquest of the Philippines.The volcano's Plinian / Ultra-Plinian eruption on 15 June 1991 produced the second largest terrestrial eruption of the 20th century after the 1912 eruption of Novarupta in the Alaska Peninsula.Complicating the eruption was the arrival of Typhoon Yunya (Diding), bringing a lethal mix of ash and rain to areas surrounding the volcano. Successful predictions at the onset of the climactic eruption led to the evacuation of tens of thousands of people from the surrounding areas, saving many lives, but the surrounding areas were severely damaged by pyroclastic flows, ash deposits, and subsequently, by the lahars caused by rainwaters re-mobilizing earlier volcanic deposits causing extensive destruction to infrastructure and changing the river systems months to years after the eruption.The effects of the eruption were felt worldwide. It ejected roughly 10,000,000,000 tonnes (1.1×1010 short tons) or 10 km3 (2.4 cu mi) of magma, and 20,000,000 tonnes (22,000,000 short tons) SO2, bringing vast quantities of minerals and metals to the surface environment. It injected more particulate into the stratosphere than any eruption since Krakatoa in 1883. Over the following months, the aerosols formed a global layer of sulfuric acid haze. Global temperatures dropped by about 0.5 °C (0.9 °F) in the years 1991-93, and ozone depletion temporarily increased substantially.