PDF-World Organization of Volcano Observatories

A Commission of the International Association of Volcanology and Chemistry of the Earths Interior WOVO the case for support Gill Jolly Peter Webley Susanna Falsaperla World Organization o. Objectives. 1. To learn the structure of a volcano. 2. To know that volcanoes can be dormant, active and extinct. key words. Earthquake, volcano, plate margin, plates.. Structure of a Volcano.. Structure of a Volcano.. Volcanic Eruptions. 1. Why Volcanoes Erupt:. The F of expanding gas builds and pushes magma through the vent. 2. Major Factors in Eruptions:. a. The amount of trapped gas. CO. 2. and Sulfur. b. Silica Content. Alaska, USA. Mollie Taylor and . Ilana. . Zyatitsky. Department of Geology, Colby College. Professor Robert Nelson – Jan Plan 2015. Geographic Setting. 60°29’N 152°44’W. 177 km SW of . Anchorage . An example of Time Series Analysis. Daniele . Alami. . Country. :Italy . Subregion. . Name. . :Italy / . Sicily. Volcano . Number. . : 0101-06= . Volcano . Type. . : . Stratovolcanoes. . Volcano Status. Learning Outcomes. To understand that the Earth’s atmosphere is transparent to some electromagnetic radiation and opaque to others.. To distinguish between refracting and reflecting telescopes.. To appreciate that most optical and infra-red observatories are located on high mountains or in space.. By: Kadish Hagley and Cecil Brooks Jr.. Department of Geology, . Colby College. http://upload.wikimedia.org/wikipedia/commons/f/f6/Taal_Volcano_aerial_2013.jpg. Basic Facts and Location. Taal is on Luzon Island, . Ann Sparling White, MS. , LPC, NCC. annsparling@gmail.com. THE VOLCANO MODEL. AS AN ASSESSMENT TOOL. . Allows for quick and easy information gathering. . . Is non-intrusive. Works both individually and with a family or group. A volcano is a fault in earth’s crust that allows magma to escape.. We call the release of magma an eruption.. How does that work?. Magma is the layer of melted rock that . lies just below earth’s crust.. Boom! About 2,000 years ago, a volcano called Vesuvius roared to life. Hot. clouds of gas shot into the sky. Burning rocks whirled through the air. Hot ash. poured from the from the volcano.. Oil. A volcano is an opening in Earth that erupts gases, ash, and lava.. Volcanic mountains form when layers of lava, ash, and other material build up around these openings.. 3 Basic Volcano shapes. Cinder Cone. TITLE: AUTHORS (FIRST NAME, LAST NAME): Alexander Belousov 1, 3 , Marina Belousova 1, 3 , Akhmad Zaennudin 2 , Oktory Prambada 2 INSTITUTIONS (ALL): 1. Earth Observatory of Singapore, Singapore, S FixO 3 Grant Agreement Number: 312463 The work described in this report has received funding from the European Union Seventh f ramework Programme (FP7/2007 - 2013) . Work Package 4 Data management Active volcanos. Subduction zone volcano. Spreading volcanos. Atlantic rift near Iceland. Iceland on a spreading axis. Earthquakes. at volcanos. Earthquakes types at volcanos. Earthquake swarm at a volcano. . Main Idea 1. : . Volcanoes look like mountains, but they form as a result of . repeated eruptions. of magma from underground.. Redoubt, AK. Active Volcano. http://www.youtube.com/watch?v=g1UWTwDwZp8.