Volcanoes :: Volcano Nature Lava Eruption Essays

ventes This paper will define and dissertate the blowhole to include types of vol slewoes, homunculusation of a vol pecko, and elements of a volcano such as, lava, inclination sherds, and gas. This paper also tells a little bit closely volcanic activity in different parts of the world. What is a volcano? A volcano is a exit in the earth from which liquefied jounce and gas erupt. The molten vibrate that erupts from the volcano forms a mound or mountain around the vent. The lava may flow out as a viscous liquid or it may explode from the vent as solid or liquid particles. Kinds of Volcanic Materials Three raw material materials that may erupt from a volcano are 1. lava, 2. rock fragments, and 3. gas. Lava Lava is the telephone for magma that has been released onto the Earths step up. When lava comes to the Earths surface, it is blushing(a) hot and may have temperatures of more than 2012 degrees Fahrenheit. Fluid lava flows fleetly consume a volcanos slopes. Sticky l ava flows more slowly. As the lava cools, it may inure into umpteen different formations. Highly fluid lava hardens into smooth, folded sheets of rock called pahoehoe. Stickier lava cools into rough, jagged sheets of rock called aa. Pahoehoe and aa hug large areas of Hawaii, where the terms originated. The stickiest lava forms flows of boulders and rubble called block flows. It may also form mounds of lava called domes. Other lava formations are sparge cones and lava tubes. Spatter cones are bury hills that can get up to 100 feet high. They build up from the spatter of geyser-like eruptions of slow lava. Lava tubes are tunnels formed from fluid lava. As the lava flows, its exterior diligence cools and hardens. yet the lava below continues to flow. After the flowing lava drains away, it leaves a tunnel. sway Fragments Rock fragment are usually called tephra and are formed from muggy magma. This magma is so sticky that its gas can not easily escape when the magma approaches t he surface or central vent. Finally, the trapped gas builds up so overmuch wardrobe that it blasts the magma into fragments. Tephra consists of volcanic pass around, volcanic ash, and volcanic bombs, (from smallest to largest size particle). Volcanic corpse consists of particles less(prenominal) than one one-hundredth inch in diameter. Volcanic dust can be carried for great distances. In 1883, the eruption of Krakatau in Volcanoes Volcano Nature Lava Eruption EssaysVolcanoes This paper will define and discuss the volcano to include types of volcanoes, formation of a volcano, and elements of a volcano such as, lava, rock fragments, and gas. This paper also tells a little bit about volcanic activity in different parts of the world. What is a volcano? A volcano is a vent in the earth from which molten rock and gas erupt. The molten rock that erupts from the volcano forms a hill or mountain around the vent. The lava may flow out as a viscous liquid or it may explode from the vent as solid or liquid particles. Kinds of Volcanic Materials Three basic materials that may erupt from a volcano are 1. lava, 2. rock fragments, and 3. gas. Lava Lava is the name for magma that has been released onto the Earths surface. When lava comes to the Earths surface, it is red hot and may have temperatures of more than 2012 degrees Fahrenheit. Fluid lava flows swiftly down a volcanos slopes. Sticky lava flows more slowly. As the lava cools, it may harden into many different formations. Highly fluid lava hardens into smooth, folded sheets of rock called pahoehoe. Stickier lava cools into rough, jagged sheets of rock called aa. Pahoehoe and aa cover large areas of Hawaii, where the terms originated. The stickiest lava forms flows of boulders and rubble called block flows. It may also form mounds of lava called domes. Other lava formations are spatter cones and lava tubes. Spatter cones are steep hills that can get up to 100 feet high. They build up from the spatter of geyser-lik e eruptions of thick lava. Lava tubes are tunnels formed from fluid lava. As the lava flows, its exterior covering cools and hardens. But the lava below continues to flow. After the flowing lava drains away, it leaves a tunnel. Rock Fragments Rock fragment are usually called tephra and are formed from sticky magma. This magma is so sticky that its gas can not easily escape when the magma approaches the surface or central vent. Finally, the trapped gas builds up so much pressure that it blasts the magma into fragments. Tephra consists of volcanic dust, volcanic ash, and volcanic bombs, (from smallest to largest size particle). Volcanic dust consists of particles less than one one-hundredth inch in diameter. Volcanic dust can be carried for great distances. In 1883, the eruption of Krakatau in