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Eruption
Eruption

... Most volcanoes are formed on land, but there are some volcanoes that are on the ocean floor. Some of these volcanoes emerge from the water because they are very high. ...
VOLCANOES!!!
VOLCANOES!!!

... More than 36,000 people killed Area around the volcano was in completely dark for about 24 hours. ...
Landforms at plate margins – Volcanoes and supervolcanoes
Landforms at plate margins – Volcanoes and supervolcanoes

... different products that can be thrown out, including ash, cinders, pumice, dust, gases and steam. The world distribution of active volcanoes (Figure 1) shows an almost perfect fit with the locations of the tectonic plate margins (see Figure 2 on page 6). ...
volcanoes
volcanoes

... A volcano is a location on the surface of the Earth where magma has erupted out of the interior of the planet. Magma is molten rock, which has melted from the extreme heat (2200°C to 5000°C) and pressure that exists inside the Earth. Once molten rock has erupted onto the Earth’s surface, it is calle ...
Volcano Report
Volcano Report

... A volcanic eruption occurs when lava flows or ejects from a vent. Vents can be located at the top of the cone shaped mountain and also on its sides, and one volcano can have many vents. Eruptions can be violent or quiet. Violent eruptions occur because new lava, steam, and gases, such as carbon diox ...
magma and lava
magma and lava

... It depends on the type of magma/lava that the volcano is made up of. It can either be felsic or mafic lava. Felsic lava is associated with explosive eruptions because it is high in silica which means it is more viscous. Since it is more viscous the dissolved gases within it cannot escape easily whic ...
Volcanoes
Volcanoes

...  Andesitic Lava ...
Volcanoes
Volcanoes

... – Famous for the May 8, 1902 eruption which killed 29,000 people and destroyed the city of St. Pierre. This is the largest number of causalities for a volcanic eruption this century. ...
Chapter 5 lesson 2
Chapter 5 lesson 2

... a long tube through which magma moves from the magma chamber to Earth’s surface the opening through which molten rock and gas leave a volcano the area covered by lava as it pours out of a volcano’s vent a bowl shaped area that forms around a volcano’s central opening a material found in magma that i ...
composite volcanoes - Mesa Public Schools
composite volcanoes - Mesa Public Schools

... The Hawaiian Islands are peaks of a long line of shield volcanoes called the Hawaiian Chain. Some of these volcanoes project above the ocean creating islands while others remain below the surface. Most of these are found on the Pacific Plate. The big island of Hawaii is the upper part of five differ ...
Slide 1
Slide 1

... Dormant- are not currently erupting but are considered likely to do so. Mt. St Helens was dormant for 123 years before it erupted in 1980. ...
Volcanoes
Volcanoes

... moving pushing up and the magma below rises forming a volcano and when the pressure builds up eruptions take place. The ring of fire is on the edge of several plates pushing against others so there are lots of volcanoes there. ...
Introduction to volcanoes, volcanic eruptions, and volcanic
Introduction to volcanoes, volcanic eruptions, and volcanic

... Lower viscosity basaltic lava (mafic) is ~45% to 54% silica ...
Volcanoes - Travelling across time
Volcanoes - Travelling across time

... The immediate effects of volcanic eruptions can be devastating, but they may be beneficial in the long term. ...
Volcano: Fill in the blanks below using words from the word bank
Volcano: Fill in the blanks below using words from the word bank

... (These waves are similar to the waves that we form when we throw a stone into a lake) ...
Earthquakes, Zones and Volcanoes
Earthquakes, Zones and Volcanoes

... % and measurements about earthquakes and volcano facts – compare to everyday objects. Roman numerals link to Pompeii. Timeline of eruptions/ earthquakes/ Tsunami ...
File - Dengelscience
File - Dengelscience

... • Silica and gas pressure determine how explosive an eruption will be. ...
Volcanoes
Volcanoes

... O These volcanoes have explosive eruptions ...
File
File

... Pumice stone, which comes from volcanoes, is very light because it contains lot of tiny bubbles. If there are enough bubbles, then pumice stone can float on water! The word, ‘volcano’ comes from the name Vulcan, who was the Roman god of fire. ...
Ch 8 Volcanoes Test – Study Guide
Ch 8 Volcanoes Test – Study Guide

... lahar   magma   mid-­‐ocean  ridge   volcano   subduction   vent   ...
Directions: Read the information below. Use this information and
Directions: Read the information below. Use this information and

... volcanoes and shield volcanoes. Cinder cones are built from lava fragments called cinders. The lava fragments are ejected from a single vent and accumulate around the vent when they fall back to earth. Cinder cones grow rapidly and soon approach their maximum size. They rarely exceed 250m in height ...
Volcanoes
Volcanoes

... Monitoring Volcanoes ...
Long ago in Mexico, a great Aztec king had a daughter named
Long ago in Mexico, a great Aztec king had a daughter named

... burying cities. But volcanoes can also create new land, and their ash helps keep soil healthy. ...
Volcanoes
Volcanoes

... Dormant- are not currently erupting but are considered likely to do so. Mt. St Helens was dormant for 123 years before it erupted in 1980. ...
Challenge and Extension - Effingham County Schools
Challenge and Extension - Effingham County Schools

... KEY CONCEPT Volcanoes form as molten rock erupts. Identify Volcano Types There are three main types of volcanoes: cinder cone, composite, and shield. Each type has certain characteristics that distinguish it from the others. The table below describes the three types of volcanoes. Use it to identify ...
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Kīlauea



Kīlauea (/kiːlaʊˈeɪ.ə/; Hawaiian: [ˈkiːlɔuˈwɛjə]) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.Kīlauea's eruptive history has been a long and active one; its name means ""spewing"" or ""much spreading"" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, samples having been recovered by remotely operated underwater vehicles from its submerged slopes; samples of other flows have been recovered as core samples. Lavas younger than 1,000 years cover 90 percent of the volcano. The oldest exposed lavas date back 2,800 and 2,100 years. The first well-documented eruption of Kīlauea occurred in 1823, and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its southwestern rift zone, and are prolonged and effusive in character. The geological record shows, however, that violent explosive activity predating European contact was extremely common, and should explosive activity start anew the volcano would become much more dangerous to civilians. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-duration historical period of activity, as well as one of the longest-duration eruptions in the world; as of January 2011, the eruption has produced 3.5 cubic kilometres (0.84 cu mi) of lava and resurfaced 123.2 km2 (48 sq mi) of land.Kīlauea's high state of activity has a major impact on its mountainside ecology where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes where left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's (and the island of Hawaiʻi's) isolation from the nearest landmass. Historically, the five volcanoes on the island were considered sacred by the Hawaiian people, and in Hawaiian mythology Kīlauea's Halemaumau Crater served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes. William Ellis, a missionary from England, gave the first modern account of Kīlauea and spent two weeks traveling along the volcano; since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, located on the rim of Kīlauea caldera, has served as the principal investigative and scientific body on the volcano and the island in general. In 1916 a bill forming the Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson; since then the park has become a World Heritage Site and a major tourist destination, attracting roughly 2.6 million people annually.
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