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TYPES OF ERUPTION: VOLCANIC ERUPTIONS
SDSADA

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Ordenar Letras MODULE 1: VOLCANOVersión en línea TYPES OF ERUPTION: VOLCANIC ERUPTIONS SDSADA por Teacher Nicole 1 These are lavas that are relatively thin and are very fluid when erupted. Shield volcanoes have basaltic lava. S T B A L A 2 These lava has moderate amounts of iron, magnesium, and calcium but is low in potassium and sodium. It ranges in temperature from about 800°C to 1000°C. It commonly erupts from stratovolcanoes as thick lava flows, some reaching several km in length. E N S D A I E T 3 These lavas are viscous and tend to form thick blocky lava flows or steep-sided piles of lava called lava domes. The magmas tend to erupt explosively, commonly also producing abundant ash and pumice. R E Y L I O T H 4 It is a compound composed of Silicon and Oxygen, also produces explosive and nonexplosive eruptions. It has a high or low viscosity and traps more gasses. N I E L I A C N T T O S C 5 It has low viscosity of lava, like basalt and low in silica N E S T O V P I I E U F F E U R 6 It has more viscous lava, like rhyolite and made up of more silica O L E P P S E V I N U E R I T X O 7 It is a stream-driven eruption as the hot rocks come in contact with water. It is short-lived, characterized by ash columns but may be an onset for of a larger eruption Y T T O I C / D E H L R E A H H R M P A R 8 It is a violent eruption due to the contact between water and magma. As a result, a large column of very fine ash and high-speed and sideway emission of pyroclastic called base surges are observed. A M O I H T A T G P A R E M C 9 It is a periodic weak to violent eruption characterized by fountain lava L O N S I O R B A T M 10 It characterized by tall eruption columns that reach up to 20 km high with pyroclastic flow and ashfall tephra. C A I V L A N U N 11 It has excessively explosive type of eruption of gas and pyroclastic N P A I N I L

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MODULE 1: VOLCANOVersión en línea

TYPES OF ERUPTION: VOLCANIC ERUPTIONS SDSADA

por Teacher Nicole

These are lavas that are relatively thin and are very fluid when erupted. Shield volcanoes have basaltic lava.

These lava has moderate amounts of iron, magnesium, and calcium but is low in potassium and sodium. It ranges in temperature from about 800°C to 1000°C. It commonly erupts from stratovolcanoes as thick lava flows, some reaching several km in length.

These lavas are viscous and tend to form thick blocky lava flows or steep-sided piles of lava called lava domes. The magmas tend to erupt explosively, commonly also producing abundant ash and pumice.

It is a compound composed of Silicon and Oxygen, also produces explosive and nonexplosive eruptions. It has a high or low viscosity and traps more gasses.

N I E L I A C N T T O S C

It has low viscosity of lava, like basalt and low in silica

N E S T O V P I I E U F F E U R

It has more viscous lava, like rhyolite and made up of more silica

O L E P P S E V I N U E R I T X O

It is a stream-driven eruption as the hot rocks come in contact with water. It is short-lived, characterized by ash columns but may be an onset for of a larger eruption

Y T T O I C / D E H L R E A H H R M P A R

It is a violent eruption due to the contact between water and magma. As a result, a large column of very fine ash and high-speed and sideway emission of pyroclastic called base surges are observed.

A M O I H T A T G P A R E M C

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MODULE 1: VOLCANOVersión en línea

por Teacher Nicole

These are lavas that are relatively thin and are very fluid when erupted. Shield volcanoes have basaltic lava.

These lava has moderate amounts of iron, magnesium, and calcium but is low in potassium and sodium. It ranges in temperature from about 800°C to 1000°C. It commonly erupts from stratovolcanoes as thick lava flows, some reaching several km in length.

These lavas are viscous and tend to form thick blocky lava flows or steep-sided piles of lava called lava domes. The magmas tend to erupt explosively, commonly also producing abundant ash and pumice.

It is a compound composed of Silicon and Oxygen, also produces explosive and nonexplosive eruptions. It has a high or low viscosity and traps more gasses.

It has low viscosity of lava, like basalt and low in silica

It has more viscous lava, like rhyolite and made up of more silica

It is a stream-driven eruption as the hot rocks come in contact with water. It is short-lived, characterized by ash columns but may be an onset for of a larger eruption

It is a violent eruption due to the contact between water and magma. As a result, a large column of very fine ash and high-speed and sideway emission of pyroclastic called base surges are observed.

It is a periodic weak to violent eruption characterized by fountain lava

It characterized by tall eruption columns that reach up to 20 km high with pyroclastic flow and ashfall tephra.

It has excessively explosive type of eruption of gas and pyroclastic

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