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 ...
... 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 ...
Geo Fun - Latitude Festival
... 4. What is another word for the "hole", or vent, in the top of the volcano? 5. Where is the main vent of the paper model volcano? Can you find a second vent drawn on the side of the model volcano? 6. Why are most volcanoes on Earth cone-shaped? VOCABULARY (Discuss the meanings and usage of the follo ...
... 4. What is another word for the "hole", or vent, in the top of the volcano? 5. Where is the main vent of the paper model volcano? Can you find a second vent drawn on the side of the model volcano? 6. Why are most volcanoes on Earth cone-shaped? VOCABULARY (Discuss the meanings and usage of the follo ...
Case Study: Extrusive Landforms and their impact on the
... is a continental mountain arc formed due to the subduction of an offshore oceanic plate beneath the continental crust. Here the Juan de Fuca plate is being subducted under the North American Plate. As the Juan de Fuca plate descends it begins to melt due to heat and pressure produced by friction at ...
... is a continental mountain arc formed due to the subduction of an offshore oceanic plate beneath the continental crust. Here the Juan de Fuca plate is being subducted under the North American Plate. As the Juan de Fuca plate descends it begins to melt due to heat and pressure produced by friction at ...
volcano eruption styles
... occur after major eruptions Ash covers sides of volcano Ash becomes unstable during heavy ...
... occur after major eruptions Ash covers sides of volcano Ash becomes unstable during heavy ...
Composite volcanoes
... • formed by alternating layers of lava and rock fragments. • often form impressive, snow-capped peaks which are often exceeding 2500m in height, 1000sq.km in surface, and 400km3 in volume. • Between eruptions they are often so quiet they seem extinct. To witness the start of a great eruption require ...
... • formed by alternating layers of lava and rock fragments. • often form impressive, snow-capped peaks which are often exceeding 2500m in height, 1000sq.km in surface, and 400km3 in volume. • Between eruptions they are often so quiet they seem extinct. To witness the start of a great eruption require ...
Volcano and Mountain Review Sheet
... ii. Mountain covers a large area, sides are gently sloped, dome-shaped c. Composite cone i. Explosive eruption then a quiet eruption follows ii. Mountain is large, sides are steep, and mountain is cone-shaped Mountains 1. Definitions: a. Mountain ...
... ii. Mountain covers a large area, sides are gently sloped, dome-shaped c. Composite cone i. Explosive eruption then a quiet eruption follows ii. Mountain is large, sides are steep, and mountain is cone-shaped Mountains 1. Definitions: a. Mountain ...
Volcano - watertown.k12.wi.us
... ___________________________ grained texture, while those at greater depths may have a coarse grained texture. Often dikes will be ___________________ resistant to erosion and leave a walllike protrusion on the surface. An example is Ship Rock (New Mexico). There also dikes in Wisconsin. 3. _________ ...
... ___________________________ grained texture, while those at greater depths may have a coarse grained texture. Often dikes will be ___________________ resistant to erosion and leave a walllike protrusion on the surface. An example is Ship Rock (New Mexico). There also dikes in Wisconsin. 3. _________ ...
clozevolcanonotes
... ___________________________ grained texture, while those at greater depths may have a coarse grained texture. Often dikes will be ___________________ resistant to erosion and leave a walllike protrusion on the surface. An example is Ship Rock (New Mexico). There also dikes in Wisconsin. 3. _________ ...
... ___________________________ grained texture, while those at greater depths may have a coarse grained texture. Often dikes will be ___________________ resistant to erosion and leave a walllike protrusion on the surface. An example is Ship Rock (New Mexico). There also dikes in Wisconsin. 3. _________ ...
Document
... _____ 12. The underground body of molten rock that feeds a volcano is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. _____ 13. An opening in the Earth's surface through which volcanic material passes is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. 14. What about ...
... _____ 12. The underground body of molten rock that feeds a volcano is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. _____ 13. An opening in the Earth's surface through which volcanic material passes is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. 14. What about ...
File
... 4. Rocks are classified by what they are made of and how they form. Igneous rocks always begin as magma. What are the two main types of igneous rocks, and what is the main difference between them? How does each type form into solid rock? ...
... 4. Rocks are classified by what they are made of and how they form. Igneous rocks always begin as magma. What are the two main types of igneous rocks, and what is the main difference between them? How does each type form into solid rock? ...
01 - Mayfield City Schools
... _____ 12. The underground body of molten rock that feeds a volcano is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. _____ 13. An opening in the Earth's surface through which volcanic material passes is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. 14. What about ...
... _____ 12. The underground body of molten rock that feeds a volcano is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. _____ 13. An opening in the Earth's surface through which volcanic material passes is a(n) a. vent. c. lava chamber. b. magma chamber. d. ash chamber. 14. What about ...
Chapter 10.1
... • Calderas - a large depression in a volcano. This is cause by the collapse of the top of a composite volcano or from the collapse of the top of a shield volcano. • Necks and Pipes – most volcanoes get magma through conduits called pipes that connect a magma chamber to the surface. A neck is when th ...
... • Calderas - a large depression in a volcano. This is cause by the collapse of the top of a composite volcano or from the collapse of the top of a shield volcano. • Necks and Pipes – most volcanoes get magma through conduits called pipes that connect a magma chamber to the surface. A neck is when th ...
FORMS OF ERUPTIONS
... The composition of the magma plays a big part in determining the manner in which energy is released during a volcanic eruption. Other factors that determine the force of an eruption: Amount of water vapor and other gases Its temperature Silica content ...
... The composition of the magma plays a big part in determining the manner in which energy is released during a volcanic eruption. Other factors that determine the force of an eruption: Amount of water vapor and other gases Its temperature Silica content ...
Shapes of igneous bodies
... Pyroclastic Deposits include – volcaniclastic – formed by volcano (process irrelevant) - pyroclastic – formed from magma/lava aerially expelled from vent - lahar – volcanic debris mixed with water/melting ice or snow Pyroclastic Fall Deposits – material falls from vertical eruption, well sorted, bla ...
... Pyroclastic Deposits include – volcaniclastic – formed by volcano (process irrelevant) - pyroclastic – formed from magma/lava aerially expelled from vent - lahar – volcanic debris mixed with water/melting ice or snow Pyroclastic Fall Deposits – material falls from vertical eruption, well sorted, bla ...
Debris Flows and Avalanches
... • Large scale landslide associated with volcanic activity- moves under gravity • Term avalanche used to emphasize the fact that material has little or no water in it when emplaced- may have steam, gas, ice, snow but not liquid water • Debris Flows or lahars are rapid, watersaturated flows. • Many de ...
... • Large scale landslide associated with volcanic activity- moves under gravity • Term avalanche used to emphasize the fact that material has little or no water in it when emplaced- may have steam, gas, ice, snow but not liquid water • Debris Flows or lahars are rapid, watersaturated flows. • Many de ...
Volcano Notes - The Science Queen
... An explosive period can release gas and ash, forming a tephra layer. Then, the eruption can switch to a quieter period, erupting lava over the top of the tephra layer. ...
... An explosive period can release gas and ash, forming a tephra layer. Then, the eruption can switch to a quieter period, erupting lava over the top of the tephra layer. ...
Volcano
... An explosive period can release gas and ash, forming a tephra layer. Then, the eruption can switch to a quieter period, erupting lava over the top of the tephra layer. ...
... An explosive period can release gas and ash, forming a tephra layer. Then, the eruption can switch to a quieter period, erupting lava over the top of the tephra layer. ...
Volcanoes - Jefferson Township Public Schools
... Radioactive decay is a breaking apart of the nucleus of an atom; as a nucleus breaks apart, it releases energy which is changed into heat. ...
... Radioactive decay is a breaking apart of the nucleus of an atom; as a nucleus breaks apart, it releases energy which is changed into heat. ...
Ch. 7.2 Volcanic Eruptions
... Only a few hundred meters high at most; very steep sides. Result from explosive eruptions of solid fragments. ...
... Only a few hundred meters high at most; very steep sides. Result from explosive eruptions of solid fragments. ...
Nevado del Ruiz
The Nevado del Ruiz (Spanish pronunciation: [neβaðo ðel ˈrwis]), also known as La Mesa de Herveo (English: Mesa of Herveo (the nearby town)), or Kumanday in the language of the local pre-Columbian indigenous people, is a volcano located on the border of the departments of Caldas and Tolima in Colombia, about 129 kilometers (80 mi) west of the capital city Bogotá. It is a stratovolcano, composed of many layers of lava alternating with hardened volcanic ash and other pyroclastic rocks. Nevado del Ruiz has been active for about two million years, since the early Pleistocene or late Pliocene epoch, with three major eruptive periods. The current volcanic cone formed during the present eruptive period, which began 150 thousand years ago.The volcano usually generates Plinian eruptions, which produce swift-moving currents of hot gas and rock called pyroclastic flows. These eruptions often cause massive lahars (mud and debris flows), which pose a threat to human life and the environment. The impact of such an eruption is increased as the hot gas and lava melts the mountain's snowcap, adding large quantities of water to the flow. On November 13, 1985, a small eruption produced an enormous lahar that buried and destroyed the town of Armero in Tolima, causing an estimated 25,000 deaths. This event later became known as the Armero tragedy—the deadliest lahar in recorded history. Similar but less deadly incidents occurred in 1595 and 1845, consisting of a small explosive eruption followed by a large lahar.The volcano is part of Los Nevados National Natural Park, which also contains several other volcanoes. The summit of Nevado del Ruiz is covered by large glaciers, although these have retreated significantly since 1985 because of global warming. The volcano continues to pose a threat to the nearby towns and villages, and it is estimated that up to 500,000 people could be at risk from lahars from future eruptions.