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Profile Documents Logout
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- Google Sites
- Google Sites

... The materials in the mantle heat, become less dense and rise. Then they cool, become more dense and sink. The cycle continues and moves the plates. 3. How was the Grand Canyon formed? Flowing water eroded existing rock layers in a gradual, destructive process. 4. What causes rock to break apart? Roo ...
Geology of the Roque Island Archipelago
Geology of the Roque Island Archipelago

... Siltstone: From silt compacted and bound together. Minerals grow in spaces between silt grains binding them and forming rock. Recognizable layers. Grains can be felt but not seen Minerals: Silica, calcite, iron oxides. Tuffs: Fine grained volcanic ash. Grain size is less than 2mm in diameter. Ash de ...
Think of one example of a “Command Word”
Think of one example of a “Command Word”

... 2 (a). 1 mark for pointing out that they are mostly found on plate boundaries. 2 marks for describing that most are found around the pacific plate or that there is an unusual volcano location in the middle of the Pacific plate. (b) 1 mark each up to 2 marks for: Steep sided ...
Task to i) Explain how continental drift works to move tectonic plates
Task to i) Explain how continental drift works to move tectonic plates

... the liquid outer core and the solid inner core. ...
Suggested Answers: Extension Questions
Suggested Answers: Extension Questions

... (c) (i) Gases are released due to loss of pressure as the magma approaches the surface, causing it to froth up and explode as eruption takes place. Rock and pumice fragments are then thrown high into the atmosphere. (ii) A mixture of hot gas and “ash” that forms a dense fluid able to flow downhill a ...
INTRODUCCIÓN: LOS ANDES
INTRODUCCIÓN: LOS ANDES

... As the Ecuadorian volcanic belt is a result of the subducted and in the upper mantle remelted oceanic Nazca plate, extends N-S along the whole country, with an average width of about 80 km. The Quaternary activity is characterized by the building of a great number of huge stratovolcanoes form the h ...
Monday 4/1 - cloudfront.net
Monday 4/1 - cloudfront.net

... • Body waves-travel thru the earth’s interior. ...
The complicated birth of a volcano: Researchers unravel
The complicated birth of a volcano: Researchers unravel

... Marine Research just published possible ...
Objective: Students will diagram faults, waves and volcanoes in
Objective: Students will diagram faults, waves and volcanoes in

... 1. divergent boundaries = occur where plate move ___________ Where are most of these boundaries found? __________ 2. convergent boundaries (mountains/subduction) = occur where plates ____ _____________. 3. transform boundaries = occur where plates _________ past each other. The sea floor spreads apa ...
Natural Hazards Case Studies - Chew Valley School | Intranet
Natural Hazards Case Studies - Chew Valley School | Intranet

... "We didn't hear any kind of alarm, even when the ash was falling and we were in the hotel . . . we turned on the radio . . . The mayor was talking and he said not to worry, that it was a rain of ash, that they had not reported anything from the Nevado, and to stay calm in our houses.There was a loca ...
Analysis on Rock Textures Submitted by WWW
Analysis on Rock Textures Submitted by WWW

... lavas; bombs are semimolten pieces of lava that solidify as they fall. Small crystals (generally feldspars) that had been formed in the magma before it was ejected are also deposited with the other pyroclastics. A tuff is composed of fine‐grained pyroclastic material and is named by the most distinc ...
The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics

... Pacific Ring of Fire ...
Study Guide - SUSDIntelEssentialsSection2Downs
Study Guide - SUSDIntelEssentialsSection2Downs

... 14. continental drift 15. plate tectonics 16. focus 17. epicenter 18. primary waves 19. secondary waves 20. seismograph 21. transform boundary 22. divergent boundary 23. convergent boundary 24. subduction 25. hot spots 26. convection 27. oceanic-continental subduction 28. continental-continental col ...
summing-up - Zanichelli online per la scuola
summing-up - Zanichelli online per la scuola

... formed as a result of the subduction of an oceanic plate beneath a continental plate and is characterised by the activity of many explosive volcanoes. ...
`I. True/False Questions: circle a “T” for true or “F” for false (10% total
`I. True/False Questions: circle a “T” for true or “F” for false (10% total

... 3. (T F) After a theory has survived much scientific scrutiny, it may be elevated to hypothesis status. 4. (T F) Convergent plate tectonic boundaries are located where plates move toward one another. 5. (T F) Transform plate boundaries only affect oceanic lithosphere. 6. (T F) A dike is a concordant ...
Dynamic Crust
Dynamic Crust

... b) ___________________________________________: Oceanic – Oceanic crust (1) ______________________ bearing minerals, brought down with the suducting plate causes the rock to __________________________. (2) This magma___________________________ through overlying ______________________ and creates dee ...
File - Ms Hicks` Classes
File - Ms Hicks` Classes

... • Ex: the boundary between the North American plate and the Pacific plate in California ...
The Mid Atlantic Ridge
The Mid Atlantic Ridge

... Mid Atlantic Ridge. However, every so often, Iceland experiences a significant earthquake. These earthquakes are a reminder of the spreading continental plates and the tensions that build up in the newly forming crust. In May 2008 an earthquake measuring 6.3 on the richter scale had its epicentre ju ...
Volcanism in Response to Plate Flexure
Volcanism in Response to Plate Flexure

... magnitude less than those typical of hot spot volcanoes. We found 4.2 to 8.5 million-yearold volcanoes at site A, suggesting episodic eruption of magma over a distance of 400 km of plate motion. Accordingly, the petit spot volcanic province is characterized by several million years of small-volume m ...
Goldschmidt2007
Goldschmidt2007

... magma during its ascent in the conduit. We can reveal this information by measuring the physico-chemical properties of volcanic ejecta. Between 16th and 18th of August 2006 a large eruption occurred on Tungurahua volcano including fire fountains, ash-, rock- and pumice falls and lava flows, as well ...
Year 9 Term 1: Earth and Space- Plate Tectonics 2015 (Week 6-10)
Year 9 Term 1: Earth and Space- Plate Tectonics 2015 (Week 6-10)

... explains how advances in scientific understanding of processes that occur within and on the Earth, influence the choices people make about resource use and management ES2 The theory of plate tectonics explains global patterns of geological activity and ...
Geology – EXAM-1 Fall-2009
Geology – EXAM-1 Fall-2009

... a. chemical weathering of olivine and plagioclase feldspar b. mechanical weathering of granite and rhyolite c. chemical weathering of orthoclase feldspar d. differential mechanical weathering of micas 39. What two factors speed up rates of chemical reaction and weathering in rocks and soils? A) low ...
Plate Tectonics plate boundaries Blas
Plate Tectonics plate boundaries Blas

... SUBDUCTION Volcanoes, mountains, and earthquakes occur at Convergent Crust Boundaries ...
POLOVINKA-ODNOBOKAYA-ACADEMII NAUK CALDERA
POLOVINKA-ODNOBOKAYA-ACADEMII NAUK CALDERA

... The melt in the upper crust chambers was compositionally evolved prior to eruption, which is suggested by the gradients in composition, temperature and volatile contents for each caldera-forming eruption. The disequilibrium mineral assemblage of the products of climactic eruptions, as well as the oc ...
Earth`s Skin: Plate Tectonics Document Contents
Earth`s Skin: Plate Tectonics Document Contents

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Volcano



A volcano is a rupture on the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.Earth's volcanoes occur because its crust is broken into 17 major, rigid tectonic plates that float on a hotter, softer layer in its mantle. Therefore, on Earth, volcanoes are generally found where tectonic plates are diverging or converging. For example, a mid-oceanic ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates coming together. Volcanoes can also form where there is stretching and thinning of the crust's interior plates, e.g., in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande Rift in North America. This type of volcanism falls under the umbrella of ""plate hypothesis"" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so-called ""hotspots"", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Volcanoes are usually not created where two tectonic plates slide past one another.Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. One such hazard is that volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature; the melted particles then adhere to the turbine blades and alter their shape, disrupting the operation of the turbine. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere (or troposphere); however, they also absorb heat radiated up from the Earth, thereby warming the upper atmosphere (or stratosphere). Historically, so-called volcanic winters have caused catastrophic famines.
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