study guide – unit 9 – plate tectonics
... magnetic reversal: magnetic minerals create same pattern on both sides, Earth’s polarity has reversed ...
... magnetic reversal: magnetic minerals create same pattern on both sides, Earth’s polarity has reversed ...
DISASTER EMERGENCY RESPONSE. Part VI.
... • It is a unique plate, because it is surrounded by subduction zones. ...
... • It is a unique plate, because it is surrounded by subduction zones. ...
Earthquakes and Volcanoes
... • Composite- made up of alternating layers of rock particles; explosive eruptions, then quite lava flows ...
... • Composite- made up of alternating layers of rock particles; explosive eruptions, then quite lava flows ...
Hawaiian Slumps
... Volcaniclastic rocks on the flanks of landslide blocks OAHU, MOLOKAI - The rocks exposed on the steep slopes of giant landslide blocks in the Nuuanu and Wailau landslides are fragmental rocks: hyaloclastite and volcaniclastic breccias. They form as 1) secondary slope mantling of unlithified breccia ...
... Volcaniclastic rocks on the flanks of landslide blocks OAHU, MOLOKAI - The rocks exposed on the steep slopes of giant landslide blocks in the Nuuanu and Wailau landslides are fragmental rocks: hyaloclastite and volcaniclastic breccias. They form as 1) secondary slope mantling of unlithified breccia ...
Geography 12
... 11. _D____This plate boundary is where ocean and continental plates crash into each other forming volcanic mountain ranges. 12. __H___ This plate boundary is where two plates move away from each other. 13. ___J__ This plate boundary two plates crash together forming fold mountain ranges. 14. __A___ ...
... 11. _D____This plate boundary is where ocean and continental plates crash into each other forming volcanic mountain ranges. 12. __H___ This plate boundary is where two plates move away from each other. 13. ___J__ This plate boundary two plates crash together forming fold mountain ranges. 14. __A___ ...
Napoleon - Kawameeh Middle School
... What are that the continents fit together like a puzzle, same fossils can be found on 2 different continents, same types of ...
... What are that the continents fit together like a puzzle, same fossils can be found on 2 different continents, same types of ...
Chapter 9 Notes
... 1. The key to understanding why volcanoes erupt is to understand how magma forms. a. Volcanoes result from magma formed in the mantle. b. When pressure is reduced, some of the solid rock of the already hot mantle melts to form magma. c. Because it is less dense than the surrounding rock, magma rises ...
... 1. The key to understanding why volcanoes erupt is to understand how magma forms. a. Volcanoes result from magma formed in the mantle. b. When pressure is reduced, some of the solid rock of the already hot mantle melts to form magma. c. Because it is less dense than the surrounding rock, magma rises ...
paleogeography (plate tectonics)
... a. seamount: a volcanic mountain that is more than 1 km tall but does not break the surface of the water i. tablemount [guyot]: a flat-topped seamount; it has been eroded by wave action at the surface or may have subsided due to tectonic movement b. abyssal hills [seaknolls]: short features under 1 ...
... a. seamount: a volcanic mountain that is more than 1 km tall but does not break the surface of the water i. tablemount [guyot]: a flat-topped seamount; it has been eroded by wave action at the surface or may have subsided due to tectonic movement b. abyssal hills [seaknolls]: short features under 1 ...
APES Earth Science Study Guide
... 23) Describe what happens at the three plate boundaries in terms of motion, effect on crust, and volcanic activity. ...
... 23) Describe what happens at the three plate boundaries in terms of motion, effect on crust, and volcanic activity. ...
Volcanic Landforms and Processes
... composition of magma. – Basalt: fluid, forms thin laterally extensive flows – Siliceous, viscous magmas (rhyolite/dacite) form thick pasty flows with steep margins. – Lobate forms, lava levees, crescent-shaped pressure ridges, irregular surfaces and lack of surface streams rhyolitic dome, Long Valle ...
... composition of magma. – Basalt: fluid, forms thin laterally extensive flows – Siliceous, viscous magmas (rhyolite/dacite) form thick pasty flows with steep margins. – Lobate forms, lava levees, crescent-shaped pressure ridges, irregular surfaces and lack of surface streams rhyolitic dome, Long Valle ...
Volcano - Curriculum Visions
... Fine, powdery material thrown out of a volcano The vertical pipe that carries molten rock to the surface ...
... Fine, powdery material thrown out of a volcano The vertical pipe that carries molten rock to the surface ...
process that occurs when tectonic plates of different densities collide
... silica and gas rich, intermediate in direction of thick, viscous and viscosity, silica and movement under ...
... silica and gas rich, intermediate in direction of thick, viscous and viscosity, silica and movement under ...
During October, researchers deployed at Mount Saint Helens
... episode, and data needed to maximize public safety. A longperiod tremor (5 -10 second period) began around 1200 hrs (GMT) on 6 Oct. and continued for at least two days. It was observed throughout the local broadband network, but not at a site ~68 km to the north. Evidence points to a local source fo ...
... episode, and data needed to maximize public safety. A longperiod tremor (5 -10 second period) began around 1200 hrs (GMT) on 6 Oct. and continued for at least two days. It was observed throughout the local broadband network, but not at a site ~68 km to the north. Evidence points to a local source fo ...
Cinder cones
... Shield Volcanoes large volcanoes with broad summit areas and low-sloping sides - low viscosity basaltic lava flows. ...
... Shield Volcanoes large volcanoes with broad summit areas and low-sloping sides - low viscosity basaltic lava flows. ...
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.