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Chapter 10 Section 3
... boundary, where plates move together. Another type of plate boundary is a divergent boundary, where plates pull apart. Finally, there is a transform boundary where plates ...
... boundary, where plates move together. Another type of plate boundary is a divergent boundary, where plates pull apart. Finally, there is a transform boundary where plates ...
2.(and other) Natural Hazard physical event that happens naturally
... People can change and adapt as a result of a natural disaster Countries may develop and establish better responses and organisational systems to deal with future emergencies. Stress can push others away, it’s too much to handle. Ridges and trenches Ridges form where tectonic plates move apart, ...
... People can change and adapt as a result of a natural disaster Countries may develop and establish better responses and organisational systems to deal with future emergencies. Stress can push others away, it’s too much to handle. Ridges and trenches Ridges form where tectonic plates move apart, ...
Geology Study Guide
... 14. Fill in the blank with correct vocabulary: S- Wave P-Wave Elastic rebound Elastically deformed Pyroclastic material Pahoehoe ...
... 14. Fill in the blank with correct vocabulary: S- Wave P-Wave Elastic rebound Elastically deformed Pyroclastic material Pahoehoe ...
Igneous Rocks Follow-Along Notes
... Use the Igneous Rocks notes to answer the following questions and fill in the following blanks ...
... Use the Igneous Rocks notes to answer the following questions and fill in the following blanks ...
Chapter 1—Plate Tectonics and California
... d. CA doesn’t have plate boundaries 9. A deep, linear, relatively narrow depression in the Earth’s surface that develops where oceanic plates subduct is a(n): a. ocean trench b. forearc basin c. volcanic arc d. backarc basin e. island arc 10. Sea floor spreading occurs at: a. subduction zones b. oce ...
... d. CA doesn’t have plate boundaries 9. A deep, linear, relatively narrow depression in the Earth’s surface that develops where oceanic plates subduct is a(n): a. ocean trench b. forearc basin c. volcanic arc d. backarc basin e. island arc 10. Sea floor spreading occurs at: a. subduction zones b. oce ...
What is the Plate Tectonic Theory?
... • States the lithosphere is divided into broken pieces (tectonic plates) that are shifting over the asthenosphere (upper mantle). ...
... • States the lithosphere is divided into broken pieces (tectonic plates) that are shifting over the asthenosphere (upper mantle). ...
document
... The focus is the location within Earth along a fault at which the first motion of an earthquake occurs. The epicenter is the point on Earth’s surface directly above an earthquake’s focus ...
... The focus is the location within Earth along a fault at which the first motion of an earthquake occurs. The epicenter is the point on Earth’s surface directly above an earthquake’s focus ...
Section 13.2
... millions of years to move. • Decreased pressure and the addition of water lower the melting temperature of mantle rock so that it melts. ...
... millions of years to move. • Decreased pressure and the addition of water lower the melting temperature of mantle rock so that it melts. ...
The theory of plate tectonics
... magma gradually rises and cools between plates new rock called igneous rock is formed. Formation and uses of Igneous Rocks The word igneous means fire. Igneous rocks are formed directly from magma as it cools. The type of igneous rock depends upon the speed at which magma cools. Slow cooling – intru ...
... magma gradually rises and cools between plates new rock called igneous rock is formed. Formation and uses of Igneous Rocks The word igneous means fire. Igneous rocks are formed directly from magma as it cools. The type of igneous rock depends upon the speed at which magma cools. Slow cooling – intru ...
Earth*s Structure
... Pangea Theory •All continents originally one land mass: Pangea 245 million years ago •Wegener’s Hypothesis: continental driftsingle land mass broke up many times over the years and moved to where they are now ...
... Pangea Theory •All continents originally one land mass: Pangea 245 million years ago •Wegener’s Hypothesis: continental driftsingle land mass broke up many times over the years and moved to where they are now ...
Document
... Economic uses Many types of igneous rocks are used as building stone, facing stone, and decorative material, such as that used for tabletops, cutting boards, and ...
... Economic uses Many types of igneous rocks are used as building stone, facing stone, and decorative material, such as that used for tabletops, cutting boards, and ...
Name: : Earth Science Mr. Herman Exeter SHS Chapter 10.3
... Sills and Laccoliths are plutons that form when magma is intruded close to the surface. Sills resemble buried lava flows and may exhibit columnar joints. Laccoliths are lens-shaped masses that arch overlying strata upward. ...
... Sills and Laccoliths are plutons that form when magma is intruded close to the surface. Sills resemble buried lava flows and may exhibit columnar joints. Laccoliths are lens-shaped masses that arch overlying strata upward. ...
Plate Tectonics - msaldrichscience
... Plate tectonics refers to the building of the features on Earths surface due to deformation caused by plate movements. Create mountain ranges, trenches, and rift valleys at or near plate boundaries. Particularly evident around rim of Pacific Ocean where subduction of oceanic plates around much ...
... Plate tectonics refers to the building of the features on Earths surface due to deformation caused by plate movements. Create mountain ranges, trenches, and rift valleys at or near plate boundaries. Particularly evident around rim of Pacific Ocean where subduction of oceanic plates around much ...
Plate Boundaries
... • The continents were once a super-continent called Pangea • the continents are plowing through the ocean floors---most people didn’t believe this ...
... • The continents were once a super-continent called Pangea • the continents are plowing through the ocean floors---most people didn’t believe this ...
ES Unit 3 standards - Springfield Public Schools
... tectonic plates. Explain the factors that determine the type of volcanic ...
... tectonic plates. Explain the factors that determine the type of volcanic ...
Words to know
... Mid ocean ridge—the fracture zone along the ocean bottom where molten mantle material comes to the surface, thus creating new crust. This fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies. ...
... Mid ocean ridge—the fracture zone along the ocean bottom where molten mantle material comes to the surface, thus creating new crust. This fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies. ...
PRE-POSTTESTwithANSWERS
... 1. The crust and upper mantle make up the Earth’s: a. lithosphere; b. asthenosphere; c. core, d. continents 2. Plates move apart at ____ boundaries. a. convergent; b. stable; c. divergent; d. transform 3. What occurs when an oceanic plate meets a continental plate? a. convection; b. subduction; c. d ...
... 1. The crust and upper mantle make up the Earth’s: a. lithosphere; b. asthenosphere; c. core, d. continents 2. Plates move apart at ____ boundaries. a. convergent; b. stable; c. divergent; d. transform 3. What occurs when an oceanic plate meets a continental plate? a. convection; b. subduction; c. d ...
Chemical Reactions, Chemical Equations, Electricity
... Evolution – the process of change over time Tectonic Plates – giant chunks of land or ocean floor in which the lithosphere is broken up into Theory of Plate Tectonics – a theory that states that Earth’s lithosphere, or land, is broken into large sections called tectonic plates that move and change p ...
... Evolution – the process of change over time Tectonic Plates – giant chunks of land or ocean floor in which the lithosphere is broken up into Theory of Plate Tectonics – a theory that states that Earth’s lithosphere, or land, is broken into large sections called tectonic plates that move and change p ...
Dual Credit Major Topics for Studying
... Dual Credit Major Topics for Studying Plate Tectonics Earth’s structure: Layers and properties (i.e. crust, mantle core) Names of plates Continental Drift Types of volcanoes; magma types (felsic and maffic) Features of volcanoes Lava types Seismic waves, earthquakes liquefaction 20 ...
... Dual Credit Major Topics for Studying Plate Tectonics Earth’s structure: Layers and properties (i.e. crust, mantle core) Names of plates Continental Drift Types of volcanoes; magma types (felsic and maffic) Features of volcanoes Lava types Seismic waves, earthquakes liquefaction 20 ...
1. 1. Draw a subduction zone in which an oceanic plate collides with
... 1. 1. Draw a subduction zone in which an oceanic plate collides with a continental plate. Label the following on your sketch: the oceanic plate, the continental plate, location of seismicity (if any), location of volcanism (if any). Draw the boundary between the crust and the mantle and the boundary ...
... 1. 1. Draw a subduction zone in which an oceanic plate collides with a continental plate. Label the following on your sketch: the oceanic plate, the continental plate, location of seismicity (if any), location of volcanism (if any). Draw the boundary between the crust and the mantle and the boundary ...
Unit 7 Study Guide Answer Key
... 14. Earthquakes occur most often at Transform boundaries. They also occur at other types of boundaries as well as fault lines. 15. Volcanoes form at hot spots (like Hawaii) as well as near Subduction Zones. They happen because magma from the mantle rises up through the crust. 16. As more and more m ...
... 14. Earthquakes occur most often at Transform boundaries. They also occur at other types of boundaries as well as fault lines. 15. Volcanoes form at hot spots (like Hawaii) as well as near Subduction Zones. They happen because magma from the mantle rises up through the crust. 16. As more and more m ...
Large igneous province
![](https://commons.wikimedia.org/wiki/Special:FilePath/Flood_Basalt_Map.jpg?width=300)
A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.