Plate Tectonics Bingo - Western Reserve Public Media
... something down (as by particles washing over it) Eruption: When ash and lava flows and gases are ejected from deep within the earth Fault: An area of stress in the earth where broken rocks slide past each other, causing a crack in the Earth’s surface Igneous rock: Rock that is formed when magma cool ...
... something down (as by particles washing over it) Eruption: When ash and lava flows and gases are ejected from deep within the earth Fault: An area of stress in the earth where broken rocks slide past each other, causing a crack in the Earth’s surface Igneous rock: Rock that is formed when magma cool ...
inner core
... constantly changes is called theory of plate tectonic. • The theory states that the earth’s outer shell, the lithosphere is divided into eight large plates. • Because each plate moves as a single unit, the interiors of the plates are generally stable. • All major activity such as ...
... constantly changes is called theory of plate tectonic. • The theory states that the earth’s outer shell, the lithosphere is divided into eight large plates. • Because each plate moves as a single unit, the interiors of the plates are generally stable. • All major activity such as ...
IGNEOUS ROCKS There are places on Earth that are so hot that
... There are places on Earth that are so hot that rocks melt to form magma. Because magma is liquid and usually less dense than surrounding solid rock, it moves upward to cooler regions of the Earth. As the magma cools, it solidifies and crystallizes into an igneous rock. Magma can cool on the Earth's ...
... There are places on Earth that are so hot that rocks melt to form magma. Because magma is liquid and usually less dense than surrounding solid rock, it moves upward to cooler regions of the Earth. As the magma cools, it solidifies and crystallizes into an igneous rock. Magma can cool on the Earth's ...
Timeline of the development of the theory of plate tectonics
... 1960 American geophysicist Harry H. Hess developed the idea that oceanic crust forms along mid-ocean ridges and spreads out laterally away from the ridges. The following year, geophysicist Robert S. Dietz named the phenomenon seafloor spreading. Hess and Dietz’s work played a pivotal role in the dev ...
... 1960 American geophysicist Harry H. Hess developed the idea that oceanic crust forms along mid-ocean ridges and spreads out laterally away from the ridges. The following year, geophysicist Robert S. Dietz named the phenomenon seafloor spreading. Hess and Dietz’s work played a pivotal role in the dev ...
PLATE TECTONICS MAPPING LAB
... 6. Most of the Pacific Ocean is on what plate? 7. What is the compass orientation of the Hawaiian Islands and many of the other smaller ridges within the Pacific Ocean? Is this significant? 8. In what compass direction is the Pacific Plate moving? 9. Name the biggest and longest mountain range in th ...
... 6. Most of the Pacific Ocean is on what plate? 7. What is the compass orientation of the Hawaiian Islands and many of the other smaller ridges within the Pacific Ocean? Is this significant? 8. In what compass direction is the Pacific Plate moving? 9. Name the biggest and longest mountain range in th ...
Structure of the Earth - Mercer Island School District
... High silica magma found in more explosive volcanoes due to build up of pressure with ...
... High silica magma found in more explosive volcanoes due to build up of pressure with ...
GE1632013UFINALEXAM
... J. a rock or sediment body that contains fluid that can be removed K. structure built perpendicular to shoreline to interrupt transport and to trap sand on upcurrent side L. name for materials blown from a volcano M. point of origination in the Earth of an earthquake N. excessive erosion O. water be ...
... J. a rock or sediment body that contains fluid that can be removed K. structure built perpendicular to shoreline to interrupt transport and to trap sand on upcurrent side L. name for materials blown from a volcano M. point of origination in the Earth of an earthquake N. excessive erosion O. water be ...
earth structure ppt
... Core – 2900 km – 6370 km large mass, higher density metal, iron and nickel ...
... Core – 2900 km – 6370 km large mass, higher density metal, iron and nickel ...
File - Paxson Science
... that if you choose to type your answers, be aware that cutting & pasting from the Internet (or other’s work) is plagiarism, and will be counted as cheating! This assignment is worth 20 points and is due Monday, October 24. Make 3 column notes for the following vocabulary words. (9 points) Column hea ...
... that if you choose to type your answers, be aware that cutting & pasting from the Internet (or other’s work) is plagiarism, and will be counted as cheating! This assignment is worth 20 points and is due Monday, October 24. Make 3 column notes for the following vocabulary words. (9 points) Column hea ...
Geology Test Study Guide Answers
... Divergent boundaries- when plates move away from one another – sea floor spreading happen, mid-ocean ridges can form. Transform boundaries- plates slide up and down against each other- earthquakes happen Volcanic Mountains- Forms at subduction zones. Ex: Mount St. Helen Earthquakes- Chapter 8 1. Wha ...
... Divergent boundaries- when plates move away from one another – sea floor spreading happen, mid-ocean ridges can form. Transform boundaries- plates slide up and down against each other- earthquakes happen Volcanic Mountains- Forms at subduction zones. Ex: Mount St. Helen Earthquakes- Chapter 8 1. Wha ...
An Introduction to Geology - e
... 13. Into how many concentric compositional layers is Earth divided? a. 1; b. 2; c. 3; d. 4; e. 5 14. Earth's core is inferred to be: a. hollow; b. composed of rock with a high silica content; c. completely molten; d. composed mostly of iron and nickel; e. completely solid. 15. The asthenosphere: a. ...
... 13. Into how many concentric compositional layers is Earth divided? a. 1; b. 2; c. 3; d. 4; e. 5 14. Earth's core is inferred to be: a. hollow; b. composed of rock with a high silica content; c. completely molten; d. composed mostly of iron and nickel; e. completely solid. 15. The asthenosphere: a. ...
NOTES Plate Tectonics
... 10. If new ocean floor is added all the time at mid-ocean ridges, why is the Earth not getting larger? Old ocean floor is subducted at continental margins. 11. Subduction - the process that occurs when ocean floor sinks beneath a deep ocean trench and returns to the mantle. ...
... 10. If new ocean floor is added all the time at mid-ocean ridges, why is the Earth not getting larger? Old ocean floor is subducted at continental margins. 11. Subduction - the process that occurs when ocean floor sinks beneath a deep ocean trench and returns to the mantle. ...
File
... 2. Convergent (boundaries of destruction) Three types of destructive boundaries: 1. Oceanic-oceanic: where two ocean plates collide 2. Oceanic-continental: where an ocean and continental plate ...
... 2. Convergent (boundaries of destruction) Three types of destructive boundaries: 1. Oceanic-oceanic: where two ocean plates collide 2. Oceanic-continental: where an ocean and continental plate ...
Michelle Tsai Week 6 – Can Catastrophic Plate Tectonics Explain
... The earth has a thin rocky outer layer about 5-70km thick, the crust, that is consisted of sedimentary rock layers, with fossils, underlying crystalline rocky basement of granites and metamorphosed sedimentary rocks. Underneath the crust, there’s a layer called mantle, which is made up of dense, war ...
... The earth has a thin rocky outer layer about 5-70km thick, the crust, that is consisted of sedimentary rock layers, with fossils, underlying crystalline rocky basement of granites and metamorphosed sedimentary rocks. Underneath the crust, there’s a layer called mantle, which is made up of dense, war ...
Plate Tectonics – Study Guide
... 1. A_____ W______ found evidence of continental drift. When he proposed this theory at first he could not identify the force that would move tectonic plates; other _____ did not accept his theory because he could not explain what could move such large plates. Later scientists linked the idea of c___ ...
... 1. A_____ W______ found evidence of continental drift. When he proposed this theory at first he could not identify the force that would move tectonic plates; other _____ did not accept his theory because he could not explain what could move such large plates. Later scientists linked the idea of c___ ...
Earth Unit Review
... Draw and Identify the layers of the earth using the following terms- crust, mantle, inner core, outer core, lithosphere, asthenosphere ...
... Draw and Identify the layers of the earth using the following terms- crust, mantle, inner core, outer core, lithosphere, asthenosphere ...
GeomorphReview1 - University of Colorado Denver
... Igneous body touching & “cooking” surrounding area ...
... Igneous body touching & “cooking” surrounding area ...
Large igneous province
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.