Rocks Foldable Directions: Use your notes and Science textbook to
... Sedimentary rocks form Igneous rocks form from Metamorphic rocks form when particles of other rocks the cooling of ____?____, when an existing rock is or the remains of plants and changed by _____?______ below Earth’s surface, or animals are _______?_____ ___?____, above Earth’s & ________?_______. ...
... Sedimentary rocks form Igneous rocks form from Metamorphic rocks form when particles of other rocks the cooling of ____?____, when an existing rock is or the remains of plants and changed by _____?______ below Earth’s surface, or animals are _______?_____ ___?____, above Earth’s & ________?_______. ...
Classification of Igneous Rocks
... Igneous rocks form by direct crystallization of minerals from a magma melt. Intrusive (plutonic) rocks crystallize at depth, whereas extrusive (volcanic and pyroclastic rocks) rocks crystallize after the magma reaches the earth's surface. In general, extrusive rocks have a finer grained texture than ...
... Igneous rocks form by direct crystallization of minerals from a magma melt. Intrusive (plutonic) rocks crystallize at depth, whereas extrusive (volcanic and pyroclastic rocks) rocks crystallize after the magma reaches the earth's surface. In general, extrusive rocks have a finer grained texture than ...
EarthLayersPlateTectonicsPP
... thermal energy as the isotopes go through radioactive decay. 3. Bombardment by Asteroids and Meteors also caused mechanical energy to be converted into thermal energy . ...
... thermal energy as the isotopes go through radioactive decay. 3. Bombardment by Asteroids and Meteors also caused mechanical energy to be converted into thermal energy . ...
Study Guide for 3rd nine week assessment 2017
... type of rocks. 15. Erosion and deposition are occurring constantly in the coastal plain 16. When El Nino occurs this causes a reduction in fish because upwelling stops and down welling begins 17. Pyrite is an ore of Iron and is easily oxidized in the presence of oxygen 18. Earthquakes are going to b ...
... type of rocks. 15. Erosion and deposition are occurring constantly in the coastal plain 16. When El Nino occurs this causes a reduction in fish because upwelling stops and down welling begins 17. Pyrite is an ore of Iron and is easily oxidized in the presence of oxygen 18. Earthquakes are going to b ...
![Hotspots [This Dynamic Earth, USGS]](http://s1.studyres.com/store/data/017105727_1-1201bcefda6f82aa93505be247414c20-300x300.png)
Changing Earth - Ms. Stinson's Science Class
... becomes denser, and sinks. This occurs where two p move together at a convergent boundary. When an oceanic plate converges with a less dense continental plate, the denser oceanic plate sinks under the continental plate. The area where an oceanic plate subducts, or goes down, into the mantle is calle ...
... becomes denser, and sinks. This occurs where two p move together at a convergent boundary. When an oceanic plate converges with a less dense continental plate, the denser oceanic plate sinks under the continental plate. The area where an oceanic plate subducts, or goes down, into the mantle is calle ...
Newid tectoneg 1
... At least twice during this long period in Earth's history the positions of the continents and their effect upon ocean currents caused the Earth to enter an ice age (at about 2300 and 700 million years ago). There is evidence for this second ice age in rocks from the Skerries just to the north of Ang ...
... At least twice during this long period in Earth's history the positions of the continents and their effect upon ocean currents caused the Earth to enter an ice age (at about 2300 and 700 million years ago). There is evidence for this second ice age in rocks from the Skerries just to the north of Ang ...
The Reykjanes Peninsula Oblique Rift, a zone of crustal extension
... segments are oblique to the over-all plate velocity vector between the North America and Eurasia Plates. Oblique and immature plate boundaries are frequently characterized by complicated fault patterns, which makes their seismogenic potential and seismic hazard difficult to assess. The Reykjanes Pen ...
... segments are oblique to the over-all plate velocity vector between the North America and Eurasia Plates. Oblique and immature plate boundaries are frequently characterized by complicated fault patterns, which makes their seismogenic potential and seismic hazard difficult to assess. The Reykjanes Pen ...
convection current
... (upper part is solid, lower part is partly melted). The upper mantle together with the crust forms the lithosphere. - The rock material in the mantle can flow very slowly. - Below the mantle is the core. The outer core is made up mainly of liquid iron and nickel, while the inner core is solid. Evide ...
... (upper part is solid, lower part is partly melted). The upper mantle together with the crust forms the lithosphere. - The rock material in the mantle can flow very slowly. - Below the mantle is the core. The outer core is made up mainly of liquid iron and nickel, while the inner core is solid. Evide ...
Think of one example of a “Command Word”
... Tectonics Plate above move. 1 mark The convection currents in the Mantle, powered by the heat from the Core, mean that the Tectonic Plates of the Earth’s crust will move. ...
... Tectonics Plate above move. 1 mark The convection currents in the Mantle, powered by the heat from the Core, mean that the Tectonic Plates of the Earth’s crust will move. ...
Guided Notes on the Causes of Plate Motions
... How does a convection current start? What causes one to stop? Does convection only take place in the upper mantle, or does it also take place in the core? ...
... How does a convection current start? What causes one to stop? Does convection only take place in the upper mantle, or does it also take place in the core? ...
Earth`s Interior Introduction
... Layers of the Earth - Mantle – _____________ km thick - rock - Upper mantle – ________________ rock (closer to surface) - ________________ mantle – plastic rock (___________ magma) ...
... Layers of the Earth - Mantle – _____________ km thick - rock - Upper mantle – ________________ rock (closer to surface) - ________________ mantle – plastic rock (___________ magma) ...
Unit 1 Plate Tectonics UNIT 2: LAYERS OF THE EARTH STUDY
... the tremendous pressure upon it. There are two types of crust: oceanic crust and continental crust. ...
... the tremendous pressure upon it. There are two types of crust: oceanic crust and continental crust. ...
Where does subduction initiate and die? Insights from global
... Our calculations indicate that the presence of the continents alterns stress distribution within a certain distance from the margins. Intra-oceanic subudction initiation is favorable during super-continent cycles while the initiation at passive continental margin prevails when continents are dispers ...
... Our calculations indicate that the presence of the continents alterns stress distribution within a certain distance from the margins. Intra-oceanic subudction initiation is favorable during super-continent cycles while the initiation at passive continental margin prevails when continents are dispers ...
doc
... 1) The rock cycle relates all types of rocks on Earth together through specific processes. 2) Rock types, in the broad sense, are defined based on their mode of formation. 3) Igneous rocks are rocks that form from the cooling and solidification of magma. 4) Further classification of igneous rocks is ...
... 1) The rock cycle relates all types of rocks on Earth together through specific processes. 2) Rock types, in the broad sense, are defined based on their mode of formation. 3) Igneous rocks are rocks that form from the cooling and solidification of magma. 4) Further classification of igneous rocks is ...
Earth Science - Faustina Academy
... Plasticlike layer below lithosphere on which plates of lithosphere float (pg. 284) Plate Boundaries When plates move, they can move toward each other and converge They also pull apart or slide alongside one another When the plates interact, result of movement is seen at plate boundaries Divergent Bo ...
... Plasticlike layer below lithosphere on which plates of lithosphere float (pg. 284) Plate Boundaries When plates move, they can move toward each other and converge They also pull apart or slide alongside one another When the plates interact, result of movement is seen at plate boundaries Divergent Bo ...
Lesson: Rock Cycle-Focus on Igneous Rocks
... 1) The rock cycle relates all types of rocks on Earth together through specific processes. 2) Rock types, in the broad sense, are defined based on their mode of formation. 3) Igneous rocks are rocks that form from the cooling and solidification of magma. 4) Further classification of igneous rocks is ...
... 1) The rock cycle relates all types of rocks on Earth together through specific processes. 2) Rock types, in the broad sense, are defined based on their mode of formation. 3) Igneous rocks are rocks that form from the cooling and solidification of magma. 4) Further classification of igneous rocks is ...
![c1b revision sheet 1[1]](http://s1.studyres.com/store/data/016683336_1-baea0f7acdab057d50ded8ac95b62330-300x300.png)
c1b revision sheet 1[1]
... The Earth is made up of 3 layers - crust, mantle and core crust - relatively thin and rocky. mantle - has the properties of a solid, but can flow very slowly. outer core - made from liquid nickel and iron inner core - made from solid nickel and iron ...
... The Earth is made up of 3 layers - crust, mantle and core crust - relatively thin and rocky. mantle - has the properties of a solid, but can flow very slowly. outer core - made from liquid nickel and iron inner core - made from solid nickel and iron ...
What are the three types of convergent boundaries? oceanic
... Potentially the most dangerous to human and most destructive to the environment; Mount St. Helens was an example of this type of volcano. Composite Stretching along the western coasts of North and South America and down the eastern coast of Asia, the CircumPacific Belt marks the location of most con ...
... Potentially the most dangerous to human and most destructive to the environment; Mount St. Helens was an example of this type of volcano. Composite Stretching along the western coasts of North and South America and down the eastern coast of Asia, the CircumPacific Belt marks the location of most con ...
Review for Seafloor Spreading, Plate Tectonics
... Describe evidence from drilling samples. Describe evidence from magnetic stripes. When was the last time the Earth’s magnetic field changed? Describe subduction and where it happens. What does density have to do with seafloor spreading? What is happening to the Atlantic and Pacific Oceans – describ ...
... Describe evidence from drilling samples. Describe evidence from magnetic stripes. When was the last time the Earth’s magnetic field changed? Describe subduction and where it happens. What does density have to do with seafloor spreading? What is happening to the Atlantic and Pacific Oceans – describ ...
Volcanoes and Igneous Activity Earth - Chapter 4
... produced along the oceanic ridge system • Mechanism of spreading» Lithosphere pulls apart » Less pressure on underlying rocks » Results in partial melting of mantle » Large quantities of basaltic magma are produced ...
... produced along the oceanic ridge system • Mechanism of spreading» Lithosphere pulls apart » Less pressure on underlying rocks » Results in partial melting of mantle » Large quantities of basaltic magma are produced ...
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.