Balancing Redox Equations
... Before we balance a Redox equation lets first refresh our memory on how to calculate oxidation numbers. Oxidation Number - The charge that an atom would have if the compound in which it were found were ionic. The rules: 1) The sum of the oxidation numbers of the atoms in a molecule must be equal to ...
... Before we balance a Redox equation lets first refresh our memory on how to calculate oxidation numbers. Oxidation Number - The charge that an atom would have if the compound in which it were found were ionic. The rules: 1) The sum of the oxidation numbers of the atoms in a molecule must be equal to ...
Precipitation and Redox Reactions
... You have to use the Activity Series on the back of your Periodic Table to determine if this will happen. If the element by itself is above the element in the compound then the reaction will occur. If the element in the compound is above the element by itself, then no reaction will occur. ...
... You have to use the Activity Series on the back of your Periodic Table to determine if this will happen. If the element by itself is above the element in the compound then the reaction will occur. If the element in the compound is above the element by itself, then no reaction will occur. ...
The Earth`s Layers Foldable
... 3. Now you may cut out the layers! Also cut out the four squares and the 12 labels. Remember to cut out The Earth's Layers title. 4. Set one piece of blue paper in front of you. Closely trim the title. Paste The Earth's Layers title in the top left corner of the paper. 5. Paste the Crust right below ...
... 3. Now you may cut out the layers! Also cut out the four squares and the 12 labels. Remember to cut out The Earth's Layers title. 4. Set one piece of blue paper in front of you. Closely trim the title. Paste The Earth's Layers title in the top left corner of the paper. 5. Paste the Crust right below ...
Earth,Notes,RevQs,Ch12
... 3. Seismology is responsible for lower gasoline prices in that it provides the means by which geologists can “see” into our planet and find the more favorable structures where petroleum is located. 4. Oceanic crust and continental crust are different in several ways. Oceanic crust is formed at ocean ...
... 3. Seismology is responsible for lower gasoline prices in that it provides the means by which geologists can “see” into our planet and find the more favorable structures where petroleum is located. 4. Oceanic crust and continental crust are different in several ways. Oceanic crust is formed at ocean ...
PHESCh10
... Batholiths • Batholiths are large masses of igneous rock that formed when magma intruded at depth, became crystallized, and subsequently was exposed by erosion. • An intrusive igneous body must have a surface exposure greater than 100 square kilometers to be considered a batholith. ...
... Batholiths • Batholiths are large masses of igneous rock that formed when magma intruded at depth, became crystallized, and subsequently was exposed by erosion. • An intrusive igneous body must have a surface exposure greater than 100 square kilometers to be considered a batholith. ...
Volcanoes and Mountain Ranges Notes
... But, because pressure increases along with temperature, the rocks in the mantle remain solid For example, a rock's melting temperature on the surface might be 1000 ºC, but 200 km below the surface under much higher pressure, the melting temperature of the rock might be 1300 ºC. 1) Change in Pressure ...
... But, because pressure increases along with temperature, the rocks in the mantle remain solid For example, a rock's melting temperature on the surface might be 1000 ºC, but 200 km below the surface under much higher pressure, the melting temperature of the rock might be 1300 ºC. 1) Change in Pressure ...
APS Continental Crust RLR.pptx
... Figure 15. Four tectonic settings for continental refining via relamination. In all cases, the relaminating layer may be thrust directly beneath existing crust, rise en bloc, perhaps in a "subduction channel", or rise as diapirs through the mantle wedge, depending on physical conditions. In all case ...
... Figure 15. Four tectonic settings for continental refining via relamination. In all cases, the relaminating layer may be thrust directly beneath existing crust, rise en bloc, perhaps in a "subduction channel", or rise as diapirs through the mantle wedge, depending on physical conditions. In all case ...
plate boundaries.
... crust, the oceanic crust which is thinner and more _____ than the continental crust, _______ below the continental crust. ...
... crust, the oceanic crust which is thinner and more _____ than the continental crust, _______ below the continental crust. ...
Rocks and Minerals Jeopardy
... 200 pts. • The grains of a sedimentary rock are made out of ___________________, while the grains of an igneous rock are made out of ________________. ...
... 200 pts. • The grains of a sedimentary rock are made out of ___________________, while the grains of an igneous rock are made out of ________________. ...
Geomorphology of Volcanic / Igneous Landscapes
... Igneous Rocks- a rock (or agglomeration of one or more minerals) that results from the cooling of magma, or molten rock. As the magma cools, minerals crystallize from the molten rock. ...
... Igneous Rocks- a rock (or agglomeration of one or more minerals) that results from the cooling of magma, or molten rock. As the magma cools, minerals crystallize from the molten rock. ...
Divergent Boundaries: Origin and Evolution of the
... •Oceanic lithosphere subducts because its overall density is greater than the underlying mantle •Subduction of older, colder lithosphere results in descending angles of nearly 90º •Younger, warmer oceanic lithosphere is more buoyant and angles of descent are small •The lithospheric slab moves horizo ...
... •Oceanic lithosphere subducts because its overall density is greater than the underlying mantle •Subduction of older, colder lithosphere results in descending angles of nearly 90º •Younger, warmer oceanic lithosphere is more buoyant and angles of descent are small •The lithospheric slab moves horizo ...
Edible Tectonics
... is solid made up of very hot iron and nickel. High pressure here keeps these metals from melting. This layer has both solid and melted parts. The melted, yet still solid part flows very slowly. The solid upper layer of the mantle and the crust join to form this. This layer is the only liquid layer o ...
... is solid made up of very hot iron and nickel. High pressure here keeps these metals from melting. This layer has both solid and melted parts. The melted, yet still solid part flows very slowly. The solid upper layer of the mantle and the crust join to form this. This layer is the only liquid layer o ...
Earth`s Layers Answer for 25 Points
... This presentation may not be sold, or redistributed without written permission, and may only be used for non-profit educational use. ...
... This presentation may not be sold, or redistributed without written permission, and may only be used for non-profit educational use. ...
Chemistry of the Non
... We divide the periodic table into metals, nonmetals and metalloids. Nonmetals occupy the upper right portion of the periodic table. • H is a special case. Electronegativity is important when determining whether an element is a metal. Nonmetals tend to have higher electronegativities than metals. • T ...
... We divide the periodic table into metals, nonmetals and metalloids. Nonmetals occupy the upper right portion of the periodic table. • H is a special case. Electronegativity is important when determining whether an element is a metal. Nonmetals tend to have higher electronegativities than metals. • T ...
Earth Science Questions and Answers for Teachers Teaching Grade 6
... The geology of California is a textbook example of global geology. We are lucky, or cursed, to have so much active geology right in our backyard. When visiting Bodega Head or the Point Reyes Peninsula (or looking at a map of these areas), students can learn that most of California resides on the No ...
... The geology of California is a textbook example of global geology. We are lucky, or cursed, to have so much active geology right in our backyard. When visiting Bodega Head or the Point Reyes Peninsula (or looking at a map of these areas), students can learn that most of California resides on the No ...
How does the Earth`s crust move?
... How does the Earth’s crust move? Volcanoes, earthquakes, and mountains, oh my. . . • The locations of volcanoes, earthquakes, and mountains were identified on maps. • Scientists noticed a pattern. • These locations show us where the edges of the plates can be found. • These edges are called Plate B ...
... How does the Earth’s crust move? Volcanoes, earthquakes, and mountains, oh my. . . • The locations of volcanoes, earthquakes, and mountains were identified on maps. • Scientists noticed a pattern. • These locations show us where the edges of the plates can be found. • These edges are called Plate B ...
Cause of Earthquakes
... When the elastic strain built up along the fault exceeds the elastic limit, the rock will break or slip at its weakest point which we call the the focus. This slippage along the fault allows the rock to “snap back” and the vibrations sends out waves of energy in all directions called seismic wav ...
... When the elastic strain built up along the fault exceeds the elastic limit, the rock will break or slip at its weakest point which we call the the focus. This slippage along the fault allows the rock to “snap back” and the vibrations sends out waves of energy in all directions called seismic wav ...
C:\Documents and Settings\Alan Smithee\My Documents\MOTM
... provide the heulandite-Ca molecule with electrical stability. The “ ~24H2O” in heulandite-Ca’s chemical formula shows that it is a hydrous (or hydrated) mineral with as many as 24 molecules of water (H2O) attached to each parent molecule (the symbol “ ” indicates attachment and “~” indicates “as man ...
... provide the heulandite-Ca molecule with electrical stability. The “ ~24H2O” in heulandite-Ca’s chemical formula shows that it is a hydrous (or hydrated) mineral with as many as 24 molecules of water (H2O) attached to each parent molecule (the symbol “ ” indicates attachment and “~” indicates “as man ...
Plate Tectonics - Scoil Mhuire Geography
... rocks such as limstone that formed beneath the sea. When two continental plates collide subduction does not occur . Colliding continental plates tend to move upwards or sideways, this can sometimes cause devasting earthquakes e.g Pakistan 2005. ...
... rocks such as limstone that formed beneath the sea. When two continental plates collide subduction does not occur . Colliding continental plates tend to move upwards or sideways, this can sometimes cause devasting earthquakes e.g Pakistan 2005. ...
Plate tect - jenniferwells-lewis
... a divergent plate boundary where continental rifting occurs Figure 2-19 ...
... a divergent plate boundary where continental rifting occurs Figure 2-19 ...