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The charge of the X ion is plus 2.
Permute and Jasperagus are is the chemical formula for Garnet.
a ruby is a precious stone that is brilliant in colour and almost glows when you hold it to the light, a garnet is a semi-precious stone, it is red as well but dull it is mostly used for costume jewellery.
Earth has a core of solid and liquid iron, a mantle of ultramafic rock, a crust of complex mineral compounds, and an atmosphere of nitrogen, oxygen, and other gases. Physical and chemical reactions on the Earth include the compound water (dihydrogen oxide or oxidane) in all three of its physical phases. Carbon-cycle (living) organisms utilize and alter the surface of the planet.More detail is provided below:---CrustEarth's crust is separated into two main types, oceanic crust and continental crust. They have differing chemical and physical properties and also differ significantly in thickness. Oceanic CrustOceanic crust is typically enriched in the elements iron and magnesium and has less aluminum than the continental crust. It may broadly be described as having a basaltic composition. This means that it predominantly contains the minerals calcium feldspars (such as Anorthite), Pyroxene and Olivine.Basalt generally has the following composition:SiO2 - 45-52 %Al2O3 - 14 %FeO - 5-14 %MgO - 5-12 %CaO - 10%Alkalis - 2-5 %TiO2 - 0.5-2 %Continental CrustContinental crust is generally thicker and less dense than oceanic crust and tends to have a higher concentration of silica, aluminum and potassium, forming minerals such as quartz, potassium (or alkali) feldspars and muscovite mica.The contintal crust is composed of a wide variaty of rock types from heavily metamorphosed and very ancient (>3Ga) cratonic and basement rocks to very young recently deposited sediments or recently erupted extrusive igneous rocks.Continental crust tends to have the following average composition:SiO2 - 57-58 %Al2O3 - 16 %FeO - 6-9 %MgO - 4-5 %CaO - 6-7%Na2O - 3 %K2O - 1-2 %TiO2 - 0.7-0.8 %---MantleThe Earth's mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust. The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.At depths shallower than approximately 460 km, these minerals form the rocks types Peridotite, Dunite (Olivine-rich Peridotite), and Eclogite.At depths greater than 410 km Olivine becomes unstable and is replaced by a number of different mineral forms known as poly-morphs which are stable at higher pressures. These include Wadsleyite which forms at depths between 410 and 520 km and Ringwoodite which forms between 520 and 600 km deep.These depths are based on a number of seismic dicontinuities at the depths of 410 km (thought to mark the transition from Olivine to Wadsleyite) and at 520 km (thought to mark the transition from Wadsleyite to Ringwoodite) respectively.At depths greater than around 650 km these upper mantle minerals start to become unstable due to the increased pressure and the minerals below this take the structure of the minerals Perovskite and Ferropericlase although with differing chemical compositions and it is this seismic discontinuity at 650 km depth that marks the transition to the lower mantle.Average mantle composition:SiO2 - 45-48 %Al2O3 - 3-4 %FeO - 7-8 %MgO - 37-39 %CaO - 3 %Na2O - 0.3-0.5 %K2O - 0.03-0.12 %TiO2 - 0.1-0.2 %---Outer coreThe Earth's outer core is composed of molten iron and nickel. ---Inner CoreThe Earth's inner core is believed to be composed of a solid iron-nickel alloy.
The mantle can be subdivided into the upper and lower mantle.The uppermost part of the upper mantle is part of the lithosphere, and is sold and rigid. The lower part of the upper mantle is partially molten, and hence can flow.The lower mantle is solid, but behaves in a plastic fashion, much like blu-tack.The mantle is predominantly composed of an ultramafic rock called peridotite.Further Detail:The Earth's mantle is the largest layer of the Earth by volume accounting for around 84% of the Earth. It is approximately 2885 kilometers thick.The Earth's mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust.The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.At depths shallower than approximately 460 km, these minerals form the rocks types Peridotite, Dunite (Olivine-rich Peridotite), and Eclogite.At depths greater than 410 km Olivine becomes unstable and is replaced by a number of different mineral forms known as poly-morphs which are stable at higher pressures. These include Wadsleyite which forms at depths between 410 and 520 km and Ringwoodite which forms between 520 and 600 km deep.These depths are based on a number of seismic dicontinuities at the depths of 410 km (thought to mark the transition from Olivine to Wadsleyite) and at 520 km (thought to mark the transition from Wadsleyite to Ringwoodite) respectively.At depths greater than around 650 km these upper mantle minerals start to become unstable due to the increased pressure and the minerals below this take the structure of the minerals Perovskite and Ferropericlase although with differing chemical compositions and it is this seismic discontinuity at 650 km depth that marks the transition to the lower mantle.Its heat comes from left over radiation from the Earth's creation.It is more denser than the crust. notIt contains more iron than silica.It is 1800 miles thick and makes up more than two thirds of earts mass
Permute and Jasperagus are is the chemical formula for Garnet.
xxxzz x3y2
Since x3y5 is a multiple of x3y2, it is automatically the LCM.
You look at the exponents. x5y2 and x3y4 The greatest common factor of these is the largest exponent of each. So the greatest common factor is: x3y2
x3y2 + 7x2y3 + 7xy - 2 + x2y3 + 8x3y2 - 3xy - 7 =9x3y2 + 8x2y3 + 4xy - 9 =xy ( 9x2y + 8xy2 + 4) - 9 =xy ( xy(9x + 8y) + 4) - 9 .This is still messy, but it's simpler than the octonomial in the question,and we can't see any more that can be done with it.
I do the coefficients first. The GCF of 10 and 15 is 5. I tackle the variables next. The GCF of x2y and x3y2 is x2y I put it all together. The GCF of 15x2y and 10x3y2 is 5x2y.
If you mean prime factors they are:42x3y2 = 2*3*7*x3y2All of the factors of it are:1, 2, 3, 6, 7, 21, 42,and any of those numbers multiplied by either x, x2, x3, y, y2, xy, xy2, x2y, x2y2, x3y, or x3y2.
a ruby is a precious stone that is brilliant in colour and almost glows when you hold it to the light, a garnet is a semi-precious stone, it is red as well but dull it is mostly used for costume jewellery.
The earth's mantle is composed in part of minerals that contain iron:The Earth's mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust.The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.However the layers of the earth that are predominantly iron (approx 85 %) are the inner and outer core.
The Earth's mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust.The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.At depths shallower than approximately 460 km, these minerals form the rocks types Peridotite, Dunite (Olivine-rich Peridotite), and Eclogite.At depths greater than 410 km Olivine becomes unstable and is replaced by a number of different mineral forms known as poly-morphs which are stable at higher pressures. These include Wadsleyite which forms at depths between 410 and 520 km and Ringwoodite which forms between 520 and 600 km deep.These depths are based on a number of seismic discontinuities at the depths of 410 km (thought to mark the transition from Olivine to Wadsleyite) and at 520 km (thought to mark the transition from Wadsleyite to Ringwoodite) respectively.At depths greater than around 650 km these upper mantle minerals start to become unstable due to the increased pressure and the minerals below this take the structure of the minerals Perovskite and Ferropericlase although with differing chemical compositions and it is this seismic discontinuity at 650 km depth that marks the transition to the lower mantle. The material at these depths is often referred to as the "post-perovskite" phase which is the high-pressure form of magnesium silicate (MgSiO3).Please see the related links for more information.
The Earth's upper mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust.The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.In the upper mantle, these minerals form the rocks types Peridotite, Dunite (Olivine-rich Peridotite), and Eclogite.
The Earth's mantle is composed of rocks that have higher concentrations of mafic minerals (containing iron and magnesium) and lower in concentrations of the felsic minerals (aluminum and silica) than the rocks of Earth's crust.The concentrations of the above elements therefore mean that the Earth's mantle is composed of a series of minerals that are predominately calcium / iron / magnesium aluminum silicates.Such as:Olivine - (Mg,Fe)2SiO4Pyroxene - X(Si,Al)2O6, where X represents either calcium, sodium, iron or magnesiumSpinel - MgAl2O4Garnet - X3Y2(SiO4)3 where X and Y can be a mixture of aluminum, iron, calcium, manganese or magnesium.At depths shallower than approximately 460 km, these minerals form the rocks types Peridotite, Dunite (Olivine-rich Peridotite), and Eclogite.At depths greater than 410 km Olivine becomes unstable and is replaced by a number of different mineral forms known as poly-morphs which are stable at higher pressures. These include Wadsleyite which forms at depths between 410 and 520 km and Ringwoodite which forms between 520 and 600 km deep.These depths are based on a number of seismic discontinuities at the depths of 410 km (thought to mark the transition from Olivine to Wadsleyite) and at 520 km (thought to mark the transition from Wadsleyite to Ringwoodite) respectively.At depths greater than around 650 km these upper mantle minerals start to become unstable due to the increased pressure and the minerals below this take the structure of the minerals Perovskite and Ferropericlase although with differing chemical compositions and it is this seismic discontinuity at 650 km depth that marks the transition to the lower mantle. The material at these depths is often referred to as the "post-perovskite" phase which is the high-pressure form of magnesium silicate (MgSiO3).Please see the related links for more information.