answersLogoWhite

0

What is the answer to X-3y2?

Updated: 8/21/2019
User Avatar

Wiki User

6y ago

Best Answer

The question contains an expression: neither an equation nor an inequality. Expressions cannot have answers.

User Avatar

Wiki User

6y ago
This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: What is the answer to X-3y2?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What is the greatest common factor of 7xxxzzzz and 34xxxxxzz?

xxxzz x3y2


What are the elements that make garnet?

Permute and Jasperagus are is the chemical formula for Garnet.


If two integers a and b can be expressed as a x3y5 and bx3y2.xy are prime numbers then find LCM of ab?

Since x3y5 is a multiple of x3y2, it is automatically the LCM.


How do you find GCF with varaibles only?

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


How do you simplify x3y2 plus 7x2y3 plus 7xy-2 plus x2y3 plus 8x3y2-3xy-7?

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.


Describe how you find the GCF of 15x2y and 10x3y2?

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 the formula for a compound is represented by X3Y2 and the charge on the Y ion is -3 what is the charge in the X ion plus 1 plus 2 plus 3 plus 4?

-946515634175


What are the factors of 42x3y2?

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.


Is the mantle of the earth iron?

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.


Difference ruby and 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.


What the composition of the earth's mantle?

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.


What elements make up the lower mantle of the earth?

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.