flow easier and like quicker is what my text books ahhh saying . (:
More iron and magnesium in magma can make it more dense and viscous. This can result in a thicker magma that is less likely to flow easily. It may also affect the melting temperature and can influence the type of volcanic eruptions that occur.
Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.Read more: Which_igneous_rock_out_of_granite_basalt_andesite_and_peridotite_has_the_lowest_silica_SiO2_content
Magnesium and iron are both more electromotive then zinc, so zinc can't displace them in a compound.
They form in essentially the same way, the only real difference being in composition. They form as magma slowly cools deep underground, allowing large crystals to form. Granite forms from magma that is rich in silica, sodium, and potassium. Diorite forms from magma that has somewhat less silica and more iron, calcium, and magnesium.
Andesitic magma is more viscous and generally has more gas trapped in it. It is this the expansion of this gas under reduced pressure that drives the explosive force of an eruption. More gas means a more violent explosion.
magnesium is an alkaline earth metal. silver, copper, lead, zinc, and iron are transition metals. alkaline earths are naturally more reactive then transition metals.
yes
No, as magnesium is more reactive, and would 'keep' the nitrate.
Gabbro forms from a magma that is rich in iron and magnesium, and poor in silica (quartz). The magma cools and crystallizes deep below the earth's surface. Gabbro is from the same kind of magma as basalt and diabase, but because it cools more slowly, it develops larger crystals.
Sodium is more reactive than either magnesium or iron.
In a short answer No. But I can't really explain why.
Peridotite, a type of ultramafic rock composed largely of the mineral olivine, has the least silica.Read more: Which_igneous_rock_out_of_granite_basalt_andesite_and_peridotite_has_the_lowest_silica_SiO2_content
Fe + MgSO4 --> FeSO4 + Mg Fe(iron)is more reactive than mg( magnesium) ........ therefore iron will displace magnesium....... hence it is a displacement reaction.............
The silica-rich magma, also called felsic magma, is more viscous than iron-rich or mafic magma. This means resists flow more (just as syrup is more viscous than water). The high viscosity means that the felsic magma can trap more gasses, leading to explosive eruptions, rather than effusive ones.
Magnesium and iron are both more electromotive then zinc, so zinc can't displace them in a compound.
Magnesium(s) + Iron(s) + HCl(aq) -> MagnesiumChloride(aq) + Hydrogen(g) + Iron(s)Iron will not react with hydrochloric acid as magnesium is more reactive than iron , so magnesium will react with hydrochloric acid to give salt and hydrogen gas while iron is deposited.METAL + ACID -> METAL SALT + HYDROGEN GAS
They form in essentially the same way, the only real difference being in composition. They form as magma slowly cools deep underground, allowing large crystals to form. Granite forms from magma that is rich in silica, sodium, and potassium. Diorite forms from magma that has somewhat less silica and more iron, calcium, and magnesium.
Iron is several times more active than silver.