<span>a) molecular, phosphorous pentafluoride
b) ionic, sodium iodide
c) molecular, sulfur dichloride
d) ionic, calcium nitrate
e) ionic, iron(III) chloride
f) ionic?, lanthanum phosphate
g) ionic, cobalt(II) carbonate
h) molecular, dinitrogen tetraoxide
hope this helps!</span><span>
</span>
Answer:
THERE IS NOTHING MENTION HERE HOW CAN ANYONE KNOW ABOUT IT?]
Explanation:
2CH₃COOH(aq) + Zn(s) → Zn(CH₃COO)₂(aq) + H₂(g)
2CH₃COOH(aq) + BaO(s) → Ba(CH₃COO)₂(aq) + H₂O(l)
CH₃COOH(aq) + NaOH(aq) → CH₃COONa(aq) + H₂O(l)
The Olivine normally crystalizes first from the magma of the mafic minerals, It crystalizes at between 1200°C and 1300°C. when the temperature of magma drops and there is a silica still remains in the magma so the olivine reacts with this silica to form pyroxene.and by more cooling of the temperature of magma and there is a silica still remains in magma pyroxene change to amphibole, and amphibole to biotite.when the pyroxene strat to form the plagioclase feldspar also forms.