Step 1: Understanding the Concept:
Evaluating mineral stability requires analyzing their chemical formulas, crystalline structures, and susceptibility to environmental weathering agents like water, oxygen, and carbonic acid.
Step 3: Detailed Explanation:
Let us analyze both statements individually:
- Statement (I) is correct: According to Goldich's Weathering Series, olivine is the least stable (most easily weathered) mineral among the primary rock-forming silicates.
It crystallizes at very high temperatures and pressures deep in the Earth's crust and is highly unstable under surface atmospheric conditions.
- Statement (II) is correct: Structurally, olivine is a nesosilicate with a chemical formula of $(\text{Mg, Fe})_2\text{SiO}_4$.
It consists of independent, individual silica tetrahedra ($SiO_4^{4-}$) that do not share oxygen atoms with each other.
These independent tetrahedra are held together in the crystal lattice purely by ionic bonds with divalent cations, namely hydrolyzable magnesium ($Mg^{2+}$) and easily oxidizable ferrous iron ($Fe^{2+}$).
Because these ionic linkages are highly vulnerable to chemical weathering processes (such as hydration, hydrolysis, and oxidation of $Fe^{2+}$ to $Fe^{3+}$), the crystal structure collapses rapidly when exposed to water and oxygen.
Therefore, both Statement (I) and Statement (II) are correct.
This corresponds to Option (A).
Step 4: Final Answer:
Both Statement (I) and Statement (II) are correct.