Step 1: Understanding the Concept:
Mineral weatherability refers to the ease with which a mineral undergoes physical and chemical breakdown under environmental conditions.
The Goldich Weathering Series ranks common rock-forming minerals based on their stability and rate of weathering.
Step 3: Detailed Explanation:
Let us analyze Goldich's stability series for minerals:
- Minerals that crystallize at high temperatures (like olivine and pyroxenes) are chemically unstable at surface conditions and weather rapidly.
- Minerals that crystallize at lower temperatures (like muscovite and quartz) are highly stable and weather very slowly.
- The order of increasing stability (decreasing weatherability) of common minerals is:
\[ \text{Olivine} < \text{Augite (Pyroxene)} < \text{Hornblende (Amphibole)} < \text{Biotite} < \text{K-Feldspar} < \text{Muscovite} < \text{Quartz} \]
- Let us analyze Sequence (A) in terms of weatherability (ease of breakdown):
Biotite has higher weatherability than highly stable minerals like Garnet and Quartz.
Augite (pyroxene) is highly unstable and has a higher weatherability than Biotite.
Garnet is a highly resistant metamorphic mineral, and Quartz is the most resistant mineral in the series.
Thus, the descending order of weatherability (from most weatherable to most stable/least weatherable) is correctly represented in Sequence (A) as:
\[ \text{Biotite} > \text{Augite} > \text{Garnet} > \text{Quartz} \]
- Let us evaluate why other options are incorrect:
- Sequence (B): Places highly stable minerals like Zircon and Tourmaline as the most weatherable, which is incorrect because they are extremely resistant to weathering.
- Sequence (C): Places Albite (feldspar) as more weatherable than Olivine, which is incorrect because Olivine is much more unstable and weathers faster than feldspars.
Therefore, only sequence (A) is correct.
Step 4: Final Answer:
The correct descending order of weatherability is represented only by sequence (A).