Not quite sure what this question is asking, but quartz is not going to weather to an aluminum-rich anything, as quartz is composed of silica and oxygen. If a weathered something is rich in aluminum, it had to have come from a source of aluminum. So you can think of your possible aluminous sources. Feldspars, micas, etc.
Yes, the minerals that make upa rock partially determine how fast it weathers. But while there is some truth in this statement, the answer has to be false because the environment the rock surface is exposed to also determines how fast it weathers.
Following Goldich Dissolution Series (Or going backwards by Bowen's Reaction Series), olivine weathers before Quartz. Quartz has a framework silicate structure and olivine has a isolated silicate structure.
The abundance of quartz and shortage of feldspar in most soil can be attributed to the weathering process. Quartz is more resistant to weathering compared to feldspar, which makes it more prevalent in soil. Over time, feldspar weathers into clay minerals and other components, leading to its lower presence in soil compared to quartz.
Calcite weathers faster than quartz because it is more soluble in water. Calcite readily dissolves in acidic conditions, such as rainwater, leading to faster weathering compared to quartz, which is more resistant to chemical weathering due to its low solubility in water. Additionally, calcite has weaker chemical bonds that make it more susceptible to breakdown compared to quartz.
feldspars. feldspars.
Yes, the minerals that make upa rock partially determine how fast it weathers. But while there is some truth in this statement, the answer has to be false because the environment the rock surface is exposed to also determines how fast it weathers.
Sedimentary rock weathers the fastest and easiest
Quartz is a mineral. No other minerals contain quartz.
quartz, feldspar, and mica
Following Goldich Dissolution Series (Or going backwards by Bowen's Reaction Series), olivine weathers before Quartz. Quartz has a framework silicate structure and olivine has a isolated silicate structure.
The abundance of quartz and shortage of feldspar in most soil can be attributed to the weathering process. Quartz is more resistant to weathering compared to feldspar, which makes it more prevalent in soil. Over time, feldspar weathers into clay minerals and other components, leading to its lower presence in soil compared to quartz.
Carbonic acid can cause weathering and dissolution of quartz over time. This is because carbonic acid readily reacts with minerals like quartz, leading to the breakdown of the rock and the eventual release of silicon and oxygen ions.
Quartz.
Calcite weathers faster than quartz because it is more soluble in water. Calcite readily dissolves in acidic conditions, such as rainwater, leading to faster weathering compared to quartz, which is more resistant to chemical weathering due to its low solubility in water. Additionally, calcite has weaker chemical bonds that make it more susceptible to breakdown compared to quartz.
A TV contains quartz, wolframite, chromite, and quartz.
Many minerals are oxides such as quartz and hematite.
Beach sand eroded from headlands composed of diorite is likely to contain the minerals quartz and feldspar. Diorite primarily consists of plagioclase feldspar and hornblende, and as it weathers, these minerals break down and contribute to the sand composition. Quartz, being highly resistant to weathering, is also commonly found in beach sand due to its prevalence in various rock types.