A weathering profile describes the vertical layers formed by the breakdown of rock and soil formation. Saprolite is a specific layer within this profile.
Saprolite is defined as rock that has been chemically weathered to the extent that it loses its original strength but retains its original fabric (texture and structure). It represents a stage of intense weathering but is still essentially in situ (in its original place) rock.
A typical weathering profile, from top to bottom, generally consists of:
Therefore, saprolite is found overlying the unweathered rock.
Based on the typical structure of a weathering profile:
The correct positioning of saprolite is immediately above the unweathered rock.
During normal weathering of a granite rock (A), clay minerals and then residue of gibbsite are formed. Which one is the correct weathering path for the rock in the given diagram ($\text{Al}_2\text{O}_3$, $\text{CaO}$, $\text{Na}_2\text{O}$ and $\text{K}_2\text{O}$ are in moles).
