Since all of these Pennine Basin sandbodies were deposited in the same area, one after the other, it is easy to
suppose that they will all have the same catchment area and the same group of heavy minerals. They do not. An interesting pattern appears when data is collected about "heavy minerals" and cross-bedding direction from all of these sandstones. There appears to be three separate source areas supplying sands with different heavy minerals into the Pennine Basin. (See Fig. 4)
Early Westphalian sandbodies with cross-beds indicating they were deposited by rivers flowing from the north (but not the Woolley Edge Rock) and contain abundant zircon that indicate the catchment was in granites; they also contain garnets that suggest there were also metamorphic rocks. These are the rocks are exposed when fold mountain belts are deeply eroded.
Slightly younger sandbodies with cross-beds from the west have very few garnets, and a variable, but significant,
chrome spinel combinations of heavy minerals. This suggests catchments of well-weathered mature sediments
(whose heavy minerals have already been destroyed) and an occasional ophiolite exposure are being weathered to supply the sediment.
The youngest sandbodies, (shown as group 3 in green on Fig. 4) starting with the Woolley Edge Rock, have cross-beds suggesting they came mainly from the east. They have an abundant number of garnet fragments of a wide variety of composition, indicating a full range of metamorphic rocks as well as monazite, indicating granites and chrome spinel weathered from ophiolites.