with pebbles and cross-beds
Table Mountain Sandstone from Table Mountain. A quartz arenite with variable levels of hematite staining.
Slaty cleavage is variably developed in strata of the rhythmite portion of the Neoproterozoic Konnarock Formation.
Foliation in the Squaw Creek Schist is highlighted in yellow (projected in black), and the axial surface of the major obvious folds are shown in red.
Annotated copy of this image: www.gigapan.com/gigapans/187745
check the surrounding hillsides!
Proterozoic dike with big feldspars.
Obverse of the sample here:
Autopano Giga stitched version (for comparison)
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