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:
Proterozoic dike with biiiiiiiiiiiiiiiiig feldspars (and flow structures, in this case). Want to see the other side of this sample? Try this: gigapan.com/gigapans/187738
Reddish quartz in this Neoproterozoic metasedimentary rock.
Sample measures 12.5 cm wide by 7 cm tall.
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