Fig. 6.7. Rare preservation of a cutbank in multistory
sandstone sheets fo rmed by flash-flood sedimentation in
an arid environment. The channel fill consists mainly of
lithofacies Sh with numerous low-angle internal thirdorder erosion surfaces. Kayenta Formation (Jurassic), Arizona
Fig. 6.8. Close-up of cutbank illustrated in Fig. 6.7. Note blocks of siltstone on the cutbank that have been eroded from
the siltstone bed at the upper left. Kayenta Formation (Jurassic), Arizona
sandstone sheets fo rmed by flash-flood sedimentation in
an arid environment. The channel fill consists mainly of
lithofacies Sh with numerous low-angle internal thirdorder erosion surfaces. Kayenta Formation (Jurassic), Arizona
Fig. 6.8. Close-up of cutbank illustrated in Fig. 6.7. Note blocks of siltstone on the cutbank that have been eroded from
the siltstone bed at the upper left. Kayenta Formation (Jurassic), Arizona
