Fig. 3

Photo of the outcrop with some vegetation after a reasonably rainy winter. Note the thin-bedded alternations of siltstone and fine-grained sandstones, which weather differentially relative to one another. Bed-thickness is likely due to variations in clay content, which, in turn, is probably controlled by variations in sea-level and clastic input. The Undichna described here is from the thicker bed marked by the arrow, which runs obliquely down the slopes on both sides of the arrow