Exposure of eolian sandstone and talus slope breccias in the McCoy Brook Formation (Jurassic) at Wasson's Bluff, Nova Scotia.  Clasts are derived from the underlying North Mountain Basalt.
<a href="//commons.wikimedia.org/wiki/User:Rygel,_M.C." title="User:Rygel, M.C.">Michael C. Rygel</a>
CC BY-SA 3.0
<span class="int-own-work" lang="en">Own work</span>