Erin Bouffe 12 October 2018

The tassiks of the active mud vents in the central area

The legacy mud flow area on the western side of Erin Bouffe, there are no active vents or mud in the area.

The surface of this area is sandy and covered by many angular sandstone blocks of various sizes

close up of some of the well rounded clasts of chert, mudstone , sand and other lithics