The Shinglemill Creek stream bed is gravel/pebble/sand and the presence of standing dead trees of mature age and layered organic and sand substrata in the lower reaches testify to numerous flood events and stream channel migrations over the years. The understory is predominately salmonberry and sword fern. The canopy is typical lowland forest of alder, maple, willow, hemlock, fir, and cedar. The steep canyon slopes are heavily forested.

4 replies
  1. natynaty
    natynaty says:

    You’ve been working hard lately. All that stress has got to be eating at you. Why not take a break and enjoy some cam girls? There’s plenty of them to enjoy at It’s wall to wall babes at this site. You’ll know that right away after your first visit.

Leave a Reply

Want to join the discussion?
Feel free to contribute!

Leave a Reply

Your email address will not be published.