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The cliffs of Cape Blanco are visible in the distance, about 6 miles away, from the north side of The Heads. This is an impressive land mass over 200 feet high. The Cape is considered a Pleistocene terrace that overlies tertiary sandstone and conglomerate. The place where the cliff color changes from light to dark marks a fault line of the Cascadia Subduction Zone. So the neck of the cape has older beds of Eocene rock (58 - 34 million years old) with thin-bedded mudstone and and graywacke sandstone (sandstone with imputities) strata. Notice the tall pinnacle along the shore to the right of the light-colored cliffs, which is over 100 feet tall! We’ll go there after a few more stops and photos. (dsc_5165ncs)

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4 comments

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  • You're doing a great job on the commentary, Randy. Lots of interesting information. Vicky

    said photo of vvvquilts vvvquilts 2007.05.23 at 23:20:21 PDT

  • Majestic. Sooo beautiful.

    said photo of 22338 22338 2007.05.23 at 12:32:41 PDT

  • It doesn't seem to be this high, that's quite a drop

    said photo of worldtripper3 worldtripper3 2007.05.23 at 12:08:48 PDT

  • That's the lighthouse in the center of the photo, right? I didn't realize it was so far back from the edge...

    said photo of habersham100 habersham100 2007.05.23 at 11:34:55 PDT

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