Wednesday, February 19, 2014
We had a pretty benign January, but it seems like the last two weeks has just been one new storm every 24 hours. Fortunately, many hit hardest at night, leaving us some very pretty days in between the squalls. Early Sunday morning, I took advantage of a lull in the action to drive out to La Push. Saturday night's storm had subsided and the drive across 101 was beautiful with clear patches and a little sunshine and fresh snow low on the hills.
I was on Third Beach by 11:00. The skies were gray - but dry - and the tide was pretty high, but it was a great dose of the Olympic Coast, which is exactly what I'd come looking for.
Third Beach, like most of the beaches along this coast, is a glorified pocket beach. Its shape is largely defined by rocky headlands - that confine the beaches - and the interaction of Pacific Ocean waves with the complicated bathymetry and clusters of sea stacks - that shapes the beaches. Ultimately, this coastline is probably a reflection of the geology -- an assortment of resistant sedimentary blocks (the headlands and stacks) with much softer stuff in between (the bays and beaches).
There's a waterfall at the south end - basically a hanging valley where the ocean has cut landward faster than the small stream can cut downward. The waves had cut into a very high sandy berm near the stream mouth - providing some indication of how dynamic this beach must be. Many of bluffs along here are actively collapsing onto the beach. Some appear to be fairly slow-moving slides, but there was a big pile down the beach that looked like it must have come down both quickly and recently.
The tide was too high and the waves too big to explore safely and I look forward to coming back for longer in nice weather and when the tide is out. But it's days like this when stuff actually happens!
By the time I got to Second Beach, an hour or so later, the wind had picked up (the tide, too, there was little beach to be seen). And by the time I got into La Push, the next storm had fully arrived. I ate my sandwich in my car out at the jetty with the wipers on high and the car rocking in the wind. La Push is worthy of a whole post in itself - several, actually - but it will have to wait for a trip where I can get some better pictures.
I drove over to Rialto Beach, but between the storm, the water level, and all those big logs on the move, I decided against walking north to Hole in the Wall. Next time! It was a very wet drive back to Seattle.
Posted by Gravel Beach at Wednesday, February 19, 2014
I have this peculiar little hang up. If you're going to spend all day in a meeting or a workshop about beach stuff, and it's held within a stone's throw of the beach, you should actually go to the beach. Even if it's only for five or ten minutes early in the morning and there's a high tide and a bitterly cold north wind.
I like the Edmonds waterfront. I guess that's because despite its developed setting, there are still beaches and most of them are publicly accessible. It's a far cry from the large spit that once separated a big salt marsh from the Sound (map is from 1872) - the marsh that's left is a small remnant of the original and the barrier is segmented into a few artificially confined pocket beaches - but I wish we could figure out how to do this with some of our other small town waterfronts.
And here are a couple of earlier posts from April 2009, when it wasn't quite so cold as this Monday morning two weeks ago.
Monday, February 17, 2014
I was up in Oak Harbor again for Sound Waters (Saturday, Feb 1st), which meant that I had a few hours in the afternoon to work my way down the island. I spent much of that walking below the bluffs south of Swan Lake, turning around when I got a little south of Fort Nugent Road (which is how about how far I got walking north from Hastie Lake (February 2012) on a comparable Saturday afternoon two years ago).
This is a wonderful stretch of 200-250' bluffs, the bulk of which are sandy units that probably belong to the Whidbey formation (lower) and Vashon advance outwash (upper). As noted previously, wind erosion is significant along here and the homes along the top are built among the perched dunes where this windblown sand collects. The dunes are largely obliterated by the development, but the sand still collects on decks and driveways.
I wish I knew more of the story of these two concrete structures. The one on the beach must have come down fairly recently, although I haven't been down here in a long time so don't know for sure. On Google Earth (image dated 8-25-2011), it is already on the beach. There's another hanging on the edge a short distance north and destined to come down soon. From their proximity and general similarity, I assume they are a pair - are these observation posts of some sort associated with the island's military history?