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Sea stacks, lots of big logs, a gravel beach, and a small spit across the mouth of Cedar Creek. And a wonderful forested slope rising up behind the beach. Apparently, Ruby Beach gets its name from the presence of red minerals in the sand and gravel. This was a quick stop, so I didn't spend much time looking at the details. There's so much other stuff to get distracted by here!
AERIAL VIEW
Dan posted from here recently and provides a bit more substance, both historic and geologic: Reading the Washington Landscape.
I guess I posted from Kalaloch in 2014 (same trip as Lake Quinault in the previous post), but that's not a good reason not to do it again. Especially when the day was so nice. This was a quick stop - time for a few photos - and then on to Ruby Beach, Port Angeles, and Seattle.
AERIAL VIEW
Like most of the streams along this coast, the creek bottoms out in a small estuary before running out to the ocean through a low place in the beach. And running out to sea is difficult when the waves are trying to flood back in. And the path is littered with huge logs.
There's a lot to make these Olympic coast beaches exciting, but the logs are what really stand out. So much wood. So much of it so big!
Aliso Beach, like Main Beach to the north, is a little longer and wider than most other beaches along this shoreline. It benefits from having formed in the vicinity of a stream mouth where the bluffs are set back farther and there's more sand to build the beach.
AERIAL VIEW
There was a significant scarp running the length of the upper beach. These cuts form when wave action lowers the beach profile - pulling the sand offshore. They are typically associated with big storms, but are often most pronounced when either nature, or humans, have created a particularly high back beach. I don't know much about the recent history here, but will assume this reflects natural processes -- although I suppose the beach could have been nourished. The lower beach also had large, distinct cusps, with a coarse gravelly lag in the hollows.
I guess there are plans to restore the estuary at the mouth of Aliso Creek. I suppose there aren't many places to do this along here - the topography, the lack of significant streams, and the dense development all conspire against the formation and maintenance of estuaries.
I often refer to this blog as my beach collection. Right now, you're in the Orange County Gallery. But you're almost at the end (but not quite). The next room, The Salton Sea Gallery, is small, but will be very different than this one and will leave you with some contrasting views of both geology and coastal development.
AERIAL VIEW
Wood's Cove is another of these wonderful little pocket-like beaches that seem to define Laguna Beach. At the bottom of Diamond Street, there is a short path and a tall flight of stairs to the rocks at the bottom. Small beaches extend in both directions, flanked by large homes perched on the edge of the bluff. And some perched beyond the edge of the bluff.
We're still working our way south through Orange County (quick time check - these are all from December 13th). Brooks Street is just one of many street-end beach accesses along this stretch of southern Laguna Beach. I wish I could have stopped at them all, but then I would have had a lot more trouble telling them apart afterwards.
AERIAL VIEW
This beach is just south of Main Beach. The base of the bluffs is anchored by a fairly continuous band of bedrock that encroaches well below the high tide line in some places. I guess this means that the homes may have a somewhat better prognosis than those built on rapidly retreating bluffs and big landslides, but I can't imagine it won't get increasingly exciting in coming decades when big storms arrive on higher tides and El Nino water levels.
For the most part, waves were pretty tame during this trip down the coast, but here they were a little larger and the surfers had definitely figured that out. Maybe they're always bigger here. Or maybe it was a fluke related to the swell direction and the offshore bathymetry.
All of these posts are from Laguna Beach, but this one is from Laguna's Main Beach, right in front of downtown. Unlike the smaller coves tucked into the convoluted coast to the north, this one is much more substantial and extends quite a ways to the south (the next post, from Brooks Street, is sort of part of the same beach.)
AERIAL VIEW
Downtown Laguna Beach, including Main Beach, are built at the mouth of Laguna Canyon, one of the larger drainages in the hills along this coast. That's why the town itself is down near sea level, instead of up on the terraces, and it's why there's room for a big, low-lying park and a wide beach, since there are no bluffs to bump up against. The coastline rises again to the south (towards the next post), although it's a little hard to distinguish the bluffs from the homes and condos built against them.
I'm not sure what the best name for this post is, but the pictures are taken from Heisler Park on Recreation Point in Laguna Beach. The beach to the northwest is Diver's Cove (below). The beach in the other direction may be Picnic Cove (above), though I'm not sure that's what it goes by locally.
AERIAL VIEW
The points along this coastline are defined by more resistant geologic units (here, I think they're volcanics), with the coves backed by bluffs of more erodible sediments. But both erode, even if it's at different rates. I wonder what this coastline will look like in 80 years?
The next several posts step southwards along Laguna Beach's coastline. There are an awful lot of fairly distinct beaches along this stretch, some more accessible than others, but I had only so much time and so much navigational talent. For each that I got to, there were several that I didn't: Victoria Beach, Treasure Island, Shaw's Cove, 1000 Steps. (More on Laguna Beach's Beaches)
AERIAL VIEW
Crescent Bay is a small pocket-like beach. I say pocket-like, because while it is bounded by rocky promontories, I suspect the nearshore sediment system is more continuous than the headlands might indicate. The big waves reach deep and the sand probably extends well offshore. The continuity of the littoral system may be determined as much by offshore bathymetry as it is by the outline of the terrestrial landscape.
As in much of southern California, the Pacific Coast Highway and a bulk of the development lie on a marine terrace (or terraces) - the legacy of a tectonically-active, uplifting coastline. But the development in Laguna Beach, much in the form of expensive homes, tends to extend right to the edge of the terrace and often drapes down over it, sometimes right to the water's edge.
Crystal Cove State Park is a long stretch of largely undeveloped bluffs and beach in the southern part of Newport Beach. The only buildings are down at Crystal Cove proper, where Los Trancos Creek empties out onto the beach.
AERIAL VIEW
The little beach enclave appears to have a long history - with some strong advocates. I haven't sorted out the whole story, but it looks like the Crystal Cove Conservancy is working with California State Parks to restore the old beach cottages on the bluff. The historical preservation part of me finds this wonderful, but the coastal geologist part of me wonders how much effort we should take to preserve structures in unsustainable locations.
But in the meantime, what a neat spot. Besides the places down at the beach, it can also be enjoyed from Ruby's Shake Shack up on the bluff along the road!
The San Diego River (not in San Diego) drains through the completely transformed Newport Bay estuary and out to the ocean in a channel defined on the western (Balboa) side by a long jetty and on the eastern (Corona Del Mar) side by a rocky promontory (and another jetty).
I believe this is all technically part of Newport Beach, although I'm still struggling with the geographic labels down here (most of what I know about the names of southern California beaches comes from Beach Boys songs and Google Maps).
AERIAL VIEW
There were lots of cool beach things to check out - the jetties, the small beach tucked into the rocks on this side, the beautiful beach cusps, and the classic California style hillside homes. These photos are taken from Lookout Point (west) and Inspiration Point (east), as well as down on the beach itself.
The western shore of Los Angeles, from Malibu south to the Palos Verdes Peninsula, consists of a long series of beaches - including Santa Monica, Venice, Dockweiler, Manhattan, Hermosa, and Redondo. I'm sure geography purists, surfers, and many Angelinos might choose to divide these up differently, but I think this captures the basic idea.
AERIAL VIEW
The Redondo Beach Pier is located at the northern end of the southernmost of these beaches, just south of the large marina complex that separates it from Hermosa Beach to the north.
The Redondo Pier is not just your typical single pier, but a strange triangle of intersecting piers, reflecting some history of multiple structures and numerous reconstructions (these things tend to attract both storms and fires).
I have nothing to add about the beach itself, other than wanting to point out that getting to it was neither encouraged nor easy. I guess you have to head south from the pier itself to do that.
This southern shore of the Palos Verdes Peninsula has a bit of a geological reputation - and not just because of its Tertiary sediments, Pleistocene marine terraces, and late Holocene cobble beaches. I first heard about Portuguese Bend in college in the context of large deep-seated landslides (and the ramifications for continuing to develop them long after the risk was recognized, as I recall). I guess the Portuguese Bend slide is perennially on the move. The impacted stretch of Palos Verdes Drive is a roller coaster with warning signs, unexpected dips, and patched asphalt. The waterlines are on the surface, which I suppose makes them easier to inspect and repair.
AERIAL VIEW
Abalone Cove is in the western portion of this messy geology. Part of it was active in the 1980s, although I guess that involved only a small area of a much larger landslide complex that extends far into the local hills. Interestingly, Wayfarer's Chapel, just up the hill from here, must be on more stable ground, as it's been there since at the early 1950s and remains intact.
The central portion of the Abalone Cove beach is armored with old concrete rubble, the lower parts of which were rounding into conglomeratic cobbles. But there were also much more appealing natural cobble beaches in both directions. By the way, that what makes these beaches more appealing isn't just that the cobbles lack rebar, but that there is still an upper beach, whereas on the armored section (as on armored beaches pretty much everywhere), the back beach is pretty much buried under the armor itself.
The bluff that rises behind the beach shows both the topography and the twisted stratigraphy typical of big landslides.
