First you have to get there. From the public parking at the corner of Hemlock and Gower we walked the few short blocks to the beach by following Gower until it bent into Ecola Court’s ramp down to the sand. At first the sand lies in loose drifts and shifts beneath your feet, causing a sideways slide with each step, and then it’s packed sand that firmly supports your every step and the walking becomes easy.
It sometimes amazes me to see so many people on an Oregon beach. Often, in winter especially, these are fairly lonely places but for the ubiquitous person with their dog somewhere down the beach. Except, of course, for weekends when people from the valley come out for the day. Having weekends off is such a rare event in my household that I’m sure my impression of many of these places is markedly different from those whose only coastal experience is on weekends, which would differ again from those who only see them at the height of tourist season. I often crave the near solitude of a winter beach, but I also enjoy sharing the space with other appreciatives at any time. There are a few places that seem not to follow the feast or famine of visitors and Cannon Beach is one of these, there always seems to be a fair number of people enjoying the space. But it’s summer now—tourist season—and today the masses are definitely out in force.
There’s a pair of young girls, one pale, one dark—a striking contrast. They make their way through the low surf to a point—the process of their determination of when to stop invisible to my distant vantage—where they turn about, and holding hands they stop…and wait. Soon a larger wave rolls in to strike them across the lower back. They squeal gleefully, their voices merging with the cries of gulls, and their bodies shake with laughter. They call out to friends to join them. Unheeded, voices lost in the ocean’s white noise, they exit the water to rally their troupe. Soon a group wades out together. A child’s life is filled with possibility made out of the simplest of experiences.
Gangs of bikers roam the beach, racing across the sand. But it’s all amiable, without discord. You’ll pass people carrying these recumbent tricycles, called funcycles, going both to and from the beach, as they’re meant for use only on the sand. I’m surprised by the number of unused and unsupervised vehicles dotting the beach, especially since the rental cost runs about $10 for the first 90-minutes. Occasionally near perfect concentric circles, like oddly placed crop circles, mar the sand’s surface with no rim track leading in or out. We all may be sure we know how they got there, but no one will claim to actually having seen them under construction.
A mother maneuvers a black shark-shaped kite against a deep blue sky while one of her daughters buries the other up to the chin in dry sand. Both of the girls giggle throughout the whole process. When they are satisfied that the one is well and truly entombed they call for their mother to come critique their expertise. This necessitates landing that great fish, and so she reels it in until it lies flopping on the sand. Then they all laugh together and with one child’s face lowered and pressed to the other while both smile up at her—the perfect cherubs—she takes their picture. Did you get it mommy? A day they’ll obviously remember.
Guys in wet suits tote surfboards into the water, but the waves uncooperatively fail to mass sufficiently to facilitate a ride of any note. I suspect they knew this and just planned to hang out together, draped across their boards amid the swells. Better off, for those seeking motion and speed, are those in the surf with their boogie boards, sliding fifteen feet or more each time, and with the short turnaround they‘re almost immediately ready to go again.
Around by Whale Park, next to Ecola Creek there’s a volleyball net. It seems to be up most of the time, yet I’ve never seen it used. Perhaps that’s because this little corner where the beach curls back into town isn’t easily seen from the main portion of the beach.
And below Haystack Rock people cluster about the tide pools. The tide is in too far for the really interesting stuff to be exposed, and what is visible are mostly only barnacles, mussels, and a few small far colonizing anemone. Although if you bend low enough you can see tiny crabs scurrying away from you into the deeper shadows of rock-filled pools, while something washed up by the tide burrows back into the sand too quickly to be identified. Being the latter part of August it’s too late in the year to see Tufted Puffins nesting on the rock, they left several weeks back, but gulls and Murres dot its surface.
At the Cannon Beach Historical Society a claim is made that Haystack is the third largest single rock formation, behind the Sugarloaf, in Brazil, and Ayres Rock (it should be called Uluru since it was returned to the aboriginals and they returned to it its proper name), in Australia. Well the Haystack Rock farther south along the Oregon coast, at Pacific City, is taller than this one just for starters. And Burringurra, in western Australia, is actually larger than Uluru, both in height and footprint. And Beacon Rock, in the Columbia River Gorge is reputedly the world’s second largest, with only the Rock of Gibraltar larger than it. And in Mexico they claim Peña de Bernal is the third largest, while Swaziland claims Sibebe Rock as second largest. It’s very confusing.
There’s usually a modifier attached to clarify such matters. The largest limestone, granite, basalt, sedimentary, tertiary, or whatever, rock. These important defining components become detached by those who don’t understand their significance, think that others won’t, and, so, imprecision rules. This irks me. I never uncovered this problem when writing the Beacon Rock piece in my Columbia River Gorge journal, and so I contribute to the problem. This irks me more. I enquired of a State Geologist who merely suggested I use a less specific claim (an obvious one I’d already used in another entry), calling all other claims listed above dubious. I doubt the later. They’re undefined claims, imprecise, and therefore rendered misleading, but they’re not untruths. And what I needed was clarification and specificity—enquiring minds want to know—and to correct past errors. Good enough for government work, huh? So, essentially, I guess, you can believe whatever you want to, and why not…everyone else does.
Regardless, Haystack Rock is amazing. It stands 235ft tall and its generous footprint was once much larger. For a period of ten- to eleven-million years, beginning about 17-million-years-ago, a series of volcanic eruptions caused massive lava flows that spread along much of the coast before coming to a hissing stop in the sea. Of course it didn’t stop right away and parts of the coastline were thrust seaward with each upwelling, most obviously in the forms of headlands, by as much as 25-miles in some places. The sea immediately began its relentless grinding and chiseling, and beaches are slowly created. Ten-thousand-years-ago the Rock was still integrated. Then it becomes more singular, and more noticeable. Now it dominates the coastline here and can be seen from many miles away.