(This post covers Sept. 11-13)
Let’s start today with Oregon Coast Geology 101. In the
photos of the Oregon coastline you undoubtedly notice the many odd-looking rock
islands (many of them stained white with bird shit) that rise up out of the
ocean not far from the shore. Many of them look like haystacks.
What causes that?
Remember the tectonic plates? The heavier Pacific (Juan de
Fuca) Plate is pushing under and uplifting the North American Plate. The
friction from this slow-motion collision creates magma which has resulted in
volcanoes which have created the Cascade Mountains 150 miles inland.
| Subduction in action? |
Here at the coast, where this plate “subduction” begins, magma
formed some 15 million years ago when sea levels were much higher. The magma
seeped through cracks in the ocean floor around this subduction zone, creating
mounds of basalt. As the sea receded the forces of the ocean ground away at the
softer sedimentary rock, but was less able to wear down the harder basalt “seeps”
that we now see along the coast today as offshore mounds and rocky headlands.
These islands provide outstanding places for shore birds to
nest and for seals and sea lions to haul out, molt, and make babies. They also
provide something interesting for us to look at when gazing at the Pacific
Ocean from the shores of Oregon and Washington.
| Drive-by photo. |
During the 100-mile move from Where-The-Sun-Never-Shines
(Sunset) Bay State Park to our new temporary home at
Where-The-Sun-Shines-Even-Less (Beverly) Beach State Park we “stopped” at two
more lighthouses (with the trailer in tow “stopping” is not always that easy,
so we did a drive-by of the Umpqua River Light and snapped the photo below).
We did actually stop and tour the Heceta Head Light which is
probably the best-preserved and most pristine of the Oregon lighthouses. It
just re-opened after extensive renovations and actually works the old-fashioned
way with a bulb inside a rotating Fresnel lens.
Because of its topography and relative isolation Oregon has
not been an easy place to build roads and one of the key factors in connecting those
roads have been bridges (Oregon has a lot of rivers, thus needs a lot of
bridges).
In a fortunate confluence many of those roads (and,
seemingly, all of the bridges) were built in the 1930s when a fellow by the
name of Conde McCullough was the chief bridge engineer for the Oregon DOT.
McCullough believed that bridges should not only be functional and structurally
sound but also aesthetically pleasing works of public art.
It’s probably not overstating the case to say that
McCullough is one of the most influential people in Oregon history.
The bridge in the first photo below was taken from the
Heceta Head Light and is the highest of the many bridges on the 101. The bridge
in the second photo is the 101 span over Spencer Creek and this photo is taken
from our campsite at Where-The-Sun-Shines-Even-Less (Beverly) Beach State Park.
On Thursday we drove north on the 101to Tillamook, stopping
at a place we’d been on a previous trip in 2007 and had ever since talked of returning.
Although it was just six years ago that trip seems like another
lifetime when we had deadlines and places we had to be. On the 2007 trip we flew
to Portland, rented a car and drove down the coast to San Francisco. On the
first day it was cold and rainy and we stopped for breakfast at a place called
The Grateful Bread; a warm, cozy little place in a laid-back little town that seemed
not to have change much since The Grateful Dead stopped touring. I told Betsy
then that I wanted to come back to this place and spend a winter writing a book.
Why? Because, well, it just seemed like a great place to write a book without a
lot of distractions in a place that encouraged indoor activity and had a great
place to eat breakfast.
The idea gained enough traction that it still comes up in
conversation every now and then.
However, there were at least two problems with this plan.
One, what to write about in the book? Two, remembering the name of the town?
I thought it was Pacifica, but when we tried to find it on
the map a few months ago we discovered there is no city by that name in Oregon.
There is however a Pacific City and that turned out to be the place we
remembered and it was, fortunately, almost exactly like we remembered.
We bought pastries, a fresh loaf of bread and a Grateful
Bread t-shirt and ate breakfast on the beach as I contemplated potential book
topics and those funny-looking rock mounds sticking out of the ocean.
From there it was on to Tillamook and its famous cheese
factory.
Now, you may be asking yourself; how did Tillamook get
itself so closely associated with cheese that the town’s motto is “cheese,
trees and ocean breeze”?
As Det. Adrian Monk would say; here’s what happened.
Tillamook is just over the coastal mountains from the
Willamette Valley and it did not take long for some of those early settlers to come
over and start cutting down trees and planting crops, expecting the coastal
plain to be as fertile as the Willamette Valley. However, because it seldom
gets very warm and is cloudy most of the time along this section of coast the
crops fared poorly. Grass, on the other hand, loved the cool, wet weather and
the dairy cows that the farmers had brought along with them to provide milk for
the family thrived. Soon, they had more dairy products than they needed for themselves
and started selling the excess. However, because milk and butter are difficult
to store and transport from such a remote location the farmers started turning
the excess milk into cheese that they could transport to Portland and other
places for sale.
Making cheese is a time-consuming, labor-intensive process
so the farmers formed small co-ops to process their milk into cheese. Those
same business dynamics led to further consolidation but the company is still owned today by the local dairy farms.
Fortunately, neither of us suffer from triskaidekaphobia
so on Friday (the 13th) we drove back up the 101 for a fantastic breakfast at the famous
Otis Café and then worked our way back down the coast stopping at viewpoints
and lighthouses before ending up on the bay front in Newport where we picked up
some fresh and delicious, but pricy, salmon fillets for supper.
We took a long walk on the beach at sunset, except that
there was (again) no sun visible to watch set. A more accurate description
would be to say that it got gradually darker as we walked along the beach.
| The family that surfs together gets eaten by sharks together. |
One of our viewpoint stops as we drove down the coast was
Cape Foulweather, so named by Capt. James Cook on a voyage in 1778. Cook, it
seems, was a lot more forthright with his naming conventions than the Oregon
Parks Department.
One of the more fascinating things that we saw on our
travels was a tsunami warning display made out of a section of concrete dock
that had broken loose when the tsunami hit Japan a few years ago and – 15
months later – washed up on the beach here in Newport.
Speaking of weird things, does anyone remember Marion Barry,
the former mayor of Washington D.C. that got busted for smoking crack and then
got in trouble for the same thing that Bill Clinton got in trouble for except
that instead of getting what Bill got in the White House Marion got his in the
visiting room at the prison where he was serving time for the aforementioned
crack smoking; and then, a few years later, after he got of prison, he was re-elected
to the D.C. city council and then as mayor?
The reason I ask is that Oregon State University has created
a new and improved strain of blackberry that for some unknown reason they have
chosen to call a marionberry. Thus, everywhere you go in Oregon they are
selling marionberry pies. Apparently they are quite tasty but, so far, I have
not been able to bring myself to try a slice of marionberry pie.
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