March 31, 2004

THE LURE OF THE SEA

I was called again, yesterday. Called to stand at the edge of the largest body of water on the planet—the Pacific Ocean. I even like saying the name—I’m in awe of it.

To get to the sea from where I live, you first must cross over the coastal range of mountains and through miles of old growth redwood forests. The western sides of the mountains settles slowly down to a flat sort of plain before the cliffs drop off abruptly into the Pacific. The view of the ocean always comes as a surprise. I haven’t traveled the road enough times to know exactly where I’m going to have the first glimpse. So it is always a unique moment with the sea always being unexpectedly beautiful.

Yesterday, it was rough, as it was the last time I was called to look. There were white caps on the top of every wave and when I drove over to the very edge of the cliffs I was surprised at how tall the waves were. Maybe because it was a sunny day, the big powerful waves seemed out of place—like they should’ve been part of a dark swirling storm.

But when went to get out of my truck, the wind was so strong I had to fight to push open the door. The wind was blowing from the northwest so I chose to let it push me to the south along a path running along the top of the cliff. Coming back, I was forced to turn my cap around, facing the brim around to the back so the wind wouldn’t blow it off my head.

It was very cold, with the wind coming off the water. But I felt it was necessary to walk along the shore for awhile—to breathe in the Pacific.

I was happy afterwards, to head back inland to the other side of the mountains where the air is warmer and the wind less strong. But sometimes I just have to go to where I went, to stand on the top of the cliffs and be in awe.

Posted by Tony at March 31, 2004 08:34 PM
Comments

Tony,

The 'flat sort of plain' is called a benchmark or ocean wavecut bench. From a combination of higer ocean level and rising land surface, the ocean level at one time was at the base of the Coast Range making the plain the erosional deposition onto the shallow nearshore ocean bottom. The San Andreas fault is not far offshore, and the shoreline cliffs continue a steep dropoff to very deep water. The present day benchmark (or beach) is the narrow strip between the cliffs and low tide level.

To knock of the wind, climb down to ocean level where the wind off the ocean has to rise up and go over the sea cliff faces. Surprising comfort zone with less wind and more warmth of sun rays. However, in your area the access places are few and can be treacherous climbs. Locals and surfers don't like to advertise them. And beware the surfers go to spots where the high tides can cut off access to get out.

Work on finding the closest and safest palces north and south where you could go and sit and meditate, shed your windbreaker cloaths, and enjoy the warmth of sun rays with crashing ocean wave sounds. If nothing else, generally the first community south has access and a couple of primo spots. Paying for access and sharing sometimes is worthwhile to knock off the harsh Pacific northwest winds...but don't post your location finds (if any) on the Internet. This is why the crowds end up in the Bodega Bay area. I use to stay in the State Park just north side of town there, and walk from the campsite into the marina area, very nice.

Posted by: LonghairSteve on April 1, 2004 04:37 PM

I have heard that we are drawn to the ocean because we are mostly water. And water wants to seek out the ocean.

I've heard the same reason as to why we are affected by the moon.

Posted by: Robert on April 2, 2004 09:39 AM
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