Monday was
the day of our first obstacle. At 9am we arrived at San Onofre State Beach,
where we expected to examine the rock units exposed around the Christianitos
Fault to see if there were any potential hazards that would affect the San
Onofre Nuclear Generating Station just down the road. Everyone wandered down to
the beach, when disaster struck! The sand had been eroded further than before,
meaning that the tide was around 1m higher than expected. We all ran around to
a path further down the beach to see if we could find another way through,
getting a bit damp in the process! There was a track that went through the
vegetation and we found our way to a small clearing, where there was a wall that
we climbed to get back to the mini buses.
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A bit damp! |
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Our climbing wall! |
We attempted
to find another way around, but at 10:45am we gave up and went back to San
Clemente Beach Cliffs to look at the rock units there. We examined the Channel
Axis Facies (a facies is a body of rock with certain characteristics that forms under certain sedimentary conditions), and the Channel Margin Facies, which are both turbidites deposited
in turbidity currents which are currents of rapidly moving, sediment laden
water which moves down a slope through another body of water.
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Channel Axis Facies |
At 4pm we
arrived at Lamont Odett Viewpoint, near Palmdale, which is on the edge of the
Pacific Plate. We then moved just down the road to the Anaverde Cut on Highway
14, which is on the edge of the North American Plate (other side of the San
Andreas Fault) to discuss deformation in an outcrop that we could see as it had
been cut for the road. The rock units had been highly folded and faulted due to
movement on the San Andreas Fault, which is a dextral strike slip fault (that
basically means that if you stand on one side of the fault, over a long time
you would see the other side of the fault move to the right). At 5:50pm we left there
and headed to Palmdale Motel where we stayed for the night.
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Folded rocks on Anaverde Cut |
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