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12.09.2013
Turn Left at the T intersection (CNB bank), follow the paved road virtually to the west end, but a sandy path takes you to the beach which you will follow all the way past the air strip. Follow Peter’s Road up the high cliff and just after the high parking lot Turn Left onto a marked, grassy footpath. Run west along the spine of the island, (Major Donald Drive) several miles to attain the Bight Road which is a traditional footpath. Turn Left (south) onto the Bight Road into the Parrot Reserve, and Left Again almost immediately onto the Nature Trail which is a grassy, rocky loop. Run north along the grassy and rocky Bight Road (a traditional trail) across the paved road, along the boardwalk and beyond.
Follow Hemmington Road to the wooden steps which carry you down to the main north road; then Turn Left (west).
At the Rubis Station Turn Left up the wooden steps, and follow Saltwater Pond Trail all the way south. At the T intersection Turn Right (west) onto the main road on the south side of the island. Run west without deviating, right back to the finish line, which was your starting line quite some time ago.
Map of California showing the SAF, Natural Landmark plaque and the Field Guide to the San Andreas Fault.
Faults can be classified according to which of the three directions of space the rocks on either side move.
If the motion is mostly horizontal and parallel to the fault plane, the fault is called a strike slip (or transform) fault.
The San Andreas Fault is a place where two tectonic plates touch, the North American and Pacific Plates. There are many major faults in California that are parallel to the SAF, like the Hayward Fault.


People often think of the SAF as a line in the ground, and that by hopping across it, they can go from one plate to the other. California is famous for its earthquakes on the SAF (1906 San Francisco Earthquake, 1857 Fort Tejon earthquake), but the state's quakes are not particularly large. Instruction #1 is to run the “airport beach loop” in counter-clockwise fashion, using the West End Crossover Road and back along the airport beach (no trespassing on the airstrip) to run through the start line again and on to the following instructions. When you reach a path called Hemmington Road (a rocky, traditional trail) Turn Right (north). It’s very rough but you will come to a boardwalk further on, then a smooth section, then a few steps down to pavement. They served to lead inhabitants up onto their agricultural grounds on top of the bluff plateau, and across and down to the former coconut groves and rocky beaches. Its notoriety comes partly from the disastrous 1906 San Francisco earthquake, but rather more importantly because it passes through California, a highly-populated state that is frequently in the news. The plates are rigid (or almost rigid) slabs of rock that comprise the crust and upper mantle of the Earth.
As the rest of the plates moves, the stuck parts deform like compressing a spring so they build up stress in the rocks along the fault. The largest earthquakes in the world occur near subduction zones, where one plate is sliding under the other (Alaska, Chile, Indonesia, etc.) Only in northwestern California north of Cape Mendocino is there a subduction zone, the Cascadia megathrust, and it is not directly related to the SAF. It 'began' when the East Pacific Rise, the boundary between the Farallon and Pacific Plates, subducted under the North American Plate near what is now Los Angeles.
With similar arithmetic, we can see that 25 million years ago, California shared not the faintest resemblance with the modern paradise we know today. Often called “Windward” the south side shore also provided valuable items that floated in from other islands, like bamboo, glass bottles and any useful items that might have been tossed from ships. This type of karst tends to erode “rough” but can be smoothed by knocking the sharp points into the hollows.


And with many research institutions dedicated to studying such an accessible fault, the SAF has become a household name.
This means that if two people face each other across the fault and it moves, each person will see the other person move to the right. The SAF is about 700 miles long as the crow flies and about 800 miles long when its curves are measured.
Although the most recent break in the ground that defines the trace of the SAF is a narrow line, the actual plate boundary should be viewed as a fault zone.
Meanwhile, the Farrallon plate continues to scrape along the bottom of the North American plate, probably destined to sink into the mantle, melt and be recycled. If the rocks move horizontally apart or together, they are called divergent or convergent, respectively.
It is roughly ten miles deep, and reaches from the Salton Sea in Imperial county to Cape Mendocino in Humboldt county. The width of a fault zone can be less than a mile wide (Olema Trough) or many miles across (Salton Trough). Given enough time, the Cascadia megathrust will produce an earthquake much larger than any quake on the SAF. When divergent, they usually open valleys on land and oceanic ridges like the Mid Atlantic Ridge. That is why we can have an earthquake on the SAF in northern California but not on the SAF in southern California.



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