On the Most Inaccessible Mountain Range on the Planet: Walking the Mid-Ocean Ridge in the Marin Headlands

What is the most inaccessible mountain range on planet Earth? The Himalaya? The southern Andes? Some mountain range in the Antarctic wastes? Nah. The most inaccessible mountain range is so difficult to visit that only a handful of humans have ever even laid eyes on it. It lies at the bottom of the sea, and is called the Mid-ocean ridge. It dwarfs the other major mountain ranges around the planet, extending for around 45,000 miles, enough to nearly circle the planet twice.

The Mid-ocean Ridge is not a high mountain range, maybe 5,000-10,000 feet high, but it lies thousands of feet beneath sea level except in extraordinary places like Iceland. Iceland is part of the Mid-ocean Ridge, but probably also includes magmas rising from a hot spot, giving it the extra elevation to rise above the waves.

So mountaineering on the Mid-ocean Ridge is beyond most mortal folk, but you can explore the surface of the ridge in a few places around the world where oceanic crust has been scraped off the sea-floor and accreted to the edge of a continent. One such place is on the Marin Headlands just north of San Francisco (I noticed in the geoblogosphere that Chuck Bailey at W&M Blogs has recently described another such spot in the somewhat more exotic Wadi Jezzi in Oman - Check it out!).

Some of the most spectacular scenery along the most beautiful coastline in the world can be found on the Marin Headlands (this post is actually a continuation of a blog series I started before the Christmas holidays). When you cross the Golden Gate Bridge headed north, take the Alexander Avenue offramp and follow Conzelman Road onto the headlands. Immediately you are treated with a gorgeous view of the Golden Gate Bridge, but the real story is behind you in the roadcuts. There are ribbon cherts (a form of deep ocean sediment derived from myriads of one-celled creatures called diatoms) lying directly on ocean-floor basalt. Lay your hands on the contact between the two and you are touching the surface of what once was part of the greatest mountain range on planet Earth!

The Marin Headlands don't lack for inaccessibility themselves. The coastline through this region is exceptionally rugged, with steep cliffs that slope directly into the surf. San Francisco Bay lies hidden behind the peninsula, and the ruggedness of the region prevented its discovery for many years (nearby Monterey Bay was visited as early as 1542, but San Francisco Bay was not discovered until 1769).

The odd looking cement structures found around the Marin Headlands are kind of a jarring reminder that the history of this region is not that of long-protected wilderness sanctuary. When World War II was being fought, San Francisco Bay was one of the most important strategic strongholds for the entire Pacific Theater of operations. There was the harbor itself through which much of the fleet operated, factories and ammunition depots, and the inland agricultural areas. That and a huge civilian population. The hills above the Golden Gate were studded with huge cannons and guns that could wreak devastation on any enemy flotilla that tried to enter the harbor. Below is Battery Mendell, just north of the Point Bonita Lighthouse.

The Marin Headlands region is a stunningly beautiful place with a fascinating geological story. The area is protected as part of the Golden Gate National Recreation Area, which is a level of protection that is more or less equivalent to a national park. It is certainly a popular destination, but it's usually possible to find some quiet corners, especially if you are willing to hike a little. While in the area, don't pass up Muir Woods National Monument. It's one of the most-visited monuments in the country, but wandering through the Redwood forest, it's not hard to see why.

Here's a Totally Unfamiliar Sight: Some Call it the Golden Gate

We are continuing our exploration of the most beautiful coastline in the world, the shoreline that runs from Big Sur to Bodega Bay. Today we'll have a look at one of the best-kept secrets of the entire state of California.

One of these times, you might find yourself in the city of San Francisco. It's a beautiful city built on a number of hills on the San Francisco Peninsula with a gorgeous stretch of beach, and a complex mix of rocks and sand dunes. If you do visit the city, try and take the time to seek out one of the unknown wonders of the city. As early as 1917, talk began of building a bridge across the opening of San Francisco Bay to the Marin Headlands. Much to the surprise of many visitors to the city, the bridge was actually built in 1937, providing a quick shortcut to the Sonoma/Napa Valley region, another part of California that no one has heard much about.

Locals call the span the Golden Gate Bridge. They try and keep it a secret from the tourists, fearing that it might get crowded and clogged by traffic. But if tourists are persistent, they can navigate their way through the back streets and find the bridge. Be aware that there will be people at one end collecting money from gullible drivers, insisting that they are simply charging a "toll" to use the bridge.

The bridge as seen from Fort Baker on the north side.

Oh, heck, I don't know how long I can drag this joke out. The bridge is only one of the most famous spans in the world and one of the most iconic symbols of California. Still it is a wonder to see, and I can't resist stopping whenever it comes into view. The setting is spectacular with steep coastal cliffs, the beautiful skyline of the City by the Bay, and the dark forests of the Presidio. When built, it had the longest span of any suspension bridge in the world at 4,200 feet, and is still the second longest in the United States. It rises nearly 250 feet above the waters of the Golden Gate. The two suspension towers are 746 feet high. A small army of thirty eight painters works continuously to protect corrosion-prone surfaces. And then there is the fascinating geology...

The bridge from the Marin Headlands.

San Francisco Bay is one of only two natural harbors along the California coast, and for two centuries has been a critical transportation and trade corridor for the state. Rivers that drain 40% of the state of California flow into the bay. It originated only 8,000 years ago as the last major ice age ended and sea level rose to flood the lower Sacramento River Valley (There were no doubt previous incarnations of the bay during earlier interglacial periods). During the ice advances sea level would drop three hundred feet or more, and the Sacramento River would flow to a delta near the Farallon Islands more than twenty miles offshore. Despite the urbanization, the bay is one of the most important estuary-wetland environments on the entire west coast of North America.

Several important fault systems cut across the Bay Area, including the well-known San Andreas, but also the less familiar Hayward, San Gregorio, Calaveras and many others. The proximity of these faults to the bridge is cause for some concern to the engineers who desire that the bridge would survive a major seismic event (retrofits have recently been completed). Part of the problem is the that the southern abutment is situated in serpentinite, a notoriously unstable rock (the cliff just visible on the right of the picture above is Baker Beach, which is made up of numerous landslide blocks).

The Golden Gate as viewed from the summit of Mt. Diablo in the east bay region.

The geology is incredibly complicated. The hills are composed of exotic terranes in the Franciscan Complex, bits and pieces of continental and oceanic crust that were carried hundreds or thousands of miles from their point of origin and accreted to the western edge of North America along a vast subduction zone. The subduction zone changed to a transform plate boundary (lateral movement along the San Andreas fault) only in the last few tens of millions of years.

Source: National Park Service

The rugged cliffs of the Marin Headlands (seen in the picture below from Fort Point) will be the subject of a follow-up post soon, but in short they are made of a complex mix of ocean floor basalt and reddish chert, a quartz-rich sedimentary rock that formed originally on the sea floor as diatomite. The diatomite was composed of trillions of microscope shells of one-celled creatures called (you guessed it) diatoms. The rock forms a solid foundation for the northern bridge abutment.

As mentioned already, the foundation of the southern abutment is in serpentinite, a far less stable rock (seen below from Baker Beach). You can see the landslides on the right side of the picture. I probably had a chance of being arrested the day I took the picture. It was September 15, 2001, just a few days after the tragedy of the Twin Towers and Flight 93. We were on a field trip with the National Association of Geoscience Teachers that had almost been cancelled. Airlines were not yet flying, and security around iconic symbols around the country was very tight. I imagine that if we had wandered closer to the base of the bridge there would have been trouble, or at least some very pointed questions from the California Highway Patrol.