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There are lots of things I haven't seen and done in my life, but I can imagine what it is going to be like to see a rhyolitic volcano erupting at close quarters, or to feel a magnitude 8 quake (6.9 is my biggest so far). But sometimes things happen that just leave me breathless, if only from the unexpectedness of it all. That's what happened to me today.
I had always heard about the Antelope Valley California Poppy State Reserve, but had never seen it, especially in the late winter or early spring when the blooms are at their peak. We were taking an alternate route home, generally following the San Andreas fault from Cajon Pass to Grapevine Summit on Interstate 5. The desert was mostly dry and barren for much of the route, but as we passed Palmdale and Lancaster, I looked west and saw something I had never seen before: orange hills. Fluorescent orange hills. As we drew closer, it was clear that the California Poppies were at their golden best.
After expending several hours using vast amounts of digital space on my camera, I started to ponder why the flowers were here, and not elsewhere across the Mojave Desert, at least not in such dominating numbers. I first considered the slightly higher elevation, the local rocks and sediment, soil conditions and drainage, but I started to realize there was another dynamic going on...the flowers are a natural phenomena, but a natural phenomena with a very human influence. About seven miles west of the Poppy preserve there is another state park: Arthur B. Ripley Desert Woodland State Park. The park preserves 580 acres of what turns out to be the native land cover of the Mojave Desert west of Lancaster and Palmdale: juniper woodland and Joshua Trees.
A century ago, this high end of the desert was cleared of Joshua Trees and Juniper, usually by chaining (dragging a huge chain between tractors that knocked down whole forests) or fires in order to put in thousands of acres of alfalfa fields and other crops. Large areas were reserved for sheep and cattle grazing as well. The natural plant cover was long gone. Much later, some of the abandoned fields started to recover, and the showy wildflowers represent some of the pioneer species (I've noticed for years that the best wildflower shows in any forested areas occur after fires: Yellowstone, Yosemite, and many other areas). Without any nearby natural vegetation, there is no way for the native Joshua Trees and other large trees and shrubs to recolonize the valley floor; they don't have any method to spread their seeds widely (Joshua Trees were once spread in giant ground sloth poop...). Despite their incredible beauty, the wildflower displays are a monument to our extensive alteration of the environment that once existed here.
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For those who are new to Geotripper, the "Other California" is my long-running web series on the fascinating geological places in my fine state that don't usually show up on the postcards (although I've been known to break my own rules every so often; California's poppies are on postcards all the time).
3 comments:
Beautiful!
Hey there! I'm headed out to Lancaster this weekend. I've been looking to see the southern half of the Neenach volcano since I was in middle school in 2010. Do you remember the exact location of the outcropping in the picture? I can't seem to find it on Google street view
Wikipedia has this to say: "The remnants of the eastern portion of the volcano, called the Neenach Formation, lie about 195 miles (314 kilometers) south of the western portion near Neenach, California. (34°44′58.30″N 118°35′51.62″WCoordinates: 34°44′58.30″N 118°35′51.62″W).[6] The formation covers about 10 square miles and is notable for the distinct and strongly linear boundary along its southerly side, where the San Andreas Fault split the original volcano. This entire southern boundary is accessible by Pine Canyon Road (Los Angeles County Route N2) between Sandberg and Three Points. Surface rock exposures in the formation appear to consist primarily of dacite and andesite flows, which have weathered into nondescript low hills with few outcrops, unlike the dramatic megaliths in the northern portion" I recall taking the picture from Lancaster Road, and I didn't have enough time to check the outcrops on Pine Canyon Road.
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