OTAY MOUNTAIN
Sometimes the good stuff is hiding in plain sight......
For years I was told to check out Otay Mountain. I resisted. To me, it did not have that impressive stature that would normally lure me to a place. It looked plain and drab and I was clueless about its floristic bounty. I judged it from afar, sadly. Then one day, I decided to give it a try. I read that it had a "few" rare plants that I thought might be nice to see. So I went.
At the time, many years ago, I was by no means qualified to suss out rare plants. But rare plants or not, Otay Mountain won me over. The views alone were beautiful. And despite being able to suss out any rare plants, I was overjoyed to see so many wonderful and beautiful plants all growing together. There was so much to explore and see. And there was a certain excitement in knowing that so many impressive plants were all tucked within this place that rises from a sprawling suburb.
Otay Mountain is a landmark for rare plants and most famously known for being home to two of California's most rare plants - Hesperocyparis forbesii (Tecate Cypress) and Fremontodendron mexicanum (Mexican Flannelbush). Otay Mountain also has its own specie of Manzanita (Arctostaphylos otayensis) and Ceanothus (Ceanothus otayensis), both of which are also rare. Apparently, some 20 species of sensitive plants and animals call Otay Mountain home.
Some Geology
Otay Mountain is part of a larger chain of extinct volcanoes called the Santiago Peak volcanics that date back to the Early Cretaceous (145 - 100.5 Ma). These former volcanoes were the result of a magmatic arc that once ran along the subduction zone between the Farallon and North American Plates. As the Farallon Plate moved eastward and subducted beneath the North American Plate, it melted and molten magma rose to the earth's surface. A chain of volcanoes then formed. The volcanic activity ultimately ceased but the Farallon Plate continued to push them eastward. Eventually the peaks crashed into the North American Plate and were added on as "accreted terrane".
For a visual explanation, check out these videos:
Today, the Santiago Peaks volcanics run from northern Baja to southern Orange County. They run as a patchwork of peaks and ridges that lie several miles inland from the immediate coastline. And what we see today is only a twisted and contorted version of what once existed.
These peaks are more like small pieces of the underbelly to a former volcano. Through eons of time, these pieces have been uplifted, warped and worn back down into a distinct mixing of rock and soil. Fault line activity placed compressive forces on them and pushed them upward into the peaks and ridgelines we see today.
When it comes to rare plants, Otay Mountain has two critical ingredients: rare geology and unique geography.
Otay Mountain is a mixture of metavolcanic and sedimentary soils. Likewise, the geology of Otay Mountain is not widespread throughout southern California. It exists as a patchwork amidst a more widespread geologic setting, which sets the stage for unique developments. In short, plant speciation and evolution begin to play their hand. And we are left with some beautiful and amazing plants.
Some Plants (rare and not) of Otay Mountain
References
Herzig, Charles T., et al. "Santiago Peak volcanics: Early Cretaceous arc volcanism of the western Peninsular Ranges batholith, southern California." Peninsular Ranges Batholith, Baja California and Southern California: Geological Society of America Memoir 211 (2014): 345-363. https://doi.org/10.1130/2014.1211(09)