Pinnacles National Monument
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Welcome to Pinnacles National MonumentPinnacles National Monument is a wonderful place to visit. The Monument itself is over 23 million years old, and is part of an extinct volcano. Being located in the San Andreas Rift Zone, a series of faults lie just east of the park. It was created when the Pacific plate wrenched off a portion of the North American plate. It is known that volcanoes occur here because the earths crust is broken, allowing magma from beneath the earth to swell up. Pinnacles National Monument has slowly drifted northward 195 miles from Lancaster, California. The other half of the volcano is called the Neenach Formation which still resides near Lancaster. Once being the size of Mount Saint Helens, the centuries of rain has weathered the rock formation to approximately 1/3 of its original size creating what is known today as the Pinnacles National Monument. With its many spires, crags and variety of terrain, it is truly a spectacular place to visit. The Pinnacles are a great representation of four different kinds of plant communities. They are chaparral, riparian, xeric and foothill woodland communities and has been preserved for future generations to enjoy.
How to Get ThereThe Pinnacles are 115 miles from San Luis Obispo and can be reached in just over 2 hours. To reach the Pinnacles from San Luis Obispo, drive north on Highway 101 to King City, then exit onto G13, follow the signs to State route 25 then north 19 miles to the monument entrance. There is a $4 day use fee.The drive itself is quite beautiful once you reach Highway 25. In the spring months the grasses are green, covered with wildflowers, accentuating the oaks and Digger Pines in the area. Once at the park, check out the Visitor Center for the history of the park and how it was constructed and note the Seismic monitoring station as well. Exploring the PinnaclesIf this is your first visit to the park, I recommend starting with the Condor Gulch Trail which reaches the High Peaks Trail, then continue over to Bear Gulch, then return on the Bear Gulch or Moss Springs Trail.
Plant Communities of the PinnaclesThe Pinnacles consist of four different plant communities. They are xeric, riparian, chaparral and foothill woodland communities.The Xeric community is best described as the barerock community. It is found on exposed cliff faces and rocky outcroppings which possess little or no soil. Lichens, mosses, spike mosses and succulents such as Dudleyas and live-forevers. Water is very scarce, little soil accumulates and the temperatures are very extreme. All plants living in this community must be very hardy and adaptable. Any pockets of soil which you may find are considered to be island oases in the Xeric Community. The Riparian community is most notable in winter when the rains come and fill local streams. The water loving plants thrive. Cattails, ferns, blackberries, willows, cottonwoods and sycamores are some of the more common species. In summer, the water goes underground to the 1 1/2 to 2 foot level, which may lead you to believe this is not a riparian community. But as long as the root systems are in the water table, these plants will flourish. Most of the major drainage channels at Pinnacles have flowing underground streams year round. The Chaparral community is by far the most expansive community in the Pinnacles. It covers 80% of the park. It is one of the parks most important features. No other National Park area has such an extensive or truly representative stand of coast-range chaparral. Chaparral covers all but a small portion of the hillsides. It is the dense brushy cover of the hills. When you look closely, you can see a great difference between north and south facing slopes of the hills. About 90% of the vegetation on the south facing slopes is chamise, a dry needle leaved plant with brittle branches. Other plants occur, but only in small patches; mainly buckwheat and manzanita. The same three plants occur on the north facing slopes, but the amount of chemise decreases significantly and there is an abundance of holly-leaf cherry and toyon. The north facing slopes have a lush green color. These two communities are called the dry-phase and moist-phase chaparral. There are several reasons for the difference between the moist-phase and the dry-phase chaparral communities. The north slope receives less sunlight during the year and is cooler. The cooler temperatures allow more moisture to be retained over a longer period of time, more plant types become established, which causes more humus to develop in the soil which can then hold more water. The south slopes have more sunlight, allowing only the hardiest plant species to survive. Neither of the two types of chaparral grow in an easy environment. All plants of the moist or dry-phase of the chaparral must be capable of handling long periods of drought and hot temperatures. The chaparral provides habitat for an amazing number of animal species.
Camping Facilities
Additional InformationFor more information on the Pinnacles National Monument contact the agencies listed below.
Pinnacles National Monument (Home Page) Superintendent 5000 Highway 146 Paicines, CA 95043 (831)389-4485
P.O. Box 15755 San Luis Obispo, CA 93406 Telephone 1-805-543-8717. Sierra Club National Office 85 Second St., Second Floor San Francisco, CA 94105-3441, USA Telephone 1-415-977-5500 (voice), 1-415-977-5799 (FAX) |
Machesna Wilderness hike
April 2002 Photo by Gary Felsman |