|Size & Location||450-acres, Penngrove, Sonoma County|
|Directions||Written Directions to Osborn / Google Maps to Osborn (Reservation Required)|
|Data & Images||Data|
|Interactive Map||Osborn Arc GIS|
|Current Weather||National Weather Service - Osborn Preserve|
Take a Virtual Tour
The 450-acre Fairfield Osborn Preserve lies on the northwest flank of Sonoma Mountain in Sonoma County, California. The preserve ranges in elevation from 1350 to 2300 ft and is characterized by active slumps and landslides and basalt exposures. Copeland Creek, a perennial drainage at upper elevations, drains into the Laguna de Santa Rosa in the Russian River watershed. Eight plant communities include upland, riparian and freshwater marsh habitats. The preserve is located in Penngrove and is a 15 minute drive from the SSU campus.
Preserve climate is typical of Mediterranean regions, with cool wet winters and hot dry summers. The majority of rainfall comes from atmospheric rivers that transport moist air to the Sonoma Coast from the tropics. Proximity to the Pacific Ocean moderates seasonal extremes: snow is rare and summer temperatures rarely exceed 100F. In the summer, fog frequently moves inland along valley bottoms, leaving the upper slopes of the mountain exposed.
Geology & Soils
Preserve soils are predominantly Goulding clay loam with extensive areas of basalt exposures. Typical soil depths are 16 to 20 inches and often occur on slopes of 15 to 45 percent. Widespread rhyolite creates highly erosive geology that occurs as slumps and landslides throughout the preserve. On the higher drier slopes, terraces of Raynor clay are associated with seeps and higher moisture retention at Turtle Pond and Cattail Marsh. The Rodgers Creek fault is about 2 miles west of the preserve and numerous side branches intercept the preserve.
Preserve lands span the Copeland Creek, Mark West and Petaluma watersheds. Both Copeland and Mark West drainages discharge into the Laguna de Santa Rosa, a 14-mile long wetland complex listed as a wetland of international importance by the Ramsar convention. The Preserve protects roughly one mile of a perennial section of upper Copeland Creek and seasonal drainages. Seasonal and perennial ponds and marshes are created by clay soils and springs. The freshwater marsh may have been formed by massive land movement along the Rodgers Creek Fault. Two perennial ponds on the property are manmade.
Principal plant communities within the Preserve are the oak woodland, chaparral, freshwater marsh, native and non-native grasslands, douglas-fir woodland, and riparian woodland.
Oak woodlands are dominated by coast live oak, California black oak, and California bay laurel and the understory includes toyon, coffeeberry, and poison oak. Grasslands in some areas still contain a rich array of native grasses and forbs. Perennial riparian zones of Copeland Creek have a high percentage of California bay laurel and also include big leaf maple, hazelnut, and alder. The deeply shaded understory contains snowberry and the uncommon California ginseng.
Animal diversity on the preserve is high due to the availability of year-round water. Perennial sections of Copeland Creek support yellow-legged frogs (Rana boylii) and pacific giant salamanders (Dicamptodon ensatus). Natural and man-made ponds are critical habitat for the federally-listed red-legged frogs (Rana draytoni), and additionally support breeding newts (Taricha granulosa and T. torosa), western pond turtles (Emys marmorata), and - on occasion- river otters. Non-native bullfrogs (Rana catesbeiana) occur in some ponds and are a threat to native species. The freshwater marsh is important habitat for sora and Virginia rails and other birds. A spring supports one of the few occurrences of the endangered pacific freshwater shrimp (Syncharis pacifica).
Top predators are still present and include mountain lion (Puma concolor), golden eagle (Aquila chrysaetos), coyote (Canis latrans), bobcat (Lynx rufus) and gray fox (Urocyon cinereoargenteus).
Archeological surface surveys indicate that the site was used as a seasonal hunting and gathering ground by Pomo, Miwok, or Wappo people, who traveled extensively to forage and barter. The earliest historical records from the 1860s show the property was part of a Spanish Land Grant. Lands were later homesteaded by families harvesting firewood, which was taken by wagonload down the mountain to Petaluma. By the 1890s the land was a working sheep and cattle ranch owned by the Duerson family.
In the 1950s, the land was purchased by Joan and William Matson Roth as a summer retreat for their family. In 1972, Joan and Bill transferred 200 acres to The Nature Conservancy to be used as an educational site in honor of Joan's father, Fairfield Osborn (1887-1969). Fairfield Osborn is known for his 1948 publication, "Our Plundered Planet," a prescient and devastating critique of human stewardship of earth's natural resources that was translated in 13 languages and read by millions worldwide. Despite his grave words, Fairfield Osborn was a man with an irreverent sense of humor. He won many supporters and was a natural leader, serving as President of the New York Zoological Society and working to establish The Conservation Foundation in 1948.
In 1997, The Nature Conservancy donated the Preserve to Sonoma State University, maintaining a conservation easement over the property for educational, research, and conservation. In 2004, the Preserve doubled in size with an additional 210-acre donation from Joan and William Roth managed under a conservation easement with the Sonoma County Agricultural Preservation and Open Space District. A final 40-acre donation was made in 2013.
"Nature may be a thing of beauty and is indeed a symphony, but above and below and within its own immutable essences, its distances, its apparent quietness and changelessness, it is an active purposeful, coordinated machine. Each part is dependent upon another, all are related to the movement of the whole. Parts of the earth, once living and productive, have died at the hand of man. Others are now dying. If we cause more to die, Nature will compensate for this in her own way, inexorably, as already she has begun to do."
- Fairfield Osborn, Jr., Our Plundered Planet, 1948
The Marjorie Osborn Education & Research Center (2,100 sq ft) has two meeting rooms for educational and research use, conferences and meetings. The larger room seats up to 24 people and includes a high-definition screen. The smaller room seats up to 15 people and has a small kitchenette that includes a small refrigerator and sink.
A wireless sensor network broadcasts data from weather stations and cameras to the internet and allows for virtual visits by classes and researchers. The trail system provides good, though sometimes rugged, access to most areas of the Preserve.
Research at the Osborn Preserve includes independent studies conducted by researchers and Preserve-coordinated efforts that target management needs. These studies have investigated diversity of phenomena including disease, invasive species, cultural surveys, and plant physiology. A detailed study of aquatic insects by Larry Serpa during the 1970s is a significant resource for researchers studying riparian communities. The Preserve may be best known for the intensive work on Sudden Oak Death conducted since the disease was first found in California in 1995.
The Preserve is open for research and educational programs, and public visitation is permitted by guided tour only. Management issues, such as invasive species control, erosion and sudden oak death, are representative of regional land management issues and create opportunities for collaborative efforts with researchers, students, agencies and organizations. As much as possible, management is results are shared with students, landowners, managers, and policymakers to highlight successful techniques that conserve natural processes.