Fields Spring
United States, Washington
Fields Spring
About Fields Spring
Fields Spring State Park is a scenic 792-acre park located in southeastern Washington's Asotin County, near the borders with Oregon and Idaho. Situated in the Blue Mountains at elevations ranging from 3,000 to over 4,500 feet, the park offers spectacular views of three states and the dramatic Grande Ronde River canyon. Named after early homesteader Charles Fields, the park preserves diverse habitats ranging from open grasslands to coniferous forests. The park's high elevation and inland location create distinct seasonal characteristics, with wildflower-filled meadows in spring, comfortable temperatures in summer, and significant snow in winter. Highway 129 provides access from Clarkston, climbing dramatically through the Grande Ronde River canyon. The park features hiking trails, camping facilities, and the historic Puffer Butte lookout tower offering panoramic vistas. The area represents a transitional zone where Cascade forest influences meet the Columbia Basin shrub-steppe and Rocky Mountain ecosystems. Wildlife is abundant, including elk herds, deer, and various bird species. The park's remote location ensures a quiet, uncrowded experience even during peak seasons.
Wildlife Ecosystems
Fields Spring State Park supports diverse wildlife adapted to the Blue Mountains ecosystem. Rocky Mountain elk herds are present year-round, with populations sometimes exceeding 100 individuals utilizing the park's meadows and forests. Mule deer and white-tailed deer both occur, taking advantage of the varied habitats from grasslands to forests. Black bears inhabit the area, particularly in summer and fall when foraging for berries and preparing for hibernation. Mountain lions occasionally pass through, hunting deer and elk populations. The forests provide habitat for ruffed grouse and blue grouse, whose drumming and hooting calls echo through the woods. Various raptor species including red-tailed hawks, northern goshawks, and occasionally golden eagles hunt in the park's open areas. The meadows and grasslands support ground squirrels, whose colonies provide prey for predators. Wild turkeys, introduced to the region, have established populations and are frequently observed. Songbirds are diverse, with species including western tanagers, mountain bluebirds, and various warblers during breeding season. The high elevation and snowpack create seasonal migration patterns, with some species present only during warmer months. Coyotes are common, their howls sometimes heard at night across the canyons.
Flora Ecosystems
Fields Spring State Park features diverse plant communities reflecting the transition between several major ecoregions. Ponderosa pine dominates forested areas, mixed with Douglas fir at higher elevations and cooler exposures. Grand fir appears on north-facing slopes where moisture is more abundant. The understory includes snowberry, serviceberry, and ninebark, providing food for wildlife and seasonal interest. Open grasslands showcase Idaho fescue, bluebunch wheatgrass, and other native bunchgrasses that once dominated the inland Northwest. Spring wildflowers are spectacular, with arrowleaf balsamroot, lupine, Indian paintbrush, and numerous other species carpeting the meadows. Aspen groves appear in wetter draws and canyon areas, their golden fall foliage creating scenic displays. The park sits at the interface where Rocky Mountain flora meets Columbia Basin and Cascade species, creating unusual diversity. Invasive species including cheatgrass and knapweed have colonized some areas, altering fire regimes and competing with natives. Riparian areas feature willows, alders, and other moisture-loving species along drainages. The high elevation means growing seasons are short, with plants adapted to cold winters and limited frost-free periods.
Geology
Fields Spring State Park sits within the Columbia River Basalt Province, covered by ancient lava flows that erupted millions of years ago. These basalt flows, part of the larger Columbia River Basalt Group, originated from fissures in eastern Washington and Oregon during the Miocene epoch. The Grande Ronde River has carved a dramatic canyon through these resistant basalt layers, creating the spectacular topography visible from the park. Individual basalt flows are visible in canyon walls and roadcuts, appearing as distinct layers with columnar jointing. The Blue Mountains represent an uplifted portion of the basalt province, with erosion exposing the layered volcanic rocks. Soils are generally thin and rocky, derived from weathered basalt with limited organic matter accumulation. Loess—wind-blown silt deposited during and after the Ice Ages—mantles some areas, creating deeper, more fertile soils. The region escaped direct glaciation, though Ice Age climates influenced vegetation and erosion processes. Puffer Butte, the park's high point, represents resistant basalt that has weathered more slowly than surrounding areas. The Grande Ronde River continues cutting deeper into the basalt, gradually lowering its bed through erosion. Occasional landslides occur on steep canyon slopes, particularly where basalt overlies weaker sediments.
Climate And Weather
Fields Spring State Park experiences a continental climate with significant seasonal temperature variations. Winter brings substantial snowfall, with accumulations often reaching several feet and creating excellent cross-country skiing conditions. Winter temperatures frequently drop below zero Fahrenheit during cold snaps, though daytime highs may reach the 30s and 40s. Spring arrives gradually, with snowmelt occurring from March through May depending on elevation and aspect. Summer temperatures are pleasant at the park's high elevation, generally in the 70s and 80s, cooler than lowland areas. Precipitation averages approximately 30-35 inches annually, more than the surrounding lowlands due to orographic enhancement. Most precipitation falls as snow during winter months, with summer generally dry except for occasional thunderstorms. Fall brings cooler temperatures and vibrant foliage colors from aspens and deciduous shrubs, peaking in late September and October. The high elevation means frost can occur during any month, limiting the growing season. Wind patterns are influenced by the Grande Ronde canyon and regional weather systems. The park's inland location results in greater temperature extremes than coastal areas. Clear, sunny skies are common during summer, providing excellent conditions for hiking and scenic viewing.
Human History
The Fields Spring area has been utilized by Native peoples for thousands of years. The Nez Perce and other groups traveled through the Blue Mountains seasonally, hunting elk and gathering plants. The region served as part of traditional territories with established travel routes and seasonal camps. Euro-American exploration began with fur traders and the Lewis and Clark expedition passing through the broader region in the early 1800s. Settlement intensified following gold discoveries in Idaho in the 1860s, with wagon roads constructed to access mining areas. Charles Fields, for whom the park is named, homesteaded in the area in the late 19th or early 20th century. Ranching and logging became primary economic activities, with timber harvested from the forested mountains. The Civilian Conservation Corps constructed some infrastructure in the area during the 1930s. The property was acquired for park purposes to preserve the scenic vistas and provide recreation access. The puffer Butte fire lookout tower served fire detection purposes for decades before becoming a scenic attraction. The park's remote location meant development remained limited, preserving much of the area's natural character.
Park History
Fields Spring State Park was established to preserve scenic mountain landscapes and provide recreation opportunities in southeastern Washington. The park was acquired through various means, with initial development focusing on camping facilities and trail access to Puffer Butte. The fire lookout tower on Puffer Butte became a popular destination, offering 360-degree views of the surrounding mountains and valleys. Over the decades, facilities were improved including campground upgrades, trail development, and interpretive features. The park has served as an important recreation destination for residents of the tri-cities area and southeastern Washington. Winter use increased as cross-country skiing gained popularity, with the park's high elevation ensuring reliable snow. Management has balanced timber harvesting in some areas with preservation of scenic and ecologically valuable forests. The park underwent facility upgrades in various phases, modernizing restrooms, campsites, and day-use areas. Environmental education programs help visitors understand Blue Mountains ecology and conservation. The park serves as habitat for elk and other wildlife, with management considering wildlife needs alongside recreation. Modern management addresses contemporary challenges including wildfire risk, invasive species, and aging infrastructure.
Major Trails And Attractions
Fields Spring State Park offers several hiking trails showcasing the park's diverse ecosystems and spectacular views. The Puffer Butte Trail climbs to the historic fire lookout tower at 4,450 feet elevation, providing panoramic views of three states. On clear days, the Wallowa Mountains, Seven Devils range, and the Cascade volcanoes are visible from the summit. The loop trail system provides options for various hiking lengths and difficulty levels through forests and meadows. Winter brings excellent cross-country skiing opportunities on snow-covered roads and trails. Wildlife observation is exceptional, particularly for elk which are frequently visible in meadows and forest openings. The park's high elevation and dark skies create excellent stargazing conditions with minimal light pollution. Photography opportunities abound from sweeping mountain vistas to intimate wildflower and wildlife shots. Nearby attractions include the Grande Ronde River canyon with its dramatic Highway 129 route. Clarkston and Lewiston provide urban amenities and access to the Snake and Clearwater river confluence. Hells Canyon National Recreation Area, North America's deepest river gorge, is accessible to the south. The town of Anatone provides limited services as the nearest community to the park.
Visitor Facilities And Travel
Fields Spring State Park offers camping and day-use facilities suitable for year-round recreation. The campground includes approximately 20 campsites accommodating tents and small RVs, though hookups are not available. Modern restroom facilities serve campers, and potable water is available during warmer months. Picnic areas with tables and fire grills are distributed throughout the park. Two cabins are available for rental, providing heated accommodation for winter visitors. The park is located approximately 30 miles south of Clarkston via Highway 129, a scenic but winding mountain road. Access requires climbing through the dramatic Grande Ronde River canyon with numerous switchbacks and steep grades. The nearest full-service communities are Clarkston, Washington and Lewiston, Idaho, offering all necessary amenities. The park operates year-round though some facilities close during winter when snow limits access. Winter visitors should be prepared for snow-covered roads and potentially challenging driving conditions. Four-wheel drive or tire chains may be necessary during winter months. Cell phone coverage is extremely limited and should not be relied upon. Reservations are recommended during summer months though the park rarely fills to capacity. The remote location and high elevation mean visitors should be self-sufficient and prepared for rapidly changing weather.
Conservation And Sustainability
Fields Spring State Park management focuses on protecting Blue Mountains ecosystems while providing diverse recreation opportunities. Wildfire management is critical, with fuel reduction projects and fire prevention education emphasized. The park's forests are managed to reduce ladder fuels and maintain fire-resilient stand structures. Invasive species management addresses cheatgrass, knapweed, and other non-natives that alter ecosystems and increase fire risk. Elk habitat management considers the importance of meadows and forest openings for these large herbivores. Forest health monitoring tracks bark beetle outbreaks, root diseases, and other threats to conifer stands. Native grassland restoration projects work to re-establish bunchgrass communities in areas degraded by past grazing or invasive species. Trail maintenance uses sustainable techniques to minimize erosion while providing access to scenic areas. The park participates in regional wildlife conservation efforts, serving as habitat for elk, deer, and other species. Water resources are limited at the high elevation, requiring conservation measures and efficient use. Visitor education emphasizes fire safety, wildlife etiquette, and Leave No Trace principles. Climate change adaptation addresses potential shifts in species composition, increased drought stress, and altered fire regimes.