Wiley's Well is a natural artesian well in the Colorado Desert of Southern California as well as the name of the surrounding region. It is west of Blythe, California, in Riverside County.
It is named after Palo Verde storekeeper and postmaster A.P. Wiley who, in 1907, made a shallow well deeper that was dug in 1876 by a stagecoach company which frequented the nearby Bradshaw Trail. Wiley expanded the well in the hope of attracting business to his remote desert store; it was maintained by local ranchers and cattlemen for years afterward. However, the rapidly falling water table meant a drop of the water's depth to 60 feet (18 m) within a dozen years. Today, the well's original depth is only about 20 feet (6.1 m) at best after wet weather and is unfit for drinking.
In 1985, the Bureau of Land Management drilled a new well 965 feet (294 m) in depth to support the new Wiley's Well Campground, one of only two developed campgrounds in the Mule Mountains Long-Term Visitor Area. The water is both hot at 90 °F/32 °C and heavily mineralized; it is pumped into a cistern to help cool it to a temperature suitable for drinking.
Wiley's Well is also a popular rockhounding site, beginning in the 1930s with the discovery of geode beds. Despite its popularity over the decades, the area remains rich with chalcedony, citrine, quartz crystals, rhyolite and jasper. Though winters are mild, making the campground a popular destination with seasonal visitors from colder climes, summer can be extremely hot with recorded temperatures as high as 130 °F (54 °C).
Wiley's Well is easily accessible via the Wiley's Well Road exit off Interstate 10, 16 miles (26 km) west of Blythe. The entrance to the campground is 9 miles (14 km) south of the highway.
Blythe is a city in eastern Riverside County, California, United States. It is in the Palo Verde Valley of the Lower Colorado River Valley region, an agricultural area and part of the Colorado Desert along the Colorado River, approximately 224 miles (360 km) east of Los Angeles and 150 miles (240 km) west of Phoenix. Blythe was named after Thomas Henry Blythe, a San Francisco financier, who established primary water rights to the Colorado River in the region in 1877. The city was incorporated on July 21, 1916. The population was 18,317 at the 2020 census.
Crater Lake National Park is an American national park located in southern Oregon. Established in 1902, Crater Lake is the fifth-oldest national park in the United States and the only national park in Oregon. The park encompasses the caldera of Crater Lake, a remnant of Mount Mazama, a destroyed volcano, and the surrounding hills and forests.
The Imperial Valley of Southern California lies in Imperial and Riverside counties, with an urban area centered on the city of El Centro. The Valley is bordered by the Colorado River to the east and, in part, the Salton Sea to the west. Farther west lies the San Diego and Imperial County border. To the north is the Coachella Valley region of Riverside County, which together with Imperial Valley form the Salton Trough, or the Cahuilla Basin, also the county line of Imperial and Riverside counties, and to the south the international boundary with Mexico.
Saline Valley is a large, deep, and arid graben, about 27 miles (43 km) in length, in the northern Mojave Desert of California, a narrow, northwest–southeast-trending tectonic sink defined by fault-block mountains. Most of it became a part of Death Valley National Park when the park was expanded in 1994. This area had previously been administered by the Bureau of Land Management. It is located northwest of Death Valley proper, south of Eureka Valley, and east of the Owens Valley. The valley's lowest elevations are about 1,000 ft (300 m) and it lies in the rain shadow of the 14,000 ft (4,300 m) Sierra Nevada range, plus the 11,000 ft (3,400 m) Inyo Mountains bordering the valley on the west.
The Chocolate Mountains of California are located in Imperial and Riverside counties in the Colorado Desert of Southern California. The mountains stretch more than 60 miles (100 km) in a northwest to southeast direction, and are located east of the Salton Sea and south and west of the Chuckwalla Mountains and the Colorado River. To the northwest lie the Orocopia Mountains.
Vidal, California is a small unincorporated community located in southeastern California, in San Bernardino County on U.S. Route 95, 38 miles (61 km) north of Blythe, California, United States and 55 miles (89 km) south of Needles. The town is 22 miles (35 km) west of the townsite of Earp, California and 23 miles (37 km) west of Parker, Arizona on State Highway 62. The community, which is two miles (3 km) north of the Riverside County line, lies at an elevation of 812 feet (247 m) above sea level. Vidal is 221 miles (356 km) from the city of San Bernardino, making it the second-farthest town in the county from the county seat behind Earp. Wyatt Earp spent the last winters of his life in Vidal, working claims of gold and copper he found nearby; the aforementioned townsite of Earp is located in and around those claims.
Chiriaco Summit is a small unincorporated community and travel stop located along Interstate 10 in the Colorado Desert of Southern California. It lies 19 miles (31 km) west of Desert Center on the divide between the Chuckwalla Valley and the Salton Sea basin at an elevation of 1,706 feet (520 m).
Corn Springs is a palm oasis situated in the Chuckwalla Mountains of the Colorado Desert in Riverside County, California, United States, seventeen miles southeast of Desert Center. Native Americans relied on the springs, and they engraved many petroglyphs on the rocks in the area. In the late 19th century, miners in the area also relied on the springs, and they established the Corn Springs Mining District in 1897.
The San Luis Reservoir is an artificial lake on San Luis Creek in the eastern slopes of the Diablo Range of Merced County, California, approximately 12 mi (19 km) west of Los Banos on State Route 152, which crosses Pacheco Pass and runs along its north shore. It is the fifth largest reservoir in California. The reservoir stores water taken from the San Joaquin-Sacramento River Delta. Water is pumped uphill into the reservoir from the O'Neill Forebay which is fed by the California Aqueduct and is released back into the forebay to continue downstream along the aqueduct as needed for farm irrigation and other uses. Depending on water levels, the reservoir is approximately nine miles (14 km) long from north to south at its longest point, and five miles (8 km) wide. At the eastern end of the reservoir is the San Luis Dam, the fourth largest embankment dam in the United States, which allows for a total capacity of 2,041,000 acre-feet (2,518,000 dam3). Pacheco State Park lies along its western shores.
The Domeland Wilderness is a federally designated wilderness area located 55 miles (89 km) northeast of Bakersfield, California USA. It encompasses 130,081 acres (526.42 km2), is jointly managed by the U.S. Forest Service and Bureau of Land Management (BLM) and is mostly within the Sequoia National Forest.
Jackson F. Kimball State Recreation Site is a state park in southern Oregon. The park is operated and maintained by the Oregon Parks and Recreation Department, and is located approximately 20 miles (32 km) southeast of Crater Lake National Park and 3 miles (4.8 km) north of Fort Klamath. The park was established in 1955, and covers 19 acres (7.7 ha) including the headwaters of the Wood River.
Joshua Tree National Park is an American national park in southeastern California, east of San Bernardino and Los Angeles and north of Palm Springs. It is named after the Joshua trees native to the Mojave Desert. Originally declared a national monument in 1936, Joshua Tree was redesignated as a national park in 1994 when the U.S. Congress passed the California Desert Protection Act. Encompassing a total of 795,156 acres – slightly larger than the state of Rhode Island – the park includes 429,690 acres of designated wilderness. Straddling San Bernardino and Riverside Counties, the park includes parts of two deserts, each an ecosystem whose characteristics are determined primarily by elevation: the higher Mojave Desert and the lower Colorado Desert. The Little San Bernardino Mountains traverse the southwest edge of the park.
The Whisky Creek Cabin is a rustic log cabin located in southwest Oregon along the section of the Rogue River that is designated as a National Wild and Scenic River. It is the oldest remaining mining cabin in the Rogue River canyon. The Bureau of Land Management purchased the cabin and surrounding property in 1973. The Whisky Creek Cabin is listed on the National Register of Historic Places in 1975.
The Warner Lakes are a chain of shallow lakes and marshes in the Warner Valley of eastern Lake County, Oregon, United States. The lakes extend the length of the valley, covering approximately 90,000 acres (360 km2).
The Ana River is a short spring-fed river in south-central Oregon. It is on the northwestern edge of the Great Basin drainage. It flows 7 miles (11 km) from springs at the foot of Winter Ridge through high desert, range, and wetlands before emptying into Summer Lake. For most of its course, the Ana River flows through the Summer Lake Wildlife Area, which is maintained by the Oregon Department of Fish and Wildlife. The river provides habitat for many mammal and bird species, as well as several fish species, including the rare Summer Lake Tui chub. The largest hybrid striped bass ever caught in Oregon was taken from Ana Reservoir in 2009.
The Summer Lake Wildlife Area is a 29.6-square-mile (77 km2) wildlife refuge located on the northwestern edge of the Great Basin drainage in south-central Oregon. It is administered by the Oregon Department of Fish and Wildlife. The refuge is an important stop for waterfowl traveling along the Pacific Flyway during their spring and fall migrations. The Summer Lake Wildlife Area also provides habitat for shorebirds and other bird species as well as wide variety of mammals and several fish species. The Ana River supplies the water for the refuge wetlands.
Fossil Lake is a dry lakebed in the remote high desert country of northern Lake County in the U.S. state of Oregon. During the Pleistocene epoch, Fossil Lake and the surrounding basin were covered by an ancient lake. Numerous animals used the lake's resources. Over time, the remains of many of these animals became fossilized in the lake sediments. As a result, Fossil Lake has been an important site for fossil collection and scientific study for well over a century. Over the years, paleontologists have found the fossil remains of numerous mammals as well as bird and fish species there. Some of these fossils are 2 million years old.
Gerber Reservoir is an irrigation impoundment created by Gerber Dam. It is located in southern Klamath County, Oregon, United States. The reservoir covers 3,815 acres (1,544 ha). The dam and reservoir are named in honor of Louis C. Gerber, an early pioneer who owned much of the land flooded by the reservoir. Today, the reservoir and surrounding property is owned by the United States Government. It is administered by the Bureau of Reclamation and the Bureau of Land Management. Gerber Reservoir is a popular outdoor recreation site with two campgrounds along its west shore.
Goldbug Hot Springs is a hot spring located in the Salmon-Challis National Forest about 20 miles south of Salmon, Idaho. The spring is along Warm Spring Creek and there are about six waterfall-fed pools. Goldbug is listed as having a temperature of 113 °F (45 °C), but the temperature of the pools will vary depending on the time of year. The pools have a sand/gravel bottom and are dammed by boulders. Due to the hike and remoteness of the trailhead, it is not usually crowded.
Nancy Lake State Recreation Area is a 22,685 acres (9,180 ha) park near Willow in the Matanuska-Susitna Borough of Alaska. Founded on July 6, 1966, and set aside specifically for recreational use, the park is home to more than a hundred lakes as well as extensive wetlands. The landscape of the park was crafted in glacial retreats around 9,000 years ago, and around this same time the first inhabitants likely moved into the area. They were eventually followed by Russian exploration, and later increases in white settlement due to commerce and the presence of gold.