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Crater Lake National Park

Crater Lake National Park is a United States National Park located in southern Oregon. Established in 1902, Crater Lake National Park is the fifth oldest national park in the United States and the only one in the state of Oregon. The park encompasses the caldera of Crater Lake, a remnant of a destroyed volcano, Mount Mazama, and the surrounding hills and forests. The lake is 1,943 feet deep at its deepest point, which makes it the deepest lake in the United States, the second deepest in North America and the ninth deepest in the world. Crater Lake is often referred to as the seventh deepest lake in the world, but this former listing excludes the approximately 3,000-foot depth of subglacial Lake Vostok in Antarctica, which resides under nearly 13,000 feet of ice, and the recent report of a 2,740-foot maximum depth for Lake O'Higgins/San Martin, located on the border of Chile and Argentina. However, when comparing its average depth of 1,148 feet to the average depth of other deep lakes, Crater Lake becomes the deepest in the Western Hemisphere and the third deepest in the world. The impressive average depth of this volcanic lake is due to the nearly symmetrical 4,000-foot deep caldera formed 7,700 years ago during the violent climactic eruptions and subsequent collapse of Mount Mazama and the relatively moist climate that is typical of the crest of the Cascade Range. The caldera rim ranges in elevation from 7,000 to 8,000 feet . The United States Geological Survey benchmarked elevation of the lake surface itself is 6,178 feet . This National Park encompasses 183,224 acres . Crater Lake has no streams flowing into or out of it. All water that enters the lake is eventually lost from evaporation or subsurface seepage. The lake's water commonly has a striking blue hue, and the lake is re-filled entirely from direct precipitation in the form of snow and rain.

Hillsboro

Hillsboro is the fifth-largest city in the State of Oregon and is the county seat of Washington County. Lying in the Tualatin Valley on the west side of the Portland metropolitan area, the city hosts many high-technology companies, such as Intel, that comprise what has become known as the Silicon Forest. At the 2010 Census, the citys population was 91,611. For thousands of years before the arrival of European-American settlers, the Atfalati tribe of the Kalapuya lived in the Tualatin Valley near the later site of Hillsboro. The climate, moderated by the Pacific Ocean, helped make the region suitable for fishing, hunting, food gathering, and agriculture. Settlers founded a community here in 1842, later named after David Hill, an Oregon politician. Transportation by riverboat on the Tualatin River was part of Hillsboros settler economy. A railroad reached the area in the early 1870s and an interurban electric railway about four decades later. These railways, as well as highways, aided the slow growth of the city to about 2,000 people by 1910 and about 5,000 by 1950, before the arrival of high-tech companies in the 1980s. Hillsboro has a council–manager government consisting of a city manager and a city council headed by a mayor. In addition to high-tech industry, sectors important to Hillsboros economy are health care, retail sales, and agriculture, including grapes and wineries. The city operates more than twenty parks and the mixed-use Hillsboro Stadium, and ten sites in the city are listed on the National Register of Historic Places . Modes of transportation include private vehicles, public buses and light rail, and aircraft using the Hillsboro Airport. The city is home to Pacific Universitys Health Professions Campus. Notable residents include two Oregon governors.

Oregon Caves National Monument and Preserve

Oregon Caves National Monument and Preserve is a National Monument and Preserve in the northern Siskiyou Mountains of southwestern Oregon in the United States. The main part of the 4,558-acre park, including the marble cave and a visitor center, is located 20 miles east of Cave Junction, on Oregon Route 46. A separate visitor center in Cave Junction occupies 4 acres of the total. Both parts of the monument, managed by the National Park Service, are in southwestern Josephine County, near the Oregon–California border. The climate is generally mild even at the caves elevation of about 4,000 feet above sea level, but icicles can form at the cave entrance, and winter snow sometimes blocks the park highway. Elijah Davidson, a resident of nearby Williams, discovered the cave in 1874. Over the next two decades, private investors failed in efforts to run successful tourist ventures at the publicly owned site. After passage of the Antiquities Act by the United States Congress, President William Howard Taft established Oregon Caves National Monument, to be managed by the United States Forest Service, in 1909. The popularity of the automobile, construction of paved highways, and promotion of tourism by boosters from Grants Pass led to large increases in cave visitation during the late 1920s and thereafter. Among the attractions at the remote monument is the Oregon Caves Chateau, a six-story hotel built in a rustic style in 1934. It is a National Historic Landmark and is part of the Oregon Caves Historic District within the monument. The Park Service, which assumed control of the monument in 1933, offers tours of the cave from mid-April through early November. In 2014, the monument was expanded by about 4,000 acres and re-designated a National Monument and Preserve. In addition, the River Styx, which flows through the cave and emerges as Cave Creek, was named to the National Wild and Scenic Rivers System. Oregon Caves is a solutional cave, with passages totaling about 15,000 feet, that formed in marble. The parent rock was originally limestone that metamorphosed to marble during the geologic processes that created the Klamath Mountains, including the Siskiyous. Although the limestone formed about 190 million years ago, the cave itself is no older than a few million years. Valued as a tourist cave, the cavern also has scientific value; sections of the cave that are not on tour routes contain fossils of national importance. In addition to cave touring, activities at the park include hiking, photography, and wildlife viewing. One of the park trails leads through the forest to Big Tree, which at 13 feet is the thickest Douglas-fir known in Oregon. Lodging and food are available at The Chateau and in Cave Junction. Camping is available at Forest Service campgrounds and private sites in the area.

John Day Fossil Beds National Monument

John Day Fossil Beds National Monument is a U.S. National Monument in Wheeler and Grant counties in east-central Oregon. Located within the John Day River basin and managed by the National Park Service, the park is known for its well-preserved layers of fossil plants and mammals that lived in the region between the late Eocene, about 45 million years ago, and the late Miocene, about 5 million years ago. The monument consists of three geographically separate units: Sheep Rock, Painted Hills, and Clarno. The units cover a total of 13,944 acres of semi-desert shrublands, riparian zones, and colorful badlands. About 184,000 people frequented the park in 2014 to engage in outdoor recreation or to visit the Thomas Condon Paleontology Center or the James Cant Ranch Historic District. Before the arrival of Euro-Americans in the 19th century, the John Day basin was frequented by Sahaptin people who hunted, fished, and gathered roots and berries in the region. After road-building made the valley more accessible, settlers established farms, ranches, and a few small towns along the river and its tributaries. Paleontologists have been unearthing and studying the fossils in the region since 1864, when Thomas Condon, a missionary and amateur geologist, recognized their importance and made them known globally. Parts of the basin became a National Monument in 1975. Averaging about 2,200 feet in elevation, the monument has a dry climate with temperatures that vary from summer highs of about 90 °F to winter lows below freezing. The monument has more than 80 soil types that support a wide variety of flora, ranging from willow trees near the river to grasses on alluvial fans to cactus among rocks at higher elevations. Fauna include more than 50 species of resident and migratory birds. Large mammals like elk and smaller animals such as raccoons, coyotes, and voles frequent these units, which are also populated by a wide variety of reptiles, fish, butterflies, and other creatures adapted to particular niches of a mountainous semi-desert terrain.

Cascade Locks

Cascade Locks is a city in Hood River County, Oregon, United States. The city took its name from a set of locks built to improve navigation past the Cascades Rapids of the Columbia River. The U.S. federal government approved the plan for the locks in 1875, construction began in 1878, and the locks were completed on November 5, 1896. The locks were subsequently submerged in 1938, replaced by Bonneville Lock and Dam, although the city lost no land from the expansion of Lake Bonneville behind the dam some 4 miles downstream of the city. The city population was 1,144 at the 2010 census. The 2007 estimate is 1,075 residents. Cascade Locks is just upstream from the Bridge of the Gods, a toll bridge that spans the Columbia River. It is the only bridge across the Columbia between Portland and Hood River. Cascade Locks is also a few miles upstream of Eagle Creek Gorge, a popular scenic area that doubles as an alternate route for the Pacific Crest Trail. Cascade Locks is used frequently by hikers along the Pacific Crest Trail to cross the Columbia River. Cascade Locks is the lowest point along the trail, which runs from the Mexican border in California to the Canadian border in Washington. Since 1999, the Confederated Tribes of Warm Springs have been pursuing an off-reservation casino to be sited in Cascade Locks. Since 2008, city officials have been pursuing an arrangement that would allow them to trade city well water for state-owned spring water and to sell it to Nestlé for bottling.

Crater Lake

Crater Lake is a caldera lake in the western United States, located in south-central Oregon. It is the main feature of Crater Lake National Park and is famous for its deep blue color and water clarity. The lake partly fills a nearly 2,148-foot deep caldera that was formed around 7,700 years ago by the collapse of the volcano Mount Mazama. There are no rivers flowing into or out of the lake; the evaporation is compensated for by rain and snowfall at a rate such that the total amount of water is replaced every 250 years. At 1,943 feet, the lake is the deepest in the United States, and the seventh or ninth deepest in the world, depending on whether average or maximum depth is measured. Crater Lake is also known for the "Old Man of the Lake", a full-sized tree which is now a stump that has been bobbing vertically in the lake for over a century. The low temperature of the water has slowed the decomposition of the wood, hence the longevity of the bobbing tree. Two islands are in Crater Lake; Wizard Island formed from a cinder cone that erupted after Crater Lake began to fill with water, and the smaller Phantom Ship has seven different trees living on it. There are also colonies of violet green swallows and several varieties of wildflowers and lichens living there. While having no indigenous fish population, the lake was stocked from 1888 to 1941 with a variety of fish. Several species have formed self-sustaining populations. Since 2002, one of the states regular-issue license plate designs has featured Crater Lake. The commemorative Oregon State Quarter, which was released by the United States Mint in 2005, features an image of Crater Lake on its reverse.

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