Ball Butte | |
---|---|
Highest point | |
Elevation | 8,091 |
Coordinates | 44°03′57″N121°40′35″W / 44.065916°N 121.676490°W Coordinates: 44°03′57″N121°40′35″W / 44.065916°N 121.676490°W |
Geography | |
Location | Deschutes, Oregon, U.S. |
Parent range | Cascade Range |
Topo map | USGS Broken Top |
Geology | |
Volcanic arc | Cascade Volcanic Arc |
Last eruption | Pleistocene |
Ball Butte is a volcanic mountain of the Cascades in Deschutes County, Oregon, United States. [1] Its summit has an elevation of 8,091 feet and is located southeast of Broken Top. [2] It is a popular back-country skiing area and is best accessed from the Dutchman Flat Sno-Park or the Upper Three Creeks Sno-Park. [3] [4]
Bend is a city in and the county seat of Deschutes County, Oregon, United States. It is the principal city of the Bend Metropolitan Statistical Area. Bend is Central Oregon's largest city, with a population of 99,178 at the time of the 2020 U.S. Census, up from 76,693 at the time of the 2010 U.S. Census, and 52,029 at the 2000 census. The Bend metro population was 198,253 as of the 2020 census. It is the fifth largest metropolitan area in Oregon.
Newberry National Volcanic Monument was designated on November 5, 1990, to protect the area around the Newberry Volcano in the U.S. state of Oregon. The monument was created within the boundaries of the Deschutes National Forest, which is managed by the U.S. Forest Service, and includes 54,822 acres of lakes, lava flows, and geologic features in central Oregon.
Mount Bachelor, formerly named Bachelor Butte, is a dormant stratovolcano atop a shield volcano in the Cascade Volcanic Arc and the Cascade Range of central Oregon. Named Mount Bachelor because it stands apart from the nearby Three Sisters, it lies in the eastern segment of the central portion of the High Cascades, the eastern segment of the Cascade Range. The volcano lies at the northern end of the 15-mile (24 km) long Mount Bachelor Volcanic Chain, which underwent four major eruptive episodes during the Pleistocene and the Holocene. The United States Geological Survey considers Mount Bachelor a moderate threat, but Bachelor poses little threat of becoming an active volcano in the near future. It remains unclear whether the volcano is extinct or just inactive.
Mount McLoughlin is a dormant steep-sided stratovolcano, or composite volcano, in the Cascade Range of southern Oregon and within the United States Sky Lakes Wilderness. It is one of the volcanic peaks in the Cascade Volcanic Arc, within the High Cascades sector. A prominent landmark for the Rogue River Valley, the mountain is north of Mount Shasta, and south-southeast of Crater Lake. It was named around 1838 after John McLoughlin, a Chief Factor for the Hudson's Bay Company. Mount McLouglin's prominence has made it a landmark to Native American populations for thousands of years.
Pilot Butte is a lava dome that was created from an extinct volcano located in Bend, Oregon. It is a cinder cone butte which rises nearly 500 feet (150 m) above the surrounding plains. Bend is one of six cities in the United States to have a volcano within its boundaries. The other examples are Mount Tabor in Portland, Oregon, Jackson Volcano in Jackson, Mississippi, Diamond Head in Honolulu, Glassford Hill in Prescott Valley and Pilot Knob in Austin, Texas.
Mount Bachelor ski resort is a ski resort located in Central Oregon, approximately 22 miles (35 km) west of Bend, along Century Drive Highway. The ski area is on the northern side of Mount Bachelor, a stratovolcano rising atop a volcanic shield in the Cascade Range.
Central Oregon is a geographic region in the U.S. state of Oregon and is traditionally considered to be made up of Deschutes, Jefferson, and Crook counties. Other definitions include larger areas, often encompassing areas to the north towards the Columbia River, eastward towards Burns, or south towards Klamath Falls. These three counties have a combined population of 200,431 as of the 2010 census, with Deschutes the largest of the three counties, having approximately four times the population of the other two counties combined. As of 2015, the most populous city in the region is Bend, with an estimated 87,014 residents. As defined by the three county definition, Central Oregon covers 7,833 square miles (20,290 km2) of land. Central Oregon has had 3 record tourism years beginning in 2012. Over 2.2 million people visited Central Oregon in 2012 and again in 2013.
Lava Butte is a cinder cone in central Oregon, United States, just west of U.S. Route 97 between the towns of Bend, and Sunriver in Deschutes County. It is part of a system of small cinder cones on the northwest flank of Newberry Volcano, a massive shield volcano which rises to the southeast. The cinder cone is capped by a crater which extends about 60 feet (20 m) deep beneath its south rim, and 160 feet (50 m) deep from the 5,020-foot (1,530 m) summit on its north side. Lava Butte is part of the Newberry National Volcanic Monument.
Black Butte is an extinct stratovolcano in the U.S. state of Oregon. Located in Jefferson County, it is part of Deschutes National Forest. Black Butte forms part of the Cascade volcanic arc. The butte lies just south of the Metolius Springs, which merge to form the headwaters of the Metolius River. The Metolius River's basin sustains a wide array of plant life, large and small mammals, and more than 80 bird species.
Diamond Peak is a volcano in Klamath and Lane counties of central Oregon in the United States. It is a shield volcano, though it might also be considered a modest stratocone. Diamond Peak forms part of the Cascade Volcanic Arc, a segment of the Cascade Range in western North America extending from southern British Columbia through Oregon to Northern California. Reaching an elevation of 8,748 feet (2,666 m), the mountain is located near Willamette Pass in the Diamond Peak Wilderness within the Deschutes and Willamette national forests. Surrounded by coniferous forest and visible in the skyline from foothills near Eugene, Diamond Peak offers a few climbing routes and can be scrambled. Diamond Peak is one of Oregon's Matterhorns.
Mount Shasta Ski Park is a ski resort located in northern California which has winter and summer operations. Winter operations include skiing & snowboarding, tubing, a backcountry cabin program, lessons, rentals, and events. In the summer they offer Scenic Chairlift Rides, Mountain Biking, and Disc Golf. They are located east of Interstate 5 along SR 89 between the city of Mount Shasta and the town of McCloud. The ski area lies about 6 mi (9.7 km) south of the summit of 14,179 ft (4,322 m) Mount Shasta, the second highest volcano in the Cascade Range behind Mount Rainier. It straddles several small volcanic buttes on the lower southern flanks of the massive stratovolcano, with 3 triple chairlifts running to the top of Coyote Butte- 6,880 ft (2,100 m), Douglas Butte- 6,600 ft (2,000 m), and Marmot Ridge- 6,150 ft (1,870 m) and 1 Quad chairlift on Grey Butte- 7,536 ft (2,297 m) Along with 2 magic carpets, one for tubing and one for learning to ski and snowboard. With a total skiable area of 636 acres and 38 conventional trails. The total skiable vertical is 1,435 ft (437 m), with 20% of the terrain rated beginner, 55% intermediate, and 25% advanced.
Hoodoo Butte is a cinder cone butte in the Cascade Range of northern Oregon, located near Santiam Pass. Immediately to the east lies Hayrick Butte, a prime example of a tuya; the two mountains' names were likely mistaken for each other, but stuck with them over time. The area has been subjected to a number of historic fires. Hoodoo is sometimes considered a subfeature of the Mount Washington shield volcano, and it forms part of the Sisters Reach, which extends from South Cinder Peak to Crane Prairie Reservoir, running for 56 miles (90 km). This region has a high vent density, with many mafic volcanoes of Pleistocene to Holocene age, such as Hoodoo. While Hoodoo has an intact summit crater that was blocked from erosion by glaciers, it has an irregular topography, giving it an open appearance.
Hayrick Butte is a tuya, a type of subglacial volcano, in Linn County, Oregon. Located in the Willamette National Forest near Santiam Pass, it lies adjacent to the cinder cone Hoodoo Butte, which has a ski area. Hayrick Butte likely formed when lava erupted underneath an overlying glacier or ice sheet, producing the flat top with near-vertical walls along the ice-contact margin as the lava cooled and hardened. Hayrick Butte has a nearly flat plateau about 0.5 miles (0.80 km) across and steep walls rising about 700 feet (0.21 km) above its surroundings. A cartographer accidentally switched the names for nearby Hoodoo Butte and Hayrick Butte; the word "hoodoo" usually refers to rock piles and pinnacles like those observed at Hayrick Butte.
Hogg Rock is a tuya volcano and lava dome in the Cascade Range of northern Oregon, located close to Santiam Pass. Produced by magma with an intermediate andesite composition, it has steep slopes and thick glassy margins. Hogg Rock exhibits normal magnetic polarity and is probably about 80,000 years old.
Pelican Butte is a steep-sided dormant shield volcano in the Cascade Range of southern Oregon. It is located 28 miles (45 km) due south of Crater Lake and 12 miles (19 km) northeast of Mount McLoughlin, and rises over 3,800 feet (1,200 m) directly above the shore of Upper Klamath Lake. Ice age glaciers carved a large cirque into the northeast flank of the mountain, forming a steep bowl which is popular in winter with backcountry skiers and snowmobilers. Several proposals have been made over the last few decades for ski area development on the northeast flanks, but none of the proposals has obtained the regulatory approval from the United States Forest Service necessary to proceed with construction. If the ski area is ever built, its skiable vertical of over 3,800 feet (1,200 m) would be the largest in Oregon exceeding the 3,590 feet (1,090 m) of Timberline Lodge ski area on Mount Hood.
Terry Peak is a mountain and ski area in the west central United States, in the Black Hills of South Dakota outside of Lead. With an elevation of 7,064 feet (2,153 m) above sea level, it is the most prominent peak in the Northern Black Hills area, and the sixth highest summit in the range; the tallest is Black Elk Peak at 7,244 feet (2,208 m).
Oregon State University–Cascades (OSU–Cascades) is a branch campus of Oregon State University (OSU) in Bend, Oregon. It is the only university in Central Oregon that offers both baccalaureate and graduate programs. OSU–Cascades also offers professional pathways and certificate programs. The 30-acre campus is the first public university to open in Oregon in more than 50 years. The campus plans to expand academically with new degree programs over a 10-year period.
The SnoCore Tour, occasionally typeset as Sno-Core, was an annual festival tour of the United States. It features performances by some of the most popular groups largely of the alternative rock and metal spectrum. Other than 2008 and 2016, the event has taken place every year since its inception in December 1995. SnoCore is marketed towards the winter sports culture.
Christina "Kiki" Cutter is a former World Cup alpine ski racer from the United States. She was the first American to win a World Cup event, a slalom race in Oslo, Norway, on February 25, 1968. Although Cutter competed on the World Cup circuit for less than three years, her five career victories led the U.S. alpine team for eleven years, surpassed by Phil Mahre in 1979.
The David A. Johnston Cascades Volcano Observatory (CVO) is a volcano observatory in the US that monitors volcanoes in the northern Cascade Range. It was established in the summer of 1980, after the eruption of Mount St. Helens. The observatory is named for United States Geological Survey (USGS) volcanologist David A. Johnston, who was swept away in the Mount St. Helens eruption on the morning of May 18, 1980. The observatory's current territory covers Oregon, Washington, and Idaho. The Cascade Range's extent includes northern California, and Cascade volcanoes in that state, such as Mount Shasta and Lassen Peak, previously fell under the CVO's jurisdiction. However, these volcanoes now fall under the jurisdiction of the California Volcano Observatory (CalVO), formed in February 2012 and based in Menlo Park, California, which monitors and researches volcanic activity throughout California and Nevada.