China Hat (Oregon)

Last updated
China Hat
USA Oregon relief location map.svg
Red triangle with thick white border.svg
China Hat
Highest point
Elevation 6,573
Coordinates 43°40′51″N121°02′02″W / 43.680874°N 121.033844°W / 43.680874; -121.033844 Coordinates: 43°40′51″N121°02′02″W / 43.680874°N 121.033844°W / 43.680874; -121.033844
Geography
Location Deschutes, Oregon, U.S.
Parent range Cascade Range
Topo map USGS China Hat
Geology
Age of rock 6.3 - 7.4 Ma [1]
Mountain type Pyroclastic cone
Volcanic arc Cascade Volcanic Arc
Last eruption Pleistocene

China Hat is a volcanic butte on the southeastern flank of Newberry Volcano in Deschutes County, Oregon, United States. It is a rhyolitic dome dating from the age of the Middle Pleistocene. [2] Both China Hat and nearby East Butte are covered by Mazama Ash and Newberry Ash. [3]

Although China Hat is often thought of as a side vent of Newberry Volcano less than ten miles away, [4] it is estimated to be older than first formation of the Newberry Caldera, 780,000 thousand years old [5] versus 500,000 years ago [6] and is on the western edge of a series of high lava plains eruptions derived from a tongue of the same mantle plume that fuels the Yellowstone Caldera [7]

China Hat Road, named after the butte, starts in Bend and heads to Fort Rock. [8] The road is a hotspot for law enforcement. [8] China Hat Campground is a campground located near China Hat butte along this road. [9]

The butte was named for its similarity in appearance, when viewed from Fort Rock, to the Asian conical hat worn by Chinese immigrant laborers. [8]

Related Research Articles

<span class="mw-page-title-main">Deschutes County, Oregon</span> County in Oregon, United States

Deschutes County is one of the 36 counties in the U.S. state of Oregon. As of the 2020 census, the population was 198,253. The county seat is Bend. The county was created in 1916 out of part of Crook County and was named for the Deschutes River, which itself was named by French-Canadian trappers of the early 19th century. It is the political and economic hub of Central Oregon. Deschutes comprises the Bend, Oregon Metropolitan Statistical Area. Deschutes is Oregon’s fastest-growing and most recently-formed county.

<span class="mw-page-title-main">Newberry National Volcanic Monument</span> Protected area in Oregon, US

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.

<span class="mw-page-title-main">Mount Bachelor</span> Dormant stratovolcano in Oregon, United States

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.

<span class="mw-page-title-main">Geology of the Lassen volcanic area</span> Geology of a U.S. national park in California

The Lassen volcanic area presents a geological record of sedimentation and volcanic activity in and around Lassen Volcanic National Park in Northern California, U.S. The park is located in the southernmost part of the Cascade Mountain Range in the Pacific Northwest region of the United States. Pacific Oceanic tectonic plates have plunged below the North American Plate in this part of North America for hundreds of millions of years. Heat and molten rock from these subducting plates has fed scores of volcanoes in California, Oregon, Washington and British Columbia over at least the past 30 million years, including these in the Lassen volcanic areas.

<span class="mw-page-title-main">Newberry Volcano</span> Shield volcano in Oregon, United States

Newberry Volcano is a large active shield-shaped stratovolcano located about 20 miles (32 km) south of Bend, Oregon, United States, 35 miles (56 km) east of the major crest of the Cascade Range, within the Newberry National Volcanic Monument. Its highest point is Paulina Peak. The largest volcano in the Cascade Volcanic Arc, Newberry has an area of 1,200 square miles (3,100 km2) when its lava flows are taken into account. From north to south, the volcano has a length of 75 miles (121 km), with a width of 27 miles (43 km) and a total volume of approximately 120 cubic miles (500 km3). It was named for the geologist and surgeon John Strong Newberry, who explored central Oregon for the Pacific Railroad Surveys in 1855. The surrounding area has been inhabited by Native American populations for more than 10,000 years.

<span class="mw-page-title-main">Mount Mazama</span> Complex volcano in the Cascade Range

Mount Mazama is a complex volcano in the state of Oregon, United States, in a segment of the Cascade Volcanic Arc and Cascade Range. Most of the mountain collapsed following a major eruption approximately 7,700 years ago. The volcano is in Klamath County, in the southern Cascades, 60 miles (97 km) north of the Oregon–California border. Its collapse, due to eruption of magma emptying the underlying magma chamber, formed a caldera that holds Crater Lake. The mountain is in Crater Lake National Park. Mount Mazama originally had an elevation of 12,000 feet (3,700 m), but following its climactic eruption this was reduced to 8,157 feet (2,486 m). Crater Lake is 1,943 feet (592 m) deep, the deepest freshwater body in the US and the second deepest in North America after Great Slave Lake in Canada.

<span class="mw-page-title-main">Belknap Crater</span> Shield volcano in the U.S. state of Oregon

Belknap Crater is a shield volcano in the Cascade Range in the U.S. state of Oregon. Located in Linn County, it is associated with lava fields and numerous subfeatures including the Little Belknap and South Belknap volcanic cones. It lies north of McKenzie Pass and forms part of the Mount Washington Wilderness. Belknap is not forested and most of its lava flows are not vegetated, though there is some wildlife in the area around the volcano, as well as a number of tree molds formed by its eruptive activity.

<span class="mw-page-title-main">Active volcano</span> Geological feature

An active volcano is a volcano which is either erupting or is likely to erupt in the future. An active volcano which is not currently erupting is known as a dormant volcano.

<span class="mw-page-title-main">Yellowstone hotspot</span> Volcanic hotspot in the United States

The Yellowstone hotspot is a volcanic hotspot in the United States responsible for large scale volcanism in Idaho, Montana, Nevada, Oregon, and Wyoming, formed as the North American tectonic plate moved over it. It formed the eastern Snake River Plain through a succession of caldera-forming eruptions. The resulting calderas include the Island Park Caldera, Henry's Fork Caldera, and the Bruneau-Jarbidge caldera. The hotspot currently lies under the Yellowstone Caldera. The hotspot's most recent caldera-forming supereruption, known as the Lava Creek Eruption, took place 640,000 years ago and created the Lava Creek Tuff, and the most recent Yellowstone Caldera. The Yellowstone hotspot is one of a few volcanic hotspots underlying the North American tectonic plate; another example is the Anahim hotspot.

<span class="mw-page-title-main">Pilot Butte (Oregon)</span> Lava dome in Bend, Oregon

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.

<span class="mw-page-title-main">Lava Butte</span> Cinder cone in central Oregon, United States

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.

<span class="mw-page-title-main">Olallie Butte</span> Mountain in United States of America

Olallie Butte is a steep-sided shield volcano in the Cascade Range of the northern part of the U.S. state of Oregon. It is the largest volcano and highest point in the 50-mile (80 km) distance between Mount Hood and Mount Jefferson. Located just outside the Olallie Scenic Area, it is surrounded by more than 200 lakes and ponds fed by runoff, precipitation, and underground seepage, which are popular spots for fishing, boating, and swimming. The butte forms a prominent feature in the Mount Jefferson region and is usually covered with snow during the winter and spring seasons.

<span class="mw-page-title-main">Hoodoo Butte</span> Mountain in Oregon, United States

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.

<span class="mw-page-title-main">Hayrick Butte</span> Mountain in United States of America

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.

<span class="mw-page-title-main">Hogg Rock</span> Mountain in the Cascade Range of northern Oregon

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.

<span class="mw-page-title-main">Blue Lake Crater</span> Volcanic crater in Oregon, United States

Blue Lake Crater is a maar, or a broad, low-relief volcanic crater, in the U.S. state of Oregon. Located in Jefferson County, it consists of three overlapping craters, which hold Blue Lake. The drainage basin for Blue Lake has very steep, forested slopes and is mostly part of the explosion crater left by the volcano's eruption. The volcano lies within the Metolius River basin, which supports a wide array of plant life, large and small mammals, and more than 80 bird species. In 2009, Governor of Oregon Ted Kulongoski signed a bill designating the Metolius River basin as an area of critical concern, preventing large-scale development on the land and protecting its wildlife.

<span class="mw-page-title-main">Horse Lava Tube System</span> A lava tube system located near Bend, Oregon

The Horse Lava Tube System is a series of lava tubes within Deschutes County, Oregon, of the United States. The system starts within the Deschutes National Forest on the northern flank of Newberry Volcano and heads north into and near the city of Bend. The system continues north to Redmond and includes the Redmond Caves. The flow diverts into the Redmond Dry Canyon, where the last known segment is known to exist; however, the basalt flow that created the system goes beyond to Crooked River Ranch and terminates just short of the Crooked River Gorge. The lava flow that created the Horse system is also referred to as the Horse Cave lobe and it filled the ancient channel of the Deschutes River which at that time flowed around the east side of Pilot Butte. The Horse Cave lobe is a part of the basalt of Lava Top Butte which also consists of the Arnold Lava Tube System, the Badlands rootless shield, and the Lava Top butte basalt. All have a geologic age around 80,000 years old.

The Paulina Mountains are a mountain range in Deschutes County, Oregon. There are 97 named mountains in the Paulina Mountains, the tallest and most famous one being Paulina Peak, which sits at 7,969 feet in elevation."Paulina Peak serves as the highest point of the Newberry Volcano, a large active stratovolcano that sits just 35 miles east of the crest of the Cascade Range. These summits are actually the remnants of an old crater called the Newberry Crater.

Boyd Cave is a lava tube within Deschutes County, Oregon, of the United States. The cave is within Deschutes National Forest and is located on the northern flank of Newberry Volcano near the city of Bend.

Pine Mountain is a rhyolitic mountain east of Bend and south of U.S. Route 20 (US 20) in eastern Deschutes County, Oregon, United States. It is the site of an astronomical observatory called the Pine Mountain Observatory. The mountain is a part of the Deschutes Formation and is the southeasternmost exposure of the formation and is of similar age to Cline Buttes. Pine Mountain is also well known for its spectacular "glass off" weather conditions which are ideal for paragliding.

References

  1. "Bimodal volcanism of the High Lava Plains and Northwestern Basin and Range of Oregon : Distribution and tectonic implications of age-progressive rhyolites". OregonState.edu. Retrieved 2018-01-04.
  2. "Newberry Volcano; The Life and Times of a Shield Volcano Complex (Field Trip 3A)". InThePlaygroundofGiants.com. Retrieved 2018-01-03.
  3. U.S. Geological Survey (1969). "Geological Survey Research 1969 Chapter D". Books.Google.com. Retrieved 2018-01-03.
  4. Jensen, Robert A. Roadside Guide to the Geology of Newberry Crater. Third edition. Bend, OR: CenOreGeoPub 2000
  5. Harris, Stephen L. Fire Mountains of the West. Third edition. Missoula, MT: Mountain Press Publishing 2005
  6. Jensen, page 24
  7. Orr, Elizabeth L. and William N. Oregon Geology. Corvallis, OR: Oregon State University Press 2012 page 115
  8. 1 2 3 "Road, butte named after the accessory worn by Chinese immigrant laborers". BendBulletin.com. Retrieved 2018-01-03.
  9. "China Hat Campground". FS.USDA.GOV. Retrieved 2018-01-03.