Sarmila/GeoWiki-Features huggingface dataset:
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 deep beneath its south rim, and deep from the summit on its north side. Lava Butte is part of the Newberry National Volcanic Monument. Volcanic history.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Sometime after 1901, the Great Northern Railway was extended south through the area. The construction crew built the rail line directly through the ʻAʻā lava flow of Lava Butte. The cinder cone was also exploited to some extent for its economic value.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
In July 1966, twenty-two astronauts trained in Central Oregon for the upcoming Moon landings, at sites including Lava Butte, Lava River Cave, and Newberry Crater. In May 1967 the U.S. Forest Service created the Lava Butte Geological Area to protect the cinder cone, with plans for recreational and interpretive development.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Lava Butte. 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.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
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 deep beneath its south rim, and deep from the summit on its north side. Lava Butte is part of the Newberry National Volcanic Monument. Volcanic history.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Lava Butte is part of the Newberry National Volcanic Monument. Volcanic history. Like the other cinder cones in the area, Lava Butte only experienced a single eruption, dated by geologists in 1977 to 6,150 carbon-14 years, equivalent to about 7,000 years ago. The eruption began with a fissure spewing hot cinders to form the cone.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Human history. The early history of Lava Butte is not known, but it is assumed that Native Americans observed the eruptions and later ascended the prominent new landmark. White settlers arriving in the 1800s also noted the landmark. In 1903, I.C. Russell was the first geologist to study the butte and speculated that it erupted as recently as 150 years ago. Dr.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Dr. Howel Williams estimated it to be much older, but incorrectly at 1,000 years old. In September 1914, Lava Butte &quot;erupted&quot; when the Bend Chamber of Commerce simulated an eruption to surprise a visiting Portland group. In 1925, USGS geologist Harold Stearns studied the Newberry area and recognized the fissure system which extends from Lava Butte to East Lake within Newberry Caldera.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
The construction crew built the rail line directly through the ʻAʻā lava flow of Lava Butte. The cinder cone was also exploited to some extent for its economic value. In June 1926, a quarry was developed in the fault scarp east of Lava Butte as a source for paving material for the first The Dalles-California Highway (later U.S. Route 97).

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
A United States Forest Service fire lookout tower was built on the summit in 1931, and in early 1933 a steep, single-lane road was constructed spiraling up to the summit. In February of that year, the local Skyliners ski club proposed a ski jump on Lava Butte, but it was never built.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
In February of that year, the local Skyliners ski club proposed a ski jump on Lava Butte, but it was never built. In June 1946, widening of the road up Lava Butte to two lanes was completed, along with constructing two small parking lots at the summit. The road was later paved in July 1950.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
In 1998 this was replaced with a new lookout built in the original L-4 style of 1931. In July 1966, twenty-two astronauts trained in Central Oregon for the upcoming Moon landings, at sites including Lava Butte, Lava River Cave, and Newberry Crater. In May 1967 the U.S.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Construction of the Lava Lands Visitor Center located just south of the cone began in April 1969 and it was finally dedicated in September 1975. In November 1990, Newberry National Volcanic Monument was created encompassing Newberry Crater, Lava Cast Forest Geological Area, Lava River Cave, and the Lava Butte Geological Area.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
From early May to mid October, a shuttle transports visitors up Red Cinder Road from the Lava Lands Visitor Center to the lookout on Lava Butte. Hiking up Red Cinder Road is a year-round option. A scenic rim trail around the top of Lava Butte is long.

Geographic entities mentioned:
surface_form: lava butte
instance_of: Mountain
countries: United States
coordinates: lat: 43.917855555556
lon: -121.35603333333
Mount Baker, Seattle. Mount Baker is a neighborhood in southeastern Seattle, Washington. The neighborhood's name comes from the view of Mount Baker in Whatcom County, that is seen by looking north over Lake Washington. It is bounded by Lake Washington to the east, Interstate 90 and then Leschi to the north, Rainier Valley to the west, and Columbia City to the south.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
In early Welsh sources, Bedwyr Bedrydant (&quot;Bedwyr of the Perfect Sinew&quot;) is a handsome, one-handed warrior under Arthur's command. His father is given as Pedrawd or Bedrawd, and his children as Amhren and Eneuawg, both members of Arthur's court. The 9th-century version of &quot;Englynion y Beddau&quot; (&quot;The Stanzas of the Graves&quot;) gives Bedwyr's final resting place on Tryfan.

Geographic entities mentioned:
surface_form: Tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
Himekami. is a Japanese new-age musical group, founded in 1980 by composer as, changing its name to Himekami in 1984. The band's name is derived from Mount Himekami in Morioka, Iwate Prefecture. The group's current line-up consists of synthesizer player, son of Yoshiaki, and vocalists Wakako Nakajima, Tomoko Fujii, Junko Shiwa, and Yoriko Sano.

Geographic entities mentioned:
surface_form: Mount Himekami
instance_of: Mountain
countries: Japan
coordinates: lat: 39.84416667
lon: 141.24694444
devilli&quot; and &quot;A. fangfangae&quot;. These species were distinguished by various morphological differences such as anal and dorsal fins, from other &quot;Alburnoides&quot; species that occur in Lake Prespa, Lake Skadar or the Danube River. The genus &quot;Alburnoides&quot; is classified in the subfamily Leuciscinae of the family Leuciscidae. Etymology.

Geographic entities mentioned:
surface_form: Lake Prespa
instance_of: Lake
countries: North Macedonia
Albania
Greece
coordinates: lat: 40.9
lon: 21.05
As director, Olcott headed a small team in Ireland: Kalem's leading lady and principal screenwriter, Gene Gauntier, and cameraman George Hollister. There, they filmed &quot;A Lad from Old Ireland&quot; in Cork area plus a scenic film &quot;The Irish Honeymoon&quot; shot in Blarney Castle, Glengarriff, Gap of Dunloe, the Lakes of Killarney and Dublin.

Geographic entities mentioned:
surface_form: Lakes of Killarney
instance_of: Group of lakes
countries: Ireland
coordinates: lat: 52.041666666667
lon: -9.55
The Santa Monica facility eventually would be used to make comedies. In December 1912, after successful &quot;air tests&quot;, Kalem sent a troupe of players and a crew headed by McGowan to Birmingham, Alabama where the Lubin Manufacturing Company had briefly begun producing films. They took over lodgings and an outdoor stage at the Bluff Park Hotel on Shades Mountain south of the city.

Geographic entities mentioned:
surface_form: Shades Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4169
lon: -86.8511
He began to incorporate peasant motifs in his symbolist poetry. He took elements not only from Slovene, but also from Irish, Scottish, Slovak, and Latvian folk motifs. He later traveled to the Austrian Littoral, visiting his mother in Trieste and living briefly in Grado before settling in the Vipava Valley for some time.

Geographic entities mentioned:
surface_form: Vipava Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 45.876147222222
lon: 13.907319444444
He has also studied at the National Judicial College, The Judge Advocate General's Legal Center and School, and Oxford University. Personal life. Minier traveled to over one hundred countries around the world. He climbed Mount Fuji and Mount Kilimanjaro and competed in police athletic events internationally. After retiring, he moved to Spring Hill, Tennessee. Career.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Assigned to the West Gulf Blockading Squadron, &quot;Meteor&quot; departed New Orleans 26 March 1864 to take up station as guard vessel between Head of Passes and Pass a l’Outre on the Mississippi River, continuing on this duty in addition to providing support for ground troops in skirmishes at the mouth of the Red River and operating off Port Hudson, Louisiana, until 10 February 1865 when she sailed for Mobile Bay.

Geographic entities mentioned:
surface_form: Head of Passes
instance_of: Landform
countries: United States
coordinates: lat: 29.157
lon: -89.254
Discography. The albums released by the band included
Awards and honours. TAAQ was featured on The WorldSpace Honours 2007 for their outstanding contributions to Indian rock scene with interviews with other Indian band members, an extensive play-through of their work by RJ Hari, and an Interview with the band themselves about &quot;10 years of TAAQ&quot;.

Geographic entities mentioned:
surface_form: Indian rock
instance_of: Mountain
countries: United States
coordinates: lat: 45.989
lon: -120.823
Birch Creek is a northwesterly-flowing stream in Beaver County, Utah. It originates on the western slope of Birch Creek Mountain in the Tushar Mountains in Fishlake National Forest, and its waters flow west into South Creek, then under Interstate 15 south of the town of Beaver, and thence to the Beaver River, and ultimately to the Sevier River and Lake. Watershed and Course.

Geographic entities mentioned:
surface_form: Birch Creek Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.218888888889
lon: -112.45416666667
Watershed and Course. Birch Creek begins as Middle Fork Birch Creek on the western slope of its namesake Birch Creek Mountain at elevation in the Tushar Mountains. Minor tributaries on Birch Creek Mountain include North Fork Birch Creek and South Fork Birch Creek. Ecology.

Geographic entities mentioned:
surface_form: Birch Creek Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.218888888889
lon: -112.45416666667
Buck Mountain (Wyoming). Buck Mountain (elevation:) is a mountain located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. Description. The mountain is the highest summit south of Garnet Canyon and is easily seen from most vantage points in Jackson Hole. Views from the summit offer excellent views of the Cathedral Group to the north.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6081079
lon: -90.3926199
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.66388889
lon: -90.52972222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.889722222222
lon: -74.404166666667
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.461944444444
lon: -105.43833333333
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6894
lon: -110.819
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9509
lon: -76.2074
surface_form: grand teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6047712
lon: -90.7190122
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.052777777778
lon: -74.532777777778
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.193333333333
lon: -78.563611111111
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.093611111111116
lon: -120.91222222222223
Buck Mountain (Wyoming). Buck Mountain (elevation:) is a mountain located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. Description. The mountain is the highest summit south of Garnet Canyon and is easily seen from most vantage points in Jackson Hole. Views from the summit offer excellent views of the Cathedral Group to the north.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Timberline Lake is located on the eastern flanks of the peak. History. The first documented summiting by people of European descent was on August 21, 1898, by T.M. Bannon and George Buck, only ten days after Grand Teton was first climbed by another party. Bannon later became the first person to climb Borah Peak, the tallest mountain in the state of Idaho.

Geographic entities mentioned:
surface_form: Grand Teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
Timberline Lake is located on the eastern flanks of the peak. History. The first documented summiting by people of European descent was on August 21, 1898, by T.M. Bannon and George Buck, only ten days after Grand Teton was first climbed by another party. Bannon later became the first person to climb Borah Peak, the tallest mountain in the state of Idaho.

Geographic entities mentioned:
surface_form: Borah Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1373891
lon: -113.78110123
Buck Mountain (Wyoming). Buck Mountain (elevation:) is a mountain located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. Description. The mountain is the highest summit south of Garnet Canyon and is easily seen from most vantage points in Jackson Hole. Views from the summit offer excellent views of the Cathedral Group to the north.

Geographic entities mentioned:
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6081079
lon: -90.3926199
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.66388889
lon: -90.52972222
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.889722222222
lon: -74.404166666667
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.461944444444
lon: -105.43833333333
surface_form: buck mountain (wyoming)
instance_of: Mountain
countries: United States
coordinates: lat: 43.6894
lon: -110.819
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9509
lon: -76.2074
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6047712
lon: -90.7190122
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.052777777778
lon: -74.532777777778
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.193333333333
lon: -78.563611111111
surface_form: buck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.093611111111116
lon: -120.91222222222223
Buck Mountain (Wyoming). Buck Mountain (elevation:) is a mountain located in the Teton Range, Grand Teton National Park, Wyoming, immediately southeast of Grand Teton. Description. The mountain is the highest summit south of Garnet Canyon and is easily seen from most vantage points in Jackson Hole. Views from the summit offer excellent views of the Cathedral Group to the north.

Geographic entities mentioned:
surface_form: the cathedral
instance_of: Mountain
countries: United States
coordinates: lat: 40.775833333333
lon: -110.71027777778
The field covered an area of about 20 km2, with crossroads stretched between the villages of Breitenfeld in the west, Seehausen in the east, Podelwitz in the north and Wiederitzsch in the south. The marshy Lober stream flowed behind Podelwitz, which ran from Schladitzer See west of the village. The Swedish army was drawn up in the open field just south of Podelwitz.

Geographic entities mentioned:
surface_form: Schladitzer See
instance_of: Lake
countries: Germany
coordinates: lat: 51.440277777778
lon: 12.338055555556
Lagan Canal. The Lagan Canal was a canal built to connect Belfast to Lough Neagh. The first section, which is a river navigation, was opened in 1763, and linked Belfast to Lisburn. The second section from Lisburn to Lough Neagh includes a small amount of river navigation, but was largely built as a canal.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
In the 1820s and 1830s, there was competition on short-haul traffic from the road network, but it was hoped that the construction of the Ulster Canal, linking Lough Neagh to Lough Erne and the River Shannon, would create long-haul traffic.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
The population was 209 at the 2000 census. Geography. According to the United States Census Bureau, the CDP has a total area of, all land. Leota is situated on the western side of the Buffalo Ridge, the drainage divide between the Mississippi River and Missouri River systems. History. The town of Leota was named after Leota Township in which it is located.

Geographic entities mentioned:
surface_form: Buffalo Ridge
instance_of: Landform
countries: United States
coordinates: lat: 43.9802
lon: -96.0106
Its source is located 10.7 miles north of Soda Lake, California in the middle of the Carrizo Plain. The creek runs generally east and northeast to terminate just east of the South Belridge Oil Field. In years of heavy rainfall it may have been a tributary to the Kern River between Buena Vista Lake and Tulare Lake. History.

Geographic entities mentioned:
surface_form: Buena Vista Lake
instance_of: Lake
countries: United States
coordinates: lat: 35.1919
lon: -119.295
This stream was named for a 19th century pioneer in the southern San Joaquin Valley region, Chico Martinez, a mesteñero, famous as the &quot;king of the &quot;mustang runners&quot;, for his skill in herding wild horses into the corrals built for their capture, at Aguaje Mesteño (Mustang Watering Place) and other places.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Saltus, California. Saltus is an abandoned mining town in San Bernardino County in the Mojave Desert that supported salt mining and evaporating in the Bristol Dry Lake Bed. Climate. Saltus is classified as a hot desert under the Köppen climate classification. Remains.

Geographic entities mentioned:
surface_form: Bristol Dry Lake Bed
instance_of: Lake
countries: United States
coordinates: lat: 34.4622
lon: -115.6738
Buchwaldskopf. The Buchwaldskopf is a hill in the southern foothills of Mount Nickel in the Taunus near Oberjosbach, Niedernhausen in Hesse, Germany. Position. The Buchwaldskopf rises in the Eichelberger Mark as part of the Taunushauptkamm.

Geographic entities mentioned:
surface_form: buchwaldskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1775
lon: 8.3247222222222
The Buchwaldskopf is a hill in the southern foothills of Mount Nickel in the Taunus near Oberjosbach, Niedernhausen in Hesse, Germany. Position. The Buchwaldskopf rises in the Eichelberger Mark as part of the Taunushauptkamm. In the Taunus Nature Park it is located in the district of Oberjosbach of the municipality of Niedernhausen, which is situated on the south-eastern flank of the Josbach.

Geographic entities mentioned:
surface_form: buchwaldskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1775
lon: 8.3247222222222
Sloan Peak. Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk River, in the Mount Baker–Snoqualmie National Forest. The summit is situated about east of the Mountain Loop Highway.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.14972222
lon: -109.84944444
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.155013
lon: -117.293429
The summit is situated about east of the Mountain Loop Highway. Sloan Peak has been called the &quot;Matterhorn of the Cascades&quot; for its sharp, high peak, which is accentuated by its impressive local relief and its isolated position west of the Cascade crest. It is easily visible from many locations in the North Cascades.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.70166666666667
lon: -109.87138888888889
surface_form: high peak
instance_of: Mountain
countries: United States
coordinates: lat: 42.1620334
lon: -74.0801381
surface_form: matterhorn
instance_of: Mountain
countries: United States
coordinates: lat: 41.8107
lon: -115.374
surface_form: matterhorn of the cascades
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
surface_form: sloan peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
Sloan Peak. Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk River, in the Mount Baker–Snoqualmie National Forest. The summit is situated about east of the Mountain Loop Highway.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: sloan peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
Sloan Peak. Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk River, in the Mount Baker–Snoqualmie National Forest. The summit is situated about east of the Mountain Loop Highway.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
It is easily visible from many locations in the North Cascades. On both the east and southwest sides, Sloan's summit rises more than one vertical mile (1.6 km) above the valley floor in less than two horizontal miles (3.2 km). The standard route on the peak climbs the South Face and Upper West Face, but it is also known as the &quot;Corkscrew Route&quot; due to its winding nature.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Sloan Peak. Sloan Peak is a mountain in the North Cascades of Washington state. It rises about east of Everett, Washington and 12 miles southwest of Glacier Peak, one of the Cascade stratovolcanoes. It is located between the north and south forks of Sauk River, in the Mount Baker–Snoqualmie National Forest. The summit is situated about east of the Mountain Loop Highway.

Geographic entities mentioned:
surface_form: sloan peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
The total elevation gain of the route is. It involves snow and glacier climbing and some rock scrambling (class 3). Other more technical routes exist on Sloan's other faces. History. Sloan Peak was first climbed by Harry Bedal and Nels Skaar on July 30, 1921, via the Corkscrew Route. Climate. Sloan Peak is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: sloan peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.0413767
lon: -121.3402434
Blossom Market Hall opened in December 2021 by Nellie and Chris Tran. The food hall occupies a historic former Masonic lodge, which was built in 1949, and houses thirteen food stalls that offer a diverse array of cuisines. The food hall's name acknowledges purple jacaranda trees grown in the San Gabriel Valley. Background.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Geography. About to the south of Nuvsvåg is Finnmark county's tallest mountain, Loppatinden, and the large glacier Øksfjordjøkelen. About to the southwest of Nuvsvåg lies the mountain Svartfjellet and the glacier Svartfjelljøkelen. Commerce. In 2015, one fishing boat was based out of this village. Another fishing boat became inoperable due to fire, that year.

Geographic entities mentioned:
surface_form: Svartfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 70.232777777778
lon: 21.998611111111
It is currently the highest number Quebec highway. Future. In January 2020, as an option for the proposed Quebec–Lévis third link, the Quebec government proposed extending Autoroute 973 to Autoroute 20 south by tunneling underneath the Quebec hill, St. Lawrence River, and central Lévis.

Geographic entities mentioned:
surface_form: Quebec hill
instance_of: Plateau
countries: Canada
coordinates: lat: 46.772
lon: -71.302
Located in the 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-southwest of Crater Lake. It was named around 1838 after John McLoughlin, a Chief Factor for the Hudson's Bay Company.

Geographic entities mentioned:
surface_form: Rogue River Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: Crater Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Geography. The major landmark for the Rogue River Valley, Mount McLoughlin reaches an elevation of. The tallest volcano in between Mount Shasta — located to the south — and South Sister to the north, it lies in the Cascade Range, in the southern portion of the U.S. state of Oregon. Most of the volcano lies in Jackson County, though the eastern side of its base lies in Klamath County.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Around the base of the mountain, there are a number of lakes, including the Lake of the Woods and Fourmile Lake. The Upper Klamath Lake, the largest body of freshwater in the state, sits to the east of Mount McLoughlin. The Summit Lake is a small lake on the northern slope of the volcano between the Rogue River and the Klamath Basin.

Geographic entities mentioned:
surface_form: Upper Klamath Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.392222222222
lon: -121.88027777778
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Nearby features. Two nearby volcanoes closely resemble Mount McLoughlin in composition. Brown Mountain, a shield volcano with a volume of, lies to the southeast, while Pelican Butte, the most prominent shield volcano in the southern Cascades of Oregon, lies to the east. Brown Mountain has been dated to between 60,000 and 12,000 years old.

Geographic entities mentioned:
surface_form: Pelican Butte
instance_of: Mountain
countries: United States
coordinates: lat: 42.513416666667
lon: -122.14527777778
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.363333333333
lon: -122.27138888889
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570555555556
lon: -90.545833333333
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6825503
lon: -90.5990127
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.455
lon: -74.419444444444
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9158
lon: -81.7458
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.8172916
lon: -84.9341175
First detected by an American explorer Peter Skene Ogden in 1827, McLoughlin has a complex name-place history. Ogden called the volcano &quot;Mt. Sastise&quot; after the Shasta Native Americans that helped him reach the Rogue Valley; this name was later exchanged with Mount Shasta in northern California, then called &quot;Pit Mountain&quot;.

Geographic entities mentioned:
surface_form: Rogue Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.440122222222
lon: -122.92615277778
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: pit mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
The Sky Lakes Wilderness covers an area of, with a width of and a length of. Designated by the United States Congress in 1984, it stretches from Crater Lake National Park to Oregon Route 140 at the south and ranges in elevation from in the Middle Fork canyon of the Rogue River to the peak of McLoughlin.

Geographic entities mentioned:
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9382689
lon: -121.8620654
surface_form: crater lake
instance_of: Lake
countries: United States
coordinates: lat: 39.0853
lon: -106.967
On average, precipitation does not exceed at medium elevations, reaching at greater heights, most of which consists of snowfall. Around the base of the mountain, there are a number of lakes, including the Lake of the Woods and Fourmile Lake. The Upper Klamath Lake, the largest body of freshwater in the state, sits to the east of Mount McLoughlin.

Geographic entities mentioned:
surface_form: lake of the woods
instance_of: Lake
countries: United States
coordinates: lat: 41.423888888889
lon: -86.228888888889
surface_form: lake of the woods
instance_of: Lake
countries: United States
coordinates: lat: 44.1071
lon: -110.845
surface_form: lake of the woods
instance_of: Lake
countries: United States
coordinates: lat: 42.3693
lon: -122.216
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 46.08111111
lon: -95.98527778
surface_form: lake of the woods
instance_of: Lake
countries: United States
coordinates: lat: 44.3155309
lon: -75.7275923
surface_form: fourmile lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7228376
lon: -97.4879312
This formed a glacial cirque with a bowl shape on the northeastern flank. Pelican Butte reaches an elevation of, and it features gradual slopes. Adjacent to Klamath Lake, it has a greater volume than McLoughlin at, and it is made up of basaltic andesite.

Geographic entities mentioned:
surface_form: pelican butte
instance_of: Mountain
countries: United States
coordinates: lat: 42.513416666667
lon: -122.14527777778
Pelican Butte reaches an elevation of, and it features gradual slopes. Adjacent to Klamath Lake, it has a greater volume than McLoughlin at, and it is made up of basaltic andesite. Like Brown Mountain, Pelican Butte has a cinder cone on the top of its summit, in addition to a glacial cirque and ravine that were excavated on its northeastern side.

Geographic entities mentioned:
surface_form: pelican butte
instance_of: Mountain
countries: United States
coordinates: lat: 42.513416666667
lon: -122.14527777778
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.363333333333
lon: -122.27138888889
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.570555555556
lon: -90.545833333333
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6825503
lon: -90.5990127
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.455
lon: -74.419444444444
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9158
lon: -81.7458
surface_form: brown mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.8172916
lon: -84.9341175
Like Brown Mountain, Pelican Butte has a cinder cone on the top of its summit, in addition to a glacial cirque and ravine that were excavated on its northeastern side. These eroded areas exhibit pyroclastic rock in a matrix with lava flows, suggesting that blocky and ʻaʻā lavas formed an outer shell around Pelican Butte's fragmented interior.

Geographic entities mentioned:
surface_form: pelican butte
instance_of: Mountain
countries: United States
coordinates: lat: 42.513416666667
lon: -122.14527777778
The Upper Klamath Lake, the largest body of freshwater in the state, sits to the east of Mount McLoughlin. The Summit Lake is a small lake on the northern slope of the volcano between the Rogue River and the Klamath Basin. The Big Butte Creek, a tributary of the Rogue River, drains the northwestern part of McLoughlin, while the Little Butte Creek is fed by the southern flanks. Ecology.

Geographic entities mentioned:
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 38.249
lon: -80.437
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 47.055833333333
lon: -123.10333333333
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 42.769444444444
lon: -75.202222222222
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 39.598611
lon: -105.644167
surface_form: summit lake
instance_of: Body of water
countries: United States
coordinates: lat: 61.766
lon: -149.321
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 63.13888889
lon: -145.55
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 43.99722222
lon: -95.85833333
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 42.860833333333
lon: -74.848888888889
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.12583333
lon: -94.82111111
surface_form: summit lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3744511
lon: -89.2071679
surface_form: summit lake
instance_of: Body of water
countries: United States
coordinates: lat: 60.6313
lon: -149.5085
Future activity. Mount McLoughlin's main volcanic cone has not erupted during the Holocene, with the last production of lava flows taking place between 30,000 and 20,000 years ago. The volcano is not currently monitored for activity or deformation. The closest seismic monitoring stations lie to the south near Mount Shasta and the Medicine Lake Volcano. Human history.

Geographic entities mentioned:
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 45.00644
lon: -93.41997
surface_form: medicine lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9841655
lon: -97.3519987
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Mount McLoughlin. Mount McLoughlin is a dormant steep-sided stratovolcano, or composite volcano, in the Cascade Range of southern Oregon, United States. Located in the Sky Lakes Wilderness, it is one of the volcanic peaks in the Cascade Volcanic Arc, within the High Cascades sector.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
The mountain can also be skied. Geography. The major landmark for the Rogue River Valley, Mount McLoughlin reaches an elevation of. The tallest volcano in between Mount Shasta — located to the south — and South Sister to the north, it lies in the Cascade Range, in the southern portion of the U.S. state of Oregon.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
state of Oregon. Most of the volcano lies in Jackson County, though the eastern side of its base lies in Klamath County. It is the sixth tallest peak in Oregon, but despite its height, Mount McLoughlin only has a volume of. The volcano includes the Wilámxa Tip and Máalsi Tip peaks, which occur on its flanks at elevations of
, respectively. It can be seen from the Interstate 5 and U.S.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Ecology. About 20 tree species can be found throughout Mount McLoughlin's surroundings, including Pacific yew at low elevations, mountain hemlock, whitebark pine, and subalpine fir at higher elevations, and lodgepole pine and red fir throughout. Other plant species include shrubs, wildflowers, junipers, heather, columbine, kinnikinnick, huckleberry, chinquapins, grouse huckleberry, and bearberry.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Fish species include Chinook salmon, rainbow trout, Coho salmon, Pacific lamprey, and coastal cutthroat trout. Geology. Little was known about Mount McLoughlin's geology until the 1970s. Much of what is known today comes from LeRoy Maynard of the center for Volcanology at the University of Oregon.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Formed towards the end of the Pleistocene Epoch, these mountains are underlain by more ancient volcanoes that subsided due to parallel north–south faulting in the surrounding region. Like other Cascade volcanoes, Mount McLoughlin was fed by magma chambers produced by the subduction of the Juan de Fuca tectonic plate under the western edge of the North American tectonic plate.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
The volcano displays a lack of snow during the summer season. Nearby features. Two nearby volcanoes closely resemble Mount McLoughlin in composition. Brown Mountain, a shield volcano with a volume of, lies to the southeast, while Pelican Butte, the most prominent shield volcano in the southern Cascades of Oregon, lies to the east.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Eruptive history. Mount McLoughlin underwent at least three distinct eruptive phases. Early activity at Mount McLoughlin was explosive, and it yielded tephra and pyroclastic rock that built about a third of the overall volume. These eruptions also yielded lava flows, but they only occurred on the lower flanks.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
The entire third stage is thought to have happened after the last Pleistocene glaciers in the area had melted, due to a general lack of weathering and fresh appearance of the solidified lava. The freshest lava flows at Mount McLoughlin occur on the southern and western flanks of the mountain, and they are thought to be between 30,000 and 20,000 years old. Future activity.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Future activity. Mount McLoughlin's main volcanic cone has not erupted during the Holocene, with the last production of lava flows taking place between 30,000 and 20,000 years ago. The volcano is not currently monitored for activity or deformation. The closest seismic monitoring stations lie to the south near Mount Shasta and the Medicine Lake Volcano. Human history.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
Ogden called the volcano &quot;Mt. Sastise&quot; after the Shasta Native Americans that helped him reach the Rogue Valley; this name was later exchanged with Mount Shasta in northern California, then called &quot;Pit Mountain&quot;. To local residents, Mount McLoughlin's English name was Mount Pitt, though it came to be referred to by other names including Mt. John Quincy Adams, Mt.

Geographic entities mentioned:
surface_form: mount mcloughlin
instance_of: Mountain
countries: United States
coordinates: lat: 42.444472222222
lon: -122.31561111111
surface_form: mt. madison
instance_of: Mountain
countries: United States
coordinates: lat: 44.328333333333
lon: -71.278333333333
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 44.1945
lon: -71.3887
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 48.6006
lon: -113.722
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6525
lon: -110.836
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
surface_form: snowy butte
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount simpson
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 39.4853
lon: -106.537