Sarmila/GeoWiki-Features huggingface dataset:
Another possibility is the cone formed under an expansion of the Mount Edziza ice cap during the Younger Dryas between 12,900 and 11,600 years ago or during a more recent glacial advance. Argon–argon dating of glassy pillow lava from Tennena Cone has yielded ages of 0.011 ± 0.033 million years and 0.005 ± 0.033 million years, but further work is required to improve the precision of these ages.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Argon–argon dating of glassy pillow lava from Tennena Cone has yielded ages of 0.011 ± 0.033 million years and 0.005 ± 0.033 million years, but further work is required to improve the precision of these ages. Since its eruption under glacial ice, Tennena Cone has been modified by glacial erosion.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Since its eruption under glacial ice, Tennena Cone has been modified by glacial erosion. This includes the steepening of its flanks and the formation of its long summit ridge, which is covered with morainal detritus. The degree of glacial erosion and the deposition of morainal detritus on the summit ridge of Tennena Cone suggest the volcano was overlain by significantly thick ice.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Miocene comendite, trachyte, alkali basalt and minor sparsely porphyritic hawaiite of the Armadillo Formation underlie the Nido Formation; they are in the form of lava flows, flow breccias, pumice, ash flows and agglutinate. The oldest geological formation underlying Tennena Cone is the Raspberry Formation, which consists of Miocene alkali basalt and minor hawaiite and mugearite.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
These features include ordinary pillow lavas and vertically oriented, distended pillow lavas, as well as massive non-pillowed lavas and interbedded gravelly sands and poorly consolidated sandstone. The subglacially emplaced lavas erupted from Tennena Cone are also of geological significance because they can be traced more than away from the vent area.

Geographic entities mentioned:
surface_form: tennena cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
Plavni (;) is a village in Reni Raion in the southern Ukrainian oblast of Odesa. It belongs to Reni urban hromada, one of the hromadas of Ukraine. Plavni is situated on the western bank of Lake Yalpuh. Until 18 July 2020, Plavni belonged to Reni Raion. The raion was abolished in July 2020 as part of the administrative reform of Ukraine, which reduced the number of raions of Odesa Oblast to seven.

Geographic entities mentioned:
surface_form: Lake Yalpuh
instance_of: Lake
countries: Ukraine
coordinates: lat: 45.416666666667
lon: 28.616666666667
It has almost no full-time residents, being populated mostly during the summer. Mamaia lies on a strip of land in length and only in width, between the Black Sea and Lake Siutghiol. The beach season is at its best between mid-June and early September, when average daytime temperatures range between. The water stays warm until mid-autumn.

Geographic entities mentioned:
surface_form: Lake Siutghiol
instance_of: Lake
countries: Romania
coordinates: lat: 44.246388888889
lon: 28.6
It is the transition ecoregion from the Great Plains prairie and steppe temperate grasslands in the south to the Taiga biome forests in the north. In central Asia the forest steppe ecotone is found in ecoregions in the mountains of the Iranian Plateau, in Iran, Afghanistan, and Balochistan.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Quevesere. Quevesere (possibly from Aymara &quot;q'iwisiña&quot; to fight, &quot;-ri&quot; a suffix, &quot;fighter&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Ocongate District. It lies south of the peak of Alcamarinayoc and northwest of Chumpe.

Geographic entities mentioned:
surface_form: Alcamarinayoc
instance_of: Mountain
countries: Peru
coordinates: lat: -13.69972222
lon: -71.09472222
surface_form: chumpe
instance_of: Mountain
countries: Peru
coordinates: lat: -13.72555556
lon: -71.08138889
surface_form: chumpe
instance_of: Mountain
countries: Peru
coordinates: lat: -11.73333333
lon: -76.04166667
Quevesere. Quevesere (possibly from Aymara &quot;q'iwisiña&quot; to fight, &quot;-ri&quot; a suffix, &quot;fighter&quot;) is a mountain in the Vilcanota mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Quispicanchi Province, Ocongate District. It lies south of the peak of Alcamarinayoc and northwest of Chumpe.

Geographic entities mentioned:
surface_form: quevesere
instance_of: Mountain
countries: Peru
coordinates: lat: -13.7225
lon: -71.0961
The forest reserve is situated in Central Uganda and is protected by the National Forestry Authority under the National Forest and Tree Planting Act. The forest reserve was gazetted in 1932 to protect Lake Victoria and the environment. Settings and structure. The forest reserve lies on the northeast side of Entebbe Bay, south of Kampala City.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Agassiz-Rosedale Bridge. The Agassiz–Rosedale Bridge is a cantilever truss bridge across the Fraser River in the Fraser Valley region of southwestern British Columbia. Linking Agassiz with the south shore, the two-lane bridge carrying BC Highway 9 is by road about west of Hope, east of Vancouver, and east of Abbotsford. Former ferries.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Ch'apini. Ch'apini (Aymara &quot;jach'a&quot; big, &quot;ch'api&quot; thorn, &quot;-ni&quot; a suffix, &quot;the big one with thorns&quot;, also spelled &quot;Chapini&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Ch'apini lies at the Luribay River, southeast of Jach'a Ch'apini (&quot;big Ch'apini&quot;).

Geographic entities mentioned:
surface_form: Jach'a Ch'apini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.12888889
lon: -67.57111111
surface_form: ch'apini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13888889
lon: -67.5625
surface_form: ch'apini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13888889
lon: -67.5625
Ch'apini. Ch'apini (Aymara &quot;jach'a&quot; big, &quot;ch'api&quot; thorn, &quot;-ni&quot; a suffix, &quot;the big one with thorns&quot;, also spelled &quot;Chapini&quot;) is a mountain in the Bolivian Andes. It is located in the La Paz Department, Loayza Province, Luribay Municipality. Ch'apini lies at the Luribay River, southeast of Jach'a Ch'apini (&quot;big Ch'apini&quot;).

Geographic entities mentioned:
surface_form: ch'apini
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.13888889
lon: -67.5625
With of land, it is the state's largest-sized city. Denver is the most populated city. Physical geography. Colorado Springs is located in the Pikes Peak area in El Paso County, along the Front Range a forty-mile corridor from the city up to Fort Carson. At the edge of the southern Rocky Mountains, it is bordered by State, National Forest Service, and Bureau of Land Management land.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
At the edge of the southern Rocky Mountains, it is bordered by State, National Forest Service, and Bureau of Land Management land. North of the city is the Palmer Divide, the plains and grasslands are to the east, and Pueblo and high desert lands lie to the south. The city was founded at the confluence of Monument Creek with Fountain Creek of the Arkansas River watershed.

Geographic entities mentioned:
surface_form: high desert
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
The mountains have been quarried for limestone. Scenic Pennsylvanian rock formations are found at Garden of the Gods. The natural gap between the sandstone Austin Bluffs is Templeton Gap, and a few westernmost portions of the city are on the east escarpment's slope of the Southern Rocky Mountains section adjacent to the Colorado Piedmont, separated by the Fall line of the Front Range. Land use.

Geographic entities mentioned:
surface_form: Templeton Gap
instance_of: Landform
countries: United States
coordinates: lat: 38.8844
lon: -104.805
After a failed assassination attempt on Genghis Khan, 100 of his men fled and nearly starved to death. While on the run these men swore allegiance to one another and remarkably these men included Buddhists, Christians, Muslims, and animists who worshiped the Eternal Blue Sky and the God Mountain of Burkhan Khaldun. Defender of Religions.

Geographic entities mentioned:
surface_form: Burkhan Khaldun
instance_of: Mountain
countries: Mongolia
coordinates: lat: 48.783333333333
lon: 109.16666666667
Pamela Pack. Pamela Shanti Pack (born circa 1976) is an American rock climber who specializes in off-width crack climbing. She has made &quot;close to 80 first ascents&quot;, many of them in Vedauwoo, Wyoming. Pack grew up in Middlebury, Vermont as the daughter of poet Robert Pack. As a child she was a competitive gymnast, but stopped after getting a stress fracture in her spine.

Geographic entities mentioned:
surface_form: Vedauwoo
instance_of: Landform
countries: United States
coordinates: lat: 41.155
lon: -105.38166666667
She was formerly an ice climber, until a 2006 attack of compartment syndrome forced her to choose a climbing style that involved less gripping. She works as a cartographer, and lives in Missoula, Montana. In 2009, &quot;Climbing&quot; magazine gave her their Golden Piton award for establishing &quot;Gabriel&quot;, a 5.13 crack route on Angels Landing in Zion National Park.

Geographic entities mentioned:
surface_form: Angels Landing
instance_of: Mountain
countries: United States
coordinates: lat: 37.2694
lon: -112.948
Tom Teršek. Tom Teršek (born 6 September 2006) is a Slovenian javelin thrower. He won the gold medal at the 2024 World Athletics U20 Championships at the age of 17 years-old. Early life. He is from Triglav in Kranj, in the Upper Carniola region of Slovenia. He attended Carniola High School.

Geographic entities mentioned:
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
She is in a Prince cover band called Princess with her friend Gretchen Lieberum. Personal life. Rudolph has been in a relationship with filmmaker Paul Thomas Anderson since 2001. They live in the San Fernando Valley with their four children.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The spire is striate. The color of the shell is light yellowish brown, variegated by darker striations, and faint revolving lines or rows of spots, often indistinctly lighter-banded in the middle. Distribution. This species occurs in the Indian Ocean off Madagascar, in the Bay of Bengal, and in the Pacific Ocean off the Philippines and Indonesia; in the South China Sea.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The apogee of Xochicalco came after the fall of Teotihuacan and it has been speculated that Xochicalco may have played a part in the fall of the Teotihuacan empire. The architecture and iconography of Xochicalco show affinities with Teotihuacan, the Maya area, and the Matlatzinca culture of the Toluca Valley. Today the residents of the nearby village of Cuentepec speak Nahuatl.

Geographic entities mentioned:
surface_form: Toluca Valley
instance_of: Valley
countries: Mexico
coordinates: lat: 19.2865
lon: -99.5595
Black-capped woodland warbler. The black-capped woodland warbler (&quot;Phylloscopus herberti&quot;) is a leaf warbler species in the family Phylloscopidae; it was formerly placed in the &quot;Old World warbler&quot; assemblage. It is native to the Western High Plateau and Bioko. Its natural habitat is subtropical or tropical moist montane forests.

Geographic entities mentioned:
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Valley Relics Museum. Valley Relics Museum is a museum located in the San Fernando Valley of Los Angeles. The &quot;LA Weekly&quot; named the Valley Relics Museum one of its 2017 winners of &quot;Best Of L.A.: Arts & Entertainment&quot;. Founded in 2013 by Tommy Gelinas, Valley Relics Museum's collection spans from the 1800s to the present day, with over 20,000 items.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Mishodaghi Mount. Mishoodaghi Mount is a mountain range in East Azerbaijan province of Iran. It is located between Tasouj, Marand, and Shabestar cities. Mishodaghi peak has several peaks including: &quot;Ali-Alamdar&quot; (highest peak 3155 m), &quot;Falak daghi&quot;, &quot;Kooseh-Baba&quot;, and &quot;Uzoun-Bel&quot;. Yam Ski Resort is located in northern foothills of Mishodaghi. Mountain peaks.

Geographic entities mentioned:
surface_form: mishodaghi mount
instance_of: Mountain
countries: Iran
coordinates: lat: 38.26666667
lon: 45.7
Mishodaghi Mount. Mishoodaghi Mount is a mountain range in East Azerbaijan province of Iran. It is located between Tasouj, Marand, and Shabestar cities. Mishodaghi peak has several peaks including: &quot;Ali-Alamdar&quot; (highest peak 3155 m), &quot;Falak daghi&quot;, &quot;Kooseh-Baba&quot;, and &quot;Uzoun-Bel&quot;. Yam Ski Resort is located in northern foothills of Mishodaghi. Mountain peaks.

Geographic entities mentioned:
surface_form: mishoodaghi mount
instance_of: Mountain
countries: Iran
coordinates: lat: 38.26666667
lon: 45.7
It was first listed as a CDP prior to the 2020 census. The CDP is in the southeastern corner of Blair County, in the southeastern corner of North Woodbury Township. It is in the valley of Clover Creek, a northward-flowing tributary of the Frankstown Branch Juniata River, and sits at the western foot of Tussey Mountain. It is southeast of Martinsburg and southeast of Roaring Spring. Education.

Geographic entities mentioned:
surface_form: Tussey Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.21
lon: -78.332222222222
Halvfarryggen Ridge. Halvfarryggen Ridge () is a broad snow-covered ridge separating the Ekström Ice Shelf and the Jelbart Ice Shelf, on the coast of Queen Maud Land, Antarctica. It was first mapped by the Norwegian–British–Swedish Antarctic Expedition, 1949–52.

Geographic entities mentioned:
surface_form: halvfarryggen
instance_of: Mountain
coordinates: lat: -71.1667
lon: -6.66667
It was first mapped by the Norwegian–British–Swedish Antarctic Expedition, 1949–52. They referred to the feature as &quot;Isrygg&quot; (ice ridge), but it was subsequently named Halvfarryggen (the half way ridge) by the Sixth Norwegian Antarctic Expedition, 1956–60.

Geographic entities mentioned:
surface_form: halvfarryggen
instance_of: Mountain
coordinates: lat: -71.1667
lon: -6.66667
The division was given the primary role of securing around of territory (the designated security zone) in north-eastern Bosnia within the NDH. The security zone encompassed the Posavina, Semberija and Majevica regions between the Sava, Bosna, Drina and Spreča rivers.

Geographic entities mentioned:
surface_form: Semberija
instance_of: Landform
countries: Bosnia and Herzegovina
coordinates: lat: 44.80083333
lon: 19.21361111
It is a tributary of the Baker River, part of the Pemigewasset River and Merrimack River watersheds. The river rises on the southernmost slopes of Mount Moosilauke in the town of Woodstock. Flowing south, it quickly enters the town of Warren and crosses twice under Route 118 before joining the main stem of the Baker.

Geographic entities mentioned:
surface_form: Mount Moosilauke
instance_of: Mountain
countries: United States
coordinates: lat: 44.024511111111
lon: -71.830916666667
Cinder Cone and the Fantastic Lava Beds. Cinder Cone is a cinder cone volcano in Lassen Volcanic National Park within the United States. It is located about northeast of Lassen Peak and provides an excellent view of Brokeoff Mountain, Lassen Peak, and Chaos Crags. The cone was built to a height of above the surrounding area and spread ash over.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
surface_form: Chaos Crags
instance_of: Mountain
countries: United States
coordinates: lat: 40.524166666667
lon: -121.52111111111
Then, like many cinder cones, it was snuffed out when several basalt lava flows erupted from its base. These flows, called the Fantastic Lava Beds, spread northeast and southwest, and dammed creeks, first creating Snag Lake on the south and then Butte Lake to the north. Butte Lake is fed by water from Snag Lake seeping through the lava beds.

Geographic entities mentioned:
surface_form: Snag Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
The volcano lies in the northeastern corner of Lassen Volcanic National Park. Nearby Snag Lake formed when lava known as the Painted Dunes flows dammed the Grassy Creek stream, which is fed by water from the central plateau of the national park area. Water from this lake feeds Butte Lake, located to the north.

Geographic entities mentioned:
surface_form: Snag Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
These flows, called the Fantastic Lava Beds, spread northeast and southwest, and dammed creeks, first creating Snag Lake on the south and then Butte Lake to the north. Butte Lake is fed by water from Snag Lake seeping through the lava beds. Nobles Emigrant Trail goes around Snag Lake and follows the edge of the lava beds.

Geographic entities mentioned:
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
Geography. Cinder Cone lies in Lassen and Shasta counties, in Northern California, within the United States. Located southwest of Butte Lake and southeast of Prospect Peak (which dwarfs Cinder Cone), it is also sometimes referred to as Black Butte or Cinder Butte. The volcano lies in the northeastern corner of Lassen Volcanic National Park.

Geographic entities mentioned:
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.9044
lon: -111.855
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 35.88222222
lon: -115.72083333
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 39.7267
lon: -122.872
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 41.3663
lon: -122.348
surface_form: prospect peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.8881
lon: -110.503
surface_form: black butte
instance_of: Mountain
countries: United States
coordinates: lat: 44.3997
lon: -121.635
Nearby Snag Lake formed when lava known as the Painted Dunes flows dammed the Grassy Creek stream, which is fed by water from the central plateau of the national park area. Water from this lake feeds Butte Lake, located to the north. Butte Lake is the sole remaining fragment of a much larger body of water filled with lava during Cinder Cone's eruptive period.

Geographic entities mentioned:
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
Water from this lake feeds Butte Lake, located to the north. Butte Lake is the sole remaining fragment of a much larger body of water filled with lava during Cinder Cone's eruptive period. Diatomite sediment, formed from the aggregation of diatoms on the lake's floor, run along the edges of the Fantastic Lava Beds and mark the margins of this former lake. Description and geology.

Geographic entities mentioned:
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Description and geology. Cinder Cone is a -high volcanic cone of loose scoria. The youngest mafic volcano in the Lassen volcanic center, it is surrounded by unvegetated block lava and has concentric craters at its summit, which have diameters of and.

Geographic entities mentioned:
surface_form: lassen volcanic center
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Cinder Cone and the Fantastic Lava Beds. Cinder Cone is a cinder cone volcano in Lassen Volcanic National Park within the United States. It is located about northeast of Lassen Peak and provides an excellent view of Brokeoff Mountain, Lassen Peak, and Chaos Crags. The cone was built to a height of above the surrounding area and spread ash over.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Cinder Cone and the Fantastic Lava Beds. Cinder Cone is a cinder cone volcano in Lassen Volcanic National Park within the United States. It is located about northeast of Lassen Peak and provides an excellent view of Brokeoff Mountain, Lassen Peak, and Chaos Crags. The cone was built to a height of above the surrounding area and spread ash over.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Nobles Emigrant Trail goes around Snag Lake and follows the edge of the lava beds. Its age has been controversial since the 1870s, when many people thought it was only a few decades old. Later, the cone and associated lava flows were thought to have formed about 1700 or during a 300-year- long series of eruptions ending in 1851. Recent studies by U.S.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Geography. Cinder Cone lies in Lassen and Shasta counties, in Northern California, within the United States. Located southwest of Butte Lake and southeast of Prospect Peak (which dwarfs Cinder Cone), it is also sometimes referred to as Black Butte or Cinder Butte. The volcano lies in the northeastern corner of Lassen Volcanic National Park.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Description and geology. Cinder Cone is a -high volcanic cone of loose scoria. The youngest mafic volcano in the Lassen volcanic center, it is surrounded by unvegetated block lava and has concentric craters at its summit, which have diameters of and.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
The youngest mafic volcano in the Lassen volcanic center, it is surrounded by unvegetated block lava and has concentric craters at its summit, which have diameters of and. Cinder Cone comprises five basaltic andesite and andesite lava flows, and it also has two cinder cone volcanoes, with two scoria cones, the first of which was mostly destroyed by lava flows from its base.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Cinder Cone comprises five basaltic andesite and andesite lava flows, and it also has two cinder cone volcanoes, with two scoria cones, the first of which was mostly destroyed by lava flows from its base. Cinder cone volcanoes are typically monogenetic, meaning that they only undergo one eruptive period before ceasing activity forever.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
The summit of Cinder Cone has a crater with a double rim ([//upload.wikimedia.org/wikipedia/commons/1/1a/Cinder_Cone_crater_in_Lassen_VNP-1200px.JPG photo]), probably created by two different phases of one eruptive period. The cone also has a widespread ash deposit identifiable for from the cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
When Cinder Cone formed, the magma feeding the eruption changed composition, shifting from basaltic andesite to andesite before returning to basaltic andesite with increased titanium content. While basaltic andesites are volcanic rocks containing 53 to 57% silica, andesites are those containing 57 to 63% silica.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
The early group of volcanic deposits at Cinder Cone, which have relatively little titanium, include older scoria cone, the Old Bench flow, the two Painted Dunes flows, and the lower part of the widespread ash layer. The second group, erupted later and comparatively rich in titanium, consists of the large, younger scoria cone, the upper part of the ash layer, and the two Fantastic Lava Beds flows.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
At the Old Bench and Painted Dunes lava flows, the volcanic ash is brightly oxidized because it interacted with the lava flows when they were still hot. It shares its compositional group with the Fantastic Lava Beds flows, which represent the last flows erupted at Cinder Cone. Ultimately, the eruptive sequence at Cinder Cone took place over the course of several months.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
It shares its compositional group with the Fantastic Lava Beds flows, which represent the last flows erupted at Cinder Cone. Ultimately, the eruptive sequence at Cinder Cone took place over the course of several months. An unusual characteristic of the Fantastic Lava Beds is the presence of anomalous quartz crystal xenocrysts (foreign bodies in igneous rock).

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
During the early 1870s, medical doctor and amateur scientist H. W. Harkness from San Francisco, California, visited the Cinder Cone area. Intrigued by the &quot;apparent youthfulness&quot; of the area's volcanic landmarks, he observed several features to argue that Cinder Cone was only about 25 years old.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
A number of other people reached out to Harkness about seeing volcanic activity in Lassen in about 1851, such as O. M. Wozencraft, which led Harkness to think that Cinder Cone had erupted recently. Though there were multiple reports of eruptive activity near Lassen in Northern California newspapers during the 1850s, the details remain inconsistent.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
The first such report, which was published in the August 21, 1850, edition of the &quot;Daily Pacific News&quot; (a San Francisco newspaper), cited an unnamed observer who claimed to have seen &quot;burning lava still running down the sides&quot; at Cinder Cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Early geologic studies. The first geologist to study Cinder Cone was Joseph Diller. One of the first USGS scientists to study volcanoes, Diller took careful notes on Cinder Cone and interviewed many Native Americans and European trappers and settlers inhabiting the Lassen region during 1850, none of whom remembered volcanic activity there.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Aware of an &quot;emigrant road&quot; (the Nobles Emigrant Trail), which had been utilized by settlers coming to California in the early 1850s, that passes close to the base of Cinder Cone, he interviewed a number of people who &quot;crossed the trail&quot; in 1853.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
They noted that a large, solitary willow bush (&quot;Salix scouleriana&quot;) near the summit of Cinder Cone had not been destroyed by any eruptive activity. The bush is still alive and has not been altered much since.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Diller therefore speculated that the explosive eruption had occurred between about 1675 and 1700 and that the younger, quiet eruption was &quot;certainly&quot; sometime before 1840. On May 6, 1907, both Cinder Cone and Lassen Peak were designated national monuments, administered by the National Forest Service.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
On the basis of other studies done at Cinder Cone, Finch thought (1) that there had been at least five separate lava-flow events, as suggested by crude, experimental magnetic measurements; (2) that the youngest lava flow was extruded in 1851, accepting Harkness' (1875) historical &quot;evidence&quot; and ignoring Diller's interviews and conclusions; and (3) that there had been at least two distinct explosive eruptions of the cone.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Through new field and laboratory work and by reinterpreting data from previous studies, USGS scientists have shown that the entire eruptive sequence at Cinder Cone represents a single continuous event.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Because the orientation of the Earth's magnetic field in northern California during the 1850s is well known and is different from the remnant magnetizations at Cinder Cone, the lava flows there could not have been erupted in 1850 or 1852.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Also, there are no discernible differences in the magnetic orientation recorded by any of the Cinder Cone lava flows, and so the flows had to be extruded during an interval of less than 50 years. Although paleomagnetic evidence can be used to rule out the 1850s as the age of Cinder Cone, it does not provide an actual age for its eruption.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
The series of eruptions that produced the volcanic deposits at Cinder Cone were complex and are by no means completely understood. However, the new studies done by USGS scientists refute the purported accounts of an eruption in the early 1850s and confirm Diller's (1891, 1893) interpretation that Cinder Cone erupted in the latter half of the 17th century.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Butte Lake is fed by water from Snag Lake seeping through the lava beds. Nobles Emigrant Trail goes around Snag Lake and follows the edge of the lava beds. Its age has been controversial since the 1870s, when many people thought it was only a few decades old.

Geographic entities mentioned:
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
Haukefjellet. Haukefjellet is a mountain in southern Norway. Haukefjellet is located on the boundary between Lærdal in Sogn og Fjordane and

Geographic entities mentioned:
surface_form: haukefjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.04972222
lon: 8.24
Mettur Dam. The Mettur Dam is one of the largest dams in India and also the largest in Tamil Nadu, located across the river Kaveri where it enters the plains. Built in 1934, it took nine years to complete. Maximum height and width of the dam are 214 and 171 feet, respectively. The dam receives inflows from its own catchment area, Kabini Dam and Krishna Raja Sagara Dams located in Karnataka.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
History. It was constructed under the supervision of an Irish engineer, Vincent Hart, who was also the chief engineer of the project. It took nine years and the effort of 17,000 men to complete the dam project. After the construction was complete, Mettur Dam over Kaveri became the largest dam in the world. The funds were provided from the taxes collected in the Madras Presidency.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Still a young scientist, this position proved to be very productive for him and allowed Sthokman to publish more than 20 articles devoted to the investigation of flow and mixture processes in the Caspian Sea. Shtokman finished his PhD in 1938.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Mirower See. Mirower See is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. At an elevation of, its surface area is.

Geographic entities mentioned:
surface_form: mirower see
instance_of: Lake
countries: Germany
coordinates: lat: 53.281388888889
lon: 12.807222222222
Phillipps Peak. Phillipps Peak is located north of Crowsnest Pass and straddles the Continental Divide marking the Alberta-British Columbia border. It was named in 1915 after Michael Phillipps who in 1873 was the first white man to cross Crowsnest Pass. It is the lower west peak of Mount Tecumseh. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: phillipps peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.66305555555556
lon: -114.65722222222222
Phillipps Peak. Phillipps Peak is located north of Crowsnest Pass and straddles the Continental Divide marking the Alberta-British Columbia border. It was named in 1915 after Michael Phillipps who in 1873 was the first white man to cross Crowsnest Pass. It is the lower west peak of Mount Tecumseh. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: phillipps peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.66305555555556
lon: -114.65722222222222
__NOTOC__
Geology. Phillipps Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks thick, wide and long over younger rock of the cretaceous period during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: phillipps peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.66305555555556
lon: -114.65722222222222
Climate. Based on the Köppen climate classification, Phillipps Peak has an alpine subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: phillipps peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.66305555555556
lon: -114.65722222222222
Phillipps Peak. Phillipps Peak is located north of Crowsnest Pass and straddles the Continental Divide marking the Alberta-British Columbia border. It was named in 1915 after Michael Phillipps who in 1873 was the first white man to cross Crowsnest Pass. It is the lower west peak of Mount Tecumseh. __NOTOC__
Geology.

Geographic entities mentioned:
surface_form: mount tecumseh
instance_of: Mountain
countries: Canada
coordinates: lat: 49.665277777777774
lon: -114.64611111111111
Homeland. They were first described, during the reign of Emperor Ba'eda Maryam (r. 1468–1478), as inhabiting the region between Enderta and Lake Ashenge (in Tigray Province), neighboring the Afars of the vassal Dankali Sultanate on the east. The area was described by Francisco Álvares during his stay in Ethiopia as being five days' journey (ca.

Geographic entities mentioned:
surface_form: Lake Ashenge
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12.580555555556
lon: 39.5
Ioni. Lake Ioni (), also known as Yonai (), (, &quot;Yunin&quot;) is a large freshwater lake in Chukotsky District, Chukotka Autonomous Okrug, Russia. It has an area of. Currently there are no permanent settlements on the shores of the lake, but there are remains of Stone Age dwellings. Reindeer herders occasionally visit the area, as well as fishermen.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: yunin
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
Ioni. Lake Ioni (), also known as Yonai (), (, &quot;Yunin&quot;) is a large freshwater lake in Chukotsky District, Chukotka Autonomous Okrug, Russia. It has an area of. Currently there are no permanent settlements on the shores of the lake, but there are remains of Stone Age dwellings. Reindeer herders occasionally visit the area, as well as fishermen.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The nearest inhabited place is Lorino, located away. Geography. The lake is located in the center of the Chukotka Peninsula, south of Kolyuchin Bay. Ioni is the largest lake in its district. It lies in the Mechigmen-Kolyuchin basin, a large intermontane basin of the western part of the Chukotka Mountains. high Mount Ioni rises to the NW of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Ioni is the largest lake in its district. It lies in the Mechigmen-Kolyuchin basin, a large intermontane basin of the western part of the Chukotka Mountains. high Mount Ioni rises to the NW of the lake. Ioni is fed by at least five streams originating in the adjacent mountains. The largest is the Priozernaya that flows into the lake from the northeast. River Yonaypilgyn is the outflow of the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
high Mount Ioni rises to the NW of the lake. Ioni is fed by at least five streams originating in the adjacent mountains. The largest is the Priozernaya that flows into the lake from the northeast. River Yonaypilgyn is the outflow of the lake. Ioni is connected by the Yuniwei channel with river Ioniveyem, part of the drainage basin of Kolyuchin Bay.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Ioni is fed by at least five streams originating in the adjacent mountains. The largest is the Priozernaya that flows into the lake from the northeast. River Yonaypilgyn is the outflow of the lake. Ioni is connected by the Yuniwei channel with river Ioniveyem, part of the drainage basin of Kolyuchin Bay. The lake freezes in the first half of September and stays under ice until June.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake freezes in the first half of September and stays under ice until June. Flora and fauna. The area surrounding Ioni has low mountain tundra vegetation. The banks of the lake are gently sloping and on the eastern side swampy with hummocks and thermokarst pools. There are no aquatic plants. Anadromous Dolly Varden char is common in the lake.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The banks of the lake are gently sloping and on the eastern side swampy with hummocks and thermokarst pools. There are no aquatic plants. Anadromous Dolly Varden char is common in the lake. Other fish species include sardine cisco, Siberian whitefish, broad whitefish, burbot, Arctic grayling, as well as Alaska blackfish in shallow thermokarst ponds.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Other fish species include sardine cisco, Siberian whitefish, broad whitefish, burbot, Arctic grayling, as well as Alaska blackfish in shallow thermokarst ponds. Migratory birds, such as the snow goose, sandhill crane and emperor goose pass through the area and stop at the lake. But owing to the short relatively warm season Ioni is not a suitable place for nesting.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Ioni. Lake Ioni (), also known as Yonai (), (, &quot;Yunin&quot;) is a large freshwater lake in Chukotsky District, Chukotka Autonomous Okrug, Russia. It has an area of. Currently there are no permanent settlements on the shores of the lake, but there are remains of Stone Age dwellings. Reindeer herders occasionally visit the area, as well as fishermen.

Geographic entities mentioned:
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
The lake freezes in the first half of September and stays under ice until June. Flora and fauna. The area surrounding Ioni has low mountain tundra vegetation. The banks of the lake are gently sloping and on the eastern side swampy with hummocks and thermokarst pools. There are no aquatic plants. Anadromous Dolly Varden char is common in the lake.

Geographic entities mentioned:
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
Other fish species include sardine cisco, Siberian whitefish, broad whitefish, burbot, Arctic grayling, as well as Alaska blackfish in shallow thermokarst ponds. Migratory birds, such as the snow goose, sandhill crane and emperor goose pass through the area and stop at the lake. But owing to the short relatively warm season Ioni is not a suitable place for nesting.

Geographic entities mentioned:
surface_form: ioni
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 65.9
lon: -173.65
It marked the debut for Francis who was later to emerge as one of the most popular British writers of the interwar years. The story is based on the construction of the Elan Valley Reservoirs, a subject that he later returned to more successfully in &quot;The House Under the Water&quot; in 1932. &quot;Undergrowth&quot; was published in 1913 by Martin Secker.

Geographic entities mentioned:
surface_form: Elan Valley Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 52.27222222222222
lon: -3.688888888888889
Nether Lochaber is made up of Onich and North Ballachulish. The community council covers these settlements as well as small settlements including Inchree, Bunree, Corrychurrachan and Keppanach; other features include Glen Righ Forest and the hills Beinn na Gucaig, Mam na Gualainn, Doire Bàn and Tom Meadhoin.

Geographic entities mentioned:
surface_form: Beinn na Gucaig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.738953
lon: -5.1702509
surface_form: Mam na Gualainn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.716007
lon: -5.0816824
Okunevo, Republic of Buryatia. Okunevo () is a rural locality (a settlement) in Bauntovsky District, Republic of Buryatia, Russia. The population was 6 as of 2010. There are 4 streets. Geography. Okunevo is located by lake Kapylyushi, in the Tsipikan river valley, 113 km northwest of Bagdarin (the district's administrative centre) by road.

Geographic entities mentioned:
surface_form: Kapylyushi
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 54.823055555556
lon: 112.26138888889