Sarmila/GeoWiki-Features huggingface dataset:
Diablo emerge from their burrows to seek mates. The Mt. Diablo Interpretive Association offers guided hikes to observe the migration. The &quot;March of the Tarantulas&quot; can begin as early as August and last through October. Every year since 1964, the Pearl Harbor survivors and their families have memorialized Pearl Harbor Day by relighting the historic Beacon atop Mount Diablo's summit.

Geographic entities mentioned:
surface_form: mount diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
surface_form: mount diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
&quot;Save Mount Diablo&quot; sponsors many spring and fall schedules of events on the mountain, Spring on Diablo and Autumn on Diablo, as well as many other special events, including its anniversary event, Moonlight on the Mountain; Four Days Diablo, a trip on the Diablo Trail; the Mount Diablo Challenge, an annual hill climb to the summit with more than 1,100 cyclists each October; and the Mount Diablo Trail Adventure, combined 10k and half-marathon hikes and runs.

Geographic entities mentioned:
surface_form: mount diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Course record. The course record for the Mount Diablo climb currently stands at 43 minutes, 33 seconds, set on October 5, 2008, by Nate English (ZteaM) 4 days after breaking his thumb in a bike accident. He broke the 44 minutes, 58 seconds record, set in 2004 by former professional cyclist Greg Drake (Webcor Cycling Team) of Redwood City, California.

Geographic entities mentioned:
surface_form: mount diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Notable people. James &quot;Grizzly&quot; Adams was a frequent visitor and resident on Mount Diablo in the mid-1850s. Robert Walter &quot;Bob&quot; Jones, the first professional baseball player from Contra Costa County, was born in the &quot;Jones House&quot; in Irish Canyon in 1889, an acquisition project of Save Mount Diablo.

Geographic entities mentioned:
surface_form: mount diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
As of December 2007, the organization recognizes 38 specific Diablo parks and preserves. The State Park adjoins park lands of the East Bay Regional Park District, including Morgan Territory Regional Preserve, Brushy Peak Regional Preserve, Vasco Caves Regional Preserve, and Round Valley Regional Preserve.

Geographic entities mentioned:
surface_form: round valley
instance_of: Valley
countries: United States
coordinates: lat: 35.15166667
lon: -115.36194444
Chwarel y Fan is the county top of the historic county of Monmouthshire, and is also the highest point in the current local government area of Monmouthshire. The summit is on a thin ridge and is crowned by a cairn. On the other sides of the valleys: to the west is Pen Twyn Mawr and to the east is Black Mountain.

Geographic entities mentioned:
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.8814
lon: -3.70848
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6
lon: -5.98
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.008333333333
lon: -3.0847222222222
Chwarel y Fan. Chwarel y Fan is a peak in the Black Mountains in south-eastern Wales. It is the highest rise on the long ridge which extends southeastwards from Rhos Dirion. The ridge continues southeastwards to the lesser summit of Bal-Mawr whose top is adorned by a trig point at above sea level. About southeast along the ridge is the lesser top of Bal-Bach at a height of just over.

Geographic entities mentioned:
surface_form: chwarel y fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.958231
lon: -3.080984
About southeast along the ridge is the lesser top of Bal-Bach at a height of just over. Chwarel y Fan is the county top of the historic county of Monmouthshire, and is also the highest point in the current local government area of Monmouthshire. The summit is on a thin ridge and is crowned by a cairn.

Geographic entities mentioned:
surface_form: chwarel y fan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.958231
lon: -3.080984
In the Iron Age the &quot;Celtic&quot; La Tène culture centred on Western Germany and Eastern France, and Germany has produced many major finds of Celtic art like the elite burials at Reinheim and Hochdorf, and &quot;oppida&quot; towns like Glauberg, Manching and Heuneburg.

Geographic entities mentioned:
surface_form: Glauberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.305556
lon: 9.008611
Her grandfather, Robert Hogg, was a conductor and a founder of the first orchestra at Balboa Theatre in downtown San Diego. Her brother, Jeff Lenhart, is a competitive sailor on U.S. sailing teams. For 60 years, on her birthday, she has ridden the Giant Dipper Roller Coaster in Mission Beach to commemorate the day. Lenhart lives in Pacific Beach, a coastal neighborhood of San Diego.

Geographic entities mentioned:
surface_form: Pacific Beach
instance_of: Landform
countries: United States
coordinates: lat: 32.797827777778
lon: -117.24031388889
The South Volcanic Zone is the most volcanically active region in Chile, and produces around one eruption per year. Its largest historical eruption was at Quizapu Crater, located to from the north side of Cerro Azul's summit, and its most active volcanoes are Llaima and Villarrica. Calabozos is a ring-shaped caldera by wide, with an elevation of.

Geographic entities mentioned:
surface_form: Llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: cerro azul
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: quizapu
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
Under its northeast edge, Calabozos is cut by a north–south trending segment of sedimentary rock that includes gypsiferous and carbonates. Calabozos is similar in age to Cerro Azul and Descabezado Grande, and its eruptions may correspond to past activity at both volcanoes. Eruption products of very similar composition (including mafic andesite, agglutinates, and dacite) make up the volcanoes.

Geographic entities mentioned:
surface_form: Descabezado Grande
instance_of: Mountain
countries: Chile
coordinates: lat: -35.583333333333
lon: -70.75
surface_form: cerro azul
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: descabezado grande
instance_of: Mountain
countries: Chile
coordinates: lat: -35.583333333333
lon: -70.75
There is also a similarity in size (all are between 40 and 70 cubic kilometers in volume). The volcano appears to be part of a north–south trending group of rhyolitic, silicic Quaternary volcanoes (including Puelche volcanic field, Laguna del Maule, and Volcán Domuyo) that veers off the north-northeast direction of the rest of the Andes.

Geographic entities mentioned:
surface_form: Puelche volcanic field
instance_of: Mountain
coordinates: lat: -35.78
lon: -70.48
surface_form: laguna del maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
surface_form: laguna del maule
instance_of: Mountain
countries: Chile
coordinates: lat: -36.0675
lon: -70.5225
The team's stated aim is to &quot;reduce eruption-caused fatalities and economic losses in developing countries&quot;. Made up of various USGS offices such as the Cascades Volcano Observatory (CVO), responsible for monitoring Mount St. Helens, the team has equipment to monitor any volcano, allowing the timely prediction of volcanic eruptions and the evacuation of nearby homes.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Threats and preparedness. Calabozos is in the South Volcanic Zone, which contains potentially deadly and active volcanoes such as Mount Hudson, Llaima, and Villarrica. Villarrica and Llaima together have more than 80 reported episodes of volcanism since 1558, and at least 40 South Volcanic Zone volcanoes have had Holocene-age eruptions.

Geographic entities mentioned:
surface_form: llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: mount hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
The last eruption occurred during Holocene time, and produced a dacitic lava flow (in volume) that extends for. Cerro Colorado, with an elevation of, forms another cone in the complex. Towards the center of the caldera, hot springs including Cajon Los Calabozos and Baños de Llolli are present.

Geographic entities mentioned:
surface_form: cerro colorado
instance_of: Mountain
countries: Chile
coordinates: lat: -22.59233333
lon: -67.92216667
Temperature is also variable, typically registering 25 degrees Celsius during the summer, but dropping below freezing at high elevations (above). Vegetation is rare in the area. The 1932 eruption of Cerro Azul's Quizapu Crater reduced much of the land to a pumice desert. Above, vegetation becomes even more sparse. Eruptive history.

Geographic entities mentioned:
surface_form: cerro azul
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
surface_form: quizapu
instance_of: Mountain
countries: Chile
coordinates: lat: -35.653333333333
lon: -70.760833333333
Calabozos. Calabozos is a Holocene caldera in central Chile's Maule Region (7th Region). Part of the Chilean Andes' volcanic segment, it is considered a member of the Southern Volcanic Zone (SVZ), one of the three distinct volcanic belts of South America.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Calabozos. Calabozos is a Holocene caldera in central Chile's Maule Region (7th Region). Part of the Chilean Andes' volcanic segment, it is considered a member of the Southern Volcanic Zone (SVZ), one of the three distinct volcanic belts of South America.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
This most active section of the Andes runs along central Chile's western edge, and includes more than 70 of Chile's stratovolcanoes and volcanic fields. Calabozos lies in an extremely remote area of poorly glaciated mountains. Calabozos and the majority of the Andean volcanoes formed from the subduction of the oceanic Nazca Plate under the continental South American continental lithosphere.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Calabozos lies in an extremely remote area of poorly glaciated mountains. Calabozos and the majority of the Andean volcanoes formed from the subduction of the oceanic Nazca Plate under the continental South American continental lithosphere. The caldera is in a transitional region between thick and thin lithosphere, and is probably supplied by a pool of andesitic and rhyolitic magma.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
It sits on a historic bed of volcanic and plutonic sedimentary rock (rock formed within the Earth) that in turn sits on top of a layer of merged sedimentary and metamorphic rock. Calabozos is responsible for the huge Loma Seca Tuff, a body of material to in volume.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Activity from the caldera has produced many other stratovolcanoes to form a complex volcano. Geography and structure. Calabozos lies in central Chile's Maule Region, near Curicó and Talca, on the western Andes. This is an area of poorly glaciated mountains that is not permanently populated. There are no roads, and it is only accessible via horse or on foot.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
surface_form: maule
instance_of: Lake
countries: Chile
coordinates: lat: -36.055
lon: -70.5
This is an area of poorly glaciated mountains that is not permanently populated. There are no roads, and it is only accessible via horse or on foot. Calabozos is part of the South Volcanic Zone, which runs along the western edge of central Chile and extends south, jumping the border to continue its course in Argentina.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Its largest historical eruption was at Quizapu Crater, located to from the north side of Cerro Azul's summit, and its most active volcanoes are Llaima and Villarrica. Calabozos is a ring-shaped caldera by wide, with an elevation of. Volcanoes have been formed by eruptions in the crater.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Cerro Colorado, with an elevation of, forms another cone in the complex. Towards the center of the caldera, hot springs including Cajon Los Calabozos and Baños de Llolli are present. The springs are as old as 0.3 mya, and may have formed directly after Calabozos's second eruption as a result of uplift caused by re-occurring activity in the caldera.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
The springs are as old as 0.3 mya, and may have formed directly after Calabozos's second eruption as a result of uplift caused by re-occurring activity in the caldera. The vents occur in two clusters, Colorado and Puesto Calabozos, and are located along the margin of a fault at the southwestern edge of the caldera. Hildreth &quot;et al&quot;.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
The vents occur in two clusters, Colorado and Puesto Calabozos, and are located along the margin of a fault at the southwestern edge of the caldera. Hildreth &quot;et al&quot;. (1983) evaluated that Calabozos could potentially be useful for the harvesting of geothermal energy, and exploratory holes have been drilled. Geology.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Under its northeast edge, Calabozos is cut by a north–south trending segment of sedimentary rock that includes gypsiferous and carbonates. Calabozos is similar in age to Cerro Azul and Descabezado Grande, and its eruptions may correspond to past activity at both volcanoes. Eruption products of very similar composition (including mafic andesite, agglutinates, and dacite) make up the volcanoes.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
The directional formation of this belt corresponds to the fold-and-thrust movement of the nearby Malargüe fault, which formed in the Tertiary and remained active until the early Pliocene or late Miocene. This may suggest that Calabozos' activity is more dependent on local processes than subduction of the Nazca Plate. Geologic record.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
The most recent volcanic phase began about 4 mya, producing largely andesitic eruptions. A series of eruptions built up a broad plateau of lava, and extended over the area where Calabozos now lies. Locally, this plateau was composed of mafic andesite with olivine, which over time gathered to form to thick layers.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
A series of eruptions built up a broad plateau of lava, and extended over the area where Calabozos now lies. Locally, this plateau was composed of mafic andesite with olivine, which over time gathered to form to thick layers. Nearby volcanoes sit on top of two mya lavas that formed during this period, while the Loma Seca Tuff lies atop andesitic deposits from Descabezado Grande. Composition.

Geographic entities mentioned:
surface_form: descabezado grande
instance_of: Mountain
countries: Chile
coordinates: lat: -35.583333333333
lon: -70.75
Composition. Calabozos lies between two different types of volcanism—to its north, andesite and rhyolite are the primary constituents of lava while its southern neighbors are composed of more mafic andesite and basalt. It is mainly basaltic andesite and rhyodacite that make up Calabozos, forming a calcalkilic suite rich with potassium.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Above, vegetation becomes even more sparse. Eruptive history. During the late Pleistocene, Calabozos erupted tuff composed primarily of rhyodacite and dacite. Three distinct eruptions have taken place within the last million years. The sheets of remaining ash left over from all of the eruptions together range from to in volume and are known as the Loma Seca Tuff.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
They appear to have been erupted in pulses, and continue for hundreds of meters. Deposition was continuous except for one interruption, which can be seen at proximity to the caldera, where the layers are replaced by thin, nonwelded sheets of lava. Another zone of nonwelded material, about and near Cajon Los Calabozos, underwent no erosion, suggesting that activity stopped, then began again.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Villarrica and Llaima together have more than 80 reported episodes of volcanism since 1558, and at least 40 South Volcanic Zone volcanoes have had Holocene-age eruptions. After the 2010 Maule earthquake, vertical movement took place along the caldera margins. Its remoteness means that Calabozos poses little threat to humans, but if necessary relief efforts could be orchestrated.

Geographic entities mentioned:
surface_form: calabozos
instance_of: Mountain
countries: Chile
coordinates: lat: -35.5
lon: -70.5
Its remoteness means that Calabozos poses little threat to humans, but if necessary relief efforts could be orchestrated. The Volcanic Disaster Assistance Program (VDAP) formed in response to the famous eruption of Nevado del Ruiz in Colombia and saved lives following the 1991 eruption of Mount Hudson in Chile by organizing evacuations.

Geographic entities mentioned:
surface_form: mount hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
A rival scheme, the Yorkshire & Glasgow Union Railway, left the ECML at Thirsk, crossed the Pennines to Hawes, then Kirkby Stephen, Appleby and so reached Clifton. The Leeds and Carlisle left the Leeds Northern Railway near Headingley and passed through Wharfedale to Hawes and the Eden Valley.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
It has had six major expansions and the facility is now at or of floor space. Buffalo Stamping is currently in the process of adding 30,000 square feet on to the structure. The plant is located on an site at the Eastern end of Lake Erie near the city of Buffalo, New York. The facility processes over 1,700 tons of steel each day and ships an average of 100 rail cars of parts manufactured daily.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Between 1878 and 1885, British naturalist Henry Walter Bates named several species of North American beetle for Flohr, including
In 1884, Flohr accompanied American zoologist Edward Drinker Cope in Mexico. Cope wrote:I am indebted to my excellent friend, Dr.

Geographic entities mentioned:
surface_form: lake Xochimilco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.285
lon: -99.102
Rib Mountain (Ontario). Rib Mountain is a mountain that straddles the border between the municipalities of Latchford, Timiskaming District and Temagami, Nipissing District in Northeastern Ontario, Canada. It divides Friday Lake on the east and Rib Lake on the west.

Geographic entities mentioned:
surface_form: rib mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 47.211003
lon: -79.667328
The seventh stage was also split into two parts. The first part was an individual mountain time trial to the Monte Terminillo, won by Valetti. He jumped to fourth place in the general classification, while Del Cancia was still in the pink jersey. In the ninth stage, Valetti escaped together with Giordano Cottur, and they won almost five minutes on all the other riders.

Geographic entities mentioned:
surface_form: Monte Terminillo
instance_of: Mountain
countries: Italy
coordinates: lat: 42.47327
lon: 12.99732
It is located in the Junín Region, Yauli Province, Morococha District, and in the Lima Region, Huarochirí Province, Chicla District. Yuraqqucha lies northwest of a lake named Waqraqucha, the Antikuna mountain pass and the peak of Antikuna. Anta Q'asa, Sillaqaqa, Inka Kancha and Pukaqucha are situated west, southwest and northwest of Yuraqqucha.

Geographic entities mentioned:
surface_form: Antikuna
instance_of: Mountain
countries: Peru
coordinates: lat: -11.58472222
lon: -76.18055556
surface_form: waqraqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.71333333
lon: -75.70083333
Yuraqqucha lies northwest of a lake named Waqraqucha, the Antikuna mountain pass and the peak of Antikuna. Anta Q'asa, Sillaqaqa, Inka Kancha and Pukaqucha are situated west, southwest and northwest of Yuraqqucha. The mountain is named after a little lake south of it. It lies in the Chicla District at.

Geographic entities mentioned:
surface_form: Anta Q'asa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5697
lon: -76.255
surface_form: Sillaqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5697
lon: -76.2372
surface_form: Inka Kancha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5825
lon: -76.2408
Yuraqqucha (Lima-Junín). Yuraqqucha (Quechua &quot;yuraq&quot; white, &quot;qucha&quot; lake, &quot;white lake&quot;, Hispanicized spelling &quot;Yuraccocha&quot;) is a mountain in the Andes of Peru, about high. It is located in the Junín Region, Yauli Province, Morococha District, and in the Lima Region, Huarochirí Province, Chicla District.

Geographic entities mentioned:
surface_form: yuraqqucha (lima-junín)
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5739
lon: -76.2186
surface_form: junín
instance_of: Lake
countries: Peru
coordinates: lat: -11.0201
lon: -76.1075
Continuing on flat roads for until it reaches the North York Moors at Great Ayton. Following the Eskdale for the final the route crosses the River Esk four times before reaching its eastern trailhead at a junction with Route 1 on the outskirts of Whitby. This section includes several steep climbs and descents, some of them are on off-road tracks.

Geographic entities mentioned:
surface_form: Eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
Dungan language. Dungan (or) is a Sinitic language spoken primarily in the Chu Valley of southeastern Kazakhstan and northern Kyrgyzstan. It is the native language of the Dungan people, a Hui subgroup that fled Qing China in the 19th century. It evolved from the Central Plains Mandarin variety spoken in Gansu and Shaanxi.

Geographic entities mentioned:
surface_form: Chu Valley
instance_of: Valley
countries: Kyrgyzstan
Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 42.8333
lon: 75.2833
Such rippled patterns result from increased cell growth near the edges of the leaf, which causes its thin, planar surface to buckle as it assumes the conformation with the lowest energy state. Infraspecific taxa. In 2009, a cultivar from Lake Poso in Sulawesi was named &quot;Nepenthes maxima&quot; 'Lake Poso'. In 2016, this taxon was described as a species in its own right, &quot;N. minima&quot;.

Geographic entities mentioned:
surface_form: Lake Poso
instance_of: Lake
countries: Indonesia
coordinates: lat: -1.97955
lon: 120.6601
Geography. Egnell Creek originates on the west flank of the massive Level Mountain shield volcano, near the headwaters of the Little Tahltan River and Dudidontu River, and about south of Meszah Peak, the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of Level Mountain. The creek flows southwest through Level Mountain's high and relatively barren lava plateau.

Geographic entities mentioned:
surface_form: Dudidontu River
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.78281
lon: -131.98693
surface_form: Meszah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4786
lon: -131.437
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Egnell Creek. Egnell Creek is a tributary of the Hackett River in northwest part of the province of British Columbia, Canada. It flows generally southwest about to join the Hackett River near the Hackett's confluence with the Sheslay River, which in turn is a tributary of the Inklin River, the main southeast fork of the Taku River.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Egnell Creek. Egnell Creek is a tributary of the Hackett River in northwest part of the province of British Columbia, Canada. It flows generally southwest about to join the Hackett River near the Hackett's confluence with the Sheslay River, which in turn is a tributary of the Inklin River, the main southeast fork of the Taku River.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Mount Egnell is located near the creek's mouth, as is the historic locality known as Egnell or Sheslay, once a telegraph station on the Yukon Telegraph Line. Egnell Creek's watershed covers, and its mean annual discharge is estimated at. The mouth of Egnell Creek is located about northwest of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about southeast of Whitehorse, Yukon.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Mount Egnell is located near the creek's mouth, as is the historic locality known as Egnell or Sheslay, once a telegraph station on the Yukon Telegraph Line. Egnell Creek's watershed covers, and its mean annual discharge is estimated at. The mouth of Egnell Creek is located about northwest of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about southeast of Whitehorse, Yukon.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The mouth of Egnell Creek is located about northwest of Telegraph Creek, British Columbia, about east of Juneau, Alaska, and about southeast of Whitehorse, Yukon. Egnell Creek's watershed's land cover is classified as 46.1% shrubland, 32.4% barren, 24.5% conifer forest, 12.8% mixed forest, and small amounts of other cover.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Egnell Creek's watershed's land cover is classified as 46.1% shrubland, 32.4% barren, 24.5% conifer forest, 12.8% mixed forest, and small amounts of other cover. Egnell Creek is in the traditional territory of the Tlingit Taku River Tlingit First Nation and the Tahltan people. Geography.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
The creek flows southwest through Level Mountain's high and relatively barren lava plateau. After about Egnell Creek enters a steep canyon carved into the escarpment on Level Mountain's western side. Below the escarpment the landscape is dominated by coniferous forests.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
After about Egnell Creek enters a steep canyon carved into the escarpment on Level Mountain's western side. Below the escarpment the landscape is dominated by coniferous forests. Egnell Creek continues southwest until it reaches the Hackett River at the former settlement of Sheslay, south of Mount Egnell and about east of the Hackett and Sheslay River confluence. History.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
History. Egnell Creek is named for Albert Egnell, a miner, fur trader, and Hudson's Bay Company (HBC) employee. In the 1880s Egnell was an employee of Rufus Sylvester, who had come to the region during the Omineca Gold Rush. In 1888 the HBC bought from Sylvester the trading post that became known as Liard Post or Lower Post, located about northeast of Egnell Creek.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
In the 1880s Egnell was an employee of Rufus Sylvester, who had come to the region during the Omineca Gold Rush. In 1888 the HBC bought from Sylvester the trading post that became known as Liard Post or Lower Post, located about northeast of Egnell Creek. At this time Egnell joined the HBC and managed Liard Post.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
At this time Egnell joined the HBC and managed Liard Post. During the 1890s Egnell conducted various operations in northwestern British Columbia, sometimes for the HBC, sometimes independently. Albert Egnell was prospecting in the area near Egnell Creek in the 1880s. It was probably around this time that Egnell Creek and Mount Egnell were named.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
During the 1890s Egnell conducted various operations in northwestern British Columbia, sometimes for the HBC, sometimes independently. Albert Egnell was prospecting in the area near Egnell Creek in the 1880s. It was probably around this time that Egnell Creek and Mount Egnell were named. The HBC built a trading post sometime before 1898 near the mouth of Egnell Creek.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Albert Egnell was prospecting in the area near Egnell Creek in the 1880s. It was probably around this time that Egnell Creek and Mount Egnell were named. The HBC built a trading post sometime before 1898 near the mouth of Egnell Creek. This post, first known as Tackoo, then Egnell or Egnell Post, was abandoned by the HBC in the late 1890s.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
Egnell died on 22 June 1900, from an accidental gun shot to his leg five days earlier. He was buried at Liard Post. In 1891–1892, the HBC constructed a trail from the mouth of Egnell Creek, near the junction of the Sheslay and Hackett rivers to the southwestern slope of Level Mountain.

Geographic entities mentioned:
surface_form: egnell creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.26629
lon: -131.80375
At this time Egnell joined the HBC and managed Liard Post. During the 1890s Egnell conducted various operations in northwestern British Columbia, sometimes for the HBC, sometimes independently. Albert Egnell was prospecting in the area near Egnell Creek in the 1880s. It was probably around this time that Egnell Creek and Mount Egnell were named.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
This post, first known as Tackoo, then Egnell or Egnell Post, was abandoned by the HBC in the late 1890s. In the early 1900s its cabin served as a repair station for the long Yukon Telegraph Line, which extended from Ashcroft, British Columbia to Dawson City, Yukon. Subsequently, a number of buildings and a mission house were constructed and the name changed to Sheslay.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Since then, the range of &quot;A. belizianus&quot; has been elaborated upon. Starting in the Mullins River of central Belize, it extends south to tributaries of Lake Izabal, in Guatemala and northern Honduras. Specific biotope preferences are unknown, as are diet and sympatry, though there is the possibility that records have been made while &quot;A. belizianus&quot; was grouped under &quot;A.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
Its altitude varies between 2,600 and 3,700 meters above sea level. The park is seven km long, three km wide with an area of 1,867 hectares. It is one of the most important natural areas of the Federal District, protecting much of the Sierra de las Cruces mountain range and represents about 15% of the Valley of Mexico. The climate of the park is relatively cold and damp due to its altitude.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Mount Unabetsu. is a Quaternary stratovolcano. Its summit is. It is located on Hokkaido's Shiretoko Peninsula on the border of Shari in Shari District, Abashiri and Shibetsu in Shibetsu District, Nemuro. Geology. The mountain is made mainly of andesite and basalt.

Geographic entities mentioned:
surface_form: mount unabetsu
instance_of: Mountain
countries: Japan
coordinates: lat: 43.87361111
lon: 144.86555556
Henry J. Wheeler Farm. The Henry J. Wheeler Farm is a farmstead in Murray, Utah, United States, that is one of the few remaining late 19th century farmsteads in the Salt Lake Valley that has not been lost to expanding housing developments of metropolitan Salt Lake City. It has been listed on the National Register of Historic Places since 1976. Description.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Lake Newell. Lake Newell is a large man-made reservoir in southern Alberta, Canada. It is located south of the city of Brooks, east of Veteran Highway. The reservoir was filled in 1914 through the construction of the Bassano Dam. It was named after T.H. Newell, a landowner and irrigation expert. The County of Newell is in turn named after the lake.

Geographic entities mentioned:
surface_form: lake newell
instance_of: Lake
countries: Canada
coordinates: lat: 50.4344
lon: -111.935
It empties into the Bow River after flowing through Rolling Hills Lake, an extension of the lake, filled when the dam was raised in 1939. Irrigation canals are built between the lake and the Bow River, as well as in the agricultural area north and east of the lake. Kinbrook Island Provincial Park was established in the eastern shore of the lake on November 14, 1951.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Work initiated in 1924 progressed rapidly, although initially, there were almost no white-and-red-white markings along the planned trail route (earlier trails were mainly marked with one or two colored stripes). Exceptions were the sections from Czantoria to Stożek (in the Silesian Beskids), from Żabnica through Pilsko to the (in the Żywiec Beskids), and from to Rytro (in the Beskid Sądecki).

Geographic entities mentioned:
surface_form: Czantoria
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 49.678804166667
lon: 18.804709444444
surface_form: Stożek
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.605277777778
lon: 18.823055555556
surface_form: Pilsko
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.527222222222
lon: 19.318333333333
By 1927, after completing the segment from Rabka to Krynica, the Polish Tatra Society reported the completion of the entire Main Western Beskid trail. However, this announcement was premature as significant additions to the trail were still made in 1928 – between Stożek and Barania Góra in the Silesian Beskids and between and in the Gorce Mountains.

Geographic entities mentioned:
surface_form: Barania Góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.611388888889
lon: 19.010555555556
According to Sosnowski's recommendations in the &quot;Guide to the Western Beskids&quot; from 1926, traversing the route from Ustroń to Krynica should take from 9 to 12 days. However, the author included in this time the opportunity to explore the Babia Góra area, traverse the optional Pieniny trail, and omitted some sections of the main trail. Main Eastern Beskid Trail.

Geographic entities mentioned:
surface_form: Babia Góra
instance_of: Mountain
countries: Poland
Slovakia
coordinates: lat: 49.573055555556
lon: 19.530555555556
It then followed the ridge towards the south to Stożek (with the) and further to. On this last peak, it changed direction to the east. It continued through towards Barania Góra, passing the along the way. Next, it descended into the Soła valley, reaching Węgierska Górka. After crossing the river, it began its route in the Żywiec Beskids. It led through to, where it reached the state border.

Geographic entities mentioned:
surface_form: Barania Góra
instance_of: Mountain
countries: Poland
coordinates: lat: 49.611388888889
lon: 19.010555555556
Next, it descended into the Soła valley, reaching Węgierska Górka. After crossing the river, it began its route in the Żywiec Beskids. It led through to, where it reached the state border. It then climbed to Pilsko (;), leaving the summit on the Czechoslovak side, and then descended to the with a variant path towards the. It then continuously followed the border through the and.

Geographic entities mentioned:
surface_form: Pilsko
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.527222222222
lon: 19.318333333333
From there, through the ridge of Polica, the trail descended about 1,200 m to the (villages Bystra, Jordanów, Rabka). In Rabka, the trail entered the Gorce Mountains. It climbed to the highest peak in the range, Turbacz, via. It led through the southwestern ridge of – through,, and – then descended to Krościenko. Upon entering the Beskid Sądecki, the trail led to and the highest peak of the range.

Geographic entities mentioned:
surface_form: Turbacz
instance_of: Mountain
countries: Poland
coordinates: lat: 49.5428
lon: 20.1039
Continuing along the border watershed ridge, it passed through,,, and, reaching. Here, it turned northwest, leaving the Polish-Czechoslovak border. The trail crossed the ridge with the culmination at Mała Rawka, and after passing the village of Wetlina, ascended and in the range. It then descended to Berehy Górne and ascended again to Połonina Caryńska, culminating at.

Geographic entities mentioned:
surface_form: Mała Rawka
instance_of: Mountain
countries: Poland
coordinates: lat: 49.1092
lon: 22.5736
The trail crossed the ridge with the culmination at Mała Rawka, and after passing the village of Wetlina, ascended and in the range. It then descended to Berehy Górne and ascended again to Połonina Caryńska, culminating at. From Ustrzyki Górne, the trail led to the highest peak of the Western Bieszczady, Tarnica, and then Halicz and, where it returned to the state border.

Geographic entities mentioned:
surface_form: Połonina Caryńska
instance_of: Mountain
countries: Poland
coordinates: lat: 49.13792
lon: 22.60368
It then descended to Berehy Górne and ascended again to Połonina Caryńska, culminating at. From Ustrzyki Górne, the trail led to the highest peak of the Western Bieszczady, Tarnica, and then Halicz and, where it returned to the state border. Finally, it passed through,, and, reaching Uzhok Pass near Sianky. Eastern section.

Geographic entities mentioned:
surface_form: Tarnica
instance_of: Mountain
countries: Poland
coordinates: lat: 49.069444444444
lon: 22.738055555556
Finally, it passed through,, and, reaching Uzhok Pass near Sianky. Eastern section. In Sianky, near the railway station, began the section of the trail originally called the Eastern Beskid Trail. This section led through the to the village of Karpatske, then onward to, Chresty,, and, reaching the highest peak of the – Pikui.

Geographic entities mentioned:
surface_form: Pikui
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.829444444444
lon: 23.000833333333
There, it left the state border, turning north and then northeast towards the village of Lavochne. The trail then ascended Trostian, where there was the, and from there it descended to Slavske via Przysłup. The red-marked trail then led to and, continuing along the state border to, which separates the Bieszczady from the Gorgany mountains.

Geographic entities mentioned:
surface_form: Trostian
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.856666666667
lon: 23.392055555556
Next, it passed through Foreszczenka to the. From there, the trail ascended back to the main watershed ridge – to Hoverla (the highest peak of the Polish Eastern Carpathians and the entire trail) – and continued through Breskul,, Turkul, Rebra, Menchul, and Dzembronia to the last peak in the range, Pip Ivan.

Geographic entities mentioned:
surface_form: Hoverla
instance_of: Mountain
countries: Ukraine
Soviet Union
Austria-Hungary
coordinates: lat: 48.16027777777778
lon: 24.5
surface_form: Breskul
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.151111111111
lon: 24.511944444444
surface_form: Turkul
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.123888888889
lon: 24.531111111111
surface_form: Menchul
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.091666666667
lon: 24.595833333333
From there, it led through the village southwards to the mouth of the stream valley, where it turned southwest. This valley trail followed the white-blue-white &quot;Beskidenverein&quot; markers to Czantoria. In 1930, shortly after the opening of the new Ustroń Polana railway station, the Polish Tatra Society marked a new trail to Czantoria from the vicinity of this station, passing through.

Geographic entities mentioned:
surface_form: Czantoria
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 49.678804166667
lon: 18.804709444444
Instead of turning north towards Czantoria and Ustroń from Kiczory near Stożek, as originally planned, the trail coming from Barania Góra was redesigned along the route of the Czechoslovak red trail (known as the &quot;Bezručova stezka&quot;) in a southwest direction. The path first descended 550 m to the Olza valley at Písek, then ascended back to Girova.

Geographic entities mentioned:
surface_form: Girova
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.531666666667
lon: 18.799722222222
These mountain huts included those at Girova (Polish Tatra Society), Skalka (&quot;Beskidenverein&quot;), under along with Dolní Lomná (Polish Tatra Society), (private, &quot;Beskidenverein&quot;), (Polish Tatra Society), under Lipí (private), and at (Polish Tatra Society). Variant trails.

Geographic entities mentioned:
surface_form: Girova
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.531666666667
lon: 18.799722222222
These include the circular in the Żywiec Beskids (from Barania Gora through Zwardoń, to Pilsko – bypassing Wegierska Gorka; 1928–1929), the Podhale trail (from Polica through to Stare Wierchy in the Gorce Mountains – bypassing Jordanów and Rabka; 1930–1932), and the Pieniny Trail (bypassing Krościenko and Przehyba, 1926–1928).

Geographic entities mentioned:
surface_form: Podhale
instance_of: Valley
countries: Poland
coordinates: lat: 49.4793
lon: 20.0291
Chef and owner Yoshinari Ichise opened the original Ramen Ryoma in Portland in 2016. Plans to open a restaurant on Southwest Morrison Street in downtown Portland were announced in 2021. California. The first San Diego location opened in Kearny Mesa in 2018. The restaurant also operates in Pacific Beach (since late 2018) and Hillcrest. The Kearny Mesa location closed in early 2021. Reception.

Geographic entities mentioned:
surface_form: Pacific Beach
instance_of: Landform
countries: United States
coordinates: lat: 32.797827777778
lon: -117.24031388889
The source is the confluence of Somo Creek and Little Somo Creek in the unincorporated community of Clifford. The river flows approximately east-southeast, and terminates in Lake Mohawksin. Prior to the existence of Lake Mohawksin, which floods the confluence, the Somo flowed into the Tomahawk, just a few hundred yards up stream of its confluence with the Wisconsin.

Geographic entities mentioned:
surface_form: Lake Mohawksin
instance_of: Lake
countries: United States
coordinates: lat: 45.4753
lon: -89.7589
Cutler Reservoir. Cutler Reservoir is a reservoir located in Cache Valley in the U.S. state of Utah. It is an impoundment on the Bear River built for irrigation, flood control, and water supply. The concrete gravity-arch Cutler Dam, built in 1927, is located in easternmost Box Elder County, although the reservoir is almost entirely in Cache County, to its east.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
The house. Upon purchasing the property, Headley found that the old Griscom home was too small and in need of extensive repairs. Headley had the house razed and built a new brick mansion overlooking Lake Iamonia. He brought in pecan and other expensive wood for the home's interior paneling and finish work. The roof was over-engineered using rafters which measured by and set every.

Geographic entities mentioned:
surface_form: Lake Iamonia
instance_of: Lake
countries: United States
coordinates: lat: 30.633119444444
lon: -84.177672222222