Sarmila/GeoWiki-Features huggingface dataset:
It is likely that crustal feedback and increased deep crustal influx of mantle-derived basalts drive increased magmatic flux. During the time of the Polan eruption on the west flank, magma output was spatially segregated with the peripheral Miño Volcano generating andesite lavas and the more central volcanos generating dacites.

Geographic entities mentioned:
surface_form: miño volcano
instance_of: Mountain
Body of water
countries: Chile
coordinates: lat: -21.183333333333
lon: -68.6
Aucanquilcha. Aucanquilcha is a massive stratovolcano located in the Antofagasta Region of northern Chile, just west of the border with Bolivia and within the Alto Loa National Reserve. Part of the Central Volcanic Zone of the Andes, the stratovolcano has the form of a ridge with a maximum height of. The volcano is embedded in a larger cluster of volcanoes known as the Aucanquilcha cluster.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Part of the Central Volcanic Zone of the Andes, the stratovolcano has the form of a ridge with a maximum height of. The volcano is embedded in a larger cluster of volcanoes known as the Aucanquilcha cluster. This cluster of volcanoes was formed in stages over eleven million years of activity with varying magma output, including lava domes and lava flows.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The volcano is embedded in a larger cluster of volcanoes known as the Aucanquilcha cluster. This cluster of volcanoes was formed in stages over eleven million years of activity with varying magma output, including lava domes and lava flows. Aucanquilcha volcano proper is formed from four units that erupted between 1.04–0.23 million years ago.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Aucanquilcha volcano proper is formed from four units that erupted between 1.04–0.23 million years ago. During the ice ages, both the principal Aucanquilcha complex and the other volcanoes of the cluster were subject to glaciation, resulting in the formation of moraines and cirques.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Systematic variations in temperature, crystal and biotite content have been recorded during the evolution of the cluster. At Aucanquilcha volcano there is some fumarolic activity, and sulfur deposits are found at the summit. Several sulfur mines lie in the complex. One mine at an altitude of was opened in 1913 and remained in use from 1950 to 1992.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
In 1986, four men were reported to be living at an altitude of, making them the highest permanent residents on Earth. Regional setting. Aucanquilcha is part of the Central Volcanic Zone (CVZ) of the Andes, a highly silicic volcanic zone in South America. The CVZ generates magmas at a rate of, one tenth of the global average of arc magma production, and lies about above the Wadati–Benioff zone.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The arc has migrated eastward towards the high Andes from the Pacific Ocean coast since the Jurassic. The arc contains andesitic volcanoes, ignimbrites and compound volcanoes and has generated over of eruption products over 28 million years. The Aucanquilcha complex lies northwest of the Altiplano–Puna volcanic complex (APVC), a local large igneous province.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The APVC is underpinned below at a depth of by a slow seismic velocity zone that has been linked to the presence of 15–25% of partial melts in the zone. The Aucanquilcha complex is much smaller volumetrically than the APVC ignimbrites, but the duration of activity and the location indicate that Aucanquilcha is a subcomponent of the APVC complex.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Such decreases may occur because of the lithostatic load imposed by the edifices on the magma chambers and the increased travel distance of the magma through the edifice. Local setting. Aucanquilcha is part of a cluster of volcanoes located between the Rio Loa and the Chile–Bolivia border. Aucanquilcha sits on top of a 2.7–3.3 mya andesite platform and rises more than over it.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Local setting. Aucanquilcha is part of a cluster of volcanoes located between the Rio Loa and the Chile–Bolivia border. Aucanquilcha sits on top of a 2.7–3.3 mya andesite platform and rises more than over it. The main volcano is composed of an east-west long chain of stratovolcanoes and has an estimated volume of. The maximum slope of the summit area is 25°.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
To the north lies the 3.3 mya old andesite Cerro Tres Monos ridge; to the west lies the east-west Cerro Polan and La Luna ridge. The volcanic cluster of which Aucanquilcha is a part contains about 19–20 volcanoes and has generated about of andesite and dacite over eleven million years.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Its volcanoes are arranged in north-south and northwestern alignments, which may indicate a rupture of the crust above shallow magma reservoirs. Aucanquilcha underwent a northwestward flank collapse, generating a debris avalanche deposit. The debris avalanche descended and ran for with an azimuth of 211°, eventually covering an area of.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Petrographically, the composition of the cluster ranges from andesite to dacite with SiO2 ranging from 62.8% to 65.7%. Andesites appear as lava flows while dacites form lava domes and dome complexes. The rocks from the main Aucanquilcha volcano are uniformly dacitic and show little evidence of temporal variation in their composition. Potassium content ranges from 1.5 to 4%.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
It is possible that solidification of magmas below the volcano insulated the feeding channels from heat loss and caused the temperatures in the system to increase. Activity waned again 2 million years ago, with magma and included crystals being drawn from depths of and forming the Aucanquilcha volcano proper.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Activity waned again 2 million years ago, with magma and included crystals being drawn from depths of and forming the Aucanquilcha volcano proper. The 10-million-year duration of activity of the Altiplano–Puna volcanic complex systems is comparable to the duration of Aucanquilcha activity.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The age of the lava flows ranges from heavily glaciated andesite flows overlying less-eroded ones to possibly postglacial lava flows that may be tens of thousands of years old. Aucanquilcha cluster. The Aucanquilcha cluster formed in four stages, each corresponding to a group. The Alconcha group, with seven volcanoes, is constructed from pyroxene, andesite and dacite and formed 11–8 mya.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Hydrothermal alteration has affected some lavas and pyroclastics from Tres Monos, and the western side has lateral and terminal moraines. The Aucanquilcha platform (3.6–2.7 mya) sits underneath the main Aucanquilcha volcano, and its lava mostly flowed north. Its southern side is a table with one hill, Cerro Campana, dated to 3.3 mya.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Its southern side is a table with one hill, Cerro Campana, dated to 3.3 mya. The platform presumably forms one third of the total volume of the Aucanquilcha cluster and may have originated from a part of the ridge of the La Luna-Polan trend, now buried beneath Aucanquilcha. Chaihuiri (2.39 mya) is a lava dome with moraines and two short lava flows; it is the youngest Polan group volcano.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The total volume of this group is, indicating a flux rate of. After the four main phases, some scoria cones of basaltic composition, including Poruñita and Luna de Tierra, formed between Aucanquilcha and Ollagüe. Aucanquilcha proper. The main Aucanquilcha volcano formed in four stages. Between 1.04–0.92 mya the bulk of the volcano formed in the &quot;Azufrera&quot; stage.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
After the four main phases, some scoria cones of basaltic composition, including Poruñita and Luna de Tierra, formed between Aucanquilcha and Ollagüe. Aucanquilcha proper. The main Aucanquilcha volcano formed in four stages. Between 1.04–0.92 mya the bulk of the volcano formed in the &quot;Azufrera&quot; stage. One lava flow toward the southwest is unusually long at.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The total volume of this stage is, indicating a flux rate of. The youngest stage, known as &quot;Angulo&quot;, lasted from 0.66 to 0.24 mya. It was centered between the Azufrera and Rodado stage edifices 0.35–0.23 mya. Most lava flows from this stage originate on a long ridge that includes Aucanquilcha's highest summit. One crater on the northeast side of the ridge fed lavas to the north.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Lava flow emissions and minor explosive activity, confined to the edifice of the volcano, are the most important risks from renewed activity. Glaciation and hydrology. The volcano is currently not glaciated despite its height, due to the aridity of the climate. The Quebrada de Chaigüire valley originates at the foot of Aucanquilcha.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The Quebrada de Chaigüire valley originates at the foot of Aucanquilcha. Some of the source springs of the Rio Loa are on Aucanquilcha and it drains the western and northwestern sides of the volcano; the eastern side drains into the Salar de Ollagüe salt pan, the northeastern into the Salar de Laguani, and the southeastern into the Salar de Carcote.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
The mine was active from 1950 to 1992. In 1977 other sulfur mines were present to the west between Cerro Polan and Cerro Gordo and south of the main Aucanquilcha massif. Amincha was closed in 1992; the last reported mining activity on the mountain was in 1994 and during the 1980s-1990s the worker camps were abandoned.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
One of them reportedly had spent two years there. These are considered to be the highest human inhabitants on Earth. Research performed on Aymara miners of the Aucanquilcha mine indicates that they are fully acclimatized to the altitude, with less hyperventilation and higher hemoglobin than acclimatized people from lower areas. Their families are born and raised at lower altitudes, however.

Geographic entities mentioned:
surface_form: aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Aucanquilcha sits on top of a 2.7–3.3 mya andesite platform and rises more than over it. The main volcano is composed of an east-west long chain of stratovolcanoes and has an estimated volume of. The maximum slope of the summit area is 25°. During the Cumbre Negra stage, a pyroclastic flow occurred on the northwestern side of the volcano. It covered on a run of and now has a volume of.

Geographic entities mentioned:
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
Lava flows, mostly from the summit areas, are dark to grey in colour and extend as far as from their vents. It is likely that two small lava domes (Cerro Cumbre Negra and Summit 5867) on the northwest flank occupy flank vents. To the north lies the 3.3 mya old andesite Cerro Tres Monos ridge; to the west lies the east-west Cerro Polan and La Luna ridge.

Geographic entities mentioned:
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
The Cerro Chinchillas lavas are the oldest of this stage; erupted from an unknown vent, they lack amphiboles. The total volume is, indicating a flux rate of. A flank collapse, possibly triggered by a large earthquake, occurred during this stage. The third stage is the &quot;Cumbre Negra&quot; stage, named after the westernmost summit and principal vent of this stage, Cerro Cumbre Negra ().

Geographic entities mentioned:
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
The Rodado stage edifice has several moraine stages on its southern slopes. Another small cirque with a moraine has been found in the northeastern side of the Cerro Cumbre Negra summit next to an Azufrera stage lava flow. A small moraine lies on the south side of the Angulo edifice; some lavas from that edifice overlie glacial deposits. Human activity and mining.

Geographic entities mentioned:
surface_form: cumbre negra
instance_of: Mountain
countries: Chile
coordinates: lat: -31.766666666667
lon: -70.733333333333
The municipality centre of Temagami is located on the north-northwestern shore of the lake. The primary outflow is an unnamed creek to Snake Island Lake, which flows via Cassels Lake, Rabbit Lake, the Matabitchuan River and Lake Timiskaming into the Ottawa River. Caribou Mountain, a large forested hill with a fire tower on its summit, rises above Caribou Lake with a topographical prominence of.

Geographic entities mentioned:
surface_form: Snake Island Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0642
lon: -79.7617
surface_form: Cassels Lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0667
lon: -79.7167
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
surface_form: rabbit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.001
lon: -79.6385
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.8464
lon: -113.532
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: island lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.9819
lon: -107.7276
Caribou Lake (Temagami). Caribou Lake is a lake in the Ottawa River drainage basin in Strathy Township of Temagami, Nipissing District in Northeastern Ontario, Canada. The municipality centre of Temagami is located on the north-northwestern shore of the lake.

Geographic entities mentioned:
surface_form: nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: caribou lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0603
lon: -79.7858
surface_form: caribou lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.425
lon: -79.4
Caribou Lake (Temagami). Caribou Lake is a lake in the Ottawa River drainage basin in Strathy Township of Temagami, Nipissing District in Northeastern Ontario, Canada. The municipality centre of Temagami is located on the north-northwestern shore of the lake.

Geographic entities mentioned:
surface_form: caribou lake (temagami)
instance_of: Lake
countries: Canada
coordinates: lat: 47.0603
lon: -79.7858
surface_form: caribou lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.425
lon: -79.4
The municipality centre of Temagami is located on the north-northwestern shore of the lake. The primary outflow is an unnamed creek to Snake Island Lake, which flows via Cassels Lake, Rabbit Lake, the Matabitchuan River and Lake Timiskaming into the Ottawa River. Caribou Mountain, a large forested hill with a fire tower on its summit, rises above Caribou Lake with a topographical prominence of.

Geographic entities mentioned:
surface_form: caribou lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0603
lon: -79.7858
surface_form: caribou mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 47.0583
lon: -79.7792
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: caribou lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.425
lon: -79.4
The album was released on 12 March 2021 and it was promoted through 4 singles: &quot;Idea of You&quot;, &quot;Domino&quot;, &quot;Something More&quot;, and &quot;I Don't Need a Hero&quot;. The first single &quot;Idea of You&quot; premiered on YouTube on December 11, 2020. Its music video has been filmed in Death Valley.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Mont Brûlé (Val d'Entremont). Mont Brûlé is a mountain of the Swiss Pennine Alps, overlooking Orsières in the canton of Valais. It lies just north of Col de Mille.

Geographic entities mentioned:
surface_form: mont brûlé
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.017638888889
lon: 7.20075
The park contains numerous lakes, such as Kinnaird, Jackson, McGuffin, Dabbs, Shaw, and Blackett, as well as many other smaller waterbodies. The Lakeland Provincial Recreation Area contains Pinehurst Lake, Seibert, Touchwood and Ironwood Lakes. Planning the provincial park.

Geographic entities mentioned:
surface_form: Pinehurst Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6631
lon: -111.417
The other major lakes, in the south-east section of the Lakeland area, are in the Sand River sub-basin. Spencer and Seibert Lakes are drained by a small unnamed creek, while Punk Creek drains Pinehurst Lake. Water from Touchwood Lake also enters Pinehurst Lake through a small creek.

Geographic entities mentioned:
surface_form: Pinehurst Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.6631
lon: -111.417
He finished grammar and theological school in Prizren, then became a monk, serving as deacon under the Serbian Orthodox Metropolitan (&quot;vladika&quot;) of Žiča. He went to the Serbian Orthodox monastery of Hilandar on Mount Athos, where he took the monastic name Jeremija (Јеремија).

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Early Winters Spires. The Early Winters Spires are two rock formations in the Liberty Bell Group of the North Cascade Range, set between Liberty Bell Mountain and Blue Lake Peak in Washington state, United States. The two spires (North and South) are virtually one granite massif, split by a deep cleft formed by jointing and erosion.

Geographic entities mentioned:
surface_form: Liberty Bell Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5154
lon: -120.658
surface_form: Blue Lake Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.50666667
lon: -120.65722222
Grange and gardens. Bennett had purchased land about Auckland—suburban farms at Epsom and Mt Eden near Three Kings in 1842 and 1843, as well as a site for his new residence on the heights of Khyber Pass Road, Lot 7, Section 3, just over 5 acres, at the head of Grafton Gully / Glen Ligar in July 1843.

Geographic entities mentioned:
surface_form: Grafton Gully
instance_of: Valley
countries: New Zealand
coordinates: lat: -36.858711111111
lon: 174.76667777778
To FitzRoy's order, he designed a transportable wooden blockhouse to shelter 20 soldiers, of which five would be made for Auckland, Russell, Whangārei and the Hutt Valley. The blockhouses measured internally 17 ft x 20 ft x 9 ft stud, with common gable weatherboard roof, loopholed walls of kauri posts vertically arranged between top and bottom plates; room enough for 16 beds.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
Also, there are alpine tundra and snow-capped peaks, including Mauna Kea, Mount Kilimanjaro, Puncak Jaya and the Andes as far south as the northernmost parts of Chile and Peru. Climate change. The climate is changing in the tropics, as it is in the rest of the world.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
From mid 2012, the Liberals had led every public poll and entered the campaign with a 20-point lead over the New Democratic Party (NDP). While the Liberals had been relatively successful in the Annapolis Valley and on Cape Breton Island during the 2009 election, they were completely shut out of the South Shore, Fundy, and Central Nova Scotia.

Geographic entities mentioned:
surface_form: Annapolis Valley
instance_of: Valley
countries: Canada
coordinates: lat: 44.979166666666664
lon: -64.89222222222222
Synopsis. Reader divides his exploration of the potato into three sections: South America, Europe, The World. South America. The first section describes the environments, The Andes Mountains and the altiplano, in which the potato developed. In the past, at least 3,000 years ago, people living in these environments began to take advantage of a naturally occurring plant.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
In colonial times Lake Malawi was known as Lake Nyasa (very similar to &quot;Knysna&quot;), while &quot;Webster's Universal Unabridged Dictionary&quot; defines the word &quot;nyanza&quot; as a noun: &quot;(African): An expanse of water, as a lake or wide river&quot;. Early history.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The population of Angvika is about 300. There is a furniture factory, a salmon fish farm, a Spa Hotel, and tourist apartments. The village of Rausand (in Molde Municipality) lies about to the south, Heggem lies about to the west, Torvikbukt lies about to the northwest&ndash;near the mountain Reinsfjellet, and the village of Flemma lies about to the north.

Geographic entities mentioned:
surface_form: Reinsfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.929722222222
lon: 7.9263888888889
The center is located in Barrio Bellavista - a neighborhood of Santiago with a strong cultural heritage - in an old house at the foot of San Cristóbal Hill (street address Constitución 183), next to the Plaza Camilo Mori and near &quot;La Chascona&quot; (the museum and former house of Pablo Neruda).

Geographic entities mentioned:
surface_form: San Cristóbal Hill
instance_of: Mountain
countries: Chile
coordinates: lat: -33.42527778
lon: -70.63333333
KRSU-TV. KRSU-TV (channel 35) is an educational independent television station in Claremore, Oklahoma, United States, serving the Tulsa area. Owned by Rogers State University, the station maintains studios on the university's campus on West Will Rogers Boulevard in Claremore, and its transmitter is located to the adjacent southeast of Oologah Lake in northern Rogers County.

Geographic entities mentioned:
surface_form: Oologah Lake
instance_of: Lake
countries: United States
coordinates: lat: 36.5546
lon: -95.5989
Saint Sava Tower, Hilandar. Saint Sava Tower (,) is a medieval defensive structure dedicated to Saint Sava, located in Serbian Orthodox Hilandar Monastery in Mount Athos, Greece. Location. The tower is one of the two towers on the Hilandar rock, located on the eastern side. On the south side is the smaller Tower of St. George. History.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
They were previously named for the indigenous Native American population of the Pacific Northwest and changed their name after being acquired by the Rainier Brewing Company, which was named for nearby Mount Rainier. History.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Hardyston is home to portions of Hamburg Mountain (east of Franklin) and Pochuck Mountain (near Scenic Lakes) within this region. The remaining northwestern portion of the township lies within the Ridge-and-valley Appalachians. The prominent feature in the ridge-and-valley portion of the Township is the Wallkill Valley, through which the Wallkill River flows northeast to New York state.

Geographic entities mentioned:
surface_form: Pochuck Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.2111
lon: -74.5306
Description. The &quot;meiyu&quot; front stretches from the Tibetan Plateau to Japan along a confluent jet stream that separates Arctic circulation to the north from tropical circulation to the south. During mid-spring to mid-summer, the upper circulation is typically west-east and the front is mostly stationary.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Along this boundary, mesoscale convective complexes (MCCs) or mesoscale convective systems (MCSs) tend to form and propagate eastward, giving a series of heavy downpours. The system extracts moisture from the South China Sea and sometimes the Bay of Bengal. The low-level warm air is lifted by the low level jet on the equator side of the baroclinic zone.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Bärenhorn. The Bärenhorn is a mountain of the Lepontine Alps, situated between Vals and Rheinwald in Graubünden, on territory of both municipalities. The northeastern face lies on territory of Safien. A popular hike starts at Zervreila, passes three remote lakes (Guraletschsee, Amperveilsee and Selvasee) and descends via Selva Alp to Vals. Vals is famous for its spa.

Geographic entities mentioned:
surface_form: Rheinwald
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.551778
lon: 9.319788
surface_form: bärenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.575555555556
lon: 9.2318888888889
Bärenhorn. The Bärenhorn is a mountain of the Lepontine Alps, situated between Vals and Rheinwald in Graubünden, on territory of both municipalities. The northeastern face lies on territory of Safien. A popular hike starts at Zervreila, passes three remote lakes (Guraletschsee, Amperveilsee and Selvasee) and descends via Selva Alp to Vals. Vals is famous for its spa.

Geographic entities mentioned:
surface_form: Guraletschsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.561
lon: 9.1376
surface_form: Amperveilsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.57138888888889
lon: 9.151388888888889
Bärenhorn. The Bärenhorn is a mountain of the Lepontine Alps, situated between Vals and Rheinwald in Graubünden, on territory of both municipalities. The northeastern face lies on territory of Safien. A popular hike starts at Zervreila, passes three remote lakes (Guraletschsee, Amperveilsee and Selvasee) and descends via Selva Alp to Vals. Vals is famous for its spa.

Geographic entities mentioned:
surface_form: bärenhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.575555555556
lon: 9.2318888888889
Pic de Bugarach. The Pic de Bugarach () or Pech de Bugarach (;; &quot;Peak of Bugarag&quot;) is the highest summit (1230 m) in the Corbières Massif in the French &quot;Midi&quot;. The western part of the mountain is located on the territory of the commune of Bugarach. Its eastern part is on the territory of Camps-sur-l'Agly. The geology of the Pic de Bugarach is striking.

Geographic entities mentioned:
surface_form: pic de bugarach
instance_of: Mountain
countries: France
coordinates: lat: 42.863611111111
lon: 2.3791666666667
Pic de Bugarach. The Pic de Bugarach () or Pech de Bugarach (;; &quot;Peak of Bugarag&quot;) is the highest summit (1230 m) in the Corbières Massif in the French &quot;Midi&quot;. The western part of the mountain is located on the territory of the commune of Bugarach. Its eastern part is on the territory of Camps-sur-l'Agly. The geology of the Pic de Bugarach is striking.

Geographic entities mentioned:
surface_form: pic de bugarach
instance_of: Mountain
countries: France
coordinates: lat: 42.863611111111
lon: 2.3791666666667
surface_form: pech de bugarach
instance_of: Mountain
countries: France
coordinates: lat: 42.863611111111
lon: 2.3791666666667
The Punilla Valley () is a broad fluvial valley in the province of Córdoba, Argentina. It is located in the center-northwest of the province, bordered by the Sierras Chicas in the east and the Sierras Grandes and the Pampa Achala in the west, oriented from north to south. In the southern part of the valley lies the San Roque Lake, fed mainly by the San Antonio River and the Cosquín River.

Geographic entities mentioned:
surface_form: Cosquín River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -31.216666666667
lon: -64.483333333333
Punilla Valley. The Punilla Valley () is a broad fluvial valley in the province of Córdoba, Argentina. It is located in the center-northwest of the province, bordered by the Sierras Chicas in the east and the Sierras Grandes and the Pampa Achala in the west, oriented from north to south.

Geographic entities mentioned:
surface_form: punilla valley
instance_of: Valley
countries: Argentina
coordinates: lat: -31.033333333333
lon: -64.5
A large part of the quarter is the nature reserve &quot;Harburger Berge&quot; (Hills of Harburg) in the south. Neugraben-Fischbek it a mixed rural and suburban area of 22.5 km2. In Neugraben-Fischbek is the highest point of Hamburg, the Hasselbrack, which has an elevation of 116.2 metres AMSL
Demographics. In 2006 the Neugraben-Fischbek quarter had a population of 27,103.

Geographic entities mentioned:
surface_form: Hasselbrack
instance_of: Mountain
countries: Germany
coordinates: lat: 53.43025
lon: 9.863833333333334
San Andrés Itzapa. San Andrés Itzapa () is a town, with a population of 24,992 (2018 census), and a municipality of Chimaltenango, Guatemala. San Andrés Itzapa is in the eastern region of Chimaltenango, while the district capital lies to the north, Acatenango lies to the south, and Parramos lies to the east. The municipality covers an area of 63.7 km2, with a total population of 32,083.

Geographic entities mentioned:
surface_form: Acatenango
instance_of: Mountain
countries: Guatemala
coordinates: lat: 14.5
lon: -90.875833333333
Lake Fannie is part of the north system of the Winter Haven Chain of Lakes. Lake Fannie is connected by canal on its west side to Lake Smart and on its east side to Lake Hamilton (Florida). However, for a number of years the water level in the canals was so low or even nonexistent that Lake Fannie did not connect into the canal system. There are no public swimming areas on this lake's shore.

Geographic entities mentioned:
surface_form: Lake Smart
instance_of: Lake
countries: United States
coordinates: lat: 28.0589
lon: -81.7109
surface_form: lake fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
surface_form: lake hamilton (florida)
instance_of: Lake
countries: United States
coordinates: lat: 28.0528
lon: -81.6548
Lake Fannie. Lake Fannie is a natural freshwater lake on the northeast side of Winter Haven, Florida. This lake has an surface area. Much of its shoreline area is swamp like, but the rest of the lake is free of surface vegetation. Lake Idyl is bordered on the north by Polk County Road 544, on part of the east side by a residential area and on most of the rest of its shoreline by woods.

Geographic entities mentioned:
surface_form: lake fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
Lake Idyl is bordered on the north by Polk County Road 544, on part of the east side by a residential area and on most of the rest of its shoreline by woods. The public has access to this lake on its north shore, along County road 544. Also, a public boat ramp, accessed from 544, in on the northeast shore of Lake Fannie. Lake Fannie is part of the north system of the Winter Haven Chain of Lakes.

Geographic entities mentioned:
surface_form: lake fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
The public has access to this lake on its north shore, along County road 544. Also, a public boat ramp, accessed from 544, in on the northeast shore of Lake Fannie. Lake Fannie is part of the north system of the Winter Haven Chain of Lakes. Lake Fannie is connected by canal on its west side to Lake Smart and on its east side to Lake Hamilton (Florida).

Geographic entities mentioned:
surface_form: lake fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Lake Fannie is part of the north system of the Winter Haven Chain of Lakes. Lake Fannie is connected by canal on its west side to Lake Smart and on its east side to Lake Hamilton (Florida). However, for a number of years the water level in the canals was so low or even nonexistent that Lake Fannie did not connect into the canal system. There are no public swimming areas on this lake's shore.

Geographic entities mentioned:
surface_form: lake fannie
instance_of: Lake
countries: United States
coordinates: lat: 28.0603
lon: -81.6895
This lake has an surface area. Much of its shoreline area is swamp like, but the rest of the lake is free of surface vegetation. Lake Idyl is bordered on the north by Polk County Road 544, on part of the east side by a residential area and on most of the rest of its shoreline by woods. The public has access to this lake on its north shore, along County road 544.

Geographic entities mentioned:
surface_form: lake idyl
instance_of: Lake
countries: United States
coordinates: lat: 28.042
lon: -81.7129
Emanda. Emanda (or Эманджа,) is a freshwater lake in Tomponsky District, Sakha Republic, Russia. The lake is located in a desolate area where there is no permanent population and few visitors. There are burbot, pike and grayling in its waters. Geography. The lake lies at above mean sea level in the basin of the Derbeke River, part of the Yana basin.

Geographic entities mentioned:
surface_form: эманджа
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 65.278333333333
lon: 135.77972222222
surface_form: emanda
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 65.278333333333
lon: 135.77972222222
Emanda. Emanda (or Эманджа,) is a freshwater lake in Tomponsky District, Sakha Republic, Russia. The lake is located in a desolate area where there is no permanent population and few visitors. There are burbot, pike and grayling in its waters. Geography. The lake lies at above mean sea level in the basin of the Derbeke River, part of the Yana basin.

Geographic entities mentioned:
surface_form: emanda
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 65.278333333333
lon: 135.77972222222
There are burbot, pike and grayling in its waters. Geography. The lake lies at above mean sea level in the basin of the Derbeke River, part of the Yana basin. It is located to the east of the river, roughly to the south of the Nelgesin Range. Lake Emanda is the largest lake of the Yana Plateau. The Seen River (Сеен), a right hand tributary of the Derbeke, is the outflow of the lake.

Geographic entities mentioned:
surface_form: emanda
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 65.278333333333
lon: 135.77972222222
Lake Emanda is the largest lake of the Yana Plateau. The Seen River (Сеен), a right hand tributary of the Derbeke, is the outflow of the lake. The minimum temperature of -58.6 °C (-73.5 °F) recorded on December 5, 2023 in Emanda, being the lowest December temperature in 40 years, according to weather historian Thierry Goose.

Geographic entities mentioned:
surface_form: emanda
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 65.278333333333
lon: 135.77972222222
Flassan. Flassan (;) is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France. Geography. Flassan is located at the foot of Mont Ventoux.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
Passing just east of Nova Scotia on September 29, Helene dropped at least across the entire province, peaking at in Cape Breton Island. Gusts peaked at across Cabot Strait, at CFB Shearwater and at Summerside, Prince Edward Island. The storm damaged power lines on the island but they were quickly repaired. The strong winds uprooted trees in the Halifax and Dartmouth, Nova Scotia area.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
The salar is located southwest of Ollagüe. It covers an area of around and its surface elevation is. The landscape of the area is dominated by the volcanoes Ollagüe to the east and Aucanquilcha to the north. Salar de Carcote basin is bordered by the Loa River basin to the west and the Salar de Ascotán basin to the south. Salar de Carcote is a remnant of an ancient lake.

Geographic entities mentioned:
surface_form: Ollagüe
instance_of: Mountain
countries: Bolivia
Chile
coordinates: lat: -21.3
lon: -68.166666666667
surface_form: Aucanquilcha
instance_of: Mountain
countries: Chile
coordinates: lat: -21.220833333333335
lon: -68.46833333333333
Lansing Sailing Club. ltno9m4m171nxgpad7a4ai4d6rp6" xml:space="preserve">Founded in 1963, the Lansing Sailing Club is located on Lake Lansing in Haslett, Michigan near the capital city of Lansing. The club has an active program of sailboat racing, junior sailing camps, adult learn to sail programs and holiday events during a sailing season that extends from mid-April through mid-October.

Geographic entities mentioned:
surface_form: Lake Lansing
instance_of: Lake
countries: United States
coordinates: lat: 42.758333333333
lon: -84.4
She was the third of her parents' seven children, but three of her brothers died in infancy and childhood. Her family later moved to South Bethlehem, Pennsylvania, in the Lehigh Valley region of the state. Personal life. In 1901, at 20 years old, she married Abraham Lincoln Knauss (1878–1965).

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
These programs include traditional music of Greece, Southern Balkans, and old Serbia, where a special emphasis is paid to the Serbo-Byzantine school, cycle of Kosovo songs, customs and ritual songs, dances from all parts of Serbia and one special rarity: songs from the Iviron monastery on Mount Athos.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Rhumel River. The Rhumel River (Tamazight: ⴰⵎⵒⵙⴰⴳⴰ, also Rhummel, Rummel, El-Kebîrl; Arabic: وادي الرمال), in antiquity, the river was called Ampsaga. is the largest river in the Constantine region of Algeria. Geography. The source of the Rhumel river is in the Ferdjioua (Mila) mountains.

Geographic entities mentioned:
surface_form: وادي الرمال
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
surface_form: rhummel
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
surface_form: rhumel river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
surface_form: ampsaga
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
surface_form: rummel
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
Rhumel River. The Rhumel River (Tamazight: ⴰⵎⵒⵙⴰⴳⴰ, also Rhummel, Rummel, El-Kebîrl; Arabic: وادي الرمال), in antiquity, the river was called Ampsaga. is the largest river in the Constantine region of Algeria. Geography. The source of the Rhumel river is in the Ferdjioua (Mila) mountains.

Geographic entities mentioned:
surface_form: rhumel river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
is the largest river in the Constantine region of Algeria. Geography. The source of the Rhumel river is in the Ferdjioua (Mila) mountains. From there it meanders through the Constantine plateau, then narrows considerably north of Aïn Smara where it forms an almost complete oxbow before infiltrating, in a SW/NE orientation, the Djebel El Hadjar limestone tables and the Aïn El Bey plateau.

Geographic entities mentioned:
surface_form: rhumel river
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
The lower Rhumel (or Oued-el-Kebir) passes through deep gorges in the Numidian mountains and empties into the sea east of the Gulf of Jijel. Tributaries. The main tributary of the Rhumel is the Oued-Boumerzoug which rises in the region of Aïn M'lila. Its waters are widely used for irrigation, and the important spa of Ain Fesguia is located towards the head of the valley.

Geographic entities mentioned:
surface_form: rhumel
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
Its waters are widely used for irrigation, and the important spa of Ain Fesguia is located towards the head of the valley. This tributary supplies drinking water to the city of Constantine, which is highly prone to flooding being situated at the confluence of the Boumerzoug and the Rhumel. Another tributary is the Oued Dekri, near the town of Chelghoum Laïd 50 km southwest of Constantine.

Geographic entities mentioned:
surface_form: rhumel
instance_of: Watercourse
countries: Algeria
France
coordinates: lat: 36.87212817
lon: 6.08567476
The feature is situated at the junction of four radial ridges. The summit is a small mesa of conglomerate rising to about 300 m above the surrounding ice. First photographed by Lincoln Ellsworth, November 23, 1935, in the course of a trans-Antarctic flight and plotted from the air photos by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
Mount Phoebe. Mount Phoebe () is a mountain between the heads of Neptune Glacier and Saturn Glacier near the east coast of Alexander Island, Antarctica. The feature is situated at the junction of four radial ridges. The summit is a small mesa of conglomerate rising to about 300 m above the surrounding ice.

Geographic entities mentioned:
surface_form: mount phoebe
instance_of: Mountain
coordinates: lat: -71.7833
lon: -68.7833
surface_form: phoebe
instance_of: Mountain
coordinates: lat: -71.7833
lon: -68.7833
Mount Phoebe. Mount Phoebe () is a mountain between the heads of Neptune Glacier and Saturn Glacier near the east coast of Alexander Island, Antarctica. The feature is situated at the junction of four radial ridges. The summit is a small mesa of conglomerate rising to about 300 m above the surrounding ice.

Geographic entities mentioned:
surface_form: mount phoebe
instance_of: Mountain
coordinates: lat: -71.7833
lon: -68.7833
surface_form: phoebe
instance_of: Mountain
coordinates: lat: -71.7833
lon: -68.7833
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
First photographed by Lincoln Ellsworth, November 23, 1935, in the course of a trans-Antarctic flight and plotted from the air photos by W.L.G. Joerg. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) from association with Saturn Glacier after Phoebe, one of the satellites of the planet Saturn, the sixth planet of the Solar System.

Geographic entities mentioned:
surface_form: phoebe
instance_of: Mountain
coordinates: lat: -71.7833
lon: -68.7833
Additionally, she took her family on adventure travel excursions that ranged from riding horses across the Gobi Desert to hiking of Spain's Camino de Santiago pilgrimage. Many of these feats, including her 2019 summiting of Aconcagua (South America's tallest peak), were accomplished after her cancer diagnosis.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
History. La Romita began as a pre Hispanic village that remained independent until the establishment of Colonia Roma and has remained semi-independent since. In the pre Hispanic period, the area was a small island called Aztacalco located near the Aztec capital of Tenochtitlan surrounded by the shallow waters of Lake Texcoco.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
Geography. The municipality, at a height of about, is the main settlement in the East Tyrolean &quot;Hochpustertal&quot;, the eastern part of the Puster Valley, stretching from Lienz up to the border with South Tyrol, Italy, in the west. The settlement is situated north of the upper Drava river, on the sunny slopes of the Villgraten Mountains.

Geographic entities mentioned:
surface_form: Hochpustertal
instance_of: Valley
countries: Italy
coordinates: lat: 46.731944444444
lon: 12.296388888889
surface_form: Puster Valley
instance_of: Valley
countries: Italy
Austria
coordinates: lat: 46.7405
lon: 12.369555555555555