Sarmila/GeoWiki-Features huggingface dataset:
Round Mountain (Washington). Round Mountain is a 5,369-foot mountain summit at the western edge of the North Cascades, in Skagit County of Washington state. It is located nine miles northwest of Darrington, Washington, and is situated on land administered by the Mount Baker-Snoqualmie National Forest.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Round Mountain is remarkable for its 4,840 feet of prominence which ranks as the most in Skagit County, and eighth-most of all the mountains in Washington state. The nearest higher peak is Whitehorse Mountain, to the south-southeast. Precipitation runoff from Round Mountain drains into tributaries of the Stillaguamish River. Climate.

Geographic entities mentioned:
surface_form: whitehorse mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.2115
lon: -121.678
The Mammals. The Mammals are a contemporary folk rock band based in the Hudson Valley area of New York, in the United States. The band tours internationally and consists of founding members and principal songwriters Mike Merenda (guitar, banjo) and Ruth Ungar (fiddle, guitar) plus Konrad Meissner (drums) and a rotating cast of players on bass, organ, and pedal steel.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Sultan Murad II proclaimed a raid into Transylvania, John Hunyadi defeated the raiding Ottoman army at the Battle of Hermannstadt in 1442. John Hunyadi and his 15,000 men defeated the 80,000-strong army of &quot;Beylerbey&quot; Şehabeddin at Zajkány (today's Zeicani), near the Iron Gate of the Danube river in 1442.

Geographic entities mentioned:
surface_form: Iron Gate
instance_of: Valley
countries: Serbia
Romania
coordinates: lat: 44.671111111111
lon: 22.529722222222
It has a distinctive shape, reflecting its name.The lake has an elevation of and a surface area of. The navigable River Havel flows through the Ellbogensee, entering it at Priepert via a long channel from the Großer Priepertsee to the north, and exiting via a long channel to the Ziernsee to the east.

Geographic entities mentioned:
surface_form: Großer Priepertsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.226283333333
lon: 13.041630555556
surface_form: Ziernsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.208192
lon: 13.076992
surface_form: priepertsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.226283333333
lon: 13.041630555556
surface_form: ellbogensee
instance_of: Lake
countries: Germany
coordinates: lat: 53.207222222222
lon: 13.0375
The navigable River Havel flows through the Ellbogensee, entering it at Priepert via a long channel from the Großer Priepertsee to the north, and exiting via a long channel to the Ziernsee to the east. At Strasen, at the western end of the lake, a canal and lock gives access to the Großer Pälitzsee, forming the first link of the Müritz–Havel–Wasserstraße.

Geographic entities mentioned:
surface_form: Großer Pälitzsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.185876122222
lon: 12.970390319444
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Ellbogensee. Ellbogensee (German, 'Elbow Lake') is a lake in the Mecklenburg Lake District, in Germany. Although most of the lake is in the district of Mecklenburgische Seenplatte in the state of Mecklenburg-Vorpommern, a portion of its southern shore is in the state of Brandenburg. It has a distinctive shape, reflecting its name.The lake has an elevation of and a surface area of.

Geographic entities mentioned:
surface_form: ellbogensee
instance_of: Lake
countries: Germany
coordinates: lat: 53.207222222222
lon: 13.0375
Iyang-Argapura. Iyang-Argapura or Mount Argopuro is a massive volcanic complex that dominates the landscape between Mount Raung and Mount Lamongan in East Java, Indonesia. Valleys up to 1,000 m deep dissect the strongly eroded Iyang volcano. No historical eruptions have been recorded within the last 500 years, but there is an unverified report about an eruption in AD 1597.

Geographic entities mentioned:
surface_form: iyang-argapura
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.97
lon: 113.57
It was called the Apple Tree Building after the tree that grew behind it. The building had to be removed in 2003, but the fireplace was saved. Young bought a large piece of land in Charlevoix on Lake Michigan from Mary Bartholomew in 1924. He partitioned the land into 85 lots, only three of which were rectangular, and began advertising it as Boulder Park.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
They reveal that other groups of humans have survived at Argonne, Brookhaven, and Harwell nuclear research facilities as well as in Tannu Tuva, and that plans are being made to establish uranium-mining colonies at Great Slave Lake or in the Congo region. Collections.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
De Lesseps Lake. De Lesseps Lake is a lake in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. The lake is part of the James Bay drainage basin. The major inflow, at the southwest, and outflow, at the north, is the De Lesseps River, which flows to Miniss Lake and then via the Miniss River, Lake St. Joseph and the Albany River to James Bay.

Geographic entities mentioned:
surface_form: lake st. joseph
instance_of: Lake
countries: Canada
coordinates: lat: 51.05
lon: -90.766666666667
De Lesseps Lake. De Lesseps Lake is a lake in the Unorganized Part of Thunder Bay District in Northwestern Ontario, Canada. The lake is part of the James Bay drainage basin. The major inflow, at the southwest, and outflow, at the north, is the De Lesseps River, which flows to Miniss Lake and then via the Miniss River, Lake St. Joseph and the Albany River to James Bay.

Geographic entities mentioned:
surface_form: de lesseps lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -90.7064
The lake is part of the James Bay drainage basin. The major inflow, at the southwest, and outflow, at the north, is the De Lesseps River, which flows to Miniss Lake and then via the Miniss River, Lake St. Joseph and the Albany River to James Bay. De Lesseps Lake Airport is located on the eastern shore of the lake.

Geographic entities mentioned:
surface_form: de lesseps lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -90.7064
The associated eruption was among the largest in Peru for which there are historical records. The volcano became active about 700,000 years ago, and activity continued into the Holocene, but whether there were historical eruptions was initially unclear; some eruptions were instead attributed to the less eroded Yucamane volcano.

Geographic entities mentioned:
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
Tutupaca features geothermal manifestations with fumaroles and hot springs. Oral tradition. The people in Candarave considered Tutupaca to be a &quot;bad&quot; mountain, while Yucamane was the &quot;good&quot; one; this may reflect that Tutupaca had recent volcanic eruptions. The Peruvian geographer Mateo Paz Soldán dedicated an ode to Tutupaca. Geology and geomorphology.

Geographic entities mentioned:
surface_form: Yucamane
instance_of: Mountain
countries: Peru
coordinates: lat: -17.18
lon: -70.2
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The ridges range from only a few meters to more than in height, and from in height. Such ridges have been observed in other collapse deposits such as at Shiveluch volcano in Russia, and have been explained by sorting processes that take place within granular flows.

Geographic entities mentioned:
surface_form: Shiveluch
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.653633333333
lon: 161.36296666667
Such large collapses of volcanoes took place in historical time at Mount Bandai in 1888 and Mount St. Helens in 1980; they can produce large avalanches of debris. Geologic context. Off the coast of Peru, the Nazca Plate subducts at beneath the South America Plate, causing volcanism in three of the four volcanic belts in the Andes, including the Central Volcanic Zone where Tutupaca is located.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Other Peruvian volcanoes include Sara Sara, Solimana, Coropuna, the Andagua volcanic field, AmpatoSabancayaHualca Hualca, Chachani, El Misti, Ubinas, Huaynaputina, Ticsani, Yucamane, Purupuruni and Casiri.

Geographic entities mentioned:
surface_form: Sara Sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: Andagua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
surface_form: Ampato
instance_of: Mountain
countries: Peru
coordinates: lat: -15.820555555555556
lon: -71.88
surface_form: Hualca Hualca
instance_of: Mountain
countries: Peru
coordinates: lat: -15.816666666667
lon: -71.883333333333
surface_form: Chachani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.194166666667
lon: -71.531666666667
surface_form: Ubinas
instance_of: Mountain
countries: Peru
coordinates: lat: -16.34861111111111
lon: -70.90222222222222
surface_form: Huaynaputina
instance_of: Mountain
countries: Peru
coordinates: lat: -16.615555555555556
lon: -70.84972222222223
surface_form: Ticsani
instance_of: Mountain
countries: Peru
coordinates: lat: -16.7675
lon: -70.5997
surface_form: Purupuruni
instance_of: Mountain
countries: Peru
coordinates: lat: -17.30916667
lon: -69.91472222
surface_form: andagua volcanic field
instance_of: Mountain
countries: Peru
coordinates: lat: -15.257
lon: -72.483
Tutupaca. Tutupaca is a volcano in the region of Tacna in Peru. It is part of the Peruvian segment of the Central Volcanic Zone, one of several volcanic belts in the Andes. Tutupaca consists of three overlapping volcanoes formed by lava flows and lava domes made out of andesite and dacite, which grew on top of older volcanic rocks.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
It is part of the Peruvian segment of the Central Volcanic Zone, one of several volcanic belts in the Andes. Tutupaca consists of three overlapping volcanoes formed by lava flows and lava domes made out of andesite and dacite, which grew on top of older volcanic rocks. The highest of these is usually reported to be tall and was glaciated in the past.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The highest of these is usually reported to be tall and was glaciated in the past. Several volcanoes in Peru have been active in recent times, including Tutupaca. Their volcanism is caused by the subduction of the Nazca Plate beneath the South America Plate.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The Peruvian government plans to monitor the volcano for future activity. Tutupaca features geothermal manifestations with fumaroles and hot springs. Oral tradition. The people in Candarave considered Tutupaca to be a &quot;bad&quot; mountain, while Yucamane was the &quot;good&quot; one; this may reflect that Tutupaca had recent volcanic eruptions.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Oral tradition. The people in Candarave considered Tutupaca to be a &quot;bad&quot; mountain, while Yucamane was the &quot;good&quot; one; this may reflect that Tutupaca had recent volcanic eruptions. The Peruvian geographer Mateo Paz Soldán dedicated an ode to Tutupaca. Geology and geomorphology. Tutupaca is north of the town of Candarave in the region of Tacna in Peru.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Geology and geomorphology. Tutupaca is north of the town of Candarave in the region of Tacna in Peru. Lake Suches lies north of the volcano, and two rivers flow nearby: the Callazas River, flowing eastward to the north of the volcano, and then southward past Tutupaca's eastern flank, and the Tacalaya River, which flows south along Tutupaca's western flank.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The local climate is cold, and the terrain is stony, with little vegetation. During the wet season, the mountain is snow-covered, and meltwater from Tutupaca and other regional mountains is an important source of water for the rivers in the region. In contrast, the volcano itself is largely unaffected by human activity.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Of these, the eastern peak (&quot;eastern Tutupaca&quot;) consists of seven presumably Holocene lava domes and is high, while the western one (&quot;western Tutupaca&quot;) consists of lava domes, lava flows and Plinian eruption deposits of Pleistocene age, and reaches a height of. The Global Volcanism Program gives heights of for the eastern and for the western summit.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The Global Volcanism Program gives heights of for the eastern and for the western summit. The western peak is the highest summit of Tutupaca. The base that Tutupaca rises from lies at elevations ranging from to and the volcano covers a surface area of about.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Proglacial processes like frost shattering have altered young volcanic products. Composition. The older complex and western Tutupaca have erupted andesite and dacite, while eastern Tutupaca has only produced dacite. Trachyandesite and trachyte also occur. The volcanic rocks erupted during the Holocene define a potassium-rich calc-alkaline suite.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The volcanic rocks erupted during the Holocene define a potassium-rich calc-alkaline suite. Dacites from eastern Tutupaca contain amphibole, apatite, biotite, clinopyroxene, iron-titanium oxides, orthopyroxene, plagioclase, quartz, and sphene. Mafic rock fragments are rarely found embedded in Tutupaca rocks. The basal volcanic rocks have suffered hydrothermal alteration, forming clays.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Mafic rock fragments are rarely found embedded in Tutupaca rocks. The basal volcanic rocks have suffered hydrothermal alteration, forming clays. Elemental sulfur deposits have been identified at Tutupaca and a 1996 map of the volcano shows a sulfur mine on its southeastern flank. Sector collapse.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Sector collapse. A wide amphitheater in eastern Tutupaca, open to the northeast, was formed by a major collapse of the volcano. Lava domes from the younger Tutupaca, as well as highly altered lavas from the older complex, are exposed within the collapse scar, which is the origin of a long debris avalanche deposit.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The differences between the two units appear to be because the first unit was formed from the basal part of Tutupaca, while the second unit was formed by the more recent lava domes of the eastern volcano and formed a granular flow. The collapse possibly started in the hydrothermal system of the volcano and progressed to affect a growing lava dome, with a total volume probably exceeding.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The total surface area covered by the collapse is about. This collapse was not the first in the history of Tutupaca: collapses on the southeast-east flanks of the volcano occurred 6,0007,500 years ago and delivered debris through glacial valleys on the eastern and southeastern side of the volcano, and on the western side of the volcano a collapse took place before 17,00025,000 years ago.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Such large collapses of volcanoes took place in historical time at Mount Bandai in 1888 and Mount St. Helens in 1980; they can produce large avalanches of debris. Geologic context. Off the coast of Peru, the Nazca Plate subducts at beneath the South America Plate, causing volcanism in three of the four volcanic belts in the Andes, including the Central Volcanic Zone where Tutupaca is located.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The basement of the region consists of folded Mesozoic sediments, and Cenozoic volcanic and sedimentary cover which overlies the Mesozoic rocks. There are many tectonic lineaments and faults which were active in the Tertiary; one of these crosses Tutupaca from north to south, and others influence the positions of geothermal features.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The Huaylillas ignimbrite complex underlies some of the volcanic centres, which include a first set of eroded volcanoes that were active between 8.4–5 and 4–2 million years ago, principally erupting lava flows. These were followed by a second set of volcanoes which were also mainly active with lava flows, such as Casiri, Tutupaca, and Yucamane.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
These were followed by a second set of volcanoes which were also mainly active with lava flows, such as Casiri, Tutupaca, and Yucamane. A third phase formed dacitic lava domes such as Purupuruni about 100,000 years ago. Other, older stratovolcanoes are found at Tutupaca and are heavily eroded by glaciers. Climate and vegetation.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Climate and vegetation. Most of the volcanoes in the Central Volcanic Zone are located at over elevation where the climate is cold with frequent freezes. Most precipitation falls between January and March, at Tutupaca it amounts to. In the Western Cordillera, altitudes between are dominated by vegetation such as cacti, herbs, Peruvian feather grass, and yareta, but also lichens and mosses.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The volcano is part of the. Eruption history. The oldest volcanic rocks of Tutupaca are 1,135,000 ± 17,000 years old. The older complex was active at first with lava flows and then with a major explosive eruption; a pumice-and-ash flow forms the &quot;Callazas&quot; deposit and may have been produced either by the older complex or by western Tutupaca.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The older complex was active at first with lava flows and then with a major explosive eruption; a pumice-and-ash flow forms the &quot;Callazas&quot; deposit and may have been produced either by the older complex or by western Tutupaca. A long hiatus separated the activity of the older complex from that of western and eastern Tutupaca.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Some authors believed that Yucamane volcano was a more likely source for these eruptions, but Samaniego 2015 &quot;et al.&quot; showed that Yucumane last erupted 3,000 years ago, implying that the reported eruptions, especially the 1802 and 1787 events, most likely occurred at Tutupaca. Tutupaca is a possible source of the AD 400-720 Khonkho tephra in the Altiplano.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Some authors believed that Yucamane volcano was a more likely source for these eruptions, but Samaniego 2015 &quot;et al.&quot; showed that Yucumane last erupted 3,000 years ago, implying that the reported eruptions, especially the 1802 and 1787 events, most likely occurred at Tutupaca. Tutupaca is a possible source of the AD 400-720 Khonkho tephra in the Altiplano.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Tutupaca along with Ubinas and Huaynaputina is one of the three volcanoes in Peru to have produced large explosive eruptions. The Peruvian Instituto Geológico, Minero y Metalúrgico (INGEMMET) has published a volcano hazard map for Tutupaca. In 2017, Tutupaca was identified as one of the volcanoes to be monitored by the future Peruvian Southern Volcano Observatory.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The fields feature fumaroles, geysers, mud pots and occurrences of sulfur, both solid and in the form of hydrogen sulfide gas, as well as siliceous sinter and travertine deposits. Hot springs at the foot of the Tutupaca volcano discharge water into the rivers. Tutupaca has been mentioned as a potential site for geothermal power generation.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
Hot springs at the foot of the Tutupaca volcano discharge water into the rivers. Tutupaca has been mentioned as a potential site for geothermal power generation. In 2013, Canada's Alterra Power and the Philippine Energy Development Corporation developed a joint venture to work on a geothermal prospect at Tutupaca, although work at Tutupaca had not begun by October 2014.

Geographic entities mentioned:
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.0308
lon: -70.4483
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
surface_form: tutupaca
instance_of: Mountain
countries: Peru
coordinates: lat: -17.02638889
lon: -70.37166667
The peloton still finished 13 minutes behind the stage winner, leading to massive re-shuffling of the overall standings. On the first of the Giro's many mountain stages in its final week, Evans rode well and stayed with the leaders through the Monte Grappa climb. He did not follow Nibali's aggressive descent of the mountain, and finished with Ivan Basso and Michele Scarponi 23 seconds back.

Geographic entities mentioned:
surface_form: Monte Grappa
instance_of: Mountain
countries: Italy
coordinates: lat: 45.873333333333
lon: 11.799166666667
This result moved Evans back into the top ten overall for the first time since the huge time loss in stage 11. The next day, Evans rode most of the climb of Monte Zoncolan with Basso, but he was dropped shortly before the summit, conceding over a minute to the Italian. The result did, however, move him up to fifth overall, and into the points classification lead.

Geographic entities mentioned:
surface_form: Monte Zoncolan
instance_of: Mountain
countries: Italy
coordinates: lat: 46.5
lon: 12.916666666667
, Ecotricity does not offer a Smart Export Guarantee tariff to small low-carbon generators such as domestic solar panel systems. Greenbird. Ecotricity is the sponsor of the Ecotricity Greenbird, a land yacht that set a new world land speed record for wind-powered vehicles on 26 March 2009 on the dry Lake Ivanpah. &quot;Nemesis&quot;.

Geographic entities mentioned:
surface_form: dry Lake Ivanpah
instance_of: Lake
countries: United States
coordinates: lat: 35.5506
lon: -115.3959
It was made in the Unified Silla Kingdom era and is well known with the name of Gatbawi Buddha (Stone Hat Buddha). It sits tall, and the hat is a thick flat stone on his head,
This single granite sculpture was made up by Uihyeon, at the top of the high rough Palgongsan and is surrounded by a screen-like rock wall as its background.

Geographic entities mentioned:
surface_form: Palgongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 36.016944444444
lon: 128.695
Bodnant Garden. Bodnant Garden () is a National Trust property near Tal-y-Cafn, Conwy, Wales, overlooking the Conwy valley towards the Carneddau mountains. Founded in 1874 and developed by five generations of one family, it was given to the National Trust in 1949.

Geographic entities mentioned:
surface_form: Carneddau
instance_of: Landform
countries: United Kingdom
coordinates: lat: 53.18114
lon: -4.00297
It is part of the larger grouping known as the Pacific Coast Ranges that extends over much of the western edge of North America from California to Alaska. The range creates a rain shadow effect for the Willamette Valley that lies to the east of the mountains, creating a more stable climate and significantly less rain than the coastal region of the state.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
To the west where the range over-shadows the Oregon Coast, the range causes more precipitation to fall on that side of the mountains, contributing to the numerous rivers that flow to the Pacific Ocean. Marys Peak in the Central Coast Range is the highest peak at 4,097 feet (1,248 m). Logging is a major industry in the range in both private and government owned forests.

Geographic entities mentioned:
surface_form: Marys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.504355555556
lon: -123.55245555556
In the east the mountains begin as foothills forming the western edge of the Willamette Valley and continue west to the coastline and beyond where the basalt formation tapers off into the continental shelf and ends at the continental slope with several banks and basins off shore.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
The Central and Northern sections contain more sedimentary rocks from the mud, silt, sand, and other volcanic debris than the lower Southern section. North. Located in the northwest portion of Oregon this section of the range has peaks as high as for Rogers Peak. Forests here are considered to be some of the most productive timber land in the world.

Geographic entities mentioned:
surface_form: Rogers Peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.664555555556
lon: -123.54845277778
Central. Located between the Salmon River and the Umpqua River on the north and south, the Central range is bounded by the Willamette Valley on the east and the Pacific Ocean to the west. This approximately long mountain range contains mountains as high as 4,097 feet (1,248 m) for Marys Peak.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Central. Located between the Salmon River and the Umpqua River on the north and south, the Central range is bounded by the Willamette Valley on the east and the Pacific Ocean to the west. This approximately long mountain range contains mountains as high as 4,097 feet (1,248 m) for Marys Peak.

Geographic entities mentioned:
surface_form: Marys Peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.504355555556
lon: -123.55245555556
History. Work on the Mount Olivet Cemetery site was announced in November 1895; it was planned to be a non-sectarian cemetery on the western slopes of San Bruno Mountain which would be subdivided into sections reserved for fraternal organizations such as the Native Sons of the Golden West, Knights of Pythias, Improved Order of Red Men, and Ancient Order of Foresters.

Geographic entities mentioned:
surface_form: San Bruno Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.6874
lon: -122.436
Inchcruin. Inchcruin is an island in Loch Lomond in Scotland. It is not to be confused with Creinch, which has occasionally been referred to as &quot;Inchcroin&quot;. Geography. Inchcruin is one of an island group just south of Luss. It is long, and in elevation at its highest point.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Little Pond (Orange County, New York). Little Pond is a lake in Orange County, in the U.S. state of New York. The pond has a surface area of. Little Pond was so named on account of its diminutive size. Just over three miles away, its twin Big Pond sits. Big Pond is rather larger than Little Pond, and is accessible from Little Pond via a hiking trail and Big Pond Road.

Geographic entities mentioned:
surface_form: little pond (orange county, new york)
instance_of: Lake
countries: United States
coordinates: lat: 41.469444444444
lon: -74.691944444444
Little Pond (Orange County, New York). Little Pond is a lake in Orange County, in the U.S. state of New York. The pond has a surface area of. Little Pond was so named on account of its diminutive size. Just over three miles away, its twin Big Pond sits. Big Pond is rather larger than Little Pond, and is accessible from Little Pond via a hiking trail and Big Pond Road.

Geographic entities mentioned:
surface_form: little pond
instance_of: Lake
countries: United States
coordinates: lat: 41.469444444444
lon: -74.691944444444
Little Pond (Orange County, New York). Little Pond is a lake in Orange County, in the U.S. state of New York. The pond has a surface area of. Little Pond was so named on account of its diminutive size. Just over three miles away, its twin Big Pond sits. Big Pond is rather larger than Little Pond, and is accessible from Little Pond via a hiking trail and Big Pond Road.

Geographic entities mentioned:
surface_form: little pond
instance_of: Lake
countries: United States
coordinates: lat: 41.469444444444
lon: -74.691944444444
surface_form: little pond
instance_of: Lake
countries: United States
coordinates: lat: 41.469444444444
lon: -74.691944444444
surface_form: big pond
instance_of: Lake
countries: United States
coordinates: lat: 42.193444444444445
lon: -73.04194444444444
surface_form: big pond
instance_of: Lake
countries: United States
coordinates: lat: 42.193444444444445
lon: -73.04194444444444
Little Pond (Orange County, New York). Little Pond is a lake in Orange County, in the U.S. state of New York. The pond has a surface area of. Little Pond was so named on account of its diminutive size. Just over three miles away, its twin Big Pond sits. Big Pond is rather larger than Little Pond, and is accessible from Little Pond via a hiking trail and Big Pond Road.

Geographic entities mentioned:
surface_form: big pond
instance_of: Lake
countries: United States
coordinates: lat: 42.193444444444445
lon: -73.04194444444444
Sunrise on the Matterhorn (Albert Bierstadt). &quot;Sunrise on the Matterhorn&quot; is painting by American artist Albert Bierstadt. Done in oil on canvas and depicting the famous Matterhorn, the painting was produced during one of Bierstadt's numerous trips to Switzerland between the years 1867 and 1897. The painting is currently in the collection of the Metropolitan Museum of Art.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
In 1830, the farms of Gordonhall, Ruthven, Knappach and Drumgellovie and the Forest of Gaick were bought by George Macpherson Grant of Ballindalloch. The farms of Uvie, Auchmore and Biallidmore and the Loch Ericht shootings were bought by Ewen Macpherson of Cluny.

Geographic entities mentioned:
surface_form: Loch Ericht
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.8323
lon: -4.3741
Hostinné. Hostinné () is a town in Trutnov District in the Hradec Králové Region of the Czech Republic. It has about 4,200 inhabitants. It lies on the Elbe river. The historic town centre is well preserved and is protected as an urban monument zone. Etymology.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Geography. Hostinné is located about west of Trutnov and north of Hradec Králové. It lies in the Giant Mountains Foothills. The highest point is at above sea level. The town is situated in a valley of the Elbe River. History. The first written mention of Hostinné is from 1270. It was founded during the reign of King Ottokar II, during the colonization of the upper Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
– chopped up the body into pieces, separating the victim's head, arms and legs with a hacksaw. According to Vandiver, Komyatti was still breathing right before the dismemberment, and he died after the decapitation of his head. The body parts were subsequently packed in six plastic bags and later disposed of near the Lake Michigan shoreline. Arrest and charges.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Of two documented speakers in Anchorage, their cot-caught merger is completed or transitional, is not fronted, is centralized, the placement of is inconsistent, and &quot;ag&quot; approaches the sound of &quot;egg&quot;. Not far from Anchorage, in Alaska's Matanuska-Susitna Valley, is a distinctly Minnesota-like accent due to immigration of Minnesotans to the valley in the 1930s. California.

Geographic entities mentioned:
surface_form: Matanuska-Susitna Valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
Shenandoah Peak. Shenandoah Peak is a summit in the U.S. state of Nevada. The elevation is. A variant name is &quot;Shenandoah Mountain&quot;. The name is a transfer from the Shenandoah Valley, in Virginia.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
The late 1960s saw the appearance of the first fuji bands. Fuji was named after Mount Fuji in Japan, purely for the sound of the word, according to Ayinde Barrister. Fuji was a synthesis of apala with the &quot;ornamented, free-rhythmic&quot; vocals of &quot;ajisari&quot; devotional musicians and was accompanied by the sakara, a tambourine-drum, and Hawaiian guitar.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Lakeland, New York. Lakeland is a hamlet (and census-designated place) in Onondaga County, New York, United States. The population was 2,786 at the 2010 census. The community name is derived from its location next to Onondaga Lake. The community is in the northwest part of the town of Geddes. History.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
The community name is derived from its location next to Onondaga Lake. The community is in the northwest part of the town of Geddes. History. From the latter part of the nineteenth century through the early years of the twentieth century, Lakeland was home to several upscale hotels and a small amusement park along the shores of Onondaga Lake. These were served by a trolley car line from Syracuse.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
All are within minutes of the New York State Fair. Geography. Lakeland is located at (43.093266, -76.245718). According to the United States Census Bureau, the CDP has a total area of, all land. Lakeland comprises the area along roughly the northern half of the southwest side of Onondaga Lake (which runs northwest to southeast). Interstate 690 passes through the community. Demographics.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
Geography. The forest lies on undulating terrain, mostly between 1500 and 1600 meters elevation. It is in the watershed of the Isiukhu and Yala rivers, which originate on the Nandi Escarpment to the east and flow westwards through the forest before emptying into Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Cross River (Lake Superior). The Cross River is a river in northern Minnesota, the United States. It is a direct tributary of Lake Superior. Originally named the river was the site of an incident in 1846 when the missionary priest Frederic Baraga landed here during a storm. He erected a wooden cross at the river's mouth as a memorial and the river became known as Cross River as a result.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Phu Luong (mountain). Phu Luong is a mountain in North Vietnam. It has an elevation of above sea level. With a topographic prominence of it is the fourth most prominent peak in Indochina (comprising Vietnam, Laos, and Cambodia). Phu Luong is located within the Yên Bái province of Vietnam.

Geographic entities mentioned:
surface_form: phu luong (mountain)
instance_of: Mountain
countries: Vietnam
coordinates: lat: 21.57083333
lon: 104.30666667
Phu Luong (mountain). Phu Luong is a mountain in North Vietnam. It has an elevation of above sea level. With a topographic prominence of it is the fourth most prominent peak in Indochina (comprising Vietnam, Laos, and Cambodia). Phu Luong is located within the Yên Bái province of Vietnam.

Geographic entities mentioned:
surface_form: phu luong
instance_of: Mountain
countries: Vietnam
coordinates: lat: 21.57083333
lon: 104.30666667
Battle of Donkey Island. The Battle of Donkey Island was a skirmish that occurred on 30 June and 1 July 2007 between elements of the U.S. Army Task Force 1-77 Armor Regiment, the 2nd Battalion 5th Marines and a numerically superior force of Islamic State of Iraq insurgents on the banks of a canal leading from Ramadi to Lake Habbaniyah in the Al Anbar province of Iraq.

Geographic entities mentioned:
surface_form: Lake Habbaniyah
instance_of: Lake
countries: Iraq
coordinates: lat: 32.296272222222
lon: 43.470725
In 1928, he took up a position as assistant professor in the laboratory for biogeochemical problems of the Academy of Sciences of the Soviet Union. He was the director of Vernadsky Institute of Geochemistry and Analytical Chemistry, Academy of Sciences of the Soviet Union (1947-1975). Mons Vinogradov, a mountain on the near side of the Moon, is named after him. So is a large crater on Mars.

Geographic entities mentioned:
surface_form: Mons Vinogradov
instance_of: Mountain
coordinates: lat: 22.35
lon: -32.52
Donats Mountain. Donats Mountain is a mountain located in the Catskill Mountains of New York south of Cobleskill. Mount Shank is located northwest, Warnerville Hill is located south-southeast, and Petersburg Mountain is located southeast of Donats Mountain.

Geographic entities mentioned:
surface_form: Mount Shank
instance_of: Mountain
countries: United States
coordinates: lat: 42.68313
lon: -74.49875
surface_form: Warnerville Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.644166666667
lon: -74.474722222222
surface_form: Petersburg Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.63313
lon: -74.44903
surface_form: donats mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.66146
lon: -74.48375
Donats Mountain. Donats Mountain is a mountain located in the Catskill Mountains of New York south of Cobleskill. Mount Shank is located northwest, Warnerville Hill is located south-southeast, and Petersburg Mountain is located southeast of Donats Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: donats mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.66146
lon: -74.48375
Donats Mountain. Donats Mountain is a mountain located in the Catskill Mountains of New York south of Cobleskill. Mount Shank is located northwest, Warnerville Hill is located south-southeast, and Petersburg Mountain is located southeast of Donats Mountain.

Geographic entities mentioned:
surface_form: donats mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.66146
lon: -74.48375
He was the son of Thomas and Louise (Nieman) Semon. His parents were born in (Germany) and immigrated to the United States when they were young. Semon grew up on his parents' Ohio farm, near Lake Erie. He attended public school in Port Clinton and then took work as a carpenter. He pursued that trade in Ohio until 1906 when he left for the west coast.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
While there, Semon became interested in modern farming practices and related technologies. After two years in Arizona, he moved to California's Imperial Valley to pursue those interests. He leased land there and planted a cantaloupe crop, but it was not a profitable venture so he returned to Los Angeles where he took up his carpentry trade once again.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
It is a couloir dominated by seracs continuously falling on it. Geography. The massif of the Grand Combin lies in Lower Valais, south of Verbier between the Val d'Entremont (west) and Val de Bagnes (west). The north-western facing side of Grand Combin is entirely covered by eternal snows and glaciers which are prone to serac falls.

Geographic entities mentioned:
surface_form: Val de Bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
surface_form: grand combin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.9375
lon: 7.2991666666667
surface_form: val de bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267
The southern and eastern walls are more steep and thus exempt of snow. The topography of the Grand Combin is intricate. Between the Val d'Entremont and the Val de Bagnes are two high ridges, nearly parallel to each other and to those valleys, which both diverge from a short transverse ridge of great height.

Geographic entities mentioned:
surface_form: Val de Bagnes
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.05
lon: 7.267