Sarmila/GeoWiki-Features huggingface dataset:
It is located in the western Santa Monica Mountains. Sandstone Peak, the highest peak in the range, and Boney Peak, are in the park with trails to their summits. Views can include the Channel Islands, Mount Baldy, and the Topatopa Mountains. The park was formerly Camp Circle X, a Boy Scout camp. The northeast section is adjacent to the Boney Mountain Wilderness in Point Mugu State Park.

Geographic entities mentioned:
surface_form: Sandstone Peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.1203
lon: -118.932
surface_form: Boney Peak
instance_of: Mountain
countries: United States
coordinates: lat: 34.1163
lon: -118.94
It is located in the western Santa Monica Mountains. Sandstone Peak, the highest peak in the range, and Boney Peak, are in the park with trails to their summits. Views can include the Channel Islands, Mount Baldy, and the Topatopa Mountains. The park was formerly Camp Circle X, a Boy Scout camp. The northeast section is adjacent to the Boney Mountain Wilderness in Point Mugu State Park.

Geographic entities mentioned:
surface_form: Mount Baldy
instance_of: Mountain
countries: United States
coordinates: lat: 34.2889
lon: -117.647
Arras Mountain. Arras Mountain is a mountain summit located in the Canadian Rockies of British Columbia, Canada. Arras Mountain is situated immediately northeast of the confluence of Icefall Brook with Valenciennes River, east-southeast of Rostrum Peak, and west of Valenciennes Mountain, and all are in the Kootenay Land District.

Geographic entities mentioned:
surface_form: Rostrum Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8307
lon: -117.1715
surface_form: Valenciennes Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.81667
lon: -117.00226
surface_form: arras mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8092
lon: -117.0822
surface_form: kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Arras Mountain. Arras Mountain is a mountain summit located in the Canadian Rockies of British Columbia, Canada. Arras Mountain is situated immediately northeast of the confluence of Icefall Brook with Valenciennes River, east-southeast of Rostrum Peak, and west of Valenciennes Mountain, and all are in the Kootenay Land District.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: arras mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8092
lon: -117.0822
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Arras Mountain. Arras Mountain is a mountain summit located in the Canadian Rockies of British Columbia, Canada. Arras Mountain is situated immediately northeast of the confluence of Icefall Brook with Valenciennes River, east-southeast of Rostrum Peak, and west of Valenciennes Mountain, and all are in the Kootenay Land District.

Geographic entities mentioned:
surface_form: arras mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8092
lon: -117.0822
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Geology. Arras Mountain is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.

Geographic entities mentioned:
surface_form: arras mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8092
lon: -117.0822
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Topographic relief is significant as the west aspect of the peak rises over above Icefall Brook in less than two kilometres. Climate. Based on the Köppen climate classification, Arras Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: arras mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8092
lon: -117.0822
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. The northwest aspect of the mountain conspicuously displays vertically-tilted anticlinal strata. Topographic relief is significant as the west aspect of the peak rises over above Icefall Brook in less than two kilometres. Climate.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Neuenfelde is part of the region &quot;Altes Land&quot;. The quarter borders in the North to the river Elbe and the Finkenwerder quarter of the borough of Hamburg-Mitte. In the West is the small quarter Cranz and the district of Stade of Lower Saxony In the south is the Neugraben-Fischbek quarter and the eastern bordern is to the quarter Francop.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The founders were an American missionary couple named Ruby and Orville Wiebe. Land for the school was donated by the American Baptist Foreign Mission Board who resided on the mission station near Stanley Pool (now Pool Malebo) on the Congo River. Until the school buildings were completed, the first classes were held in buildings on the mission station. With the assistance of the U.S.

Geographic entities mentioned:
surface_form: Pool Malebo
instance_of: Lake
countries: Republic of the Congo
Democratic Republic of the Congo
coordinates: lat: -4.2819444444444
lon: 15.488611111111
Geography. The Town of Phelps is located in the northeast corner of Vilas County along the border with Michigan. The headwaters of the Wisconsin River are in the northwest corner of the town at Lac Vieux Desert. Much of the town is a part of the Chequamegon-Nicolet National Forest.

Geographic entities mentioned:
surface_form: Lac Vieux Desert
instance_of: Lake
countries: United States
coordinates: lat: 46.137294
lon: -89.112605
To the southwest, WIS 17 connects to US Highway 45/WIS 32 and the rest of the Wisconsin State Highway System approximately north of Eagle River. County Trunk Highway E (CTH-E) begins in the Central business district of the unincorporated community of Phelps and runs northwest to serve the area around Lac Vieux Desert before ending at US 45/WIS 32 approximately south of Land o' Lakes.

Geographic entities mentioned:
surface_form: Lac Vieux Desert
instance_of: Lake
countries: United States
coordinates: lat: 46.137294
lon: -89.112605
The lake is fed by 52 inflowing rivers, the four main ones being the Msta, the Pola, the Lovat, and the Shelon. It is drained through a single outlet, the Volkhov, into Lake Ladoga, and subsequently via the Neva into the Gulf of Finland. The source of the Volkhov is marked by the Peryn Chapel built in the 1220s.

Geographic entities mentioned:
surface_form: Lake Ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: lake ladoga
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
Lake Ilmen. Lake Ilmen (,) is a large lake in Novgorod Oblast, Russia. A historically important lake, it formed a vital part of the medieval trade route from the Varangians to the Greeks. The city of Veliky Novgorod, which is a major trade center of the route, lies below the lake's sole outflow, via the Volkhov River.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
surface_form: lake ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Lake Ilmen. Lake Ilmen (,) is a large lake in Novgorod Oblast, Russia. A historically important lake, it formed a vital part of the medieval trade route from the Varangians to the Greeks. The city of Veliky Novgorod, which is a major trade center of the route, lies below the lake's sole outflow, via the Volkhov River.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
surface_form: lake ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Lake Ilmen. Lake Ilmen (,) is a large lake in Novgorod Oblast, Russia. A historically important lake, it formed a vital part of the medieval trade route from the Varangians to the Greeks. The city of Veliky Novgorod, which is a major trade center of the route, lies below the lake's sole outflow, via the Volkhov River.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The city of Veliky Novgorod, which is a major trade center of the route, lies below the lake's sole outflow, via the Volkhov River. According to Max Vasmer's &quot;Etymological Dictionary&quot;, the name of the lake originates from Finnic &quot;Ilmajärvi&quot;, which means &quot;air lake&quot;. Thanks to Novgorodian colonisation, many lakes in Russia have names deriving from Lake Ilmen.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ilmajärvi
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
The city of Veliky Novgorod, which is a major trade center of the route, lies below the lake's sole outflow, via the Volkhov River. According to Max Vasmer's &quot;Etymological Dictionary&quot;, the name of the lake originates from Finnic &quot;Ilmajärvi&quot;, which means &quot;air lake&quot;. Thanks to Novgorodian colonisation, many lakes in Russia have names deriving from Lake Ilmen.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
surface_form: lake ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Thanks to Novgorodian colonisation, many lakes in Russia have names deriving from Lake Ilmen. Yuri Otkupshchikov has argued that the presence of the name &quot;Ilmen&quot; in Southern Russia cannot be explained by Novgorodian colonisation alone, and proposed a Slavic etymology instead. The average surface area of the lake is (it may vary between and depending on water level).

Geographic entities mentioned:
surface_form: ilmen
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 58.266666666667
lon: 31.283333333333
Yuri Otkupshchikov has argued that the presence of the name &quot;Ilmen&quot; in Southern Russia cannot be explained by Novgorodian colonisation alone, and proposed a Slavic etymology instead. The average surface area of the lake is (it may vary between and depending on water level). The lake is fed by 52 inflowing rivers, the four main ones being the Msta, the Pola, the Lovat, and the Shelon.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The 16th-century Tibetan Buddhist author Taranatha mentions Chanakya as one of Bindusara's &quot;great lords&quot;. According to him, Chanakya destroyed the nobles and kings of 16 towns and made Bindusara the master of all the territory between the eastern and the western seas (Arabian Sea and the Bay of Bengal). Source.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
These contain about 74 volcanoes with post-glacial activity; they include both monogenetic volcanoes, stratovolcanoes and volcanic complexes. Llaima and Villarrica are among the most active of these volcanoes. The Southern and Austral volcanic zones are separated by a gap without volcanic activity, close to the Chile Triple Junction.

Geographic entities mentioned:
surface_form: Llaima
instance_of: Mountain
countries: Chile
coordinates: lat: -38.697407
lon: -71.730445
surface_form: villarrica
instance_of: Mountain
countries: Chile
coordinates: lat: -39.42
lon: -71.939166666667
surface_form: villarrica
instance_of: Lake
countries: Chile
coordinates: lat: -39.25
lon: -72.083333333333
The movement between the South America Plate and the Scotia Plate is taken up by strike-slip faulting. In terms of composition, Lautaro, Aguilera and Viedma form one group distinct from Burney, and Reclus lies between these two. southeast of Monte Burney lies Fueguino, a volcanic field with possible historical activity in 1820 and 1712. Fueguino is the southernmost Holocene volcano in the Andes.

Geographic entities mentioned:
surface_form: Fueguino
instance_of: Mountain
countries: Chile
coordinates: lat: -54.95
lon: -70.25
surface_form: fueguino
instance_of: Mountain
countries: Chile
coordinates: lat: -54.95
lon: -70.25
surface_form: fueguino
instance_of: Mountain
countries: Chile
coordinates: lat: -54.95
lon: -70.25
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Holocene eruptions have near-identical composition. Minerals found in Burney rocks include amphibole, plagioclase and pyroxene; foreign components include clinopyroxene and olivine crystals as well as granite xenoliths stemming from the Patagonian batholith. Magnesium-poor adakites have been found at Monte Burney. Fueguino volcanic rocks also include adakites but these are richer in magnesium.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
The movement between the South America Plate and the Scotia Plate is taken up by strike-slip faulting. In terms of composition, Lautaro, Aguilera and Viedma form one group distinct from Burney, and Reclus lies between these two. southeast of Monte Burney lies Fueguino, a volcanic field with possible historical activity in 1820 and 1712. Fueguino is the southernmost Holocene volcano in the Andes.

Geographic entities mentioned:
surface_form: lautaro
instance_of: Mountain
countries: Chile
coordinates: lat: -49.019
lon: -73.504
surface_form: reclus
instance_of: Mountain
countries: Chile
coordinates: lat: -50.9639
lon: -73.5847
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Fueguino is the southernmost Holocene volcano in the Andes. Large explosive eruptions have occurred at Aguilera, Reclus and Burney but due to the long distance between these volcanoes and critical infrastructure they are considered a low hazard. A wide caldera lies in the area, which is partly filled by pyroclastic flows. Some of these flows extend outside the caldera.

Geographic entities mentioned:
surface_form: reclus
instance_of: Mountain
countries: Chile
coordinates: lat: -50.9639
lon: -73.5847
surface_form: aguilera
instance_of: Mountain
countries: Chile
coordinates: lat: -50.402222222222
lon: -73.788055555556
Research history. The appearance of the mountain was considered &quot;majestic&quot; in 1899. Eric Shipton explored the area in 1962, and after a failed attempt in 1963 climbed Monte Burney on 10 March 1973, reaching its summit together with Peter Radcliffe and Roger Perry. Auer in 1974 did correlate some tephras on Tierra del Fuego with Monte Burney, one of which was later linked to Reclus.

Geographic entities mentioned:
surface_form: reclus
instance_of: Mountain
countries: Chile
coordinates: lat: -50.9639
lon: -73.5847
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Llaima and Villarrica are among the most active of these volcanoes. The Southern and Austral volcanic zones are separated by a gap without volcanic activity, close to the Chile Triple Junction. The strongest volcanic eruption in the region occurred 7,750 years before present at Cerro Hudson volcano, which deposited tephra all over southern Patagonia and Tierra del Fuego.

Geographic entities mentioned:
surface_form: hudson volcano
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
surface_form: cerro hudson
instance_of: Mountain
countries: Chile
coordinates: lat: -45.92
lon: -72.95
Monte Burney. Monte Burney is a volcano in southern Chile, part of its Austral Volcanic Zone which consists of six volcanoes with activity during the Quaternary. This volcanism is linked to the subduction of the Antarctic Plate beneath the South America Plate and the Scotia Plate. Monte Burney is formed by a caldera with a glaciated stratovolcano on its rim.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Monte Burney is a volcano in southern Chile, part of its Austral Volcanic Zone which consists of six volcanoes with activity during the Quaternary. This volcanism is linked to the subduction of the Antarctic Plate beneath the South America Plate and the Scotia Plate. Monte Burney is formed by a caldera with a glaciated stratovolcano on its rim. This stratovolcano in turn has a smaller caldera.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
It is one of the many English language placenames in the region, which are the product of the numerous English research expeditions such as these by Robert FitzRoy and Phillip Parker King in 1825–1830. Geography and geomorphology. Monte Burney is on the northwest Muñoz Gomera Peninsula. This area lies in the Patagonian region of Chile, which is known for its spectacular fjords.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
A wide caldera lies in the area, which is partly filled by pyroclastic flows. Some of these flows extend outside the caldera. On the western rim of the caldera, the high Monte Burney volcano developed. It is not a simple volcanic cone, has its own summit caldera with a crescent of spires, and a steep wall on the northern side with uncertain origin.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Such a limited range of composition is typical for these volcanoes but might reflect the small amount of research conducted on them. Tephras of rhyolitic composition were generated by Monte Burney during the Pleistocene, according to compositional data. Holocene eruptions have near-identical composition.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Fueguino volcanic rocks also include adakites but these are richer in magnesium. These adakitic magmas reflect the subduction of a relatively hot and young Antarctic Plate. In the case of Monte Burney, these magmas then underwent some fractionation during ascent, as it was retarded by the tectonic regimen, which is somewhat compressive. Eruptive history.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Eruptive history. Eruptions occurred at Monte Burney during the Pleistocene. Two eruptions around 49,000 ± 500 and 48,000 ± 500 years before present deposited tephra in Laguna Potrok Aike, a lake approximately east of Monte Burney; there they reach thicknesses of and respectively.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Other Pleistocene eruptions are recorded there at 26,200 and 31,000 years ago, with additional eruptions having occurred during marine isotope stage 3. Holocene tephras from Monte Burney have also been found in this lake. According to the Potrok Aike record, Monte Burney may be the most active volcano in the region during the late Quaternary.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Holocene tephras from Monte Burney have also been found in this lake. According to the Potrok Aike record, Monte Burney may be the most active volcano in the region during the late Quaternary. Radiocarbon dating and tephrochronology has evidenced Holocene activity at Burney.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
These ashes have also been found at Lake Arturo, the first discovery of them in the Argentine Tierra del Fuego, and in coastal sediment cores and dunes on Tierra del Fuego. Further findings were made at Ushuaia, Brunswick Peninsula, a number of other sites and for MB1 on the Falklands Islands about away from Monte Burney.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Further eruptions occurred 90 ± 100, 800 ± 500, 3,740 ± 10, 7,390 ± 200 BCE, and 1,529 ± 28, 1,944 ± 29, 10,015 and 1,735 years before present. The last two were small eruptions. Some of these eruptions have left traces in cave deposits south of Monte Burney. Tephra from an eruption that occurred about 2,000 years before present reached a thickness of in a peat bog away from Monte Burney.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
The last two were small eruptions. Some of these eruptions have left traces in cave deposits south of Monte Burney. Tephra from an eruption that occurred about 2,000 years before present reached a thickness of in a peat bog away from Monte Burney. One tephra around 1805 BCE found at the Siple Dome in Antarctica may be linked to Monte Burney but the timing of the tephra is problematic.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
One tephra around 1805 BCE found at the Siple Dome in Antarctica may be linked to Monte Burney but the timing of the tephra is problematic. Two tephras at Fiordo Vogel and Seno Skyring have been linked to Monte Burney; they are dated 4,254 ± 120 and 9,009 ± 17 - 9,175 ± 111 years before present.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
A reworked tephra identified at Hooker's Point, East Falkland, may come from a mid-Holocene eruption that took place between the MB1 and MB2 events. Reports from natives, mentioned in 1847, of a volcano at the end of a bay that makes the ground tremble probably refer to Monte Burney, which is visible on clear days from.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
This eruption appeared to coincide with an earthquake and tsunami on 24 June 1910 in the area. An unconfirmed report of an eruption in 1920 exists, as well as reports of a flash of light and earthquakes during the night of 24 June 1970. No reports of such activity were identified in the contemporaneous newspaper ', however. Shallow seismic activity occurs to this day at Monte Burney. Climate.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Research history. The appearance of the mountain was considered &quot;majestic&quot; in 1899. Eric Shipton explored the area in 1962, and after a failed attempt in 1963 climbed Monte Burney on 10 March 1973, reaching its summit together with Peter Radcliffe and Roger Perry. Auer in 1974 did correlate some tephras on Tierra del Fuego with Monte Burney, one of which was later linked to Reclus.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Auer in 1974 did correlate some tephras on Tierra del Fuego with Monte Burney, one of which was later linked to Reclus. In 2015 the Chilean geological agency SERNAGEOMIN began setting up volcano monitoring equipment on Monte Burney, the first volcano in the Magallanes Patagonia region to be monitored.

Geographic entities mentioned:
surface_form: monte burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
Nearby sites of interest. Not far from Hānaiakamalama is the Pali Lookout, site of the battle of Nuʻuanu Pali, where Kamehameha I defeated the forces of the King of Oahu, consolidating his claim as monarch of the Hawaiian Islands.

Geographic entities mentioned:
surface_form: Nuʻuanu Pali
instance_of: Landform
countries: United States
coordinates: lat: 21.370277777778
lon: -157.79694444444
Kamień Lagoon. Kamień Lagoon is a lagoon on the Oder River in north-western Poland. It is part of the Dziwna. Both the lagoon and the Dziwna are part of Poland's internal waters. Several settlements lie on the shores of the lagoon, notably (in order of population) Kamień Pomorski, Dziwnów, Międzywodzie, Wrzosowo and Dziwnówek.

Geographic entities mentioned:
surface_form: kamień lagoon
instance_of: Body of water
countries: Poland
coordinates: lat: 53.9903
lon: 14.7486
There are also three small villages on Chrząszczewska Island: Chrząszczewo, Chrząszczewko and Buniewice. Until 1945, the lagoon was referred to by its German name of &quot;Camminer Bodden&quot;. In 1949, it officially became called &quot;Kamieński Zalew&quot;, and in 1991 the words in its name were reversed, its new name being &quot;Zalew Kamieński&quot;.

Geographic entities mentioned:
surface_form: zalew kamieński
instance_of: Body of water
countries: Poland
coordinates: lat: 53.9903
lon: 14.7486
He took part in the Battle of Tulagi and 3rd Defense Battalion under his command successfully hit three enemy ships that had beached themselves to land troops. He later took part in the Battle for Henderson Field at the end of October 1942 and his battalion defensed the Lunga Point against the enemy counterattack from the sea.

Geographic entities mentioned:
surface_form: Lunga Point
instance_of: Landform
countries: Solomon Islands
coordinates: lat: -9.416666666666666
lon: 160.03333333333333
Allen Creek (Scotland County, Missouri). Allen Creek is a stream in Scotland County, Missouri. A variant name was &quot;Allens Branch&quot;. The creek has the name of the local Allen family.

Geographic entities mentioned:
surface_form: allen creek
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
Allen Creek (Scotland County, Missouri). Allen Creek is a stream in Scotland County, Missouri. A variant name was &quot;Allens Branch&quot;. The creek has the name of the local Allen family.

Geographic entities mentioned:
surface_form: allen
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
As of July 2022, Kajaki Dam generates up to 151 MW of electricity. Water supply accord. Under an accord signed between Afghanistan and Iran in 1973, Afghanistan agreed to release water at a rate of at least. In 1998, Afghanistan briefly stopped the flow of water to Iran, using a canal to divert water of Helmand River southward into the Godzareh Depression.

Geographic entities mentioned:
surface_form: Godzareh Depression
instance_of: Lake
countries: Afghanistan
coordinates: lat: 29.835278
lon: 61.941667
In 1998, Afghanistan briefly stopped the flow of water to Iran, using a canal to divert water of Helmand River southward into the Godzareh Depression. As a result, the Hamun Lake dried up, as did regional pastures, leading to a decline of flora, fauna, cattle and birds in the northern part of the Sistan and Baluchestan Province of Iran.

Geographic entities mentioned:
surface_form: Hamun Lake
instance_of: Group of lakes
countries: Iran
Afghanistan
coordinates: lat: 30.7653
lon: 61.6372
Kura bleak. The Kura bleak (&quot;Alburnus filippii&quot;) is a species of ray-finned fish in the genus &quot;Alburnus&quot;. It is native to the Caspian Sea basin, from the Kura River and Aras River in the east to the Sefīd-Rūd in Iran.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Torfmoorsee. Torfmoorsee is a lake in North Rhine-Westphalia, Germany. At an elevation of, its surface area is 0.48 km2.

Geographic entities mentioned:
surface_form: torfmoorsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.283888888889
lon: 7.5638888888889
Topographic relief is significant as the north aspect rises above Uncompahgre Gorge in 1.5 mile. Historic mines are located on the slopes of Abrams Mountain. This iconic feature of the Ouray landscape can be seen for many miles while driving Highway 550 south from Montrose toward Ouray, and it dominates the San Juan Skyway from Red Mountain Pass to Ironton Park. Etymology.

Geographic entities mentioned:
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.4867
lon: -86.8064
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.3918
lon: -121.145
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.60041
lon: -120.98678
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.5231
lon: -111.876
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.415277777778
lon: -121.46694444444
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.45588
lon: -121.3891607
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.064444444444
lon: -117.24638888889
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.2979
lon: -119.441
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.26751
lon: -74.54952
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.5356
lon: -113.424
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.1122
lon: -105.181
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.9036
lon: -107.702
surface_form: red mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.9783
lon: -110.872
The name commemorates Abram Cutler (born November 2, 1832), the first judge of Ouray County and notary public who administered the oath to Ouray's original town board. Originally a civil engineer, he assisted Ferdinand Vandeveer Hayden with the 1874 survey of this area, so the possibility exists that Hayden named the mountain to honor Cutler.

Geographic entities mentioned:
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
It is situated four miles south of the town of Ouray, on land managed by Uncompahgre National Forest. It is part of the San Juan Mountains, which are a subset of the Rocky Mountains, and is west of the Continental Divide. Topographic relief is significant as the north aspect rises above Uncompahgre Gorge in 1.5 mile. Historic mines are located on the slopes of Abrams Mountain.

Geographic entities mentioned:
surface_form: uncompahgre gorge
instance_of: Landform
countries: United States
coordinates: lat: 38.0189
lon: -107.676
Abrams Mountain. Abrams Mountain, also known as Mount Abram or Mount Abrams, is a mountain summit located on the shared boundary of Ouray County with San Juan County in southwest Colorado, United States. It is situated four miles south of the town of Ouray, on land managed by Uncompahgre National Forest.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: abrams mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.962222222222
lon: -107.64055555556
Abrams Mountain. Abrams Mountain, also known as Mount Abram or Mount Abrams, is a mountain summit located on the shared boundary of Ouray County with San Juan County in southwest Colorado, United States. It is situated four miles south of the town of Ouray, on land managed by Uncompahgre National Forest.

Geographic entities mentioned:
surface_form: abrams mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.962222222222
lon: -107.64055555556
Topographic relief is significant as the north aspect rises above Uncompahgre Gorge in 1.5 mile. Historic mines are located on the slopes of Abrams Mountain. This iconic feature of the Ouray landscape can be seen for many miles while driving Highway 550 south from Montrose toward Ouray, and it dominates the San Juan Skyway from Red Mountain Pass to Ironton Park. Etymology.

Geographic entities mentioned:
surface_form: abrams mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.962222222222
lon: -107.64055555556
Climate. According to the Köppen climate classification system, Abrams Mountain is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring. Precipitation runoff from the mountain drains into the Uncompahgre River.

Geographic entities mentioned:
surface_form: abrams mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.962222222222
lon: -107.64055555556
Monument to the Unknown Soldier, Lima. The Monument to the Unknown Soldier is a memorial located on a plain on the slopes of the northern side of Morro Solar in the district of Chorrillos, in Lima, Peru. It is dedicated to those killed during the War of the Pacific. History. It was built during the second government of President Augusto B. Leguía, as part of an urban program to modernize the city.

Geographic entities mentioned:
surface_form: Morro Solar
instance_of: Mountain
countries: Peru
coordinates: lat: -12.18345
lon: -77.031872222222
The population was 3,244 at the 2020 census. It is home to Wellington State Park, Sugar Hill State Forest, and Profile Falls on the Smith River. Surrounded by hills and lakes, Bristol includes the lower two-thirds of Newfound Lake, a resort area. The primary settlement in town, where 1,911 people resided at the 2020 census, is defined by the U.S.

Geographic entities mentioned:
surface_form: Newfound Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.662778
lon: -71.775278
The town of Beekman, Dutchess County, New York, is named for his son, Col. Henry Beekman, who owned a grant there in 1703, known as the Beekman Patent. In the Rhinebeck Village Historic District is the Beekman Arms Inn, claimed to be the oldest continuously-operated inn in the United States. The historic hotel in the Hudson Valley has operated continuously since 1766.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Sauroconcha caperteeana. &quot;Sauroconcha caperteeana&quot; is a species of air-breathing land snails, terrestrial pulmonate gastropod molluscs in the family Camaenidae. The species was first described in 2008 by Weihong Zhang and Michael Shea. It is found in the Capertee Valley of New South Wales, in rocky outcrops where it lives, under and among rocks.

Geographic entities mentioned:
surface_form: Capertee Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.0483
lon: 150.134
It is the seat of government of the district of Garmisch-Partenkirchen (abbreviated &quot;GAP&quot;), in the Oberbayern region, which borders Austria. Nearby is Germany's highest mountain, Zugspitze, at above sea level. The town is known as the site of the 1936 Winter Olympic Games, the first to include alpine skiing, and hosts a variety of winter sports competitions. History.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
In addition there are special seasonal long-distance services, including ICEs, to Berlin, Hamburg, Dortmund, Bremen and Innsbruck. It is the terminus of the Außerfern Railway to Reutte in Tirol / Kempten im Allgäu and the Bavarian Zugspitze Railway (with sections of rack railway) to the Zugspitze, the highest mountain in Germany.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
There are several accessible high and low-level hiking trails from the town that have especially good views. Sports. Garmisch-Partenkirchen is a favoured holiday spot for skiing, snowboarding, and hiking, having some of the best skiing areas (Garmisch Classic and Zugspitze) in Germany. It was the site of the 1936 Winter Olympics, the first to feature alpine skiing.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Points of interest. South of Partenkirchen is the Partnach Gorge, where the Partnach river surges spectacularly through a narrow, gap between high limestone cliffs. The Zugspitze (local name &quot;Zugspitz&quot;) is south of Garmisch near the village of Grainau. The highest mountain in Germany, it actually straddles the border with Austria.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Vistulan dialect. The Vistulan dialect () was a dialect of Low Prussian, which belongs to Low German. The dialect was spoken in West Prussia (today in Poland) around Zarnowitzer See, Danzig and Graudenz. It had a border to Mundart der Weichselwerder. It is related to Nehrungisch. Geography.

Geographic entities mentioned:
surface_form: Zarnowitzer See
instance_of: Lake
countries: Poland
coordinates: lat: 54.763
lon: 18.053
It had a border to Mundart der Weichselwerder. It is related to Nehrungisch. Geography. East Pomeranian had a border to Low Prussian according to Ē- and Ō-vowels running from Zarnowitzer See via Karthaus, West of Schöneck, to Preußisch-Stargard, to Bromberg and south of Vistula to East of Thorn. In West Prussian Kulmerland, East Pomeranian was spoken to Wąbrzeźno, Radzyń Chełmiński and Łasin.

Geographic entities mentioned:
surface_form: Zarnowitzer See
instance_of: Lake
countries: Poland
coordinates: lat: 54.763
lon: 18.053
The border of difference between a differentiation of nominative/accusative versus dative forms among strong masculine and neutral plurals ran from Lake Gardno (Garder See) to Kościerzyna (Berent) to Kartuzy (Karthaus) via Skarszewy (Schöneck) to Świecie (Schwetz).

Geographic entities mentioned:
surface_form: Lake Gardno
instance_of: Lake
countries: Poland
coordinates: lat: 54.653888888889
lon: 17.112222222222
The border of realization of Middle Low German i and u as e respectively o apart from before Low German nt, ng nk and g for example &quot;op&quot; ran from Łebsko Lake (Lebasee), West of Lębork (Lauenburg)-Bytów (Bütow)-Kruschinsee-West of Starogard Gdański (Preußisch Stargard)-South and West of Vistula river.

Geographic entities mentioned:
surface_form: Łebsko Lake
instance_of: Lake
countries: Poland
coordinates: lat: 54.713611111111
lon: 17.408888888889
Gettysburg Railroad Station), and President Woodrow Wilson used the Round Top Branch to depart the Great Camp on his special train. Similarly, President Franklin D. Roosevelt's southbound train passed the Eternal Light Peace Memorial and stopped at a special station from where he motored to Oak Hill to dedicate the memorial during the 1938 Gettysburg reunion.

Geographic entities mentioned:
surface_form: Oak Hill
instance_of: Landform
countries: United States
coordinates: lat: 39.8867
lon: -77.2342
(In the mid 1990s the line's junction at Gettysburg was moved west to Seminary Ridge.) In 1996 the line was purchased by the RailAmerica subsidiary, Delaware Valley Railroad Company, which created a new operating company, Gettysburg Railway, that included Gettysburg Scenic Rail Tours. The line was sold October 1997 to John H. Marino, who operated the line until 2001.

Geographic entities mentioned:
surface_form: Seminary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 39.2536
lon: -77.2536
Indigenous peoples and European exploration. With the draining of the Champlain Sea around 10,000 years ago the Ottawa Valley became habitable. The Algonquin people (Anishinaabe) who call the Ottawa River the &quot;Kichi Sibi&quot; or &quot;Kichissippi&quot; meaning &quot;Great River&quot; or &quot;Grand River&quot; maintained a trade route along the Ottawa River for a relatively short time.

Geographic entities mentioned:
surface_form: Ottawa Valley
instance_of: Valley
countries: Canada
coordinates: lat: 45.91682
lon: -77.13276
The word &quot;Ottawa&quot; is in relation to the Ottawa people, the First Nation who hunted, camped, traded, and traveled in the area, and also lived far to the west along Georgian Bay and Lake Huron. When Étienne Brûlé in 1610 became the first European to travel up the Ottawa River, followed by Samuel de Champlain in 1613, they were assisted by Algonquin guides.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
The Algonquin were not the only people in present-day Ontario. During the 17th century, the Algonquians and Hurons fought a bitter war against the Iroquois. Champlain's travels brought him to Lake Nipissing and Georgian Bay to the center of Huron country near Lake Simcoe. During these voyages, Champlain aided the Hurons in their battles against the Iroquois Confederacy.

Geographic entities mentioned:
surface_form: Lake Nipissing
instance_of: Lake
countries: Canada
coordinates: lat: 46.283333333333
lon: -80
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Promotion. The song's release was accompanied by a music video filmed in various landmarks around Greece, including the Acropolis, Plaka, Monastiraki, the Odeon of Herodes Atticus, Omonoia, Mount Lycabettus, Rafina and the Athens International Airport.

Geographic entities mentioned:
surface_form: Mount Lycabettus
instance_of: Mountain
countries: Greece
coordinates: lat: 37.981944444444
lon: 23.743055555556
The local environment is one of the primary assets because it attracts numerous hikers wishing to practise hiking across this valley. The village is 20 km away from Sierra de Francia and is near other villages like San Martín del Castañar, La Alberca o Miranda del Castañar, Bejar and places like Peña de Francia.

Geographic entities mentioned:
surface_form: Sierra de Francia
instance_of: Mountain
countries: Spain
coordinates: lat: 40.55
lon: -6.1
surface_form: Peña de Francia
instance_of: Mountain
countries: Spain
coordinates: lat: 40.512777777778
lon: -6.1688888888889
Location. The Rio Flor do Prado Ecological Station has an area of in the municipality of Aripuanã, Mato Grosso. It is to the east of the Roosevelt River. The area is on the right bank of the Flor do Prado River, a tributary of the Roosevelt River, and is bordered by indigenous territories. It is in the Amazon biome. It has just over 66% open rainforest and about 34% dense rainforest. Conservation.

Geographic entities mentioned:
surface_form: Flor do Prado River
instance_of: Watercourse
countries: Brazil
coordinates: lat: -10.713075
lon: -60.446436
Helmer House Inn. The most notable structure within the community of Helmer is the Helmer House Inn, which is located along Helmer Creek just north of Manistique Lake at 2747 Helmer Road (County Road 377). The building was constructed in 1881–1882 as a mission house and manse by Roy Mills of the Presbyterian church from Newberry.

Geographic entities mentioned:
surface_form: Manistique Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2347
lon: -85.784
Helmer sits at an elevation of above sea level. Helmer is located along the northeast shores of Manistique Lake along H-33 (Manistique Lakes Road) and the western terminus of H-44 (Ten Curves Road). Aside from Newberry, the nearest sizable communities include McMillan to the north, Curtis to the south, Engadine to the southeast, and Germfask and Seney to the west.

Geographic entities mentioned:
surface_form: Manistique Lake
instance_of: Lake
countries: United States
coordinates: lat: 46.2347
lon: -85.784
There is some slight evidence for Viking use of the area, at least as a seasonal camp, as the Danes of Limerick made a number of devastating raids in the area in the 9th and 10th centuries, and though the annalistic evidence is ambiguous, seem to have made some sort of semi-permanent camp along the river or in Lough Corrib.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
It was first created in a redistribution ahead of the 1888 colonial election, and existed until the 1912 state election. Woothakata electorate covered the western Atherton Tableland and the total catchment area of the Mitchell River on lower Cape York Peninsula, including the towns of Chillagoe and Herberton.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Before North Korea announced they had conducted the test, seismic activity had already been detected in North Korea by the United States Geological Survey (USGS) and the seismic network operated by the Comprehensive Nuclear-Test-Ban Treaty Organization (CTBTO) Preparatory Commission, near the site of previous nuclear tests at Mantapsan in Kilju County.

Geographic entities mentioned:
surface_form: Mantapsan
instance_of: Mountain
countries: North Korea
coordinates: lat: 41.29861111
lon: 129.08166667