Sarmila/GeoWiki-Features huggingface dataset:
The Bransfield Strait, the result of this extension, is presumed to be four million years old or less; magnetic anomalies created by the formation of new basaltic crust and aligned with the axis of the Bransfield Rift indicate that the newly formed oceanic crust in the Bransfield Strait is roughly 1.3 million years old.

Geographic entities mentioned:
surface_form: Bransfield Strait
instance_of: Body of water
countries: Antarctica
coordinates: lat: -63
lon: -59
Campus. The school includes 79 learning spaces, specialist learning spaces, sports courts, car parking, an indigenous garden and a wetlands walk. A multipurpose hall is located on the campus and is stated to be the largest indoor community multi-sport and entertainment facility in the Northern Tablelands. Armidale Intensive English Centre.

Geographic entities mentioned:
surface_form: Northern Tablelands
instance_of: Plateau
countries: Australia
coordinates: lat: -30.595277777777778
lon: 151.5
Ajuran Empire. In the mid-17th century, the Oromos began expanding from their homeland around Lake Abaya in southern Ethiopia towards the southern Somali coast while the Ajuran Empire was at the height of its power. The Garen rulers conducted several military expeditions, known as the &quot;Gaal Madow&quot; wars, against the Oromo warriors.

Geographic entities mentioned:
surface_form: Lake Abaya
instance_of: Lake
countries: Ethiopia
coordinates: lat: 6.236
lon: 37.832
Lake Eleyele is located at the northwestern part of the city, while the Osun River, Asejire Lake bounds the city to the east and the fifth rivers boundary Ibadan with other Oke-Oguns towns, witch call Odo-ogun Rivers across Lagos State, Ogun State, Osun State, Iseyin Town and Eruwa Town boundary to Ibadan. Climate.

Geographic entities mentioned:
surface_form: Asejire Lake
instance_of: Lake
countries: Nigeria
coordinates: lat: 7.36694444
lon: 4.13333333
Many streams and ephemeral creeks head in springs or disappear into sinkholes. Geology. Geologically, southwestern Utah is at the margin between the geologic provinces known as the Colorado Plateau and the Basin and Range Province, the former of which features flat lying sediments while the latter is characterized by steep horsts and grabens.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
After the Oligocene and Miocene, during which volcanism was characterized by calderas and stratovolcanoes, beginning 8 million years ago smaller volumes of mostly mafic magma formed lava domes, shield volcanoes, volcanic cones and volcanic plugs. The Markagunt Plateau is part of the High Plateaus geologic province, in the Colorado Plateau and at its margins with the Basin and Range Province.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
During the Pleistocene, the Bull Lake glaciation and the Pinedale glaciation took place on the Markagunt Plateau and eroded and buried some lava flows. Hazards. Large volcanic eruptions in the 1980s such as Mount St. Helens raised public awareness about the dangers emanating from volcanic activity.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: mount st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
surface_form: st. helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Midway Valley sits at an elevation of 9800 feet (2987 m) and has a subalpine climate (Köppen &quot;Dfc&quot;). There is another SNOTEL weather station north of Midway Valley along the Brian Head-Panguitch Lake Scenic Byway, roughly halfway between Panguitch Lake and Brian Head. Eruption history. Volcanism in the Markagunt volcanic field occurred in three stages.

Geographic entities mentioned:
surface_form: brian head
instance_of: Mountain
countries: United States
coordinates: lat: 37.681111111111
lon: -112.83138888889
surface_form: brian head
instance_of: Mountain
countries: United States
coordinates: lat: 37.681111111111
lon: -112.83138888889
Formed in a region of older volcanics, it consists of several cinder cones and associated lava flows. Some of the lava flows feature lava tubes such as Mammoth Cave, while others have formed lava dams and lakes like Navajo Lake. Volcanism took place during the Pliocene and latest Pleistocene but may have continued into the Holocene; legends of the Southern Paiute may reflect past eruptions.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Towns in the area include Duck Creek Village and Mammoth Creek. The volcanic field is on a plateau bordered to the south by the Pink Cliffs and to the west by the cliffs of Cedar Breaks National Monument, and features lava flows and over 25 cinder cones mostly between Panguitch Lake and Navajo Lake although older volcanics occur south of Panguitch.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
Lava flows almost reach Panguitch Lake. Lava flows have blocked surface drainages, forming Navajo Lake which drains underground into two watersheds and was later further dammed by humans; another lava-dammed lake downstream from Navajo Lake is now a meadow and Blue Spring Valley also saw the development of lava dams.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: spring valley
instance_of: Valley
countries: United States
surface_form: spring valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9968
lon: -123.12
The Markagunt Plateau is considered to be a low-risk volcano. Renewed activity may impact the reservoir and popular recreation site of Navajo Lake less than south of the Markagunt Plateau volcanic field as well as Utah State Route 14 and U.S. Route 89 which are constructed across lava flows from the volcanic field.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
On the Miller Knoll flows, surface exposure dating has yielded ages of 38,000 - 36,000 years ago for the middle member and of 34,000 ± 4,000 and 32,000 ± 3,000 for two other flows which are likely of the same age. The middle member is overlaid by the Dry Valley flow which is also younger than the other two flows.

Geographic entities mentioned:
surface_form: dry valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2478257
lon: -90.9673466
Markagunt Plateau. Markagunt Plateau is a volcanic field in southern Utah, United States. Formed in a region of older volcanics, it consists of several cinder cones and associated lava flows. Some of the lava flows feature lava tubes such as Mammoth Cave, while others have formed lava dams and lakes like Navajo Lake.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Geography and geomorphology. The Markagunt Plateau is in southern Utah in the counties Iron County, Garfield County and Kane County. Cedar City lies west and Kanab south of the volcanic field, which is crossed by Utah State Route 14, Utah State Route 143 and Utah State Route 148. Towns in the area include Duck Creek Village and Mammoth Creek.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Past glaciation has eroded some vents. Some recent vents formed along lineaments and faults; this includes the chain of over 19 cinder cones that generated the Henrie Knolls flows. Lava flows in the Markagunt Plateau are blocky and have flow fronts which reach heights of; many were erupted from fissure vents.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Lava flows in the Markagunt Plateau are blocky and have flow fronts which reach heights of; many were erupted from fissure vents. Some of the lava flows of Markagunt Plateau are among the youngest in Utah; these are sparsely vegetated and blocky, while others are cut by streams and stream terraces.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Some of the lava flows of Markagunt Plateau are among the youngest in Utah; these are sparsely vegetated and blocky, while others are cut by streams and stream terraces. Bowers Cave and Mammoth Cave are lava tubes set in lava flows on the Markagunt Plateau, the long Duck Creek Lava Tube is among the longest and highest lava tubes in the United States.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
As a consequence, water on the Markagunt Plateau flows underground through sinkholes developed in limestone rocks, and the burial of surface drainages by highly permeable lava flows likely aided in their development; some sinkholes have formed in basalt and other karstic features are also found in the volcanic field. Many streams and ephemeral creeks head in springs or disappear into sinkholes.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Composition. Volcanic rocks erupted on the Markagunt Plateau range from alkali basalt over basalt and basaltic andesite to andesite and latite, and define calc-alkaline and tholeiitic suites which appear to become more silicic over time. Phenocrysts include clinopyroxene, olivine and plagioclase, with not all minerals present in all flows.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Phenocrysts include clinopyroxene, olivine and plagioclase, with not all minerals present in all flows. Volcanic rocks at Markagunt Plateau are unusual for the common occurrence of subalkaline volcanics; most other recent volcanic centres in the Basin and Range Province have produced alkali basalts.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Eruption history. Volcanism in the Markagunt volcanic field occurred in three stages. The first stage saw activity mainly at the margins of the Markagunt Plateau between 5.3 and 2.8 million years ago; the cinder cones and lava flows produced during this stage are heavily eroded.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
Aside from volcanism, landsliding, aeolian, alluvial fan and floodplain sedimentation took place in the area, beavers built beaver dams on watercourses and peat accumulated at several sites. During the Pleistocene, the Bull Lake glaciation and the Pinedale glaciation took place on the Markagunt Plateau and eroded and buried some lava flows. Hazards.

Geographic entities mentioned:
surface_form: markagunt plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.6167
lon: -112.833
surface_form: bull
instance_of: Watercourse
countries: United States
coordinates: lat: 49.46663
lon: -115.45205
Giluwe rat. The Giluwe rat (&quot;Rattus giluwensis&quot;) is a species of rodent in the family Muridae. It is found only in Papua New Guinea, on Mount Giluwe and the subalpine grasslands of the Kaijende Highlands.

Geographic entities mentioned:
surface_form: Mount Giluwe
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -6.0388888888889
lon: 143.88611111111
It surmounts Rogosh Glacier to the northeast and east. The feature is named after the settlement of Kumanovo in Northeastern Bulgaria. Location. Kumanovo Peak is located at, which is 5 km south-southeast of Manastir Peak, 6.9 km west of Dymcoff Crag in Lovech Heights, 8.7 km northwest of Skilly Peak, and 10.45 km southeast of Mount Quandary. British mapping in 1978.

Geographic entities mentioned:
surface_form: Manastir Peak
instance_of: Mountain
coordinates: lat: -64.8658
lon: -61.4206
surface_form: Dymcoff Crag
instance_of: Mountain
coordinates: lat: -64.90055556
lon: -61.23777778
surface_form: Skilly Peak
instance_of: Mountain
coordinates: lat: -64.9833
lon: -61.2667
surface_form: Mount Quandary
instance_of: Mountain
coordinates: lat: -64.866666666667
lon: -61.566666666667
surface_form: quandary
instance_of: Mountain
coordinates: lat: -64.866666666667
lon: -61.566666666667
surface_form: kumanovo peak
instance_of: Mountain
coordinates: lat: -64.90805556
lon: -61.38277778
Kumanovo Peak. Kumanovo Peak (,) is the rocky, partly ice-free peak rising to 1002 m in Ivanili Heights on Oscar II Coast in Graham Land. It surmounts Rogosh Glacier to the northeast and east. The feature is named after the settlement of Kumanovo in Northeastern Bulgaria. Location.

Geographic entities mentioned:
surface_form: kumanovo peak
instance_of: Mountain
coordinates: lat: -64.90805556
lon: -61.38277778
Dublin School. The Dublin School is an independent college-preparatory school with a student body of 169. It is located in the United States in Dublin, New Hampshire, near Dublin Pond and Mount Monadnock. Of the 169 enrolled, approximately 70% are boarding students. History. The school was founded in September 1935 by Paul Lehmann, who owned and operated the school with his wife, Nancy.

Geographic entities mentioned:
surface_form: Dublin Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.906388888889
lon: -72.083888888889
surface_form: Mount Monadnock
instance_of: Mountain
countries: United States
coordinates: lat: 42.860833333333
lon: -72.108055555556
Fenwick (fishing). Fenwick is a brand name of Pure Fishing. Fenwick is named after Lake Fenwick in Kent, Washington where 5 Seattle businessmen founded the company in 1952.

Geographic entities mentioned:
surface_form: Lake Fenwick
instance_of: Lake
countries: United States
coordinates: lat: 47.365833333333335
lon: -122.27111111111111
Břidličná hora. Břidličná hora () is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. It is located in the municipality of Vernířovice. The peak is approximately 6 km southwest of the summit of Praděd mountain, situated on its main ridge between the summits of Jelení hřbet and Pecný. Airplane crash.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
The mountain, with a slightly domed summit area, is well-visible and recognizable. When looking west at the main ridge, one can see the characteristic &quot;tooth&quot; of the summit rock formation of Petrovy kameny, and further to the right along this ridge, the following peaks: Vysoká hole → → → → Břidličná hora.

Geographic entities mentioned:
surface_form: Vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
surface_form: břidličná hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.03297222222222
lon: 17.18686111111111
surface_form: vysoká
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.4039
lon: 18.3611
surface_form: vysoká hole
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.06263888888889
lon: 17.235611111111112
It is visible from two key viewpoints, including the road around the summit of Praděd, where it is marked on an informational panel, and the road around Dlouhé stráně, as well as from the viewpoint on its summit, also marked on an informational panel.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: Dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
surface_form: dlouhé stráně
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.07125
lon: 17.15675
The highest measured speed was 15 cm a year. The stone runs and other periglacial formations are among the most valuable of their kind in the Czech Republic. Waters. The main ridge (crest) of Praděd mountain, running from to pass and further to pass, forms part of the boundary of the European watershed, dividing the drainage basins of the Baltic Sea and the Black Sea.

Geographic entities mentioned:
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
In addition to Břidličná hora, the reserve also encompasses other mountains or peaks such as Velký Máj, Jelení hřbet, Čertova stěna, Pecný, Pec, Ztracené kameny, Ztracené skály and Zelené kameny. The reserve covers a total area of 652.09 ha and was established on 19 March 2008 to protect the environment around the main ridge of Praděd mountain.

Geographic entities mentioned:
surface_form: praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
Skřítek – Ztracené skály – summit of Ztracené kameny – summit of Pec – summit of Pecný – Břidličná hora mountain – Jelení studánka – Jelení hřbet mountain – Sedlo nad Malým kotlem pass – Velký Máj mountain – &quot;U Františkovy myslivny&quot; – Zámčisko–S mountain – Zámčisko–SZ mountain – &quot;U Kamenné chaty&quot;
Sobotín – Vernířovice – Špičák mountain – Čertova stěna – Břidličná hora mountain – Jelení studánka – Jelenka mountain – Mravenčí sedlo pass – Zelené kameny – Skřítek
Cycling routes and ski trails.

Geographic entities mentioned:
surface_form: břidličná hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.03297222222222
lon: 17.18686111111111
Břidličná hora. Břidličná hora () is a mountain in the Hrubý Jeseník mountain range in the Czech Republic. It has an elevation of above sea level. It is located in the municipality of Vernířovice. The peak is approximately 6 km southwest of the summit of Praděd mountain, situated on its main ridge between the summits of Jelení hřbet and Pecný. Airplane crash.

Geographic entities mentioned:
surface_form: břidličná hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.03297222222222
lon: 17.18686111111111
Secondary summit. Břidličná hora is a mountain with a double peak. Approximately 1.2 km northwest of the main summit, there is a secondary summit referred to as &quot;Břidličná hora–SZ&quot;, with an elevation of 984 m above sea level and geographic coordinates, separated from the main summit by a low pass at an elevation of 980 m above sea level. It is situated within dense mixed forest.

Geographic entities mentioned:
surface_form: břidličná hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.03297222222222
lon: 17.18686111111111
&quot;Pod Ztracenými kameny&quot; – Pecný mountain – Špičák mountain – Jestřábí vrch mountain – Branka pass – Homole mountain – mountain – – mountain – &quot;Uhlířská cesta&quot;
&quot;Nad Karlovem&quot; – Klobouk mountain – Mravencovka pass – Jelenec – Jelenka mountain – &quot;Alfrédka&quot; – Břidličná hora mountain – Pecný mountain – Zelené kameny – Skřítek

Geographic entities mentioned:
surface_form: břidličná hora
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.03297222222222
lon: 17.18686111111111
Neapolitan pizza. Neapolitan pizza (;) is the version of the round pizza typically prepared in the Italian city of Naples and characterised by a soft, thin dough with high edges. The tomatoes are traditionally either San Marzano tomatoes or, which grow on the volcanic plains to the south of Mount Vesuvius, and the cheese is traditionally or.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Huhtiniemi. Huhtiniemi is a neighborhood in the city of Lappeenranta in South-Eastern Finland. It is located 2 kilometers west of the town center on a cape of the same name, that extends into lake Saimaa in the North. The campus of the Lappeenranta University of Technology is located to the west of Huhtiniemi.

Geographic entities mentioned:
surface_form: Saimaa
instance_of: Lake
countries: Finland
coordinates: lat: 61.25
lon: 28.25
South Guard. South Guard is a remote mountain summit located near the northern end of the Great Western Divide of the Sierra Nevada mountain range, in Tulare County of northern California. It is situated in Kings Canyon National Park, south of North Guard, and one mile south of Mount Brewer, which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: North Guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.7165267
lon: -118.4900379
surface_form: Mount Brewer
instance_of: Mountain
countries: United States
coordinates: lat: 36.7085
lon: -118.485
South Guard. South Guard is a remote mountain summit located near the northern end of the Great Western Divide of the Sierra Nevada mountain range, in Tulare County of northern California. It is situated in Kings Canyon National Park, south of North Guard, and one mile south of Mount Brewer, which is the nearest higher neighbor.

Geographic entities mentioned:
surface_form: south guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.693459
lon: -118.483874
Topographic relief is significant as the west aspect rises above Cloud Canyon in 3.5 miles, and the east aspect rises above Lake Reflection in two miles. South Guard ranks as the 103rd highest summit in California, and the third-highest point of the northern Great Western Divide. History. The names South Guard and North Guard first appeared on either side of Mt. Brewer on Lieutenant Milton F.

Geographic entities mentioned:
surface_form: south guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.693459
lon: -118.483874
South Guard ranks as the 103rd highest summit in California, and the third-highest point of the northern Great Western Divide. History. The names South Guard and North Guard first appeared on either side of Mt. Brewer on Lieutenant Milton F. Davis’ map of 1896. The first ascent of South Guard's lower 12,964-ft peak was made July 26, 1916, by Walter L. Huber, James Rennie, Florence C.

Geographic entities mentioned:
surface_form: south guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.693459
lon: -118.483874
surface_form: mt. brewer
instance_of: Mountain
countries: United States
coordinates: lat: 36.7085
lon: -118.485
surface_form: north guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.7165267
lon: -118.4900379
History. The names South Guard and North Guard first appeared on either side of Mt. Brewer on Lieutenant Milton F. Davis’ map of 1896. The first ascent of South Guard's lower 12,964-ft peak was made July 26, 1916, by Walter L. Huber, James Rennie, Florence C. Burrell, and Inezetta Holt.

Geographic entities mentioned:
surface_form: south guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.693459
lon: -118.483874
Cotter on July 4, 1864. Climate. South Guard is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift).

Geographic entities mentioned:
surface_form: south guard
instance_of: Mountain
countries: United States
coordinates: lat: 36.693459
lon: -118.483874
Important collectors were the reverends William Mounsey and Baptist Noel Turner, active in the Vale of Belvoir, whose collections were in 1795 described by John Nicholls in the first part of his &quot;The History and Antiquities of the County of Leicestershire&quot;.

Geographic entities mentioned:
surface_form: Vale of Belvoir
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.92
lon: -0.86
Truro Island. Truro Island lies within the Arctic Archipelago in the Qikiqtaaluk Region of northern Canada's territory of Nunavut. It is one of the mid-waterway islands in the McDougall Sound between Bathurst Island and Cornwallis Island. Long and narrow, the island is. Collaborative Interdisciplinary Cryospheric Experiment.

Geographic entities mentioned:
surface_form: McDougall Sound
instance_of: Watercourse
countries: Canada
coordinates: lat: 75.25
lon: -97.5
Genevieve County in the U.S. state of Missouri. The peak has an elevation of. The peak lies about two miles southwest of Bloomsdale and I-55. The peak is the high point of a complex ridge between Coots Creek and Carpenter Branch extending to the Fourche a Du Clos on the southwest side of Bloomsdale. Pikes Peak most likely takes its name from the taller Pikes Peak, in the Rocky Mountains.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Mount Burley. Mount Burley () is a peak, high, located southwest of Doris Bay, South Georgia. It was named by the UK Antarctic Place-Names Committee for Lieutenant Commander Malcolm K. Burley, Royal Navy, leader of the British Combined Services Expedition which surveyed this vicinity in 1964–65.

Geographic entities mentioned:
surface_form: mount burley
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.4833
lon: -36.15
Antennaria anaphaloides. &quot;Antennaria anaphaloides&quot;, the pearly pussytoes, is a North American species of plants in the family Asteraceae. It is native to western Canada (British Columbia, Alberta, Saskatchewan) and the western United States (primarily the Rocky Mountains, with additional populations in the Great Basin and northeastern part of the Colorado Plateau).

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Once a single province, it now comprises the provinces of Kasaï Province, Kasaï-Central, Sankuru, Kasaï-Oriental, and Lomami Province. It shares its name with the Kasai River. Historically, the Kasaï region has been a stronghold for the Union for Democracy and Social Progress (UDPS) party.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
Republic Act No. 11550 officially designated Buluan as the capital of Maguindanao del Sur. History. Buluan used to comprise a vast area surrounding Lake Buluan when it was created as one of the municipalities of Cotabato on August 8, 1947, by Executive Order No. 82 of Pres. Manuel Roxas. On August 3, 1951, the municipality of Tacurong was created out of its south-western portion.

Geographic entities mentioned:
surface_form: Lake Buluan
instance_of: Lake
countries: Philippines
coordinates: lat: 6.6405555555556
lon: 124.825
Mount Rohr. Mount Rohr is a mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated east of Pemberton, east of Cayoosh Mountain, and northeast of Joffre Peak, its nearest higher peak.

Geographic entities mentioned:
surface_form: Cayoosh Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.4031
lon: -122.5244
surface_form: Joffre Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.33303
lon: -122.45268
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is situated east of Pemberton, east of Cayoosh Mountain, and northeast of Joffre Peak, its nearest higher peak. Highway 99 traverses the southern base of the mountain between Cayoosh Pass and the west end of Duffy Lake, while Mount Chief Pascall rises on the opposite (south) side of this highway.

Geographic entities mentioned:
surface_form: Mount Chief Pascall
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3606
lon: -122.4468
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's name was submitted by Rev. Damasus Payne, a mountaineer, to honor Rev. Victor Sebastian Rohr (1873-1965), who spent 40 years in British Columbia and was a missionary to the First Nations in the region between Skookumchuck and Williams Lake. The name was officially adopted on April 21, 1966, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7172
lon: -63.0503
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7714
lon: -63.6689
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.11695
lon: -122.07195
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: williams lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.62
lon: -63.5953
Mount Rohr. Mount Rohr is a mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated east of Pemberton, east of Cayoosh Mountain, and northeast of Joffre Peak, its nearest higher peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Rohr. Mount Rohr is a mountain summit located in the Cayoosh Range of the Lillooet Ranges, in southwestern British Columbia, Canada. It is situated east of Pemberton, east of Cayoosh Mountain, and northeast of Joffre Peak, its nearest higher peak.

Geographic entities mentioned:
surface_form: mount rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
Highway 99 traverses the southern base of the mountain between Cayoosh Pass and the west end of Duffy Lake, while Mount Chief Pascall rises on the opposite (south) side of this highway. Mount Rohr forms the westernmost boundary of Duffey Lake Provincial Park as it also represents the park's highest point. The mountain's name was submitted by Rev. Damasus Payne, a mountaineer, to honor Rev.

Geographic entities mentioned:
surface_form: mount rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
Climate. Based on the Köppen climate classification, Mount Rohr is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Mount Rohr.

Geographic entities mentioned:
surface_form: mount rohr
instance_of: Mountain
countries: Canada
coordinates: lat: 50.3989
lon: -122.4085
Highway 99 traverses the southern base of the mountain between Cayoosh Pass and the west end of Duffy Lake, while Mount Chief Pascall rises on the opposite (south) side of this highway. Mount Rohr forms the westernmost boundary of Duffey Lake Provincial Park as it also represents the park's highest point. The mountain's name was submitted by Rev. Damasus Payne, a mountaineer, to honor Rev.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Distribution and habitat. &quot;Calytrix merralliana&quot; grows on yellow sand and gravelly sand between the Southern Cross-Kalgoorlie districts and Lake Cronin in the Coolgardie and Mallee bioregions of inland Western Australia.

Geographic entities mentioned:
surface_form: Lake Cronin
instance_of: Lake
countries: Australia
coordinates: lat: -32.385555555556
lon: 119.765
In 2001, Pitou was inducted into the New England Women's Sports Hall of Fame. Pitou moved with her family from New York to Center Harbor, New Hampshire at the age of three. There she began skiing on a hill in her backyard, later progressing to the nearby Gilford Outing Club and Belknap Mountain (now Gunstock) ski areas.

Geographic entities mentioned:
surface_form: Belknap Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.517855555556
lon: -71.369238888889
Young Island (Nunavut). Young Island is an uninhabited member of the Arctic Archipelago in the territory of Nunavut. It lies in the Parry Channel, southwest of Lowther Island, and northeast of Hamilton Island. Two more Young Islands lie within Nunavut. One is a member of the Low Islands, in Ungava Bay, near Aupaluk; the other is a member of the Hopewell Islands, in Hudson Bay, near Inukjuak.

Geographic entities mentioned:
surface_form: Parry Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 74.33333333
lon: -93
Constantiaberg. Constantiaberg is a large, whale-backed mountain that forms part of the mountainous spine of the Cape Peninsula in Table Mountain National Park, Cape Town, South Africa. It lies about 7 km south of Table Mountain, on the southern side of Constantia Nek. The mountain is 927 m high. It is not known who first ascended the peak.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The mountain is 927 m high. It is not known who first ascended the peak. Constantiaberg, Devil's Peak and Table Mountain are the highest mountains in the range that stretches from Table Mountain all the way to Cape Point. The range, made up of resistant sandstones of the Table Mountain Group, dominates the southern suburbs of the city on the verge of the Cape Flats.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: devil's peak
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.954752777778
lon: 18.439263888889
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
surface_form: table mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Constantiaberg. Constantiaberg is a large, whale-backed mountain that forms part of the mountainous spine of the Cape Peninsula in Table Mountain National Park, Cape Town, South Africa. It lies about 7 km south of Table Mountain, on the southern side of Constantia Nek. The mountain is 927 m high. It is not known who first ascended the peak.

Geographic entities mentioned:
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
Constantiaberg. Constantiaberg is a large, whale-backed mountain that forms part of the mountainous spine of the Cape Peninsula in Table Mountain National Park, Cape Town, South Africa. It lies about 7 km south of Table Mountain, on the southern side of Constantia Nek. The mountain is 927 m high. It is not known who first ascended the peak.

Geographic entities mentioned:
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
surface_form: table mountain national park
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The range, made up of resistant sandstones of the Table Mountain Group, dominates the southern suburbs of the city on the verge of the Cape Flats. The lower eastern slopes of Constantiaberg are covered by the commercial pine and gum plantations of Tokai forest, and are crisscrossed with hiking trails and gravel roads that are used for harvesting the trees.

Geographic entities mentioned:
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
The forest is popular for walking, running and mountain biking. The western slopes of the mountain overlook the magnificent scenery of Hout Bay. A tarred road leads to the summit of Constantiaberg, where an important VHF mast is located. The mast is about 100 m high and is visible for perhaps 80 kilometers in any direction.

Geographic entities mentioned:
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
It was constructed in the 1960s and is used to transmit signals for many local television and radio channels, and also to support cellular networks. The South African Weather Service has a radar installation at the summit. Constantiaberg is home to a variety of bird and plant species. The mountain is covered mainly by fynbos, a botanical biome native to the Western Cape.

Geographic entities mentioned:
surface_form: constantiaberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.0542
lon: 18.3856
The mountain is 927 m high. It is not known who first ascended the peak. Constantiaberg, Devil's Peak and Table Mountain are the highest mountains in the range that stretches from Table Mountain all the way to Cape Point. The range, made up of resistant sandstones of the Table Mountain Group, dominates the southern suburbs of the city on the verge of the Cape Flats.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Estaragne. The Estaragne (Pic d'Estaragne) is a French Pyrenean summit, culminating at m. Topography. The peak is located in the Hautes-Pyrénées department, in the Néouvielle massif, near Saint-Lary-Soulan in the Pyrénées National Park and near the Néouvielle National Nature Reserve. History.

Geographic entities mentioned:
surface_form: néouvielle
instance_of: Mountain
countries: France
coordinates: lat: 42.834633
lon: 0.115281
surface_form: néouvielle
instance_of: Mountain
countries: France
coordinates: lat: 42.834633
lon: 0.115281
Estaragne. The Estaragne (Pic d'Estaragne) is a French Pyrenean summit, culminating at m. Topography. The peak is located in the Hautes-Pyrénées department, in the Néouvielle massif, near Saint-Lary-Soulan in the Pyrénées National Park and near the Néouvielle National Nature Reserve. History.

Geographic entities mentioned:
surface_form: pic d'estaragne
instance_of: Mountain
countries: France
coordinates: lat: 42.7972
lon: 0.12944
surface_form: estaragne
instance_of: Mountain
countries: France
coordinates: lat: 42.7972
lon: 0.12944
surface_form: estaragne
instance_of: Mountain
countries: France
coordinates: lat: 42.7972
lon: 0.12944
Estaragne. The Estaragne (Pic d'Estaragne) is a French Pyrenean summit, culminating at m. Topography. The peak is located in the Hautes-Pyrénées department, in the Néouvielle massif, near Saint-Lary-Soulan in the Pyrénées National Park and near the Néouvielle National Nature Reserve. History.

Geographic entities mentioned:
surface_form: estaragne
instance_of: Mountain
countries: France
coordinates: lat: 42.7972
lon: 0.12944
Topography. The peak is located in the Hautes-Pyrénées department, in the Néouvielle massif, near Saint-Lary-Soulan in the Pyrénées National Park and near the Néouvielle National Nature Reserve. History. The etymology of the name &quot;Estaragne&quot; is unclear, although there is a small valley and stream with the same name just to the northeast of the peak. Ecology.

Geographic entities mentioned:
surface_form: estaragne
instance_of: Mountain
countries: France
coordinates: lat: 42.7972
lon: 0.12944
Mbosi people. The Mbochi (or M'Boshi) are a Bantu ethnic group in Central Africa. Their language originates from the regions of the African Great Lakes where they began, after a long migration from the east to the centre, over the years, until 1850. This central African ethnic group as a population is concentrated in the northern region of the Republic of the Congo.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Geography. The ridge is an eroded remnant of a sandstone layer that is approximately AMSL, situated immediately south of Wentworth Falls. The Tableland is the major southerly spur of the main spine of the Blue Mountains Range and forms the beginning of the Southern Escarpment, an unbroken series of tall sandstone cliffs which fringes the Jamison, Megalong, Kanimbla, and Hartley Valleys.

Geographic entities mentioned:
surface_form: Jamison
instance_of: Valley
countries: Australia
coordinates: lat: -33.7582
lon: 150.334
surface_form: Megalong
instance_of: Valley
countries: Australia
coordinates: lat: -33.733333333333
lon: 150.25
The plateau was named by Governor Macquarie after King George III. It extends southwards from Wentworth Falls and is the eastern boundary of the Jamison Valley. There are also views from several points along the ridge, accessed via paths breaking off the main fire trail.

Geographic entities mentioned:
surface_form: Jamison Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.7582
lon: 150.334
Kuhn served initially with an engineer company and then on the staff of the Engineer School, both at Willets Point, New York. In 1888, he was assigned to the Detroit Engineer District as assistant district engineer, which included supervision of river and harbor projects on the east shore of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Güferhorn. The Güferhorn is a mountain in the Lepontine Alps, located between the valleys of Vals and Hinterrhein in Graubünden. At 3,379 metres above sea level it is the highest summit of the Lepontine Alps lying east of the Rheinwaldhorn. The northern side of the massif is covered by the Güfergletscher, a 2 kilometres long glacier.

Geographic entities mentioned:
surface_form: Rheinwaldhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.493611111111
lon: 9.04
Güferhorn. The Güferhorn is a mountain in the Lepontine Alps, located between the valleys of Vals and Hinterrhein in Graubünden. At 3,379 metres above sea level it is the highest summit of the Lepontine Alps lying east of the Rheinwaldhorn. The northern side of the massif is covered by the Güfergletscher, a 2 kilometres long glacier.

Geographic entities mentioned:
surface_form: güferhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5125
lon: 9.0630833333333
The northern side of the massif is covered by the Güfergletscher, a 2 kilometres long glacier. It lies above 2,600 metres on the east side of a ridge starting at the summit of the Güferhorn and separating the valleys of Länta and Canaltal, both converging at the Zervreilasee, south of Vals.

Geographic entities mentioned:
surface_form: güferhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.5125
lon: 9.0630833333333
Wolves and moose on Isle Royale. The single predator-single prey relationship between wolves and moose on Isle Royale in Lake Superior is unique, and has been the subject of detailed study since 1958.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
In 2018, three females and one male wolf from Minnesota were transferred to the island system. Isle Royale National Park is made up of about 400 islands, and is in the northwest portion of Lake Superior. It is about from Michigan's shore, and from the Canadian shore. The main island is about long, and wide at the widest point, with an area of.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
As an isolated island, Isle Royale initially had neither wolves nor moose. The moose are believed to have either swum across Lake Superior from Minnesota in the early 1900s or were stocked on the island by humans for the purpose of recreational hunting. In 1949 a few wolves, possibly only a single pair, crossed an ice bridge from Ontario to the island during a harsh winter.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
This isolated Quasdanovich's force from Wurmser's main army by Lake Garda, and freed the French to concentrate on the main force at Castiglione delle Stiviere, further south; Bonaparte's victory at the Battle of Castiglione forced Wurmser across the Mincio River, and allowed the French to return to the siege of Mantua.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Following this clash, the impenetrable Württemberg fortress, Hohentwiel, capitulated to the French, in what the Duke of Württemberg considered a scandalous lack of military courage.

Geographic entities mentioned:
surface_form: Hohentwiel
instance_of: Mountain
countries: Germany
coordinates: lat: 47.764722222222
lon: 8.8188888888889
Death. He died in Detroit on April 29, 1994. His corpse was cremated and his ashes were scattered in Lake Michigan. Publications. In 1980, Sutsakhan published &quot;The Khmer Republic at War and the Final Collapse&quot;, which remains a major source of information on the Cambodian Civil War.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Melitaea sindura. &quot;Melitaea sindura&quot; is a butterfly of the family Nymphalidae. It is found in Kashmir, Chitral and Tibet.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
They chose their name (derived from Mount Vesuvius) because, in their words, &quot;Like lava, so long held back, that must at last pour out around us, [our idea of feminist equality] is in no way incendiary but in all ways regenerating.&quot;
With the overthrow of King Louis-Philippe of France in 1848, the newly formed Republic lifted all restrictions on the press and assembly.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
RockNess 2008. RockNess 2008 was the third RockNess Festival to take place. It took place on 7 June and 8 June. Fatboy Slim returned to Loch Ness to headline the Saturday on the mainstage. The other main headliners were Razorlight, The View, Underworld, 2manydjs and Annie Mac. Due to the death the previous year, tighter restrictions were put in place for car park access at the 2008 event.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45