Sarmila/GeoWiki-Features huggingface dataset:
The Kingdom of Xiutu is closely associated to the Shajing culture (700–100 BCE), which managed to prosper along rivers amid general aridification. The Shajing Culture was able to flourish along the lower Shiyang River as the Zhuye Lake was retreating, while the city of Xiutu prospered along the Hongshui River, permitting a flourishing of nomadic culture within a context of drought.

Geographic entities mentioned:
surface_form: Zhuye Lake
instance_of: Lake
countries: People's Republic of China
surface_form: Hongshui River
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 36.831944444444446
lon: 92.8775
The predecessors of Xiutu in the area of the Hexi Corridor, before the Xiongnu occupation around 176 BCE, were probably the Yuezhi. The city of Xiutu (休屠城), about north of Wuwei, has left monumental ruins (), located on the ancient border of Zhuye Lake. After the conquests of Huo Qubing (121 BCE) the city would be incorporated just inside of the Great Wall built under the Han dynasty.

Geographic entities mentioned:
surface_form: Zhuye Lake
instance_of: Lake
countries: People's Republic of China
Aranđelovac. Aranđelovac (,) is a town and a municipality located in the Šumadija District of central Serbia., the municipality has a population of 41,297 inhabitants, while the town has 22,881 inhabitants. It is situated beneath the mountains Bukulja and Venčac, at about above sea level, away from Belgrade. The municipality encompasses two towns and 18 village communities.

Geographic entities mentioned:
surface_form: Bukulja
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.29861111
lon: 20.52916667
surface_form: Venčac
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.262777777778
lon: 20.592777777778
Route. Charles E. Cawley was appointed Chief Engineer, who instructed his recently appointed assistant Frederick Banister to set out the first few miles. The proposed route through the Irwell Valley was then approved by Chief Inspector of Railways Major General Sir Charles W. Pasley on 23 September 1846. The railway began from a junction with the Manchester and Bolton Railway, in Clifton.

Geographic entities mentioned:
surface_form: Irwell Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.66
lon: -2.31
Libyan Desert. The Libyan Desert, which covers most of Libya, is one of the most arid and sun-baked places on Earth. In places, decades may pass without seeing any rainfall at all, and even in the highlands rainfall seldom happens, once every 5–10 years. At Uweinat, the last recorded rainfall was in September 1998.

Geographic entities mentioned:
surface_form: Uweinat
instance_of: Mountain
countries: Libya
Egypt
Sudan
coordinates: lat: 21.919444444444
lon: 24.922222222222
With the discovery of oil in the 1950s also came the discovery of a massive aquifer underneath much of Libya. The water in the Nubian Sandstone Aquifer System pre-dates the last ice ages and the Sahara Desert itself. This area also contains the Arkenu structures, which were once thought to be two impact craters. Politics and elections.

Geographic entities mentioned:
surface_form: Arkenu structures
instance_of: Mountain
countries: Libya
coordinates: lat: 22.101388888889
lon: 23.798333333333
Vassar was the second of the Seven Sisters colleges, higher education schools that were strictly for women, and historically sister institutions to the all-male Ivy League colleges. It was chartered by its namesake, brewer Matthew Vassar, in 1861 in the Hudson Valley, about north of New York City. The first person appointed to the Vassar faculty was astronomer Maria Mitchell, in 1865.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Haplochromis acidens. &quot;Haplochromis acidens&quot; is a species of cichlid endemic to Lake Victoria. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Sandnes, Bygland. Sandnes is a village in Bygland municipality in Agder county, Norway. The village is located on a small flat area between the lake Åraksfjorden to the west and the steep mountainside to the east. The county road 323 runs through the village on its way to the larger village of Åraksbø, about to the north.

Geographic entities mentioned:
surface_form: Åraksfjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.925555555556
lon: 7.7116666666667
Geography. The Laisälven river has its source at an altitude of 850 metres near Nasafjället on the border with Norway, flowing with streams and seals through mountainous landscapes down to the lakes Iraft at Adolfström, Mittisjön and Gautosjön at Gautosjö. The river then flows into the nearly three mile long lake Laisan, where the communities of Laisvall and Laisvallby are located.

Geographic entities mentioned:
surface_form: Iraft
instance_of: Lake
countries: Sweden
coordinates: lat: 66.2851
lon: 16.6089
Downstream of the mouth of the Dellikälven, the Laisälven passes through largely uninhabited areas before entering the Vindelälven in the upper part of the lake Nedre Gautsträsket about 10 km north of Sorsele. The average water flow at the mouth is 57 m³/s. Use. In Iraft, Mittisjön and Gautosjön there are char and trout.

Geographic entities mentioned:
surface_form: Nedre Gautsträsket
instance_of: Lake
countries: Sweden
coordinates: lat: 65.6006
lon: 17.4635
Sutton Waldron. Sutton Waldron is a village and civil parish in north Dorset, England, situated on the A350 road between Iwerne Minster and Fontmell Magna, in the Blackmore Vale under the scarp of Cranborne Chase, north of Blandford Forum and south of Shaftesbury. In the 2011 census the parish had 93 dwellings, 87 households and a population of 200.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
surface_form: Cranborne Chase
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 50.961419444444
lon: -2.0440888888889
It is narrow along its east–west axis. The city bisects the Kōfu Basin and is 250 to 300 meters above sea level. Kōfu is surrounded by mountains on all sides. Three quarters of Kōfu's territory is a part of Mount Kinpu in the north. Much of the northern portion of the city is within the Chichibu Tama Kai National Park. Mount Fuji is visible in the distance from Kōfu to the south. Climate.

Geographic entities mentioned:
surface_form: Mount Kinpu
instance_of: Mountain
countries: Japan
coordinates: lat: 35.87166666666667
lon: 138.62527777777777
It is narrow along its east–west axis. The city bisects the Kōfu Basin and is 250 to 300 meters above sea level. Kōfu is surrounded by mountains on all sides. Three quarters of Kōfu's territory is a part of Mount Kinpu in the north. Much of the northern portion of the city is within the Chichibu Tama Kai National Park. Mount Fuji is visible in the distance from Kōfu to the south. Climate.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Collepino. Collepino is a village in Umbria, central Italy. It is a &quot;frazione&quot; of the &quot;comune&quot; of Spello. Geography. Collepino is situated on a hill 600m.a.s. at the flank of Monte Subasio on a panoramic road from Spello to Assisi
History. Collepino can be traced back to the 13th century. The inhabitants were shepherds and woodworkers at the nearby Abbey S. Silvestro.

Geographic entities mentioned:
surface_form: Monte Subasio
instance_of: Mountain
countries: Italy
coordinates: lat: 43.064166666667
lon: 12.6625
Schänzel Tower. The Schänzel Tower () is a 13-metre-high viewing tower on the Steigerkopf near Edenkoben in the county of Südliche Weinstraße in the German state of Rhineland-Palatinate. It was built in 1874 and is the highest-located tower in the mountain range of the Palatinate Forest. Location.

Geographic entities mentioned:
surface_form: Steigerkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.2981
lon: 8.02722
Since then, Delphi has been considered by Greeks to be the center of the world, as the site of the original &quot;omphalos&quot; &quot;navel of the Earth.&quot;
Hesiod's telling of the myth in &quot;The Theogony&quot; says Zeus set up for veneration at Mount Parnassus the same stone given by his mother Rhea to his father Kronos to eat in his place, which had allowed Zeus to begin his reign.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The Lyngos mountains are drained by the river Aoos to the west and by the river Venetikos, a tributary of the Haliacmon, to the east. The nearest mountain ranges are the Vasilitsa to the north, Chasia to the east, Lakmos to the south and Tymfi to the west. The nearest villages are Vovousa to the west and Perivoli to the north. The town Metsovo is about 15 km to the south.

Geographic entities mentioned:
surface_form: Vasilitsa
instance_of: Mountain
countries: Greece
coordinates: lat: 40.0597
lon: 21.1998
surface_form: tymfi
instance_of: Mountain
countries: Greece
coordinates: lat: 39.997222222222
lon: 20.813888888889
surface_form: vasilitsa
instance_of: Mountain
countries: Greece
coordinates: lat: 40.0597
lon: 21.1998
Lyngos. Lyngos (), also transliterated as &quot;Lygos&quot;, is a remote mountain range in the eastern Ioannina and the western Grevena regional unit in northwestern Greece. It is a part of the Pindus mountain range. Its highest point is the Avgo, at 2,177 m elevation.

Geographic entities mentioned:
surface_form: lygos
instance_of: Mountain
countries: Greece
coordinates: lat: 39.89
lon: 21.13
surface_form: lyngos
instance_of: Mountain
countries: Greece
coordinates: lat: 39.89
lon: 21.13
Lyngos. Lyngos (), also transliterated as &quot;Lygos&quot;, is a remote mountain range in the eastern Ioannina and the western Grevena regional unit in northwestern Greece. It is a part of the Pindus mountain range. Its highest point is the Avgo, at 2,177 m elevation.

Geographic entities mentioned:
surface_form: lyngos
instance_of: Mountain
countries: Greece
coordinates: lat: 39.89
lon: 21.13
After departing at 8:58am, Roosevelt and his party arrived at 6.20pm on 14 January at Casablanca’s Medouina Airport, having over the previous 50 hour travelled. As the 314’s were not required until the return leg they flew to Pan American’s flying boat base at Fisherman’s Lake in Liberia and remained there for two weeks.

Geographic entities mentioned:
surface_form: Fisherman’s Lake
instance_of: Lake
countries: Liberia
coordinates: lat: 6.7352777777778
lon: -11.251111111111
Wildnörderer. The Wildnörderer is a mountain in the Nauderer group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: wildnörderer
instance_of: Mountain
countries: Austria
coordinates: lat: 46.891388888889
lon: 10.615277777778
The width of this body of water generally varies from 1 to, except the bay at the mouth of the Muskiki River which extends to. Lake Soscumica has many islands, peninsulas and bays. This lake is crossed by the Nottaway River which drains the Lake Matagami (located in the South). The confluence of the Nottaway River with Soscumica Lake is located at North of downtown Matagami, Quebec.

Geographic entities mentioned:
surface_form: Lake Matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
surface_form: matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
Lake Soscumica has many islands, peninsulas and bays. This lake is crossed by the Nottaway River which drains the Lake Matagami (located in the South). The confluence of the Nottaway River with Soscumica Lake is located at North of downtown Matagami, Quebec. Lake Soscumica is located at South of Kauskwepatinach Hill with a peak of. Toponymy.

Geographic entities mentioned:
surface_form: matagami
instance_of: Lake
countries: Canada
coordinates: lat: 49.8667
lon: -77.4464
surface_form: soscumica lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.2725
lon: -77.4592
Soscumica Lake. Soscumica Lake is a lake of the southern portion of Eeyou Istchee James Bay (municipality), in the administrative region of Nord-du-Québec, in the province of in south-western Quebec, Canada. The southern part of Lake Soscumica extends into Millet Township. Forestry is the main economic activity of the sector.

Geographic entities mentioned:
surface_form: soscumica lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.2725
lon: -77.4592
The surface of the lake is usually frozen from early November to mid-May, however, safe ice circulation is generally from mid-November to mid-April. Geography. With a length of, Soscumica Lake is shaped like a large V open to the Southwest. The northern part (East-West direction) has an arm length of; the arm of the north-south axis measures.

Geographic entities mentioned:
surface_form: soscumica lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.2725
lon: -77.4592
Do Hezar River. sruj2oxrkteanqds9sz2qbve8mhu" xml:space="preserve">The Do Hezar River is located in Mazandaran Province in northern Iran. It flows northward through the Central Alborz mountain range, eventually combining with the Se Hezar River before flowing into the Caspian Sea as the Cheshmeh Kileh River. Central Alborz mountain range map.

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
Cauldcleuch Head. Cauldcleuch Head is a hill in an unnamed range of Roxburghshire hills north of Langholm, part of the Southern Uplands of Scotland. The highest hill in this range, it has an isolation of approximately 26 km. Parts of the Gorrenberry Jubilee Wood can be found in the Billhope glen to its southwest, where the easiest line of ascent is found.

Geographic entities mentioned:
surface_form: cauldcleuch head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.283333333333
lon: -2.8666666666667
Keekozhur. Keekozhur, also spelt as Keekozhoor, is a small village on the side of Pamba River, situated 4 km from Ranni and 9 km from Kozhencherry. It is in the state of Kerala, India. It is 15 km from the Pathanamthitta district headquarters. The village is located under Ranny and Cherukole Panchayats. Community life.

Geographic entities mentioned:
surface_form: Pamba River
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Cerro Overo. Cerro Overo is a volcanic crater in Chile. It lies at the foot of Chiliques volcano and close to Laguna Lejía, over ignimbrites of Pliocene age erupted by the La Pacana volcano. It is wide and deep and formed through combined explosive-effusive eruptions. The lavas are of lower crustal provenience and are among the least silicic in the region. Geography and geomorphology.

Geographic entities mentioned:
surface_form: Laguna Lejía
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
Volcanism occurs due to the subduction of the Nazca Plate off the west coast of South America. Changes in its geometry over time have caused variations in the volcanic activity in the Central Volcanic Zone, the latest of which helped build the Puna-Altiplano, the highest volcanically active high plateau in the world.

Geographic entities mentioned:
surface_form: Puna
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The maar is set into Pliocene-age ignimbrites erupted by the La Pacana caldera, and the underlying rocks range in age from Permian to Miocene and include both volcanic and sedimentary rocks.

Geographic entities mentioned:
surface_form: La Pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
surface_form: pacana
instance_of: Mountain
countries: Chile
coordinates: lat: -23.16666667
lon: -67.41666667
A thick layer of ejecta surrounds the maar and has a conspicuous black colour. Cerro Overo lies on the high Altos del Toro Blanco ridge at the northeastern foot of Chiliques volcano. The La Albondiga lava dome lies about southwest of Cerro Overo. Closed lakes and basins are widespread in the region; Laguna Lejia is such a spring-fed lake west-northwest of Cerro Overo. Geology.

Geographic entities mentioned:
surface_form: laguna lejia
instance_of: Lake
countries: Chile
coordinates: lat: -23.5
lon: -67.6925
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
Cerro Overo. Cerro Overo is a volcanic crater in Chile. It lies at the foot of Chiliques volcano and close to Laguna Lejía, over ignimbrites of Pliocene age erupted by the La Pacana volcano. It is wide and deep and formed through combined explosive-effusive eruptions. The lavas are of lower crustal provenience and are among the least silicic in the region. Geography and geomorphology.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
It is wide and deep and formed through combined explosive-effusive eruptions. The lavas are of lower crustal provenience and are among the least silicic in the region. Geography and geomorphology. Cerro Overo is a wide volcanic crater, which is elongated in east-west direction. Its maximum depth is about. A thick layer of ejecta surrounds the maar and has a conspicuous black colour.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
Its maximum depth is about. A thick layer of ejecta surrounds the maar and has a conspicuous black colour. Cerro Overo lies on the high Altos del Toro Blanco ridge at the northeastern foot of Chiliques volcano. The La Albondiga lava dome lies about southwest of Cerro Overo. Closed lakes and basins are widespread in the region; Laguna Lejia is such a spring-fed lake west-northwest of Cerro Overo.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
A thick layer of ejecta surrounds the maar and has a conspicuous black colour. Cerro Overo lies on the high Altos del Toro Blanco ridge at the northeastern foot of Chiliques volcano. The La Albondiga lava dome lies about southwest of Cerro Overo. Closed lakes and basins are widespread in the region; Laguna Lejia is such a spring-fed lake west-northwest of Cerro Overo. Geology.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
Geology. Geologically, Cerro Overo is part of the Central Volcanic Zone (CVZ) of the Andes, which is represented by Lascar and Chiliques volcanoes around Cerro Overo. The CVZ is one of four volcanic belts that are located in the Andes, and which include the Northern Volcanic Zone, the Central Volcanic Zone, the Southern Volcanic Zone and the Austral Volcanic Zone.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
A fault like the Miscanti fault may have controlled its formation; the maar lies at the intersection of several north-northeast trending lineaments with a northwest-southeast trending regional tectonic structure. Most likely, the faults allowed the magma to bypass the crustal structures that intercept mafic magmas such as these of Cerro Overo before they reach the surface.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
Most likely, the faults allowed the magma to bypass the crustal structures that intercept mafic magmas such as these of Cerro Overo before they reach the surface. An aquifer may exist inside the Cerro Overo diatreme. Composition. Cerro Overo has erupted basaltic andesite, which contains phenocrysts of clinopyroxene, olivine and plagioclase. Quartz occurs as xenoliths and xenocrysts.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
An aquifer may exist inside the Cerro Overo diatreme. Composition. Cerro Overo has erupted basaltic andesite, which contains phenocrysts of clinopyroxene, olivine and plagioclase. Quartz occurs as xenoliths and xenocrysts. The volcanic rocks define a calc-alkaline suite.

Geographic entities mentioned:
surface_form: cerro overo
instance_of: Mountain
countries: Chile
coordinates: lat: -23.5175
lon: -67.6625
It was described botanically in 2001. The distribution and range of &quot;B. jaapii&quot; is extremely limited; confined entirely to the summit forests and scrublands of a singular mountain in Camaroon (Mount Kupe, a dormant volcano on the Western High Plateau), at elevations of approximately 1,800 meters. It was first collected in November (during flowering), 1985 as a new discovery by D.W.

Geographic entities mentioned:
surface_form: Mount Kupe
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.801
lon: 9.707
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Craugastor vulcani. &quot;Craugastor vulcani&quot; is a species of frog in the family Craugastoridae. It is endemic to the Sierra de los Tuxtlas range in southern Veracruz state, Mexico. Its name refers to its type locality on the San Martin Tuxtla volcano. Common name Volcan San Martin rainfrog has been proposed for it. Description.

Geographic entities mentioned:
surface_form: San Martin Tuxtla
instance_of: Mountain
countries: Mexico
coordinates: lat: 18.557455555556
lon: -95.200402777778
This was the Association's most successful jamboree. In 1971, the Association participated in the 13th World Scout Jamboree held in Asagiri Heights, Japan. In 1974, the National Jamboree was held in Tam Bình, Gia Định (modern-day Ho Chi Minh City) under the name &quot;Tự Lực&quot; (&quot;Self-sufficiency&quot;).

Geographic entities mentioned:
surface_form: Asagiri Heights
instance_of: Plateau
countries: Japan
coordinates: lat: 35.41333333
lon: 138.59111111
Muskrat Lake (New York). Muskrat Lake (formerly Squaw Lake) is located south of Inlet, New York. Fish species present in the lake are brook trout, white sucker, and black bullhead. Access by carry down on the east shore.

Geographic entities mentioned:
surface_form: muskrat lake (new york)
instance_of: Lake
countries: United States
coordinates: lat: 43.63330555555556
lon: -74.73908333333333
Muskrat Lake (New York). Muskrat Lake (formerly Squaw Lake) is located south of Inlet, New York. Fish species present in the lake are brook trout, white sucker, and black bullhead. Access by carry down on the east shore.

Geographic entities mentioned:
surface_form: muskrat lake
instance_of: Lake
countries: United States
coordinates: lat: 43.63330555555556
lon: -74.73908333333333
Roteck. The Roteck () is the highest peak in the Texel group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: roteck
instance_of: Mountain
countries: Italy
coordinates: lat: 46.723611111111
lon: 10.984166666667
Fagernes Airport, Leirin. Fagernes Airport, Leirin (;) is a general aviation airport in Fagernes, in the municipality of Nord-Aurdal, Innlandet county, Norway. It has been an airport for passenger flights, serving Fagernes and the surrounding valleys of Valdres, Hallingdal and Gudbrandsdal in Southern Norway, from Oslo. Opened in 1987, it was owned and operated by state-owned Avinor.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
The Linns were a literary family: Susan wrote fiction and poetry, her brother John Blair Linn was a poet, and her sister, Elizabeth, married Charles Brockden Brown, who wrote novels. De Witt owned a considerable amount of land in the Finger Lakes area, and held four slaves at his residence in Albany, New York, but by 1810 he had freed them, a common practice of the area.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
In 730, Winibald returned to England and engaged a third brother and several amongst his kindred and acquaintance to accompany him in his journey back to Rome to begin a monastic life there. Around 737, Boniface visited Rome. By this time Willibald had returned from his travels, and had become a monk at Monte Cassino. Boniface recruited both nephews for the German mission.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
The Santa Catalina Mountains lie to the northeast, the Rincon Mountains are to the east of Tucson, and the Santa Rita Mountains lie to the south. Additionally, the Sierrita Mountains lie due south, the Roskruge Mountains lie to the west across Avra Valley, the Silver Bell Mountains lie to the northwest, and the Tortolita Mountains lie to the north across the Santa Cruz Valley. Parks and preserves.

Geographic entities mentioned:
surface_form: Avra Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.2212
lon: -111.342
It has the form of a symmetrical uneroded shield volcano with an &quot;impressive&quot; appearance and an ice-filled wide caldera. Like other volcanoes in the Executive Committee Range, it is a paired volcano with the northwesterly high Whitney Peak and the southeasterly high Marks Peak, which is the main summit of Mount Hampton.

Geographic entities mentioned:
surface_form: Marks Peak
instance_of: Mountain
coordinates: lat: -76.5
lon: -125.75
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
It appears that Whitney Peak is the older half of the edifice and that volcanic activity then migrated to Mount Hampton. More generally, volcanism in the Executive Committee Range migrated southwards over time at an average rate of, although Mount Hampton and its southern neighbour Mount Cumming were simultaneously active 10 million years ago.

Geographic entities mentioned:
surface_form: Mount Cumming
instance_of: Mountain
coordinates: lat: -76.66667
lon: -126
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Mount Hampton. Mount Hampton is a shield volcano with a circular ice-filled caldera. It is a twin volcano with Whitney Peak to the northwest and has erupted phonolite rocks. It is the northernmost of the volcanoes which comprise the Executive Committee Range in Marie Byrd Land, Antarctica and was active during the Miocene. Geography and geology.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
Geography and geology. Mount Hampton is the northernmost volcano of the Executive Committee Range in Marie Byrd Land, Antarctica. It has the form of a symmetrical uneroded shield volcano with an &quot;impressive&quot; appearance and an ice-filled wide caldera.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
Like other volcanoes in the Executive Committee Range, it is a paired volcano with the northwesterly high Whitney Peak and the southeasterly high Marks Peak, which is the main summit of Mount Hampton. The northwesterly summit is associated with its own caldera, which is partly cut by the Mount Hampton caldera on the southeastern flank and buried by the lava flows from the latter.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
Mount Hampton is one of the oldest volcanoes of Antarctica and was active during the Miocene. Despite this, it is less eroded than some younger volcanoes in the region; in general, the ages of the Marie Byrd Land volcanoes are not correlated to their erosion status. It appears that Whitney Peak is the older half of the edifice and that volcanic activity then migrated to Mount Hampton.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
Last parasitic eruptions took place around 11.4 million years ago and the youngest radiometric dates are 8.3 million years. As at other volcanoes of Marie Byrd Land, the parasitic activity at Mount Hampton occurred after a long period of dormancy.

Geographic entities mentioned:
surface_form: hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
surface_form: mount hampton
instance_of: Mountain
coordinates: lat: -76.483333333333
lon: -125.8
Mount Hampton. Mount Hampton is a shield volcano with a circular ice-filled caldera. It is a twin volcano with Whitney Peak to the northwest and has erupted phonolite rocks. It is the northernmost of the volcanoes which comprise the Executive Committee Range in Marie Byrd Land, Antarctica and was active during the Miocene. Geography and geology.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
In general, composition is unique for each volcano in the Executive Committee Range. Eruption history. Mount Hampton is one of the oldest volcanoes of Antarctica and was active during the Miocene. Despite this, it is less eroded than some younger volcanoes in the region; in general, the ages of the Marie Byrd Land volcanoes are not correlated to their erosion status.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
As at other volcanoes of Marie Byrd Land, the parasitic activity at Mount Hampton occurred after a long period of dormancy. However, the presence around the caldera rim of snow-covered inactive high ice towers indicate that the mountain is geothermally active and may have erupted during the Holocene.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Rasuwillka. Rasuwillka (Quechua, hispanicized spelling &quot;Rasuhuilca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Ayacucho Region, Lucanas Province, Chipao District, and in the Sucre Province, Morcolla District. Rasuwillka lies northwest of Qarwarasu.

Geographic entities mentioned:
surface_form: qarwarasu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.33194444
lon: -73.75694444
Rasuwillka. Rasuwillka (Quechua, hispanicized spelling &quot;Rasuhuilca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Ayacucho Region, Lucanas Province, Chipao District, and in the Sucre Province, Morcolla District. Rasuwillka lies northwest of Qarwarasu.

Geographic entities mentioned:
surface_form: rasuwillka
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3225
lon: -73.7831
Rasuwillka. Rasuwillka (Quechua, hispanicized spelling &quot;Rasuhuilca&quot;) is a mountain in the Andes of Peru, about high. It is located in the Ayacucho Region, Lucanas Province, Chipao District, and in the Sucre Province, Morcolla District. Rasuwillka lies northwest of Qarwarasu.

Geographic entities mentioned:
surface_form: rasuwillka
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3225
lon: -73.7831
surface_form: rasuhuilca
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3225
lon: -73.7831
He is recognized as the first scientist to perform extensive exploration of the Julian Alps. In 1777 he was the first to try to ascend to the top of Triglav (2864 m), the highest peak in Slovenia, and reached Mali Triglav (2725 m). In 1789 he published a description of the 1786 debris flow at the Slano Blato Landslide.

Geographic entities mentioned:
surface_form: Triglav
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.378333
lon: 13.836667
Carl Mountain. Carl Mountain is a mountain located in the Catskill Mountains of New York east-northeast of Phoenicia. Tremper Mountain is located southwest, and Mount Tobias is located southeast of Carl Mountain.

Geographic entities mentioned:
surface_form: Mount Tobias
instance_of: Mountain
countries: United States
coordinates: lat: 42.05842
lon: -74.2157
surface_form: carl mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.40505
lon: -73.53236
Carl Mountain. Carl Mountain is a mountain located in the Catskill Mountains of New York east-northeast of Phoenicia. Tremper Mountain is located southwest, and Mount Tobias is located southeast of Carl Mountain.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: carl mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.40505
lon: -73.53236
Carl Mountain. Carl Mountain is a mountain located in the Catskill Mountains of New York east-northeast of Phoenicia. Tremper Mountain is located southwest, and Mount Tobias is located southeast of Carl Mountain.

Geographic entities mentioned:
surface_form: carl mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.40505
lon: -73.53236
state of Washington. From its western end just north of the city of Yakima, the ridge runs east-southeast through the Yakima Training Center to its eastern end at Hanford Reach National Monument and the Hanford Site. Yakima Ridge is paralleled on the north by Umtanum Ridge and on the south by the Rattlesnake Hills. Moxee Valley and Black Rock Valley lie south of Yakima Ridge.

Geographic entities mentioned:
surface_form: hanford reach
instance_of: Landform
countries: United States
coordinates: lat: 46.2794
lon: -119.268
Yakima Ridge. Yakima Ridge is a long anticline mountain ridge in Yakima County and Benton County in the U.S. state of Washington. From its western end just north of the city of Yakima, the ridge runs east-southeast through the Yakima Training Center to its eastern end at Hanford Reach National Monument and the Hanford Site.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
Yakima Ridge. Yakima Ridge is a long anticline mountain ridge in Yakima County and Benton County in the U.S. state of Washington. From its western end just north of the city of Yakima, the ridge runs east-southeast through the Yakima Training Center to its eastern end at Hanford Reach National Monument and the Hanford Site.

Geographic entities mentioned:
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
state of Washington. From its western end just north of the city of Yakima, the ridge runs east-southeast through the Yakima Training Center to its eastern end at Hanford Reach National Monument and the Hanford Site. Yakima Ridge is paralleled on the north by Umtanum Ridge and on the south by the Rattlesnake Hills. Moxee Valley and Black Rock Valley lie south of Yakima Ridge.

Geographic entities mentioned:
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
Yakima Ridge is paralleled on the north by Umtanum Ridge and on the south by the Rattlesnake Hills. Moxee Valley and Black Rock Valley lie south of Yakima Ridge. Yakima Ridge is part of the Yakima Fold Belt of east-tending long ridges formed by the folding of Miocene Columbia River basalt flows. The Yakima River cut a water gap through Yakima Ridge at Selah Gap.

Geographic entities mentioned:
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
surface_form: black rock
instance_of: Mountain
countries: United States
coordinates: lat: 39.343055555556
lon: -79.110555555556
Yakima Ridge is paralleled on the north by Umtanum Ridge and on the south by the Rattlesnake Hills. Moxee Valley and Black Rock Valley lie south of Yakima Ridge. Yakima Ridge is part of the Yakima Fold Belt of east-tending long ridges formed by the folding of Miocene Columbia River basalt flows. The Yakima River cut a water gap through Yakima Ridge at Selah Gap.

Geographic entities mentioned:
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
Moxee Valley and Black Rock Valley lie south of Yakima Ridge. Yakima Ridge is part of the Yakima Fold Belt of east-tending long ridges formed by the folding of Miocene Columbia River basalt flows. The Yakima River cut a water gap through Yakima Ridge at Selah Gap. The river cut through other ridges at locations including Umtanum Ridge Water Gap and Union Gap at Ahtanum Ridge.

Geographic entities mentioned:
surface_form: yakima ridge
instance_of: Mountain
countries: United States
coordinates: lat: 46.5902
lon: -120.078
Moxee Valley and Black Rock Valley lie south of Yakima Ridge. Yakima Ridge is part of the Yakima Fold Belt of east-tending long ridges formed by the folding of Miocene Columbia River basalt flows. The Yakima River cut a water gap through Yakima Ridge at Selah Gap. The river cut through other ridges at locations including Umtanum Ridge Water Gap and Union Gap at Ahtanum Ridge.

Geographic entities mentioned:
surface_form: ahtanum ridge
instance_of: Landform
countries: United States
coordinates: lat: 46.5069
lon: -120.816
In 1864, Wentworth ran for Congress as a Republican, and was elected for his last term (serving March 4, 1865March 3, 1867) representing Illinois's 1st congressional district. While he was in the House, there was a controversial vote to settle a boundary issue between Wisconsin and Illinois, with Wisconsin claiming land as far as the tip of Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Beartooth Mountain. Beartooth Mountain () is in the Beartooth Mountains in the U.S. state of Montana. The peak is one of the tallest in the Beartooth Mountains, the 11th tallest in Montana (tied with Bowback Mountain) and is in the Absaroka-Beartooth Wilderness in Custer National Forest. Along a ridge to the northeast lies the spire known as Bears Tooth ().

Geographic entities mentioned:
surface_form: Bowback Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.12777778
lon: -109.61833333
Beartooth Mountain. Beartooth Mountain () is in the Beartooth Mountains in the U.S. state of Montana. The peak is one of the tallest in the Beartooth Mountains, the 11th tallest in Montana (tied with Bowback Mountain) and is in the Absaroka-Beartooth Wilderness in Custer National Forest. Along a ridge to the northeast lies the spire known as Bears Tooth ().

Geographic entities mentioned:
surface_form: Bears Tooth
instance_of: Mountain
countries: United States
coordinates: lat: 45.06277778
lon: -109.5625
Beartooth Mountain. Beartooth Mountain () is in the Beartooth Mountains in the U.S. state of Montana. The peak is one of the tallest in the Beartooth Mountains, the 11th tallest in Montana (tied with Bowback Mountain) and is in the Absaroka-Beartooth Wilderness in Custer National Forest. Along a ridge to the northeast lies the spire known as Bears Tooth ().

Geographic entities mentioned:
surface_form: beartooth mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.06083333
lon: -109.56861111
Features. The monument protects the Medicine Lake Volcano and surrounding highlands in Klamath National Forest, Shasta–Trinity National Forest, and Modoc National Forest northeast of Mount Shasta and south of Lava Beds National Monument. These highlands provide clean water for communities downstream through its extensive aquifers. The area includes numerous cinder cones and lava fields.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
On January 2, 2025, the &quot;Washington Post&quot; reported that President Biden would establish Sáttítla Highlands National Monument along with Chuckwalla National Monument. Biden planned to do so at an event in the Coachella Valley on January 7, but it was canceled due to a Santa Ana windstorm and rescheduled to be at the White House on January 14.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Beachcroft married Charlotte Emily Bonner-Maurice in 1877. There were no children. In his spare time, Beachcroft was an early Alpinist. He first travelled to the Alps in 1864 with Douglas Freshfield, and, in 1877, he climbed the Matterhorn. He was also active in the Alpine Club, and served on its committee from 1889 to 1891. In addition, he served as Master of the Clothworkers' Company in 1913/14.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
'Aqqaba. Aqqaba () is a Palestinian town located on a slope in the Jordan Valley in the northern West Bank, 15 kilometers northeast of Jenin in the Tubas Governorate of the State of Palestine. According to the Palestinian Central Bureau of Statistics (PCBS), the town had a population of 8,239 inhabitants in the 2017 census. History.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
'Aqqaba is made up of three main families: Abu Arra, Abu Ghannam and al-Masri. During clear weather, Haifa could be seen from the west on the Mediterranean Sea as well as the summit of Jabal ash-Sheikh in Lebanon, while from the east the mountains of Ajloun in Jordan are clearly seen day and night. 'Aqqaba is the highest point in the Tubas Governorate.

Geographic entities mentioned:
surface_form: Jabal ash-Sheikh
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
Mongaup Mountain. Mongaup Mountain is a mountain located in the Catskill Mountains of New York west of Frost Valley. Cradle Rock Ridge is located north, and Beaver Kill Range is located east-northeast of Mongaup Mountain.

Geographic entities mentioned:
surface_form: mongaup mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9884
lon: -74.6774
Mongaup Mountain. Mongaup Mountain is a mountain located in the Catskill Mountains of New York west of Frost Valley. Cradle Rock Ridge is located north, and Beaver Kill Range is located east-northeast of Mongaup Mountain.

Geographic entities mentioned:
surface_form: mongaup mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9884
lon: -74.6774
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Mongaup Mountain. Mongaup Mountain is a mountain located in the Catskill Mountains of New York west of Frost Valley. Cradle Rock Ridge is located north, and Beaver Kill Range is located east-northeast of Mongaup Mountain.

Geographic entities mentioned:
surface_form: mongaup mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9884
lon: -74.6774
surface_form: rock ridge
instance_of: Lake
countries: United States
coordinates: lat: 40.9129
lon: -74.4639
Word of Kim's donation soon spread, resulting in King Jeongjo complimenting her and stating that he would grant her a wish. Gim's wish was to see both the palace in the capital city of Hanyang and Mt. Geumgang, which was an unusual request, considering that for 200 years women of Jeju had been forbidden to leave the island.

Geographic entities mentioned:
surface_form: Mt. Geumgang
instance_of: Mountain
countries: North Korea
coordinates: lat: 38.656763888889
lon: 128.10490277778
All signals were dropped after Andy weakened to a tropical storm. A minimum pressure of was recorded at the Hong Kong Royal Observatory (HKO) on July 29. Waglan Island recorded a peak wind speed of. Meanwhile, Green Island observed a peak wind gust of. Tate's Cairn observed of rain during the passage of the storm, the highest in the vicinity of Hong Kong. Overall, damage in Hong Kong was minor.

Geographic entities mentioned:
surface_form: Tate's Cairn
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.358
lon: 114.218
Inchmahome Priory. Inchmahome Priory is situated on Inchmahome, the largest of three islands in the centre of the Lake of Menteith, close to Aberfoyle, Scotland. The name &quot;Inchmahome&quot; comes from the Gaelic &quot;Innis MoCholmaig&quot;, meaning island of St Colmaig.

Geographic entities mentioned:
surface_form: Lake of Menteith
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.176666666667
lon: -4.2941666666667
Early life and education. Danon was born in Ramat Gan to Joseph and Yoheved Danon. His father, Joseph Danon, was born in Egypt, and moved to Israel in 1950. Joseph was severely wounded by shrapnel in the Jordan Valley during the War of Attrition. This caused him to enter a coma and after recovering suffered brain damage and was permanently deaf for the remainder of his life.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Koolbury railway station. Koolbury is the name of a closed railway station on the Main North railway line in the Hunter Region of New South Wales, Australia. The station opened in 1909 and has been removed, no trace now remains.

Geographic entities mentioned:
surface_form: Hunter Region
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
His later journals contain a detailed study of the flight of birds and several different designs for wings based in structure upon those of bats which he described as being less heavy because of the impenetrable nature of the membrane. There is a legend that Leonardo tested the flying machine on Monte Ceceri with one of his apprentices, and that the apprentice fell and broke his leg.

Geographic entities mentioned:
surface_form: Monte Ceceri
instance_of: Mountain
countries: Italy
coordinates: lat: 43.80083333
lon: 11.30694444
He later undertook numerous expeditions and was the first person to visit both the North Pole and South Pole by surface means and the first to completely cross Antarctica on foot. In May 2009, at the age of 65, he reached the summit of Mount Everest. According to the &quot;Guinness Book of World Records&quot; in 1984, he was the world's greatest living explorer.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925