Sarmila/GeoWiki-Features huggingface dataset:
They spin sheet webs on the underside of leaves, where they also lay their eggs. Although predominantly a diurnal hunter, the spider is also likely to eat nectar. Distribution and habitat. The species is endemic to Kenya. The holotype was found on Mount Elgon in 1938 at an altitude of above sea level. It lives in vegetation of the &quot;Podocarpus&quot; genus. It thrives in mountainous areas.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Discovered by the Australasian Antarctic Expedition (1911–1914) under Douglas Mawson, and named after Eric Webb (Webb Subglacial Trench, q.v.), chief magnetician of the Main Base Party of the expedition.

Geographic entities mentioned:
surface_form: Webb Subglacial Trench
instance_of: Landform
coordinates: lat: -70
lon: 146
In retaliation for the invasion of Maui Kahekili II and his brother Kaʻeokulani led a fleet of 700 war canoes in an attack on the north coast of Hawaii. Kamehameha met them with his own fleet, including &quot;Fair American&quot;, and drove them off after a long naval battle off the shore of the Waipio Valley.

Geographic entities mentioned:
surface_form: Waipio Valley
instance_of: Valley
countries: United States
coordinates: lat: 20.1197
lon: -155.593
Many gypsy tours have been held over the years and are still a regular event for many vintage and modern motorcycle groups. The annual gypsy tour to Laconia, New Hampshire near Lake Winnipesaukee began in 1916 and is the oldest continuous motorcycle event in the U.S. Australia. A number of rallies are held throughout Australia throughout the year.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Lok Lo Ha. Lok Lo Ha () is a village and valley northeast of Wo Liu Hang in Fo Tan, Sha Tin District, Hong Kong. Administration. Lok Lo Ha is a recognized village under the New Territories Small House Policy. History. Lok Lo Ha was historically a sea-shore village. A stone pier for the sampan ferry to Yuen Chau Kok was built at Lok Lo Ha in 1917.

Geographic entities mentioned:
surface_form: lok lo ha
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.4019
lon: 114.201
Administration. Lok Lo Ha is a recognized village under the New Territories Small House Policy. History. Lok Lo Ha was historically a sea-shore village. A stone pier for the sampan ferry to Yuen Chau Kok was built at Lok Lo Ha in 1917. In 2018, a KMB bus on route 872 passed by this stop, overturning a few stops later, killing 19.

Geographic entities mentioned:
surface_form: lok lo ha
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.4019
lon: 114.201
History. Lok Lo Ha was historically a sea-shore village. A stone pier for the sampan ferry to Yuen Chau Kok was built at Lok Lo Ha in 1917. In 2018, a KMB bus on route 872 passed by this stop, overturning a few stops later, killing 19. It has been noted that the name of the village literally means “falling down from the road”, which coincidentally describes the bus accident.

Geographic entities mentioned:
surface_form: lok lo ha
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 22.4019
lon: 114.201
The remote peak ranks as the 17th-highest mountain in Oregon. The peak is situated 2.6 miles southeast of Glacier Peak and 3.3 miles southeast of Eagle Cap which is the nearest higher neighbor. Precipitation runoff from the mountain's north slope drains into headwaters of the West Fork Wallowa River, and all other slopes into headwaters of the Imnaha River.

Geographic entities mentioned:
surface_form: Eagle Cap
instance_of: Mountain
countries: United States
coordinates: lat: 45.1636
lon: -117.302
Zagora, Greece. Zagora () is a village and a former municipality on the Pelion peninsula in Magnesia, Thessaly, Greece. Since the 2011 local government reform it is part of the municipality Zagora-Mouresi, of which it is the seat and a municipal unit. The municipal unit has an area of 96.101 km2.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
Sheep Mountain (Flathead County, Montana). Sheep Mountain () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana.

Geographic entities mentioned:
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.3417
lon: -113.471
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.976944444444
lon: -120.38861111111
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.83444444444444
lon: -147.5125
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.785277777778
lon: -107.88611111111
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0248432
lon: -121.418174
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.2883
lon: -117.713
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.5439
lon: -110.524
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.064444444444
lon: -114.36027777778
Moroni had been commanded by his father to seal the plates and &quot;hide up the record in the earth&quot; (Mormon 8:4). Adherents of Mormonism believe that Moroni, as an angel, appeared to Joseph Smith in 1823 and directed him to where the plates were hidden. According to Joseph Smith's account, this was the Hill Cumorah, near Palmyra, New York. Manuscript title.

Geographic entities mentioned:
surface_form: Hill Cumorah
instance_of: Mountain
countries: United States
coordinates: lat: 43.0062
lon: -77.224
Road. Wotton-under-Edge is on the B4058 road and is from the M5 motorway. Rail. Brunel's Bristol and Gloucester Railway passes within of Wotton-under-Edge, following a curve to the west to stay on the gentler Vale of Berkeley and avoid Wotton Hill, Nibley Knoll and Stinchcombe Hill as it heads north. It carries a wide mix of local, intercity and freight trains.

Geographic entities mentioned:
surface_form: Vale of Berkeley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.683333333333
lon: -2.35
Nevado de Chañi is the physical limit between the provinces of Jujuy and Salta. Many peaks higher than 5,000m are part of the group, such as the Cerro Paño (5.517 m) and Nevado del Castillo (5.565 m). The highest summit of Nevado de Chañi is named Cumbre General Belgrano. The normal route to the main summit is by the east side and is technically easy.

Geographic entities mentioned:
surface_form: general belgrano
instance_of: Mountain
countries: Argentina
coordinates: lat: -29
lon: -67.85
surface_form: nevado de chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
surface_form: chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
surface_form: belgrano
instance_of: Lake
countries: Argentina
coordinates: lat: -47.85111111
lon: -72.14722222
Nevado de Chañi. Nevado de Chañi is a mountain in the Andes of the Jujuy Province in Argentina. It has a height of 5,949 metres. It lies at about 50 km northwest of San Salvador de Jujuy. The Nevado de Chañi is a compact mountain group located between the meridians of longitude West 65º42’ and 65º48’ and the parallels of latitude South 24º00’ and 24º10’.

Geographic entities mentioned:
surface_form: nevado de chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
surface_form: chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
It lies at about 50 km northwest of San Salvador de Jujuy. The Nevado de Chañi is a compact mountain group located between the meridians of longitude West 65º42’ and 65º48’ and the parallels of latitude South 24º00’ and 24º10’. The main summit (according to the last available surveys) is 5,949m (24º03’S and 65º44’W) and it is the highest point in the province of Jujuy.

Geographic entities mentioned:
surface_form: nevado de chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
surface_form: chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
Some more recent surveys give about 5,900. The height of 5,949 has been measured many times with modern global positioning systems by summiteers since the early 2000s. Nevado de Chañi is the physical limit between the provinces of Jujuy and Salta. Many peaks higher than 5,000m are part of the group, such as the Cerro Paño (5.517 m) and Nevado del Castillo (5.565 m).

Geographic entities mentioned:
surface_form: nevado de chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
surface_form: chañi
instance_of: Mountain
countries: Argentina
coordinates: lat: -24.063333333333
lon: -65.745833333333
At that time, there was another low-pressure area on the Pacific coast, and both systems were producing rainfall across Central America. At 1200 UTC on October 14, the National Hurricane Center (NHC) indicated that Tropical Depression Sixteen developed about northeast of Cabo Gracias a Dios, a point where the border of Nicaragua and Honduras meet the Caribbean.

Geographic entities mentioned:
surface_form: Cabo Gracias a Dios
instance_of: Landform
countries: Honduras
coordinates: lat: 15.0064851
lon: -83.1301235
The tropical depression added to weeks of heavy rainfall that killed 16 people, many caused by people attempting to cross swollen rivers. Toward the end of October 2008, Lake Managua overflowed, causing flooding in the capital city of Managua. Across the country, 2,273 people evacuated to storm shelters after the floods damaged or destroyed 1,333 houses.

Geographic entities mentioned:
surface_form: Lake Managua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 12.333333333333
lon: -86.416666666667
The Schächentaler Windgällen is a mountain massif in the Schwyzer Alps, overlooking Unterschächen in the canton of Uri. The two named peaks are &quot;Höch Windgällen&quot; (2764 m) and &quot;Läged Windgällen&quot; (2572 m). The mountain massif lies between the valley of Muotathal (north) and Schächental (south). The Schächentaler Windgällen are located a few kilometres west of Klausen Pass.

Geographic entities mentioned:
surface_form: Schächental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.864
lon: 8.761
surface_form: schächental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.864
lon: 8.761
Schächentaler Windgällen. The Schächentaler Windgällen is a mountain massif in the Schwyzer Alps, overlooking Unterschächen in the canton of Uri. The two named peaks are &quot;Höch Windgällen&quot; (2764 m) and &quot;Läged Windgällen&quot; (2572 m). The mountain massif lies between the valley of Muotathal (north) and Schächental (south).

Geographic entities mentioned:
surface_form: schächentaler windgällen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.887916666667
lon: 8.7916388888889
Schächentaler Windgällen. The Schächentaler Windgällen is a mountain massif in the Schwyzer Alps, overlooking Unterschächen in the canton of Uri. The two named peaks are &quot;Höch Windgällen&quot; (2764 m) and &quot;Läged Windgällen&quot; (2572 m). The mountain massif lies between the valley of Muotathal (north) and Schächental (south).

Geographic entities mentioned:
surface_form: höch windgällen
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.887916666667
lon: 8.7916388888889
The fossils of common domesticates are not found at excavated sites in East Africa (e.g., Lake Turkana Basin, Lake Nakuru Basin, Serengeti Plains, Lake Eyasi), suggesting they were not present during the transition into the Pastoral Neolithic. Limited cave painting evidence from Mt. Elgon, Kenya is consistent with the presence of northern African breeds of cattle during the Pastoral Neolithic.

Geographic entities mentioned:
surface_form: Lake Eyasi
instance_of: Lake
countries: Tanzania
coordinates: lat: -3.66667
lon: 35.08333
Shore Line Subdivision. The Shore Line Subdivision is a railroad line owned and operated by Grand Trunk Western Railroad (GTW), a subsidiary of Canadian National (CN), which connects the cities of Detroit, Michigan and Toledo, Ohio, paralleling the shore of Lake Erie. Description.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The NATO reporting name Dagu A class was given to the Type 716 LCAC, which achieved speed over during trials in Dianshan Lake, before being sent to South China Sea for further evaluation. Ships of the Type 716 measured long with a width of and a height of. The vessels had a displacement of and a capacity for a platoon of 32 troops or of cargo.

Geographic entities mentioned:
surface_form: Dianshan Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31.12
lon: 120.97055555556
Highway 30 parallels U.S. Highway 14 and Interstate Highway 90 throughout its route. The Pipestone National Monument is located immediately north of Highway 30 in Pipestone. Lake Shetek State Park is located near Highway 30 in Murray County on the shore of Lake Shetek. The park is located immediately north of the town of Currie and northeast of Slayton. Highway 30 passes through the Richard J.

Geographic entities mentioned:
surface_form: Lake Shetek
instance_of: Lake
countries: United States
coordinates: lat: 44.12
lon: -95.69
Pellenes obvolutus. &quot;Pellenes obvolutus&quot; is a species of jumping spider in the genus &quot;Pellenes&quot; that lives on Mount Elgon in Kenya. The spider has been found in savanna and grassland. It is a hairy medium-sized spider with a carapace that is between long and an abdomen between long. The female is larger than the male and has a different pattern on its abdomen.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
&quot;Pellenes&quot; spiders can be found across the Afrotropical, Holarctic and Indomalayan realms. &quot;Pellenes obvolutus&quot; is endemic to Kenya. The female holotype was found during 1948 living on Mount Elgon at an altitude of above sea level. Other specimens have been collected in the local area. The spider lives in savanna and grassland, often in areas with &quot;Combretum&quot; trees.

Geographic entities mentioned:
surface_form: Mount Elgon
instance_of: Mountain
countries: Uganda
Kenya
coordinates: lat: 1.1185
lon: 34.5265
Degraff Creek. Degraff Creek flows into the Mohawk River in Amsterdam, New York.

Geographic entities mentioned:
surface_form: degraff creek
instance_of: Watercourse
countries: United States
coordinates: lat: 42.92027778
lon: -74.16305556
The NHC issued tropical cyclone warnings and watches across much of southern Florida, with a hurricane warning ultimately covering all of South Florida from Longboat Key on the west coast to Titusville, including Lake Okeechobee and the Florida Keys. A tropical storm watch extended northward on the west coast to Steinhatchee River.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
It is owned and operated by the Canadian Broadcasting Corporation alongside Ici Radio-Canada Télé flagship CBFT-DT (channel 2). The two stations share studios at Maison Radio-Canada on René Lévesque Boulevard East in Downtown Montreal; CBMT-DT's transmitter is located atop Mount Royal. History.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
However, in 1997, CKMI switched its affiliation to the Global Television Network. CBMT set up a full-power rebroadcaster, CBVE, on CKMI's old channel 5, while CKMI moved to channel 20. CBMT transmits from the Mount Royal candelabra tower, in Mount Royal Park, overlooking the city of Montreal. As a result, channel 6 experiences severe multipath interference in parts of the city and South Shore.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Wallkill River. The Wallkill River, a tributary of the Hudson, drains Lake Mohawk in Sparta, New Jersey, flowing from there generally northeasterly to Rondout Creek in New York, just downstream of Sturgeon Pool, near Rosendale, with the combined flows reaching the Hudson at Kingston.

Geographic entities mentioned:
surface_form: Sturgeon Pool
instance_of: Lake
countries: United States
coordinates: lat: 41.8436
lon: -74.0428
The river is unusual because it flows north between two major south-flowing rivers, the Hudson and the Delaware River. It also has the unusual distinction of being a river that drains into a creek, due to being impounded shortly before the Rondout confluence into a small body of water called Sturgeon Pool near Rifton, and what reaches the Rondout from there is the lesser flow. Course.

Geographic entities mentioned:
surface_form: Sturgeon Pool
instance_of: Lake
countries: United States
coordinates: lat: 41.8436
lon: -74.0428
The broad valley of the Wallkill River nestles between the main Appalachian Mountains and the New York-New Jersey Highlands, supporting much local agriculture. It is a part of the Great Appalachian Valley. In the beginning of its course it drains the eastern section of Sussex County, New Jersey, then flows through the Wallkill River National Wildlife Refuge at the New Jersey/New York state line.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
In 1892, construction of the line from Jaffa to Jerusalem was finally completed. It was built along the &quot;donkeys' trail&quot;, an ancient route ascending to Jerusalem which passed through Nahal Sorek and the Valley of Rephaim. The station was inaugurated on 26 September 1892 in the presence of the city's dignitaries, Jews and Arabs.

Geographic entities mentioned:
surface_form: Valley of Rephaim
instance_of: Valley
countries: Israel
coordinates: lat: 31.763202777778
lon: 35.219122222222
Location. The Balondo live in fifteen settlements in the South-west coastal region of Cameroon. The landscape comprises coastal mangrove swamps to the north-west of Mount Cameroon, forest reserves of the Mokoko River and Meme River in Ekondo-Titi subdivision, and two major palm plantations in Upper Balondo (Ekondo-Etiti subdivision) and Lower Balondo (Bamuso subdivision).

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Enna (stream). The Enna is a stream in the Bergamo Alps of northern Italy. It begins near Morterone, cuts through the Val Taleggio, passes near the village of Taleggio, and after flows into the Brembo river at San Giovanni Bianco. The Enna cuts a gorge called the Orrido della Val Taleggio.

Geographic entities mentioned:
surface_form: Val Taleggio
instance_of: Valley
countries: Italy
coordinates: lat: 45.8833
lon: 9.6
Political importance. El Sherana was included in the 1988 proposal of BHP to mine at the nearby Coronation Hill which also had been briefly mined for uranium in the 1950s. Opposed environmental campaigns came from many organisations including the Kakadu Action Group founded by Lindsay Mollison, part of the Australian Conservation Foundation.

Geographic entities mentioned:
surface_form: Coronation Hill
instance_of: Mountain
countries: Australia
coordinates: lat: -13.5868
lon: 132.6035
The last glaciation partly affected the Macizo de Ayllón forming some glacial cirques such as those found at the source of the Berbellido river, next to the Pico del Lobo, and at the Peña Cebollera Vieja. Granitic zones.

Geographic entities mentioned:
surface_form: Peña Cebollera Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: cebollera vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
The rest of the fluvial currents pour their waters into these two main rivers. Duratón River. Although it does not begin to take shape until it joins the rivers Caslilla and de la Hoz at Sepúlveda, the Duratón river, which rises on the southern slopes on the Madrid side of the Cebollera Vieja, receives water on its right bank from small streams that originate in the Sierra de Ayllón.

Geographic entities mentioned:
surface_form: Cebollera Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: duratón
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.583
lon: -4.122
surface_form: cebollera vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
From the northern slope of the Cebollera Vieja, it receives water from two streams that usually dry up in summer in most of its sections, the Cerezuelo river and the Serrano river, both of which rise on the slopes of the Pico del Lobo. Riaza River. The Riaza river rises near Puerto de la Quesera and receives water from the Sierra de Ayllón, mainly on its right bank.

Geographic entities mentioned:
surface_form: Cebollera Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: cebollera vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
Jarama River. It rises at the foot of the Cebollera Vieja and receives its major tributaries on its left bank, extending its basin from the Loma de la Cebollera to the Sierra del Ocejón.

Geographic entities mentioned:
surface_form: Cebollera Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: la cebollera
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: cebollera vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
The main tributaries of the Jarama through the Sierra de Ayllón are the Ermito river, which has its source under the Cervunal; the Berbellido river, which rises in Pico del Lobo and passes through Bocígano; the Jaramilla river, which after rising under Puerto de la Quesera leaves a deep and beautiful gorge to its mouth; the Arroyo de Vallosera, which rises in Pico de la Tornera and after cutting through a gorge in the area of La Vereda flows into the El Vado reservoir, next to the ruins of El Vado, and Arroyo del Soto, union of several minor streams that flow down from Ocejón and leave between it and Cabeza de Ranas a valley where Majaelrayo, Robleluengo, Campillo, El Espinar and Roblelacasa are located.

Geographic entities mentioned:
surface_form: Ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
It rises under the Atalaya and follows a winding path between mountains until it flows into the Sorbe river between Peña del Pinarejo and the Loma de las Piquerinas. To the north of the Ocejón rises the Arroyo de la Chorrera, which passes through Valverde and leaves the Chorreras de Despeñalagua on its way before flowing into the river.

Geographic entities mentioned:
surface_form: Ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
To the north of the Ocejón rises the Arroyo de la Chorrera, which passes through Valverde and leaves the Chorreras de Despeñalagua on its way before flowing into the river. And under the southern slope of the Ocejón the Seco river or Barranco del Covachón, which passes through Palancares. Fauna. Among the insects it is worth mentioning the great diversity that exists in the Macizo de Ayllón.

Geographic entities mentioned:
surface_form: Ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
Thus, with the creation of the &quot;Comunidades de Villa y Tierra&quot; the different towns that flourished again in the Sierra de Ayllón were divided into several of these: El Cardoso de la Sierra, Colmenar de la Sierra, El Vado, the area of the Cebollera Vieja and Cebollera Nueva, Somosierra, Santo Tomé del Puerto, Cerezos de Abajo and Cerezos de Arriba came under the jurisdiction of the &quot;Común de Villa y Tierra de Sepúlveda&quot;, which passed during the 14th century in good part to the Mendoza family, within the Marquisate of Montesclaros since the 15th century, from which fact still remains a House between El Cardoso and Colmenar; the area between the Sierra del Ocejón and the rivers Jaramilla and Berbedillo reaching south to Almiruete were included within the &quot;Común de Villa y Tierra de Ayllón&quot;, in the hands of the Marquis of Villena; Riofrío and Hontanares under the jurisdiction of the &quot;Comunidad de Cilla y Tierra de Fresno de Cantespino&quot;; from the Sierra del Ocejón and the Sorbe river eastward, including the term of Valverde de los Arroyos, is under the jurisdiction of the &quot;Común de Villa y Tierra de Atienza,&quot; and later, towards the 14th century, would be included in the newly created County of Galve, in the hands of the Zúñiga and, later, of the Mendoza and the dukes of Alba; the south of the massif in the districts of Valdepeñas, Tortuero and Valdesotos came under the jurisdiction of the &quot;Común de Villa y Tierra de Uceda&quot;, controlled since 1249 by Sancho of Castile, archbishop of Toledo and son of king Ferdinand III; Tamajón would remain as a land of Royal manor forming its own jurisdiction.

Geographic entities mentioned:
surface_form: Vieja
instance_of: Mountain
countries: Spain
coordinates: lat: 41.165044444444
lon: -3.5397111111111
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
Today there are two main economic engines in the area. On the one hand, the retirements, due to the high average age of its inhabitants. On the other hand, there is tourism, especially in the villages surrounding Pico Ocejón and in the Riaza area. Numerous rural lodgings, hikers and mountaineers routes through mountains and forests, and La Pinilla ski resort are its main tourist attractions.

Geographic entities mentioned:
surface_form: Pico Ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
The hydrographic system in the mountain chain has a high degree of conservation until the arrival of the rivers to the line of regulating reservoirs located south of the natural area, &quot;(Pontón de la Oliva, Vado reservoir, Beleña reservoir, Alcorlo reservoir)&quot;.

Geographic entities mentioned:
surface_form: pontón
instance_of: Mountain
countries: Spain
coordinates: lat: 42.231566666667
lon: -3.2063277777778
The massif was raised during the alpine orogeny, having a very broken relief, with steep slopes and a complicated and dense hydrographic system. It borders to the west with the Sierra de Somosierra and the Sierra del Rincón, to the east with the Sierra de Pela and Alto Rey mountain, to the north with the Meseta Norte and to the south with the Campiña de Guadalajara.

Geographic entities mentioned:
surface_form: meseta
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
Sierra de Ayllón. The Sierra de Ayllón (Ayllón mountain chain) or Macizo de Ayllón (Ayllón massif) is a mountain chain of the Iberian Peninsula, belonging to the Sistema Central, of which it constitutes one of its easternmost spurs. It is located between the Spanish provinces of Guadalajara, Segovia and Madrid.

Geographic entities mentioned:
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Orography and relief. There are three relief units that form the Macizo de Ayllón: the peneplain, areas of undulating surface located at the ends of the massif, mainly to the north and south; the valleys, short in the north and very long and narrow in the south, leaving little room for meadows, and the mountain range itself.

Geographic entities mentioned:
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
The Aguisejo river, which rises near Villacadima and in turn receives water from other smaller streams including the Arroyo de Vadillo, which after rising in the Pedrosa beech forest under the Mesa Peñota, flows into the left bank of the Aguisejo river, and the Cobos river, which has its source in the Majada de la Sierra, one of the last northern foothills of the Macizo de Ayllón.

Geographic entities mentioned:
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Thus, the Duratón river and the Aguisejo river border the Macizo de Ayllón from west to east in the north. Tagus Basin. The southern slope of the Sierra de Ayllón, which flows into the Tagus Basin, originates in the northern foothills of the massif.

Geographic entities mentioned:
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: duratón river
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.583
lon: -4.122
And under the southern slope of the Ocejón the Seco river or Barranco del Covachón, which passes through Palancares. Fauna. Among the insects it is worth mentioning the great diversity that exists in the Macizo de Ayllón. Numerous species of lepidoptera, coleoptera, hymenoptera and diptera can be observed throughout the mountain chain, some of them autochthonous and exclusive to the area.

Geographic entities mentioned:
surface_form: macizo de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Sierra de Ayllón. The Sierra de Ayllón (Ayllón mountain chain) or Macizo de Ayllón (Ayllón massif) is a mountain chain of the Iberian Peninsula, belonging to the Sistema Central, of which it constitutes one of its easternmost spurs. It is located between the Spanish provinces of Guadalajara, Segovia and Madrid.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
The natural area of Ayllón occupies the Paleozoic massif of the Sierra de Ayllón, in the province of Guadalajara, including the main core whose highest peak is the Pico del Lobo (2269 m), and the Sierras de la Concha (1865 m), Pico Ocejón (2048 m) and Alto Rey (1852 m). The Sierra de Ayllón is the eastern end of the Sistema Central, where the bioclimatic level is dominant.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
surface_form: ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
surface_form: pico ocejón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1046
lon: -3.2555
The natural area of Ayllón occupies the Paleozoic massif of the Sierra de Ayllón, in the province of Guadalajara, including the main core whose highest peak is the Pico del Lobo (2269 m), and the Sierras de la Concha (1865 m), Pico Ocejón (2048 m) and Alto Rey (1852 m). The Sierra de Ayllón is the eastern end of the Sistema Central, where the bioclimatic level is dominant.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Granitic zones. From west to east, from Puerto de Somosierra to El Cervunal, and from north to south, from Riaza to Puerto del Cardoso, following the right bank of the Ermito river, granite abounds among the rocks that form the mountains of this area of the Sierra de Ayllón. Gneissic zones. The gneiss is, however, the least widespread of the three predominant rocks in the Sierra de Ayllón.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Gneissic zones. The gneiss is, however, the least widespread of the three predominant rocks in the Sierra de Ayllón. It forms mainly in the area of El Cardoso de la Sierra to the south until the Jarama river acts as a natural boundary between the Sierra de Ayllón and the Campiña. Orography and relief.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
The mountain chain is distributed in a main ridge, which runs from west to east to the north of the mountain chain, and three secondary ridges, which leave the main one from north to south. The &quot;two-thousands&quot; of the Sierra de Ayllón. In the heart of the Sierra de Ayllón rise the last peaks of more than 2000 meters of the Sistema Central. Climate.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Climate. The mountain climate of the Sierra de Ayllón is marked by two fundamental factors: on the one hand, the latitude, marking the Mediterranean character with hot summers and low rainfall; on the other hand, the orientation of the massif causes the interception of the low-pressure areas of Atlantic origin bringing with it a greater rainfall on the northern slopes than in the south.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Riaza River. The Riaza river rises near Puerto de la Quesera and receives water from the Sierra de Ayllón, mainly on its right bank. Its tributaries are longer, although equally of little flow.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Tagus Basin. The southern slope of the Sierra de Ayllón, which flows into the Tagus Basin, originates in the northern foothills of the massif. It is much more complicated than the northern slope and the rivers and streams, much longer, run tortuously squeezed between mountains, giving rise to ravines and gorges, until they flow into the two main rivers in the area: the Jarama and the Sorbe.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Sorbe River. The Sorbe River is the natural boundary between the Sierra de Ayllón, on its right bank, and the Sierra de Alto Rey, on its left bank. It is the result of the union of two minor rivers in the area known as &quot;Junta de los ríos&quot;, between ravines on the slopes of Alto de las Cabras and Peña del Osar, on the Alto Rey side, and Peña de Pinarejo, on the Ayllón side.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
The Sorbe flows between Alarilla and Humanes, under the Muela de Alarilla, in the Henares river. Together with the Lillas and the Arroyo de la Dehesa, the Sorbe receives water from the Sierra de Ayllón from three other tributaries with permanent flow, which also follow winding paths and leave deep cuts in their courses.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Together with the Lillas and the Arroyo de la Dehesa, the Sorbe receives water from the Sierra de Ayllón from three other tributaries with permanent flow, which also follow winding paths and leave deep cuts in their courses. Further north, the Sonsaz river, which gives its name to the extensive hunting reserve that encompasses a large part of the valleys and mountains of the Sierra de Ayllón.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Other species of great interest such as Bonelli's eagle &quot;(Hieraaetus fasciatus)&quot;, Egyptian vulture &quot;(Neophron percnopterus) &quot;the common rock trush and the blue rock thrush &quot;(Monticola saxatilis and Monticola solitarius)&quot; use the Sierra de Ayllón as a breeding area.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
The Pyrenean oak groves of the Sierra de Ayllón, &quot;(Festuco heterophyllae-Quercetum pyrenaicae&quot; and &quot;Luzulo forsteri-Quercetum pyrenaicae)&quot;, are the most extensive and representative of Castilla-La Mancha, presenting as characteristic cortege &quot;Arenaria montana, Luzula forsteri, Viola riviniana, Poa nemoralia, Primula veris, Viola sylvatica, Holcus molli, Conopodium bourgaei, etc.&quot;.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
As for the rest of the towns in the area, the loss of inhabitants is continuous, although it is true that in some areas there is a stabilization of the population due mainly to rural tourism in some of its municipalities, which gives a certain air, although scarce, of economic prosperity in the Sierra de Ayllón. Populations.

Geographic entities mentioned:
surface_form: sierra de ayllón
instance_of: Mountain
countries: Spain
coordinates: lat: 41.1667
lon: -3.43333
Douro Basin. It is the last foothills of the mountain chain which pours water to the northern slope. The rivers and streams pour their waters directly from the mountain to the valley, so they are generally short and not very abundant. Two rivers stand out above the rest, the Duratón river and the Riaza river, both of which flow into the Douro river after a long journey. They are exceptions.

Geographic entities mentioned:
surface_form: duratón river
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.583
lon: -4.122
Laval extension. Announced in 1998 by the STCUM, the project to extend the Orange Line past the Henri-Bourassa terminus to the city of Laval, passing under the Rivière des Prairies, was launched March 18, 2002. The extension was decided and funded by the Government of Quebec.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Miseryfjellet. Miseryfjellet (Misery Mountain), at, is the tallest peak on Bear Island (Bjørnøya) of the Norwegian Svalbard archipelago in the Barents Sea. Miseryfjellet is on the eastern side of Bear Island and contains three distinct component peaks, Urd, Verdande and Skuld. These peaks are named after the three Norns in Norse Mythology.

Geographic entities mentioned:
surface_form: miseryfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 74.423333333333
lon: 19.191666666667
In it had a population of. History. In 1988 four families received land from the Israel Land Administration in return for giving up their land on Mount Meron. The site had previously been the Arab village of Qaddita, whose residents fled during the 1948 Arab–Israeli War. Rabbi Tarfon was buried in the area.

Geographic entities mentioned:
surface_form: Mount Meron
instance_of: Mountain
countries: Mandatory Palestine
Israel
Ottoman Empire
coordinates: lat: 32.9975
lon: 35.41222222222222
Atwood Lake (New York). Atwood Lake is a small lake southeast of Wilmurt in Herkimer County, New York. It drains northwest via an unnamed creek that flows into Spectacle Lake.

Geographic entities mentioned:
surface_form: spectacle lake
instance_of: Lake
countries: United States
coordinates: lat: 47.461944444444
lon: -121.28083333333
surface_form: spectacle lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3664648
lon: -74.89983
surface_form: spectacle lake
instance_of: Lake
countries: United States
coordinates: lat: 45.570277777778
lon: -93.404166666667
surface_form: spectacle lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2397024
lon: -74.5797024
Atwood Lake (New York). Atwood Lake is a small lake southeast of Wilmurt in Herkimer County, New York. It drains northwest via an unnamed creek that flows into Spectacle Lake.

Geographic entities mentioned:
surface_form: atwood lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3649409
lon: -74.8978361
Shortly thereafter the Kirnitzsch enters the narrow Kirnitzsch Valley (&quot;Kirnitzschtal&quot;). It flows through the valley for about to the Lichtenhain Waterfall. After another it discharges into the Elbe at Bad Schandau. Over its last few kilometres it is followed by the Kirnitzschtal tramway that runs parallel to the Kirnitzsch.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
La Rösa. La Rösa is a hamlet in the upper part of the Val Poschiavo in the canton of Graubünden, Switzerland. It lies at above sea level on the southern approach to the Bernina Pass, and is in the municipality of Poschiavo, some north of the village of the same name. Because of the elevation difference between the two villages, the distance between them by road is.

Geographic entities mentioned:
surface_form: Val Poschiavo
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.308888888889
lon: 10.061388888889
A 7 km snow-cleared hiking trail follows the old cart track up to Ospizio Bernina, making the hamlet a popular starting point for winter snow-shoe tours, while in summer the hotel operates as an information hub for the Val Poschiavo section of the Via Albula/Bernina long-distance path.

Geographic entities mentioned:
surface_form: Val Poschiavo
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.308888888889
lon: 10.061388888889
Location. Cayley Glacier terminates on the Danco Coast of the Antarctic Peninsula, on the west side of Graham Land. It flows north from the south end of the Detroit Plateau and the north end of the Herbert Plateau into Hughes Bay, which opens onto the Gerlache Strait. Baldwin Peak is a prominent feature of the east side of te glacier.

Geographic entities mentioned:
surface_form: Detroit Plateau
instance_of: Plateau
coordinates: lat: -64.1667
lon: -60
surface_form: Herbert Plateau
instance_of: Landform
coordinates: lat: -64.53333333
lon: -61.25
Named after the settlement of Kormyansko in Northern Bulgaria. Egerika Range. A mostly ice-covered range extending in south–north direction and wide, rising to high in the north foothills of Herbert Plateau. Connected to Obretenik Bastion to the south by Kormyansko Saddle. Surmounts Blériot Glacier to the west, Hughes Bay to the northwest and Cayley Glacier to the east.

Geographic entities mentioned:
surface_form: Herbert Plateau
instance_of: Landform
coordinates: lat: -64.53333333
lon: -61.25
In October 1840, at 28 years of age, Grey was appointed Governor of South Australia. Hill River development. In the 1990s a proposed utilization of coal deposits at Mount Lesueur north of the river by the Hill River Power Development Company Pty Ltd, was abandoned in 1990 due to the creation of the Mount Leseuer National Park. Uses.

Geographic entities mentioned:
surface_form: Mount Lesueur
instance_of: Mountain
countries: Australia
coordinates: lat: -30.1755
lon: 115.19908333333
Blekketjernshøgda. Blekketjernshøgda is a mountain of the municipality of Nittedal in Akershus, Norway. It has a height of 613 meters above sea level.

Geographic entities mentioned:
surface_form: blekketjernshøgda
instance_of: Mountain
countries: Norway
coordinates: lat: 60.17746
lon: 10.78213
The population was 1,109 at the 2020 census. Pacific City is home to the Cape Kiwanda State Natural Area. History. In 1845, Mr. Johnson, a cook on an English ship sailing along the Columbia River, deserted and traveled down the Willamette Valley. Establishing a land claim in Champoeg, he began removing brush and that summer set off a burn to clear debris.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Dünkheger. Dünkheger (&quot;Dungheger ûûl&quot;;), also known as Mount Altun Obo (;;), is the highest peak of Baitag Bogda (,), a mountain range in the Altai Mountains of Asia. It has an elevation of and is on the international border between Qitai County, China and Khovd Province, Mongolia.

Geographic entities mentioned:
surface_form: dünkheger
instance_of: Mountain
countries: Mongolia
People's Republic of China
coordinates: lat: 45.2
lon: 90.9
Dünkheger. Dünkheger (&quot;Dungheger ûûl&quot;;), also known as Mount Altun Obo (;;), is the highest peak of Baitag Bogda (,), a mountain range in the Altai Mountains of Asia. It has an elevation of and is on the international border between Qitai County, China and Khovd Province, Mongolia.

Geographic entities mentioned:
surface_form: dünkheger
instance_of: Mountain
countries: Mongolia
People's Republic of China
coordinates: lat: 45.2
lon: 90.9
surface_form: dungheger
instance_of: Mountain
countries: Mongolia
People's Republic of China
coordinates: lat: 45.2
lon: 90.9
The second husband of Malamaʻihanaʻae was Haunaʻakamahala, who was a priest, and he ordered the construction of a &quot;heiau&quot; (temple). Their daughter was Lady Kapo-a-Kauluhailea, who married her half-brother Kahai and became the mother of the great Kalaunuiohua. It is unknown when did Malamaʻihanaʻae die. Her son's royal court was located in Waipio Valley.

Geographic entities mentioned:
surface_form: Waipio Valley
instance_of: Valley
countries: United States
coordinates: lat: 20.1197
lon: -155.593
This includes portions of the Eurasian land mass currently or traditionally considered as the continent of Asia. The continent is commonly described as the region east of the Ural Mountains, the Caucasus Mountains, the Caspian Sea, Black Sea and Red Sea, bounded by the Pacific, Indian, and Arctic Oceans. This article gives an overview of the many regions of Asia during prehistoric times.

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
At the southwestern edge of North Asia is Caucasus. It is a region at the border of Europe and Asia, situated between the Black and the Caspian seas. Caucasus is home to the Caucasus Mountains, which contain Europe's highest mountain, Mount Elbrus.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
It is a region at the border of Europe and Asia, situated between the Black and the Caspian seas. Caucasus is home to the Caucasus Mountains, which contain Europe's highest mountain, Mount Elbrus. The southern part of the Caucasus consists of independent sovereign states, whereas the northern parts are under the jurisdiction of the Russian Federation.

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875