Sarmila/GeoWiki-Features huggingface dataset:
Climate. Based on the Köppen climate classification, Table Top Mountain has a subarctic climate with cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Boundary Ranges (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: table top mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1407
lon: -73.9163
surface_form: table top mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.2922
lon: -134.501
Weather systems coming off the Gulf of Alaska are forced upwards by the Boundary Ranges (orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The month of July offers the most favorable weather for viewing and climbing Table Top Mountain.

Geographic entities mentioned:
surface_form: table top mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1407
lon: -73.9163
surface_form: table top mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.2922
lon: -134.501
The genealogy of Saint Kerrill of Clonkeenkerrill is given as &quot;Caireall mac Curnáin mac Treana mac Fionnchada mac Náir mac Earca mac Tiobraide mac Soghain Salbhuidhe mac Fiacha Araidhe&quot;. His grandfather, Treana mac Fionnchada, was the eponym of the Cinel Trena, who were apparently located close to Knockma, as evinced by the placename Tír Mhic Trena (the land of the sons of Trena).

Geographic entities mentioned:
surface_form: Knockma
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.48186111
lon: -8.96054444
Mount al-Hass. Mount Ḥaṣṣ or Mount Aḥaṣṣ (; northern Syrian vernacular: ǧabal əl-Ḥəṣṣ) is a 500-metre-high plateau (maximum height 638 m) on the northern fringe of the Syrian Desert. It is located in the Safīrah District of Aleppo Governorate in Syria. Location and description.

Geographic entities mentioned:
surface_form: mount al-hass
instance_of: Mountain
countries: Syria
coordinates: lat: 35.97
lon: 37.31166667
surface_form: al-hass
instance_of: Mountain
countries: Syria
coordinates: lat: 35.97
lon: 37.31166667
Conflicting claims regarding both the kingdom's extent and arguable nonexistence were pursued in diplomatic exchanges. The British and Miskito definition applied to the whole eastern seaboard of Central America from the Aguan River to the Chiriqui Lagoon area. History.

Geographic entities mentioned:
surface_form: Chiriqui Lagoon
instance_of: Lake
countries: Panama
coordinates: lat: 9.033333333333333
lon: -82.01666666666667
At the request of the civil population and an American captain of a United States brig the Nicaraguan commandant of the port, Colonel Manuel Quijano, was removed and later dropped off at Cape Gracias a Dios to find his own way back to Nicaragua. The Nicaraguan government protested, but the British did not take action against MacDonald for the incident.

Geographic entities mentioned:
surface_form: Cape Gracias a Dios
instance_of: Landform
countries: Honduras
coordinates: lat: 15.0064851
lon: -83.1301235
The kingdom was claimed to extend from Cape Honduras in the north to the mouth of the San Juan River in the south, and south to the area around the Chiriquí Lagoon.

Geographic entities mentioned:
surface_form: Chiriquí Lagoon
instance_of: Lake
countries: Panama
coordinates: lat: 9.033333333333333
lon: -82.01666666666667
After the ultimatum expired, Miskito-British forces led by the King and Patrick Walker, and backed by two British warships, seized San Juan del Norte. They also destroyed Serapaqui, where the British prisoners captured during the first attempt on San Juan del Norte were interned, and advanced to Lake Nicaragua, during which Walker drowned.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
G. Squier, tried to get Nicaragua, El Salvador and Honduras to form a common front against the British, who were now threatening to annex Tiger Island (&quot;El Tigre&quot;) in Honduras' Pacific coast. After British and American forces nearly clashed in El Tigre, both governments reprimanded the commanders of their forces there and concluded the Clayton–Bulwer Treaty on April 18, 1850.

Geographic entities mentioned:
surface_form: Tiger Island
instance_of: Mountain
countries: Honduras
coordinates: lat: 13.265555555556
lon: -87.637777777778
It lies on the Médanos Isthmus and covers of desert and coastal habitat, including salt marshes. It is made up of three zones: an alluvial plain, formed by the delta of the Mitare River and some smaller streams; an aeolian plain, composed of three types of dunes; and a littoral plain with a belt of mangrove swamps. The massive sand dunes, known as Médanos, spread over an area of approximately.

Geographic entities mentioned:
surface_form: Mitare River
instance_of: Watercourse
countries: Venezuela
coordinates: lat: 11.404667
lon: -69.968788
Mount Barre. Mount Barre () is a mountain with an ice-covered, pyramidal peak, 2,195 m, standing 2 nautical miles (3.7 km) northeast of Mount Gaudry in the south part of Adelaide Island. Discovered and surveyed in 1909 by the French Antarctic Expedition under Charcot.

Geographic entities mentioned:
surface_form: Mount Gaudry
instance_of: Mountain
coordinates: lat: -67.5333
lon: -68.6167
surface_form: gaudry
instance_of: Mountain
coordinates: lat: -67.5333
lon: -68.6167
surface_form: mount barre
instance_of: Mountain
coordinates: lat: -67.5
lon: -68.55
Mount Barre. Mount Barre () is a mountain with an ice-covered, pyramidal peak, 2,195 m, standing 2 nautical miles (3.7 km) northeast of Mount Gaudry in the south part of Adelaide Island. Discovered and surveyed in 1909 by the French Antarctic Expedition under Charcot.

Geographic entities mentioned:
surface_form: mount barre
instance_of: Mountain
coordinates: lat: -67.5
lon: -68.55
It is native to California from Santa Clara County to San Diego County, as well as from Mohave County in Arizona. The plant grows on the slopes of the Transverse Ranges, and the Inner South California Coast Ranges adjacent to the western edge of the Central Valley—San Joaquin Valley. Description.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Penrhiw-ceibr. Penrhiw-ceibr (formerly Penrhiwceiber) is an electoral ward in the Cynon Valley, Rhondda Cynon Taf, Wales. Its boundaries are coterminous with the village and community of Penrhiwceiber. The ward elects two councillors to Rhondda Cynon Taf County Borough Council. Background. Penrhiwceiber was created in 1898 as a ward to Mountain Ash Urban District Council.

Geographic entities mentioned:
surface_form: Cynon Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.657
lon: -3.461
It is an herbaceous perennial or subshrub native to southeastern Nigeria, Cameroon, and Bioko island in Equatorial Guinea. Its natural habitat is tropical montane forest from 2,000 to 2,950 meters elevation. It has been recorded at Pico Basilé on Bioko, on Mount Cameroon and Mann's Spring, Bokwangwo, Bamboutos, Mount Oku, and the Adamawa Plateau in Cameroon, and Mabile-Ngelyaki in Nigeria.

Geographic entities mentioned:
surface_form: Pico Basilé
instance_of: Mountain
countries: Equatorial Guinea
coordinates: lat: 3.5833333333333
lon: 8.7666666666667
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
surface_form: Mount Oku
instance_of: Mountain
countries: Cameroon
coordinates: lat: 6.1997222222222
lon: 10.518888888889
surface_form: Adamawa Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 9.8
lon: 14.08333333
The 2004 season of the Montserrat Championship was the seventh recorded season of top flight association football competition in Montserrat, with records for any competition held between 1975 and 1995 not available, the third iteration of the championship since the 1996–97 season was abandoned when the Soufrière Hills erupted causing widespread devastation to the island, and, as of 2015, the last recorded season of competitive football on the island.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
The nearest inhabited place is Zhanatogan (Жаңатоған), Karkaraly District. Geography. Kyzyltas is one of the ranges of the southern part of the Kazakh Upland system (Saryarka). The slightly higher Kyzylarai massif rises to the southeast and the Karkaraly and Kent mountain ranges lie to the northeast. The ridges of the Kyzyltas are deeply dissected by gorges, valleys and ravines.

Geographic entities mentioned:
surface_form: Kyzylarai
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 48.4433
lon: 75.5292
surface_form: Kent
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49.224444444444444
lon: 76.03944444444444
The slightly higher Kyzylarai massif rises to the southeast and the Karkaraly and Kent mountain ranges lie to the northeast. The ridges of the Kyzyltas are deeply dissected by gorges, valleys and ravines. The Nura river has its sources in the range and flows northwards and then westwards into Lake Tengiz. Its main tributary Sherubaynura also has its sources in Kyzyltas.

Geographic entities mentioned:
surface_form: Lake Tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
surface_form: tengiz
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 50.439722222222
lon: 68.9
The Nura river has its sources in the range and flows northwards and then westwards into Lake Tengiz. Its main tributary Sherubaynura also has its sources in Kyzyltas. Other rivers originating in the range are the Zhamshi, Zharly and Tokrau; the latter flows southwards towards Lake Balkhash, but its waters get lost in the semidesert sands. The highest point is Kushoky (Қушоқы), a high summit.

Geographic entities mentioned:
surface_form: Lake Balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
surface_form: balkhash
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.540833333333
lon: 74.878888888889
Kyzyltas. Kyzyltas () is a range of mountains in Aktogay District, Karaganda Region, Kazakhstan. The nearest inhabited place is Zhanatogan (Жаңатоған), Karkaraly District. Geography. Kyzyltas is one of the ranges of the southern part of the Kazakh Upland system (Saryarka). The slightly higher Kyzylarai massif rises to the southeast and the Karkaraly and Kent mountain ranges lie to the northeast.

Geographic entities mentioned:
surface_form: kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
The nearest inhabited place is Zhanatogan (Жаңатоған), Karkaraly District. Geography. Kyzyltas is one of the ranges of the southern part of the Kazakh Upland system (Saryarka). The slightly higher Kyzylarai massif rises to the southeast and the Karkaraly and Kent mountain ranges lie to the northeast. The ridges of the Kyzyltas are deeply dissected by gorges, valleys and ravines.

Geographic entities mentioned:
surface_form: kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
Kyzyltas is one of the ranges of the southern part of the Kazakh Upland system (Saryarka). The slightly higher Kyzylarai massif rises to the southeast and the Karkaraly and Kent mountain ranges lie to the northeast. The ridges of the Kyzyltas are deeply dissected by gorges, valleys and ravines. The Nura river has its sources in the range and flows northwards and then westwards into Lake Tengiz.

Geographic entities mentioned:
surface_form: kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
The Nura river has its sources in the range and flows northwards and then westwards into Lake Tengiz. Its main tributary Sherubaynura also has its sources in Kyzyltas. Other rivers originating in the range are the Zhamshi, Zharly and Tokrau; the latter flows southwards towards Lake Balkhash, but its waters get lost in the semidesert sands. The highest point is Kushoky (Қушоқы), a high summit.

Geographic entities mentioned:
surface_form: kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
The highest point is Kushoky (Қушоқы), a high summit. Other important peaks are Kimatas (Қиматас) —, Korpetai (Көрпетай) —, Zhantau (Жантау) —, Sorang (Сораң) —, Kyzyltas (peak) —, Zhylandy (Жыланды) —, Keregetas (Керегетас) —, Nurtai (Нұртай) —, Otar (Отар) —, Saryzhol (Сарыжол) —, Akshoky (Ақшоқы) —, Akkemer (Ақкемер) —, Kyzyladyr (Қызыладыр) — and Berikkara (Берікқара) —. Flora.

Geographic entities mentioned:
surface_form: kyzyltas
instance_of: Mountain
countries: Kazakhstan
coordinates: lat: 49
lon: 74.733333333333
It was also recorded as the wettest March in 48 years. Impact. &quot;Usually, from February, western disturbances tend to subside. But this year, not only were the disturbances more active, they extended up to April. Also, there was an induced low pressure, which pulled moisture both from the Bay of Bengal and the Arabian Sea.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Cornizzolo. Monte Cornizzolo (Insubric &quot;Curnisciöö&quot;) is a mountain situated between the province of Como and the province of Lecco, Lombardy, northern Italy, particularly in the territory of the village of Canzo. The peak reaches 1,241 metres in altitude. It houses the Marisa Consigliere mountain hut, open every Sunday throughout the year, at 1,100 metres above sea level.

Geographic entities mentioned:
surface_form: monte cornizzolo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.83723518817086
lon: 9.301895486138065
surface_form: curnisciöö
instance_of: Mountain
countries: Italy
coordinates: lat: 45.83723518817086
lon: 9.301895486138065
surface_form: cornizzolo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.83723518817086
lon: 9.301895486138065
Cornizzolo. Monte Cornizzolo (Insubric &quot;Curnisciöö&quot;) is a mountain situated between the province of Como and the province of Lecco, Lombardy, northern Italy, particularly in the territory of the village of Canzo. The peak reaches 1,241 metres in altitude. It houses the Marisa Consigliere mountain hut, open every Sunday throughout the year, at 1,100 metres above sea level.

Geographic entities mentioned:
surface_form: cornizzolo
instance_of: Mountain
countries: Italy
coordinates: lat: 45.83723518817086
lon: 9.301895486138065
Prospect Mountain (Vermont). Prospect mountain is a mountain located in the town of Woodford, Vermont in Bennington County, Vermont. The mountain is located in the southern region of Vermont's Green Mountains. It is home to the Prospect Mountain Nordic Ski Area, which has the highest base elevation of any ski area in New England, accounting for its abundance of natural snow.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Prospect Mountain (Vermont). Prospect mountain is a mountain located in the town of Woodford, Vermont in Bennington County, Vermont. The mountain is located in the southern region of Vermont's Green Mountains. It is home to the Prospect Mountain Nordic Ski Area, which has the highest base elevation of any ski area in New England, accounting for its abundance of natural snow.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain (vermont)
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
The mountain is located in the southern region of Vermont's Green Mountains. It is home to the Prospect Mountain Nordic Ski Area, which has the highest base elevation of any ski area in New England, accounting for its abundance of natural snow. Prospect Mountain can be counted on to provide a long season for cross-country skiing.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
It is home to the Prospect Mountain Nordic Ski Area, which has the highest base elevation of any ski area in New England, accounting for its abundance of natural snow. Prospect Mountain can be counted on to provide a long season for cross-country skiing. Since the mid-1930s, when Alex Drysdale opened the first rope tow on Prospect Mountain in Woodford, the mountain has been used for recreation.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Prospect Mountain can be counted on to provide a long season for cross-country skiing. Since the mid-1930s, when Alex Drysdale opened the first rope tow on Prospect Mountain in Woodford, the mountain has been used for recreation. Around 1938, William D.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Since the mid-1930s, when Alex Drysdale opened the first rope tow on Prospect Mountain in Woodford, the mountain has been used for recreation. Around 1938, William D. Mundell, future Vermont poet laureate, purchased land and opened the Woodford Ski Area in the lower part of what would eventually become the current-day Prospect Mountain Nordic Ski Area.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
William Morse, with a contract to rebuild Route 9 from Bennington, likely reopened Prospect in 1961–62 with a new 3,200 foot long T-Bar. With the new lift and vertical drop expanded to some 675 feet, Prospect Mountain became a mid-sized ski area. Morse sold the ski area to Bennington attorney Joseph Parks in October 1978.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Morse sold the ski area to Bennington attorney Joseph Parks in October 1978. Night skiing and cross country skiing (the former Timberlane Trails touring center) operations were added for 1979–1980. Prospect Mountain has over 35 kilometers of expertly groomed ski trails, and offers excellent skiing to everyone from racers to families. Snowshoe and backcountry ski trails are available.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Steve Whitham and Andrea Amodeo purchased the ski area from Joe Parks in 1991. After deciding to sell it, they worked with the Prospect Mountain Association (PMA) to transition ownership. PMA is primarily a volunteer organization that relies the energy and efforts of season pass holders and supporters. Steve Whitham is staying on as the Mountain Manager and is now an employee of PMA.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Williams College Nordic ski teams have used Prospect Mountain for training and race events, as have Mount Anthony Union High School and Mount Greylock Regional High School in Williamstown, Mass.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: mount greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Prospect Mountain will now serve as the home base for the Williams Nordic team and host the college's winter carnival, Newell said, adding that the PMA has a nine-member board of directors, including four associated with the college.

Geographic entities mentioned:
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0772
lon: -90.7395
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.424722222222
lon: -73.745555555556
surface_form: prospect mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.8744
lon: -73.0669
Dorchester Friary. Dorchester Friary, also known as Dorchester Priory, was a Franciscan friary formerly located in Dorchester, Dorset, England. The friary stood on the north side of the town (), on the banks of the River Frome, a little east of the site of Dorchester Castle. Possibly a royal foundation, it was in existence by 1267, and it was dissolved in 1538.

Geographic entities mentioned:
surface_form: River Frome
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 50.6958
lon: -1.98861
Lough Cullin. Lough Cullin () is a lake in County Mayo in Ireland. With its immediate neighbour to the north, Lough Conn, it is connected to the Atlantic by the River Moy. Lough Cullin is noted for its trout and salmon fishing. In Celtic mythology, Lough Cullin was created when Fionn mac Cumhaill was hunting with his hounds; Cullin and Conn. They came across a wild boar.

Geographic entities mentioned:
surface_form: Lough Conn
instance_of: Lake
countries: Ireland
coordinates: lat: 54.043333333333
lon: -9.245
Lough Cullin. Lough Cullin () is a lake in County Mayo in Ireland. With its immediate neighbour to the north, Lough Conn, it is connected to the Atlantic by the River Moy. Lough Cullin is noted for its trout and salmon fishing. In Celtic mythology, Lough Cullin was created when Fionn mac Cumhaill was hunting with his hounds; Cullin and Conn. They came across a wild boar.

Geographic entities mentioned:
surface_form: lough cullin
instance_of: Lake
countries: Ireland
coordinates: lat: 53.9702
lon: -9.1745
surface_form: lough cullin
instance_of: Lake
countries: Ireland
coordinates: lat: 52.316756
lon: -7.112918
With its immediate neighbour to the north, Lough Conn, it is connected to the Atlantic by the River Moy. Lough Cullin is noted for its trout and salmon fishing. In Celtic mythology, Lough Cullin was created when Fionn mac Cumhaill was hunting with his hounds; Cullin and Conn. They came across a wild boar. Finn and the hounds attempted to chase it.

Geographic entities mentioned:
surface_form: lough cullin
instance_of: Lake
countries: Ireland
coordinates: lat: 53.9702
lon: -9.1745
surface_form: lough cullin
instance_of: Lake
countries: Ireland
coordinates: lat: 52.316756
lon: -7.112918
Before 2007, the lake was called Lac Saint-François. It was renamed to avoid confusion with Petit lac Saint-François (Ashberham) which is located 1.5 km northwest of it. In 1815, the vast territory where the lake is located was not yet surveyed as mentioned by Joseph Bouchette in his book “Description topographique du Bas-Canada”.

Geographic entities mentioned:
surface_form: petit lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.98833
lon: -71.27184
surface_form: petit lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.53695
lon: -72.03667
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Grand lac Saint François. This lake is located southeast of the city of Thetford Mines. It is the source of the Saint-François River. Much of the lake is surrounded by the Frontenac National Park. Located in a forest environment, this lake is one of the main attractions of Parc national de Frontenac. The resort is very dense on the north shore of Grand Lac Saint-François.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac saint françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Located in a forest environment, this lake is one of the main attractions of Parc national de Frontenac. The resort is very dense on the north shore of Grand Lac Saint-François. The surface of this body of water is generally frozen from mid-November to the end of April; however, the period of safe traffic on the ice is usually from mid-December to the end of March. Geography.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
The maximum width of the lake is in the northern part, where the lake forms a long bay stretching southwest to the retaining dam located at the mouth. Grand lac Saint-François is the main head water body of the Saint-François River. This river flows a priori for 10.7 km towards the southwest to join Lake Aylmer at Disraeli, which the current crosses to head south. Toponymy.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Later, in 1917, the dam at the outlet of the lake will raise the level by 7 meters and increase the area to its present size. Petit lac Saint-François is located 1.5 km northwest of Grand lac Saint-François.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Petit lac Saint-François is located 1.5 km northwest of Grand lac Saint-François. Following the request of the riparian municipalities and in order to avoid confusion with other hydronyms using the name “Lac Saint-François”, on May 10, 2007, the name “Grand lac Saint-François” was changed. formalized by the Commission de toponymie du Québec replacing the designation &quot;Lac Saint-François&quot;.

Geographic entities mentioned:
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 48.866666666667
lon: -57.433333333333
surface_form: grand lac
instance_of: Lake
countries: Canada
coordinates: lat: 45.933611111111
lon: -66.032777777778
surface_form: grand lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
The maximum width of the lake is in the northern part, where the lake forms a long bay stretching southwest to the retaining dam located at the mouth. Grand lac Saint-François is the main head water body of the Saint-François River. This river flows a priori for 10.7 km towards the southwest to join Lake Aylmer at Disraeli, which the current crosses to head south. Toponymy.

Geographic entities mentioned:
surface_form: lake aylmer
instance_of: Lake
countries: Canada
coordinates: lat: 45.8144
lon: -71.3767
This seigneury was bounded by this watercourse, as indicated in an act of 1638 signed by the governor of Montmagny. The Abénaqui s name the lake &quot;Ônkobagak&quot;, which means &quot;connected lake&quot;. Before 2007, the lake was called Lac Saint-François. It was renamed to avoid confusion with Petit lac Saint-François (Ashberham) which is located 1.5 km northwest of it.

Geographic entities mentioned:
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Petit lac Saint-François is located 1.5 km northwest of Grand lac Saint-François. Following the request of the riparian municipalities and in order to avoid confusion with other hydronyms using the name “Lac Saint-François”, on May 10, 2007, the name “Grand lac Saint-François” was changed. formalized by the Commission de toponymie du Québec replacing the designation &quot;Lac Saint-François&quot;.

Geographic entities mentioned:
surface_form: lac saint-françois
instance_of: Lake
countries: Canada
coordinates: lat: 45.8986
lon: -71.1578
Religious significance. Bhuikhel is of sacred significance because it is the site of the Samyak ceremony of Kathmandu. This alms-giving festival is held in all the three cities of the Kathmandu Valley at differing intervals. In Bhaktapur, Samyak is celebrated annually, in Patan it occurs every five years, and in Kathmandu it takes place once every 12 years. The most recent one was held in 2005.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Beginning in the Rio Piedras district of barrio Oriente in San Juan at Jesus de Piñero Avenue (PR-17), it runs through Trujillo Alto, Gurabo and San Lorenzo on the Caguas Valley, and western Yabucoa and eastern Patillas on the Sierra de Cayey, before ending in the Patillas Pueblo downtown area on the southeastern coastal plain of Puerto Rico.

Geographic entities mentioned:
surface_form: Caguas Valley
instance_of: Valley
countries: United States
coordinates: lat: 18.231388888888887
lon: -66.03944444444444
Each Region of Colombia has their own indigenous culture that influenced the local culture, such as the Quechua in the Southwest, the Quimbaya in the Paisa Region, the Zenú and Tairona in the Caribbean, the Calima in Valle del Cauca, and the largest indigenous influence in Colombia, the Muisca in the Altiplano Cundiboyacense.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
This is attributed to the fact that Colombia was not a unified nation during the Pre-Columbian Era and different regions had different indigenous civilizations inhabiting it, such as the Quimbaya in the Paisa region, the Muisca in the Altiplano Cundiboyacense, the Zenú and the Tairona in the Caribbean, the Pubenenses in Popayán, the Incas in Nariño, and the Calima in Valle del Cauca.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
In the west, the basin is bound by uplifted areas with the small Ñirihuau Basin. The area of the basin is sparsely populated, with Gastre and Paso del Sapo representing some of the few villages in the basin. The Chubut River crosses the basin in the south in the Altar Valley. Basin evolution.

Geographic entities mentioned:
surface_form: Altar Valley
instance_of: Valley
countries: United States
coordinates: lat: 31.82
lon: -111.4
Indigenous people include Arapaso, Bará, Barasana, Desana, Carapanã, Kotiria, Cubeo, Macuna, Pira-tapuya, Siriano, Tucano and Tuyuka of the Tucanoan languages group, Baniwa, Baré, Koripako, Tariana, Warekena of the Arawakan languages group and Hupda and of the Nadahup languages group. The Eastern Tucano live along the Uaupés River and its tributaries, and the Pira Paraná River in Colombia.

Geographic entities mentioned:
surface_form: Pira Paraná River
instance_of: Watercourse
countries: Colombia
coordinates: lat: -0.432567
lon: -70.253337
Grindleford is popular with walkers and climbers due to its proximity to a variety of landscapes, including open moorland, wooded river valleys (including Padley Gorge), several gritstone escarpments, and the broad Hope Valley.

Geographic entities mentioned:
surface_form: Padley Gorge
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.3055
lon: -1.6248
surface_form: Hope Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.34727
lon: -1.7455
Mount Binuluan. Mount Binuluan (also known as Ambalatungan) is a remote volcano in the Kalinga province of the Cordillera Administrative Region of the Philippines. The mountain is part of the Cordillera Central mountain range on Luzon island, the largest island in the country. Binuluan exhibits active volcanism through numerous fumarole fields, solfataras and hot springs on its slope.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Mount Binuluan. Mount Binuluan (also known as Ambalatungan) is a remote volcano in the Kalinga province of the Cordillera Administrative Region of the Philippines. The mountain is part of the Cordillera Central mountain range on Luzon island, the largest island in the country. Binuluan exhibits active volcanism through numerous fumarole fields, solfataras and hot springs on its slope.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
surface_form: ambalatungan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Binuluan exhibits active volcanism through numerous fumarole fields, solfataras and hot springs on its slope. There were reports of possible eruptions in 1952 and 1986 (or 1987), but they are unverified. Geography. Mount Binuluan is one of the highest peaks in the area. The mountain is surrounded by the municipalities of Lubuagan, Pasil and Tinglayan in Kalinga province.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Southeast of the mountain is the Chico River flowing from southwest to northeast direction, while due northwest of the mountain is Pasil River, also flowing from southwest to northeast direction merging with Chico River just past the mountain. Mount Binuluan belongs to a range of mountains situated between the two rivers, trending southwest to northeast.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Geology. The Smithsonian Institution's Global Volcanism Program list Binuluan under the Ambalatungan Group. The Bumabag and Podakan volcanoes could possibly be flank vents of Mount Binuluan. The Philippines Institute of Volcanology and Seismology (PHIVOLCS) lists Binuluan or Ambalatungan as an inactive volcano. Geothermal features. Mount Binuluan exhibits a number of active geothermal features.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Possible eruptions. A possible phreatic or steam eruption was reported from Mount Binuluan in 1952, during which a sulfur-rich debris flow killed a dozen people. Details about the eruption in 1952 are still scant.

Geographic entities mentioned:
surface_form: mount binuluan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
South of this line of mountains are Mount Chumangil and Mount Patoc, the other volcano of the Central Cordillera Range displaying strong fumarolic activity. Geology. The Smithsonian Institution's Global Volcanism Program list Binuluan under the Ambalatungan Group. The Bumabag and Podakan volcanoes could possibly be flank vents of Mount Binuluan.

Geographic entities mentioned:
surface_form: ambalatungan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Geology. The Smithsonian Institution's Global Volcanism Program list Binuluan under the Ambalatungan Group. The Bumabag and Podakan volcanoes could possibly be flank vents of Mount Binuluan. The Philippines Institute of Volcanology and Seismology (PHIVOLCS) lists Binuluan or Ambalatungan as an inactive volcano. Geothermal features. Mount Binuluan exhibits a number of active geothermal features.

Geographic entities mentioned:
surface_form: ambalatungan
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.31
lon: 121.1
Just southwest of Binuluan is Mount Mosimus, followed by Mount Cauitan and Mount Alchan (Alchanon), the 19th and 20th tallest mountain in the Philippines. South of this line of mountains are Mount Chumangil and Mount Patoc, the other volcano of the Central Cordillera Range displaying strong fumarolic activity. Geology.

Geographic entities mentioned:
surface_form: mount patoc
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.146666666667
lon: 120.98
surface_form: patoc
instance_of: Mountain
countries: Philippines
coordinates: lat: 17.146666666667
lon: 120.98
Cathedral Rock. Cathedral Rock is a natural sandstone butte near Sedona, Arizona, and one of the most-photographed sights in Arizona, United States. The rock formation is located in the Coconino National Forest in Yavapai County, about west of Arizona Route 179, and about south of the &quot;Y&quot; intersection of State Routes 179 and 89A in uptown Sedona.

Geographic entities mentioned:
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
Cathedral Rock is a natural sandstone butte near Sedona, Arizona, and one of the most-photographed sights in Arizona, United States. The rock formation is located in the Coconino National Forest in Yavapai County, about west of Arizona Route 179, and about south of the &quot;Y&quot; intersection of State Routes 179 and 89A in uptown Sedona. The summit elevation of Cathedral Rock is.

Geographic entities mentioned:
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
The summit elevation of Cathedral Rock is. The Cathedral Rock trail (USFS Trail #170) is a popular short, steep ascent from the Back O' Beyond trailhead to the saddle points or &quot;gaps&quot; in Cathedral Rock. Geologically, Cathedral Rock is carved from the Permian Schnebly Hill formation, a redbed sandstone formed from coastal sand dunes near the shoreline of the ancient Pedregosa Sea.

Geographic entities mentioned:
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
Geologically, Cathedral Rock is carved from the Permian Schnebly Hill formation, a redbed sandstone formed from coastal sand dunes near the shoreline of the ancient Pedregosa Sea. Ripple marks are prominent along the lower Cathedral Rock trail, and a black basalt dike may be seen in the first saddle.

Geographic entities mentioned:
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
surface_form: cathedral rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.82
lon: -111.793
The couple had two daughters: Harriet Stratemeyer Adams (1892–1982) and Edna C. Squier (1895–1974), both of whom would later take over the future Stratemeyer Syndicate. Stratemeyer enjoyed the outdoors and often took annual summer trips to the Great Lakes, Lake George and Lake Champlain with his family. They traveled as far as the west coast and Yosemite.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Arlberg-Kandahar. 8v6xllt82a9cepp6kd7cfdlfiawdn" xml:space="preserve">The Arlberg-Kandahar race (often abbreviated A-K or AK) is an annual alpine skiing event. The first edition of the race was held in 1928 in St. Anton, in the Arlberg district of Austria. The location originally alternated between St. Anton and Mürren, Switzerland.

Geographic entities mentioned:
surface_form: Arlberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.13
lon: 10.211
The Vevey–Montreux–Chillon–Villeneuve tramway (VMCV) was a metre gauge electric tramway in the Swiss canton of Vaud. It linked the towns of Vevey, Montreux and Villeneuve close to the shoreline of Lake Geneva, and also served the famous Château de Chillon. The line was formed by a merger of the Vevey–Montreux–Chillon tramway (VMC) and the Chillon–Byron–Villeneuve tramway (CBV).

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
History. The Saxon &quot;Ostmark&quot; initially referred to the vast &quot;Marca Geronis&quot; ('Gero's March'), established about 939 under the rule of King Otto I in the settlement area of the Polabian Slavs (Sorbs), beyond the Saxon Eastern border on the Elbe and Saale rivers.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Lyman Glacier (North Cascades). Lyman Glacier is in Wenatchee National Forest in the U.S. state of Washington and is just northeast of Chiwawa Mountain. Between the years 1890 and 2008, Lyman Glacier has retreated and lost 86 percent of its area, a reduction in its surface from.

Geographic entities mentioned:
surface_form: Chiwawa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.163333333333
lon: -120.90722222222
Moel Ysgyfarnogod. is a mountain in Snowdonia, North Wales and is the northernmost of the Rhinogydd. Rhinog Fawr lies directly south. It overlooks Llyn Trawsfynydd, and from the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog. It may be climbed from Trawsfynydd in the east, or from Talsarnau in the west.

Geographic entities mentioned:
surface_form: Rhinog Fawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.841688888889
lon: -3.9968694444444
Moel Ysgyfarnogod. is a mountain in Snowdonia, North Wales and is the northernmost of the Rhinogydd. Rhinog Fawr lies directly south. It overlooks Llyn Trawsfynydd, and from the summit it is possible to see the towns of Porthmadog and Blaenau Ffestiniog. It may be climbed from Trawsfynydd in the east, or from Talsarnau in the west.

Geographic entities mentioned:
surface_form: moel ysgyfarnogod
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.89115
lon: -3.9961694444444
The sediments containing the fossil logs are part of the widespread and colorful Chinle Formation, from which the Painted Desert gets its name. Beginning about 60 million years ago, the Colorado Plateau, of which the park is part, was pushed upward by tectonic forces and exposed to increased erosion.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Lack of plant cover makes the Chinle especially susceptible to weathering. About 60 million years ago, tectonic movements of the Earth's crust began to uplift the Colorado Plateau, of which the Painted Desert is part. Eventually parts of the plateau rose to above sea level. This warping of the Earth's surface led to the gradual and continuing destruction of the plateau by erosion.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
The Climb (1986 film). &quot;The Climb&quot; is a 1986 Canadian-British co-produced adventure drama film, directed by Donald Shebib. A dramatization of mountaineer Hermann Buhl's 1953 attempt to climb Nanga Parbat, the film stars Bruce Greenwood as Buhl alongside James Hurdle, Kenneth Welsh, Ken Pogue, Thomas Hauff, Guy Bannerman, David James Elliott and Tom Butler as members of his expedition.

Geographic entities mentioned:
surface_form: Nanga Parbat
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.239166666667
lon: 74.59
Tom Bähler, a long-time close associate of composer Quincy Jones as well as being associate producer and arranger of &quot;We Are the World&quot;, lives in California's Santa Ynez Valley north of Los Angeles and continues to occasionally produce as well as record.

Geographic entities mentioned:
surface_form: Santa Ynez Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5473
lon: -119.858
A blueberry farm surrounds the lake. Larsen Lake is the headwaters of Kelsey Creek. History. Historically, Phantom Lake drained into Larsen Lake through the marshy, low-lying region between them. This watershed then drained into Kelsey Creek and Lake Washington. In the 1880s, settlers redirected the outflow of Phantom Lake into nearby Lake Sammamish through what is now Weowna Creek.

Geographic entities mentioned:
surface_form: Phantom Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.5933
lon: -122.125
surface_form: larsen lake
instance_of: Lake
countries: United States
coordinates: lat: 47.605094
lon: -122.140349
surface_form: phantom lake
instance_of: Lake
countries: United States
coordinates: lat: 43.025322
lon: -101.510685