Sarmila/GeoWiki-Features huggingface dataset:
A joint Army-Navy unit patrolled the lower east coast of Florida. Other troops patrolled the northern part of the territory to protect against Seminole raids. Colonel Taylor saw the first major action of the campaign. Leaving Fort Gardiner on the upper Kissimmee with 1,000 men on December 19, Taylor headed towards Lake Okeechobee. In the first two days out ninety Seminoles surrendered.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
Crescent Range. The Crescent Range, sometimes referred to as the Randolph Mountains, is located in the White Mountains of New Hampshire in the United States. The highest peak in the range is Black Crescent Mountain, with an elevation of.

Geographic entities mentioned:
surface_form: Black Crescent Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.439227777778
lon: -71.270355555556
The film was shot in Eastmancolor, with sets designed by art directors Isabella and Werner Schlichting. It was shot at three studios in Vienna, the Rosenhugel, Sievering and Schönbrunn Studios. Location shooting took place around the city, and in the Wachau. It was the first Austrian film to be made in Cinemascope. Plot.

Geographic entities mentioned:
surface_form: Wachau
instance_of: Valley
countries: Austria
coordinates: lat: 48.36444
lon: 15.43417
Hallingdal District Court () was a district court in Buskerud county, Norway. The court was based in Nesbyen. The court existed until 2021. It had jurisdiction over the Hallingdal valley which included the municipalities of Flå, Gol, Hemsedal, Hol, Nesbyen, and Ål. Cases from this court could be appealed to Borgarting Court of Appeal. The court was a court of first instance.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
Cases from this court were heard by a combination of professional judges and lay judges. History. The court was created on 9 August 1825 when the old district court covering both Ringerike and Hallingdal was divided into two. On 26 April 2021, Hallingdal District Court was merged with the Drammen District Court and Kongsberg og Eiker District Court to create the new Buskerud District Court.

Geographic entities mentioned:
surface_form: Hallingdal
instance_of: Valley
countries: Norway
coordinates: lat: 60.633333333333
lon: 9.05
Status. Kisangani, in eastern Zaire, is the third-largest city in the country. Since October 1996 and the capture of Bukavu, the rebels, initially Banyamulenge supported by Rwandan soldiers, have been advancing from the African Great Lakes region. Kisangani is the gateway to western Zaire and the capital Kinshasa.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Manor, Scottish Borders. Manor is a parish in Peeblesshire in the Scottish Borders, whose church lies on the west bank of Manor Water 3 miles south-west of Peebles. The parish consists of the valley of Manor Water, a tributary of the River Tweed and extends about 9 miles north to south and about 3 miles wide.

Geographic entities mentioned:
surface_form: Manor Water
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 55.642822
lon: -3.225243
It lies in Southern Iberia on the Costa del Sol (&quot;Coast of the Sun&quot;) of the Mediterranean, primarily in the left bank of the Guadalhorce. The urban core originally developed in the space between the Gibralfaro Hill and the Guadalmedina. Málaga's history spans about 2,800 years, making it one of the oldest continuously inhabited cities in Western Europe.

Geographic entities mentioned:
surface_form: Gibralfaro Hill
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
History. Phoenicians from Tyre founded a colony named &quot;Malake&quot; about 770BC (,). The town controlled access to the Guadalmedina and served as a waypoint on trade routes between Phoenicia and the Strait of Gibraltar. Like other Phoenician colonies, it fell under Carthaginian rule during the 6th or 5th centuryBC.

Geographic entities mentioned:
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
Like other Phoenician colonies, it fell under Carthaginian rule during the 6th or 5th centuryBC. The Phoenician and Later Roman urban core developed around an area running from the Gibralfaro Hill to the mouth of the &quot;Malaca flumen&quot; (Guadalmedina). After the Punic Wars, the Roman Republic took control of the town known to them as &quot;Malaca&quot;.

Geographic entities mentioned:
surface_form: Gibralfaro Hill
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
The highest point in the range (and in the municipality) is the &quot;Pico Reina&quot;, rising up to above sea level. The city centre is located around the mouth of the Guadalmedina and close to the Guadalhorce's mouth (where the airport is located). The Totalán Creek constitutes the eastern boundary of Málaga with the municipality of Rincón de la Victoria.

Geographic entities mentioned:
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
The city centre is located around the mouth of the Guadalmedina and close to the Guadalhorce's mouth (where the airport is located). The Totalán Creek constitutes the eastern boundary of Málaga with the municipality of Rincón de la Victoria. The Gibralfaro is a high foothill from which the and the Alcazaba fortress overlook the city. Climate.

Geographic entities mentioned:
surface_form: Gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
The old historic centre of Málaga reaches the harbour to the south. In the north it is surrounded by mountains, the Montes de Málaga (part of the Baetic Cordillera) lying in the southern base of the Axarquía hills, and two rivers, the Guadalmedina – the historic center is located on its left bank – and the Guadalhorce, which flows west of the city into the Mediterranean, in the Churriana district.

Geographic entities mentioned:
surface_form: Guadalmedina
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.70621
lon: -4.425791
The Roman theatre of Málaga, which dates from the 1st century BC, was rediscovered in 1951. The Moors left posterity the dominating presence of the Castle of Gibralfaro, which is connected to the Alcazaba, the lower fortress and royal residence. Both were built during the Taifa period (11th century) and extended during the Nasrid period (13th and 14th centuries).

Geographic entities mentioned:
surface_form: Castle of Gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
The Málaga harbour is also the second busiest cruise port of the Iberian Peninsula. A popular walk leads up the hill to the Gibralfaro castle (a Parador), offering panoramic views over the city. The castle is next to the Alcazaba, the old Muslim palace, which in turn is next to the inner city of Málaga.

Geographic entities mentioned:
surface_form: Gibralfaro
instance_of: Mountain
countries: Spain
coordinates: lat: 36.72333333
lon: -4.41083333
Brothers Water. Brothers Water is a small lake in the Hartsop valley, in the eastern region of the Lake District in England. Once called Broad Water, it lies at the northern end of Kirkstone Pass, affording views on the descent towards Patterdale. The name was changed in the 19th century after two brothers drowned there.

Geographic entities mentioned:
surface_form: broad water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.60253
lon: -4.09606
Brothers Water. Brothers Water is a small lake in the Hartsop valley, in the eastern region of the Lake District in England. Once called Broad Water, it lies at the northern end of Kirkstone Pass, affording views on the descent towards Patterdale. The name was changed in the 19th century after two brothers drowned there.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
Once called Broad Water, it lies at the northern end of Kirkstone Pass, affording views on the descent towards Patterdale. The name was changed in the 19th century after two brothers drowned there. The lake is not among the most popular in the national park, being shallow and full of reeds. Water lilies bloom in July, providing colour.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
On the western side of Brothers Water is Hartsop Hall. The 16th-century building passed to Sir John Lowther in the 17th century and is now owned by the National Trust. The village of Hartsop lies near the northeast corner of the lake. Brothers Water may be classified in either of two ways: as one of the Lake District's smallest lakes or one of its largest tarns.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The 16th-century building passed to Sir John Lowther in the 17th century and is now owned by the National Trust. The village of Hartsop lies near the northeast corner of the lake. Brothers Water may be classified in either of two ways: as one of the Lake District's smallest lakes or one of its largest tarns. The lake is home to a trout population and harbours a rare species of fish, the schelly.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Brothers Water. Brothers Water is a small lake in the Hartsop valley, in the eastern region of the Lake District in England. Once called Broad Water, it lies at the northern end of Kirkstone Pass, affording views on the descent towards Patterdale. The name was changed in the 19th century after two brothers drowned there.

Geographic entities mentioned:
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
Water lilies bloom in July, providing colour. To the north-east of Brothers Water is the village of Hartsop, which has several 17th-century stone farm buildings and cottages. Some of the buildings still contain spinning-rooms where villagers would have made their own clothing, selling any surplus in the local market towns.

Geographic entities mentioned:
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
A walk through woodland skirts the western shore. From its northern end the walk leads to Patterdale. Southward it heads over Kirkstone Pass to Ambleside. On the western side of Brothers Water is Hartsop Hall. The 16th-century building passed to Sir John Lowther in the 17th century and is now owned by the National Trust. The village of Hartsop lies near the northeast corner of the lake.

Geographic entities mentioned:
surface_form: brothers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.505555555556
lon: -2.925
Sara Sara (Aymara &quot;sara&quot; an ounce, Quechua &quot;sara&quot; maize, the reduplication indicates that there is a group or a complex of something) is a mountain in the Wansu mountain range in the Andes of Peru. It is situated in the Apurímac Region, Antabamba Province, in the districts of Antabamba and Juan Espinoza Medrano. Sara Sara lies south of Quri Waraqa and Huch'uy Sara Sara.

Geographic entities mentioned:
surface_form: Quri Waraqa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6014
lon: -72.7861
surface_form: Huch'uy Sara Sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6158
lon: -72.7947
surface_form: quri waraqa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6014
lon: -72.7861
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: quri
instance_of: Mountain
countries: Peru
coordinates: lat: -13.6403
lon: -71.6556
surface_form: quri
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8358
lon: -71.5186
surface_form: huch'uy sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6158
lon: -72.7947
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6381
lon: -72.7881
Sara Sara (Apurímac). Sara Sara (Aymara &quot;sara&quot; an ounce, Quechua &quot;sara&quot; maize, the reduplication indicates that there is a group or a complex of something) is a mountain in the Wansu mountain range in the Andes of Peru. It is situated in the Apurímac Region, Antabamba Province, in the districts of Antabamba and Juan Espinoza Medrano.

Geographic entities mentioned:
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: sara sara (apurímac)
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6381
lon: -72.7881
Sara Sara (Apurímac). Sara Sara (Aymara &quot;sara&quot; an ounce, Quechua &quot;sara&quot; maize, the reduplication indicates that there is a group or a complex of something) is a mountain in the Wansu mountain range in the Andes of Peru. It is situated in the Apurímac Region, Antabamba Province, in the districts of Antabamba and Juan Espinoza Medrano.

Geographic entities mentioned:
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -15.323527777778
lon: -73.449361111111
surface_form: sara sara
instance_of: Mountain
countries: Peru
coordinates: lat: -14.6381
lon: -72.7881
Most of the Serbian queen consorts were Byzantine women (such as Eudokia Angelina, Simonida, Maria Palaiologina, Irene Kantakouzene, Helena Palaiologina). Manuel I of Constantinople recognized Sava as the first Archbishop of the Serbs. Hilandar on Mount Athos became one of the most important cultural and religious centres of the Serbian people.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Cultural relations. Hilandar, Serbian Orthodox monastery on Mount Athos, holds immense significance for Serbian culture. It was founded in 1198 and is considered a sacred site for Serbian Orthodoxy. Saint Sava’s campaign for the autocephaly of the Serbian Orthodox Church in 1219 is closely tied to Hilandar, where he was tonsured as a monk.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
&quot;For details of the San Mateo coast, see List of watercourses in the San Francisco Bay Area.&quot;
Carrizo Plain. The Carrizo Plain is a large enclosed valley near the Central Coast which drains into Soda Lake. Death Valley. Streams terminating in the Badwater Basin in Death Valley National Park.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
It is from this period that the name 'Howardsville' was first used. Within ten years of the canal coming to the town, local investors set up the Howardsville and Rockfish Gap Turnpike Company and during the 1840s cut a road from the river over the Blue Ridge Mountains and across the Shenandoah Valley south of Staunton all the way to the Appalachians. However, the turnpike was never successful.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
2006 Mumbai sweet seawater incident. The 2006 Mumbai &quot;sweet&quot; seawater incident witnessed hundreds of residents of Mumbai drinking the seawater at Mahim Creek, amid claims that the foul-smelling water had suddenly turned sweet by a miracle and could now cure illnesses. Authorities in Mumbai warned against drinking the polluted water because of health risks.

Geographic entities mentioned:
surface_form: Mahim Creek
instance_of: Watercourse
countries: India
coordinates: lat: 19.052601
lon: 72.8393824
Hoàn Kiếm district. Hoàn Kiếm () is one of the four original urban districts (quận) of Hanoi, the capital city of Vietnam. It is named after the scenic Hoàn Kiếm Lake. The lake is in the heart of the district and serves as the focal point of the city's public life. The majority of tourist attractions in Hanoi are also located in the district.

Geographic entities mentioned:
surface_form: Hoàn Kiếm Lake
instance_of: Lake
countries: Vietnam
coordinates: lat: 21.028888888889
lon: 105.8525
At a Christmas party, a BBC executive expressed a wish for the ratings of a third series &quot;to go like Everest&quot;, indicating a steep slope with his hands. Bathurst replied, &quot;But, Everest goes down the other side ...&quot; The show was not recommissioned.

Geographic entities mentioned:
surface_form: Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
Ear Mountain. Ear Mountain (Inupiaq: &quot;Iŋiġagik&quot;) is an isolated mountain located on the Seward Peninsula in the U.S. state of Alaska.

Geographic entities mentioned:
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.823611111111
lon: -112.69027777778
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.9219
lon: -166.246
state of Alaska. The mountain, with an elevation of (GeoNames gives it elevation as), has a belt of Cretaceous tin &quot;granites.&quot; Though the mountain is located in an area long known for its tin deposits, it was only in 1953 and 1954 during a survey by the US Bureau of Mines that tin deposits were confirmed to be on Ear Mountain. Geography.

Geographic entities mentioned:
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.823611111111
lon: -112.69027777778
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.9219
lon: -166.246
Geography. Located on the Seward Peninsula, the Ear Mountain is north of Teller, and southwest of Shishmaref Inlet. It is an isolated mountain formation surrounded by coastal flats and valleys of streams with elevation ranging from. The mountain is free-standing, with a summit altitude of above sea level. Its northeast slopes are moderate and it forms three peaks of, and.

Geographic entities mentioned:
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.823611111111
lon: -112.69027777778
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.9219
lon: -166.246
The mountain experiences more rain and fog than at the Shishmaref Inlet. Geology. The sedimentary rocks surrounding Ear Mountain consist mainly of quartzites and dark slates, which resemble the slates near York and have been correlated with them. The core of the mountain is a granite boss or stock intruded in these slates.

Geographic entities mentioned:
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.823611111111
lon: -112.69027777778
surface_form: ear mountain
instance_of: Mountain
countries: United States
coordinates: lat: 65.9219
lon: -166.246
Skoddemedet Peak. Skoddemedet Peak () is a rock peak about 5 nautical miles (9 km) southwest of Hogfonna Mountain, in the Borg Massif of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Skoddemedet (the fog landmark).

Geographic entities mentioned:
surface_form: skoddemedet peak
instance_of: Mountain
coordinates: lat: -72.83333333
lon: -3.85
Skoddemedet Peak. Skoddemedet Peak () is a rock peak about 5 nautical miles (9 km) southwest of Hogfonna Mountain, in the Borg Massif of Queen Maud Land. Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and named Skoddemedet (the fog landmark).

Geographic entities mentioned:
surface_form: skoddemedet
instance_of: Mountain
coordinates: lat: -72.83333333
lon: -3.85
Ricker, a geologist with the party. Location. The Ricker Hills are just west of the Hollingsworth Glacier, which flows along their east side, and south of the David Glacier. The Antarctic Plateau is to their west and south, with various scattered peaks or nunataks emerging from the ice. Features. Features of the Ricker Hills include the Morris Basin in the north and Benson Knob in the south.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Dietlikon railway station. Dietlikon railway station () is a railway station in the Swiss canton of Zürich and municipality of Dietlikon (Glatt Valley). The station is located on the Zürich to Winterthur railway line. It lies within fare zone 121 of the Zürcher Verkehrsverbund (ZVV).

Geographic entities mentioned:
surface_form: Glatt Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.416666666667
lon: 8.5666666666667
To the south of the station, the three tracks diverge into two twin-track railway lines, one to Zürich via Wallisellen and the other to Zürich via. To the north of the station the three tracks merge into the twin-track line to. Dietlikon station is not to be confused with Dietikon railway station located in Dietikon in the Limmat Valley (canton of Zürich). Service.

Geographic entities mentioned:
surface_form: Limmat Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.5
lon: 8.25
SR 224 heads north and crosses the Carter Valley, then crosses Long Ridge before crossing the North Fork Holston River. The state highway veers west and curves back east around Pine Ridge before reaching its northern terminus at US 58 and US 421 (Hilton Road) a short distance to the east of Moccasin Gap on the eastern edge of the town of Weber City, where US 58 and US 421 intersect US 23.

Geographic entities mentioned:
surface_form: Moccasin Gap
instance_of: Landform
countries: United States
coordinates: lat: 36.6348
lon: -82.5551
Reisalpe. The Reisalpe (1,399 m) is the highest mountain in the Gutenstein Alps and lies between Lilienfeld, Hohenberg and Kleinzell in Lower Austria. It is a popular destination, both for hikers in summer and also for ski mountaineering and snowshoe walks in winter, and is classed as relatively safe from avalanches.

Geographic entities mentioned:
surface_form: reisalpe
instance_of: Mountain
countries: Austria
coordinates: lat: 47.956666666667
lon: 15.663611111111
It is a popular destination, both for hikers in summer and also for ski mountaineering and snowshoe walks in winter, and is classed as relatively safe from avalanches. Near the summit stands a Madonna, recently joined by a summit cross, as well as the Reisalpe refuge hut (&quot;Schutzhaus&quot;) opened on 9 October 1898.

Geographic entities mentioned:
surface_form: reisalpe
instance_of: Mountain
countries: Austria
coordinates: lat: 47.956666666667
lon: 15.663611111111
A small Austrian Armed Forces hut is also located in the vicinity of the summit. Schutzhaus. In October 1898, the Reisalpe Schutzhaus was opened. It had taken three years to build, and seven hundred people attended the elaborate opening ceremony. The Reisalpe poem was read out loud:<poem>
&quot;Great calm and deep peace is only with you,
when you are on this land. What is the magic of the forest?

Geographic entities mentioned:
surface_form: reisalpe
instance_of: Mountain
countries: Austria
coordinates: lat: 47.956666666667
lon: 15.663611111111
In addition to 1,100 destroyed houses, many temples were razed. An additional 1,000 homes were also damaged. The slope of Mount Ibuki collapsed which was accompanied by a &quot;thunderous roar.&quot; Fifty homes on Lake Biwa were totally razed and 20 others were destroyed. A toppling cliffside at a Gifu marble quarry left one dead and five wounded.

Geographic entities mentioned:
surface_form: Mount Ibuki
instance_of: Mountain
countries: Japan
coordinates: lat: 35.417777777778
lon: 136.40611111111
Lake Muir Nature Reserve. Lake Muir Nature Reserve is a protected area in Western Australia. It encompasses Lake Muir and several smaller lakes and wetlands. It is an important refuge for water birds, and home to several rare plants and plant communities. Geography. The reserve is located in the South West region, in the shires of Manjimup and Cranbook, 55 km south east of Manjimup.

Geographic entities mentioned:
surface_form: Lake Muir
instance_of: Lake
countries: Australia
coordinates: lat: -34.446944444444
lon: 116.74833333333
Geographic distribution. Yazidis are concentrated primarily in agricultural areas around Mount Aragats, northwest of Yerevan. They live in 19 villages in the Aragatsotn Province, two villages in the Armavir Province, and one village in the Ararat Province. Armenian Catholics live mainly in the northern region, in seven villages in the Shirak Province and six villages in the Lori Province.

Geographic entities mentioned:
surface_form: Mount Aragats
instance_of: Mountain
countries: Armenia
coordinates: lat: 40.523055555556
lon: 44.195277777778
The 2011 Armenian census counted 2,874 Molokans and the 2022 census counted 2,000 Molokans. In 1802, Alexander I ordered that adherents of religious sects should be relocated to southern areas of the Russian Empire; Armenian regions such as Lori, Lake Sevan, Dilijan, and Zangezur were chosen for new Russian settlements.

Geographic entities mentioned:
surface_form: Lake Sevan
instance_of: Lake
countries: Armenia
coordinates: lat: 40.310555555556
lon: 45.349166666667
It then goes northwest as it enters a large wooded area before coming to an intersection with SR 285, where it turns northeast and crosses into Cumberland County. It then becomes curvy as it passes through the rolling hills and farmland of the Cumberland Plateau before passing just north of Lake Tansi Village and having an intersection with SR 282, northeast of Meadow Park Lake.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Description. Sawtooth Peak is located seven miles west-southwest of Joseph, Oregon, in the Wallowa Mountains. It is set within the Eagle Cap Wilderness on land managed by Wallowa–Whitman National Forest. The peak is situated one mile north of Legore Lake and line parent Twin Peaks. Precipitation runoff from the mountain drains into tributaries of the Lostine River and Wallowa River.

Geographic entities mentioned:
surface_form: Legore Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3096
lon: -117.3466
Manulea cereola. &quot;Manulea&quot; (&quot;Setema&quot;) &quot;cereola&quot; is a moth of the family Erebidae. It is found in Fennoscandia, the Baltic States, European Russia as well as the Alps and Urals. The species was first described by Jacob Hübner in 1803. The wingspan is 18–32 mm. The larvae feed on various lichen species from the genus &quot;Parmelia&quot;.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Then it passes through Winona where it has a concurrency with Route 19. US 60 passes through Chicopee, Van Buren and Ellsinore. Next, US 60 has a concurrency with US 67 until it enters Poplar Bluff as it leaves the Ozark Plateau. In Poplar Bluff, US 60 separates from US 67 at a cloverleaf interchange. After leaving Poplar Bluff, US 60 intersects Route 51 north of Fisk.

Geographic entities mentioned:
surface_form: Ozark Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Mount Brett. Mount Brett is a summit located in the Massive Range of Alberta, Canada It is situated in Banff National Park, west of Banff townsite, in the Canadian Rockies. Its nearest higher peak is Mount Ball, to the west. History. Mount Brett was named in 1916 for Robert Brett (1851–1929). Doctor Brett was a surgeon who first came to Banff in 1885.

Geographic entities mentioned:
surface_form: Mount Ball
instance_of: Mountain
countries: Canada
coordinates: lat: 51.156388888889
lon: -116.00638888889
Mount Brett. Mount Brett is a summit located in the Massive Range of Alberta, Canada It is situated in Banff National Park, west of Banff townsite, in the Canadian Rockies. Its nearest higher peak is Mount Ball, to the west. History. Mount Brett was named in 1916 for Robert Brett (1851–1929). Doctor Brett was a surgeon who first came to Banff in 1885.

Geographic entities mentioned:
surface_form: mount brett
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1614
lon: -115.819
Its nearest higher peak is Mount Ball, to the west. History. Mount Brett was named in 1916 for Robert Brett (1851–1929). Doctor Brett was a surgeon who first came to Banff in 1885. He later served as the second Lieutenant Governor of Alberta starting in 1915. The first ascent of Mount Brett was made in 1916 by C.F. Hogeboom, A.H. Bent, James Outram, E.G. Ritchie, and K.D. McClelland.

Geographic entities mentioned:
surface_form: mount brett
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1614
lon: -115.819
McClelland. The mountain's name became official on November 2, 1956 when approved by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Brett is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount brett
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1614
lon: -115.819
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Brett is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C.

Geographic entities mentioned:
surface_form: mount brett
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1614
lon: -115.819
Climate. Based on the Köppen climate classification, Mount Brett is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 C with wind chill factors below −30 C. Precipitation runoff from Mount Brett drains into tributaries of the Bow River, which is a tributary of the Saskatchewan River.

Geographic entities mentioned:
surface_form: mount brett
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1614
lon: -115.819
The first ascent of Mount Brett was made in 1916 by C.F. Hogeboom, A.H. Bent, James Outram, E.G. Ritchie, and K.D. McClelland. The mountain's name became official on November 2, 1956 when approved by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Brett is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Pyrénées-Orientales department is located in the extreme south of France, eastern section of the Pyrenees mountain range and the. The mountainous region of the county consists of the Albera massif to the southeast, the Corbières massif to the north, and the historic regions of Vallespir, Conflent, Cerdagne, and Capcir, which make up almost 50% of the department's total area.

Geographic entities mentioned:
surface_form: Capcir
instance_of: Valley
countries: France
coordinates: lat: 42.6
lon: 2.1166666666667
Elpoca Mountain. Elpoca Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Evan-Thomas, to the north. Elpoca Mountain is situated 4.0 kilometres south of Mount Jerram, and 2.0 km east of Gap Mountain, and all are within Peter Lougheed Provincial Park.

Geographic entities mentioned:
surface_form: Mount Evan-Thomas
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7659
lon: -115.0953
The nearest higher peak is Mount Evan-Thomas, to the north. Elpoca Mountain is situated 4.0 kilometres south of Mount Jerram, and 2.0 km east of Gap Mountain, and all are within Peter Lougheed Provincial Park. Precipitation runoff from the west side of the mountain drains into tributaries of the Kananaskis River, whereas the east side drains into Elbow River. History.

Geographic entities mentioned:
surface_form: Mount Jerram
instance_of: Mountain
countries: Canada
coordinates: lat: 50.7001
lon: -115.0503
surface_form: gap mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.65611111111111
lon: -115.05416666666666
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elpoca mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
Elpoca Mountain. Elpoca Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Evan-Thomas, to the north. Elpoca Mountain is situated 4.0 kilometres south of Mount Jerram, and 2.0 km east of Gap Mountain, and all are within Peter Lougheed Provincial Park.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elpoca mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
Elpoca Mountain. Elpoca Mountain is a mountain summit located at the southern end of the Opal Range in the Canadian Rockies of Alberta, Canada. The nearest higher peak is Mount Evan-Thomas, to the north. Elpoca Mountain is situated 4.0 kilometres south of Mount Jerram, and 2.0 km east of Gap Mountain, and all are within Peter Lougheed Provincial Park.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elpoca mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
The nearest higher peak is Mount Evan-Thomas, to the north. Elpoca Mountain is situated 4.0 kilometres south of Mount Jerram, and 2.0 km east of Gap Mountain, and all are within Peter Lougheed Provincial Park. Precipitation runoff from the west side of the mountain drains into tributaries of the Kananaskis River, whereas the east side drains into Elbow River. History.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The steeply tilted strata are virtually the same in each peak of the Opal Range, with softer layers sandwiched between harder layers. Climate. Based on the Köppen climate classification, Elpoca Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elpoca mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
Climate. Based on the Köppen climate classification, Elpoca Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. June through September offer the most favorable weather to climb Elpoca Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: elpoca mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.66676
lon: -115.0187
After the Kingdom of Italy entered the First World War on 24 May 1915, he fought with the 4th Bersaglieri Regiment on the Karst Plateau (where he became commander of the 14th Company, XXXVII Bersaglieri Battalion) and later, after promotion to captain, in the 14th Bersaglieri Regiment, being wounded on Monte Zebio in June 1916, during the battle of Asiago.

Geographic entities mentioned:
surface_form: Monte Zebio
instance_of: Mountain
countries: Italy
coordinates: lat: 45.92611111
lon: 11.50861111
The estimated chance that a given person would get hit and injured during their lifetime is around 1 in a trillion. On January 24, 1978, the Soviet Kosmos 954 () reentered and crashed near Great Slave Lake in the Northwest Territories of Canada. The satellite was nuclear-powered and left radioactive debris near its impact site.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Currently, the only producing area in Canada is northern Saskatchewan, although other areas have had active mines in the past. Discovery of uranium. Canada's first recorded discovery of uranium was likely in 1847, when pitchblende, a major uranium-bearing mineral, was found at Theano Point, Lake Superior by B. A. Stanard, and described by geologist J. L. LeConte in the American Journal of Science.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
A 45 metre shaft was sunk and 150 metres of drifting was done. The mine was not profitable and was abandoned before going into full production. Canada's first commercially important uranium discovery was in 1930, when prospector Gilbert LaBine discovered pitchblende on the shores of the Great Bear Lake in the Northwest Territories.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
The headquarters was founded by Gotthilf Hempel. Nowadays, the AWI has several buildings within the city of Bremerhaven. Potsdam. The Forschungsstelle Potsdam is situated on the Telegrafenberg next to Potsdam. It belongs to AWI since 1992. The research focuses on the atmospheric physics and atmospheric chemistry of the atmosphere on the one hand and periglacial research on the other hand. Sylt.

Geographic entities mentioned:
surface_form: Telegrafenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.3814
lon: 13.0644
South Branch Machias River. The South Branch Machias River is a river in Aroostook County, Maine. From the outflow of Center Pond () in Maine Township 10, Range 8, WELS, the river runs east to its confluence with the Machias River in T.10 R.7 WELS. Via the Machias and Aroostook rivers, it is part of the Saint John River watershed.

Geographic entities mentioned:
surface_form: Aroostook
instance_of: Watercourse
countries: United States
Canada
coordinates: lat: 46.345043
lon: -68.802268
Antarctic Plateau. The Antarctic Plateau, Polar Plateau or King Haakon VII Plateau is a large area of East Antarctica that extends over a diameter of about, and includes the region of the geographic South Pole and the Amundsen–Scott South Pole Station. This huge continental plateau is at an average elevation of about. Exploration.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
surface_form: king haakon vii plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
surface_form: polar plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Shackleton named this plateau the King Edward VII Plateau in honour of the king of the United Kingdom. In December 1911, while returning from the first journey to the South Pole, the Norwegian explorer Roald Amundsen decided to name this plateau the King Haakon VII Plateau in honour of the newly elected king of Norway.

Geographic entities mentioned:
surface_form: amundsen
instance_of: Mountain
coordinates: lat: -67.233333333333
lon: 100.75
surface_form: king haakon vii plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Cryomorphaceae and Flavobacteriaceae); and Cyanobacteria. According to research, polar microorganisms should be considered as not only deposited airborne particles, but also as active components of the snowpack ecology of the Antarctic Plateau. No penguins live on the Antarctic Plateau, and few birds routinely fly over it, except mostly Antarctic petrels, snow petrels and south polar skuas.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Exploration. This plateau was first sighted in 1903 during the &quot; Discovery&quot; Expedition to the Antarctic, which was led by Robert Falcon Scott. Ernest Shackleton became the first to cross parts of this plateau in 1909 during his &quot; Nimrod&quot; Expedition, which turned back in bad weather when it had reached a point from the South Pole.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Exploration. This plateau was first sighted in 1903 during the &quot; Discovery&quot; Expedition to the Antarctic, which was led by Robert Falcon Scott. Ernest Shackleton became the first to cross parts of this plateau in 1909 during his &quot; Nimrod&quot; Expedition, which turned back in bad weather when it had reached a point from the South Pole.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Antarctic Plateau. The Antarctic Plateau, Polar Plateau or King Haakon VII Plateau is a large area of East Antarctica that extends over a diameter of about, and includes the region of the geographic South Pole and the Amundsen–Scott South Pole Station. This huge continental plateau is at an average elevation of about. Exploration.

Geographic entities mentioned:
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Byrd of Virginia, an officer in the U.S. Navy. The other two members of its crew were the co-pilot and the photographer. Climate. The high elevations of the Antarctic Plateau, combined with its high latitudes and its extremely long, sunless winters, mean that the temperatures here are the lowest in the world in most years, falling as low as. Fauna.

Geographic entities mentioned:
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Fauna. The nearly continuous frigid winds that blow across the Antarctic Plateau, especially in the austral winter, make the environment inhospitable to life. Microbial abundance is low (<103 cells/ml of snowmelt). The microbial community is mainly composed of members of the Alphaproteobacteria class (e.g.

Geographic entities mentioned:
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Cryomorphaceae and Flavobacteriaceae); and Cyanobacteria. According to research, polar microorganisms should be considered as not only deposited airborne particles, but also as active components of the snowpack ecology of the Antarctic Plateau. No penguins live on the Antarctic Plateau, and few birds routinely fly over it, except mostly Antarctic petrels, snow petrels and south polar skuas.

Geographic entities mentioned:
surface_form: antarctic plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Ernest Shackleton became the first to cross parts of this plateau in 1909 during his &quot; Nimrod&quot; Expedition, which turned back in bad weather when it had reached a point from the South Pole. Shackleton named this plateau the King Edward VII Plateau in honour of the king of the United Kingdom.

Geographic entities mentioned:
surface_form: king edward vii plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
Earthfasts (TV series). &quot;Earthfasts&quot; is a BBC children's drama series based upon the 1966 book of the same title by William Mayne. It was filmed on location in Richmond and Wensleydale, North Yorkshire, and was aired in 1994. Plot summary. Schoolboys Keith and David (Chris Downs & Paul Nicholls) hear drumming under the hill on the moor near their homes, and set out to investigate.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
In addition, pilgrimages which have gradually lost their former religious zeal and taken on a more secular slant are sometimes held to their summits. Some renowned mountains are Aiako Harria, Hernio, Txindoki, Aizkorri and Izarraitz, amongst others. The Aralar Natural Park is a conservation area on the border of Gipuzkoa and Navarre in the Aralar Range.

Geographic entities mentioned:
surface_form: Hernio
instance_of: Mountain
countries: Spain
coordinates: lat: 43.171386111111
lon: -2.1515805555556
surface_form: Txindoki
instance_of: Mountain
countries: Spain
coordinates: lat: 43.023888888889
lon: -2.0869444444444
surface_form: Aizkorri
instance_of: Mountain
countries: Spain
coordinates: lat: 42.9513544
lon: -2.3253425
Currently, the main road cutting through Gipuzkoa largely follows that layout, i.e. the N-1 E-5 from Irun to Donostia and on to Altsasu all along the Oria River for the most part (gateway to Navarre through the pass of Etxegarate). Also, the major Irun-Madrid railway runs close to the river up to its very origin on the slopes of Aizkorri at train stop Otzaurte in Zegama.

Geographic entities mentioned:
surface_form: Aizkorri
instance_of: Mountain
countries: Spain
coordinates: lat: 42.9513544
lon: -2.3253425
Battle of the Kodori Valley. The Battle of the Kodori Valley was a military operation during the Russo-Georgian War in the Upper Kodori Valley of Abkhazia, a breakaway region of Georgia. It was the only part of Abkhazia under Georgian control before this military conflict.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
It was the only part of Abkhazia under Georgian control before this military conflict. On 9 August 2008, the Abkhaz military, with support by Russian forces, launched an operation to remove the remaining Georgian troops from the disputed gorge. After three days, the Georgian military left the Upper Kodori Valley. Abkhaz and Russian army mobilization.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8
Fighting. On the morning of 9 August 2008, the United Nations Observer Mission in Georgia (UNOMIG) was asked by the Abkhaz authorities to remove its monitors from the Upper Kodori Valley and all UNOMIG personnel left the valley. Abkhaz president Sergei Bagapsh ordered to expel the Georgian military from the Upper Kodori Valley.

Geographic entities mentioned:
surface_form: Kodori Valley
instance_of: Valley
countries: Georgia
coordinates: lat: 43.1
lon: 41.8