Sarmila/GeoWiki-Features huggingface dataset:
Saint-Michel-de-Vax. Saint-Michel-de-Vax is a rural commune and hamlet in the Tarn department in southern France. The hamlet is located on a largely wooded Causse just east of the road between the small towns of Saint-Antonin-Noble-Val and Cordes. The hamlet has no local amenities and consists of about 30 houses, a church and a partially ruined chateau.

Geographic entities mentioned:
surface_form: Causse
instance_of: Plateau
countries: France
coordinates: lat: 44.15
lon: 3.25
History. The initial Duke of Edinburgh Award was founded in the United Kingdom in 1956 by HRH, the Duke of Edinburgh, Prince Philip, alongside Lord Hunt, leader of the first successful ascent of Mount Everest and Kurt Hahn, a German educationalist. They were also in close association with Edmund Hillary who was also on the first ascent of Everest.

Geographic entities mentioned:
surface_form: Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
It is geographically the largest municipality in Tokyo. Mount Kumotori, Tokyo's highest peak at 2017 m, divides Okutama from the Okuchichibu region of the neighboring Saitama and Yamanashi Prefectures. Tokyo's northernmost and westernmost points lie in Okutama, as does Lake Okutama, an important source of water for Tokyo, situated above the Ogōchi Dam in the town. Surrounding municipalities.

Geographic entities mentioned:
surface_form: Mount Kumotori
instance_of: Mountain
countries: Japan
coordinates: lat: 35.855277777778
lon: 138.94361111111
It is situated within Olympic National Park, immediately south and 1,400 feet above the shore of Upper Lena Lake. Mount Lena lies across the lake to the north, Mount Stone is 2.8 miles to the west-southwest, and The Brothers approximately four miles to the northeast. Precipitation runoff from the mountain drains south to the Hamma Hamma River via Boulder, Delta, and Lena Creeks.

Geographic entities mentioned:
surface_form: Mount Stone
instance_of: Mountain
countries: United States
coordinates: lat: 47.6064
lon: -123.267
surface_form: the brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
surface_form: brothers
instance_of: Mountain
countries: United States
coordinates: lat: 47.6537193
lon: -123.140575
surface_form: mount lena
instance_of: Mountain
countries: United States
coordinates: lat: 47.63983
lon: -123.21519
surface_form: mount stone
instance_of: Mountain
countries: United States
coordinates: lat: 47.63926
lon: -123.33573
Mount Bretherton. Mount Bretherton is a mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park, immediately south and 1,400 feet above the shore of Upper Lena Lake. Mount Lena lies across the lake to the north, Mount Stone is 2.8 miles to the west-southwest, and The Brothers approximately four miles to the northeast.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount bretherton
instance_of: Mountain
countries: United States
coordinates: lat: 47.61954
lon: -123.21044
Bretherton was one of three members of the O'Neil expedition who reportedly made the first ascent of Mount Olympus on September 22, although it is now believed they probably climbed a subsidiary peak named &quot;Athena&quot;. Climate. Based on the Köppen climate classification, Mount Bretherton is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
Mount Bretherton. Mount Bretherton is a mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park, immediately south and 1,400 feet above the shore of Upper Lena Lake. Mount Lena lies across the lake to the north, Mount Stone is 2.8 miles to the west-southwest, and The Brothers approximately four miles to the northeast.

Geographic entities mentioned:
surface_form: mount bretherton
instance_of: Mountain
countries: United States
coordinates: lat: 47.61954
lon: -123.21044
Topographic relief is significant as it rises over above the river in two miles. The non-technical ascent of Mount Bretherton involves hiking eight miles (one-way) and 5,300 feet elevation gain via the Upper Lena Lake Trail and cross-country above the lake, with most favorable conditions from July through September.

Geographic entities mentioned:
surface_form: mount bretherton
instance_of: Mountain
countries: United States
coordinates: lat: 47.61954
lon: -123.21044
surface_form: lena lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4047
lon: -113.338
Climate. Based on the Köppen climate classification, Mount Bretherton is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains. As fronts approach, they are forced upward by the peaks (orographic lift), causing them to drop their moisture in the form of rain or snow.

Geographic entities mentioned:
surface_form: mount bretherton
instance_of: Mountain
countries: United States
coordinates: lat: 47.61954
lon: -123.21044
Mount Bretherton. Mount Bretherton is a mountain summit located in the Olympic Mountains, in Jefferson County of Washington state. It is situated within Olympic National Park, immediately south and 1,400 feet above the shore of Upper Lena Lake. Mount Lena lies across the lake to the north, Mount Stone is 2.8 miles to the west-southwest, and The Brothers approximately four miles to the northeast.

Geographic entities mentioned:
surface_form: lena lake
instance_of: Lake
countries: United States
coordinates: lat: 48.4047
lon: -113.338
Great Plains toad. The Great Plains toad (&quot;Anaxyrus cognatus&quot;) is a relatively large species of true toad native to central North America. Distribution. The amphibian is native throughout the Canadian Prairies (northern Great Plains) in southern Alberta, Manitoba, and Saskatchewan; and into northern Mexico in the Sonoran Desert and Mexican Plateau. Description.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Nyassachromis prostoma. &quot;Nyassachromis prostoma&quot; is a species of fish in the family Cichlidae. It is endemic to Lake Malawi and found in Malawi and Tanzania.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
This park has a fishing pier, a walking trail around a pond, a playground and picnic facilities. This Lake is part of the south part of the Winter Haven Chain of Lakes system. A canal on the southwest side connects Lake Hartridge to Lake Idylwild. Another canal on the northeast side connects the lake to Lake Conine. This lake has no public swimming areas.

Geographic entities mentioned:
surface_form: Lake Idylwild
instance_of: Lake
countries: United States
coordinates: lat: 28.0503
lon: -81.7567
surface_form: lake hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
This Lake is part of the south part of the Winter Haven Chain of Lakes system. A canal on the southwest side connects Lake Hartridge to Lake Idylwild. Another canal on the northeast side connects the lake to Lake Conine. This lake has no public swimming areas. Nothing is reported on the species of fishes in this lake.

Geographic entities mentioned:
surface_form: Lake Conine
instance_of: Lake
countries: United States
coordinates: lat: 28.06
lon: -81.7251
Lake Hartridge. Lake Hartridge, with somewhat of a figure eight shape, has a surface area of. This lake is on the north side of Winter Haven in Polk County, Florida. Most of the lake's west shore is bordered by residential areas. The northwest shore is bordered by woods. The north shore is bordered woods and clearings. The northeast is bordered by more clearings.

Geographic entities mentioned:
surface_form: lake hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
At the very southeast corner is Aldora Park, a small public park. The south shore is bordered by a large church. On the southwest shore is Lake Hartridge Nature Park, a public park. Lake Hartridge has public access at both Lake Hartridge Nature Park and Aldora Park. The Nature Park has a public boat ramp just off Beach Parkway.

Geographic entities mentioned:
surface_form: lake hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
The south shore is bordered by a large church. On the southwest shore is Lake Hartridge Nature Park, a public park. Lake Hartridge has public access at both Lake Hartridge Nature Park and Aldora Park. The Nature Park has a public boat ramp just off Beach Parkway. This park has a fishing pier, a walking trail around a pond, a playground and picnic facilities.

Geographic entities mentioned:
surface_form: lake hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
surface_form: lake hartridge
instance_of: Lake
countries: United States
coordinates: lat: 28.0567
lon: -81.7429
The Nature Park has a public boat ramp just off Beach Parkway. This park has a fishing pier, a walking trail around a pond, a playground and picnic facilities. This Lake is part of the south part of the Winter Haven Chain of Lakes system. A canal on the southwest side connects Lake Hartridge to Lake Idylwild. Another canal on the northeast side connects the lake to Lake Conine.

Geographic entities mentioned:
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Harding Lake. Harding Lake is a lake in the Fairbanks North Star Borough in Interior Alaska. It is named for President Warren G. Harding, who visited Alaska just before he died. Prior to that it was known as Salchaket Lake Access to the lake is via the Richardson Highway
Fish species.

Geographic entities mentioned:
surface_form: harding lake
instance_of: Lake
countries: United States
coordinates: lat: 64.42262
lon: -146.85454
Recreation Area. The lake is home to the Harding Lake State Recreation Area a park which features a large campground, boat launch, and facilities for sports and outdoor games. This is one of the oldest units in the Alaska State Park system, having been founded in 1967, before the formal state park network was even in place.

Geographic entities mentioned:
surface_form: harding lake
instance_of: Lake
countries: United States
coordinates: lat: 64.42262
lon: -146.85454
Røwde was a skilled advertiser with a sense for performing media stunts. In the 1930s he displayed a giant tire at a truckstop between Gjersjøen and Mosseveien in Ås Municipality. He instituted &quot;the world's largest car race&quot; from Oslo to Askim in 1939 and Rally Viking in the 1950s.

Geographic entities mentioned:
surface_form: Gjersjøen
instance_of: Lake
countries: Norway
coordinates: lat: 59.783333333333
lon: 10.783333333333
Hanover Township, Lehigh County, Pennsylvania. Hanover Township is a township in Lehigh County, Pennsylvania, United States. As of the 2010 census, the township had a population of 1,571. It is a suburb of Allentown and Bethlehem and part of the Lehigh Valley metropolitan area, which had a population of 861,899 and was the 68th-most populous metropolitan area in the U.S. as of the 2020 census.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Ranni, Kerala. Ranni (or Ranny) is a town in the Pathanamthitta district of Kerala, India, and the 16th largest &quot;taluk&quot; in the state. The town is situated on both sides of the Pamba River. It falls under the Thiruvalla Revenue Division and is located 27 km from Thiruvalla railway station and NH 183 in Thiruvalla. Etymology.

Geographic entities mentioned:
surface_form: Pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Geography. Ranni is located in southwestern India at. It has an average elevation of 131 m (433 ft) above sea level. However, towards the east, the elevation is much higher. The river Pamba flows through Ranni township. According to the 2001 Census of India, Ranni spans a total of. Out of the total area, or 70% are forest. Climate.

Geographic entities mentioned:
surface_form: Pamba
instance_of: Watercourse
countries: India
coordinates: lat: 9.5
lon: 76.416666666667
Abandoned granite quarries and clay banks where bricks were made suggest the early economic activities of the area. Geography. According to the United States Census Bureau, the town has a total area of, of which is land and is water. Jefferson is located on the Great Bay of Damariscotta Lake. Damariscotta Lake State Park is a State Park located in Jefferson. 2010 census.

Geographic entities mentioned:
surface_form: Damariscotta Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.147
lon: -69.486
Monte Brè funicular. The Monte Brè funicular, or &quot;Funicolare Cassarate - Monte Brè&quot;, is a funicular railway in the city of Lugano in the Swiss canton of Ticino. The line links a lower station in the Lugano suburb of Cassarate with an upper station at near the summit of the Monte Brè. The top yields views of the city and Lake Lugano.

Geographic entities mentioned:
surface_form: Monte Brè
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.008611111111
lon: 8.9863888888889
The Monte Brè funicular, or &quot;Funicolare Cassarate - Monte Brè&quot;, is a funicular railway in the city of Lugano in the Swiss canton of Ticino. The line links a lower station in the Lugano suburb of Cassarate with an upper station at near the summit of the Monte Brè. The top yields views of the city and Lake Lugano. The funicular is composed of two separate and independent sections.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
The Monte Brè funicular is one of three operational funiculars within the Lugano area. The other two are the Monte San Salvatore funicular, which ascends Monte San Salvatore on the opposite side of the city, and the Lugano Città–Stazione funicular, which links the city centre with the railway station. History.

Geographic entities mentioned:
surface_form: Monte San Salvatore
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.976666666667
lon: 8.9480555555556
They returned to South Africa in 1948 for the birth of their son. Louw left South Africa to live in Israel after finishing school at 17. She was one of the first students on the Mount Scopus campus in Jerusalem. Louw moved to Brighton in the UK in 1976. After a variety of jobs, she received a PhD in Organisational informatics in the NHS at the University of Brighton in 1994.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
Fish Hoek. Fish Hoek (, meaning either Fish Corner or Fish Glen) is a coastal suburb of Cape Town at the eastern end of the Fish Hoek Valley on the False Bay side of the Cape Peninsula in the Western Cape, South Africa. Previously a separate municipality, Fish Hoek is now part of the City of Cape Town. History.

Geographic entities mentioned:
surface_form: Fish Hoek Valley
instance_of: Valley
countries: South Africa
coordinates: lat: -34.125
lon: 18.3958
Nowadays, alcohol is available in restaurants and bars, but only recently have there been bottle stores allowed. Geography. Fish Hoek is situated in a bay at the end of a broad, low valley, between two and three kilometres wide, which runs from east to west across the Cape Peninsula from Fish Hoek on the False Bay side to Noordhoek and Kommetjie on the Atlantic side.

Geographic entities mentioned:
surface_form: valley
instance_of: Valley
countries: South Africa
coordinates: lat: -34.125
lon: 18.3958
Climate. Fish Hoek has a mild mediterranean climate and is spared over hot summer days by the south-easterly wind known locally as &quot;the Cape Doctor&quot;. The mountains nearby are famous for large numbers of complex caves in sandstones of the Table Mountain Group. Caves are usually found in limestones and it is not common to find complex cave systems in pure sandstone. Economy.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Luzon is the largest and northernmost major island of the Philippines, located in the western Pacific Ocean. Geography. The ecoregion includes several volcanic and non-volcanic mountains that exceed in altitude. The volcanic mountains include Mt. Makiling, Mount Banahaw, Mount Isarog, Mayon Volcano, and Bulusan Volcano.

Geographic entities mentioned:
surface_form: Mount Banahaw
instance_of: Mountain
countries: Philippines
coordinates: lat: 14.066666666667
lon: 121.48333333333
surface_form: Mount Isarog
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.659166666667
lon: 123.37333333333
In May 2014, she sang at the Torch-lighting ceremony on Mount Herzl held as part of the Israel Independence Day celebrations. On early 2015, Rada signed a contract with the label Discograph (belonging to Harmonia Mundi), for the distribution of her &quot;Ester Rada&quot; album across Europe.

Geographic entities mentioned:
surface_form: Mount Herzl
instance_of: Mountain
countries: Israel
coordinates: lat: 31.774117
lon: 35.180567
It has long been known from the emerald and chrysoberyl mine on the Takovaya stream, near Yekaterinburg in the Urals of Russia, where large crystals occur in mica-schist. It is also found with topaz and amazonite in the granite of the Ilmen Mountains in the southern Urals and of the Pikes Peak region in Colorado, US.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
It is also found with topaz and amazonite in the granite of the Ilmen Mountains in the southern Urals and of the Pikes Peak region in Colorado, US. Additionally in Colorado, phenakite is found in the Mount Antero area with aquamarine, bertrandite, and fluorite.

Geographic entities mentioned:
surface_form: Mount Antero
instance_of: Mountain
countries: United States
coordinates: lat: 38.674166666667
lon: -106.24611111111
Hårteigen. Hårteigen is a characteristic mountain in Vestland county, Norway. It sits on and is visible from most parts of the vast Hardangervidda plateau. The mountain is located in the municipality of Ullensvang, and it is inside the Hardangervidda National Park. At an elevation of above sea level, the peak of Hårteigen rises above the surrounding plateau which is fairly level.

Geographic entities mentioned:
surface_form: hårteigen
instance_of: Mountain
countries: Norway
coordinates: lat: 60.195402777778
lon: 7.0683611111111
It sits on and is visible from most parts of the vast Hardangervidda plateau. The mountain is located in the municipality of Ullensvang, and it is inside the Hardangervidda National Park. At an elevation of above sea level, the peak of Hårteigen rises above the surrounding plateau which is fairly level. It is located about northeast of the town of Odda. Name.

Geographic entities mentioned:
surface_form: hårteigen
instance_of: Mountain
countries: Norway
coordinates: lat: 60.195402777778
lon: 7.0683611111111
Ukleisee. Ukleisee is a lake in Kreis Ostholstein, Schleswig-Holstein, Germany. At an elevation of 26.5 m, its surface area is 0.32 km². This lake is (as numerous other lakes in this area) a kettle hole, remaining from Weichselian glaciation.

Geographic entities mentioned:
surface_form: ukleisee
instance_of: Lake
countries: Germany
coordinates: lat: 54.184438888889
lon: 10.637169444444
Cairn Bannoch. Cairn Bannoch () is a mountain in the White Mounth, a mountainous plateau in the Scottish Highlands. It is about seventeen miles south of the River Dee near Balmoral.

Geographic entities mentioned:
surface_form: cairn bannoch
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.927728
lon: -3.278419
Nevertheless, summer low water flows rarely drop below. While conducting surveys for irrigation projects in the early 1900s, the U.S. Reclamation Service (now Bureau of Reclamation) noted that the spring-fed Fall River alone contributed a year-round flow of about, from an aquifer fed in part by Mount Shasta snowmelt.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Much of this water rises at what is often called &quot;Thousand Springs&quot; a few miles above Fall River Mills, west of Ahjumawi Lava Springs State Park. Hat Creek and Burney Creek, spring-fed from the Lassen Peak area, supplied a further to the Pit River.

Geographic entities mentioned:
surface_form: Lassen Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.488055555555555
lon: -121.505
Flows for these two dams are supplemented by a diversion from the McCloud River, a tributary of the Pit River. Water is diverted from the McCloud River at Lake McCloud about south of Mount Shasta, through a tunnel to Iron Canyon Reservoir, and then through another tunnel to the James B. Black Powerhouse, which outlets into the Pit River on the upper end of Pit 6 Reservoir.

Geographic entities mentioned:
surface_form: Lake McCloud
instance_of: Lake
countries: United States
coordinates: lat: 41.131111111111
lon: -122.07055555556
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Native peoples also grew hostile towards Euro-American settlers and traders, who entered the region in great numbers beginning in the mid-19th century, especially during and after the California Gold Rush in 1848. There was little conflict at first with outsiders who were just passing through the area on their way to the Sacramento Valley.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
General. Tikkakoski is located in the far northern part of Jyväskylä near its borders with Laukaa and Uurainen, approximately north of the city center. The biggest lake in the area is Luonetjärvi, which discharges into lake Korttajärvi via the river Autiojoki, while smaller ponds include Myllylampi, Koivulampi, Likolampi and Liinalampi. Hietajärvi is not a separate lake, but a part of Luonetjärvi.

Geographic entities mentioned:
surface_form: Korttajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.3378
lon: 25.6916
The highest elevations occur in the Tarahumara range. The exact elevations of the highest peaks are not known within accurate enough ranges to determine their relative elevation. The highest point is probably Cerro Mohinora, located at. Estimates for the height of the mountain start around and go up to. However, Cerro Barajas, at, may be as high as although other sources give as the elevation.

Geographic entities mentioned:
surface_form: Cerro Mohinora
instance_of: Mountain
countries: Mexico
coordinates: lat: 25.95611111
lon: -107.04777778
In this area, the Sierra Madre begins to give way to the Basin and Range Province. Subranges of this area include the Sierra de Alica and the Sierra Pajaritos, both in Nayarit, and the Sierra los Huicholes, Sierra de Morones, Sierra Nochistlán, and Sierra Fría extending eastwards into Jalisco, Zacatecas, and Aguascalientes. Water.

Geographic entities mentioned:
surface_form: Sierra Fría
instance_of: Mountain
countries: Mexico
coordinates: lat: 22.216111111111
lon: -102.61888888889
The tuffs are above a thick formation of lava rock. Around five or six units have been identified, mostly around the Copper Canyon area. These tuffs have allowed wide-ranging correlation with formations in other geographical areas, for example Death Valley. During the Miocene, three periods of volcanism marked separate events in the Sierras. Each period is marked by different volcanic processes.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Some of these faults may have allowed ignimbrites to erupt from the surface, and so there may be some association between the ignimbrite occurrence and faults; this can be used to find out information about different kinds of basement rock present. There are two faults dividing the Sierra Madre from the central Mexican Plateau.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Additionally, there are reserves such as La Michilía in the southern Sierra Madre, or the Tutuaca reserve in western Chihuahua, which was established in 2000 under a new system of management. Other protected areas in the Sierra include the Bavispe, Campo Verde, Cerro Mohinora, Papigochic, and Sierra de Álamos–Río Cuchujaqui flora and fauna protection areas.

Geographic entities mentioned:
surface_form: Cerro Mohinora
instance_of: Mountain
countries: Mexico
coordinates: lat: 25.95611111
lon: -107.04777778
The lake is, it has an area of 6.8 hectares and measures 300 metres by 270 metres. Its only headstream is a ditch from the meadows to the north, a ditch also carries its waters away to the Feisneck which in turn empties into the Müritz. The lake is mostly surrounded by meadows, only the eastern shore has a row of bushes.

Geographic entities mentioned:
surface_form: Müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
surface_form: feisneck
instance_of: Lake
countries: Germany
coordinates: lat: 53.495833333333
lon: 12.707777777778
Waupacksee. The Waupacksee is a lake on the southeastern edge of the town of Waren (Müritz) in the district of Mecklenburgische Seenplatte in the German state of Mecklenburg-Western Pomerania. The lake is, it has an area of 6.8 hectares and measures 300 metres by 270 metres.

Geographic entities mentioned:
surface_form: waupacksee
instance_of: Lake
countries: Germany
coordinates: lat: 53.50556
lon: 12.71528
Waupacksee. The Waupacksee is a lake on the southeastern edge of the town of Waren (Müritz) in the district of Mecklenburgische Seenplatte in the German state of Mecklenburg-Western Pomerania. The lake is, it has an area of 6.8 hectares and measures 300 metres by 270 metres.

Geographic entities mentioned:
surface_form: waupacksee
instance_of: Lake
countries: Germany
coordinates: lat: 53.50556
lon: 12.71528
surface_form: müritz
instance_of: Lake
countries: Germany
coordinates: lat: 53.416666666667
lon: 12.683333333333
Mashkovtsev (volcano). Mashkovtsev () is a small stratovolcano located in the southern part of the Kamchatka Peninsula, Russia. It is the southernmost holocene volcano of Kamchatka.

Geographic entities mentioned:
surface_form: mashkovtsev (volcano)
instance_of: Mountain
countries: Russian Empire
Soviet Union
Russia
coordinates: lat: 51.1
lon: 156.72
Mashkovtsev (volcano). Mashkovtsev () is a small stratovolcano located in the southern part of the Kamchatka Peninsula, Russia. It is the southernmost holocene volcano of Kamchatka.

Geographic entities mentioned:
surface_form: mashkovtsev
instance_of: Mountain
countries: Russian Empire
Soviet Union
Russia
coordinates: lat: 51.1
lon: 156.72
Zeus had intercourse with Persephone in the form of a serpent, producing Dionysus. He is taken to Mount Ida where (like the infant Zeus) he is guarded by the dancing Curetes. Zeus intended Dionysus to be his successor as ruler of the cosmos, but a jealous Hera incited the Titans to kill the child.

Geographic entities mentioned:
surface_form: Mount Ida
instance_of: Mountain
countries: Turkey
County Road 712. County Road 712 is Midway Road, an east–west road providing one of the few access points to I-95 within the county. The western terminus is an intersection with Okeechobee Road (SR 70) west of Port St. Lucie; the eastern terminus of CR 712 is an intersection with Indian River Drive (CR 707) on the western edge of the Indian River near Indian River Estates.

Geographic entities mentioned:
surface_form: Indian River
instance_of: Body of water
countries: United States
coordinates: lat: 28.05527778
lon: -80.57611111
The Nordic states and the state of Novgorod soon began expanding northwards, dividing Sámi lands into spheres of interest. A system of joint taxation was established for parts of the Sámi area, so that, for example, the Sámi between the Lyngen Alps and the White Sea needed to pay taxes to both Norway/Denmark–Norway and Novgorod/Grand Duchy of Moscow/Tsardom of Russia.

Geographic entities mentioned:
surface_form: Lyngen Alps
instance_of: Mountain
countries: Norway
coordinates: lat: 69.51189
lon: 19.89262
The only place in historical Jerusalem where water is flowing year-round, thanks to the nearby Gihon Spring, allowing for permanent growth of natural vegetation and agriculture, is at the confluence of the Kidron and the Central (aka Tyropoeon) valleys. The area known as the King's Garden is today planted with many fruit trees that are nourished by the water run-off from the Pool of Siloam.

Geographic entities mentioned:
surface_form: Kidron
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
surface_form: Central (aka Tyropoeon)
instance_of: Valley
countries: State of Palestine
Israel
coordinates: lat: 31.776947222222
lon: 35.234238888889
The Kidron Valley, which cuts through Silwan, was divided by its local inhabitants into three sections, proceeding from north to south; 1st &quot;Wady Sitti Mariam&quot; (Valley of My Lady Mary), 2nd &quot;Wady Fer'aun&quot; (Pharaoh's Valley), and 3rd &quot;Wady Eyûb&quot; (Valley of Job).

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Madom da Sgióf. The Madom da Sgióf is a mountain of the Swiss Lepontine Alps, located between Maggia and Brione in the canton of Ticino.

Geographic entities mentioned:
surface_form: madom da sgióf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.268055555556
lon: 8.7761388888889
Archaeology. Tel Hanaton, an archaeological site associated with the biblical location lies to the east of the kibbutz. The tel is in the western end of the Beit Netofa Valley, and covers an area of roughly 100 dunam (25 acres). It was occupied from the Bronze Age through the Ottoman Empire.

Geographic entities mentioned:
surface_form: Tel Hanaton
instance_of: Mountain
countries: Israel
coordinates: lat: 32.785555555556
lon: 35.256944444444
Archaeology. Tel Hanaton, an archaeological site associated with the biblical location lies to the east of the kibbutz. The tel is in the western end of the Beit Netofa Valley, and covers an area of roughly 100 dunam (25 acres). It was occupied from the Bronze Age through the Ottoman Empire.

Geographic entities mentioned:
surface_form: Beit Netofa Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.80956667
lon: 35.33246111
Career. In January 2024, Vatan transferred to the Fenerbahçe Sailing. She competed at the Last Chance Regatta of the Sailing at the 2024 Summerto Olympics – Qualification in Hyères, France. She reached the semi-finals, and so was qualified to represent Turkey at the 2024 Summer Olympics competing in the Women's windsurfer – IQFoil event. Personal life.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Near the town's central business district, the byway is joined with US 11W/SR 1 via trumpet interchange. The concurrency to US 11W continues until reaching Briar Fork Creek at the base of Clinch Mountain, where US 11W splits off and heads west along the Richland Valley towards Knoxville, and the byway northbound into Poor Valley ascending the southern slope of Clinch Mountain.

Geographic entities mentioned:
surface_form: Poor Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.185555555556
lon: -83.695555555556
Chunta Q'atawi. Chunta Q'atawi (Aymara &quot;chunta&quot; prolonged, lengthened, &quot;q'atawi&quot; lime, &quot;prolonged lime (mountain)&quot;, Hispanicized spelling &quot;Chuntajatahui&quot;) is a mountain in the Andes of Peru. It is situated in the Puno Region, Carabaya Province, Crucero District.

Geographic entities mentioned:
surface_form: chunta q'atawi
instance_of: Mountain
countries: Peru
coordinates: lat: -14.28972222
lon: -69.94361111
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
Chunta Q'atawi. Chunta Q'atawi (Aymara &quot;chunta&quot; prolonged, lengthened, &quot;q'atawi&quot; lime, &quot;prolonged lime (mountain)&quot;, Hispanicized spelling &quot;Chuntajatahui&quot;) is a mountain in the Andes of Peru. It is situated in the Puno Region, Carabaya Province, Crucero District.

Geographic entities mentioned:
surface_form: chunta q'atawi
instance_of: Mountain
countries: Peru
coordinates: lat: -14.28972222
lon: -69.94361111
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -11.4964
lon: -76.3772
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7836
lon: -72.5717
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
surface_form: chunta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.4222
lon: -73.8572
The building was grade II listed in 1986. On completion, it could seat a congregation of 700 worshippers, but by 2016 it was hosting fortnightly services with fewer than ten attendees. It was threatened with closure in 2015, but a friends group was set up to fund running costs and repairs, and it survives as the last Methodist chapel in Swaledale.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
North Burnaby. North Burnaby is a general name for a large neighbourhood in the City of Burnaby, British Columbia, that includes a number of smaller ones. It stretches from Boundary Road in the west to Burnaby Mountain with Simon Fraser University in the east and is bounded by Burrard Inlet to the north and the Lougheed Highway to the south.

Geographic entities mentioned:
surface_form: Burnaby Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.2792
lon: -122.909
The Egå stream has its source at Geding Lake and from here it flows through the Geding-Kasted bog, the lake of Egå Engsø, the suburban area of Egå and the beach park of Åkrogen, before it terminates at the Bay of Aarhus. The Egå suburb. The suburban area of Egå is located approximately 7 km north of the Aarhus city centre and is named after the Egå stream, that flows through the area.

Geographic entities mentioned:
surface_form: Geding Lake
instance_of: Lake
countries: Denmark
coordinates: lat: 56.1963
lon: 10.0899
surface_form: Egå Engsø
instance_of: Lake
countries: Denmark
coordinates: lat: 56.218
lon: 10.221
Route 101, near the small community of Piedmont. With an official maximum depth of, it is officially the second deepest lake in the state of Washington (after Lake Chelan). A lake-wide bathymetric survey was performed from 2013 to 2014 by Eian Ray and Jeff Engea and the results of this survey show the maximum depth as being.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Anadromous fish such as steelhead and coastal cutthroat trout migrated into the valley from lower waters. Approximately 8,000 years ago, a great landslide from one of the Olympic Mountains dammed Indian Creek, and the deep valley filled with water. Many geologists believe that Lake Crescent and nearby Lake Sutherland formed at the same time, but became separated by the landslide.

Geographic entities mentioned:
surface_form: Lake Sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Many geologists believe that Lake Crescent and nearby Lake Sutherland formed at the same time, but became separated by the landslide. This theory is supported by Klallum tribe legend which tells a story of Mount Storm King being angered by warring tribes and throwing a boulder to cut Lake Sutherland in two, resulting in Lake Crescent.

Geographic entities mentioned:
surface_form: Mount Storm King
instance_of: Mountain
countries: United States
coordinates: lat: 48.0557
lon: -123.741
surface_form: mount storm king
instance_of: Mountain
countries: United States
coordinates: lat: 48.0557
lon: -123.741
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
In the c. 1,100 BCE event, an earthquake triggered the Sledgehammer Point Rockslide, which fell from Mount Storm King and entered waters at least deep, generating a megatsunami with an estimated maximum run-up height of. It is not certain whether the lake was named for its crescent shape or for its proximity to Crescent Bay, which was named by Henry Kellett in 1846.

Geographic entities mentioned:
surface_form: Mount Storm King
instance_of: Mountain
countries: United States
coordinates: lat: 48.0557
lon: -123.741
surface_form: mount storm king
instance_of: Mountain
countries: United States
coordinates: lat: 48.0557
lon: -123.741
It is not certain whether the lake was named for its crescent shape or for its proximity to Crescent Bay, which was named by Henry Kellett in 1846. In 1849 two British–Canadian fur trappers, John Sutherland and John Everett, forged inland from Crescent Bay. The two lakes they found became known as Lake Sutherland and Everett Lake. Later, Everett Lake was renamed Lake Crescent.

Geographic entities mentioned:
surface_form: Lake Sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Lake Crescent is known for brilliant blue waters and exceptional clarity caused by low levels of nitrogen in the water that inhibit the growth of algae. The lake is located in a popular recreational area and features several trails, including the Spruce Railroad Trail, Pyramid Mountain trail, and the Barnes Creek trail to Marymere Falls.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.6397
lon: -148.515
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 57.8017
lon: -152.5775
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.28333333
lon: -109.75444444
This theory is supported by Klallum tribe legend which tells a story of Mount Storm King being angered by warring tribes and throwing a boulder to cut Lake Sutherland in two, resulting in Lake Crescent. The results of the landslide are easily visible from the summit of Pyramid Mountain.

Geographic entities mentioned:
surface_form: pyramid
instance_of: Lake
countries: United States
coordinates: lat: 40.033333333333
lon: -119.56666666667
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0748
lon: -123.807
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 63.6397
lon: -148.515
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 57.8017
lon: -152.5775
surface_form: pyramid mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.28333333
lon: -109.75444444
The two lakes they found became known as Lake Sutherland and Everett Lake. Later, Everett Lake was renamed Lake Crescent. It has also been known as Big Lake and Elk Lake. In 1890, while the Port Crescent Improvement Company was promoting its townsite near the lake, M.J. Carrigan started the &quot;Port Crescent Leader&quot; to help boost the town.

Geographic entities mentioned:
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0725
lon: -95.345
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1722398
lon: -67.6821052
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 45.819722222222
lon: -96.113055555556
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 31.1667
lon: -101.483
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9742
lon: -121.802
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.025277777778
lon: -115.07138888889
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.919166666667
lon: -95.521944444444
surface_form: big lake
instance_of: Lake
countries: United States
coordinates: lat: 33.8847
lon: -109.415
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 45.867222222222
lon: -95.804722222222
surface_form: elk lake
instance_of: Lake
countries: United States
coordinates: lat: 44.85
lon: -85.3833
Lake Crescent. Lake Crescent is a deep lake located entirely within Olympic National Park in Clallam County, Washington, United States, approximately west of Port Angeles on U.S. Route 101, near the small community of Piedmont. With an official maximum depth of, it is officially the second deepest lake in the state of Washington (after Lake Chelan).

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 46.9075
lon: -122.9125
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 41.5699
lon: -123.113
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 26.0506
lon: -81.3425
surface_form: piedmont
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -80
surface_form: deep lake
instance_of: Lake
countries: United States
coordinates: lat: 39.773
lon: -107.3
They were unable to determine the maximum depth with their equipment. During a 1970 depth survey conducted by the students of the fisheries program at Peninsula College in Port Angeles, Washington, students used instruments that could not record measurements beyond a depth of. This became known as the &quot;official&quot; depth of the lake as recorded by the National Park Service.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Origins. The lake was formed when glaciers carved deep valleys during the last Ice Age. Initially, the Lake Crescent valley drained into the Indian Creek valley and then into Elwha River. Anadromous fish such as steelhead and coastal cutthroat trout migrated into the valley from lower waters.

Geographic entities mentioned:
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.30944444
lon: -91.99777778
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.51944444
lon: -93.5225
surface_form: indian creek
instance_of: Watercourse
countries: United States
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.9747757
lon: -90.1978958
Anadromous fish such as steelhead and coastal cutthroat trout migrated into the valley from lower waters. Approximately 8,000 years ago, a great landslide from one of the Olympic Mountains dammed Indian Creek, and the deep valley filled with water. Many geologists believe that Lake Crescent and nearby Lake Sutherland formed at the same time, but became separated by the landslide.

Geographic entities mentioned:
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.30944444
lon: -91.99777778
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.51944444
lon: -93.5225
surface_form: indian creek
instance_of: Watercourse
countries: United States
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.9747757
lon: -90.1978958
Lake Crescent. Lake Crescent is a deep lake located entirely within Olympic National Park in Clallam County, Washington, United States, approximately west of Port Angeles on U.S. Route 101, near the small community of Piedmont. With an official maximum depth of, it is officially the second deepest lake in the state of Washington (after Lake Chelan).

Geographic entities mentioned:
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
Using GIS statistical analysis, this survey also estimated that the lake contains around of fresh water. Lake Crescent is known for brilliant blue waters and exceptional clarity caused by low levels of nitrogen in the water that inhibit the growth of algae.

Geographic entities mentioned:
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
During the Lake Crescent Bathymetric Survey, it was speculated that the erroneous depth record of from the 1980s was a result of the sonar signal reflecting off the steep underwater slopes near the shore. History. Scientists have found evidence of four very large landslides entering Lake Crescent between about 5,200 BCE and about 1,100 BCE. In the c.

Geographic entities mentioned:
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
In 1849 two British–Canadian fur trappers, John Sutherland and John Everett, forged inland from Crescent Bay. The two lakes they found became known as Lake Sutherland and Everett Lake. Later, Everett Lake was renamed Lake Crescent. It has also been known as Big Lake and Elk Lake. In 1890, while the Port Crescent Improvement Company was promoting its townsite near the lake, M.J.

Geographic entities mentioned:
surface_form: lake crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037