Sarmila/GeoWiki-Features huggingface dataset:
The peak is named after the town of Beloslav in Northeastern Bulgaria. Location. Beloslav Peak is located at, which is 4.44 km southeast of Mount Havener, 8.37 km southwest of Gubesh Peak, 4.97 km northwest of Taylor Spur and 8.92 km northeast of McPherson Peak. US mapping in 1961, updated in 1988.

Geographic entities mentioned:
surface_form: Mount Havener
instance_of: Mountain
coordinates: lat: -78.45
lon: -84.6167
surface_form: Gubesh Peak
instance_of: Mountain
coordinates: lat: -78.4567
lon: -84.1661
surface_form: McPherson Peak
instance_of: Mountain
coordinates: lat: -78.5333
lon: -84.7
However, on each day she becomes more and more monstrous, until the young man flees in terror without giving her the final kisses. He later marries another girl, but the food at their wedding feast is mysteriously poisoned with serpent venom and everyone who eats it dies. Other Germanic water sprites include Lorelei and the nixie. In Britain.

Geographic entities mentioned:
surface_form: Lorelei
instance_of: Mountain
countries: Germany
coordinates: lat: 50.139444444444
lon: 7.7288888888889
It is located about north of county town Mullingar. Clonava is one of 35 townlands of the civil parish of Street in the barony of Moygoish in the Province of Leinster. The townland covers, including of water; part of the western end of Lough Derravaragh and the majority of the small lake, Lough Ruddan. The townland contains the settlement of Clonave.

Geographic entities mentioned:
surface_form: Lough Derravaragh
instance_of: Lake
countries: Ireland
coordinates: lat: 53.6526
lon: -7.3587
C. LaRue. He had piloted a boat for the 1922 USGS survey of Glen Canyon. Freeman's flamboyant articles about the 1922 trip were a contributing factor to his being invited to participate in the 1923 trip. On the Grand Canyon cruise, Freeman's nickname was &quot;The Gorilla.&quot; While portaging their boats at Lava Falls, the trip experienced a stunning up and down rise in river flow.

Geographic entities mentioned:
surface_form: Glen Canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.86443
lon: -111.58794
Off BC Highway 3, the locality is by road about southeast of Princeton and south of Penticton. Name origin. &quot;Chopaka&quot; (pronounced like tobacco) signifies &quot;lofty&quot; or &quot;grand&quot; and refers to Chopaka Mountain, which dominates the area. The word is the anglicized version of &quot;c̓up̓áq̓&quot;, which can mean &quot;sticking out mountain&quot;.

Geographic entities mentioned:
surface_form: Chopaka Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.9575
lon: -119.785
Bukit Daun. Bukit Daun (, means: &quot;Leaves Hill&quot;) is a stratovolcano, located in a sparsely populated region in Sumatra, Indonesia. A 600 m wide of crater lake is located at the summit. A smaller crater lake, Tologo Kecil, is found in the south-west flank.

Geographic entities mentioned:
surface_form: bukit daun
instance_of: Mountain
countries: Indonesia
coordinates: lat: -3.38
lon: 102.37
Sangay is on the eastern edge of the Andes Mountains in central Ecuador about south of Quito and east of Riobamba. It lies within Sangay National Park. Two nearby volcanoes, Tungurahua and El Altar, are also located within the national park. The three volcanoes reach exceed above sea level with El Altar being the tallest.

Geographic entities mentioned:
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: El Altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
surface_form: tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
surface_form: el altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
Mariners traveling in the vicinity were cautioned about the possibility of debris. Ecology. Sangay is one of two active volcanoes in the Sangay National Park, the other being Tungurahua to the north. As such it has been listed as a UNESCO World Heritage Site since 1983.

Geographic entities mentioned:
surface_form: Tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: tungurahua
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.4669444444444
lon: -78.441666666667
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Sangay. Sangay (also known as Macas, Sanagay, or Sangai) is an active stratovolcano in central Ecuador. It exhibits mostly strombolian activity. Geologically, Sangay marks the southern boundary of the Northern Volcanic Zone, and its position straddling two major pieces of crust accounts for its high level of activity.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Sangay. Sangay (also known as Macas, Sanagay, or Sangai) is an active stratovolcano in central Ecuador. It exhibits mostly strombolian activity. Geologically, Sangay marks the southern boundary of the Northern Volcanic Zone, and its position straddling two major pieces of crust accounts for its high level of activity.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
surface_form: sangai
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Geologically, Sangay marks the southern boundary of the Northern Volcanic Zone, and its position straddling two major pieces of crust accounts for its high level of activity. Sangay's approximately 500,000-year-old history is one of instability; two previous versions of the mountain were destroyed in massive flank collapses, evidence of which still litters its surroundings today.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Sangay's approximately 500,000-year-old history is one of instability; two previous versions of the mountain were destroyed in massive flank collapses, evidence of which still litters its surroundings today. Due to its remoteness, Sangay hosts a significant biological community with fauna such as the mountain tapir, giant otter, Andean cock-of-the-rock and king vulture.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Due to its remoteness, Sangay hosts a significant biological community with fauna such as the mountain tapir, giant otter, Andean cock-of-the-rock and king vulture. Since 1979, its ecological community has been protected as part of the Sangay National Park.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Moore in 1929. History. Folklore sourced from native people in the region compared Sangay to a lighthouse surrounded by a sea, which represented the dense jungle. The density of the jungle caused people to lose their way, but seeing ash and steam emissions from the volcano would help orient travelers along their way.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
The density of the jungle caused people to lose their way, but seeing ash and steam emissions from the volcano would help orient travelers along their way. Scientists have interpreted folklore like this as evidence of frequent and long-lasting eruptive activity at Sangay.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Altogether the cities may have reached a population between 15,000 and 100,000 people. They were surrounded by agricultural fields that archaeologist Stéphen Rostain speculates may have been particularly productive because their proximity to Sangay. Seventeen additional archaeological sites had been located prior to the 2024 announcement including potential monuments.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Modern development of the eastern side of the volcano began in the early 20th Century. The volcano and lands surrounding it were placed in a National Wildlife Reserve by the Ecuadorian government in 1975. This became Sangay National Park in 1979, which was expanded in 1992. The United Nations added it to their list of World Heritage Sites in 1983.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
The modern native inhabitants of the region primarily consist of Quechua people. The name Sangay comes from the Quechuan languages and is translated as &quot;the frightener.&quot;
Geography. Sangay is on the eastern edge of the Andes Mountains in central Ecuador about south of Quito and east of Riobamba. It lies within Sangay National Park.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
The name Sangay comes from the Quechuan languages and is translated as &quot;the frightener.&quot;
Geography. Sangay is on the eastern edge of the Andes Mountains in central Ecuador about south of Quito and east of Riobamba. It lies within Sangay National Park. Two nearby volcanoes, Tungurahua and El Altar, are also located within the national park.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
The three volcanoes reach exceed above sea level with El Altar being the tallest. The principal rivers draining Sangay are the Llushin, Palora, and the Upano, each of which have numerous smaller tributaries on the middle and upper slopes. Flash flooding from significant rainfall is frequent and erosion is a problem despite thick forests. Rivers drain east into the Amazon Basin.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Regional setting. Lying at the eastern edge of the Andean cordillera, Sangay was formed by volcanic processes associated with the subduction of the Nazca Plate under the South American Plate at the Peru–Chile Trench. It is the southernmost volcano in the Northern Volcanic Zone, a subgroup of Andean volcanoes whose northern limit is Nevado del Ruiz in Colombia.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
The older southern rock is more thermally stable than the northern rock, and to this is attributed the long break in volcanic activity in the Andes; Sangay occupies a position at the boundary between these two bodies, accounting for its high level of activity. Formation. Sangay developed in three distinct phases.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
This thick block, the best-preserved specimen of Sangay's early construction, consists of sequentially layered breccias, pyroclastic flows, and lahar deposits. Acidic andesites with just under 60% silicon dioxide dominate these flows, but more basic andesites can be found as well.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Sangay's second structure is believed to have had an east-to-west elongated summit, and like its first summit structure, it suffered a catastrophic collapse that created a debris avalanche wide and up to in length. It was likely less voluminous than the volcano's first version, and its summit lay near Sangay's current summit. Recent activity.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Uniquely, in its 500,000 years of activity, its magma plume has never changed composition or moved a significant distance. Mainly andesitic in composition, Sangay is highly active. The earliest report of a historical eruption was in 1628; ash fell as far away as Riobamba, located northwest of Sangay, and was severe enough to cover pastures and starve local livestock.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
After a brief pause, it erupted again on August 8, 1934, and has not completely quelled ever since, with heavy eruptive periods occurring in 1934–1937 and 1941–1942. Eruptions at Sangay exhibit strombolian activity, producing ashfall, lava flows, pyroclastic flows, and lahars. All known eruptions at the volcano have had a Volcanic Explosivity Index (VEI) of 3 or less.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
Eruptions at Sangay exhibit strombolian activity, producing ashfall, lava flows, pyroclastic flows, and lahars. All known eruptions at the volcano have had a Volcanic Explosivity Index (VEI) of 3 or less. Despite its activity, Sangay is located in a remote, uninhabited region; only a large Plinian eruption could threaten occupied areas to its west.

Geographic entities mentioned:
surface_form: sangay
instance_of: Mountain
countries: Ecuador
coordinates: lat: -2.0025
lon: -78.340833333333
It lies within Sangay National Park. Two nearby volcanoes, Tungurahua and El Altar, are also located within the national park. The three volcanoes reach exceed above sea level with El Altar being the tallest. The principal rivers draining Sangay are the Llushin, Palora, and the Upano, each of which have numerous smaller tributaries on the middle and upper slopes.

Geographic entities mentioned:
surface_form: altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
surface_form: el altar
instance_of: Mountain
countries: Ecuador
coordinates: lat: -1.6641666666667
lon: -78.411111111111
During the 1870s, thanks to the decline of the coffee region of the Paraíba Valley and some areas of sugar production, many owners of plantations invested not only in the cotton textile industry, but also in other manufacturing sectors. Deployment of a railway network throughout the national territory also stimulated the emergence of new industrial activities, mainly in São Paulo.

Geographic entities mentioned:
surface_form: Paraíba Valley
instance_of: Valley
countries: Brazil
coordinates: lat: -22.75
lon: -45.15
In nature. Polygons appear in rock formations, most commonly as the flat facets of crystals, where the angles between the sides depend on the type of mineral from which the crystal is made. Regular hexagons can occur when the cooling of lava forms areas of tightly packed columns of basalt, which may be seen at the Giant's Causeway in Northern Ireland, or at the Devil's Postpile in California.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Many of the animals collected by La Marmora were sent to Franco Andrea Bonelli at Turin University, and he also corresponded with Bonelli's successor, Giuseppe Gené. The highest point of Sardinia is Punta La Marmora, commemorating the physical and geological surveys of the island Marmora conducted

Geographic entities mentioned:
surface_form: Punta La Marmora
instance_of: Mountain
countries: Italy
coordinates: lat: 39.988055555556
lon: 9.3241666666667
Cape au Moine. The Cape au Moine (1,941 m) is a mountain of the Swiss Prealps, located on the border between the cantons of Vaud and Fribourg. It lies north of the Col de Jaman and south of the Col de Soladier, among of a crest of peaks extending roughly north into Fribourg to the Dent de Lys, on the range between Lake Geneva and the valley of Gruyère.

Geographic entities mentioned:
surface_form: Dent de Lys
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.507638888889
lon: 7.0029444444444
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: gruyère
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.65
lon: 7.1
Cape au Moine. The Cape au Moine (1,941 m) is a mountain of the Swiss Prealps, located on the border between the cantons of Vaud and Fribourg. It lies north of the Col de Jaman and south of the Col de Soladier, among of a crest of peaks extending roughly north into Fribourg to the Dent de Lys, on the range between Lake Geneva and the valley of Gruyère.

Geographic entities mentioned:
surface_form: cape au moine
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38066
lon: 7.17107
surface_form: cape au moine
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.4702
lon: 6.97892
The winners of the ANFA League Cup qualify for the 1998–99 Asian Cup Winners' Cup. First round proper. Champion of each district advances to second round. Unlike other districts, Kathmandu Valley teams participated in a qualifying group stage tournament. Dang District. The champion of the Dang District is unknown. Mahottari District. The champion of the Mahottari District is unknown.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Lupeni Coal Mine. Lupeni Coal Mine is an underground mining exploitation, one of the largest in Romania located in Lupeni, one of six cities in the Jiu Valley region of Hunedoara County. The legal entity managing the Lupeni mine is the National Hard Coal Company which was set up in 1998. The mine has reserves of 65 million tonnes of coal.

Geographic entities mentioned:
surface_form: Jiu Valley
instance_of: Valley
countries: Romania
coordinates: lat: 43.77805556
lon: 23.81333333
Colne Valley (disambiguation). m7icqttr7dmp8e2sacs7bd01gurj" xml:space="preserve">Colne Valley is a valley in West Yorkshire.

Geographic entities mentioned:
surface_form: Colne Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.6272
lon: -1.8624
Otagi Nenbutsu-ji. Otagi Nenbutsu-ji () is a Buddhist temple located in the hillside of the Arashiyama neighborhood of Kyoto, Japan. It is known for the 1,200 moss-covered arhat statues that cover the hillside around the temple grounds. History. Otagi Nenbutsu-ji was originally founded by Empress Shōtoku around Kyoto's Gion district in the year 766.

Geographic entities mentioned:
surface_form: Arashiyama
instance_of: Mountain
countries: Japan
coordinates: lat: 35.00958333333333
lon: 135.6663888888889
In the 13th century, it was again destroyed during a civil war. Over time the temple fell into disrepair and was eventually moved to its current location in Arashiyama in 1922, in an attempt to save the core structure of the temple building. However, the temple received another serious blow in 1950 when it suffered typhoon damage. Restoration.

Geographic entities mentioned:
surface_form: Arashiyama
instance_of: Mountain
countries: Japan
coordinates: lat: 35.00958333333333
lon: 135.6663888888889
Trisaetum Winery. Trisaetum is a winery located in Oregon's Willamette Valley. Established in 2003 by Andrea and James Frey, the winery, pronounced &quot;tris-say-tum&quot;, was named after the founders two children, Tristen and Tatum. The winery is still family owned and operated and produces small lots of critically acclaimed Pinot Noir and Riesling from its estate vineyards.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
This glacier is named after Gullfaxi, the golden-maned horse of Norse mythology. Geography. Guldfaxe is a large, active glacier flowing from the eastern side of the Greenland ice sheet. The Guldfaxe glacier flows roughly eastward between sharp nunataks and flows into the right side of the Rimfaxe Glacier shortly before its terminus in the Sehested Fjord.

Geographic entities mentioned:
surface_form: Sehested Fjord
instance_of: Body of water
countries: Greenland
coordinates: lat: 63.05
lon: -42
Monte Novegno. Monte Novegno is a mountain of the Veneto, Italy. It has an elevation of 1552 metres.

Geographic entities mentioned:
surface_form: monte novegno
instance_of: Mountain
countries: Italy
coordinates: lat: 45.76666667
lon: 11.31666667
surface_form: novegno
instance_of: Mountain
countries: Italy
coordinates: lat: 45.76666667
lon: 11.31666667
Summit Lake (Sudbury District). Summit Lake () is a lake in geographic Shenango Township in the Unorganized North Part of Sudbury District in Northeastern Ontario, Canada.

Geographic entities mentioned:
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1081
lon: -84.6292
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0422
lon: -93.7006
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.2736
lon: -79.7622
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4753
lon: -84.8669
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0464
lon: -76.8425
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.15006
lon: -104.73377
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.2636
lon: -84.5308
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.49
lon: -84.3683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4256
lon: -87.7375
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.25
lon: -124.683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.28861111111111
lon: -122.65972222222223
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4831
lon: -92.6544
surface_form: summit lake (sudbury district)
instance_of: Lake
countries: Canada
coordinates: lat: 48.42638888888889
lon: -82.72083333333333
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0072
lon: -114.026
Summit Lake (Sudbury District). Summit Lake () is a lake in geographic Shenango Township in the Unorganized North Part of Sudbury District in Northeastern Ontario, Canada.

Geographic entities mentioned:
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.1081
lon: -84.6292
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0422
lon: -93.7006
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.2736
lon: -79.7622
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.4753
lon: -84.8669
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.0464
lon: -76.8425
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.15006
lon: -104.73377
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.2636
lon: -84.5308
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.49
lon: -84.3683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4256
lon: -87.7375
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.25
lon: -124.683
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.28861111111111
lon: -122.65972222222223
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.4831
lon: -92.6544
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.42638888888889
lon: -82.72083333333333
surface_form: summit lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.0072
lon: -114.026
Hydrology. Summit Lake is about long and wide, and lies at an elevation of. There are two unnamed creeks as inflows, located at the south and northeast tips of the lake. The primary outflow is Shiners Creek, towards Shiners Lake, at the northwest corner of the lake, which flows via the Nemegosenda River, Kapuskasing River, Mattagami River and Moose River into James Bay.

Geographic entities mentioned:
surface_form: moose
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91444444444444
lon: -118.80638888888889
Its southern part borders Kedah and Perak of Malaysia. Geography. Yala province is in southern Thailand. The highest point of the Sankalakhiri Range (Northern Titiwangsa Mountains), the -high Ulu Titi Basah (ฮูลูติติปาซา), is on the Thai/Malaysian border between Yala province and Perak. The total forest area is or 32.5 percent of provincial area. National parks.

Geographic entities mentioned:
surface_form: Ulu Titi Basah
instance_of: Mountain
countries: Malaysia
coordinates: lat: 5.8
lon: 101.317
Lake Whitney (Connecticut). Lake Whitney is a lake in Hamden, Connecticut, that is a part of the Mill River. The lake was a water source for the New Haven, Connecticut, metro area, until its associated treatment plant became antiquated in the 1990s. A new water treatment facility was constructed in the early 2000s rated for up to 15 million gallons per day.

Geographic entities mentioned:
surface_form: lake whitney
instance_of: Lake
countries: United States
coordinates: lat: 41.352
lon: -72.911
The lake was a water source for the New Haven, Connecticut, metro area, until its associated treatment plant became antiquated in the 1990s. A new water treatment facility was constructed in the early 2000s rated for up to 15 million gallons per day. Lake Whitney now serves as one of four primary sources of surface water for the RWASouth Central Connecticut Regional Water Authority.

Geographic entities mentioned:
surface_form: lake whitney
instance_of: Lake
countries: United States
coordinates: lat: 41.352
lon: -72.911
Residents of these desert cities and unincorporated communities share Sierra Highway, Angeles Forest Highway, Angeles Crest Highway (State Route 2), and the Antelope Valley Freeway (State Route 14) for commutes to the San Fernando Valley and Los Angeles Basin in order to get to work.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In most varieties of Swedish that use an alveolar (in particular, the central and northern forms), the combination of with dental consonants () produces retroflex consonant realizations (), a recursive sandhi process called &quot;retroflexion&quot;. Thus, ('map') is realized as, ('north') as, ('Vänern') as, and ('fresh') as. The process of retroflexion is not limited to just one dental, and e.g.

Geographic entities mentioned:
surface_form: Vänern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.916666666667
lon: 13.5
The movement to form the new county began in 2005 with a letter to &quot;The Washington Post&quot;. Under the proposal, the area of Loudoun County west of the Catoctin Mountain watershed, known as the Loudoun Valley would be separated from the portion of the county east of that watershed. The eastern portion of Loudoun would retain its name and county government.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
surface_form: Loudoun Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.2329
lon: -77.735
The eastern portion of Loudoun would retain its name and county government. Purcellville would become the seat of the new county's government. Its name is derived from the Catoctin Mountain whose watershed would make its eastern border and Catoctin Creek which flows through its proposed boundary.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Kennaway Lake. Kennaway Lake () is a small lake in the municipality of Dysart et al, Haliburton County in Central Ontario, Canada. It is in the Ottawa River drainage basin. Geography. Kennaway Lake has an area of and lies at an elevation of. It is long and wide. The nearest named community is Kennaway, to the north. There are no inflows.

Geographic entities mentioned:
surface_form: kennaway lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.13777777777778
lon: -78.175
It may have been built on the site of a much older sanctuary. The temple from the year 161 AD was dedicated to Zeus Bomos (&quot; Zeus, the altar&quot;), a local name for the main Syrian god Baal. Zeus' temples were often built on mountains; another was in close proximity on the summit of Jebel Sheikh Baraqat (south of Refade), and several around the summit of Hermon.

Geographic entities mentioned:
surface_form: Hermon
instance_of: Mountain
countries: Lebanon
Israel
Syria
coordinates: lat: 33.4
lon: 35.85
It is present in the Canadian Rockies of Alberta and British Columbia. First defined by A. McGugan in 1963, it is named for Mount Ishbel of the Sawback Range in Banff National Park, and parts of the group were first described in the vicinity of the mountain at Ranger Canyon and Johnston Canyon. Lithology.

Geographic entities mentioned:
surface_form: Mount Ishbel
instance_of: Mountain
countries: Canada
coordinates: lat: 51.26555555555556
lon: -115.77527777777777
Ch'uxña Quta (Loayza). Ch'uxña Quta (Aymara &quot;ch'uxña&quot; green, &quot;quta&quot; lake, &quot;green lake&quot;, Hispanicized spelling &quot;Chojñakhota, Chojna Khota, Chojna Kkota, Chojña Kkota&quot;) is a mountain in the Bolivian Andes, about 4,920 metres (16,142 ft) high. It lies in the Kimsa Cruz mountain range, west of Wallatani Lake.

Geographic entities mentioned:
surface_form: Wallatani Lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.008333333333333
lon: -67.34722222222223
surface_form: wallatani lake
instance_of: Lake
countries: Bolivia
coordinates: lat: -17.008333333333333
lon: -67.34722222222223
Ch'uxña Quta (Loayza). Ch'uxña Quta (Aymara &quot;ch'uxña&quot; green, &quot;quta&quot; lake, &quot;green lake&quot;, Hispanicized spelling &quot;Chojñakhota, Chojna Khota, Chojna Kkota, Chojña Kkota&quot;) is a mountain in the Bolivian Andes, about 4,920 metres (16,142 ft) high. It lies in the Kimsa Cruz mountain range, west of Wallatani Lake.

Geographic entities mentioned:
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.7425
lon: -68.5806
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.12861111
lon: -69.15333333
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.48611111111111
lon: -67.92916666666666
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.014166666666666
lon: -69.09083333333334
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8775
lon: -68.9731
surface_form: ch'uxña quta (loayza)
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17
lon: -67.38333333
Ch'uxña Quta (Loayza). Ch'uxña Quta (Aymara &quot;ch'uxña&quot; green, &quot;quta&quot; lake, &quot;green lake&quot;, Hispanicized spelling &quot;Chojñakhota, Chojna Khota, Chojna Kkota, Chojña Kkota&quot;) is a mountain in the Bolivian Andes, about 4,920 metres (16,142 ft) high. It lies in the Kimsa Cruz mountain range, west of Wallatani Lake.

Geographic entities mentioned:
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -15.7425
lon: -68.5806
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.12861111
lon: -69.15333333
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -16.48611111111111
lon: -67.92916666666666
surface_form: ch'uxña quta
instance_of: Lake
countries: Bolivia
coordinates: lat: -15.014166666666666
lon: -69.09083333333334
surface_form: ch'uxña quta
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.8775
lon: -68.9731
Course. The Huai River originates in Tongbai Mountain in Henan province. It flows through southern Henan, northern Anhui, and northern Jiangsu where it pools into Lake Hongze. Nowadays the Huai River then runs southwards as the Sanhe River by way of the Gaoyou Lake and Shaobo Lake, emptying into the Yangtze River at Sanjiangying (三江营) near Yangzhou.

Geographic entities mentioned:
surface_form: Gaoyou Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.83333333
lon: 119.33333333
surface_form: Shaobo Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 32.61666667
lon: 119.43333333
Aberbargoed Grasslands. Aberbargoed Grasslands is a Site of Special Scientific Interest in the Rhymney Valley in Mid & South Glamorgan, South Wales. The area was designated a national nature reserve in 2012 largely due to its population of marsh fritillary butterflies. It is managed by Caerphilly County Borough. Geography.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
It is managed by Caerphilly County Borough. Geography. The site covers an area of of the Rhymney Valley, located on a southwest-facing slope, roughly from Bargoed. Parts of the site had previously been used as farmland. Due to the site never being routinely drained, the wet grasslands area has produced a fertile breeding ground for wildlife.

Geographic entities mentioned:
surface_form: Rhymney Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.697777777778
lon: -3.2294444444444
It is part of the Pamir-Alay mountain system. The range runs approximately east to west. Its highest summit is Pik Tandykul (), reaching 5544 m. It forms the southern border of the Fergana Valley, and in the south it falls steeply to the Alay Valley. The southern slopes of the range drain into the Kyzylsuu or Vakhsh River, a tributary of the Amu Darya.

Geographic entities mentioned:
surface_form: Pik Tandykul
instance_of: Mountain
countries: Kyrgyzstan
Tajikistan
coordinates: lat: 39.44833333
lon: 71.08333333
It is part of the Pamir-Alay mountain system. The range runs approximately east to west. Its highest summit is Pik Tandykul (), reaching 5544 m. It forms the southern border of the Fergana Valley, and in the south it falls steeply to the Alay Valley. The southern slopes of the range drain into the Kyzylsuu or Vakhsh River, a tributary of the Amu Darya.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
surface_form: Alay Valley
instance_of: Valley
countries: Kyrgyzstan
coordinates: lat: 39.666666666667
lon: 72.966666666667
Some imprecise sources seem to use the term for the whole southern curve of the Tian Shan corresponding to the southern border of Kyrgyzstan, to up north until the perpendicular extension known as Fergana Range, but strictly speaking the Alay Mountains are strictly north of Alay Valley, while confusingly, Trans-Alay Range of Pamir Mountains lies to the south of that valley, as well as Turkestan Range and Zarafshan Range at far southwest.

Geographic entities mentioned:
surface_form: Alay Valley
instance_of: Valley
countries: Kyrgyzstan
coordinates: lat: 39.666666666667
lon: 72.966666666667
Mosambik Lake. Mosambik Lake is a lake in the Lake Superior drainage basin in Algoma District, Ontario, Canada. It is about long and wide and lies at an elevation of. The primary inflow is the Magpie River from North Wejinabikun Lake on the west side of the lake, and there are several unnamed creek inflows, including one from Kabiskagami Lake on the southwest side.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The primary inflow is the Magpie River from North Wejinabikun Lake on the west side of the lake, and there are several unnamed creek inflows, including one from Kabiskagami Lake on the southwest side. The primary outflow is also the Magpie River, which flows downstream from the north end of the lake towards Esnagi Lake, and eventually into Lake Superior.

Geographic entities mentioned:
surface_form: Esnagi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.61666666666667
lon: -84.55
The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the ninth-highest mountain in Tasmania, and is one of the summits of Cradle Mountain. The peak is composed of dolerite columns, similar to many of the other mountains in the area and rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. Cradle Mountain has four named summits.

Geographic entities mentioned:
surface_form: Cradle Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
Smithies Peak. The Smithies Peak, sometimes incorrectly called Smithies Towers, is a mountain in the Central Highlands region of Tasmania, Australia. The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the ninth-highest mountain in Tasmania, and is one of the summits of Cradle Mountain.

Geographic entities mentioned:
surface_form: lake st clair
instance_of: Lake
countries: Australia
coordinates: lat: -42.066666666667
lon: 146.16666666667
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
The peak is composed of dolerite columns, similar to many of the other mountains in the area and rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. Cradle Mountain has four named summits. In order of height they are Cradle Mountain (); Smithies Peak; Weindorfers Tower (); and Little Horn ().

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
The peak is composed of dolerite columns, similar to many of the other mountains in the area and rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. Cradle Mountain has four named summits. In order of height they are Cradle Mountain (); Smithies Peak; Weindorfers Tower (); and Little Horn ().

Geographic entities mentioned:
surface_form: cradle mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -41.684644444444
lon: 145.951275
surface_form: smithies peak
instance_of: Mountain
countries: Australia
coordinates: lat: -41.68
lon: 145.95
Smithies Peak. The Smithies Peak, sometimes incorrectly called Smithies Towers, is a mountain in the Central Highlands region of Tasmania, Australia. The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the ninth-highest mountain in Tasmania, and is one of the summits of Cradle Mountain.

Geographic entities mentioned:
surface_form: smithies towers
instance_of: Mountain
countries: Australia
coordinates: lat: -41.68
lon: 145.95
surface_form: smithies peak
instance_of: Mountain
countries: Australia
coordinates: lat: -41.68
lon: 145.95
Smithies Peak. The Smithies Peak, sometimes incorrectly called Smithies Towers, is a mountain in the Central Highlands region of Tasmania, Australia. The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the ninth-highest mountain in Tasmania, and is one of the summits of Cradle Mountain.

Geographic entities mentioned:
surface_form: smithies peak
instance_of: Mountain
countries: Australia
coordinates: lat: -41.68
lon: 145.95
The mountain is situated in the Cradle Mountain-Lake St Clair National Park. At above sea level, it is the ninth-highest mountain in Tasmania, and is one of the summits of Cradle Mountain. The peak is composed of dolerite columns, similar to many of the other mountains in the area and rises above the glacially formed Dove Lake (), Lake Wilks and Crater Lake. Cradle Mountain has four named summits.

Geographic entities mentioned:
surface_form: dove lake
instance_of: Lake
countries: Australia
coordinates: lat: -41.658055555556
lon: 145.96194444444
The main rock formations in the stream's watershed are the Mauch Chunk Formation, the Spechty Kopf Formation, the Pocono Formation, and the Buddys Run Member of the Catskill Formation. Course. Long Hollow begins on Catawissa Mountain in Roaring Creek Township. It flows east for a few tenths of a mile. The stream then enters Beaver Township.

Geographic entities mentioned:
surface_form: Catawissa Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.9199
lon: -76.3168
Cirque Mountain. Cirque Mountain is a mountain located northeast of Mount Caubvick, in Labrador, Canada. It is the third-highest mountain in Labrador, after Caubvick (1,652 m) and Torngarsoak Mountain (1,595 m), and lies in the Selamiut Range, which is a subrange of the Torngat Mountains.

Geographic entities mentioned:
surface_form: Mount Caubvick
instance_of: Mountain
countries: Canada
coordinates: lat: 58.8877
lon: -63.7097
surface_form: cirque mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.9336
lon: -63.5492
Cirque Mountain. Cirque Mountain is a mountain located northeast of Mount Caubvick, in Labrador, Canada. It is the third-highest mountain in Labrador, after Caubvick (1,652 m) and Torngarsoak Mountain (1,595 m), and lies in the Selamiut Range, which is a subrange of the Torngat Mountains.

Geographic entities mentioned:
surface_form: Torngarsoak Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.9503
lon: -63.7992
Cirque Mountain. Cirque Mountain is a mountain located northeast of Mount Caubvick, in Labrador, Canada. It is the third-highest mountain in Labrador, after Caubvick (1,652 m) and Torngarsoak Mountain (1,595 m), and lies in the Selamiut Range, which is a subrange of the Torngat Mountains.

Geographic entities mentioned:
surface_form: cirque mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.9336
lon: -63.5492
It is the third-highest mountain in Labrador, after Caubvick (1,652 m) and Torngarsoak Mountain (1,595 m), and lies in the Selamiut Range, which is a subrange of the Torngat Mountains. Before 1971, it was believed that Cirque Mountain was the highest peak in Canada east of the Rocky Mountains and south of Baffin Island; that distinction is now known to belong to Mount Caubvick.

Geographic entities mentioned:
surface_form: cirque mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 58.9336
lon: -63.5492
A domed mountain, it lies at the heart of a vast roadless area. It is possible to reach the peak from Glen Tilt or via the Linn of Dee by mountain bike. It is the triple point between the catchment area of three rivers: the River Dee, the River Spey and the River Tay.

Geographic entities mentioned:
surface_form: Glen Tilt
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.833
lon: -3.776
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
Carn an Fhidhleir. Carn an Fhidhleir (994 m) is a mountain in the Grampian Mountains of Scotland. It lies on the border of Inverness-shire, Perthshire and Aberdeenshire, in one of the most remote areas of Scotland between the Cairngorms and the Mounth. A domed mountain, it lies at the heart of a vast roadless area.

Geographic entities mentioned:
surface_form: carn an fhidhleir
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.935874
lon: -3.801675
The gross area reaches 120 square kilometers, while the protection area reaches 114 square kilometers. Shiwang Peak is the highest one with an elevation of 1342 meters above sea level. Together with Wutai Mountain in Shanxi, Emei Mountain in Sichuan and Putuo Mountain in Zhejiang. Jiuhua Mountain is called one of the four great Buddhist mountains in China.

Geographic entities mentioned:
surface_form: emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
It is one of the four famous Buddhist mountains in China, one of the first batch of 5A level scenic spots in China, one of the first batch of natural and cultural heritage sites in China, and the main scenic spot of &quot;two mountains and one lake&quot; (Jiuhua Mountain, Taiping Lake, Huangshan) tourism development strategy in Anhui Province.

Geographic entities mentioned:
surface_form: taiping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.36
lon: 118
Mount Jiuhua. Mount Jiuhua () located in Chizhou, Anhui Province in China is an important Buddhist site and natural scenic spot.

Geographic entities mentioned:
surface_form: mount jiuhua
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.482222
lon: 117.804444
History. Mount Jiuhua was called Mount Lingyang during the time of the Han dynasty. It was called Mount Jiuzi (九子山) during the Liang and Chen dynasties of the South Dynasties period. A legend says that the great poet Li Bai of the Tang dynasty travelled here and wrote &quot;Magic is divided to two branches, sacred mountain generates nine glories.&quot; (), giving rise to its name Mount Jiuhua.

Geographic entities mentioned:
surface_form: mount jiuhua
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.482222
lon: 117.804444
surface_form: mount jiuhua
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 30.482222
lon: 117.804444
The North East railway line then continues through northern Victoria to Melbourne. There are six tunnels on the line: the Picton tunnel, the Yerrinbool tunnel, the Aylmerton tunnel, the Gib (Mt Gibraltar) tunnel, and the two &quot;up&quot; track tunnels in the Bethungra Spiral. The line north of Macarthur is maintained by the Transport Asset Holding Entity.

Geographic entities mentioned:
surface_form: Mt Gibraltar
instance_of: Mountain
countries: Australia
coordinates: lat: -34.465333333333
lon: 150.42826666667
Montechino. Montechino is a hamlet of forty inhabitants. It is a frazione of the comune of Gropparello, in the province of Piacenza, in Emilia-Romagna, Italy. Geography. Montechino lies in the Val Riglio, part of the Val Nure. The village is above sea level, from Gropparello and from Piacenza. History. For centuries, the feudal lords of the Nicelli family ruled much of the Val Nure.

Geographic entities mentioned:
surface_form: Val Nure
instance_of: Valley
countries: Italy
coordinates: lat: 44.7
lon: 9.56667
Geography. Kawakami is located in mountainous eastern Nagano Prefecture, bordered by Yamanashi Prefecture to the south, Gunma Prefecture to the north and Saitama Prefecture to the east. Mount Kinpu (2499 meters) is partly located within this village. The source of the Chikuma River, the longest river in Japan, is in Kawakami.

Geographic entities mentioned:
surface_form: Mount Kinpu
instance_of: Mountain
countries: Japan
coordinates: lat: 35.87166666666667
lon: 138.62527777777777
The last Ohio Electric Interurban car ran through the gorge on February 15, 1929. Dillon Dam (1961). Construction of Dillon Dam began in June 1946, but work was halted due to lack of funds, and then a shortage of materials due to the outbreak of the Korean War. Construction on the dam resumed in 1958 and it was completed in June 1961.

Geographic entities mentioned:
surface_form: Dillon Dam
instance_of: Lake
countries: United States
coordinates: lat: 40.0026127
lon: -82.0966435