Sarmila/GeoWiki-Features huggingface dataset:
With its wide expanse through the heart of the San Fernando Valley, Van Nuys Boulevard became known from the 1950s through the 1970s as a center of teenage cruising. Its car culture was celebrated in several motion pictures, including &quot;Van Nuys Boulevard&quot;.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Wadi Hamra (Gilf Kebir). Wadi Hamra (, &quot;red valley&quot;) is a valley of Gilf Kebir, in New Valley Governorate in the extreme south-west of Egypt. It is known for its vegetation and rock encarvings. Geography.

Geographic entities mentioned:
surface_form: wadi hamra
instance_of: Valley
countries: Egypt
coordinates: lat: 23.852222222222
lon: 25.451111111111
It is situated in the Arequipa Region, La Unión Province, Puyca District, and in the Cusco Region, Chumbivilcas Province, Santo Tomás District. It lies northwest of Qullpa and north of Pichaqani.

Geographic entities mentioned:
surface_form: pichaqani
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7808
lon: -72.4897
surface_form: pichaqani
instance_of: Mountain
countries: Peru
coordinates: lat: -15.3142
lon: -70.8392
Kuntur K'uchu. Kuntur K'uchu (Quechua &quot;kuntur&quot; condor, &quot;k'uchu&quot; corner, &quot;condor corner&quot;, Hispanicized spelling &quot;Condorcucho&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high. It is situated in the Arequipa Region, La Unión Province, Puyca District, and in the Cusco Region, Chumbivilcas Province, Santo Tomás District.

Geographic entities mentioned:
surface_form: condor
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: condor
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur k'uchu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7403
lon: -72.4867
Kuntur K'uchu. Kuntur K'uchu (Quechua &quot;kuntur&quot; condor, &quot;k'uchu&quot; corner, &quot;condor corner&quot;, Hispanicized spelling &quot;Condorcucho&quot;) is a mountain in the Wansu mountain range in the Andes of Peru, about high. It is situated in the Arequipa Region, La Unión Province, Puyca District, and in the Cusco Region, Chumbivilcas Province, Santo Tomás District.

Geographic entities mentioned:
surface_form: kuntur
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4156
lon: -72.0636
surface_form: kuntur k'uchu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.7403
lon: -72.4867
Rural civil parishes. The civil parish of Foz do Arelho has a beach on the Atlantic Ocean, from the centre of town. The Lagoa de Óbidos, which straddles the border with the municipality of Óbidos, is a lagoon that empties into the Atlantic Ocean near Foz do Arelho. The ocean beach and the lagoon beach have each been awarded a Blue Flag by the Foundation for Environmental Education.

Geographic entities mentioned:
surface_form: Lagoa de Óbidos
instance_of: Lake
countries: Portugal
coordinates: lat: 39.40969
lon: -9.20775
Lake Pepin. Lake Pepin () is a naturally occurring lake on the Mississippi River on the border between the U.S. states of Minnesota and Wisconsin. It is located in a valley carved by the outflow of an enormous glacial lake at the end of the last Ice Age.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
The lake formed when the Mississippi, a successor to the glacial river, was partially dammed by a delta from a tributary stream and spread out across the ancient valley. It is the 4th largest lake in Wisconsin. Lake Pepin is now a corridor for water, highway, and rail transportation. Known as the birthplace of water skiing, it hosts a variety of recreational activities. Geography.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Geography. Lake Pepin has a surface area of about and an average depth of, It is up to 2 miles (3.2 km) wide and
The wide area of the lake stretches from Bay City, Wisconsin, in the north, down to Reads Landing, Minnesota, in the south. The villages of Pepin, Maiden Rock, and Stockholm are on the Wisconsin side, while Frontenac State Park takes up a large part of the Minnesota side.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Geography. Lake Pepin has a surface area of about and an average depth of, It is up to 2 miles (3.2 km) wide and
The wide area of the lake stretches from Bay City, Wisconsin, in the north, down to Reads Landing, Minnesota, in the south. The villages of Pepin, Maiden Rock, and Stockholm are on the Wisconsin side, while Frontenac State Park takes up a large part of the Minnesota side.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
Lakeside highways are U.S. Route 61 on the Minnesota side, and across the lake Wisconsin State Highway 35 is just inland from the railroad. Both are National Scenic Byways and parts of the Great River Road. Maiden Rock, on Lake Pepin, is one site said to be the locale where a Dakota woman named Winona leapt to her death. Geology.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
The lake backed up behind this sediment dam as far north as the location of Saint Paul. In the 10,000 years since the lake's creation, ongoing sedimentation into Lake Pepin has caused its upper end to migrate downstream some 80 km (50 mi) to its present location east (river direction south) of Red Wing, Minnesota. Ecology.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Pepin's natural flora are threatened by these increased rates of sedimentation, leading the Lake Pepin Legacy Alliance to call the phenomenon a &quot;wet desert.&quot; Some theorize the lake is filling in at a rate of ten times greater than pre-colonization, due largely to increased run-off from farms along the Minnesota River.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Popular culture. Pepin, Wisconsin, is the birthplace of author Laura Ingalls Wilder. In &quot;Little House in the Big Woods&quot;, the first book in her &quot;Little House&quot; series, Laura's father visits Lake Pepin in the first chapter and her family visits the lake in the &quot;Going to Town&quot; chapter.

Geographic entities mentioned:
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.4982
lon: -92.3013
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
surface_form: lake pepin
instance_of: Lake
countries: United States
coordinates: lat: 44.473333333333
lon: -93.592222222222
Ansan (Gangwon). Ansan () is a mountain in Inje County, Gangwon Province, South Korea. It is in the north-western area of Seoraksan National Park. It has an elevation of.

Geographic entities mentioned:
surface_form: ansan (gangwon)
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.14
lon: 128.33
Ansan (Gangwon). Ansan () is a mountain in Inje County, Gangwon Province, South Korea. It is in the north-western area of Seoraksan National Park. It has an elevation of.

Geographic entities mentioned:
surface_form: ansan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.14
lon: 128.33
During the last two weeks of February 2017, filming locations for &quot;A Wrinkle in Time&quot; were in Central Otago, New Zealand. Actors and crew were in New Zealand for two weeks to shoot scenes in the Southern Alps, including at Hunter Valley Station near Lake Hāwea, with cast and crew treated to a traditional Māori pōwhiri and karakia.

Geographic entities mentioned:
surface_form: Lake Hāwea
instance_of: Lake
countries: New Zealand
coordinates: lat: -44.5
lon: 169.28333333333
The sinkhole is named after the reddish-brown colour of the surrounding cliffs, coloured by iron oxides. Like the nearby Blue Lake, it is presumed that the lake emerged when the ceiling of a large cave hall collapsed. The lake is inhabited with endemic and endangered spotted minnow (&quot;Delminichthys adspersus&quot;) and Imotski spined loach (&quot;Cobitis illyrica&quot;).

Geographic entities mentioned:
surface_form: blue lake
instance_of: Lake
countries: Croatia
coordinates: lat: 43.45079
lon: 17.21033
Red Lake (Croatia). Red Lake () is a sinkhole containing a karst lake near the city of Imotski, Croatia. It is known for its numerous caves and high cliffs, reaching over above normal water level and continuing below the water level.

Geographic entities mentioned:
surface_form: red lake (croatia)
instance_of: Lake
countries: Croatia
coordinates: lat: 43.454444444444
lon: 17.198888888889
Red Lake (Croatia). Red Lake () is a sinkhole containing a karst lake near the city of Imotski, Croatia. It is known for its numerous caves and high cliffs, reaching over above normal water level and continuing below the water level.

Geographic entities mentioned:
surface_form: red lake
instance_of: Lake
countries: Croatia
coordinates: lat: 43.454444444444
lon: 17.198888888889
The lake is inhabited with endemic and endangered spotted minnow (&quot;Delminichthys adspersus&quot;) and Imotski spined loach (&quot;Cobitis illyrica&quot;). In the dry period of the year, this fish can be occasionally seen in surrounding springs, rivers and lakes, suggesting that there is an underground connection between Red Lake and other water bodies.

Geographic entities mentioned:
surface_form: red lake
instance_of: Lake
countries: Croatia
coordinates: lat: 43.454444444444
lon: 17.198888888889
Queen Charlotte (1810 ship). &quot;Queen Charlotte&quot; was the ship-rigged ship-sloop constructed for the Upper Canada Provincial Marine in 1810 as part of the fleet renewal in the lead-up to the War of 1812. Ordered in 1809, the ship was designed by Master Shipwright William Bell and constructed at Amherstburg Royal Naval Dockyard in Amherstburg, Upper Canada on Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Description and construction. In 1809, with increased threat of war with the United States, Sir James Craig, the Governor-General of British North America ordered two ships in January 1809 as part of the fleet renewal of the Upper Canada Provincial Marine. One was to be constructed on Lake Ontario, the other on Lake Erie.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The 1st-century Roman writer Pliny the Elder and the 1st-century BCE Latin poet Horace both state that the Monte Soratte was within Faliscan territory; it likely functioned as the border between Faliscan country and Capenate territory.

Geographic entities mentioned:
surface_form: Monte Soratte
instance_of: Mountain
countries: Italy
coordinates: lat: 42.2456168
lon: 12.501944
To the west, the corners of the roughly square area were on the slopes of the Monti Sabatini in the south and the Monti Cimini in the north. Pollen samples from Lake Bracciano, Lake Monterosi and Lake Vico reveal that the montane forests, formed by oaks, were very dense until the 2nd century BC.

Geographic entities mentioned:
surface_form: Lake Vico
instance_of: Lake
countries: Italy
coordinates: lat: 42.317
lon: 12.175
The northern border of the enclosure went along the ridge of the Monti Cimini, the southern along the ridge connecting the Monti Sabatini and Monte Soratte, the western along the highlands connecting the two large volcanic lakes.

Geographic entities mentioned:
surface_form: Monte Soratte
instance_of: Mountain
countries: Italy
coordinates: lat: 42.2456168
lon: 12.501944
It was common for the clothing of young girls to be covered in metal plates sometimes adorned with swastikas. Within a Faliscan tomb on the slopes of Monte Greco are the bodies of a mother and daughter, both buried in a trench tomb. Both women wore jewelry, although mother has larger amounts of jewelry and the highest-quality jewelry.

Geographic entities mentioned:
surface_form: Monte Greco
instance_of: Mountain
countries: Italy
coordinates: lat: 41.7973
lon: 13.9943
The administrative centre of the municipality was the village of Bjelland where Bjelland Church is located. The municipality existed from 1838 until 1902. It was located in the Mandalen valley in the northern parts of the present-day municipalities of Lyngdal and Lindesnes in what is now Agder county. History.

Geographic entities mentioned:
surface_form: Mandalen
instance_of: Valley
countries: Norway
coordinates: lat: 58.38
lon: 7.52777778
Rogers Peaks. 9qy3d6ysjtstygt1sh98wj1a1bh1" xml:space="preserve">#REDIRECT Sør Rondane Mountains

Geographic entities mentioned:
surface_form: rogers peaks
instance_of: Mountain
coordinates: lat: -72.25
lon: 24.5167
Pocumtuck Mountain. Pocumtuck Mountain is a mountain peak in Charlemont, Massachusetts, located west of the abandoned Catamount settlement. Its summit ledge features wide views of western Franklin County and northern Berkshire County. Pocumtuck Mountain is often confused with the nearby Pocumtuck Range in Deerfield, Massachusetts.

Geographic entities mentioned:
surface_form: catamount
instance_of: Mountain
countries: United States
coordinates: lat: 42.1569
lon: -73.4814
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: pocumtuck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.651944444444
lon: -72.774166666667
Pocumtuck Mountain is often confused with the nearby Pocumtuck Range in Deerfield, Massachusetts. The mountain was named after the Pocumtuc Indians on October 16, 1855 during one of Catamount's Old Homes Days Festival. Such festivals were held often on the scenic mountain – including one visited by Massachusetts Governor John Davis Long.

Geographic entities mentioned:
surface_form: catamount
instance_of: Mountain
countries: United States
coordinates: lat: 42.1569
lon: -73.4814
The mountain was named after the Pocumtuc Indians on October 16, 1855 during one of Catamount's Old Homes Days Festival. Such festivals were held often on the scenic mountain – including one visited by Massachusetts Governor John Davis Long. Except for areas belonging to Catamount State forest, the ledges and surrounding land are privately owned. Trespassing for any reason is not permitted.

Geographic entities mentioned:
surface_form: catamount
instance_of: Mountain
countries: United States
coordinates: lat: 42.1569
lon: -73.4814
Pocumtuck Mountain. Pocumtuck Mountain is a mountain peak in Charlemont, Massachusetts, located west of the abandoned Catamount settlement. Its summit ledge features wide views of western Franklin County and northern Berkshire County. Pocumtuck Mountain is often confused with the nearby Pocumtuck Range in Deerfield, Massachusetts.

Geographic entities mentioned:
surface_form: pocumtuck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.651944444444
lon: -72.774166666667
Its summit ledge features wide views of western Franklin County and northern Berkshire County. Pocumtuck Mountain is often confused with the nearby Pocumtuck Range in Deerfield, Massachusetts. The mountain was named after the Pocumtuc Indians on October 16, 1855 during one of Catamount's Old Homes Days Festival.

Geographic entities mentioned:
surface_form: pocumtuck mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.651944444444
lon: -72.774166666667
As a result, it is a net oil and gas importer. The pipeline network in Romania included: 1,738 km for crude oil, 2,321 km for petroleum products and 708 km for natural gas, in 1999. Several major new pipelines are planned, especially the Nabucco Pipeline for Caspian oilfields, the longest one in the world.

Geographic entities mentioned:
surface_form: Caspian
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The main church of the municipality was Moe Church, just south of the village of Vormstad, the administrative centre of the municipality. Most of the population lived in the Orkdalen valley along the river Orklaelva and near the lake Hostovatnet. The main village areas were Vormstad, Svorkmo, and Hoston.

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
surface_form: Hostovatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.1863
lon: 9.566
On 1 January 1963, Orkland Municipality (population: 1,707) was merged with Orkanger Municipality (population: 2,874), Geitastrand Municipality (population: 559), and Orkdal Municipality (population: 4,152) to form a new, larger Orkdal Municipality. Name. The municipality is named after the Orkdalen valley (). The first element is the genitive case of the name of the river (now called Orklaelva).

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
Geography. The municipality was located in the Orkdalen valley, about southwest of the city of Trondheim. Orkdal Municipality was located to the north, Skaun Municipality and Hølonda Municipality were to the east, Meldal Municipality was to the south, and Rindal Municipality (in Møre og Romsdal county) was to the west.

Geographic entities mentioned:
surface_form: Orkdalen
instance_of: Valley
countries: Norway
coordinates: lat: 63.233333333333
lon: 9.7666666666667
Frakes, Frank B. Frakes (father of geologist Lawrence A. Frakes, the namesake of Mount Frakes in Antarctica), George H. Frakes, Samantha May Frakes, Bertha Frakes (Bittick), and Nellie Almeda Frakes. In 1903, at the age of 43, he won the wrestling championship of the Antelope Valley. Legacy. After Frank Frakes' death, his ranch eventually became the Edgewater Park Club while the land of Samuel H.

Geographic entities mentioned:
surface_form: Mount Frakes
instance_of: Mountain
coordinates: lat: -76.8
lon: -117.7
Longridge Farmhouse. Longridge Farmhouse is a historic building in Bishopdale, North Yorkshire, a valley in England. The farmhouse was built for George and Elizabeth Dodsworth, and is dated 1653, although its kitchen may be older. The building was Grade II* listed in 1969, along with its outbuilding, which appears to have originally been part of the house, and has been converted into a garage.

Geographic entities mentioned:
surface_form: Bishopdale, North Yorkshire
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
Oasis Mountain. Oasis Mountain is a summit in the U.S. state of Nevada. The elevation is. Oasis Mountain was so named for its greenish color, when viewed from afar.

Geographic entities mentioned:
surface_form: oasis mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.048
lon: -116.75312
Thompson encountered Kaúxuma next on Rainy Lake, near the Upper Columbia River, in July 1809, where he says &quot;she had set herself up for a prophetess and gradually had gained, by her shrewdness, some influence among the natives as a dreamer, and expounder of dreams.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Tyrrell. In 1823, John Franklin (of the Franklin Expedition to look for a Northwest Passage) wrote that eight years earlier (in 1815) a &quot;manlike woman&quot; had been present at Fort Chipewyan, near Lake Athabasca, whose followers believed him to possess &quot;supernatural abilities,&quot; and who predicted great change would come to Native peoples in the area.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
The &quot;daimyō&quot; is riding in a closed &quot;kago&quot; (palanquin), with a long straggling line of retainers in front and in back, some of whom are carrying his luggage. In the background is the post station, behind which are the high peaks of the Ena Mountains, indicating that the procession is heading towards home in the west.

Geographic entities mentioned:
surface_form: Ena Mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 35.443055555556
lon: 137.59694444444
Oklahoma Lake. Oklahoma Lake is located in north east Oklahoma City in the Canadian river valley and borders the North Canadian River by Westminster Road. The surface area is around with a island and the shoreline is primarily sand. The lake is fed from ground water and the water is usually calm because of the low elevation. The primary fish species are crappie, bass, and channel catfish.

Geographic entities mentioned:
surface_form: oklahoma lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6019
lon: -97.3303
Oklahoma Lake. Oklahoma Lake is located in north east Oklahoma City in the Canadian river valley and borders the North Canadian River by Westminster Road. The surface area is around with a island and the shoreline is primarily sand. The lake is fed from ground water and the water is usually calm because of the low elevation. The primary fish species are crappie, bass, and channel catfish.

Geographic entities mentioned:
surface_form: oklahoma lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6019
lon: -97.3303
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The surface area is around with a island and the shoreline is primarily sand. The lake is fed from ground water and the water is usually calm because of the low elevation. The primary fish species are crappie, bass, and channel catfish. Oklahoma Lake activities include swimming, camping, picnics, fishing, and jet-ski sports.

Geographic entities mentioned:
surface_form: oklahoma lake
instance_of: Lake
countries: United States
coordinates: lat: 35.6019
lon: -97.3303
Descending to the southwest onto the playa in the north end of Animas Valley the cutoff route passed to the west through Stein's Pass, then southwest of its mouth to the Cienega of San Simon on the San Simon River. The cutoff then ran west through Puerto del Dado, from there it crossed the middle Sulphur Springs Valley and Willcox Playa to Croton Springs.

Geographic entities mentioned:
surface_form: Animas Valley
instance_of: Valley
countries: United States
Mexico
coordinates: lat: 31.9489
lon: -108.807
Descending to the southwest onto the playa in the north end of Animas Valley the cutoff route passed to the west through Stein's Pass, then southwest of its mouth to the Cienega of San Simon on the San Simon River. The cutoff then ran west through Puerto del Dado, from there it crossed the middle Sulphur Springs Valley and Willcox Playa to Croton Springs.

Geographic entities mentioned:
surface_form: Sulphur Springs Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.4987
lon: -110.031
Who's on Top? &quot;Who's on Top?&quot; is the debut documentary directed by Taiwanese American filmmaker Devin Fei-Fan Tau about four queer athletes who climb Mount Hood, in the U.S. state of Oregon. The 2020 film is narrated by George Takei. Release. &quot;Who's on Top?&quot; was shown during the Northwest Film Center's 2021 Portland International Film Festival.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
state of Oregon. The 2020 film is narrated by George Takei. Release. &quot;Who's on Top?&quot; was shown during the Northwest Film Center's 2021 Portland International Film Festival. The film was made available on multiple streaming services on May 18, 2021, the 41st anniversary of the eruption of Mount St. Helens. Reception.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Cyprinus qionghaiensis. &quot;Cyprinus qionghaiensis&quot; is a critically endangered species of fish in the genus &quot;Cyprinus&quot; from Qiong Lake in Yunnan, China.

Geographic entities mentioned:
surface_form: Qiong Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 27.82149
lon: 102.31019
British Columbia Highway 18. Highway 18 is a short main vehicle route in the Cowichan Valley Regional District on Vancouver Island, connecting the city of Duncan on the Trans-Canada Highway with the community of Lake Cowichan, on the shore of Cowichan Lake. The highway first opened to vehicle traffic in 1953, and was re-routed to a straighter and wider alignment in 1970.

Geographic entities mentioned:
surface_form: Cowichan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.875
lon: -124.26
In March 1751, electing to enlarge his Irish estate (he had inherited his father’s Curraghmore property and, in 1735, had bought the late Sir Henry Caldwell’s house at Ballyshannon), he purchased the extensive holdings of the insolvent Everard family in and around the town of Fethard, County Tipperary, for £30,500 and somewhat later he acquired several properties in County Fermanagh from Sir James Caldwell and spent £19,500 buying the Kilmore estate of 15,500 acres on the north-east side of Lough Erne.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Zhuye Lake. Zhuye Lake () is the terminal lake of the Shiyang River, which is located in the east of the Hexi Corridor in Gansu Province, China. Zhuye Lake is located in the marginal area of the Asian monsoon and is affected by both the Asian monsoon system and the Westerly jet.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Zhuye Lake () is the terminal lake of the Shiyang River, which is located in the east of the Hexi Corridor in Gansu Province, China. Zhuye Lake is located in the marginal area of the Asian monsoon and is affected by both the Asian monsoon system and the Westerly jet. By understanding the Holocene record in Zhuye Lake, the interaction of different climate systems during the Holocene can be studied.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
At the same time, the Asian monsoon system is climatically dynamic; changes in its sphere of influence can result in severe drought or flood over large, densely populated, regions. In addition, Zhuye Lake and the surrounding area in arid NW China are in ecological imbalance – a consequence of human impacts and climate.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
In addition, Zhuye Lake and the surrounding area in arid NW China are in ecological imbalance – a consequence of human impacts and climate. Understanding the environmental history here can assist climatological forecasting of the Asian monsoon system and ecosystem reconstruction. Reference guide of the Late Quaternary climate change for Zhuye Lake and the Hexi Corridor.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Reference guide of the Late Quaternary climate change for Zhuye Lake and the Hexi Corridor. Zhuye Lake and the Hexi Corridor are located in the northern edge of the Qinghai-Tibetan Plateau, on the northern side of the Qilian Mountains, while in a transition zone between the Gobi Desert and highland. The area is in the northwest margin of the Asian summer monsoon.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
surface_form: tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: qinghai-tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
surface_form: qinghai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
The reference guide is designed to organize literatures in relevant disciplines, which is good for scientists to understand the late Quaternary environments easily, while the guide also represents the research progress of Lanzhou University on the late Quaternary environments. Millennial-scale environmental changes in Zhuye Lake, northwest China.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Millennial-scale environmental changes in Zhuye Lake, northwest China. Lake records from Zhuye Lake show that early Holocene was relatively humid and the mid-Holocene environment was characterized by an appropriate combination of precipitation and evaporation. An arid trend appeared during the late Holocene.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
There was a centennial-scale drought event during the mid-Holocene, which was recorded by sand layers in various locations of the lake basin. Environmental changes in Zhuye Lake are mainly affected by the evolution of the Asian summer monsoon, but also affected by the mid-latitude westerlies, reflecting the interaction of the two large circulation systems.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
This change in water conditions was related to the strong early-to-mid Holocene Asian summer monsoon that brings more rainfall to this area. As a result, the runoff was high and the erosion was intensive correspondingly. This changing pattern of Holocene moisture conditions were also affected by the mid-latitude westerlies to some extent. Millennial-scale climate change cycles in Zhuye Lake.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Millennial-scale climate change cycles in Zhuye Lake. Paleoenvironmental proxies in lake sediments from Zhuye Lake show that there are distinct ~256 ~512 ~1024 climate cycles, which are consistent with millennial-scale and centennial-scale climate cycles in the typical Asian summer monsoon domain during the Holocene.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
These records from monsoon marginal zones reflected regional responses to global scale Holocene climate cycles. Mid-Holocene dry intervals in Zhuye Lake. Mid-Holocene drought events were widely recovered from lake sediments in monsoon marginal zones, but the time scales and mechanisms are still in dispute.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
The drought event could be primarily controlled by changes in the ratio of water and heat and the interaction between the summer monsoon and the westerly winds. Chronologies in Zhuye Lake. Chronologies of lake sediments in Zhuye Lake were mainly from pollen concentrates, bulk organic matter, bulk inorganic matter and mollusk shells AMS 14C and conventional 14C dating, as well as OSL dating.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Chronologies in Zhuye Lake. Chronologies of lake sediments in Zhuye Lake were mainly from pollen concentrates, bulk organic matter, bulk inorganic matter and mollusk shells AMS 14C and conventional 14C dating, as well as OSL dating. A comparison between different dating methods and results shows that the reservoir effect was relatively weak during the Holocene.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
The result is consistent with the lake sediment proxies from various sites of the lake basin. Palynological records in Zhuye Lake. Along with millennial-scale environmental and ecological changes, pollen records in Zhuye Lake reflected basin-wide vegetation history well.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Palynological records in Zhuye Lake. Along with millennial-scale environmental and ecological changes, pollen records in Zhuye Lake reflected basin-wide vegetation history well. However, affected by the complicated topography of the lake basin, there are some differences in pollen assemblages from different sites of the lake basin.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Pollen concentration was high and pollen types were rich during the mid-Holocene. A late Holocene dry tendency was also recorded by pollen assemblages in the lake. Pollen records in Zhuye Lake are consistent with other proxy records and indicate environmental changes in the lake and watershed reliably. Lithology, minerals and SEM (Scanning Electron Microscopy) analysis of quartz sands.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Lithology, minerals and SEM (Scanning Electron Microscopy) analysis of quartz sands. Lake sediment lithology, minerals and SEM (Scanning Electron Microscopy) analysis of quartz sands are also good indicators reflecting the evolution of the lake in arid regions. Lacustrine sediments in Zhuye Lake are mainly characterized by grey silts.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
The region is rich in carbonate minerals, forming a huge inorganic carbon pool. SEM analysis of quartz sands reveals that sand sediments are from diverse sources in the region. Sands in the lake have experienced both the aeolian and the lacustrine deposition processes, indicating the complicated formation processes of those sand layers. Geochemical proxies in Zhuye Lake.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Lake sediment geochemical proxies correspond well with other sediment proxies, indicating high precipitation and runoff during the early Holocene, the highest primary productivity in the mid-Holocene and an arid trend in late Holocene. Paleo-lake geomorphology of Zhuye Lake.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Paleo-lake geomorphology of Zhuye Lake. Height measurements and OSL/14C dating of paleo-shorelines in Zhuye Lake can better understand the formation and evolution of lake levels during the late Quaternary. According to field surveys, there are 9 paleo-shorelines and one lake terrace in the northeast of Zhuye Lake.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Atmospheric circulation features and the evaporation play important roles in millennial-scale lake evolution. Lake evaporation is mainly affected by relative humidity, temperature, vapor pressure and sunshine duration. According to modern observations, temperature and relative humidity have important roles in Holocene millennial-scale lake level changes at Zhuye Lake.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Further studies have shown that lake level changes are mainly controlled by many factors, and the basin-wide precipitation is the main controlling factor, but the lake evaporation and the basin-wide evapotranspiration also affect millennial-scale changes of lake area. Modern climate change processes in Zhuye Lake and monsoon marginal zones.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
The Zhuye Lake record is a typical record in monsoon marginal zones, which matches well with the simulation results, and the simulation method further explains the mechanism of the millennial-scale lake evolution.

Geographic entities mentioned:
surface_form: zhuye lake
instance_of: Lake
countries: People's Republic of China
Millennial-scale environmental changes in Yanchi Lake, northwest China. The Yanchi Lake record is consistent with paleoclimate records from typical monsoon domain and the Qinghai-Tibet Plateau, which indicates the lake expansion during the Late Glacial and early Holocene and a lake retreat during the late Holocene.

Geographic entities mentioned:
surface_form: qinghai
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 37
lon: 100
Noguera Pallaresa. The Noguera Pallaresa (;,) is a river in Catalonia, Spain. It is named after the Pallars region. Course. Its source is at &quot;Era Font d'era Noguereta&quot; in the municipality of Naut Aran (Aran Valley) at an elevation of about and barely from those of the Garonne.

Geographic entities mentioned:
surface_form: noguera pallaresa
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.9064
lon: 0.8901
Course. Its source is at &quot;Era Font d'era Noguereta&quot; in the municipality of Naut Aran (Aran Valley) at an elevation of about and barely from those of the Garonne. While the Garonne flows toward the Atlantic Ocean, the Noguera Pallaresa flows to the Segre, and enters that river from the right just before the reservoir of Camarasa (Noguera): its waters then flow to the Mediterranean.

Geographic entities mentioned:
surface_form: noguera pallaresa
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.9064
lon: 0.8901
surface_form: noguera pallaresa
instance_of: Watercourse
countries: Spain
coordinates: lat: 41.9064
lon: 0.8901
Mount Bogong is a popular backcountry skiing mountain through winter but only has snow for the mid winter-spring months. It is around by road and walking track or direct to Mount Beauty. Falls Creek and Mount Hotham ski resorts are also nearby. Camping is relatively safe below the treeline but the summit ridgeline is very exposed.

Geographic entities mentioned:
surface_form: Mount Hotham
instance_of: Mountain
countries: Australia
coordinates: lat: -36.983333333333
lon: 147.13333333333
Etymology. In the Australian Aboriginal Waywurru and Dhudhuroa languages, the mountain is named &quot;Warkwoolowler&quot;, meaning the mountain where Aboriginal people collected the &quot;boo.gong fly&quot;. Additionally, in the Dhudhuroa language the word &quot;Bugung&quot; means the brown moth, referring to &quot;Agrotis infusa&quot;. Flora and fauna.

Geographic entities mentioned:
surface_form: bugung
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
Etymology. In the Australian Aboriginal Waywurru and Dhudhuroa languages, the mountain is named &quot;Warkwoolowler&quot;, meaning the mountain where Aboriginal people collected the &quot;boo.gong fly&quot;. Additionally, in the Dhudhuroa language the word &quot;Bugung&quot; means the brown moth, referring to &quot;Agrotis infusa&quot;. Flora and fauna.

Geographic entities mentioned:
surface_form: warkwoolowler
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
Mount Bogong. Mount Bogong, located in the Alpine National Park and part of the Victorian Alps of the Great Dividing Range, is the highest mountain in Victoria, Australia, at above sea level. The Big River separates the massif of the mountain from the Bogong High Plains to the south.

Geographic entities mentioned:
surface_form: mount bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
The Big River separates the massif of the mountain from the Bogong High Plains to the south. From the nearby town of Mount Beauty to its summit, Mount Bogong rises more than, thus making it one of the highest peaks in Australia not only in terms of its elevation above sea level, but also in terms of actual base-to-summit prominence.

Geographic entities mentioned:
surface_form: mount bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
From the nearby town of Mount Beauty to its summit, Mount Bogong rises more than, thus making it one of the highest peaks in Australia not only in terms of its elevation above sea level, but also in terms of actual base-to-summit prominence. Mount Bogong is a popular backcountry skiing mountain through winter but only has snow for the mid winter-spring months.

Geographic entities mentioned:
surface_form: mount bogong
instance_of: Mountain
countries: Australia
coordinates: lat: -36.7325
lon: 147.30583333333334
Loader then dumps it into Dumper. After all the salt has been dug up, it gets loaded on a conveyor belt into a cargo ship named Selene to be taken to the public works to be used for icy roads. This was filmed in Goderich Harbour, Ontario at the Sifto Canada salt mine on Lake Huron. Groomer, a snow groomer, explains how he grooms snow at night while the ski hill is closed.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
SH-66 continues east, passing into Oklahoma City, where it becomes N.W. 39th Expressway. SH-66 has an interchange with the Kilpatrick Turnpike on the far west edge of the city. The highway passes just to the north of Lake Overholser. Near where the road crosses over the North Canadian River, the inlet to the lake, it crosses from Canadian County into Oklahoma County. N.W.

Geographic entities mentioned:
surface_form: Lake Overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
Location. The Renneckenberg lies in the Saxony-Anhalt Nature Park and the Harz National Park just under 3 kilometres north of the village of Schierke in the borough of Wernigerode. Its summit rises about 300 metres east of the &quot;Kreisstraße&quot; (county road), the K 1356 or &quot;Brockenstraße&quot;, that runs from Schierke up to the highest mountain in the Harz, the Brocken (1141.1 m).

Geographic entities mentioned:
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
Towards the south the terrain descends into the valley of the Cold Bode and the village of Schierke. To the west-southwest there is a saddle (900.6 m) on the K 1356 which links to the Heinrichshöhe (ca. 1045 m). To the west the countryside runs across to the Brocken via the &quot;Brockenbett&quot; through which the upper reaches of the Ilse flow. Description.

Geographic entities mentioned:
surface_form: Heinrichshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.789444444444
lon: 10.629166666667
surface_form: heinrichshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.789444444444
lon: 10.629166666667
West of the summit in the direction of the K 1356 and about 912 metres high is the ski hut of the Wernigerode Ski Club. At the southern end of the Renneckenberg where it transitions to the &quot;Brockenbett&quot;, the valley between the Heinrichshöhe and the Brocken to the west and the Renneckenberg to the east, on the K 1356, is the &quot;Gelber Brink&quot; (900.6 m) which is no.

Geographic entities mentioned:
surface_form: Heinrichshöhe
instance_of: Mountain
countries: Germany
coordinates: lat: 51.789444444444
lon: 10.629166666667
surface_form: Brocken
instance_of: Mountain
countries: Germany
Kingdom of Prussia
coordinates: lat: 51.800555555556
lon: 10.617222222222
surface_form: renneckenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.790555555556
lon: 10.649722222222
surface_form: renneckenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.790555555556
lon: 10.649722222222
Renneckenberg. The Renneckenberg (formerly &quot;Rennekenberg&quot;) is a mountain, roughly high, in the High Harz part of the Harz mountain range of central Germany within the borough of Wernigerode in the state of Saxony-Anhalt. Location.

Geographic entities mentioned:
surface_form: renneckenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.790555555556
lon: 10.649722222222
Towards the north-northwest the mountainsides of the Renneckenberg descend into the valley of the River Ilse; towards the northeast they lead towards the Hoher Wand (758 m) and the &quot;Ohrenklippen&quot; crags; and towards the east they drop into the valley Holtemme which rises on the mountain in the area where it transitions to the Hohnekamm (900.6 m, with its &quot;Hohneklippen&quot;) to the south-southeast.

Geographic entities mentioned:
surface_form: renneckenberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.790555555556
lon: 10.649722222222
Although two doctors came along, quinine was rarely used to treat fever that became more pronounced as they made their ascent up the river; instead, miasma was thought the main contributory reason for an epidemic of fever. Laird went up the Niger to the confluence of the Benue River (then called the Shary or Tchadda), which he was the first white man to ascend.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
Valle Po. The Valle Po (literally &quot;Po valley&quot;) is a valley of the Cottian Alps in the province of Cuneo, Piedmont, Northern Italy. Geography. The valley gives rise to the longest river in Italy, the Po, before it enters the Pianura Padana (or the Plain of the Po). It has a length of some 32 km, from Saluzzo to Crissolo, and is home to the Monviso mountain.

Geographic entities mentioned:
surface_form: Pianura Padana
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: pianura padana
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889