Sarmila/GeoWiki-Features huggingface dataset:
Chrysovitsi. Chrysovitsi () is a mountain village and a community in the municipal unit of Falanthos, Arcadia, Greece. The community includes the village Mantaiika, 5 km southeast of Chrysovitsi. Built on the slopes of Mainalo at 1,100 m, Chrysovitsi is one of the highest villages in the Peloponnese. It is a traditional settlement since November 23, 1998 (Law 908D) and its code number is 12317201.

Geographic entities mentioned:
surface_form: Mainalo
instance_of: Mountain
countries: Greece
coordinates: lat: 37.6583
lon: 22.2517
The village’s houses are all on the slope of the mountain. Allowing a great view over the valley, a green pasture – in fact a small karstic plain – kind of a typical arcadian landscape. Forest fires are a permanent threat in the Mainalo mountains. History. The settlement dates back to the 15th century.

Geographic entities mentioned:
surface_form: Mainalo
instance_of: Mountain
countries: Greece
coordinates: lat: 37.6583
lon: 22.2517
History. The reservoir was built at the end of the 19th century for the Newcastle and Gateshead Water Company. The reservoir forms part of a series of reservoirs along the A68 which are connected by tunnels and aqueducts from Catcleugh Reservoir to Whittle Dene; from where drinking water is supplied to Newcastle upon Tyne, Gateshead, and some surrounding areas.

Geographic entities mentioned:
surface_form: Whittle Dene
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 55.009
lon: -1.9
The reservoirs that form the chain are, from northwest to southeast: Catcleugh Reservoir → Colt Crag Reservoir → Little Swinburne Reservoir → Hallington Reservoirs → Whittle Dene.

Geographic entities mentioned:
surface_form: Whittle Dene
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 55.009
lon: -1.9
It is one of a series of similar formations that extend along the western edge of Kati Thanda (Lake Eyre) from Marree to Dalhousie Springs including Freeling Springs, and the Blanche Cup and the Bubbler in the Wabma Kadarbu Mound Springs Conservation Park, among others.

Geographic entities mentioned:
surface_form: Kati Thanda
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
The park covers, and was justified on the basis of preserving plant diversification. Location. The Bakossi Mountains are part of the Cameroon Line, running inland in a northeasterly direction from Mount Cameroon. The mountains have an area of about and typical elevation of to. The highest peak is Mount Kupe at.

Geographic entities mentioned:
surface_form: Mount Cameroon
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.2166666666667
lon: 9.1725
Location. The Bakossi Mountains are part of the Cameroon Line, running inland in a northeasterly direction from Mount Cameroon. The mountains have an area of about and typical elevation of to. The highest peak is Mount Kupe at. The mountains contain what may be the largest area of cloud or submontane forest in West-Central Africa.

Geographic entities mentioned:
surface_form: Mount Kupe
instance_of: Mountain
countries: Cameroon
coordinates: lat: 4.801
lon: 9.707
The valley consists of forests, lakes and agricultural land. Most of the valley is made up of the lake Maridalsvannet, which serves as the primary source of drinking water for 90% of Oslo's population. The only hydroelectric powerplant within the City of Oslo, Hammeren Hydroelectric Power Station is located at Brekke in Maridalen.

Geographic entities mentioned:
surface_form: Maridalsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.98444444
lon: 10.77833333
Maridalen. Maridalen is a valley in the north of Oslo, Norway, just above the suburb of Kjelsås. Considering that Maridalen is within the Oslo city limits, this area has a very low population density. The valley consists of forests, lakes and agricultural land.

Geographic entities mentioned:
surface_form: maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
The valley consists of forests, lakes and agricultural land. Most of the valley is made up of the lake Maridalsvannet, which serves as the primary source of drinking water for 90% of Oslo's population. The only hydroelectric powerplant within the City of Oslo, Hammeren Hydroelectric Power Station is located at Brekke in Maridalen.

Geographic entities mentioned:
surface_form: maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
The valley is a popular recreational area featuring many hiking trails, cycling tracks for summer usage, and groomed cross-country trails in winter. Both the lake and valley are protected by the community. Maridalen Church and the church ruins of the ancient St. Margaret's Church are located north of Maridalsvannet. A bus route runs along Maridalen, starting at Nydalen Subway Station. Railway.

Geographic entities mentioned:
surface_form: maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
Both the lake and valley are protected by the community. Maridalen Church and the church ruins of the ancient St. Margaret's Church are located north of Maridalsvannet. A bus route runs along Maridalen, starting at Nydalen Subway Station. Railway. The Gjøvik Railway Line passes through Maridalen. Originally, the trains stopped at three stations in the area.

Geographic entities mentioned:
surface_form: maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
Maridalen Church and the church ruins of the ancient St. Margaret's Church are located north of Maridalsvannet. A bus route runs along Maridalen, starting at Nydalen Subway Station. Railway. The Gjøvik Railway Line passes through Maridalen. Originally, the trains stopped at three stations in the area. Movatn Station (created in 1900) is an unstaffed station at Movatn.

Geographic entities mentioned:
surface_form: maridalen
instance_of: Valley
countries: Norway
coordinates: lat: 59.99333333
lon: 10.77555556
Frøylandsvatnet (Sandnes). Frøylandsvatnet is a lake in the municipality of Sandnes in Rogaland county, Norway. The lake lies on the south side of the village of Hommersåk, about northeast of the city of Sandnes. The lake empties into a small river that runs out of the north end of the lake. The river runs through Hommersåk into an arm of the Gandsfjorden.

Geographic entities mentioned:
surface_form: frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
surface_form: frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.91416667
lon: 5.86027778
René Brunelle Provincial Park is a provincial park in both the municipality of Moonbeam and the geographic Township of Gurney in Unorganized North Cochrane District, Cochrane District, in Northeastern Ontario, Canada. Established in 1957 and named in 1981 for René Brunelle, it is operated by Ontario Parks and has camping, hiking, swimming and other facilities on or near Remi Lake. Geography.

Geographic entities mentioned:
surface_form: Remi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.423333333333
lon: -82.175833333333
Established in 1957 and named in 1981 for René Brunelle, it is operated by Ontario Parks and has camping, hiking, swimming and other facilities on or near Remi Lake. Geography. The park is on the north and east shores of Remi Lake. A second, smaller, non-contiguous portion of the park is southwest of the lake in the municipality of Moonbeam.

Geographic entities mentioned:
surface_form: Remi Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.423333333333
lon: -82.175833333333
Tláhuac has experienced the fastest rate of population growth in Mexico City since the 1960s. Much of the area is former lakebed where Lake Chalco and Lake Xochimilco met, with the town of San Pedro Tláhuac originally on an island. There are still some lake areas along with four major canals and wetlands, also under conservation status.

Geographic entities mentioned:
surface_form: Lake Chalco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.267
lon: -98.983
surface_form: Lake Xochimilco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.285
lon: -99.102
The borough extends over 89.5.km2 of territory, accounting for 5.75% of Mexico City. The borough is part of the Valley of Mexico, in the Trans-Mexican Volcanic Belt that extends across central Mexico. The borough expands over much of the former Lake Chalco and Lake Xochimilco where the two connected, which were drained over the centuries since the Spanish conquest.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
The first grand operas (1828–1829). The first opera of the grand opera canon is, by common consent, Daniel Auber's &quot;La muette de Portici&quot; (1828). This tale of a revolution set in Naples in 1647, which culminates in an eruption of Mount Vesuvius into which the heroine throws herself, embodied the musical and scenic sensationalism that would become the genre's hallmark.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
Beginning in Yellowstone National Park, western Wyoming, it flows across the arid Snake River Plain of southern Idaho, the rugged Hells Canyon on the borders of Idaho, Oregon and Washington, and finally the rolling Palouse Hills of southeast Washington. It joins the Columbia River just downstream from the Tri-Cities, Washington, in the southern Columbia Basin.

Geographic entities mentioned:
surface_form: Columbia Basin
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Joined by Pacific Creek and Buffalo Fork below the dam, it meanders southward through the alpine valley of Jackson Hole situated on the plain in front of the Teton Range to the west and the Gros Ventre Range to the east. Below the town of Jackson it forms the Snake River Canyon of Wyoming, turns west and crosses into Idaho, where the Palisades Dam forms Palisades Reservoir.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
The Snake River continues flowing west, through the C. J. Strike Reservoir where it is joined from the left by the Bruneau River, then through the Morley Nelson Snake River Birds of Prey National Conservation Area before entering farmland on the western side of Idaho's Treasure Valley. Passing west of Boise, it crosses briefly into Oregon before turning north to form the Oregon–Idaho border.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
To the south are numerous small isolated mountain ranges of the Basin and Range Province, such as the Independence and Albion Mountains. To the east are more ranges of the Rockies including the Tetons and the Wind River Range; the latter includes Gannett Peak, the highest point in the Snake River basin at.

Geographic entities mentioned:
surface_form: Gannett Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.184202777778
lon: -109.65423333333
While the Snake River course beyond Jackson Hole was not directly impacted by glaciations, its landscape was dramatically changed by Ice Age flooding events. About 30,000 years ago, the climate of western North America was much wetter than today. The Great Salt Lake Basin filled with water to form the massive Lake Bonneville, about the size of modern-day Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
By the time the Americans annexed Oregon Territory in 1848, beaver were nearly extirpated across much of the Rocky Mountains. Starting in the 1840s, the Oregon Trail became well established, and thousands of settlers passed through the Snake River Plain on their way to the Willamette Valley.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Boise, initially bypassed due to a steep grade, was connected three years later. In addition to commerce, the railroad also opened the Snake River region – which just a few years ago had been seen as a remote, rough frontier – to recreation. The Union Pacific heavily promoted tourism in places like Shoshone Falls, Payette Lake and Soda Springs, Idaho.

Geographic entities mentioned:
surface_form: Payette Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.95
lon: -116.085
Snake River sockeye once numbered to up 150,000 adults. Between 24,000 and 30,000 sockeye returned to Wallowa Lake in the Grande Ronde River watershed, but the run was eliminated by 1905 due to overharvest and unscreened irrigation diversions. The Payette Lake population once numbering up to 100,000 was blocked by the Black Canyon Dam in 1924.

Geographic entities mentioned:
surface_form: Payette Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.95
lon: -116.085
The population was 2,602 at the 2010 census, out of 6,240 in the entire town of Oakland. Geography. The CDP is in northern Kennebec County, in the eastern part of the town of Oakland at. It sits along Messalonskee Stream at the outlet of Messalonskee Lake. The village center is on the north side of the stream, but developed land exists on both sides.

Geographic entities mentioned:
surface_form: Messalonskee Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.4780812
lon: -69.7900748
The river Danube and its tributaries overflowed in many places, flooding parts of Germany, Bavaria in particular. Several floodings and landslides were reported in Lower Austria and Styria. The floods also meant the temporary closure of many mountain passes, amongst them the Gotthard in Switzerland, and the Arlberg in Austria. On a section of the Arlberg, the road and rail were washed away.

Geographic entities mentioned:
surface_form: Arlberg
instance_of: Mountain
countries: Austria
coordinates: lat: 47.13
lon: 10.211
Haute-Savoie. Haute-Savoie () is a department in the Auvergne-Rhône-Alpes region of Southeastern France, bordering both Switzerland and Italy. Its prefecture is Annecy. To the north is Lake Geneva; to the south and southeast are Mont Blanc and the Aravis mountain range. It holds its name from the Savoy historical region, as does the department of Savoie, located south of Haute-Savoie.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Geography. Haute-Savoie comprises four arrondissements, divided into 279 communes and 17 cantons. To the north, it borders the Swiss canton of Geneva and Lake Geneva; to the east the Swiss canton of Valais and Italy's Aosta Valley; to the west the French department of Ain; and to the south the department of Savoie.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
To the north, it borders the Swiss canton of Geneva and Lake Geneva; to the east the Swiss canton of Valais and Italy's Aosta Valley; to the west the French department of Ain; and to the south the department of Savoie. Haute-Savoie has the largest range of elevations of all the departments in France; the lowest point is in the Rhône Valley, and the highest Mont Blanc at.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Lakes. Haute-Savoie has significant freshwater resources. Lake Annecy is a major attraction, along with the town of Évian-les-Bains, perhaps the best-known town on the French shore of Lake Geneva, and known worldwide for its Evian mineral water. Haute-Savoie is entirely within the watershed of the Rhone. Agriculture.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
One of Ortegon HighWalking's early projects focused on creating paired paintings, one of which would depict a Native American woman and the other of which depicted where the subject lived. She painted a mural in Denver's River North Art District depicting Mount Blue Sky (at the time Mount Evans), with &quot;Evans&quot; crossed out and replaced with &quot;Blue Sky&quot;. Dance.

Geographic entities mentioned:
surface_form: Mount Blue Sky
instance_of: Mountain
countries: United States
coordinates: lat: 39.5883
lon: -105.644
A video of Ortegon HighWalking dancing jingle dress was included in Jeffrey Gibson's exhibit &quot;the space in which to place me&quot; at the United States pavilion at the 2024 Venice Biennale. In July 2024, Ortegon HighWalking was included in the exhibition Elemental Landscapes at History Jackson Hole in Jackson Hole, Wyoming. Personal life. She is married to Jason HighWalking.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Also known in the video games and interactive film industries as “Dai”. He is the co-founder and CEO of video game and interactive film developer and publisher Wales Interactive. Biography. Banner was born on 1 November 1972 in Rhondda, Wales. He attended Treorchy Comprehensive School and Tonypandy Comprehensive School, then Mid Glamorgan Centre for Art, Design and Technology.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Prior to the recording in the United States, the band recorded several demos of the songs from the album during a retreat to Cajón del Maipo in Chile. The album spawned the singles &quot;Bolsa de Mareo&quot;, &quot;Olor a Gas&quot; and &quot;La Torre de Babel&quot;.

Geographic entities mentioned:
surface_form: Cajón del Maipo
instance_of: Valley
countries: Chile
coordinates: lat: -33.633333333333
lon: -70.35
Washington is the second most populous state on the West Coast and in the Western United States, after California. Mount Rainier, an active stratovolcano, is the state's highest elevation at, and is the most topographically prominent mountain in the contiguous U.S.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Britain and the United States agreed to what has since been described as &quot;joint occupancy&quot; of lands west of the Continental Divide to the Pacific Ocean as part of the Anglo-American Convention of 1818, which established the 49th parallel as the international boundary west from Lake of the Woods to the Rocky Mountains.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
Fur trapper James Sinclair, on orders from Sir George Simpson, Governor of the Hudson's Bay Company, led some 200 settlers from the Red River Colony west in 1841 to settle on Hudson Bay Company farms near Fort Vancouver. The party crossed the Rockies into the Columbia Valley, near present-day Radium Hot Springs, British Columbia, then traveled south-west down the Kootenai River and Columbia River.

Geographic entities mentioned:
surface_form: Columbia Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.0333
lon: -116.617
states to have been providing legal abortions before the 1973 Supreme Court decision in &quot;Roe v. Wade&quot; which loosened abortion laws nationwide. On May 18, 1980, following a period of heavy tremors and small eruptions, the north face of Mount St. Helens slid off in the largest landslide in recorded history before erupting violently, destroying a large part of the top of the volcano.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
The Cascade Range has several volcanoes, which reach altitudes significantly higher than the rest of the mountains. From north to south, these major volcanoes are Mount Baker, Glacier Peak, Mount Rainier, Mount St. Helens, and Mount Adams. All are active volcanoes. Mount Rainier—the tallest mountain in the state—is south of the city of Seattle, from which it is prominently visible.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
While the Puget Sound lowlands are known for clouds and rain in the winter, the western slopes of the Cascades receive larger amounts of precipitation, often falling as snow at higher elevations. Mount Baker, near the state's northern border, is one of the snowiest places in the world. In 1999, it set the world record for snowfall in a single season—.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
East of the Cascades, a large region experiences strong rain shadow effects. Semi-arid conditions occur in much of Eastern Washington with the strongest rain shadow effects at the relatively low elevations of the central Columbia Plateau—especially the region just east of the Columbia River from about the Snake River to the Okanagan Highland.

Geographic entities mentioned:
surface_form: Columbia Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 45.999444444444
lon: -119.00138888889
Washington is home to four of the five longest floating bridges in the world: the Evergreen Point Floating Bridge, Lacey V. Murrow Memorial Bridge and Homer M. Hadley Memorial Bridge over Lake Washington, and the Hood Canal Bridge which connects the Olympic Peninsula and Kitsap Peninsula. Among its most famous bridges is the Tacoma Narrows Bridge, which collapsed in 1940 and was rebuilt.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Brent Knoll (village). Brent Knoll, formerly known as South Brent, is a village and civil parish in Somerset, England, which lies on the southern edge of Brent Knoll – a hill with a height of 137 metres (450 ft) that dominates the low surrounding landscape of the Somerset Levels. History. The village of Brent Knoll lies at the south west base of the hill.

Geographic entities mentioned:
surface_form: Brent Knoll
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.254
lon: -2.946
Lake Wenatchee. Lake Wenatchee is a glacier- and snowmelt-fed lake situated in the Wenatchee National Forest on the eastern slopes of the Cascades Mountain Range in the state of Washington. Lake Wenatchee covers and reaches a depth of. Lake Wenatchee is the source of the Wenatchee River. Its main tributaries are the White River and the Little Wenatchee River.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
Lake Wenatchee. Lake Wenatchee is a glacier- and snowmelt-fed lake situated in the Wenatchee National Forest on the eastern slopes of the Cascades Mountain Range in the state of Washington. Lake Wenatchee covers and reaches a depth of. Lake Wenatchee is the source of the Wenatchee River. Its main tributaries are the White River and the Little Wenatchee River.

Geographic entities mentioned:
surface_form: lake wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
Lake Wenatchee covers and reaches a depth of. Lake Wenatchee is the source of the Wenatchee River. Its main tributaries are the White River and the Little Wenatchee River. At its eastern end, the lake is breasted by Lake Wenatchee State Park. Lake Wenatchee State Airport, an unimproved grass and dirt landing strip, is adjacent to the north side of the state park.

Geographic entities mentioned:
surface_form: lake wenatchee
instance_of: Lake
countries: United States
coordinates: lat: 47.82267
lon: -120.7772
Aftermath. DeNA's upset win against SoftBank was their first Japan Series title in 26 years, their first championship since DeNA purchased the team, and their third overall. Their win was only the second time since the implementation of the playoffs that a team that finished the regular season in third place went on to win the Japan Series and the first time for Central League team.

Geographic entities mentioned:
surface_form: DeNA
instance_of: Mountain
countries: Iran
coordinates: lat: 30.951666666667
lon: 51.4375
departure on Labor Day of 1967. The ferry system sold the ship later in the year on December 19. It was first used as a warehouse on Lake Union, than sold again in 1975, where it was moved to Coos Bay, Oregon to be used as a restaurant. The restaurant failed, and instead her superstructure was removed to become a warehouse again, but this time shore-based.

Geographic entities mentioned:
surface_form: Lake Union
instance_of: Lake
countries: United States
coordinates: lat: 47.6392
lon: -122.3337
Visible from the village from east to west are Burnt Mountain Ridge, Burnt Mountain, Baldy Mountain, Chapel Peak, Garret Peak, Clark Peak, Mount Daly, and Capitol Peak. Neither Snowmass Mountain nor Snowmass Peak, at the headwaters of Snowmass Creek, are visible from Snowmass Village. The geologic unit Mancos Shale underlies most of the area.

Geographic entities mentioned:
surface_form: Snowmass Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.118755555556
lon: -107.06645833333
surface_form: Snowmass Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.1108
lon: -107.052
The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end. Two of the Umba's main tributaries, the Kana and the Muna, flow into the Umba through Lake Kanozero.

Geographic entities mentioned:
surface_form: Lake Umbozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.680833333333
lon: 34.410833333333
surface_form: umbozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.680833333333
lon: 34.410833333333
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake has two outflow channels: At Zasheyek-Kanozero at the very southern end of the lake the Rodvinga channel exits through the Kanoserskiy Falls, while five kilometers to the northeast the Kitsa channel leaves the lake over the Padun Falls. The channels rejoin in Lake Ponchozero about ten kilometers downriver. Lake Kanozero is also known for the Kanozero Petroglyphs.

Geographic entities mentioned:
surface_form: Lake Ponchozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.866666666667
lon: 34.333333333333
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: ponchozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 66.866666666667
lon: 34.333333333333
Lake Kanozero. Kanozero () is a lake on the river Umba in Murmansk Oblast in Russia. The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
surface_form: lake kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
Lake Kanozero. Kanozero () is a lake on the river Umba in Murmansk Oblast in Russia. The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
Lake Kanozero. Kanozero () is a lake on the river Umba in Murmansk Oblast in Russia. The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end. Two of the Umba's main tributaries, the Kana and the Muna, flow into the Umba through Lake Kanozero.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
The lake is 32 km long and between three and six kilometers wide. Ita area is. It is situated about halfway between Lake Umbozero and the White Sea. The Umba river enters the lake on the east side, about five kilometers from its northern end. Two of the Umba's main tributaries, the Kana and the Muna, flow into the Umba through Lake Kanozero.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
surface_form: lake kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
Two of the Umba's main tributaries, the Kana and the Muna, flow into the Umba through Lake Kanozero. The lake has two outflow channels: At Zasheyek-Kanozero at the very southern end of the lake the Rodvinga channel exits through the Kanoserskiy Falls, while five kilometers to the northeast the Kitsa channel leaves the lake over the Padun Falls.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
The lake has two outflow channels: At Zasheyek-Kanozero at the very southern end of the lake the Rodvinga channel exits through the Kanoserskiy Falls, while five kilometers to the northeast the Kitsa channel leaves the lake over the Padun Falls. The channels rejoin in Lake Ponchozero about ten kilometers downriver. Lake Kanozero is also known for the Kanozero Petroglyphs.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.512777777778
lon: 179.54527777778
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
surface_form: kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
surface_form: lake kanozero
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 67.045555555556
lon: 34.136388888889
Yorkshire Blue and White. The Yorkshire Blue and White pig, also known as the Bilsdale Blue, or as the &quot;Blood Breed&quot;, was a breed of domestic pig originating in the United Kingdom. It is now considered extinct. Characteristics and history.

Geographic entities mentioned:
surface_form: Bilsdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.331
lon: -1.122
Geography. The Western Allegheny Plateau ecoregion is located on the western Allegheny Plateau, which is within the central region of the Appalachian Plateau. The World Wildlife Fund defines the ecoregion as being the northern part of the Appalachian mixed mesophytic forests.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
Petrer joins together with the city of Elda to form a conurbation with over 95,000 inhabitants. The creek Rambla dels Molins (&quot;Riverbed of the Mills&quot;), a tributary of the river Vinalopó, runs through the urban area of Petrer. The economy of Petrer is based on the industries of footwear, furs, plastics, construction materials and pottery.

Geographic entities mentioned:
surface_form: Vinalopó
instance_of: Watercourse
countries: Spain
coordinates: lat: 38.7399236
lon: -0.578145
Inning am Ammersee. Inning am Ammersee (,) is a municipality in Bavaria, Germany, in the district of Starnberg, in the Regierungsbezirk of Oberbayern. It lies on the shores of lake Ammersee.

Geographic entities mentioned:
surface_form: Ammersee
instance_of: Lake
countries: Germany
coordinates: lat: 48
lon: 11.116666666667
Mount Erasmus. Mount Erasmus is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Amery, to the north-northwest. Mount Erasmus can be seen from the Icefields Parkway west of Saskatchewan Crossing, with optimum photography conditions in morning light. History.

Geographic entities mentioned:
surface_form: Mount Amery
instance_of: Mountain
countries: Canada
coordinates: lat: 52.036944444444444
lon: -116.98166666666667
Mount Erasmus. Mount Erasmus is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Amery, to the north-northwest. Mount Erasmus can be seen from the Icefields Parkway west of Saskatchewan Crossing, with optimum photography conditions in morning light. History.

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
Mount Erasmus. Mount Erasmus is a mountain summit located in the North Saskatchewan River valley of Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Mount Amery, to the north-northwest. Mount Erasmus can be seen from the Icefields Parkway west of Saskatchewan Crossing, with optimum photography conditions in morning light. History.

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. Mount Erasmus was named by James Hector in 1859 during the Palliser expedition for Peter Erasmus (1833-1931), who was an interpreter and guide for that exploration into the Canadian Rockies. Peter's skills as a Métis interpreter opened up the west for scientists, explorers, and government officials. The first ascent of the mountain was made in 1950 by John C. Oberlin and Fred Ayres.

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
Oberlin and Fred Ayres. The mountain's name was officially adopted in 1957 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Erasmus is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Erasmus is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
Winter temperatures can drop below -20 °C with wind chill factors below -30 °C. In terms of favorable weather conditions, summer months are best for climbing. Precipitation runoff from Mount Erasmus drains into tributaries of the North Saskatchewan River. Further reading. &quot;Buffalo Days and Nights&quot;, Author Peter Erasmus as told to Henry Thompson, Publisher Glenbow-Alberta Institute, 1976

Geographic entities mentioned:
surface_form: mount erasmus
instance_of: Mountain
countries: Canada
coordinates: lat: 51.96
lon: -116.9206
History. Mount Erasmus was named by James Hector in 1859 during the Palliser expedition for Peter Erasmus (1833-1931), who was an interpreter and guide for that exploration into the Canadian Rockies. Peter's skills as a Métis interpreter opened up the west for scientists, explorers, and government officials. The first ascent of the mountain was made in 1950 by John C. Oberlin and Fred Ayres.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The first ascent of the mountain was made in 1950 by John C. Oberlin and Fred Ayres. The mountain's name was officially adopted in 1957 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Mount Erasmus is composed of sedimentary rock laid down from the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Its natural habitats are tropical moist lowland and montane forests, with breeding taking place in streams. It is threatened by habitat loss and chytridiomycosis. The common name refers to La Loma, its type locality on the trail between Chiriquí Lagoon and Boquete, in the Bocas del Toro Province of Panama. Description.

Geographic entities mentioned:
surface_form: Chiriquí Lagoon
instance_of: Lake
countries: Panama
coordinates: lat: 9.033333333333333
lon: -82.01666666666667
Interpretation. The narrative states that the location for this punishment of Achan, which lies between Jericho and Ai, became known as the &quot;vale of Achor&quot; in memory of him. This narrative is probably an etiological myth providing a folk etymology for &quot;Achor&quot;, at the point in the narrative where the vale of Achor is necessarily crossed.

Geographic entities mentioned:
surface_form: Achor
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.83686
lon: 35.399773
vii. 20). Achan is held up by the rabbis as a model of the penitent sinner; because his public confession and subsequent punishment saved him from eternal doom in Gehenna. &quot;Every culprit before he is to meet his penalty of death,&quot; says the Mishnah Sanh. vi.

Geographic entities mentioned:
surface_form: Gehenna
instance_of: Valley
countries: Israel
coordinates: lat: 31.76916667
lon: 35.22805556
official number 216260 with signal LKQG. A Standard World War I cargo ship, she was laid down as &quot;War Flag&quot;, but named &quot;Lake Sunapee&quot; after the lake in New Hampshire. She was launched on 28 December 1917, while World War I was still in progress. The ship was a single deck vessel with a grain capacity of and bunker capacity of. She was long, wide and deep.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: United States
coordinates: lat: 43.375833333333
lon: -72.056388888889
From 1953 to 1955, Frank conducted classified defense research. His log home in Moose wasn't winterized, so the family lived in various places around the Jackson Hole valley, including stays on the Murie Ranch, the old Budge house in Wilson, and a house in Jackson.

Geographic entities mentioned:
surface_form: Jackson Hole
instance_of: Valley
countries: United States
coordinates: lat: 43.516666666667
lon: -110.83333333333
Warnman people. The Warnman, also spelt Wanman, are an Aboriginal Australian people of Western Australia's Pilbara region. Country. The Warnman people's territory extends over some. Their southern boundary lies around the McKay Range and the area of Kumpupintil Lake. Westwards, it reaches &quot;Wadurara&quot; on the Rudall River (&quot;Karlamilyi&quot;).

Geographic entities mentioned:
surface_form: Kumpupintil Lake
instance_of: Lake
countries: Australia
coordinates: lat: -23.5
lon: 122.83333333333
Steven Fought was nominated by the Democratic Party to take Foister's place on the general election ballot. District 9. The 9th district spans the coast of Lake Erie from Toledo to the west side of Cleveland, taking in Port Clinton, Sandusky, Lorain, Lakewood, Brook Park, and Brooklyn. It had been held by Democrat Marcy Kaptur since 1983. District 10.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Attorney General McGrath also came to California to campaign for the Democrats, and freshman Senator Hubert Humphrey of Minnesota tirelessly worked the San Joaquin Valley, talking to farmers and workers. Name-calling and supporters: the final days. Douglas adopted Boddy's &quot;Tricky Dick&quot; nickname for Nixon, and also referred to him as &quot;pee wee&quot;.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Gold Lake (King County, Washington). Gold Lake is a freshwater lake located on a valley on the west skirt of Wild Goat Peak, in King County, Washington. Gold Lake is surrounded by prominent peaks and lakes at the heart of the Alpine Lakes Wilderness, including Big Snow Mountain and Iron Cap Mountain. Waterfalls.

Geographic entities mentioned:
surface_form: Wild Goat Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.552335
lon: -121.334317
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Gold Lake (King County, Washington). Gold Lake is a freshwater lake located on a valley on the west skirt of Wild Goat Peak, in King County, Washington. Gold Lake is surrounded by prominent peaks and lakes at the heart of the Alpine Lakes Wilderness, including Big Snow Mountain and Iron Cap Mountain. Waterfalls.

Geographic entities mentioned:
surface_form: Big Snow Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.534722222222
lon: -121.36583333333
surface_form: Iron Cap Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.553888888889
lon: -121.28472222222
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
Waterfalls. The outflow of Gold Lake joins the creeks from Moira Lake, Fools Gold Lake and other snow melting creeks to empty as the inflow of Lake Dorothy, which is the origin of the East Fork of the Miller River. Shortly after the Gold Lake outflow, the creek plunges into an unrated waterfall, Gold Lake Falls.

Geographic entities mentioned:
surface_form: Fools Gold Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.549659
lon: -121.366225
surface_form: Lake Dorothy
instance_of: Lake
countries: United States
coordinates: lat: 47.5864756
lon: -121.384297
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
Access. Access to Gold Lake is through Dutch Miller Gap trail 1030 starting at Dingford Creek gate. The trail leads to a ridge of Big Snow Mountain towards Wild Goat Peak. Gold Lake is on the west side of the ridge, and Chetwoot Lake on the opposite side. The trail passes alongside Hardscrabble Creek and through Hardscrabble Lakes on the south skirt of Hardscrabble Dome.

Geographic entities mentioned:
surface_form: Chetwoot Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.556666666667
lon: -121.31444444444
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
Gold Lake (King County, Washington). Gold Lake is a freshwater lake located on a valley on the west skirt of Wild Goat Peak, in King County, Washington. Gold Lake is surrounded by prominent peaks and lakes at the heart of the Alpine Lakes Wilderness, including Big Snow Mountain and Iron Cap Mountain. Waterfalls.

Geographic entities mentioned:
surface_form: gold lake (king county, washington)
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Waterfalls. The outflow of Gold Lake joins the creeks from Moira Lake, Fools Gold Lake and other snow melting creeks to empty as the inflow of Lake Dorothy, which is the origin of the East Fork of the Miller River. Shortly after the Gold Lake outflow, the creek plunges into an unrated waterfall, Gold Lake Falls.

Geographic entities mentioned:
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
Access. Access to Gold Lake is through Dutch Miller Gap trail 1030 starting at Dingford Creek gate. The trail leads to a ridge of Big Snow Mountain towards Wild Goat Peak. Gold Lake is on the west side of the ridge, and Chetwoot Lake on the opposite side. The trail passes alongside Hardscrabble Creek and through Hardscrabble Lakes on the south skirt of Hardscrabble Dome.

Geographic entities mentioned:
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889
The trail leads to a ridge of Big Snow Mountain towards Wild Goat Peak. Gold Lake is on the west side of the ridge, and Chetwoot Lake on the opposite side. The trail passes alongside Hardscrabble Creek and through Hardscrabble Lakes on the south skirt of Hardscrabble Dome. It follows a ridge towards Wild Snow Peak with Gold Lake on the north side of this ridge.

Geographic entities mentioned:
surface_form: gold lake
instance_of: Lake
countries: United States
coordinates: lat: 47.55
lon: -121.34388888889