Sarmila/GeoWiki-Features huggingface dataset:
The system covers approximately and contains four individual wetland cells, in addition to levees, canals and ditches. The Marsh Flow-Way treats water pumped into it from Lake Apopka. The lake's water has excessive amounts of phosphorus, algae and suspended matter. Water flows west to east and is controlled by screw gates and riser boards in the individual cells.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Treated water from all cells collects in a pump basin, where water is pumped into the Apopka Beauclair Canal. Most of the cleaner, treated water returns to Lake Apopka, while the remainder flows downstream toward Lake County Water Authority's nutrient removal facility (NuRF). Dominant vegetation communities growing in flow-way cells are shallow marsh and shrub swamp species.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Harvesting shad from other lakes has resulted in an improved food web, reduced algae, improved water clarity and improved conditions for game fish populations. This procedure may produce the same results in Lake Apopka. Through the fall of 2011, gizzard shad harvesting has removed about 8,400 metric tons (18.5 million pounds) of fish from the lake.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Restoring aquatic habitat. The District has planted wetland plant species behind protective barriers in Lake Apopka to provide habitat for fish and wildlife. These planting efforts are becoming less necessary as the lake's water quality and clarity improve and native aquatic plants re-establish themselves.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Challenges. Restoring Florida's most polluted large lake has come with unforeseen problems. An estimated 676 birds died on former farms at Lake Apopka during late 1998 and early 1999. Most were American white pelicans, wood storks and great blue herons. Organochlorine pesticide (OCPs) residues remaining from agricultural practices were primary the cause of bird deaths.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
The District has conducted research to better understand the accumulation of OCPs through the food chain, from contaminated soil to fish, and from fish to fish-eating birds. The knowledge generated guides restoration of the former farmlands at Lake Apopka and is applicable to other projects designed to restore ecosystems impacted by agriculture. Water quality improvements in Lake Apopka.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
The knowledge generated guides restoration of the former farmlands at Lake Apopka and is applicable to other projects designed to restore ecosystems impacted by agriculture. Water quality improvements in Lake Apopka. Lake Apopka has responded to the reductions in external phosphorus loading from the watershed to the lake with improved lake water quality.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Water quality improvements in Lake Apopka. Lake Apopka has responded to the reductions in external phosphorus loading from the watershed to the lake with improved lake water quality. Total phosphorus, chlorophyll and Secchi transparency showed improving trends between 1987 and 2010. However, during this 23-year period, three events contributed to a worsening of water quality within a given year.

Geographic entities mentioned:
surface_form: lake apopka
instance_of: Lake
countries: United States
coordinates: lat: 28.620555555556
lon: -81.621944444444
Located northwest of Longyearbyen, it is the northernmost airport in the world with public scheduled flights. The first airport (or more accurately airstrip) near Longyearbyen (in Adventdalen) was constructed during World War II by the Luftwaffe, it was the first airstrip on Svalbard. It was first put into use for occasional flights in 1959, but could only be operated a few months a year.

Geographic entities mentioned:
surface_form: Adventdalen
instance_of: Valley
countries: Norway
coordinates: lat: 78.21222222
lon: 15.8
Lufttransport provides services to Ny-Ålesund Airport and Svea Airport, using Dornier 228 turboprop aircraft. There are also regular charter flights. On 29 August 1996, Vnukovo Airlines Flight 2801 crashed into Operafjellet mountain about from the airport. All 141 people on board the Tupolev Tu-154M were killed. It is the worst air crash in Norwegian history.

Geographic entities mentioned:
surface_form: Operafjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 78.225
lon: 16.051666666667
The municipality (originally the parish) is named after the old &quot;Vennesla&quot; farm () since the first Vennesla Church was built there. The first element is &quot;vendil&quot; which comes from the word which means &quot;small twig&quot;. This may have been an old name for an arm of Venneslafjorden. The last element is which means &quot;swamp&quot; or &quot;shallow water&quot;. Coat of arms.

Geographic entities mentioned:
surface_form: Venneslafjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.28111111
lon: 7.96416667
The neighboring municipalities are Evje og Hornnes (to the north), Birkenes and Iveland (to the east), and Kristiansand (to the south and west), and Lindesnes (to the west). The river Otra runs through the municipality from north to south. Both of the lakes Kilefjorden and Venneslafjorden are located along the river. The river Songdalselva runs through the western part of the municipality.

Geographic entities mentioned:
surface_form: Kilefjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.434166666667
lon: 7.8086111111111
surface_form: Venneslafjorden
instance_of: Lake
countries: Norway
coordinates: lat: 58.28111111
lon: 7.96416667
Eulogies were delivered at the Porat Yosef Yeshiva and in the Geula neighborhood. MK Meshulam Nahari said &quot;who would have thought that... a rabbi could be murdered in Israel?&quot; He is buried on the Mount of Olives. Asher Dahan was sentenced to life imprisonment for the murder.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
The artist worked with L.A. design consultant AECOM as well as the bridge's builder, Skanska USA, on the final design and construction. The woven-basket look of the bridge's support columns emulate the woven baskets of the native Chumash people of the San Gabriel Valley while the underside of the bridge evokes a Western diamondback rattlesnake. Former service.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Shams al-Din Muhammad ibn al-Muqaddam. Shams al-Din Muhammad ibn al-Muqaddam (; died at Mount Arafat on 9 February 1188) was the 1st Emir of Baalbek under Ayyubid Dynasty, Although he was not from Ayyubid origin. He was a military commander first in the service of Nur ad-Din, the Zengid ruler of Syria and Iraq, later of Saladin, the Ayyubid ruler of Egypt, Syria and Iraq. Biography.

Geographic entities mentioned:
surface_form: Mount Arafat
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.354831
lon: 39.983886
While on the Hajj, he was wounded in the eyes during a skirmish between Syrian and Iraqi pilgrims in the tent of the Iraqi pilgrims' leader at Mount Arafat, where he eventually died on 9 February 1188.

Geographic entities mentioned:
surface_form: Mount Arafat
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 21.354831
lon: 39.983886
With the city's changes in population, its western boundary has moved farther west and its southern boundary farther south. In 1961, San Fernando Valley residents for a time backed an unsuccessful plan to move the 10th District seat to the Valley after it was left vacant with the resignation of Council Member Charles Navarro. Geography.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Salar de Ascotán, also known as Salar de Cebollar, is a salt flat in northern Chile. Its drainage basin is and is shared with Bolivia. The basin is bordered on the north by the Salar de Carcote basin, on the east by small endorheic basins, including those of Laguna Cañapa and Laguna Hedionda, from which it is separated by the crest of the Cerros de Cañapa, Cerro Araral and others.

Geographic entities mentioned:
surface_form: Cerro Araral
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.6
lon: -68.183333333333
To the south, the basin is bordered by the San Pedro de Inacaliri River basin, while to the west the drainage divide between the salt flat and the Upper Loa River basin is marked by the summits of a chain of volcanoes culminating in Palpana. Salar de Ascotán has a surface area of and the train line of the FCAB runs on the west side of the salt flat for over.

Geographic entities mentioned:
surface_form: Palpana
instance_of: Mountain
countries: Chile
coordinates: lat: -21.546666666667
lon: -68.5225
He was 11 years old. This first family drama broke the painter and he decided to settle permanently in Sélestat where a street now bears his name. In 1934, he remained so depressed that he retired to the Tännchel mountains where he lived as a hermit in the Grimmelshütte, a poor forest shelter. This place, known for ancient megalithic cults, seemed to have encouraged him to move forward.

Geographic entities mentioned:
surface_form: Tännchel
instance_of: Mountain
countries: France
coordinates: lat: 48.234722222222
lon: 7.2588888888889
Xuanzang Temple (Taiwan). Xuanzang Temple or Syuentzang Temple () is a Buddhist temple located in the Sun Moon Lake tourist area, Yuchih Township of Nantou County, Taiwan. History.

Geographic entities mentioned:
surface_form: Sun Moon Lake
instance_of: Lake
countries: Taiwan
coordinates: lat: 23.866666666667
lon: 120.91666666667
It sits on a hill named &quot;Cinglong&quot; () near the Sun Moon Lake, the largest body of water in Taiwan.

Geographic entities mentioned:
surface_form: Sun Moon Lake
instance_of: Lake
countries: Taiwan
coordinates: lat: 23.866666666667
lon: 120.91666666667
It is part of an unnamed range forming the most northerly group of peaks in the Garibaldi Ranges, the other two most notable being Mount Weart, known as the Armchair because of its shape, and Mount Currie, which overlooks the First Nations Reserve of the same name and the neighbouring town of Pemberton.

Geographic entities mentioned:
surface_form: Mount Weart
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1664
lon: -122.78602
surface_form: mount currie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.24861111111111
lon: -122.78194444444445
surface_form: mount weart
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1664
lon: -122.78602
surface_form: mount currie
instance_of: Mountain
countries: Canada
coordinates: lat: 50.80305555555555
lon: -115.49222222222222
Climbing and access. A steep hike leads to a backcountry shelter and camping area at Wedgemount Lake, which is an approximately three-hour hike (without heavy gear) from a parking lot near the Wedgemont Green Lake railstop and track-crossing of the CNR. Across Wedgemount Lake from the cabin is the glacier, and above that the summit.

Geographic entities mentioned:
surface_form: Wedgemount Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
surface_form: wedgemount lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
surface_form: wedgemount lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
surface_form: green lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.16675
lon: -107.71732
surface_form: green lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.678
lon: -77.1351
surface_form: green lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.416667
lon: -121.209722
surface_form: green lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.15
lon: -122.93611111111112
Most of Wedge is in a provincial park, so helicopters are not allowed to drop people off there. In the early 1970s the glacier that now almost reaches the eastern end of Wedgemount Lake extended into the lake and at its terminus was approximately ten metres in height. Climate.

Geographic entities mentioned:
surface_form: wedgemount lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
Wedge Mountain, prominence:, often locally referred to as The Wedge or simply &quot;Wedge&quot;, is the highest summit in the Garibaldi Ranges and therefore also Garibaldi Provincial Park, and is among the nearest of the many peaks visible from the Whistler Blackcomb Ski Area, lying north across the valley of Billygoat Pass from the Spearhead Range, which includes one of that resort's two flagship mountains, Blackcomb.

Geographic entities mentioned:
surface_form: the wedge
instance_of: Mountain
countries: Canada
coordinates: lat: 50.8491
lon: -115.137
surface_form: the spearhead
instance_of: Mountain
countries: Canada
coordinates: lat: 50.086388888889
lon: -122.86388888889
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: the wedge
instance_of: Mountain
countries: Canada
coordinates: lat: 50.13305555555556
lon: -122.79333333333334
surface_form: wedge mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.13305555555556
lon: -122.79333333333334
Wedge Mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: wedge mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.13305555555556
lon: -122.79333333333334
Wedge's very high prominence is defined by the divide between the Green and Cheakamus Rivers at a locality at the south end of Alta Lake known as Tokum Corners. The mountain sits astride the boundary between the New Westminster and Lillooet Land Districts. Climbing and access.

Geographic entities mentioned:
surface_form: alta lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.11472222222222
lon: -122.98194444444445
Climate. Based on the Köppen climate classification, Wedge Mountain is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: wedge mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.13305555555556
lon: -122.79333333333334
Mount Clairvaux. Mount Clairvaux is located on the border of Alberta and British Columbia, SE of the Yellowhead Pass. Clairvaux is the French word for &quot;clear valleys.&quot;.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount clairvaux
instance_of: Mountain
countries: Canada
coordinates: lat: 52.8056
lon: -118.415
Mount Clairvaux. Mount Clairvaux is located on the border of Alberta and British Columbia, SE of the Yellowhead Pass. Clairvaux is the French word for &quot;clear valleys.&quot;.

Geographic entities mentioned:
surface_form: mount clairvaux
instance_of: Mountain
countries: Canada
coordinates: lat: 52.8056
lon: -118.415
Spines may be present on the branches and leaves, and the twigs, petioles and lower surface of the leaves are hairy. Inflorescences have up to 12 mauve flowers about diameter, and the fruit is an orange or red berry about diameter. It occurs on the McIlwraith Range on Cape York Peninsula and on mostly higher ground (such as the Windsor and Atherton Tablelands in the Cairns region. Conservation.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Geographic distribution. The Pennsylvania Dutch live primarily in the Delaware Valley and in the Pennsylvania Dutch Country, a large area that includes South Central Pennsylvania, in the area stretching in an arc from Bethlehem and Allentown in the Lehigh Valley westward through Reading, Lebanon, and Lancaster to York and Chambersburg.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Schurmsee. The Schurmsee is a tarn that lies at a height of 794 metres in the municipality of Forbach in the Northern Black Forest in Germany. It is located on a line between Hundsbach and Schönmünzach. The lake covers an area of 1.6 hectares and is up to 13 metres deep. Its volume is about 180,000 cubic metres.

Geographic entities mentioned:
surface_form: schurmsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.6133
lon: 8.31876
From the 960-metre-high mountain of &quot;Schurmseehöhe&quot; there is a good view over the whole lake. There is a circular walk around the tarn. The normal route to the Schurmsee runs on a wide forest track from Schönmünzach for a distance of about 4 kilometres and climbing through around 300 metres.

Geographic entities mentioned:
surface_form: schurmsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.6133
lon: 8.31876
Allen was also the founding chief executive officer of UnitingCare Australia's Cutting Edge community services agency in the Goulburn Valley. Gender and Sexuality Commissioner. Victoria was the first Australian state to establish an Equality portfolio and a commissioner for gender and sexuality within this department.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Lake Sutherland. Lake Sutherland is located on the Olympic Peninsula about west of Port Angeles, Washington. The lake is located just to the east of Lake Crescent. Lake Sutherland drains into Indian Creek, which is a tributary of the Elwha River. Lake Sutherland is named for the Canadian fur trapper John Sutherland who, with John Everett, explored the lake around 1865.

Geographic entities mentioned:
surface_form: Lake Crescent
instance_of: Lake
countries: United States
coordinates: lat: 48.0595755
lon: -123.8291037
Lake Sutherland and Indian Creek sustained anadromous fish populations until construction of the Elwha Dam in 1913 blocked access to the ocean, eliminating several salmon species from Indian Creek and landlocking others. The lake contains a population of kokanee sockeye salmon, which spawn in Lake Sutherland and until the removal of the Elwha Dam in 2012 migrated to Lake Aldwell.

Geographic entities mentioned:
surface_form: Lake Aldwell
instance_of: Lake
countries: United States
coordinates: lat: 48.0944
lon: -123.557
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Lake Sutherland. Lake Sutherland is located on the Olympic Peninsula about west of Port Angeles, Washington. The lake is located just to the east of Lake Crescent. Lake Sutherland drains into Indian Creek, which is a tributary of the Elwha River. Lake Sutherland is named for the Canadian fur trapper John Sutherland who, with John Everett, explored the lake around 1865.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Lake Sutherland. Lake Sutherland is located on the Olympic Peninsula about west of Port Angeles, Washington. The lake is located just to the east of Lake Crescent. Lake Sutherland drains into Indian Creek, which is a tributary of the Elwha River. Lake Sutherland is named for the Canadian fur trapper John Sutherland who, with John Everett, explored the lake around 1865.

Geographic entities mentioned:
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.30944444
lon: -91.99777778
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.51944444
lon: -93.5225
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
surface_form: indian creek
instance_of: Watercourse
countries: United States
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.9747757
lon: -90.1978958
Lake Sutherland is named for the Canadian fur trapper John Sutherland who, with John Everett, explored the lake around 1865. Lake Sutherland and Indian Creek sustained anadromous fish populations until construction of the Elwha Dam in 1913 blocked access to the ocean, eliminating several salmon species from Indian Creek and landlocking others.

Geographic entities mentioned:
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.30944444
lon: -91.99777778
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.30944444
lon: -91.99777778
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.51944444
lon: -93.5225
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 36.51944444
lon: -93.5225
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
surface_form: indian creek
instance_of: Watercourse
countries: United States
surface_form: indian creek
instance_of: Watercourse
countries: United States
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.9747757
lon: -90.1978958
surface_form: indian creek
instance_of: Watercourse
countries: United States
coordinates: lat: 37.9747757
lon: -90.1978958
Lake Sutherland. Lake Sutherland is located on the Olympic Peninsula about west of Port Angeles, Washington. The lake is located just to the east of Lake Crescent. Lake Sutherland drains into Indian Creek, which is a tributary of the Elwha River. Lake Sutherland is named for the Canadian fur trapper John Sutherland who, with John Everett, explored the lake around 1865.

Geographic entities mentioned:
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
The lake contains a population of kokanee sockeye salmon, which spawn in Lake Sutherland and until the removal of the Elwha Dam in 2012 migrated to Lake Aldwell. Lake Sutherland lies just outside Olympic National Park and is private land. The lake is surrounded by houses. There is also a reservoir in San Diego County, Situated between Ramona and Julian, with the same name.

Geographic entities mentioned:
surface_form: lake sutherland
instance_of: Lake
countries: United States
coordinates: lat: 48.0779116
lon: -123.7085698
Staircase Falls. Staircase Falls is a series of waterfalls located on the southern side of Yosemite Valley in Yosemite National Park, California. The falls descend a total of into Yosemite Valley over a series of steps. Staircase Falls is relatively ephemeral and is usually dry by the end of June. The falls are located immediately behind Camp Curry on cliffs below Glacier Point.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
The nearest city is Lübeck. The town belongs to the (historical) region of Holstein, today in the German state of Schleswig-Holstein. Oldenburg was the chief town of the Wagrians, one of the Slavic peoples that migrated as far west as the river Elbe in or after the 6th century (see Völkerwanderung), also known as Wends and Obotrites. They arrived about A.D.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
To the east is the Guyot massif, which rises to over 6,000 feet (1,829 m) for long stretches. To the west is the Le Conte massif, which culminates in a 6,593-foot (2,009 m) summit. The ridge immediately to the south connecting the two massifs, known as &quot;the Sawteeth,&quot; consists of a series of jagged, steep cliffs, the most well-known of which spans the northern face of Charlies Bunion.

Geographic entities mentioned:
surface_form: Charlies Bunion
instance_of: Mountain
countries: United States
coordinates: lat: 35.638888888889
lon: -83.372219444444
surface_form: charlies bunion
instance_of: Mountain
countries: United States
coordinates: lat: 35.638888888889
lon: -83.372219444444
surface_form: sawteeth
instance_of: Mountain
countries: United States
coordinates: lat: 44.1133
lon: -73.8507
Route 321 between Gatlinburg and Cosby. One Whaley family would eventually be displaced three times by eminent domain—once when the NPS purchased their farm in Greenbrier, then again when the Tennessee Valley Authority purchased their land for the construction of Norris Dam, and a third time when their land was purchased in Oak Ridge for the Manhattan Project.

Geographic entities mentioned:
surface_form: oak ridge
instance_of: Landform
countries: United States
coordinates: lat: 37.46
lon: -121.722
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 35.959166666667
lon: -83.850277777778
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: tennessee valley
instance_of: Valley
countries: United States
coordinates: lat: 37.8611
lon: -122.534
The hotel made a convenient jumping point for excursions to nearby Mount Le Conte and Mount Guyot. Its foundation remains today, just off Ramsey Prong Road. National park. Tourism and heavy logging led to increased demands from conservationists to protect the Great Smoky Mountains.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 35.705
lon: -83.2575
The rests in the bed of Injun Creek. The Ramsey Cascades Trail follows Ramsey Prong four miles (6 km) up the slope of Mount Guyot to Ramsey Cascades, a waterfall nestled between Guyot Spur and Greenbrier Pinnacle. For decades, hikers have used Ramsey Prong to bushwhack to the Appalachian Trail, just below Guyot's summit.

Geographic entities mentioned:
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 39.4587
lon: -105.938
surface_form: mount guyot
instance_of: Mountain
countries: United States
coordinates: lat: 44.1681
lon: -71.534
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countries: United States
coordinates: lat: 35.7069
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surface_form: mount guyot
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countries: United States
coordinates: lat: 35.705
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Greenbrier Pinnacle, a ridge descending from the western flank of Old Black westward to the Middle Fork valley, nearly closes off Greenbrier Cove entirely. Over a dozen streams flow north from the crest of the Pinnacle, each of them cutting narrow hollows with traces of fertile bottomland.

Geographic entities mentioned:
surface_form: the pinnacle
instance_of: Mountain
countries: United States
coordinates: lat: 35.207816666667
lon: -81.312627777778
surface_form: the pinnacle
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countries: United States
coordinates: lat: 40.6128
lon: -75.9114
Later settlers. The upper watershed of the Middle Fork of the Little Pigeon River consists of a series of streams, some flowing down from Grapeyard Ridge to the west and a dozen or so flowing down from Greenbrier Pinnacle to the east. Each of these streams has cut a deep hollow, isolating the bottomlands of each amidst low ridges.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Like the Sugarlands and Roaring Fork to the west, Greenbrier's bottomlands and streambeds are coated with sandstone, phyllite, and slate rocks of all sizes. During the Ice Ages, the cold weather caused fracturing of the high mountain slopes, creating boulder fields. Over the centuries, erosional forces carried these boulders to lower elevations.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 41.0887
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Middleton settled further down the valley, near Emert's Cove. In 1818, the family of John Ownby (1781–1859), a veteran of the War of 1812, settled downstream from the Whaleys. The Whaley and Ownby families spread quickly throughout the valley. In the early 20th century, a map of Greenbrier showed the location of 26 homes—11 were Whaleys and 10 were Ownbys. Later settlers.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 34.155833333333334
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countries: United States
coordinates: lat: 61.3833
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Around 1800, William Whaley (1788–1880) and his brother Middleton Whaley (1794–1855) became the first permanent Euro-American settlers in Greenbrier. The Whaleys hailed from Edgefield District, South Carolina, and crossed the Smokies at Dry Sluice Gap (near Charlies Bunion), which is just above Porters Flat.

Geographic entities mentioned:
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countries: United States
coordinates: lat: 35.638888888889
lon: -83.372219444444
Greenbrier (Great Smoky Mountains). Greenbrier is a valley in the northern Great Smoky Mountains of Tennessee, located in the southeastern United States. Now a recreational area located within the Great Smoky Mountains National Park, Greenbrier was once home to several Appalachian communities.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Now a recreational area located within the Great Smoky Mountains National Park, Greenbrier was once home to several Appalachian communities. Greenbrier is situated along the Middle Fork of the Little Pigeon River, stretching from Porters Flat in the south to Emert's Cove in the north, at the present park boundary.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The area also includes the Middle Fork's immediate watershed from the crest of Grapeyard Ridge to the west (opposite the Roaring Fork area) to Snag Mountain in the east. The area is sometimes called Big Greenbrier to distinguish it from Little Greenbrier, which is located between Wears Valley and Elkmont several miles to the west. Geology.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The area is sometimes called Big Greenbrier to distinguish it from Little Greenbrier, which is located between Wears Valley and Elkmont several miles to the west. Geology. The ridges surrounding Greenbrier are among the highest in the Appalachian range. To the east is the Guyot massif, which rises to over 6,000 feet (1,829 m) for long stretches.

Geographic entities mentioned:
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The ridge immediately to the south connecting the two massifs, known as &quot;the Sawteeth,&quot; consists of a series of jagged, steep cliffs, the most well-known of which spans the northern face of Charlies Bunion. Greenbrier Pinnacle, a ridge descending from the western flank of Old Black westward to the Middle Fork valley, nearly closes off Greenbrier Cove entirely.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: old black
instance_of: Mountain
countries: United States
coordinates: lat: 35.7147
lon: -83.2553
This rock type, created from ancient ocean sediments 750 million years ago, dominates the mid-level elevations in the north-central Smokies. As the elevation increases to the south, a thrust fault known as the Greenbrier Fault separates the Roaring Fork sandstone from Thunderhead sandstone and Anakeesta Formation, both of which are common along the Smokies crests.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
surface_form: thunderhead
instance_of: Mountain
countries: United States
coordinates: lat: 35.568611111111
lon: -83.706388888889
To the north, as the land flattens out (near the park boundary), another thrust fault, the Gatlinburg Fault, separates the Roaring Fork formation from a layer of siltstone, which underlies the foothills around Emert's Cove. Like the Sugarlands and Roaring Fork to the west, Greenbrier's bottomlands and streambeds are coated with sandstone, phyllite, and slate rocks of all sizes.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Early history. The name &quot;greenbrier&quot; refers to the thorny vines of the genus &quot;Smilax&quot; that are common throughout the southern Appalachians. Although it is unknown when the upper Middle Fork valley obtained this name, it was being called &quot;Greenbrier&quot; as early as the 1830s. The name is not uncommon elsewhere in the region.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The name is not uncommon elsewhere in the region. The Cherokee were the first inhabitants of the Greenbrier area and may have had a seasonal settlement at Porters Flat, near Greenbrier's southern tip. As late as the early 20th century, residents of Greenbrier often referred to Porters Flat as &quot;Indian Nation,&quot; which may hearken back to its days as a Cherokee settlement.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The name is not uncommon elsewhere in the region. The Cherokee were the first inhabitants of the Greenbrier area and may have had a seasonal settlement at Porters Flat, near Greenbrier's southern tip. As late as the early 20th century, residents of Greenbrier often referred to Porters Flat as &quot;Indian Nation,&quot; which may hearken back to its days as a Cherokee settlement.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
As late as the early 20th century, residents of Greenbrier often referred to Porters Flat as &quot;Indian Nation,&quot; which may hearken back to its days as a Cherokee settlement. Around 1800, William Whaley (1788–1880) and his brother Middleton Whaley (1794–1855) became the first permanent Euro-American settlers in Greenbrier.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Most communities took the name of the stream upon which they were situated. Along with Greenbrier Cove, the most prominent of these small communities included Copeland, Soak Ash, Webb Creek, Ramsey Creek, Noisy Creek, Redwine Creek, and Little Bird Branch, all at the base of Greenbrier Pinnacle, and Laurel Creek (now Rhododendron Creek), located on Grapeyard Ridge.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
David Proffitt (1847–1909), also a veteran of the war, settled further upstream, just below the Whaley lands, sometime around 1870. Around the same time, James Redwine, a circuit rider, settled along the creek that now bears his name. Benjamin Christenberry Parton (1832–1916), the son of a migrant farm worker, and his wife Margaret arrived in Greenbrier sometime in the 1850s.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Benjamin Christenberry Parton (1832–1916), the son of a migrant farm worker, and his wife Margaret arrived in Greenbrier sometime in the 1850s. Parton, who survived a gunshot wound to the head during the Civil War, settled in the narrow flats just above the confluence of Little Bird Branch and the Middle Fork, at the western base of Greenbrier Pinnacle.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The residents of Greenbrier were largely pro-Union during the Civil War, although most tried to avoid the conflict altogether. A small force led by Confederate commander William Holland Thomas passed through Greenbrier while fleeing to North Carolina after being chased out of Gatlinburg. On the way, they inflicted minor damage to the farms of known Union supporters.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
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The location of Shults' mine (or if it existed at all) is unknown. Most small communities in the Greenbrier area had at least one general store. Greenbrier residents would typically trade chickens, eggs, and animal furs for clothing, salt, pepper, coal oil, and medicine. As roads improved in the late 19th century, Greenbrier farmers could haul excess crops to Knoxville.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
These crops were typically corn or potatoes. Others dug ginseng, which was plentiful in the Smokies at the time, while others used their excess corn to make moonshine. Bill Cardwell, who lived in the northern part of Greenbrier in the early 20th century, was said to have regularly sold moonshine to the sheriff of Sevier County. 20th century.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
A national forest was established by the Weeks Act of 1911, and in 1926 the Great Smoky Mountains Park Commission began buying up land for a national park. While the residents of Greenbrier were displaced, many simply moved to the other side of the park boundary to Emert's Cove and the Webb Mountain area.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
While the residents of Greenbrier were displaced, many simply moved to the other side of the park boundary to Emert's Cove and the Webb Mountain area. Two former Greenbrier residents, Conley Huskey and Glenn Cardwell, would eventually serve as the mayor of Pittman Center, just two miles (3 km) north of Greenbrier.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Many former residents of Greenbrier went on to become pastors, reflecting Greenbrier residents' deeply held religious beliefs. Members of Greenbrier's Primitive Baptist community continued to meet as late as the 1980s. In 1933, the Civilian Conservation Corps established Camp David Chapman at near the confluence of Rhododendron Creek and the Middle Fork.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
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Members of Greenbrier's Primitive Baptist community continued to meet as late as the 1980s. In 1933, the Civilian Conservation Corps established Camp David Chapman at near the confluence of Rhododendron Creek and the Middle Fork. This camp, which constructed most of the roads and trails in the Greenbrier area, provided valuable employment to locals during the Great Depression. Greenbrier today.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
For decades, hikers have used Ramsey Prong to bushwhack to the Appalachian Trail, just below Guyot's summit. A side trail at the end of Ramsey Prong Road leads to the summit of Greenbrier Pinnacle. The Porters Creek Trail follows Porters Creek to Porters Flat, where it passes the Messer Barn site before ascending to a backcountry campsite.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
A side trail at the end of Ramsey Prong Road leads to the summit of Greenbrier Pinnacle. The Porters Creek Trail follows Porters Creek to Porters Flat, where it passes the Messer Barn site before ascending to a backcountry campsite. The Old Settlers Trail, one of the longest trails in the park, connects Greenbrier to the Cosby area.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The Old Settlers Trail, one of the longest trails in the park, connects Greenbrier to the Cosby area. The trail was envisioned as a lower-elevation alternative to the Appalachian Trail and was built by connecting the old roads in the various communities that existed between Greenbrier and Maddron Bald. The trail passes dozens of rock walls and chimney falls, as well as the Tyson McCarter Place.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
The trail passes dozens of rock walls and chimney falls, as well as the Tyson McCarter Place. Spur trails connect with several cemeteries, including Parton Cemetery and Lindsey Cemetery. Timber rattlesnakes are not an uncommon sight on the trail, as large numbers have long been known to live on the slopes of Greenbrier Pinnacle. Historical sites.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
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instance_of: Valley
countries: United States
coordinates: lat: 35.7069
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John Messer Barn. Located along the Porters Creek Trail, the John Messer Barn was constructed in 1875 by Pinkney Whaley. The only remaining structure of the pre-park community of Greenbrier Cove, it was added to the National Register in 1976. The Messer Barn is a type of double-cantilever barn unique to East Tennessee and rarely found outside its immediate vicinity.

Geographic entities mentioned:
surface_form: greenbrier
instance_of: Valley
countries: United States
coordinates: lat: 35.7069
lon: -83.3831
Greenbrier is situated along the Middle Fork of the Little Pigeon River, stretching from Porters Flat in the south to Emert's Cove in the north, at the present park boundary. The area also includes the Middle Fork's immediate watershed from the crest of Grapeyard Ridge to the west (opposite the Roaring Fork area) to Snag Mountain in the east.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Over a dozen streams flow north from the crest of the Pinnacle, each of them cutting narrow hollows with traces of fertile bottomland. Greenbrier is underlain by a Precambrian metamorphic rock formation of the Ocoee Supergroup known as Roaring Fork Sandstone. This rock type, created from ancient ocean sediments 750 million years ago, dominates the mid-level elevations in the north-central Smokies.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
To the north, as the land flattens out (near the park boundary), another thrust fault, the Gatlinburg Fault, separates the Roaring Fork formation from a layer of siltstone, which underlies the foothills around Emert's Cove. Like the Sugarlands and Roaring Fork to the west, Greenbrier's bottomlands and streambeds are coated with sandstone, phyllite, and slate rocks of all sizes.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Trails. The Grapeyard Ridge Trail follows Rhododendron Creek over the south slope of Brushy Mountain to the Jim Bales Place at Roaring Fork. The trail passes the remains of the CCC Camp David Chapman, several Rayfield homesites, and the 1920s-era remains of a wrecked Nichols and Shepard self-propelled, steam-powered engine (known as a traction engine). The rests in the bed of Injun Creek.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
The John Messer Barn in Greenbrier Cove and the Tyson McCarter Place along Webb Creek are listed on the National Register of Historic Places, and the Smoky Mountain Hiking Club Cabin has been deemed eligible for the National Register by the Tennessee Historical Commission.

Geographic entities mentioned:
surface_form: smoky mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0594
lon: -113.68
Chauler Fort. Chauler Fort is a small fort located north of Nashik, in the Indian state of Maharashtra. This fort can be visited in a day from Nashik. The nearest town is Satana. History. The history is similar to the Salher and Mulher forts. The fort was ruled by King Gawali. This fort was under the control of Maratha empire until it was captured by British forces in 1818. Places to see.

Geographic entities mentioned:
surface_form: Salher
instance_of: Mountain
countries: India
coordinates: lat: 20.72472222
lon: 73.94277778
Geography. The Blanche River originates in the mountains on the north shore of Lake Breeches, in the municipality of Saint-Jacques-le-Majeur-de-Wolfestown. This head area is located southeast of the “Chalet Hill” (altitude:), at southeast of the village of Saint-Jacques-le-Majeur-de-Wolfestown and northeast of Breeches Lake. The Blanche River empties on the west bank of the rivière au Pin.

Geographic entities mentioned:
surface_form: Breeches Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.9075
lon: -71.476666666667