Sarmila/GeoWiki-Features huggingface dataset:
The main rock formations in the lake's watershed include Burgoon Sandstone and the Mauch Chunk Formation. The lake is dammed by the Lake Jean Dam and is owned by the Pennsylvania Department of Conservation and Natural Resources. Lake Jean historically had a low pH due to impairment by atmospheric deposition. The lake has become less acidic, but continues to be impaired by mercury.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The lake was named by Colonel R. Bruce Ricketts in 1905 after Jean Holberton Ricketts, his eldest daughter. A new dam was created for it in the 1950s. In 2015, the lake was partially drained so that repair work could be done on the control tower of the Lake Jean Dam. Lake Jean is stocked with trout and contains various species of warmwater game fish and panfish.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
A new dam was created for it in the 1950s. In 2015, the lake was partially drained so that repair work could be done on the control tower of the Lake Jean Dam. Lake Jean is stocked with trout and contains various species of warmwater game fish and panfish. The large tracts of forest in the lake's watershed are mainly deciduous, but there is some coniferous forest.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Its main uses are recreation and fishing and it is one of the common destinations of visitors to Ricketts Glen State Park, in which it is located. Geography. The main outflow of Lake Jean is an unnamed tributary of Kitchen Creek. Its inflows include unofficially named streams such as &quot;Beaver Tributary&quot; and &quot;Ganoga Tributary&quot;, as well as direct drainage.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The lake has a highly irregular shape. Its maximum length is and its maximum width is. The largest inflow to Lake Jean is the outlet of Ganoga Lake, which is northwest of Lake Jean. Drainage from a tract of wetland also flows into the lake. There are several coves and inlets on the lake, especially on its western side, where there are also some wetlands. The lake also has a few islands.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The lake is located within Ricketts Glen State Park. It is in the northernmost part of the watershed of Fishing Creek. The main rock formation in the watershed of Lake Jean is the Burgoon Sandstone, which contains interbedded gray shale, conglomerate, and mudstone. However, a small patch of the Mauch Chunk Formation occurs in the northern part of the watershed.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The only soil in the watershed is the Wellsboro-Oquaga-Morris Association. However, the Lackawanna-Arnot-Morris Association occurs near the watershed's southwestern border. Lake Jean is dammed by the earthen Lake Jean Dam, which is high and long. As of 1980, the dam and its eastern and western dikes can handle 73 percent of the probable maximum flood without overtopping.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
By 2007, the pH had increased to 6.5 to 7.4, within Pennsylvania's criteria for pH. However, the lake is still impaired by mercury from atmospheric deposition. The hydraulic retention time of water in Lake Jean is 0.6 years. The average discharge of the lake's outflow is 3.6 cubic feet per second. On August 6, 1974, the water temperature of the lake at a depth of was.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The Secchi depth of the lake was measured to be in the 1970s. The specific conductance at this time ranged from 32 to 33 micro-siemens per centimeter at. The daily load of acidity at the outflow of Lake Jean is. The total maximum daily load of acidity at this point is. The lake's various inflows require an 87 to 97 percent reduction to meet their total maximum daily load requirements.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
In the 1970s, two measurements of water hardness in the lake were 5 and 8 milligrams per liter. In the 1970s, two measurements of the concentration of hydrogen ions in Lake Jean ranged from 0.00020 to 0.00160 milligrams per liter. The dissolved oxygen concentration was 9.5 milligrams per liter and the carbon dioxide concentration ranged from 0.6 to 5.1 milligrams per liter.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
The concentration of silica ranged between 0 and 0.1 milligrams per liter. In the 1970s, two measurements of the sodium concentration in filtered waters of Lake Jean ranged from 1.10 to 3.50 milligrams per liter. The potassium concentration was twice measured to be 0.60 milligrams per liter.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Bruce Ricketts' logging industry. However, a natural lake was originally in that location. Boating and fishing were being done on the lake as early as the early 1900s. In 1958, the Pennsylvania Fish Commission declared Lake Jean unsuitable for fishing, as its fish population was unbalanced. Fishing in the lake was forbidden until 1961, as attempts were made to chemically reclaim the lake.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Fishing in the lake was forbidden until 1961, as attempts were made to chemically reclaim the lake. The Pennsylvania Department of Environmental Resources added 106 tons of cement stack dust to the lake's frozen surface in the winter of 1959 for this purpose. In 1995, the Pennsylvania Department of Conservation and Natural Resources began adding lime to Lake Jean to combat its acidity.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
In June 2015, the lake will be entirely drained to repair the dam's control tower. It will take about two weeks to drain the lake, though a stream of water will still flow through its deepest parts. In 2015, the project was expected to cost $800,000. Lake Jean was reopened in May 2016. Biology. Lake Jean is listed on the Luzerne County Natural Areas Inventory.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Lake Jean was reopened in May 2016. Biology. Lake Jean is listed on the Luzerne County Natural Areas Inventory. Warmwater game fish and panfish inhabit Lake Jean. Specific fish in the lake include trout, smallmouth bass, largemouth bass, crappie, bluegill, and pickerel. Additionally, pumpkinseed and yellow perch have been observed within the lake. It is stocked with trout.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
Recreation. Lake Jean is mainly used for recreation and fishing. According to &quot;Times Leader&quot;, most of the 330,000 annual visitors to Ricketts Glen State Park visit Lake Jean. In 2014, the Pennsylvania Fish and Boat Commission temporarily lifted fishing restrictions in Lake Jean in preparation for the lake's draining. Ice fishing is permitted on the lake in the wintertime.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
There are picnic facilities along Lake Jean. Jeff Mitchell's book &quot;Paddling Pennsylvania: Canoeing and Kayaking the Keystone State's Rivers and Lakes&quot; describes Lake Jean as being &quot;known for its beauty&quot; and &quot;one of the finest lakes for paddling in Pennsylvania&quot;. The 0.8-mile-long Beach Trail at Ricketts Glen State Park goes along Lake Jean.

Geographic entities mentioned:
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
surface_form: lake jean
instance_of: Lake
countries: United States
coordinates: lat: 41.34111111
lon: -76.29083333
It also connects with Highway 981. It is about long. Highway 980 traverses the Porcupine Provincial Forest in the Porcupine Hills and it is the main access to several lakes including Townsend, Isbister, Elbow, Spirit, Smallfish, and Woody. The highway follows Woody River, Midnight Creek, and Little Armit River for much of its route through the Porcupine Hills.

Geographic entities mentioned:
surface_form: Townsend
instance_of: Lake
countries: Canada
coordinates: lat: 52.48334
lon: -101.75046
surface_form: Isbister
instance_of: Lake
countries: Canada
coordinates: lat: 53.30005
lon: -106.85057
surface_form: Smallfish
instance_of: Lake
countries: Canada
coordinates: lat: 52.40001
lon: -101.65045
surface_form: Woody
instance_of: Lake
countries: Australia
coordinates: lat: -33.81361111
lon: 121.91444444
It also connects with Highway 981. It is about long. Highway 980 traverses the Porcupine Provincial Forest in the Porcupine Hills and it is the main access to several lakes including Townsend, Isbister, Elbow, Spirit, Smallfish, and Woody. The highway follows Woody River, Midnight Creek, and Little Armit River for much of its route through the Porcupine Hills.

Geographic entities mentioned:
surface_form: Woody River
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1583
lon: -101.60919
surface_form: Midnight Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.50002
lon: -101.71762
Plot. 12-year-old Bird has moved with her single mom Jenny from a San Fernando Valley suburb to a neighborhood in Echo Park. Compounding this transition is the arrival of Bird's first period, which makes itself embarrassingly known at a school picnic. Bird and her free-spirited, impulsive mom both learn about what it means to become a woman. Reception.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
It is one of two clear-channel stations in Philadelphia, the other being sister station KYW. Its signal covers the Philadelphia metropolitan area and much of the Lehigh Valley region of eastern Pennsylvania and parts of New Jersey, Delaware, and Maryland. At night, it can be received in much of the Eastern United States and Eastern Canada with a good radio.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Road KP-21 passes by the southern lakeshore. Zhaksybay was named after a Kazakh person. Geography. Zhaksybay is an endorheic lake located in the southern sector of the Turgay Plateau between the sources of the Ulkayak and the Tobol rivers. The lake lies at an elevation of. Small lake Batpakkol lies to the east of the southeastern shore and is connected to it by a channel.

Geographic entities mentioned:
surface_form: Turgay Plateau
instance_of: Mountain
Plateau
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 51
lon: 63
surface_form: zhaksybay
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 51.5399
lon: 63.382
Its shores are irregular, mostly flat and swampy, but rocky in the south. The bottom is muddy. The lake freezes between November and April. Lake Akmolakol lies to the northeast, Urkash to the southwest, and Zharman to the east. Flora and fauna. The lake basin is surrounded by steppe vegetation and is used for grazing local cattle. The water is fresh in the spring.

Geographic entities mentioned:
surface_form: Zharman
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.583333333333336
lon: 64.45
Zhaksybay (lake). Zhaksybay () is a lake in Nauyrzym District, Kostanay Region, Kazakhstan. The lake is located to the northeast of Razdolnoye. Road KP-21 passes by the southern lakeshore. Zhaksybay was named after a Kazakh person. Geography. Zhaksybay is an endorheic lake located in the southern sector of the Turgay Plateau between the sources of the Ulkayak and the Tobol rivers.

Geographic entities mentioned:
surface_form: zhaksybay
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 51.5399
lon: 63.382
Zhaksybay () is a lake in Nauyrzym District, Kostanay Region, Kazakhstan. The lake is located to the northeast of Razdolnoye. Road KP-21 passes by the southern lakeshore. Zhaksybay was named after a Kazakh person. Geography. Zhaksybay is an endorheic lake located in the southern sector of the Turgay Plateau between the sources of the Ulkayak and the Tobol rivers. The lake lies at an elevation of.

Geographic entities mentioned:
surface_form: zhaksybay
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 51.5399
lon: 63.382
The lake lies at an elevation of. Small lake Batpakkol lies to the east of the southeastern shore and is connected to it by a channel. Zhaksybay has a roughly oval shape, with an inlet in the north, and a maximum length of approximately. Its shores are irregular, mostly flat and swampy, but rocky in the south. The bottom is muddy. The lake freezes between November and April.

Geographic entities mentioned:
surface_form: zhaksybay
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 51.5399
lon: 63.382
The Kuselbach valley floor lies at 215 m above sea level. Prominent elevations on the Kuselbach's right bank are the Rammelsbacher Kopf (256 m) and the Remigiusberg (368 m), while over on the left bank is the Hinzigberg, which near the Schlichterhof reaches a height of almost 300 m. The great basalt quarry, locally known as “Dimpel”, spreads over the whole Rammelsbacher Kopf.

Geographic entities mentioned:
surface_form: Remigiusberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.5225
lon: 7.44067
Zindlenspitz. The Zindlenspitz (2,097 m) is a mountain of the Schwyzer Alps, located on the border between the Swiss cantons of Schwyz and Glarus. It lies on the range between the Wägitalersee and the Obersee, south of the Brünnelistock.

Geographic entities mentioned:
surface_form: Wägitalersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.089444444444
lon: 8.9211111111111
surface_form: Brünnelistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.084188888889
lon: 8.9725611111111
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.08695
lon: 9.0137777777778
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.2189
lon: 8.84657
surface_form: obersee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.7845
lon: 9.68147
Zindlenspitz. The Zindlenspitz (2,097 m) is a mountain of the Schwyzer Alps, located on the border between the Swiss cantons of Schwyz and Glarus. It lies on the range between the Wägitalersee and the Obersee, south of the Brünnelistock.

Geographic entities mentioned:
surface_form: zindlenspitz
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.076277777778
lon: 8.9611138888889
state of Tennessee. Via the Big South Fork and the Cumberland and Ohio rivers, it is part of the Mississippi River watershed. The New River rises on Frozen Head, a notable mountain of Morgan County, Tennessee. Named for its frequent winter appearance, Frozen Head is the focal point of Frozen Head State Park and Natural Area.

Geographic entities mentioned:
surface_form: Frozen Head
instance_of: Mountain
countries: United States
coordinates: lat: 36.1225
lon: -84.457777777778
The Joaquin Rocks are at an elevation of, and are the most distinguishing feature of Joaquin Ridge. The three pillars of rock are clearly visible on the ridge for many miles from many directions in the San Joaquin Valley and from their summits have a view of much of the valley. It is located, west-northwest of Black Mountain (Anticline Ridge) and southwest of Ragged Valley. History.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The Joaquin Rocks are at an elevation of, and are the most distinguishing feature of Joaquin Ridge. The three pillars of rock are clearly visible on the ridge for many miles from many directions in the San Joaquin Valley and from their summits have a view of much of the valley. It is located, west-northwest of Black Mountain (Anticline Ridge) and southwest of Ragged Valley. History.

Geographic entities mentioned:
surface_form: Ragged Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.361666666666665
lon: -120.42361111111111
He had previously been a member of the Parti Québécois. In the 1984 election, he said he was on a secret mission &quot;to survey Lake Winnipeg to find out how we can flush out the next of crows&quot; that were affecting Canada's freight rates (this was a comical reference to the Crow Rate). Ouellet received 2,152 votes (3.63%), finishing fourth against Liberal candidate Alfonso Gagliano.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Description and current usage. Since 1936, through negotiations initiated by The Birmingham Civic Society with the owner, Calthorpe Estates, it has been the clubhouse for Edgbaston Golf Club. Edgbaston Hall, and its lodge house, are Grade II listed buildings. The grounds, which includes Edgbaston Pool, are now divided into an 18-hole golf course and a nature reserve. History.

Geographic entities mentioned:
surface_form: Edgbaston Pool
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.4548
lon: -1.9211
Despite their small size these trees can exceed 165 years at breast height. Rivers and streams. Cattaraugus Creek is a fifth to sixth-order stream (depending upon the exact delineation of headwater tributaries), and is the largest tributary to eastern Lake Erie. Flow is highly variable, and can range from typical summer lows of less than to floods exceeding.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The cliffs along Zoar Valley's gorges are composed of Devonian silt stones and shale, and are part of the Canadaway Formation. The valley's gorges expose stratifications of the Onondaga Escarpment. Cliffs near the confluence of Cattaraugus Creek's South and Main branches reach heights of up to when measured to the tops of nearby hills. History.

Geographic entities mentioned:
surface_form: onondaga
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Zoar Valley. Zoar Valley is an area of deep gorges along the Main and South branches of Cattaraugus Creek in western New York, United States. The valley is located along the border of Erie County and Cattaraugus County, roughly between the villages of Gowanda to the west and Springville to the east.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
The valley is located along the border of Erie County and Cattaraugus County, roughly between the villages of Gowanda to the west and Springville to the east. The core area surrounding the confluence of the Cattaraugus Creek's Main and South branches is protected as the Zoar Valley Multiple Use Area, a conservation area located within the towns of Collins, Otto, and Persia.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
The protected area is managed by the New York State Department of Environmental Conservation, and is open to the public for fishing, hunting, hiking, white-water rafting, and wildlife and scenic viewing. Canyon depths within the Zoar Valley Multiple Use Area are the greatest within the entire Cattaraugus Creek corridor, ranging up to along the South Branch and along the Main Branch.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Several nearly vertical rock faces approach in height. The property also contains large stands of old-growth forest with trees of unusual size and height, which are further protected as part of the state-designated Zoar Valley Unique Area. Geography and geology.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Geography and geology. Zoar Valley is located along the border of Erie County and Cattaraugus County in New York, roughly between the villages of Gowanda to the west and Springville to the east. Cattaraugus Creek flows through the valley. An additional gorge formed by the Cattaraugus Creek's South Branch stretches south toward the village of Cattaraugus.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Cattaraugus Creek flows through the valley. An additional gorge formed by the Cattaraugus Creek's South Branch stretches south toward the village of Cattaraugus. The cliffs along Zoar Valley's gorges are composed of Devonian silt stones and shale, and are part of the Canadaway Formation. The valley's gorges expose stratifications of the Onondaga Escarpment.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
The valley's gorges expose stratifications of the Onondaga Escarpment. Cliffs near the confluence of Cattaraugus Creek's South and Main branches reach heights of up to when measured to the tops of nearby hills. History. Zoar Valley was named by Ahaz Allen, an early 19th-century settler of the region. The name is of biblical origin, referring to the city of Zoar from the Book of Genesis.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
surface_form: allen
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
The name is of biblical origin, referring to the city of Zoar from the Book of Genesis. The extent of Zoar Valley's use by Native Americans is unclear due to subsequent disturbance by farming and settlement activities; however, findings from nearby archaeological sites suggest that indigenous peoples likely made use of the area.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Land management. The state-managed Zoar Valley Multiple Use Area encompasses a area along an section of the Cattaraugus Creek's Main Branch canyon and a stretch of the smaller South Branch, centered around the confluence of the two streams. The Multiple Use Area is maintained by the New York State Department of Environmental Conservation.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
In 2007, the state established the Zoar Valley Unique Area, a area which further protects and preserves the entire state-owned length of the gorge's cliffs and bottomlands, in addition to a buffer area along the gorge's upper rim and along several larger side creeks, where sufficient state-owned land is available.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Within the Unique Area, activities such as logging and gas drilling are prohibited. Prior to being designated as a Unique Area, the old-growth forest within the state-owned portion of Zoar Valley was at danger of being logged; the additional protection was the result of lobbying by activists and local residents.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Traditional natural resource management activities, including logging, are permitted to take place outside of the Unique Area. Approximately of plantation forests were established within the Zoar Valley Multiple Use Area during the 1960s and 1970s. Most are composed of non-native conifers, although several native hardwood plantations are present as well.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
An American chestnut plantation is also maintained as a joint venture with the American Chestnut Foundation, with the goal of developing chestnut blight-resistant trees. Additional protected lands within Zoar Valley include The Nature Conservancy's Deer Lick Nature Sanctuary, which preserves of old-growth forest and was designated as a National Natural Landmark in 1967.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Additional protected lands within Zoar Valley include The Nature Conservancy's Deer Lick Nature Sanctuary, which preserves of old-growth forest and was designated as a National Natural Landmark in 1967. The sanctuary is located along the Cattaraugus Creek's South Branch, adjacent to the Zoar Valley Multiple Use Area. Two other privately owned conservation areas, the William P.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Old-growth forests. Forests within Zoar Valley include some of the finest old-growth stands in the eastern United States. Throughout Zoar Valley, a total of of old-growth forest has been recorded; of this, nearly are found within the Zoar Valley Multiple Use Area, with an additional located in the adjacent Deer Lick Nature Sanctuary.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Old-growth forests. Forests within Zoar Valley include some of the finest old-growth stands in the eastern United States. Throughout Zoar Valley, a total of of old-growth forest has been recorded; of this, nearly are found within the Zoar Valley Multiple Use Area, with an additional located in the adjacent Deer Lick Nature Sanctuary.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Ecological integrity and environmental health of the Cattaraugus are generally good. The river edge and immediate riparian zone are largely intact for most of the river's length. There is only one dam on the main stream, located within Scoby Dam Park about upstream from the Zoar Valley Multiple Use Area. Although a barrier to fish, it does not regulate flow.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
During summer storm events, especially after a prolonged dry period, bacterial levels can exceed 10,000 colony forming units (cfu); bacterial levels are low most other times. Numerous small waterfalls cascade into the Zoar Valley canyon. Most are cascades, but there are a few straight drops of greater than. Above the falls are dozens of small headwater streams that drain the surrounding uplands.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
These streams and the Cattaraugus Creek were extensively disturbed by an intense flash flood in August 2009. Recreation. Zoar Valley is a popular regional destination for outdoor recreation. The Zoar Valley Multiple Use Area is open to the public for activities including fishing, hunting, hiking, white-water rafting, and nature study.

Geographic entities mentioned:
surface_form: zoar valley
instance_of: Valley
countries: United States
coordinates: lat: 42.4397
lon: -78.8733
Zoar Valley's old growth is primarily deciduous, and varies in character and species composition depending upon location and landform characteristics. Northern hardwood stands, including eastern hemlock, sugar maple, American beech, yellow birch, northern red oak, and tulip tree, are widespread, especially on mesic north-facing slopes and on the lower reaches of south-facing slopes.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Zoar Valley. Zoar Valley is an area of deep gorges along the Main and South branches of Cattaraugus Creek in western New York, United States. The valley is located along the border of Erie County and Cattaraugus County, roughly between the villages of Gowanda to the west and Springville to the east.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Geography and geology. Zoar Valley is located along the border of Erie County and Cattaraugus County in New York, roughly between the villages of Gowanda to the west and Springville to the east. Cattaraugus Creek flows through the valley. An additional gorge formed by the Cattaraugus Creek's South Branch stretches south toward the village of Cattaraugus.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Evidence of early use by settlers includes records of farming as early as 1842, in addition to evidence of shale mining and the establishment of two lime kilns during the early 1800s. Sawmills, gas wells, and a cheese factory were also established in the valley during the 19th century. A Boy Scout camp was formerly located near the confluence, and a cable car was used to cross Cattaraugus Creek.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Foundations of several camp buildings remain visible. The Niagara, Lockport and Ontario Power Company purchased property near the confluence in 1926, with the intention of building a hydroelectric dam in the valley. However, the brittleness of the valley's shale cliffs was found to be unsuitable for construction of the dam, and the project was abandoned.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The Niagara, Lockport and Ontario Power Company purchased property near the confluence in 1926, with the intention of building a hydroelectric dam in the valley. However, the brittleness of the valley's shale cliffs was found to be unsuitable for construction of the dam, and the project was abandoned. State ownership within the valley began in 1961 with the gift of by Herbert F.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
However, the brittleness of the valley's shale cliffs was found to be unsuitable for construction of the dam, and the project was abandoned. State ownership within the valley began in 1961 with the gift of by Herbert F. Darling Sr., who had purchased land from the Niagara Mohawk Power Corporation in 1952 with the intention of preserving the property.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Additional lands were later added under the 1960 Multiple Use Bond Act. For a time in the 1960s, a hippie commune was located within the valley. By 1971, overnight use of the property was prohibited due to &quot;irresponsible behavior on the part of some campers&quot;. Land management.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Two other privately owned conservation areas, the William P. Alexander Preserve and the Rodger Sweetland Memorial Preserve, are owned by the Nature Sanctuary Society of Western New York. Outside of these protected areas, old-growth forests in the valley are unprotected, and some have been clearcut in recent years. Old-growth forests.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Ouseburn. The wooded gorge of the Ouseburn in the east of the city is known as Jesmond Dene and forms another recreation area, linked by Armstrong Park and Heaton Park to the Ouseburn Valley, where the river finally reaches the River Tyne. The springtime dawn chorus at 55 degrees latitude has been described as one of the best in the world.

Geographic entities mentioned:
surface_form: Jesmond Dene
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.99
lon: -1.59
surface_form: Ouseburn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.974
lon: -1.59
The springtime dawn chorus at 55 degrees latitude has been described as one of the best in the world. The dawn chorus of the Jesmond Dene green space has been professionally recorded and has been used in various workplace and hospital rehabilitation facilities. Quayside.

Geographic entities mentioned:
surface_form: Jesmond Dene
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.99
lon: -1.59
The new building opened on 21 June 2009 and was named after the 18th-century local composer Charles Avison; the building was first opened by Dr Herbert Loebl. Later that year it was officially opened by Queen Elizabeth II. Seven Stories, the National Centre for Children's Books, opened in 2005 in the Ouseburn Valley. Festivals and fairs.

Geographic entities mentioned:
surface_form: Ouseburn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.974
lon: -1.59
The small music venue Think Tank? was a nominee for Best Small Venue in NME in 2015. The Cluny in Ouseburn Valley is &quot;one of the most important venues for breaking bands in the region&quot;. Trillians Rock Bar is well-noted for its rock and metal shows, and The Head of Steam is a 90-capacity basement venue described as &quot;one of Newcastle's staple venues&quot;. Independent cinema.

Geographic entities mentioned:
surface_form: Ouseburn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.974
lon: -1.59
The cave descends several hundred feet below the surface, where an underground river, grottos, and chimneys can be found. The underground stream is supplied by a large underground lake located beneath English Mountain. The temperature inside the caverns remains at a near-constant 58 degrees and tends to stay the same year-round.

Geographic entities mentioned:
surface_form: English Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9007
lon: -83.2977
After graduation, he worked for General Electric in Canada, where he worked on water management. He then attended University of Wisconsin–Madison, where he graduated with a PhD in environmental engineering in 1978. His PhD project involves the study of Polychlorinated biphenyls in Lake Michigan at the University of Wisconsin–Madison.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Early life and education. Miller was born on June 14, 2000 in Portland, Oregon, in the United States, where he also spent his childhood. His father is Kelly Miller, a ski patroller in Mount Hood while his mother is Polly Bisquera whose roots traces to Santa Cruz, Manila, in the Philippines. His first experience in skiing was when he was 1½ years old.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Potawatomi Islands. The Potawatomi Islands is the most common historic name given to the string of islands that delineate the transition from Green Bay to Lake Michigan, one of the Great Lakes. The archipelago is also termed the &quot;Grand Traverse Islands&quot;. The largest of the islands is Washington Island, in Door County, Wisconsin.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Additionally, a hurricane watch was issued from Chokoloskee to Tarpon Springs. On September 14, a tropical storm warning was issued for Lake Okeechobee and the Florida east coast from Jupiter to Saint Augustine. Due to the storm, schools in six counties along the west coast were closed. All aircraft from MacDill Air Force Base were evacuated to Kansas as a precaution.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
In 1939–46, I looked at many areas, which include East Africa (especially Tanganyika), the Mingan Territory in Quebec, the Peace River Valley in Alberta, the Matanuska Valley in Alaska, the New Hebrides in the Pacific, and British Guiana in South America. About three years ago I concentrated on British Honduras.

Geographic entities mentioned:
surface_form: Matanuska Valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
I Squadron was back in Kiel by 11 August, though the late arrival of the s delayed the participation of I Squadron in the annual autumn fleet training. The maneuvers began with exercises in the German Bight, followed by a mock attack on the fortifications in the lower Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Helenesee. Helenesee is a lake in Brandenburg, Germany. Its surface area is ca. 250 ha. With a depth of 56.63 m, the Helenseee is the second deepest lake in Brandenburg, only surpassed by the lake Großer Stechlinsee. It is situated approximately 8 kilometers in the south of Frankfurt (Oder). It was formed after the flooding of a former open-pit mining which started in 1958.

Geographic entities mentioned:
surface_form: helenesee
instance_of: Lake
countries: Germany
coordinates: lat: 52.271111111111
lon: 14.4875
At first, the Prussians kept good discipline, but it soon became a general rout. With the battle over, the Tirailleurs were able to rest, having been able to rout an entire army. North West Push. By 22 October, the two bridgeheads over the Elbe were taken and the Cavalry Reserve, IV, and VI Corps were closing into the fortress of Magdeburg.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The border follows that river to the Amur River, and to the confluence of the latter with the Ussuri River. It divides the Bolshoy Ussuriysky Island at the confluence of the two rivers, and then runs south along the Ussuri. The border crosses Lake Khanka, and finally runs to the south-west. The China–Russia border ends when it reaches the Tumen River, which is the northern border of North Korea.

Geographic entities mentioned:
surface_form: Lake Khanka
instance_of: Lake
countries: Russia
People's Republic of China
Russian Empire
Soviet Union
coordinates: lat: 45.016666666667
lon: 132.41666666667
Its western end point is the China–Kazakhstan–Russia tripoint, whose location is defined by the trilateral agreement as, elevation, 3327 m. Its eastern end is the western China–Mongolia–Russia tripoint, at the top of the peak Tavan Bogd Uul (Mt Kuitun), at the coordinates, elevation 4374 m. Sino-Soviet border (1917–1991).

Geographic entities mentioned:
surface_form: Tavan Bogd
instance_of: Mountain
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 49.145833333333
lon: 87.819166666667
Talkin. Talkin is a village in Cumbria, England, close to Talkin Tarn. Toponymy. The name is of Brittonic origin. The Brittonic dialect known as Cumbric was formerly spoken in the area. According to A. M. Armstrong, et al., the first element, &quot;tal&quot;, means &quot;brow&quot; or &quot;end&quot; in Brittonic and modern Welsh, Cornish, and Breton. The second element is unclear.

Geographic entities mentioned:
surface_form: Talkin Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.922
lon: -2.71
First Division. The First Division's California route north from Los Angeles followed the Stockton - Los Angeles Road that was established as a southern route to the goldfields during the California Gold Rush. The route went through the San Fernando Valley, with a stop at Rancho Los Encinos.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The route went through the San Fernando Valley, with a stop at Rancho Los Encinos. It proceeded over Fremont Pass out of the Valley, up San Francisquito Canyon and over San Francisquito Pass, to the Fort Tejon Pass, where it dropped to the San Joaquin Valley. The Butterfield route split off the Stockton - Los Angeles Road at Elkhorn Spring Station.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Louis Ranch). It crossed over the Diablo Mountains at Pacheco Pass to reach to Gilroy. It then proceeded north through the Santa Clara Valley and San Jose, to its western terminus in San Francisco, also the headquarters of the First Division of the Butterfield Overland Mail. Second Division.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
The Mexican route also provided stations with water in the Sonoran Desert, from the Colorado River's spring flooding into the Alamo River and New River. The route then reentered California to cross the Yuha Desert, and proceeded through the present day Carrizo Impact Area, then up Carrizo Wash through the Carrizo Badlands, to Carrizo Springs Station.

Geographic entities mentioned:
surface_form: Carrizo Badlands
instance_of: Landform
countries: United States
coordinates: lat: 32.8517
lon: -116.137
About 2.5 km north of Eschenstruth, in the area of the Söhre (Stiftswald Kaufungen), the Bielstein (528.7 m above sea level) rises with its approximately 15‑m‑high basalt column known as the Bilsteinkirche. Slightly to the west stands the Michelskopf (about 485 m above sea level), where former basalt quarries have given rise to the Michelskopf lakes.

Geographic entities mentioned:
surface_form: Michelskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.252222222222
lon: 9.6502777777778
Production. The character of Yately comes from Blaenllechau in the Rhondda, near actor Stanley Baker's birthplace of Ferndale. Footage of a Hawlett's lorry going over the edge of a quarry was reused in &quot;The Heiress&quot; episode of the Rank Organisation television series &quot;Interpol Calling&quot;.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
These punitive operations have now become known as the Nebo killings of early 1869. In March of the same year, Johnstone was again out with his troops endeavouring to punish &quot;the blacks&quot; after the killing of a Chinese shepherd at Mt Heilcalong station near Lake Elphinstone. Property manager at Bellenden Plains. Johnstone resigned from the Native Police in 1869.

Geographic entities mentioned:
surface_form: Lake Elphinstone
instance_of: Lake
countries: Australia
coordinates: lat: -21.533333333333
lon: 148.23333333333
Again this area was found to be populated by Aboriginals with numerous gunyah style houses, rafts and canoes observed along the banks. Johnstone and a number of troopers set out from here and managed to climb to the summit of Mount Bellenden Ker. At Constantine Point at the mouth of the Mulgrave River, Johnstone found a large gunyah and stole the mummified remains of an Aboriginal woman from it.

Geographic entities mentioned:
surface_form: Mount Bellenden Ker
instance_of: Mountain
countries: Australia
coordinates: lat: -17.264166666667
lon: 145.85388888889
After serving in World War I, Day returned to his hometown; continuing to work as an artist. An avid outdoors man, he hiked the Katahdin region of Northern Maine long before it had trails. His adventures were featured in many outdoor sporting stories by Edmund Ware Smith; which Day also illustrated.

Geographic entities mentioned:
surface_form: Katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275