Sarmila/GeoWiki-Features huggingface dataset:
The main entrance area consisted of a bathhouse and picnic grounds near the beach. The lake was the site of city-sponsored swim meets for children in the 1920s. Eventually, due to the lake's growing popularity, the facilities at Crystal Lake had to be expanded. In 1942 a new bathhouse was constructed and the beach was extended by the Works Progress Administration.

Geographic entities mentioned:
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
In 1987, the fieldstone-constructed bathhouse underwent a renovation sponsored by the City Parks and Recreation Department and still stands at the site today. Hermit of Mosquito Pond. The story of the Hermit of Mosquito Pond is about a man who lived secluded on Crystal Lake for 60 years. Charles Alan Lambert came to Manchester in the 1840s.

Geographic entities mentioned:
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
Over the years his hermit lifestyle made him into a kind of local celebrity, and he became the object of great curiosity. Despite his secluded lifestyle he would be visited by hundreds of people every summer. Mr. Lambert lived at his hermit homestead for over 60 years, spending the last two years of his life with the Sisters of Mercy at the House of St. John for aged men.

Geographic entities mentioned:
surface_form: the sisters
instance_of: Mountain
countries: United States
coordinates: lat: 36.331111111111
lon: -115.68388888889
Campus. The UWM campus is located in a residential area on Milwaukee’s upper East Side. The campus is five blocks from the shoreline of Lake Michigan, and is less than a ten-minute drive from downtown Milwaukee. The Milwaukee County Transit System provides the campus with access to public bus transportation in Milwaukee. The campus is divided into central, north, west, and northwest quads.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
She held a prominent political role, and was considered &quot;head and counsel of advice to the gentlemen and chiefs of Ulster&quot;. Biography. Her father was Cúconnacht Maguire, Lord of Fermanagh. On 8 October 1537, Cúconnacht was murdered on the island of Craghan in Lough Erne. Siobhán was married three times. Her first husband was Feardorcha &quot;Matthew&quot; O'Neill, 1st Baron Dungannon.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Dam failure. On 19 May 2020 at 17:46 EDT heavy rainfall pushed inflows far beyond design capacity and the east embankment of Edenville Dam gave way. Immediate, mandatory evacuations were ordered for residents of Edenville and nearby Sanford. Roughly downstream the impounded water overtopped – but did not breach – the Sanford Dam, forcing the evacuation of much of Midland another downstream.

Geographic entities mentioned:
surface_form: Sanford Dam
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -84.383333333333
In the Northern Cape, the formation is intruded by dolerite sills. The sediments are considered to be deposited in an anoxic environment. Besides pyrite, the shales contain dolomite lenses near the base. The rocks are highly folded and faulted by the Cape orogeny forming the Cape Fold Belt, and thus, interpreted as &quot;decollement&quot;. Depositional environments.

Geographic entities mentioned:
surface_form: Cape Fold Belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
These rocks can therefore be classified as overmature, likely because of the thermotectonic processes related to the Cape orogeny forming the Cape Fold Belt overprint on lower Karoo rocks in the study area. It is possible that the maturity of the shales decreases farther north in the Karoo basin.

Geographic entities mentioned:
surface_form: Cape Fold Belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
It rises to about 300 metres above sea level and is not open to the public. It is covered in remnant bushland and is easily visible from Saddleback Mountain. It is named after an early settlement on the banks of the Shoalhaven known as Coolangatta and is only indirectly related to the better-known Coolangatta, Queensland. Protected status.

Geographic entities mentioned:
surface_form: saddleback mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -34.7
lon: 150.8
Coolangatta Mountain. Coolangatta Mountain, also known as Cullunghutti, is a small mountain rising from the Shoalhaven River Plain in New South Wales. It rises to about 300 metres above sea level and is not open to the public. It is covered in remnant bushland and is easily visible from Saddleback Mountain.

Geographic entities mentioned:
surface_form: coolangatta mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -34.8435
lon: 150.7154
Protected status. The NSW National Parks & Wildlife Service undertook a cultural study of the area around Coolangatta Mountain in 2004, which documented the mountain's significance to Aboriginal peoples. In 2008, the Office of Environment & Heritage purchased a parcel of on its slopes after consulting with local Aboriginal representatives.

Geographic entities mentioned:
surface_form: coolangatta mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -34.8435
lon: 150.7154
She had no interest in food.&quot;
She is the mother of two children, Nicholas Wolfert and Leila Wolfert. She is married to crime fiction writer William Bayer. They live in the Hudson Valley, NY. Alzheimer's activist. In late 2013 she said that she had been diagnosed with MCI (Mild Cognitive Impairment), an early stage of Alzheimer's disease.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
The Appalachian Trail and Webster Cliff Trail approach from Mount Jackson in the south and meet Crawford Path just north of the summit before continuing to the northeast. Mount Eisenhower and Mount Monroe lie on the ridge northeast of Mount Pierce. All three of these peaks are included on the peak-bagging list of four-thousand footers in New Hampshire.

Geographic entities mentioned:
surface_form: Mount Eisenhower
instance_of: Mountain
countries: United States
coordinates: lat: 44.240666666667
lon: -71.350333333333
surface_form: Mount Monroe
instance_of: Mountain
countries: United States
coordinates: lat: 44.255561111111
lon: -71.3225
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 40.416944444444
lon: -124.12083333333
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 44.226
lon: -71.366
The trail primarily follows the Crawford Path, the oldest continually used hiking trail in the United States. Crawford Path was established in 1819 by Abel and Ethan Crawford, who referred to the mountain as Bald Mountain. The Appalachian Trail and Webster Cliff Trail approach from Mount Jackson in the south and meet Crawford Path just north of the summit before continuing to the northeast.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
Mount Pierce (New Hampshire). Mount Pierce is a mountain in the Presidential Range in the White Mountains of New Hampshire that is approximately high.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 40.416944444444
lon: -124.12083333333
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 44.226
lon: -71.366
Mount Pierce (New Hampshire). Mount Pierce is a mountain in the Presidential Range in the White Mountains of New Hampshire that is approximately high.

Geographic entities mentioned:
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 40.416944444444
lon: -124.12083333333
surface_form: mount pierce
instance_of: Mountain
countries: United States
coordinates: lat: 44.226
lon: -71.366
Crawford Path was established in 1819 by Abel and Ethan Crawford, who referred to the mountain as Bald Mountain. The Appalachian Trail and Webster Cliff Trail approach from Mount Jackson in the south and meet Crawford Path just north of the summit before continuing to the northeast. Mount Eisenhower and Mount Monroe lie on the ridge northeast of Mount Pierce.

Geographic entities mentioned:
surface_form: webster
instance_of: Lake
countries: United States
coordinates: lat: 42.0425
lon: -71.843333333333
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 44.1945
lon: -71.3887
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 48.6006
lon: -113.722
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6525
lon: -110.836
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
surface_form: mount jackson
instance_of: Mountain
countries: United States
coordinates: lat: 39.4853
lon: -106.537
Mount Pierce is a mountain in the Presidential Range in the White Mountains of New Hampshire that is approximately high. Formerly called Mount Clinton for 19th-century governor DeWitt Clinton of New York, in 1913 it was renamed after President Franklin Pierce (1804–1869), the only president born in New Hampshire, although it was several decades before the name was widely recognized.

Geographic entities mentioned:
surface_form: mount clinton
instance_of: Mountain
countries: United States
coordinates: lat: 44.226
lon: -71.366
Its summit offers a wide view of New Hampshire's mountains. The shortest trail route to the summit of Pierce is from a parking lot to the west of the mountain on Mount Clinton Road just off Route 302. The trail primarily follows the Crawford Path, the oldest continually used hiking trail in the United States.

Geographic entities mentioned:
surface_form: mount clinton
instance_of: Mountain
countries: United States
coordinates: lat: 44.226
lon: -71.366
Atlanta straddles the Eastern Continental Divide, such that rainwater that falls on the south and east side of the divide flows into the Atlantic Ocean, while rainwater on the north and west side of the divide flows into the Gulf of Mexico. Atlanta sits atop a ridge south of the Chattahoochee River, which is part of the ACF River Basin.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Production. Originally, the idea was to portray two male characters, one of whom would mistake the other one for his wife, it took three years for the script to develop from the original idea of Fabrice du Welz. The film was shot in Belgium's Hautes Fagnes natural reserve and in the village of Bullange. Filming also took place in Mondorf-les-Bains, Luxembourg.

Geographic entities mentioned:
surface_form: Hautes Fagnes
instance_of: Plateau
countries: Belgium
Germany
coordinates: lat: 50.521389
lon: 6.102778
Its length is 36 km, of which 31 km are in Bulgaria and 5 km are in Serbia. The river takes its source at the foothills of the summit of Chekanska Buka (1,136 m), the highest peak of the Viskyar Mountain. It then flows near the village of Pishtane and received its tributary the Ozarnovska reka near the village of Povalirazh, flowing eastwards until that point.

Geographic entities mentioned:
surface_form: Viskyar Mountain
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.761111111111
lon: 22.944166666667
Kerch as a city starts its history in the 7th century BC, when Greek colonists from Miletus founded a city-state named Panticapaeum on Mount Mithridat near the mouth of the Melek-Chesme river. Panticapaeum subdued nearby cities and by 480 BC became the capital of the Kingdom of Bosporus.

Geographic entities mentioned:
surface_form: Mount Mithridat
instance_of: Mountain
countries: Russia
coordinates: lat: 45.348333333333
lon: 36.467222222222
Archaeology. Archaeological digs in Kerch were launched under Russian auspices in the middle of the 19th century. Since then the site of ancient Panticapaeum city on Mount Mithridat has been systematically excavated. Located nearby are several ancient burial mounds (kurgans) and excavated cities. Kerch takes part in UNESCO's &quot;Silk Road&quot; programme.

Geographic entities mentioned:
surface_form: Mount Mithridat
instance_of: Mountain
countries: Russia
coordinates: lat: 45.348333333333
lon: 36.467222222222
It takes the form of a northwest-southeast aligned ridge which rises to a height of 393m (1289 feet) and which overlooks the valley of the River Usk to the west and south. To the northeast are panoramic views across Llangorse Lake to the Black Mountains There is a viewfinder on the summit erected as a monument to Eirene Lloyd White, Baroness White of Rhymney.

Geographic entities mentioned:
surface_form: Llangorse Lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.930961111111
lon: -3.2627555555556
According to the Anglepoise website, these were so well produced that when a crashed Vickers Wellington bomber was salvaged from Loch Ness in Scotland in 1985, the lamp still worked after being given a new battery – despite being submerged for around four decades. A key feature of the Anglepoise design and patent is the placement of all springs (either three or four) near the base.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
When his grandfather died in 1453, Colin succeeded him to become 2nd Lord Campbell. Colin was still a minor and was placed in the custody of his uncle, Colin Campbell, 1st of Glenorchy. In 1457, he was created Earl of Argyll by King James II of Scotland, who was grateful for the loyalty of his father during the troubles early in his reign. In 1460, Campbell had a commission as Bailie of Cowal.

Geographic entities mentioned:
surface_form: Glenorchy
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.48
lon: -4.82
Hogan River. The Hogan River is a tributary of the Boisvert River (Normandin River), flowing into the unorganized territory of the Lac-Ashuapmushuan, Quebec, in the Regional County Municipality (RCM) of Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in Quebec, in Canada. This river crosses successively the cantons of Sarrasin and Rinfret.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: hogan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.826944444444
lon: -73.8825
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Hogan River. The Hogan River is a tributary of the Boisvert River (Normandin River), flowing into the unorganized territory of the Lac-Ashuapmushuan, Quebec, in the Regional County Municipality (RCM) of Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in Quebec, in Canada. This river crosses successively the cantons of Sarrasin and Rinfret.

Geographic entities mentioned:
surface_form: hogan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.826944444444
lon: -73.8825
The forest Road R1004 (heading northeast) that connects to route 167 serves the northwestern part of the Boisvert River (Normandin River) Valley (Normandin River) and the eastern part of the Armitage River. Forest Road R0210 (North–south direction) serves the eastern part of the Boisvert River (Normandin River) Valley and the southern Hogan River Valley.

Geographic entities mentioned:
surface_form: hogan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.826944444444
lon: -73.8825
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Forest Road R0210 (North–south direction) serves the eastern part of the Boisvert River (Normandin River) Valley and the southern Hogan River Valley. The surface of the Hogan River is usually frozen from early November to mid-May, however, safe ice movement is generally from mid-November to mid-April. Toponymy. The term &quot;Hogan&quot; is a family name of English origin.

Geographic entities mentioned:
surface_form: hogan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.826944444444
lon: -73.8825
The surface of the Hogan River is usually frozen from early November to mid-May, however, safe ice movement is generally from mid-November to mid-April. Toponymy. The term &quot;Hogan&quot; is a family name of English origin. The toponym &quot;Hogan River&quot; was formalized on March 28, 1972, at the Commission de toponymie du Québec, when it was created.

Geographic entities mentioned:
surface_form: hogan river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.826944444444
lon: -73.8825
This river crosses successively the cantons of Sarrasin and Rinfret. Forestry is the main economic activity of this valley; recreational tourism activities, second. The forest Road R1004 (heading northeast) that connects to route 167 serves the northwestern part of the Boisvert River (Normandin River) Valley (Normandin River) and the eastern part of the Armitage River.

Geographic entities mentioned:
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
surface_form: normandin river
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.203333333333
lon: -73.7975
Kutlovitsa Glacier. Kutlovitsa Glacier (,) is the 9.4 km long and 4.2 km wide glacier in southern Aristotle Mountains on Oscar II Coast in Graham Land, Antarctica situated north of Flask Glacier. It is draining the southeast slopes of Madrid Dome, and flowing southeastwards along the north slopes of Mount Fedallah to join Belogradchik Glacier.

Geographic entities mentioned:
surface_form: Mount Fedallah
instance_of: Mountain
coordinates: lat: -65.7167
lon: -62.8667
By day, KNWQ is powered at 10,000 watts. As 1140 AM is a clear-channel frequency, on which XEMR-AM in Monterrey and WRVA in Richmond share Class A status, KNWQ must reduce power at night to 2,500 watts to avoid interference. Programming is also heard on several FM translators in the Coachella Valley. Programming.

Geographic entities mentioned:
surface_form: Coachella Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.72
lon: -116.2
Lochend Loch (Coylton). Lochend Loch, which once had nearly three acres in surface area is now only a small freshwater loch remnant. It lies in the South Ayrshire Council Area, lying on the hill above Joppa, between Gallowhill and Lochend Farm. The loch.

Geographic entities mentioned:
surface_form: lochend loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.448709
lon: -4.510519
The loch. Lochend Loch was a post-glacial 'Kettle Hole' lying within a substantial depression and fed by the relatively minor flow of the Joppa Burn, field runoff and rainfall, its outflow running into the Water of Coyle as the Barwhey or Barquey Burn. A small islet is indicated on the early OS maps, no longer shown when the loch level was lowered in the late 1890s or early 1900s.

Geographic entities mentioned:
surface_form: lochend loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.448709
lon: -4.510519
Young Spanish Eclectic House on the southwest corner of Carmelo and 11th Avenue in Carmel. In 1935 Stanton opened an office in the Hotel Del Monte in Monterey, establishing a practice that included school and hospital work in the Monterey area and across the San Joaquin Valley. He collaborated closely with sculptor Joseph Jacinto Mora (1876–1947) on multiple projects.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Stanton met his wife Virginia Young (1903-1994) at University of California, Berkeley. They married on December 8, 1922 in Solano County, California. They had three children. Death. Stanton died at his home in Carmel Valley on September 1, 1983, at the age of 83.

Geographic entities mentioned:
surface_form: Carmel Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.4748315
lon: -121.7205075
Mount Armour. Mount Armour, also named Boundary Peak 175, is a mountain in Alaska and British Columbia, located on the Canada–United States border, and part of the Southern Icefield Ranges of the Saint Elias Mountains.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount armour
instance_of: Mountain
countries: Canada
coordinates: lat: 59.9077
lon: -138.7131
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Armour. Mount Armour, also named Boundary Peak 175, is a mountain in Alaska and British Columbia, located on the Canada–United States border, and part of the Southern Icefield Ranges of the Saint Elias Mountains.

Geographic entities mentioned:
surface_form: mount armour
instance_of: Mountain
countries: Canada
coordinates: lat: 59.9077
lon: -138.7131
Early life. Donald Harlow Bochkay was born on September 19, 1916, in Ashtabula, Ohio, and was of Hungarian descent. At the age of nine, he moved with his family to the San Fernando Valley, California, and in 1935, he graduated from Hollywood High School in Los Angeles. Military career.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Whitchurch-Stouffville. Whitchurch-Stouffville (2021 population 49,864) is a town in the Greater Toronto Area of Ontario, Canada, approximately north of downtown Toronto, and north-east of Toronto Pearson International Airport. It is in area, and located in the mid-eastern area of the Regional Municipality of York on the ecologically-sensitive Oak Ridges Moraine.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The largest urban area is the community of Stouffville proper (2021 pop. 36,753), while other communities in the larger town include Ballantrae, Bethesda, Bloomington, Cedar Valley, Gormley, Lemonville, Lincolnville, Musselman's Lake, Pine Orchard, Pleasantville, Preston Lake, Ringwood, Vandorf, Vivian, and Wesley Corners. History.

Geographic entities mentioned:
surface_form: Musselman's Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
The Vandorf Trail ran from the source waters of the Rouge River to Newmarket, across the heights of the hamlet of Vandorf. The Rouge Trail ran along the Rouge River and northwest from Musselman Lake; both were part of the aboriginal and Coureur des bois trail system leading through dense forests from Lake Ontario to Lake Simcoe.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
The Rouge Trail ran along the Rouge River and northwest from Musselman Lake; both were part of the aboriginal and Coureur des bois trail system leading through dense forests from Lake Ontario to Lake Simcoe. The territory was the site of several Native villages, including Iroquoian peoples' settlements around Preston Lake, Vandorf, and Musselman Lake.

Geographic entities mentioned:
surface_form: Musselman Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
Stouffville's growth was aided by the establishment of the Toronto and Nipissing Railway, built in 1871, which connected Stouffville and Uxbridge with Toronto. In 1877, a second track was built north to Jackson's Point on Lake Simcoe. These connections were created in large part to provide a reliable and efficient means of transporting timber harvested and milled in these regions.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Under the current draft plan, approaches for two of the three landing strips would be directly above Whitchurch–Stouffville communities: the first over Ballantrae, Musselman's Lake and the north-east corner of urban Stouffville, with planes descending (or ascending) from 535 to 365 metres (with an allowable building height in Stouffville of 43 metres); the second over Gormley and the Dickson Hill area (near the Walmart and Smart Centre).

Geographic entities mentioned:
surface_form: Musselman's Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
Environmental protection, including environmental assessments for new development and natural preservation measures, was identified as matter of high importance by residents, but low on a scale of satisfaction. In the hamlet of Musselman's Lake, 72% of residents in 2009 were concerned about the environmental health of the lake and the surrounding community.

Geographic entities mentioned:
surface_form: Musselman's Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
Geography and environment. The greatest portion of Whitchurch–Stouffville lies on the Oak Ridges Moraine. The moraine consists of knobby hills between 290 and 373 meters above sea level of irregularly bedded layers of unconsolidated sand and gravel (built-up glacial debris) deposited by the meltwater of the Wisconsin glacier some twenty-five thousand to ten thousand years ago.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
In a few cases the retreating glacier left behind and buried huge blocks of ice which, when melted, created deep, water-filled depressions known as kettle lakes. Preston Lake, Van Nostrand Lake and Musselman Lake are three such examples. The boundaries of Whitchurch–Stouffville contain a watershed divide.

Geographic entities mentioned:
surface_form: Musselman Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
The boundaries of Whitchurch–Stouffville contain a watershed divide. Streams and rivers at the top of the Oak Ridges Moraine flow northward into the Lake Simcoe basin, part of the Lake Huron watershed. The southern sections (south of Bloomington Road) make up the headwaters of the Rouge River and Duffins Creek, both of which flow into the Lake Ontario basin.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Streams and rivers at the top of the Oak Ridges Moraine flow northward into the Lake Simcoe basin, part of the Lake Huron watershed. The southern sections (south of Bloomington Road) make up the headwaters of the Rouge River and Duffins Creek, both of which flow into the Lake Ontario basin. These headwaters include many smaller streams and creeks throughout southern Whitchurch–Stouffville.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
In 2012, Whitchurch–Stouffville's forest cover was 28.9%. Whitchurch–Stouffville's water supply system is both groundwater-based with five municipal wells and since 2009 lake-based (Lake Ontario) as well. 5,500 cubic metres of water are withdrawn from the Oak Ridges Aquifer and the Thorncliffe Aquifer daily.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Whitchurch–Stouffville has a continental climate moderated by the Great Lakes and influenced by warm, moist air masses from the south, and cold, dry air from the north. The Oak Ridges Moraine affects levels of precipitation: as air masses arrive from Lake Ontario and reach the elevated ground surface of the moraine, they rise causing precipitation.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
In the same year, the unemployment rate for Whitchurch–Stouffville was 6.3% (up from 4.8% in 2006), but below the Ontario average of 8.3%. Whitchurch–Stouffville is York Region's largest &quot;mineral aggregate resource area;&quot; these gravel sites and designated resource areas are located north and south of Bloomington Road, and all lie within the boundaries of the Oak Ridges Moraine.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Access to Musselman's Lake via Cedar Beach Trailer Park was lost in 2012, while access to Preston Lake was lost when Landford Development purchased the west-shore beach and trailer park and built estate properties with a shared private beach.

Geographic entities mentioned:
surface_form: Musselman's Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
The fair is held on the weekend before Thanksgiving. It is held at the Markham fairgrounds, directly south of the Stouffville town border. Bruce's Mill Conservation Area hosts an annual &quot;Sugarbush Maple Syrup Festival&quot; over four weeks in March and April. In February the Musselman Lake community hosts an annual &quot;Winter Carnival&quot; at Cedar Beach.

Geographic entities mentioned:
surface_form: Musselman Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
Films and television series shot at &quot;Shadow Lake Centre&quot; in Whitchurch–Stouffville (Musselman Lake) include &quot;1-800-Missing&quot;, &quot;Tarzan & Jane&quot; (2002), &quot;The Crossing&quot; (2000), &quot;Run the Wild Fields&quot;, &quot;Ice Men&quot; (2005), &quot;Top Cops&quot;, &quot;The Loretta Claiborne Story&quot;, &quot;True Romance&quot; (1993), &quot;Ready or Not&quot;, &quot;The White Dog Sacrifice&quot;, and &quot;The Littlest Hobo&quot; (Summitview Public School).

Geographic entities mentioned:
surface_form: Musselman Lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.0308
lon: -79.2731
It is set within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest, and is only one mile outside the boundary of North Cascades National Park. Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker. Mount Ann can be seen south of Artist Point which is at the end of the Mount Baker Highway.

Geographic entities mentioned:
surface_form: Mount Shuksan
instance_of: Mountain
countries: United States
coordinates: lat: 48.8316
lon: -121.603
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
Precipitation runoff from the mountain drains into Swift Creek and Shuksan Creek, which empty into Baker Lake. Topographic relief is significant as the west aspect rises above Swift Creek in approximately one mile. The mountain is unofficially named in association with nearby Lake Ann. Due to its proximity to the Mt. Baker Ski Area, Mount Ann is a winter destination for skiing and snowshoeing.

Geographic entities mentioned:
surface_form: lake ann
instance_of: Lake
countries: United States
coordinates: lat: 44.87111111
lon: -93.55972222
Mount Ann can be seen south of Artist Point which is at the end of the Mount Baker Highway. Precipitation runoff from the mountain drains into Swift Creek and Shuksan Creek, which empty into Baker Lake. Topographic relief is significant as the west aspect rises above Swift Creek in approximately one mile. The mountain is unofficially named in association with nearby Lake Ann.

Geographic entities mentioned:
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 47.3515175
lon: -121.3017165
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker lake
instance_of: Lake
countries: United States
coordinates: lat: 40.6481
lon: -121.376
Mount Ann. Mount Ann is a mountain summit located in the North Cascades in Whatcom County of Washington state. It is set within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest, and is only one mile outside the boundary of North Cascades National Park. Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
Mount Ann. Mount Ann is a mountain summit located in the North Cascades in Whatcom County of Washington state. It is set within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest, and is only one mile outside the boundary of North Cascades National Park. Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker. Mount Ann can be seen south of Artist Point which is at the end of the Mount Baker Highway. Precipitation runoff from the mountain drains into Swift Creek and Shuksan Creek, which empty into Baker Lake.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
Topographic relief is significant as the west aspect rises above Swift Creek in approximately one mile. The mountain is unofficially named in association with nearby Lake Ann. Due to its proximity to the Mt. Baker Ski Area, Mount Ann is a winter destination for skiing and snowshoeing. Climate. Mount Ann is located in the marine west coast climate zone of western North America.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mt. baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
As a result, the west side of the North Cascades experiences high precipitation, especially during the winter months in the form of snowfall. Mount Ann is situated near the Mt. Baker Ski Area, which recorded the world's greatest snowfall for one season,), which was recorded during the 1998–1999 season.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mt. baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
With the North American Plate overriding the Pacific Plate, episodes of volcanic igneous activity persisted. Mount Baker, a stratovolcano that is southwest of Mount Ann, began forming in the Pleistocene. In addition, small fragments of the oceanic and continental lithosphere called terranes created the North Cascades about 50 million years ago.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
Mount Ann. Mount Ann is a mountain summit located in the North Cascades in Whatcom County of Washington state. It is set within the Mount Baker Wilderness, on land managed by Mount Baker-Snoqualmie National Forest, and is only one mile outside the boundary of North Cascades National Park. Mount Ann is situated immediately southwest of line parent Mount Shuksan and northeast of Mount Baker.

Geographic entities mentioned:
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
The mountain is unofficially named in association with nearby Lake Ann. Due to its proximity to the Mt. Baker Ski Area, Mount Ann is a winter destination for skiing and snowshoeing. Climate. Mount Ann 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 Cascade Mountains.

Geographic entities mentioned:
surface_form: mount ann
instance_of: Mountain
countries: United States
coordinates: lat: 48.816459
lon: -121.666554
BBC research report 1963-50 shows that the town of Holyhead fell just outside the service area of the Llanddona main transmitter and points out that co-channel interference (presumably from Divis in Northern Ireland, about 170 km to the northwest across the Irish Sea) was &quot;severe&quot;. January 1984 – present.

Geographic entities mentioned:
surface_form: Divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Early life. Büttikofer was born in Ranflüh (part of Rüderswil, Canton of Bern) in the Emmental where his father Jakob was a school teacher. He attended village school until the age of 16 and then studied French for one year, after which he attended a teacher training college in Hofwil until the age of 20.

Geographic entities mentioned:
surface_form: Emmental
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.91922
lon: 7.77868
Andrews, Oregon. Andrews is a ghost town in Harney County, Oregon, United States. It is located south of Steens Mountain and near the Alvord Desert. History. The community was named for Peter Andrews, who settled in the area about 1880. A post office was established on Andrews' property in 1890.

Geographic entities mentioned:
surface_form: Steens Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.636419444444
lon: -118.57671666667
Canoe Lake (Madawaska Valley). Canoe Lake is a lake in the Township of Madawaska Valley in Combermere, Renfrew County, Ontario, Canada. It is long and wide, and the primary outflow is an unnamed creek to Negeek Lake on the Madawaska River.

Geographic entities mentioned:
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.2292
lon: -90.8125
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.549166666666665
lon: -78.71805555555555
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.3161
lon: -77.2389
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.5792
lon: -82.0747
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.2803
lon: -83.0389
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.9956
lon: -77.4561
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.2731
lon: -82.4611
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.5917
lon: -76.5453
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.3636
lon: -77.6011
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.85305555555556
lon: -86.96222222222222
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.2803
lon: -80.0503
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.0958
lon: -80.5669
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.6228
lon: -94.9281
surface_form: canoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.166666666666664
lon: -108.25083333333333
Rumsey, California. Rumsey is an unincorporated community and census-designated place (CDP) in Yolo County, California. It is located northwest of Esparto, in the Capay Valley, in the northwestern part of the county. Rumsey's ZIP Code is 95679 and its area code 530. It lies at an elevation of 420 feet (128 m). History.

Geographic entities mentioned:
surface_form: Capay Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7107
lon: -122.047
Historically attested Native American populations, such as the Sierra Miwok, Mono and Paiute, belong to the Uto-Aztecan and Utian phyla. In the mid-19th century, a band of Native Americans called the Ahwahnechee lived in Yosemite Valley. The California Gold Rush greatly increased the number of non-indigenous people in the region.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Native Americans. Humans may have lived in the Yosemite area as long as 8,000 to 10,000 years ago. Habitation of the Yosemite Valley proper can be traced to about 3,000 years ago, when vegetation and game in the region was similar to that present today; the western slopes of the Sierra Nevada had acorns, deer, and salmon, while the eastern Sierra had pinyon nuts and obsidian.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
A year later, in mid-1853, the Ahwahneechee returned to the valley but they betrayed the hospitality of their former Mono hosts by stealing horses that the Mono had taken from non-indigenous ranchers. In return, the Monos tracked down and killed many of the remaining Ahwahneechee, including Tenaya (Tenaya Lake is named after the fallen chief).

Geographic entities mentioned:
surface_form: Tenaya Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.8308
lon: -119.4583
Two other competing routes, the Big Oak Flat Road (July 1874) and the Wawona Road (1875), quickly followed. The completion of the first transcontinental railroad, along with the extension of Central Pacific Railroad services to towns in the San Joaquin Valley, boosted tourism from across the country.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Two-thirds of a million visited in 1946, 1 million in 1954, 2 million by 1966, 3 million in the 1980s, and 4 million in the 1990s. Recreational activities. Half Dome is a prominent and iconic granite dome that rises above the floor of Yosemite Valley. It was first climbed on October 12, 1875, by the Scottish blacksmith of Yosemite Valley, George C. Anderson.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Bighorn sheep, which were driven locally extinct through hunting and disease, have been reintroduced in the east of the park. The Park Service and the Yosemite Fund have also helped peregrine falcons and great gray owls to re-establish themselves. Tule elk, which had been hunted almost to extinction, were housed in a pen in Yosemite before being moved to the Owens Valley in eastern California.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
It was created for the 1890 election. In the change from the 2001 to the 2011 electoral map, it lost Saint-André-du-Lac-Saint-Jean and part of the unorganized territory of Passes-Dangereuses to Roberval electoral district. It is named for Lac Saint-Jean. Linguistic demographics. per cent mother tongue – single answers

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03