Sarmila/GeoWiki-Features huggingface dataset:
In 1825, the summit was one of those used as a base for mapping Ireland as part of the Ordnance Survey's Principal Triangulation. The surveyors, which included Thomas Drummond, camped on the summit and built a wall to shield themselves from the weather. Drummond's team shone a limelight from Slieve Snaght towards Thomas Colby's team on Divis away, the first time a limelight was used for surveying.

Geographic entities mentioned:
surface_form: Divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Slieve Snaght. Slieve Snaght () is a mountain in the middle of the Inishowen peninsula of County Donegal, Ireland. It rises to a height of, making it the highest mountain in Inishowen, and is one of the northernmost mountains of Ireland. It should not be confused with the mountain of the same name in the nearby Derryveagh range.

Geographic entities mentioned:
surface_form: slieve snaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.196461111111
lon: -7.3342888888889
It includes the lesser summits of Slieve Main, Crocknamaddy and Damph. Name. The mountain is said to be so named because snow lies on its summit until late May. In &quot;Cath Maige Tuired&quot; (&quot;The Battle of Moytura&quot;), a tale from Irish mythology, Slieve Snaght is called one of the &quot;twelve chief mountains&quot; of Ireland.

Geographic entities mentioned:
surface_form: slieve snaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.196461111111
lon: -7.3342888888889
In &quot;Cath Maige Tuired&quot; (&quot;The Battle of Moytura&quot;), a tale from Irish mythology, Slieve Snaght is called one of the &quot;twelve chief mountains&quot; of Ireland. There is a tradition of pilgrimage to the top of Slieve Snaght at Lughnasa, and a holy well near the summit, called &quot;Tobar na Súl&quot; (&quot;well of the eyes&quot;), is said to cure blindness. History.

Geographic entities mentioned:
surface_form: slieve snaght
instance_of: Mountain
countries: Ireland
coordinates: lat: 55.196461111111
lon: -7.3342888888889
Two other schools, Saint John's School of Alberta and Saint John's School of Ontario were founded on the same ideas in later years. The school closed in the early 1990s, struggling for funds and credibility after a canoeing disaster on Lake Timiskaming where 13 people died of hypothermia. Incidents.

Geographic entities mentioned:
surface_form: Lake Timiskaming
instance_of: Lake
countries: Canada
coordinates: lat: 47.333333333333
lon: -79.5
Incidents. In the fall of 1973, the National Film Board of Canada filmed the two-week canoe trip on the Red River and Lake Winnipeg, with the 13- to 15-year-old boys who had just arrived at the school. It was part of CBC-TV's series, &quot;West.&quot;
In early 1976, a boy by the name of Ted Milligan collapsed while on one of the school's lengthy snowshoe hikes, and froze to death.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Then he toured the eastern, the southern, the western, and the northern parts of the country; in each place he offered burnt-offering to Heaven at each of the four peaks (Mount Tai, Mount Huang, Mount Hua and Mount Heng), sacrificed to the hills and rivers, set in accord the seasons, months, and days, established uniform measurements of length and capacities, and reinforced ceremonial laws.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
The majority of the lake is situated within Voyageurs National Park in St. Louis County, Minnesota, and the surrounding wilderness of Ontario. Namakan Lake forms part of the interconnected Namakan Reservoir system, which includes Kabetogama Lake, Sand Point Lake, Crane Lake, and Little Vermilion Lake. Geography.

Geographic entities mentioned:
surface_form: Kabetogama Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.45833333
lon: -93.04194444
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
It sits at an elevation of about 1,122 feet (342 m) above sea level. The lake is characterized by a rugged shoreline, dotted with numerous islands, coves, and peninsulas. Hydrology. Namakan Lake receives water from several sources, including Ash River and Crane Lake. Its outflow occurs through the historic Kettle Falls, where water passes into Rainy Lake to the north. Historical significance.

Geographic entities mentioned:
surface_form: Rainy Lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.636944444444
lon: -93.031388888889
Namakan Lake. Namakan Lake is a large freshwater lake located along the international border between northern Minnesota, United States, and Ontario, Canada. The majority of the lake is situated within Voyageurs National Park in St. Louis County, Minnesota, and the surrounding wilderness of Ontario.

Geographic entities mentioned:
surface_form: ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Namakan Lake. Namakan Lake is a large freshwater lake located along the international border between northern Minnesota, United States, and Ontario, Canada. The majority of the lake is situated within Voyageurs National Park in St. Louis County, Minnesota, and the surrounding wilderness of Ontario.

Geographic entities mentioned:
surface_form: ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Namakan Lake. Namakan Lake is a large freshwater lake located along the international border between northern Minnesota, United States, and Ontario, Canada. The majority of the lake is situated within Voyageurs National Park in St. Louis County, Minnesota, and the surrounding wilderness of Ontario.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Namakan Lake forms part of the interconnected Namakan Reservoir system, which includes Kabetogama Lake, Sand Point Lake, Crane Lake, and Little Vermilion Lake. Geography. Namakan Lake covers an area of approximately 24,066 acres (97.4 km²) and has a maximum depth of around 150 feet (46 m). It sits at an elevation of about 1,122 feet (342 m) above sea level.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
It sits at an elevation of about 1,122 feet (342 m) above sea level. The lake is characterized by a rugged shoreline, dotted with numerous islands, coves, and peninsulas. Hydrology. Namakan Lake receives water from several sources, including Ash River and Crane Lake. Its outflow occurs through the historic Kettle Falls, where water passes into Rainy Lake to the north. Historical significance.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Historical significance. During the 18th and 19th centuries, Namakan Lake played a critical role in the fur trade, serving as a key transportation route for French-Canadian voyageurs navigating between the Great Lakes and the interior of Canada. Today, this legacy is honored within Voyageurs National Park. Ecology.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Today, this legacy is honored within Voyageurs National Park. Ecology. Namakan Lake lies within the boreal forest biome, supporting diverse wildlife such as black bears, gray wolves, moose, bald eagles, and common loons. The lake itself is home to walleye, northern pike, smallmouth bass, and black crappie. Recreation.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
The lake itself is home to walleye, northern pike, smallmouth bass, and black crappie. Recreation. Namakan Lake is a popular destination for boating, canoeing, kayaking, and angling. As it lies within Voyageurs National Park, visitors can also enjoy remote campsites, hiking trails, and wildlife observation.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Conservation. Namakan Lake is part of the Namakan Reservoir Operating Plan, which regulates water levels to balance ecological health, recreational access, and hydroelectric power production. The lake benefits from federal protections under the management of Voyageurs National Park.

Geographic entities mentioned:
surface_form: namakan lake
instance_of: Lake
countries: Canada
United States
coordinates: lat: 48.456693
lon: -92.585364
Ecology. Namakan Lake lies within the boreal forest biome, supporting diverse wildlife such as black bears, gray wolves, moose, bald eagles, and common loons. The lake itself is home to walleye, northern pike, smallmouth bass, and black crappie. Recreation. Namakan Lake is a popular destination for boating, canoeing, kayaking, and angling.

Geographic entities mentioned:
surface_form: pike
instance_of: Watercourse
countries: Canada
United States
coordinates: lat: 45.07083333333333
lon: -73.09722222222223
By contrast, in Victoria there was an early and major change to Mitchell's route. Mitchell's original route between Albury and Melbourne went through Mitchellstown on the Goulburn River and took a long detour to the west of Mount Macedon. In March 1837 Charles Bonney blazed a new trail from Mitchellstown through Kilmore to Melbourne, a route that took a day and a half off the previous journey.

Geographic entities mentioned:
surface_form: Mount Macedon
instance_of: Mountain
countries: Australia
coordinates: lat: -37.38291
lon: 144.57625
The mouth of Tortue Lake is located west of a bay in lake Manitou, east of lake Nipisso and northwest of the north shore of the Gulf of St. Lawrence. The river flows more or less in parallel to the west of the Manitou River and to the east of the Bouleau River.

Geographic entities mentioned:
surface_form: lake Manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: lake Nipisso
instance_of: Lake
countries: Canada
coordinates: lat: 50.85667
lon: -65.82417
surface_form: lake manitou
instance_of: Lake
countries: Canada
coordinates: lat: 50.87361
lon: -65.28778
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Lawrence. The river flows more or less in parallel to the west of the Manitou River and to the east of the Bouleau River. Upper course of the Turtle River (segment of)
Lower course of the Turtle River (segment of)
Lower course of the Turtle River (segment of)
The mouth of the Tortue River is in the municipality of Rivière-au-Tonnerre in the Minganie Regional County Municipality.

Geographic entities mentioned:
surface_form: Bouleau River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.281944
lon: -65.514722
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Basin. Part of the river basin is in the unorganized territories of Rivière-Nipissis and Lac-Jérôme and part in the municipality of Rivière-au-Tonnerre. It lies between the basins of the Sault Plat River to the west and the Manitou River to the east. A map of the ecological regions of Quebec shows the river basin in sub-regions 6j-T and 6m-T of the east spruce/moss subdomain.

Geographic entities mentioned:
surface_form: Sault Plat River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.29277777777778
lon: -65.44305555555556
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
Tortue River. It flows into the Gulf of Saint Lawrence. The southern part of the Tortue River watershed is served by the route 138 which runs along the north shore of the estuary of Saint Lawrence. Location. The river originates from Turtle Lake (length: octopus-shaped; altitude:). This lake has an island in its center-north.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Tortue River. It flows into the Gulf of Saint Lawrence. The southern part of the Tortue River watershed is served by the route 138 which runs along the north shore of the estuary of Saint Lawrence. Location. The river originates from Turtle Lake (length: octopus-shaped; altitude:). This lake has an island in its center-north.

Geographic entities mentioned:
surface_form: turtle lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3167
lon: -124.95
surface_form: turtle lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.0597
lon: -79.8353
surface_form: turtle lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5967
lon: -108.631
A painted metal bridge carries Quebec Route 138 over the river nears its mouth. Toponymy. The origin of the name is unknown. It was made official on 5 December 1968. The names of local European settlers are reflected in Moïse Maher Lake, located between the Manitou River and the Tortue River, and in the Ruisseau Philippe Henley, a tributary of the Tortue river. Basin.

Geographic entities mentioned:
surface_form: manitou
instance_of: Lake
countries: Canada
coordinates: lat: 45.7775
lon: -81.98333333333333
surface_form: tortue river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
surface_form: tortue river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
Tortue River. It flows into the Gulf of Saint Lawrence. The southern part of the Tortue River watershed is served by the route 138 which runs along the north shore of the estuary of Saint Lawrence. Location. The river originates from Turtle Lake (length: octopus-shaped; altitude:). This lake has an island in its center-north.

Geographic entities mentioned:
surface_form: tortue river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
Lawrence. The river flows more or less in parallel to the west of the Manitou River and to the east of the Bouleau River. Upper course of the Turtle River (segment of)
Lower course of the Turtle River (segment of)
Lower course of the Turtle River (segment of)
The mouth of the Tortue River is in the municipality of Rivière-au-Tonnerre in the Minganie Regional County Municipality.

Geographic entities mentioned:
surface_form: tortue river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
surface_form: turtle river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
surface_form: turtle river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
surface_form: turtle river
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.300830555556
lon: -65.374169444444
Lower Valley, adjacent to the Lake, is the county's more populous part. The Upper Valley consists mostly of the Ogden Valley, the watershed of the Ogden River. The county's highest elevation is Willard Peak in the Wasatch Mountains, at ASL. The county has an area of, of which is land and (13%) is water. It is the second-smallest county in Utah by land area and third-smallest by total area.

Geographic entities mentioned:
surface_form: Ogden Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.2602196
lon: -111.8116053
Lower Valley, adjacent to the Lake, is the county's more populous part. The Upper Valley consists mostly of the Ogden Valley, the watershed of the Ogden River. The county's highest elevation is Willard Peak in the Wasatch Mountains, at ASL. The county has an area of, of which is land and (13%) is water. It is the second-smallest county in Utah by land area and third-smallest by total area.

Geographic entities mentioned:
surface_form: Willard Peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.383055555556
lon: -111.97416666667
Shipping and transportation. However, with the greatest Great Lake, Lake Superior, surrounding the peninsula, and multiple natural harbors, Keweenaw County's history is much more entwined in shipping and transportation. Nineteen of the properties listed—over half—were directly related to Great Lakes shipping.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Piz Languard. Piz Languard is a mountain of the Livigno Alps, overlooking Pontresina in the canton of Graubünden. With a height of above sea level, it is one of the highest summits of the Livigno Alps and the highest summit of the range that lies west of the Livigno Pass (2,315 m). The summit can be accessed via a trail from the heights of Pontresina and is a popular goal for hikers.

Geographic entities mentioned:
surface_form: piz languard
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.488472222222
lon: 9.9564722222222
The pass known as the Triebener Tauern runs over this section from Trieben to Judenburg. Summit. The highest mountains in the Seckau Alps are the Geierhaupt (2,417 m), the Hochreichhart (2,416 m), the prominent Seckauer Zinken (2,398 m) and the Maierangerkogel (2,356 m). Importance. The Seckau Tauern are primarily of regional significance for mountain sports throughout the year.

Geographic entities mentioned:
surface_form: Geierhaupt
instance_of: Mountain
countries: Austria
coordinates: lat: 47.3747
lon: 14.6358
Geography. Bahadurpur, a gram panchayat, is located at. Jamuria CD Block is part of the Ajay Damodar Barakar tract. This area is sort of an extension of the Chota Nagpur Plateau. It is a rocky undulating area with laterite soil, with the Ajay on the north, the Damodar on the south and the Barakar on the west. For ages the area was heavily forested and infested with plunderers and marauders.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The borough maintains an aggressive cleaning protocol for both the boardwalk and the beach. The boardwalk runs from Ocean Avenue in the north to Manasquan Inlet in the south and is primarily lined by private residences. The boardwalk, originally built in the 1800s, which once featured numerous pavilions and an amusement park, was wooden until it was replaced by asphalt in the 1950s.

Geographic entities mentioned:
surface_form: Manasquan Inlet
instance_of: Landform
countries: United States
coordinates: lat: 40.1025
lon: -74.035
The boardwalk, originally built in the 1800s, which once featured numerous pavilions and an amusement park, was wooden until it was replaced by asphalt in the 1950s. The Manasquan Inlet is the northern terminus of the inland portion of the Intracoastal Waterway. It provides surfers with waves that are corralled, refracted, and enlarged by the jetty protruding out into the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Manasquan Inlet
instance_of: Landform
countries: United States
coordinates: lat: 40.1025
lon: -74.035
Point Pleasant Beach. The Point Pleasant Beach boardwalk is located about north of the Seaside Heights boardwalk. The promenade extends from the Manasquan Inlet in the northern end of the borough to the border with Bay Head in the south. Attractions include bars, eateries, arcades, two mini-golf courses, a fun house, an amusement park, an aquarium, and souvenir shops. Seaside Heights.

Geographic entities mentioned:
surface_form: Manasquan Inlet
instance_of: Landform
countries: United States
coordinates: lat: 40.1025
lon: -74.035
Leksvik Municipality was located to the southwest, Verran Municipality was located to the north, and Inderøy Municipality was located to the east (across the strait). The lake Meltingvatnet lies along the municipal border with Leksvik. The highest point in the municipality is the tall mountain Storknuken. Government.

Geographic entities mentioned:
surface_form: Meltingvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 63.783845
lon: 10.7448664
The population of Hanover Township was 11,785 at the 2020 census. Hanover Township is northeast of Allentown, north of Philadelphia, and west of New York City. Hanover Township is part of the Lehigh Valley metropolitan area, which has a population of 861,899 and is the 68th-most populated metropolitan area in the U.S. as of the 2020 census. Geography. According to the U.S.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Elterwater. Elterwater is a village in the English Lake District and the county of Cumbria. The village lies half a mile (800 m) north-west of the lake of Elter Water, from which it derives its name. Both are situated in the valley of Great Langdale. Elterwater Bridge is a Grade II listed structure dating to at least the 18th century. Economic activity.

Geographic entities mentioned:
surface_form: Elter Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.427469444444
lon: -3.025875
Elterwater. Elterwater is a village in the English Lake District and the county of Cumbria. The village lies half a mile (800 m) north-west of the lake of Elter Water, from which it derives its name. Both are situated in the valley of Great Langdale. Elterwater Bridge is a Grade II listed structure dating to at least the 18th century. Economic activity.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Vesturhópsvatn. Vesturhópsvatn is a lake in northern Iceland. It is located in the municipality of Húnaþing vestra. Geography. The surface of the Vesturhópsvatn is about 10 km2; the maximum depth is 28m.

Geographic entities mentioned:
surface_form: vesturhópsvatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.468888888889
lon: -20.648611111111
Aden Crater. Aden Crater is a small shield volcano located in Doña Ana County, about southwest of Las Cruces, New Mexico. It is located in the northwest part of the Aden-Afton basalt field, which is part of the central area of the Potrillo volcanic field. A fossilized ground sloth, now at the Peabody Museum, was found in a fumarole roughly 100' deep located on the SE portion of the crater rim.

Geographic entities mentioned:
surface_form: Potrillo volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 31.9
lon: -107.2
Aden Crater. Aden Crater is a small shield volcano located in Doña Ana County, about southwest of Las Cruces, New Mexico. It is located in the northwest part of the Aden-Afton basalt field, which is part of the central area of the Potrillo volcanic field. A fossilized ground sloth, now at the Peabody Museum, was found in a fumarole roughly 100' deep located on the SE portion of the crater rim.

Geographic entities mentioned:
surface_form: aden crater
instance_of: Mountain
countries: United States
coordinates: lat: 32.0695
lon: -107.058
A fossilized ground sloth, now at the Peabody Museum, was found in a fumarole roughly 100' deep located on the SE portion of the crater rim. Several ground sloth coprolites were also recovered and were stored in the Geology department at UTEP. No volcanic activity at Aden Crater is known from historic times. The most recent known activity has been dated to roughly 16,000 years ago.

Geographic entities mentioned:
surface_form: aden crater
instance_of: Mountain
countries: United States
coordinates: lat: 32.0695
lon: -107.058
The second group of flows were less fluid and accumulated closer to the vent to form the shield of the crater. Description. Aden Crater is an Icelandic-type shield volcano, formed by repeated eruptions of very fluid olivine basalt. This has built a very low hill in diameter with slopes of just 3 to 5 degrees.

Geographic entities mentioned:
surface_form: aden crater
instance_of: Mountain
countries: United States
coordinates: lat: 32.0695
lon: -107.058
Further Reading. Williams, Wendi JW (1999) Evolution of Quaternary intraplate mafic lavas detailed using helium-3 surface exposure and argon-40/argon-39 dating, and elemental and helium, strontium, neodymium and lead isotopic signatures: Potrillo volcanic field, New Mexico, United States of America and San Quintin volcanic field, Baja California Norte, Mexico. ProQuest Dissertations & Theses.

Geographic entities mentioned:
surface_form: potrillo volcanic field
instance_of: Mountain
countries: United States
coordinates: lat: 31.9
lon: -107.2
The hill is topped by a crater about in diameter whose rim is composed of lava spatter that dips steeply into the crater (30 to 45 degrees). The crater itself contains a former lava lake, with a spatter cone and collapse pit in the southeastern part of the crater. The surrounding area has such features as explosion craters, collapse pits, spatter cones, and hornitos.

Geographic entities mentioned:
surface_form: lava lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9203
lon: -121.773
The Holy Spirit is represented as a manifestation of Divine Wisdom who is called &quot;Mother&quot;. The feminine aspect of the Spirit is an indication of Semitic influence on the language of the gospel. The Spirit takes Jesus to Mount Tabor by a single hair, echoing Old Testament themes in the stories of Ezekiel (Ezekiel 8:3) and Habbakuk (Dan. 14:36 LXX).

Geographic entities mentioned:
surface_form: Mount Tabor
instance_of: Mountain
countries: Israel
coordinates: lat: 32.68625
lon: 35.392916666667
Early community. In 1846, Alexander Caulfield Anderson visited Lillooet Village (not to be confused with later named Lillooet). On a grassy island above Lillooet Lake, the residents numbered 50 men (plus women and children). The island lies in the vicinity of the later Owl Creek general community.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
Douglas Road. The Douglas Road, a.k.a. the Lillooet Trail, Harrison Trail or Lakes Route, was a goldrush-era transportation route from the British Columbia Coast to the Interior (NB another route known as the Lillooet Trail was the Lillooet Cattle Trail, which used some of the same route but was built 25 years later).

Geographic entities mentioned:
surface_form: Interior
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
Despite their efforts the route was little-used by 1861 or so, although it remained in use by locals and the occasional traveller for years afterwards. Regular steamer service to and from Port Douglas ended in the 1890s, although small-steamer traffic on Anderson and Seton Lakes continued for decades after, ending on Seton Lake only in the 1950s. Route.

Geographic entities mentioned:
surface_form: Seton Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
surface_form: Seton Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
From there a route by boat and road went to Port Pemberton. A trail then went into Pemberton and made a wide turn to Port Anderson. From there, another water to road route went straight to Lillooet, where it joined the old Cariboo Road. Description. The route begins at Port Douglas, British Columbia, at the head of Harrison Lake and the head of river navigation from the Strait of Georgia.

Geographic entities mentioned:
surface_form: Harrison Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.55
lon: -121.83333333333
The route begins at Port Douglas, British Columbia, at the head of Harrison Lake and the head of river navigation from the Strait of Georgia. From there a land portion of the route follows the lower Lillooet River to Port Lillooet at the south end of Lillooet Lake, where steamers and canoes carried travellers to Port Pemberton, at the mouth of the Birkenhead River near present-day Mount Currie.

Geographic entities mentioned:
surface_form: Lillooet Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.25
lon: -122.5
The next land portion of the route, known as the Long Portage or the Pemberton Portage, follows the lower Birkenhead River then diverges from it to Birken Lake (a.k.a. Summit Lake or Gates Lake) and then via the Gates River to present-day D'Arcy at the head of Anderson Lake, then known as Port Anderson.

Geographic entities mentioned:
surface_form: Gates Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.4772
lon: -122.62618
There packers and ultimately a short mule-drawn &quot;railway&quot; shuttled men and freight to the head of Seton Lake, where another collection of steamers carried them to the foot of that lake and a final five-mile wagon road to the boomtowns of Cayoosh Flat, Parsonville and Marysville (today's Lillooet).

Geographic entities mentioned:
surface_form: Seton Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.7
lon: -122.167
In response to the Cariboo Gold Rush, a toll road from there to Fort Alexandria was built by entrepreneur Gustavus Blin Wright, followed the Fraser Canyon for about twenty miles, then cut up eastwards onto the Cariboo Plateau via the town of Clinton, where the later Cariboo Wagon Road met the older route.

Geographic entities mentioned:
surface_form: Cariboo Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 50.81652
lon: -118.81904
Austerity Mountain. Austerity Mountain is a mountain in British Columbia, Canada. Description. Austerity Mountain is the second-highest point of the Adamant Range which is a subrange of the Selkirk Mountains, and it ranks as the fifth-highest peak in the Selkirks. It is located northwest of Golden and north of Glacier National Park.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: austerity mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.73322
lon: -117.91901
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is located northwest of Golden and north of Glacier National Park. Austerity is highly glaciated with the Granite Glacier to the north and Austerity Glacier to the south. Precipitation runoff and glacial meltwater from the mountain's slopes drains into tributaries of the Columbia River. Topographic relief is significant as the summit rises above Austerity Creek in and above Kinbasket Lake in.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Austerity Mountain. Austerity Mountain is a mountain in British Columbia, Canada. Description. Austerity Mountain is the second-highest point of the Adamant Range which is a subrange of the Selkirk Mountains, and it ranks as the fifth-highest peak in the Selkirks. It is located northwest of Golden and north of Glacier National Park.

Geographic entities mentioned:
surface_form: austerity mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.73322
lon: -117.91901
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's current toponym was officially adopted on March 31, 1924, by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Austerity Mountain is located in a subarctic climate zone with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: austerity mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.73322
lon: -117.91901
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
History. The first ascent of the summit was made on July 20, 1911, by Howard Palmer, Edward Holway, and Frederic King Butters. This first ascent party named the peak &quot;Mount Austerity.&quot; Photographs of Austerity appeared in Howard Palmer's 1914 book, &quot;Mountaineering and Explorations in the Selkirks&quot;.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
She was nicknamed &quot;Sadie Mae Glutz&quot; by Manson and a man who was creating a fake ID for her at the time. Atkins later claimed to have believed Manson was Jesus. The growing &quot;Manson Family&quot; settled at the Spahn Ranch in the San Fernando Valley in southern California, where, on October 7, 1968, Atkins bore a son by Bruce White, whom Manson called Zezozose Zadfrack Glutz.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In addition to serving as a legislator, she worked as an attorney in private practice. Hawaii House of Representatives. For 24 years, Luke served in the Hawaii House of Representatives as the representative for Makiki, Punchbowl, Nuuanu, Dowsett Highlands, Pacific Heights and Pauoa.

Geographic entities mentioned:
surface_form: Punchbowl
instance_of: Mountain
countries: United States
coordinates: lat: 21.3125
lon: -157.84611111111
surface_form: Nuuanu
instance_of: Landform
countries: United States
coordinates: lat: 21.370277777778
lon: -157.79694444444
Climbers who climb all of the Hewitts are called &quot;Hewitteers&quot;, with the first English & Welsh Hewitteer being Edward Moss on 22 July 1951. On 5 December 2018, the BBC announced that Foel Penolau had been re-surveyed and promoted to Hewitt status (and by definition, to Simm status). As has Foel Cedig. Hewitt mountains by height.

Geographic entities mentioned:
surface_form: Foel Penolau
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.894242
lon: -3.990612
Climbers who climb all of the Hewitts are called &quot;Hewitteers&quot;, with the first English & Welsh Hewitteer being Edward Moss on 22 July 1951. On 5 December 2018, the BBC announced that Foel Penolau had been re-surveyed and promoted to Hewitt status (and by definition, to Simm status). As has Foel Cedig. Hewitt mountains by height.

Geographic entities mentioned:
surface_form: Foel Cedig
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.84281
lon: -3.51331
Wilmette, Illinois. Wilmette is a village in Cook County, Illinois, United States. Bordering Lake Michigan, Kenilworth, Winnetka, Skokie, Northfield, Glenview, and Evanston, Illinois, it is located north of Chicago's downtown district. Wilmette had a population of 28,170 at the 2020 census. The first and only Baháʼí House of Worship in North America is located in Wilmette.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The Mallinckrodt Center contains the new home of the Meskill Senior Center. Geography. Wilmette is located on the western shore of Lake Michigan and is a near northern suburb of Chicago, immediately North of Evanston at (42.077178, -87.723736). The North Shore Channel drainage canal is supplied with water from Lake Michigan at Wilmette Harbor.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
West Rock Ridge State Park is a public recreation area located in New Haven, Hamden, and Woodbridge, Connecticut. The state park is named for the trap rock West Rock Ridge, which is part of the Metacomet Ridge extending from Long Island Sound to the Vermont border. The park's of open west-facing cliffs offer vistas encompassing Metropolitan New Haven and suburban towns to the west.

Geographic entities mentioned:
surface_form: West Rock Ridge
instance_of: Mountain
countries: United States
coordinates: lat: 41.380841666667
lon: -72.978319444444
The park is part of a larger area of protected open space including state, municipal, and non-profit owned land. Geography. West Rock Ridge consists largely of diabase, much like its sister formation East Rock. It runs north-northwest out of New Haven and forms the boundary between the towns of Woodbridge and Hamden.

Geographic entities mentioned:
surface_form: East Rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.327222222222
lon: -72.904722222222
Over time the site led to the formation of a burgeoning population, which began to be known as La Cruz. History. La Cruz was created on 23 July 1969 by decree 4354. In Pre-Columbian times the area currently known as the canton de La Cruz, was part of a province of the Indians called Chorotegas whose domains ranged from the Nicoya Peninsula to Lake Nicaragua, made up of several villages or domains.

Geographic entities mentioned:
surface_form: Lake Nicaragua
instance_of: Lake
countries: Nicaragua
coordinates: lat: 11.5742
lon: -85.3563
In the summer of 1917 he was sent to the southern Appalachian region to study copper deposits
of the Ducktown type. In 1919, with Esper S. Larsen, Jr., he made geologic maps of the southern end of the San Luis Valley in New Mexico. In the early 1920s he published several reports with Hugh D. Miser.

Geographic entities mentioned:
surface_form: San Luis Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.2
lon: -105.42
Entirely located in the Chicoutimi borough of Saguenay, it is the most urbanized and dammed river in Saguenay–Lac-Saint-Jean. Used by the Montagnais of the Saguenay River before the arrival of Europeans, it was at that time the first portage from the main access road to Lac Saint-Jean. In the 20th century, it was developed from its source to its mouth for hydropower purposes.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Finally, it flows into the Saguenay River. The Chicoutimi River flows mainly in the Saguenay graben, a vast elevated valley that overlooks the lowlands surrounding the Saguenay River. The soils of this large depression are composed of Quaternary marine sediments, such as silt and clay, deposited at the end of the Pleistocene and during the beginning of the Holocene by the Laflamme Sea.

Geographic entities mentioned:
surface_form: Saguenay graben
instance_of: Valley
countries: Canada
coordinates: lat: 48.5
lon: -71.3333
Du Laurentides Wildlife Reserve, the basin follows, in several places, steep slopes. The latter would also include three sub-basins (rivers Pikauba, Cyriac and aux-Écorces), two reservoirs (Kenogami and Pikauba) and part of the territory of each of the 5 former cities of Chicoutimi, Laterrière, Lac-Kénogami, Arvida and Jonquière which are now part of city of Saguenay.

Geographic entities mentioned:
surface_form: Pikauba
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.324722
lon: -71.4408329
Benjamin Rudyerd wrote to Governor Bell in 1633,
At first the island was vulnerable to attack. Samuel Axe and Workmaster Goodman were given responsibility for fortification. Both men became involved in a dispute with Governor Philip Bell and left with Sussex Camock to Cabo Gracias a Dios on the Mosquito Shore to the west. Other men also moved to the Cape.

Geographic entities mentioned:
surface_form: Cabo Gracias a Dios
instance_of: Landform
countries: Honduras
coordinates: lat: 15.0064851
lon: -83.1301235
Smith married in July 1876. Subsequently, his wife and he had four sons and two daughters. He gave more prominent attention to the fauna of the African Great Lakes and the marine molluscs of South Africa, and also the non-marine mollusc fauna of Borneo and New Guinea. In the British Museum.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Engle Peak. Engle Peak is a mountain summit in Sanders County, Montana. Description. Engle Peak is located east of Noxon, Montana, along the boundary of the Cabinet Mountains Wilderness, on land managed by Kaniksu National Forest. It is set west of the Continental Divide in the Cabinet Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: engle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.009444444444
lon: -115.61916666667
Engle Peak. Engle Peak is a mountain summit in Sanders County, Montana. Description. Engle Peak is located east of Noxon, Montana, along the boundary of the Cabinet Mountains Wilderness, on land managed by Kaniksu National Forest. It is set west of the Continental Divide in the Cabinet Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: engle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.009444444444
lon: -115.61916666667
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Topographic relief is significant as the summit rises above Engle Lake in one-half mile (0.8 km). Engle Lake is named after pioneer Isaac Engle (1855–1928) who homesteaded nearby. Engle Peak is named after Roy Engle of Noxon who saved the lives of 25 crewmembers fighting a 1910 forest fire. The mountain's toponym has been officially adopted by the U.S.

Geographic entities mentioned:
surface_form: engle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.009444444444
lon: -115.61916666667
Engle Peak is named after Roy Engle of Noxon who saved the lives of 25 crewmembers fighting a 1910 forest fire. The mountain's toponym has been officially adopted by the U.S. Board on Geographic Names, and has appeared in publications since 1875. An ascent of the summit involves hiking 3.9 miles with 3,489-feet of elevation gain on the Engle Peak Trail. Climate.

Geographic entities mentioned:
surface_form: engle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.009444444444
lon: -115.61916666667
An ascent of the summit involves hiking 3.9 miles with 3,489-feet of elevation gain on the Engle Peak Trail. Climate. Based on the Köppen climate classification, Engle Peak is located in a subarctic climate zone characterized by long, usually very cold winters, and cool to mild summers. Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.

Geographic entities mentioned:
surface_form: engle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.009444444444
lon: -115.61916666667
In 1987 Röhrl set up a new record in the Pikes Peak International Hill Climb for being the first driver to win the 12.42 miles (19.99 km) long mountain track to the Pikes Peak in less than 11 minutes. In his 600 hp (440 kW) Audi Sport Quattro S1 E2 he did the American hillclimb in 10 minutes and 47.850 seconds to reach Pikes Peak on the road which at that time was mainly covered with gravel.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Geography and nature divide the island itself into three distinct parts: the fertile and forested north (which suffered major damage in the August 2021 forest fires); the forested mountainous centre, with agriculture limited to the coastal valleys; and the barren south. The main mountains include Dirfi (), Kantili (), Pyxaria () in the northeast and Ochi () in the south.

Geographic entities mentioned:
surface_form: Dirfi
instance_of: Mountain
countries: Greece
coordinates: lat: 38.6268
lon: 23.8409
surface_form: Kantili
instance_of: Mountain
countries: Greece
coordinates: lat: 38.699
lon: 23.435
Vytegra (river). The Vytegra () is a river in Vytegorsky District of Vologda Oblast in Russia. It nominally flows out of Lake Matkozero and is a tributary of Lake Onega. It is long, and the area of its basin. The principal tributary is the Tagazhma (left). The river is a part of the Volga–Baltic Waterway.

Geographic entities mentioned:
surface_form: Lake Onega
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 61.690555555556
lon: 35.655555555556
Vonbreen. Vonbreen (Hope Glacier) is a glacier in Haakon VII Land and Andrée Land at Spitsbergen, Svalbard. It has an extension of about 25 kilometers, and is located south of Woodfjorden. The name is a translation of the German language &quot;Hoffnungs-Gletscher&quot;, suggested by Bock and Poninski in 1908. The glacier borders to Eidsvollfjellet, the highest mountain in Haakon VII Land.

Geographic entities mentioned:
surface_form: Eidsvollfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 79.1606
lon: 13.3444
Geography. Oakdale is situated along the Emory River (between river miles 17 and 19) in a relatively hilly area atop the Cumberland Plateau, and is concentrated primarily in two areas on each side of the river. The western side is located along a slope that descends from State Route 299 to a flood plain along the river, and includes the town hall, fire department, and several houses.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
Monte Magnodeno. Monte Magnodeno is a mountain of Lombardy, Italy, with an elevation of. It is located in the Bergamasque Prealps, between the provinces of Lecco and Bergamo. The peak has a small mountain hut operated by the National Alpini Association.

Geographic entities mentioned:
surface_form: monte magnodeno
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8392408
lon: 9.4400797
surface_form: magnodeno
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8392408
lon: 9.4400797
&quot;Bandeirantes&quot;. Between 1648 and 1652, Antônio Raposo Tavares, a &quot;bandeirante&quot; from São Paulo, set off on his journey up the Paraguay river basin, reached Guaporé (now Rondônia), crossed the Altiplano, and traveled down the Amazon river to Gurupá, in Pará, near its mouth. It was the first Luso-Brazilian expedition of extensive reconnaissance. Portuguese occupation.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
It was listed on the National Register of Historic Places in 1973 and was designated the official state ship of Pennsylvania by the Pennsylvania General Assembly in 1988. &quot;Niagara&quot; was constructed from 1812 to 1813 to protect the vulnerable American coastline on Lake Erie from the British and played a pivotal role in the battle for the lake.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Construction. In the beginning of September 1812, Daniel Dobbins, a merchant on the Great Lakes, arrived in Washington, D.C., to warn the United States government of the vulnerability of the Lake Erie coastline to a British attack. Dobbins had been captured by the British after a surprise attack at Fort Mackinac in Michigan, but was able to negotiate his release.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Hamilton also granted $2,000 to be used for the construction and appointed Dobbins, a civilian, to the rank of sailing master in the United States Navy. On 31 December, Captain Isaac Chauncey, the commander of naval forces on Lake Ontario, arrived in Erie for a day, made some alterations to Dobbins' ship design and authorized him to build, additionally, two brigs.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889