Sarmila/GeoWiki-Features huggingface dataset:
YMCA Camp Letts sits on a peninsula at the northern end of the Rhode River, and the Smithsonian Environmental Research Center occupies most of the northwestern shore of the Rhode River. Carrs Wharf. Carrs Wharf is a community park on the Rhode River. Early settlement. &quot;Rhode River Hundred&quot; is listed in records of some of the earliest settlements in the Province of Maryland.

Geographic entities mentioned:
surface_form: rhode river
instance_of: Landform
countries: United States
coordinates: lat: 38.87583333
lon: -76.52055556
Carrs Wharf. Carrs Wharf is a community park on the Rhode River. Early settlement. &quot;Rhode River Hundred&quot; is listed in records of some of the earliest settlements in the Province of Maryland. In 1651, Robert Harwood surveyed Harwood Plantation on the Rhode River.

Geographic entities mentioned:
surface_form: rhode river
instance_of: Landform
countries: United States
coordinates: lat: 38.87583333
lon: -76.52055556
Early settlement. &quot;Rhode River Hundred&quot; is listed in records of some of the earliest settlements in the Province of Maryland. In 1651, Robert Harwood surveyed Harwood Plantation on the Rhode River. A deed was written by Thomas Harwood of Streatley, Berks County (Berkshire), England to his son Richard Harwood for &quot;Hookers Purchase&quot; at the head of Muddy Creek.

Geographic entities mentioned:
surface_form: rhode river
instance_of: Landform
countries: United States
coordinates: lat: 38.87583333
lon: -76.52055556
In 1651, Robert Harwood surveyed Harwood Plantation on the Rhode River. A deed was written by Thomas Harwood of Streatley, Berks County (Berkshire), England to his son Richard Harwood for &quot;Hookers Purchase&quot; at the head of Muddy Creek. The steamboat &quot;Emma Giles&quot; served the Rhode River between 1891 and 1932, making five trips per week.

Geographic entities mentioned:
surface_form: rhode river
instance_of: Landform
countries: United States
coordinates: lat: 38.87583333
lon: -76.52055556
India Hook, South Carolina. India Hook is a census-designated place (CDP) in York County, South Carolina, United States. The majority of India Hook is annexed into the city of Rock Hill, but as of 2010 India Hook is still considered to be a CDP. It is one of the three communities located on Lake Wylie. The population was 2,051 at the 2010 census. Geography.

Geographic entities mentioned:
surface_form: Lake Wylie
instance_of: Lake
countries: United States
coordinates: lat: 35.085805555556
lon: -81.058583333333
The route was in use even a few decades ago until the 1959 Chinese crackdown in Tibet. It was commonly used by traders traveling to Tibet through Jelep La (&quot;La&quot; stands for mountain pass) as an overnight base. The route started from Kalimpong and passed through Pedong, Aritar, Dzuluk and Jelepla to Chumbi valley in Tibet. Climate. Dzuluk is at an altitude of about 9,400  feet.

Geographic entities mentioned:
surface_form: Chumbi valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
Dzuluk can be reached from Siliguri by various hired vehicle in roughly 7 hours. Tourists can also travel to Dzuluk from Gangtok in roughly 4 hours by hiring vehicles. Nearby places. The three-level switchback roads of Dzuluk offer views of the Kangchenjunga and its mountain range. The other attractions of the place include lakes, temples, forests, and a route that leads to Tibet.

Geographic entities mentioned:
surface_form: Kangchenjunga
instance_of: Mountain
countries: India
Nepal
coordinates: lat: 27.7
lon: 88.133333
Masik River. The Masik River is a river on Banks Island, in Canada's Northwest Territories. It is a part of the Arctic Ocean watershed. The river is named after the polar researcher August Masik (1887–1976).

Geographic entities mentioned:
surface_form: masik river
instance_of: Watercourse
countries: Canada
coordinates: lat: 71.53861
lon: -123.78365
Masik River. The Masik River is a river on Banks Island, in Canada's Northwest Territories. It is a part of the Arctic Ocean watershed. The river is named after the polar researcher August Masik (1887–1976).

Geographic entities mentioned:
surface_form: masik river
instance_of: Watercourse
countries: Canada
coordinates: lat: 71.53861
lon: -123.78365
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Geography. Mess Creek originates from an unnamed lake behind an alluvial fan at. From its source the creek flows about north into Mess Lake and then continues northwest for another into the Stikine River. About midway through its course, Mess Creek is bounded on the east by the Mess Creek Escarpment.

Geographic entities mentioned:
surface_form: Mess Lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.4667
lon: -130.883
From its source the creek flows about north into Mess Lake and then continues northwest for another into the Stikine River. About midway through its course, Mess Creek is bounded on the east by the Mess Creek Escarpment. This is a long, often cliff-like feature forming the western edge of the Mount Edziza volcanic complex. The final of Mess Creek flows through a gorge.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
The final of Mess Creek flows through a gorge. Mess Creek contains seven named right tributaries. The first one is Tadekho Creek which flows northwest into Mess Creek just south of Mess Lake. Kitsu Creek is the second named right tributary which flows northwest and then north into Mess Creek. The third named right tributary is Raspberry Creek which flows northwest into Mess Creek.

Geographic entities mentioned:
surface_form: Tadekho Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.43296
lon: -130.90399
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The final of Mess Creek flows through a gorge. Mess Creek contains seven named right tributaries. The first one is Tadekho Creek which flows northwest into Mess Creek just south of Mess Lake. Kitsu Creek is the second named right tributary which flows northwest and then north into Mess Creek. The third named right tributary is Raspberry Creek which flows northwest into Mess Creek.

Geographic entities mentioned:
surface_form: Kitsu Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.51636
lon: -130.85398
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Kitsu Creek is the second named right tributary which flows northwest and then north into Mess Creek. The third named right tributary is Raspberry Creek which flows northwest into Mess Creek. Taweh Creek, the fourth named right tributary, flows northwest into Mess Creek west of Mount Edziza. The fifth named right tributary, Crayke Creek, flows southwest into Mess Creek off Mount Edziza.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The third named right tributary is Raspberry Creek which flows northwest into Mess Creek. Taweh Creek, the fourth named right tributary, flows northwest into Mess Creek west of Mount Edziza. The fifth named right tributary, Crayke Creek, flows southwest into Mess Creek off Mount Edziza. Elwyn Creek is the sixth named right tributary which flows west into Mess Creek.

Geographic entities mentioned:
surface_form: Crayke Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.73298
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The fifth named right tributary, Crayke Creek, flows southwest into Mess Creek off Mount Edziza. Elwyn Creek is the sixth named right tributary which flows west into Mess Creek. The seventh named right tributary is Dagaichess Creek which flows southeast into Mess Creek just south of Telegraph Creek. Only two left tributaries of Mess Creek are named.

Geographic entities mentioned:
surface_form: Elwyn Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Two groups of hot springs occur along Mess Creek. The Mess Lake Hot Springs near the southeastern corner of Mess Lake have deposited massive tufa over an area of more than. Discharge at these hot springs may be linked to shallow hydrothermal systems driven by residual magmatic heat as they are adjacent to The Ash Pit, a recently active eruptive centre of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: The Ash Pit
instance_of: Mountain
countries: Canada
coordinates: lat: 57.45
lon: -130.78
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
Mess Creek. Mess Creek, formerly known as Mestua, is a tributary of the Stikine River in northwestern British Columbia, Canada. It flows north and northwest for about, through a lake and a gorge to join the Stikine River, which in turn flows southwest across the Canada–United States border into Alaska where it empties into various straits of the Inside Passage.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Mess Creek. Mess Creek, formerly known as Mestua, is a tributary of the Stikine River in northwestern British Columbia, Canada. It flows north and northwest for about, through a lake and a gorge to join the Stikine River, which in turn flows southwest across the Canada–United States border into Alaska where it empties into various straits of the Inside Passage.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It flows north and northwest for about, through a lake and a gorge to join the Stikine River, which in turn flows southwest across the Canada–United States border into Alaska where it empties into various straits of the Inside Passage. The northern half of Mess Creek forms a western boundary of Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The northern half of Mess Creek forms a western boundary of Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Mess Creek's watershed covers and its estimated mean annual discharge is. The mouth of Mess Creek is located about southwest of Telegraph Creek, about west of Iskut and about southwest of Dease Lake in Cassiar Land District.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Mess Creek's watershed covers and its estimated mean annual discharge is. The mouth of Mess Creek is located about southwest of Telegraph Creek, about west of Iskut and about southwest of Dease Lake in Cassiar Land District. Mess Creek's watershed's land cover is classified as 38.7% conifer forest, 25% barren, 15.9% shrubland, 10% snow/glacier, 8.3% herbaceous and small amounts of other cover.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The mouth of Mess Creek is located about southwest of Telegraph Creek, about west of Iskut and about southwest of Dease Lake in Cassiar Land District. Mess Creek's watershed's land cover is classified as 38.7% conifer forest, 25% barren, 15.9% shrubland, 10% snow/glacier, 8.3% herbaceous and small amounts of other cover. Geography.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Mess Creek's watershed's land cover is classified as 38.7% conifer forest, 25% barren, 15.9% shrubland, 10% snow/glacier, 8.3% herbaceous and small amounts of other cover. Geography. Mess Creek originates from an unnamed lake behind an alluvial fan at. From its source the creek flows about north into Mess Lake and then continues northwest for another into the Stikine River.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Mess Creek originates from an unnamed lake behind an alluvial fan at. From its source the creek flows about north into Mess Lake and then continues northwest for another into the Stikine River. About midway through its course, Mess Creek is bounded on the east by the Mess Creek Escarpment. This is a long, often cliff-like feature forming the western edge of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
About midway through its course, Mess Creek is bounded on the east by the Mess Creek Escarpment. This is a long, often cliff-like feature forming the western edge of the Mount Edziza volcanic complex. The final of Mess Creek flows through a gorge. Mess Creek contains seven named right tributaries. The first one is Tadekho Creek which flows northwest into Mess Creek just south of Mess Lake.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
This is a long, often cliff-like feature forming the western edge of the Mount Edziza volcanic complex. The final of Mess Creek flows through a gorge. Mess Creek contains seven named right tributaries. The first one is Tadekho Creek which flows northwest into Mess Creek just south of Mess Lake. Kitsu Creek is the second named right tributary which flows northwest and then north into Mess Creek.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The first one is Tadekho Creek which flows northwest into Mess Creek just south of Mess Lake. Kitsu Creek is the second named right tributary which flows northwest and then north into Mess Creek. The third named right tributary is Raspberry Creek which flows northwest into Mess Creek. Taweh Creek, the fourth named right tributary, flows northwest into Mess Creek west of Mount Edziza.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The fifth named right tributary, Crayke Creek, flows southwest into Mess Creek off Mount Edziza. Elwyn Creek is the sixth named right tributary which flows west into Mess Creek. The seventh named right tributary is Dagaichess Creek which flows southeast into Mess Creek just south of Telegraph Creek. Only two left tributaries of Mess Creek are named.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Elwyn Creek is the sixth named right tributary which flows west into Mess Creek. The seventh named right tributary is Dagaichess Creek which flows southeast into Mess Creek just south of Telegraph Creek. Only two left tributaries of Mess Creek are named. The first one is Schaft Creek which flows north into Mess Creek on the west side of Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The seventh named right tributary is Dagaichess Creek which flows southeast into Mess Creek just south of Telegraph Creek. Only two left tributaries of Mess Creek are named. The first one is Schaft Creek which flows north into Mess Creek on the west side of Mount Edziza Provincial Park. The other named left tributary, Tudadela Creek, flows north into Mess Creek. Geology.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Only two left tributaries of Mess Creek are named. The first one is Schaft Creek which flows north into Mess Creek on the west side of Mount Edziza Provincial Park. The other named left tributary, Tudadela Creek, flows north into Mess Creek. Geology. Mess Creek flows through a long and narrow graben-like depression bounded by steeply-dipping faults that extend to the north.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The other named left tributary, Tudadela Creek, flows north into Mess Creek. Geology. Mess Creek flows through a long and narrow graben-like depression bounded by steeply-dipping faults that extend to the north. A more than fault along the eastern edge of this structure shows signs of having been active contemporaneously with volcanism of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The downthrowing of this fault during the Holocene may have been due to the draining of magma chambers following eruptions at the Mount Edziza volcanic complex. Two groups of hot springs occur along Mess Creek. The Mess Lake Hot Springs near the southeastern corner of Mess Lake have deposited massive tufa over an area of more than.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
The Mess Creek Hot Springs south of Mess Lake have a recorded temperature of and may be discharging from a deeply circulating hydraulic system along a major fault on the western side of Mess Creek valley. History. The historic Yukon Telegraph Trail runs along the eastern side of Mess Creek.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
History. The historic Yukon Telegraph Trail runs along the eastern side of Mess Creek. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
History. The historic Yukon Telegraph Trail runs along the eastern side of Mess Creek. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The other named left tributary, Tudadela Creek, flows north into Mess Creek. Geology. Mess Creek flows through a long and narrow graben-like depression bounded by steeply-dipping faults that extend to the north. A more than fault along the eastern edge of this structure shows signs of having been active contemporaneously with volcanism of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
It has vertically displaced Holocene basalt flows by and older basalt flows by, such that the western side of the fault has been downthrown. The downthrowing of this fault during the Holocene may have been due to the draining of magma chambers following eruptions at the Mount Edziza volcanic complex. Two groups of hot springs occur along Mess Creek.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
It follows the story of the Manuel Rodríguez Patriotic Front members as they develop a plan to kill the Chilean dictator in Cajón del Maipo in 1986, known as &quot;Operación Siglo XX&quot;. Plot. The film is set in Chile during September 1986, a time when the country was enduring 13 years of dictatorship under Augusto Pinochet.

Geographic entities mentioned:
surface_form: Cajón del Maipo
instance_of: Valley
countries: Chile
coordinates: lat: -33.633333333333
lon: -70.35
It is surrounded by D.A.R. State Park. The house was listed on the National Register of Historic Places in 1980. Description and history. The John Strong Mansion stands on the west side of Vermont Route 17W, overlooking Lake Champlain in western Addison. It occupies a modest square parcel, now completely surrounded by D.A.R. State Park.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Skillern Peak. Skillern Peak, at above sea level is a peak in the Smoky Mountains of Idaho. The peak is located in Sawtooth National Forest in Camas County. It is located in the watershed of Big Smoky Creek, a tributary of the South Fork of the Boise River. It is about northwest of Big Peak and southeast of Paradise Peak.

Geographic entities mentioned:
surface_form: skillern peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.6874
lon: -114.816
Skillern Peak, at above sea level is a peak in the Smoky Mountains of Idaho. The peak is located in Sawtooth National Forest in Camas County. It is located in the watershed of Big Smoky Creek, a tributary of the South Fork of the Boise River. It is about northwest of Big Peak and southeast of Paradise Peak. No roads or trails go to the summit, although a trail is on the side of the mountain.

Geographic entities mentioned:
surface_form: paradise peak
instance_of: Mountain
countries: United States
coordinates: lat: 60.2675
lon: -149.1931
surface_form: big peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.6687
lon: -114.729
surface_form: paradise peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.7385
lon: -114.849
This watercourse is also known as Corte Madera Creek, although the actual stream of that name flows into San Francisco Bay further north at Point San Quentin. This watercourse has a catchment basin of about and drains the south-eastern slopes of Mount Tamalpais and much of the area in and around the town of Mill Valley; this stream discharges to Richardson Bay. History.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
In 1834, the governor of Alta California José Figueroa awarded to John T. Reed the first land grant in Marin, Rancho Corte Madera del Presidio. Watershed. The Arroyo Corte Madera del Presidio watershed drains of the southeast and east flanks of Mount Tamalpais. Arroyo Corte Madera del Presidio is joined by long Old Mill Creek on the right in Mill Valley.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
Arroyo Corte Madera del Presidio is joined by long Old Mill Creek on the right in Mill Valley. Old Mill Creek, and its long Cascade Creek tributary, both begin high on the south flank of the east peak of Mount Tamalpais. Cascade Creek has a small dam and reservoir which was built by noted engineer Michael M. O'Shaughnessy for The Tamalpais Land & Water Co. for water supply to Mill Valley.

Geographic entities mentioned:
surface_form: Mount Tamalpais
instance_of: Mountain
countries: United States
coordinates: lat: 37.9291
lon: -122.578
He left for India for the first time in 1538, on the fleet's flagship that transported viceroy Dom Garcia de Noronha, his cousin. Later, under the government of Noronha's successor, governor Dom Estevão da Gama, he joined an expedition to the Red Sea, and - after the Battle of El Tor - he was formally knighted by da Gama in Saint Catherine's Monastery, at the foot of Mount Sinai, in April 1541.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
The road would head into Philadelphia and possibly follow the path of the Manayunk Canal. Around Gustine Lake, the Manayunk Expressway would have an interchange with US 1 (Roosevelt Expressway). The freeway could have intersected with the Girard Avenue Expressway. The road was to pass through Center City and intersect with I-676/US 30.

Geographic entities mentioned:
surface_form: Gustine Lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0137
lon: -75.2046
Cap-Santé is on the northern bank of the Saint Lawrence River, west of Quebec City. Legend has it that this community's name was coined when soldiers suffering from an unknown disease miraculously recovered from a cure discovered in the village. The old settlement is situated just west of the nearby Jacques-Cartier River and on the embankment of the Saint Lawrence River. History.

Geographic entities mentioned:
surface_form: Jacques-Cartier River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
The quay is on the Saint Lawrence River. In 1759 following the defeat of the French at the Battle of the Plains of Abraham during the Seven Years' War, the commander of the French forces, Chevalier de Lévis, ordered the construction of Fort Jacques-Cartier at the mouth of the Jacques-Cartier River from materials originally destined for the construction of a church.

Geographic entities mentioned:
surface_form: Jacques-Cartier River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
Now one of them stepped up to me and asked me did I know
The green woods of Kilclooney or the Glens of Aherlow
Or could I tell where Crowley fell his native land to free
Or the tower that Captain Mackey sacked down Erin’s lovely Lee
‘Tis I can tell where Crowley fell ‘twas in Kilclooney Woods
And the tower that Captain Mackey sacked twas was by his side I stood.

Geographic entities mentioned:
surface_form: Glens of Aherlow
instance_of: Valley
countries: Ireland
coordinates: lat: 52.419
lon: -8.193
Schafberg (Boltigen). The Schafberg is a mountain peak above Boltigen located on the border between the cantons of Fribourg and Bern, north of Jaun. With a height 2,239 metres above sea level, it is the highest summit on the range lying north of the Jaun Pass. It is also the most isolated mountain in the canton of Fribourg.

Geographic entities mentioned:
surface_form: schafberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.63694444
lon: 7.31694444
He later sent an additional fifteen pounds to Bailey saying he would wrestle him at any time and any location with ten days notice. Meeske finally wrestled for the heavyweight championship against Bailey on November 22 at Melbourne Stadium, defeating him and becoming the recognized heavyweight champion of Australia. After his victory he went on holiday to Gippsland Lakes.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
Pony Creek (North Fork North Fabius River tributary). Pony Creek is a stream in Scotland County in the U.S. state of Missouri. It is a tributary of the North Fork North Fabius River. Pony Creek most likely was named for the fact local Indians owned ponies.

Geographic entities mentioned:
surface_form: pony creek
instance_of: Watercourse
countries: United States
coordinates: lat: 40.4866997
lon: -92.2224051
Sant Roc d'Amer. Sant Roc, also known as Sant Roc d'Amer, Sant Roc de la Barroca and Grony, is a mountain of the Catalan Transversal Range, Catalonia, Spain. It has an elevation of 591 metres above sea level.

Geographic entities mentioned:
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
Sant Roc d'Amer. Sant Roc, also known as Sant Roc d'Amer, Sant Roc de la Barroca and Grony, is a mountain of the Catalan Transversal Range, Catalonia, Spain. It has an elevation of 591 metres above sea level.

Geographic entities mentioned:
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
This mountain has a striking appearance and is quite visible from the road between Bonmatí and Sant Martí de Llémena. The steep cliffs on the southern and northeastern sides of the mountain are known as Cingles de Sant Roc. Historic sites. There are paleolithic archaeological sites in different points of the mountain; these are some of the oldest prehistoric sites of the area.

Geographic entities mentioned:
surface_form: cingles de sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
There are paleolithic archaeological sites in different points of the mountain; these are some of the oldest prehistoric sites of the area. There is also a small church with a Saint Roch shrine on top. This church is known as Ermita de Sant Roc and was mentioned in documents dating from 1447 as the parish church of La Barroca village, located 3 km to the northwest, past the Puig d'Elena mountain.

Geographic entities mentioned:
surface_form: sant roc
instance_of: Mountain
countries: Spain
coordinates: lat: 42.0174863364
lon: 2.66189985111
Vitim Nature Reserve. Vitim Nature Reserve () (also Vitimsky) is a Russian 'zapovednik' (strict nature reserve) in the mountains 400 km northeast of Lake Baikal in the Irkutsk region of Siberia. It covers the upper reaches of the Vitim River, a left tributary of the Lena River.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
It was formally established in 1982, and covers. Topography. The Vitim Reserve is in rugged mountain terrain with deep river valleys. It ascends from Lake Oron in the west to the top of the Kodar Mountain ridge in the south and east of the reserve. The Vitim River runs along the western border of the reserve. Climate and Ecoregion. Vitim is located in the &quot;East Siberian taiga&quot; ecoregion.

Geographic entities mentioned:
surface_form: Lake Oron
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 57.1025
lon: 116.53138889
They are mainly found in Puget Sound, the Oregon Coast Range, and the California Coast Ranges, but are also scattered on the west slope of the Sierra Nevada and Cascade mountain ranges. They are rare south of Santa Barbara County, with isolated stands south to Palomar Mountain in California.

Geographic entities mentioned:
surface_form: Palomar Mountain
instance_of: Mountain
countries: United States
Mexico
coordinates: lat: 33.363483333333
lon: -116.83639444444
Jelawat caused $43,200 thousand worth of damages throughout its onslaught. North Indian Ocean. The season began on January 30 with the formation of a tropical depression classified as BOB 01 over the Bay of Bengal. The storm's formation was the first January tropical cyclone in the basin since 2019. The JTWC later issued a TCFA on the system, designated as &quot;Invest 90B&quot;.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The JTWC later issued a TCFA on the system, designated as &quot;Invest 90B&quot;. It weakened after continued land interaction with Sri Lanka. After almost four months of inactivity, the IMD began to monitor a disturbance which was located in the Bay of Bengal on May 6. The system steadily improved and was upgraded to a depression by the IMD, classified as &quot;BOB 02&quot;.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
It later intensified into a Category 5-equivalent typhoon after striking Guam, becoming the strongest storm of the month and currently worldwide. In the Northern Indian Ocean basin, the IMD began monitoring a tropical depression which formed in the Bay of Bengal on May 9. The system was later named Mocha by the IMD after intensifying into a tropical storm.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
They evacuate the town to avoid more casualties. With all her men killed, Sheriff Alvarez (Sherilyn Fenn) and her partner Gunderson (Bruce Davison) try to call off an air strike after they spot Henderson and Quinn on Mount Rushmore trying to trap the creature. Gunderson gets killed when Bigfoot kicks his patrol car into a tree, crushing Henderson.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Liqiliqini (Peru). Liqiliqini (Aymara &quot;liqiliqi, liqi liqi&quot; Southern lapwing or Andean lapwing, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the Southern lapwing (or Andean lapwing)&quot;, also spelled &quot;Lecceleccene, Lejelejene&quot;) is a mountain in the northern extensions of the Apolobamba mountain range in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: liqiliqini
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5347
lon: -69.4067
Sapu Mhicha. Sapu Mhichā () is a Nepalese dish of the Newa community, made up of buffalo leaf tripe stuffed with bone marrow. Sapu Mhichā is a special delicacy of the Newa cuisine of the Kathmandu Valley and is usually prepared during special occasions. The delicacy is one of the dishes served to honor a man when he goes to the home of his wife's parents for festival dinners.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
The roadway continues as Young Harris Road to the unincorporated community of Warne, North Carolina. History. SR 66 originally existed in two sections north and south of the state's highest peak, Brasstown Bald. The southern route provided access to the top of the mountain, while the northern portion was only accessible by a long-closed wagon road built in the 1950s.

Geographic entities mentioned:
surface_form: Brasstown Bald
instance_of: Mountain
countries: United States
coordinates: lat: 34.874197222222
lon: -83.810652777778
Geography. The lake consists of four main bays, two in the south, two in the north. The main section of the lake is where it reaches its deepest depths, going as deep as 40 metres below the surface, which is slightly deeper than significantly larger Lake Winnipeg. There are many islands in Lac Grand, the largest being Ile-Des-Peres in Priest's Bay.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: lake winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
surface_form: winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Lac Grand's only outflow is into Lac Dam (sometimes spelled Lac Dame), which flows into Lac Brassard and finally Lac McGregor. There are several minerals to be found in the area, the most prominent being mica, both blue and black in colour, but green, caramel and black serpentine as well as olivine can be found as well. History. The lake used to be the location of a mica mine.

Geographic entities mentioned:
surface_form: blue
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.1
lon: -119.283
There are many islands in Lac Grand, the largest being Ile-Des-Peres in Priest's Bay. Lac Grand has two inflows, including a stream and waterfall from Lac McArthur and a narrow section of water from Lac Vert. Lac Grand's only outflow is into Lac Dam (sometimes spelled Lac Dame), which flows into Lac Brassard and finally Lac McGregor.

Geographic entities mentioned:
surface_form: lac mcgregor
instance_of: Lake
countries: Canada
coordinates: lat: 50.4239
lon: -112.852
There are many islands in Lac Grand, the largest being Ile-Des-Peres in Priest's Bay. Lac Grand has two inflows, including a stream and waterfall from Lac McArthur and a narrow section of water from Lac Vert. Lac Grand's only outflow is into Lac Dam (sometimes spelled Lac Dame), which flows into Lac Brassard and finally Lac McGregor.

Geographic entities mentioned:
surface_form: lac mcarthur
instance_of: Lake
countries: Canada
coordinates: lat: 46.37083
lon: -78.32389
surface_form: lac grand
instance_of: Lake
countries: Canada
coordinates: lat: 45.681
lon: -75.653
surface_form: lac vert
instance_of: Lake
countries: Canada
coordinates: lat: 48.365833
lon: -71.644999
surface_form: lac vert
instance_of: Lake
countries: Canada
coordinates: lat: 47.4525
lon: -70.92972222222222
surface_form: lac mcarthur
instance_of: Lake
countries: Canada
coordinates: lat: 48.2066
lon: -81.2132
Lac Grand (Quebec). Lake Grand (Lac Grand) is a private lake in the Outaouais region of Quebec, Canada. It covers an area of about 377 hectares and lies at an elevation of above sea level. There are no settlements on the lake, although it has many cottages on its shore. Despite having many cottages, some permanent residents live on the lake.

Geographic entities mentioned:
surface_form: lac grand (quebec)
instance_of: Lake
countries: Canada
coordinates: lat: 45.681
lon: -75.653
Lac Grand (Quebec). Lake Grand (Lac Grand) is a private lake in the Outaouais region of Quebec, Canada. It covers an area of about 377 hectares and lies at an elevation of above sea level. There are no settlements on the lake, although it has many cottages on its shore. Despite having many cottages, some permanent residents live on the lake.

Geographic entities mentioned:
surface_form: lac grand
instance_of: Lake
countries: Canada
coordinates: lat: 45.681
lon: -75.653
The main section of the lake is where it reaches its deepest depths, going as deep as 40 metres below the surface, which is slightly deeper than significantly larger Lake Winnipeg. There are many islands in Lac Grand, the largest being Ile-Des-Peres in Priest's Bay. Lac Grand has two inflows, including a stream and waterfall from Lac McArthur and a narrow section of water from Lac Vert.

Geographic entities mentioned:
surface_form: lac grand
instance_of: Lake
countries: Canada
coordinates: lat: 45.681
lon: -75.653
surface_form: lac grand
instance_of: Lake
countries: Canada
coordinates: lat: 45.681
lon: -75.653
Hatun Urqu (Huancavelica). Hatun Urqu (Quechua &quot;hatun&quot; big, &quot;urqu&quot;, mountain, &quot;big mountain&quot;, Hispanicized spelling &quot;Jatunorcco&quot;) is a mountain in the Huancavelica Region in Peru, about high. It is situated in the Huaytará Province, in the west of the Pilpichaca District.

Geographic entities mentioned:
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5194
lon: -71.8017
surface_form: hatun urqu (huancavelica)
instance_of: Mountain
countries: Peru
coordinates: lat: -13.3444
lon: -74.7222
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8719
lon: -71.7319
Hatun Urqu (Huancavelica). Hatun Urqu (Quechua &quot;hatun&quot; big, &quot;urqu&quot;, mountain, &quot;big mountain&quot;, Hispanicized spelling &quot;Jatunorcco&quot;) is a mountain in the Huancavelica Region in Peru, about high. It is situated in the Huaytará Province, in the west of the Pilpichaca District.

Geographic entities mentioned:
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5194
lon: -71.8017
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.3444
lon: -74.7222
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8719
lon: -71.7319
It is situated in the Huaytará Province, in the west of the Pilpichaca District. Hatun Urqu lies south of the mountain Yana Urqu (&quot;black mountain&quot;, Hispanicized &quot;Yanaorcco&quot;). Between these mountains there is an intermittent stream. It flows to the river Qullpamach'ay (&quot;salpeter cave&quot;, &quot;Jollpamachay&quot;) south of Hatun Urqu.

Geographic entities mentioned:
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.5194
lon: -71.8017
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.3444
lon: -74.7222
surface_form: hatun urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8719
lon: -71.7319
It is situated in the Huaytará Province, in the west of the Pilpichaca District. Hatun Urqu lies south of the mountain Yana Urqu (&quot;black mountain&quot;, Hispanicized &quot;Yanaorcco&quot;). Between these mountains there is an intermittent stream. It flows to the river Qullpamach'ay (&quot;salpeter cave&quot;, &quot;Jollpamachay&quot;) south of Hatun Urqu.

Geographic entities mentioned:
surface_form: yanaorcco
instance_of: Mountain
countries: Peru
coordinates: lat: -13.085277777778
lon: -74.978055555556
surface_form: yanaorcco
instance_of: Mountain
countries: Peru
coordinates: lat: -13.19138889
lon: -71.975
This is a protected and isolated area, having been kept closed by the Soviet Union since 1944. Western Sayan. At 92°E the Western Sayan system is pierced by the Ulug-Khem () or Upper Yenisei River, and at 106°, at its eastern extremity, it terminates above the depression of the Selenga-Orkhon Valley.

Geographic entities mentioned:
surface_form: Orkhon Valley
instance_of: Valley
countries: Mongolia
coordinates: lat: 47.556666666667
lon: 102.83138888889
It stretches almost at a right angle to the Western Sayan for in a roughly northeast/southwest direction between the Shapshal Range of the Eastern Altai in the west and the Abakan Range of the Kuznetsk Alatau in the east. From the Mongolian plateau the ascent is on the whole gentle, but from the plains of Siberia it is much steeper.

Geographic entities mentioned:
surface_form: Mongolian plateau
instance_of: Plateau
countries: Mongolia
People's Republic of China
Russia
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 107
The range includes a number of subsidiary ranges of an Alpine character, such as the Aradan, Borus, Oy, Kulumys, Mirsky, Kurtushibin, Uyuk, Sheshpir-Taiga, Ergak-Targak-Taiga, Kedran and Nazarovsky ranges. The most important peaks are Kyzlasov Peak (), Aradansky Peak (), Bedelig Golets (), Samzhir (), Borus () and Zvezdny Peak (). Between the breach of the Yenisei and Lake Khövsgöl at 100° 30' E.

Geographic entities mentioned:
surface_form: Kyzlasov Peak
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 51.651666666666664
lon: 89.20138888888889
In the central part, towards the upper reaches of the Kazyr and Kizir rivers, several ridges, such as the Kryzhin Range form a cluster culminating in the high Grandiozny Peak, the highest point in Krasnoyarsk Krai.

Geographic entities mentioned:
surface_form: Grandiozny Peak
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 53.89333333333333
lon: 96.0075
This was more of a probation post, to determine his fitness for more remote and unsupervised postings and after six months he received a transfer. The new appointment was in the West Suk District of Kerio Province. He was affiliated with the Royal African Society and authored
&quot;The Horn of Africa&quot; for the Royal Institute of International Affairs in October 1954 (Vol. 30, #4, pp. 440–449).

Geographic entities mentioned:
surface_form: Kerio
instance_of: Valley
countries: Kenya
coordinates: lat: 0.6401
lon: 35.6086
R. Ramanathan, who was from the University of Rangoon, to conduct further research at IACS. By early 1922, Raman came to a conclusion, as he reported in the &quot;Proceedings of the Royal Society of London&quot;:True to his words, Ramanathan published an elaborate experimental finding in 1923. His subsequent study of the Bay of Bengal in 1924 provided the full evidence.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Mostly covered by lush vegetation, it forms the floor of Marshwood Vale in the west of Dorset and can be seen in stream beds, where the land has been excavated, and along the coast to the west of Seatown. The sides of the vale are mainly made from the clays and sands of the upper and lower Lias, while younger strata from the Cretaceous Period (145–66 Mya), crown the higher points.

Geographic entities mentioned:
surface_form: Marshwood Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.78
lon: -2.83
These deposits occurred in a deep marine environment, 38° north. Deposited in an oxygen-deficient environment, the Kimmeridge beds make up the major part of the Purbeck Monocline and the periphery of the Weymouth Anticline. They form a low-lying band running north to south through the Blackmore Vale, and underpin the strip of land between the isle of Portland and the mainland.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
In 1550 the church was built. Geography. It is located in the southeasternmost part of the province of Biscay and limits at west with Abadiño, at east with Elorrio and at south with the province of Álava. The Ibaizabal river forms here, when it joins the Zumalegi river, which itself originates in the Anboto mountain.

Geographic entities mentioned:
surface_form: Anboto
instance_of: Mountain
countries: Spain
coordinates: lat: 43.089083333333
lon: -2.5953638888889
Studies published about the Muisca astronomy in 2011 and 2017 by Julio Bonilla Romero, revealed that the Sun seen from the northeastern corner of Bolívar Square, at the June solstice rises exactly above Monserrate and at the December solstice above Guadalupe Hill. At the equinoxes of March and September, Sué rises from the valley between these two landmarks in the Eastern Hills of the city.

Geographic entities mentioned:
surface_form: Monserrate
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.605833
lon: -74.056389
surface_form: Guadalupe Hill
instance_of: Mountain
countries: Colombia
coordinates: lat: 4.59194
lon: -74.0544
Østernvann. Østernvann is a lake north of Fossum in the municipality of Bærum in Akershus county, Norway.

Geographic entities mentioned:
surface_form: østernvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.969
lon: 10.588
M. Stanley to Africa to discover the course of the Congo River, and Stanley named after him a mountain to the north-east of Albert Edward Nyanza. Arnold must also be credited with the first idea of a great trunk line traversing the entire African continent, for in 1874 he first employed the phrase &quot;Cape to Cairo railway&quot; subsequently popularised by Cecil Rhodes.

Geographic entities mentioned:
surface_form: Albert Edward Nyanza
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6