Sarmila/GeoWiki-Features huggingface dataset:
Mount York. Mount York, a mountain in the western region of the Explorer Range, part of the Blue Mountains Range that is a spur off the Great Dividing Range, is located approximately west of Sydney, just outside Mount Victoria in New South Wales, Australia.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
Mount York. Mount York, a mountain in the western region of the Explorer Range, part of the Blue Mountains Range that is a spur off the Great Dividing Range, is located approximately west of Sydney, just outside Mount Victoria in New South Wales, Australia.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
surface_form: mount victoria
instance_of: Mountain
countries: Australia
coordinates: lat: -41.3308
lon: 147.837
Mount York has an elevation of and is a projection of the Blue Mountains dissected plateau, creating a promontory of the western escarpment with a minor rise at its summit. Description. Mount York is mainly forested in Eucalypt growth, mostly open canopied. Several small creeks that flow into the Coxs River system run down its side.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
Several small creeks that flow into the Coxs River system run down its side. A twin promontory to its immediate east branching from the southern origin of Mount York promontory is also an extension of the western escarpment. Lockley Promontory and Mount York Promontory both jut northwest from the western escarpment, and begin at Mount Victoria, a small mountain village.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
A twin promontory to its immediate east branching from the southern origin of Mount York promontory is also an extension of the western escarpment. Lockley Promontory and Mount York Promontory both jut northwest from the western escarpment, and begin at Mount Victoria, a small mountain village. Several bushwalking tracks are to be found here, including Berghofers Pass, Lockyers Road and Coxs Road.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
surface_form: mount victoria
instance_of: Mountain
countries: Australia
coordinates: lat: -41.3308
lon: 147.837
Several bushwalking tracks are to be found here, including Berghofers Pass, Lockyers Road and Coxs Road. The tracks branch off from Mount York and descend into the valley below, or in the case of Berghofers, in the direction of Little Hartley, west of Mount Victoria.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
surface_form: mount victoria
instance_of: Mountain
countries: Australia
coordinates: lat: -41.3308
lon: 147.837
Many termite mounds can be seen along the road. The mountain is about two to three hundred metres above the Hartley Valley. History. The mountain now known as Mount York lies on the traditional lands of the Dharug people, very close to the eastern edge of traditional lands of the Wirajuri people.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
Mount York was the point where Gregory Blaxland, William Lawson and William Wentworth viewed the Hartley Valley and the 'west' for the first time during their successful crossing of the Blue Mountains in 1813, although some Europeans had already reached the valley before them.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
However, their 'first crossing' and opening of the west to farming in 1813 is commemorated with several memorials atop the summit, one with their faces set in stone. There are two metal fenced lookouts, a westward facing and northward facing one. Mount York was the site of various attempts to build a pass to the plains west of the Blue Mountains. The first was Coxs Road, constructed in 1813.

Geographic entities mentioned:
surface_form: mount york
instance_of: Mountain
countries: Australia
coordinates: lat: -33.553
lon: 150.22
Also still visible is Berghofers Pass, which was abandoned because of later developments, and which has also been turned into a walking track. John Berghofer, who was responsible for this pass, is interred at Mount Victoria Cemetery.

Geographic entities mentioned:
surface_form: mount victoria
instance_of: Mountain
countries: Australia
coordinates: lat: -41.3308
lon: 147.837
Some time later, when manufacturing became important, the arsenal expanded to a second area south and west in Springfield, where water power was available. Around that time, the Mill River was dammed to form a mile-long lake called Watershops Pond. The main shops were behind the dam and a foundry was built below it.

Geographic entities mentioned:
surface_form: Watershops Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.1042
lon: -72.5499
Haplochromis pharyngomylus. &quot;Haplochromis pharyngomylus&quot; is a species of cichlid endemic to Lake Victoria. This species can reach a length of SL. This species feeds mainly on mollusks with both bivalves and gastropods eaten in approximately equal proportions.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
North Arapaho Peak. North Arapaho Peak is the highest summit of the Indian Peaks in the northern Front Range of the Rocky Mountains of North America.

Geographic entities mentioned:
surface_form: north arapaho peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.026666666667
lon: -105.65
Between North Arapaho Peak and neighboring South Arapaho Peak sits Arapaho Glacier, which is owned by the City of Boulder as part of its water supply. North and South Arapahoe Peaks are connected by a, Class 4 connecting ridge. West of these peaks is Arapaho Pass. Climate.

Geographic entities mentioned:
surface_form: north arapaho peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.026666666667
lon: -105.65
Of the 101 sites explored in the Tantamayo region, 25 were studied in particular in 1955 and 1956 in the company of Marc Corcos. Many of the monuments discovered, such as those at Piruro, Japallán, Selmín Granero and Susupillo, reveal a type of architecture previously unknown in South America (3- and 4-storey buildings).

Geographic entities mentioned:
surface_form: Susupillo
instance_of: Mountain
countries: Peru
coordinates: lat: -9.4
lon: -76.6844
I want a paper and I don't have one. Sell me your paper.&quot; The deal was done and the &quot;Tulsa Democrat&quot; became the &quot;Tulsa Tribune&quot; on December 1, 1919. Jones immediately took up a long-running local political issue: the Spavinaw Water Project. Tulsa leaders had been studying alternative sources of city water since at least 1915.

Geographic entities mentioned:
surface_form: Spavinaw Water Project
instance_of: Lake
countries: United States
coordinates: lat: 36.3818
lon: -95.0477
She got underway for the east coast, transiting the Panama Canal 6 December. Three days later off the coast of Florida, a PBM–3D (Mariner) landed close aboard to ask assistance. Peterson towed the disabled plane to Ponce de Leon Inlet where a crash boat from New Smyrna took over the tow. She then continued up the coast to Charleston, South Carolina, arriving 10 December 1945.

Geographic entities mentioned:
surface_form: Ponce de Leon Inlet
instance_of: Landform
countries: United States
coordinates: lat: 29.0725
lon: -80.91861111
Where it is found. Kuna Crest granodiorite is tied to Kuna Peak, also in Yosemite, and Kuna Crest, being first identified on Kuna Crest, from which Kuna Peak rises. It is exposed at Glacier Point, and is found, on the east end of Yosemite Valley. It is also found on the west side of the pluton and near Tioga Pass on the east side of the Sierra Nevada batholith.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Nevertheless, the origin of the &quot;Dead lake&quot; etymology remains speculative and unknown. Geography. Lough Marrave lies north east of Keshcarrigan village, and east of Lough Scur. The lake is very small and shallow, covering a surface-area of about, and might be considered a continuation of Lough Scur, as they share the same level and connected by a half-mile channel.

Geographic entities mentioned:
surface_form: Lough Scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
surface_form: lough scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
Geography. Lough Marrave lies north east of Keshcarrigan village, and east of Lough Scur. The lake is very small and shallow, covering a surface-area of about, and might be considered a continuation of Lough Scur, as they share the same level and connected by a half-mile channel. Lough Marrave is connected to St. John's Lough and Lough Scur by the Shannon–Erne Waterway. Ecology.

Geographic entities mentioned:
surface_form: Lough Scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
surface_form: lough scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
Geography. Lough Marrave lies north east of Keshcarrigan village, and east of Lough Scur. The lake is very small and shallow, covering a surface-area of about, and might be considered a continuation of Lough Scur, as they share the same level and connected by a half-mile channel. Lough Marrave is connected to St. John's Lough and Lough Scur by the Shannon–Erne Waterway. Ecology.

Geographic entities mentioned:
surface_form: St. John's Lough
instance_of: Lake
countries: Ireland
coordinates: lat: 54.040277777778
lon: -7.8630555555556
surface_form: Lough Scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
surface_form: lough scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
The primary human settlements at Lough Marrave are Keshcarrigan and Fenagh villages. Lough Marrave is bounded by the townlands of Gubroe to the south and east, Killmacsherwell to the north, and Rossy to the west. Heritage. The Keshcarrigan Bowl was discovered in the canal between Lough Scur and Lough Marrave in the 19th century, and is today preserved at the National Museum of Ireland.

Geographic entities mentioned:
surface_form: Lough Scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
surface_form: lough scur
instance_of: Lake
countries: Ireland
coordinates: lat: 54.02527778
lon: -7.95583333
surface_form: lough marrave
instance_of: Lake
countries: Ireland
coordinates: lat: 54.03333333333333
lon: -7.933333333333334
Lough Marrave. Lough Marrave () is a small freshwater lake in County Leitrim in the northwest of Ireland. Etymology. () translates to &quot;. It is plausible Lough Marrave served a pagan sacrificial purpose, and the Keshcarrigan Bowl was deposited there as a ritual offering.

Geographic entities mentioned:
surface_form: lough marrave
instance_of: Lake
countries: Ireland
coordinates: lat: 54.03333333333333
lon: -7.933333333333334
Etymology. () translates to &quot;. It is plausible Lough Marrave served a pagan sacrificial purpose, and the Keshcarrigan Bowl was deposited there as a ritual offering. There is a reference in the &quot; to an unidentified and &quot; on the &quot;road to Fenagh&quot;, with a marginal note attributed to Tadhg O'Roddy (1700) adding: &quot;.

Geographic entities mentioned:
surface_form: lough marrave
instance_of: Lake
countries: Ireland
coordinates: lat: 54.03333333333333
lon: -7.933333333333334
Lough Marrave is connected to St. John's Lough and Lough Scur by the Shannon–Erne Waterway. Ecology. The presence and type of fish found in Lough Marrave is not recorded. The ecology of County Leitrim waterways, such as Lough Marrave, is threatened by zebra mussel and other invasive species. Human settlement. The primary human settlements at Lough Marrave are Keshcarrigan and Fenagh villages.

Geographic entities mentioned:
surface_form: lough marrave
instance_of: Lake
countries: Ireland
coordinates: lat: 54.03333333333333
lon: -7.933333333333334
The ecology of County Leitrim waterways, such as Lough Marrave, is threatened by zebra mussel and other invasive species. Human settlement. The primary human settlements at Lough Marrave are Keshcarrigan and Fenagh villages. Lough Marrave is bounded by the townlands of Gubroe to the south and east, Killmacsherwell to the north, and Rossy to the west. Heritage.

Geographic entities mentioned:
surface_form: lough marrave
instance_of: Lake
countries: Ireland
coordinates: lat: 54.03333333333333
lon: -7.933333333333334
Before European colonization, the land was inhabited for thousands of years by the Mi'kmaq. Later, the community was named after George Germain, 1st Viscount Sackville. Upper Sackville is situated in the Sackville River valley immediately north of Middle Sackville and south of Mount Uniacke on Trunk 1. It is approximately by road from Downtown Halifax.

Geographic entities mentioned:
surface_form: Sackville River
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.7331
lon: -63.6658
surface_form: Mount Uniacke
instance_of: Mountain
countries: Canada
coordinates: lat: 44.89194444444445
lon: -63.826388888888886
Bituminous coal was mined at nearby Minersville and transported by inclined plane. Transportation of iron ore was from over 100 miles away via canal, but this proved difficult, as did transportation of flux from the Nittany Valley. The financial Panic of 1837 forced the furnace to close in 1838.

Geographic entities mentioned:
surface_form: Nittany Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.9
lon: -77.7
Ninety Five Hill. Ninety Five Hill is a summit located in Central New York Region of New York located in the Town of Remsen in Oneida County, west-northwest of Ninety Six Corners.

Geographic entities mentioned:
surface_form: ninety five hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.35118
lon: -75.12183
Ninety Five Hill. Ninety Five Hill is a summit located in Central New York Region of New York located in the Town of Remsen in Oneida County, west-northwest of Ninety Six Corners.

Geographic entities mentioned:
surface_form: ninety five hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.35118
lon: -75.12183
surface_form: oneida
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
Hoggestabben Butte. Hoggestabben Butte () is a prominent butte, high, standing north of Mount Hochlin and being its highest northern outlier, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Hoggestabben (the chopping block).

Geographic entities mentioned:
surface_form: Mount Hochlin
instance_of: Mountain
coordinates: lat: -72.0833
lon: 4.05
surface_form: hofmann
instance_of: Mountain
coordinates: lat: -82.6667
lon: 160.6
surface_form: hoggestabben
instance_of: Mountain
coordinates: lat: -72
lon: 3.96667
Hoggestabben Butte. Hoggestabben Butte () is a prominent butte, high, standing north of Mount Hochlin and being its highest northern outlier, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Hoggestabben (the chopping block).

Geographic entities mentioned:
surface_form: hoggestabben butte
instance_of: Mountain
coordinates: lat: -72
lon: 3.96667
Hoggestabben Butte. Hoggestabben Butte () is a prominent butte, high, standing north of Mount Hochlin and being its highest northern outlier, in the Mühlig-Hofmann Mountains of Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by the Sixth Norwegian Antarctic Expedition (1956–60) and named Hoggestabben (the chopping block).

Geographic entities mentioned:
surface_form: hoggestabben
instance_of: Mountain
coordinates: lat: -72
lon: 3.96667
Pulham. Pulham is a village and civil parish in the county of Dorset in south-west England. It is situated in the Blackmore Vale, southeast of Sherborne. In the 2011 Census the civil parish had 105 dwellings, 103 households and a population of 269.

Geographic entities mentioned:
surface_form: Blackmore Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.94
lon: -2.31
Reiss also attributes the burning of the Albanian villages in the Preševo Valley, carried out by the Serbian army during the First Balkan War and described by the then war correspondent of the &quot;Kiev Thought&quot; Lev Trotsky, to the Bulgarian army and presents the villages as &quot;Serbian&quot;.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
- He died before reaching the hospital. After his death, his body was buried in the Topčider cemetery and, at his own request, his heart was buried in the Saint Peter Church on Kajmakčalan hill. The urn containing his heart was later demolished as revenge by the Bulgarians in World War II. Legacy.

Geographic entities mentioned:
surface_form: Kajmakčalan
instance_of: Mountain
countries: Greece
North Macedonia
coordinates: lat: 40.930277777778
lon: 21.786111111111
The Funicular Rigiblick () is a funicular railway in the north-east of the city of Zürich, Switzerland. It links a lower station served by Zürich tram routes 9 and 10 and Zürich trolleybus route 33, with an upper station at Rigiblick on the Zürichberg hill. The Rigiblick funicular is one of two funiculars within the city of Zürich, the other being the Polybahn funicular in the city centre.

Geographic entities mentioned:
surface_form: Zürichberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.3856
lon: 8.56694
Of the agricultural land, 64.3% is used for growing crops and 6.2% is pastures, while 7.7% is used for orchards or vine crops. All the water in the municipality is flowing water. The municipality is located in the low hills between Lake Biel and the Seeland region. It consists of the villages of Epsach, Klus and Baar.

Geographic entities mentioned:
surface_form: Lake Biel
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.085555555556
lon: 7.1741666666667
Mount Inglismaldie. Mount Inglismaldie is the second-highest peak of the Fairholme Range in Banff National Park. It is located immediately west of Mount Girouard in the Bow River valley south of Lake Minnewanka. The mountain was named in 1886 by park superintendent George A. Stewart after Inglismaldie Castle in Kincardineshire, Scotland. The first ascent of the mountain was made in 1933 by H.

Geographic entities mentioned:
surface_form: Mount Girouard
instance_of: Mountain
countries: Canada
coordinates: lat: 51.236111111111114
lon: -115.40305555555555
Mount Inglismaldie. Mount Inglismaldie is the second-highest peak of the Fairholme Range in Banff National Park. It is located immediately west of Mount Girouard in the Bow River valley south of Lake Minnewanka. The mountain was named in 1886 by park superintendent George A. Stewart after Inglismaldie Castle in Kincardineshire, Scotland. The first ascent of the mountain was made in 1933 by H.

Geographic entities mentioned:
surface_form: mount inglismaldie
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2417
lon: -115.421
Wylie, Betts, Dickson, W. Innes, L. DeCouteur, J. Miskow, Sadler, and Vallance with guide Lawrence Grassi. Geology. Like other mountains in Banff National Park, Mount Inglismaldie is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate.

Geographic entities mentioned:
surface_form: mount inglismaldie
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2417
lon: -115.421
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Inglismaldie is located in a subarctic climate 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: mount inglismaldie
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2417
lon: -115.421
Climate. Based on the Köppen climate classification, Mount Inglismaldie is located in a subarctic climate with cold, snowy winters, and mild summers. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Inglismaldie drains into Lake Minnewanka and the Bow River.

Geographic entities mentioned:
surface_form: mount inglismaldie
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2417
lon: -115.421
Mount Inglismaldie. Mount Inglismaldie is the second-highest peak of the Fairholme Range in Banff National Park. It is located immediately west of Mount Girouard in the Bow River valley south of Lake Minnewanka. The mountain was named in 1886 by park superintendent George A. Stewart after Inglismaldie Castle in Kincardineshire, Scotland. The first ascent of the mountain was made in 1933 by H.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is located immediately west of Mount Girouard in the Bow River valley south of Lake Minnewanka. The mountain was named in 1886 by park superintendent George A. Stewart after Inglismaldie Castle in Kincardineshire, Scotland. The first ascent of the mountain was made in 1933 by H. Foster, J. Packer, M.C. Wylie, Betts, Dickson, W. Innes, L. DeCouteur, J.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The city hosts the second-largest flour-mills in Greece, &quot;Kepenou-Mills&quot;. Energy sector. Acciona has completed the largest wind park in Greece, on the Panachaiko mountain, overlooking the city of Patras. The Public Electric Company, operates a small hydroelectric plant on river Glafkos. IT sector.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
Kjeglefjella. Kjeglefjella (Cone Mountains) is a mountain range in Nordenskiöld Land at Spitsbergen, Svalbard. It is located between Hollendardalen, Passfjellbreen, Lailadalen and Colesbukta, and has an extension of about fourteen kilometers. Among the mountains in the range are Vesle Kjeglefjellet, Luxtoppen, Noxtoppen, Ravnhøgda, Vesuv, Vestalfjellet, Rundkollen and Oppkuven.

Geographic entities mentioned:
surface_form: Hollendardalen
instance_of: Valley
countries: Norway
coordinates: lat: 78.0582
lon: 14.5816
Finger Ridges. The Finger Ridges () are several mainly ice-free ridges and spurs extending over a distance of about, east–west, in the northwestern part of the Cook Mountains in Antarctica. Location. The Finger Ridges are in the northwest of the Cook Mountains, to the east of Butcher Ridge, north of Harvey Peak and west of Henry Mesa. The highest points on the main ridge are about.

Geographic entities mentioned:
surface_form: Harvey Peak
instance_of: Mountain
coordinates: lat: -79.2167
lon: 157.017
Bishopdale is a dale in the Yorkshire Dales National Park in North Yorkshire, England. The dale is a side dale on the south side of Wensleydale, and extends for some south west from Aysgarth. Bishopdale is also the name of a civil parish, which includes only the sparsely populated upper reaches of the dale, from the head of the dale as far downstream as Howesyke and Howgill Gill. Geography.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
The Bishopdale Beck flows through the dale to join the River Ure about east of Aysgarth. The B6160 road follows the path of the river from its junction with the A684 to the watershed at Kidstones Pass where it continues to Cray and Buckden in Upper Wharfedale. The highest point in the dale on the road is to be found at Kidstones, some above sea level.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
Bishopdale, North Yorkshire. Bishopdale is a dale in the Yorkshire Dales National Park in North Yorkshire, England. The dale is a side dale on the south side of Wensleydale, and extends for some south west from Aysgarth.

Geographic entities mentioned:
surface_form: bishopdale, north yorkshire
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
Bishopdale, North Yorkshire. Bishopdale is a dale in the Yorkshire Dales National Park in North Yorkshire, England. The dale is a side dale on the south side of Wensleydale, and extends for some south west from Aysgarth.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
Bishopdale is a dale in the Yorkshire Dales National Park in North Yorkshire, England. The dale is a side dale on the south side of Wensleydale, and extends for some south west from Aysgarth. Bishopdale is also the name of a civil parish, which includes only the sparsely populated upper reaches of the dale, from the head of the dale as far downstream as Howesyke and Howgill Gill. Geography.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
Geography. There are three villages in the dale, all in its lower part: West Burton, Thoralby and Newbiggin. The Bishopdale Beck flows through the dale to join the River Ure about east of Aysgarth. The B6160 road follows the path of the river from its junction with the A684 to the watershed at Kidstones Pass where it continues to Cray and Buckden in Upper Wharfedale.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
The highest point in the dale on the road is to be found at Kidstones, some above sea level. From 1974 to 2023 it was part of the district of Richmondshire, it is now administered by the unitary North Yorkshire Council. Civil parish of Bishopdale. Bishopdale civil parish includes only the sparsely populated upper reaches of the dale.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
From 1974 to 2023 it was part of the district of Richmondshire, it is now administered by the unitary North Yorkshire Council. Civil parish of Bishopdale. Bishopdale civil parish includes only the sparsely populated upper reaches of the dale. It extends from the head of the dale as far downstream as Howesyke and Howgill Gill.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
It extends from the head of the dale as far downstream as Howesyke and Howgill Gill. The civil parish of Bishopdale was a township of the ancient parish of Aysgarth, and became a separate civil parish in 1866. It now shares a grouped parish council, the Aysgarth & District Parish Council, with Aysgarth, Newbiggin, Thoralby and Thornton Rust.

Geographic entities mentioned:
surface_form: bishopdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.25
lon: -2.01667
She remembered a boy shouting &quot;fire&quot; while a brass band was playing on the deck of the ship to entertain the travelers. She recounted the images of mothers and children with their clothing on fire drowning in the rough waters of Hell Gate. Others were killed as they were drawn into the blades of the paddlewheel.

Geographic entities mentioned:
surface_form: Hell Gate
instance_of: Landform
countries: United States
coordinates: lat: 40.78102
lon: -73.92452
He grew up in great poverty, from six to sixteen in Beckenried, his mother's home village. As a boy, he tended goats on the Buochserhorn, combed silk and spun cotton; later, he gathered resin with his father, searched for roots for doctors and distillers, and wood for coopers and other craftsmen. As he grew older, he worked as a farmhand. Matthys did not attend school until he was 21 years old.

Geographic entities mentioned:
surface_form: Buochserhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.945555555556
lon: 8.4286111111111
Dicaeus (mythology). In Greek mythology, Dicaeus or Dikaios () was a son of Poseidon and brother was Syleus. They lived near the Mountain Pelion in Thessaly. Mythology. Dicaeus hosted Herakles. Unlike Syleus, who was killed by Herakles, Dicaeus was a just man, which was suggested by the very literal meaning of his name (Δίκαιος = Just). The Dicaea city in Thrace was named after him.

Geographic entities mentioned:
surface_form: Mountain Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
On 17 July 1940 the 1st (Royal) Natal Carbineers sailed for Kenya as part of the 1st South African Brigade. Their destination was the Italian colonial empire in East Africa. For the next 10 months the Regiment participated in the South African advance through Italian Somaliland and Abyssinia (now Ethiopia), until Italian resistance was broken at Amba Alagi in May 1941. Western Desert 1941–1943.

Geographic entities mentioned:
surface_form: Amba Alagi
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.983333333333
lon: 39.55
Medicine Grizzly Lake. Medicine Grizzly Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is surrounded by high peaks including Triple Divide Peak to the west and Mount James to the north.

Geographic entities mentioned:
surface_form: Mount James
instance_of: Mountain
countries: United States
coordinates: lat: 48.5844
lon: -113.492
surface_form: triple divide peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.573055555556
lon: -113.51666666667
Medicine Grizzly Lake. Medicine Grizzly Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is surrounded by high peaks including Triple Divide Peak to the west and Mount James to the north.

Geographic entities mentioned:
surface_form: medicine grizzly lake
instance_of: Lake
countries: United States
coordinates: lat: 48.5664
lon: -113.496
They gag at a gnat and swallow a camel.&quot;
Morals. The 9th District councilman opined that San Fernando Valley communities would &quot;not be having problems with topless-bottomless bars if moral levels matched those&quot; of his Downtown Los Angeles and South L.A. district. &quot;We have clean-minded people and a clean district,&quot; he said.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Taxonomy. &quot;Hibbertia hamulosa&quot; was first formally described in 2000 by Judith R. Wheeler in the journal &quot;Nuytsia&quot; from specimens collected by Ruurd Dirk Hoogland on the south-west slope of East Mount Barren in 1971. The specific epithet (&quot;hamulosa&quot;) means &quot;armed with small hooks&quot;, referring to the hairs on the outside of the sepals. Distribution and habitat.

Geographic entities mentioned:
surface_form: East Mount Barren
instance_of: Mountain
countries: Australia
coordinates: lat: -33.9231
lon: 120.025
Charles de Gaulle Bridge. The Charles de Gaulle Bridge is a bridge that links the eastern tip of the island of Montreal, Quebec over the Rivière des Prairies to the Lanaudière region near the city of Charlemagne.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Mount Olympus (Utah). Mount Olympus in the U.S. state of Utah is one of the most prominent and recognizable mountains visible from practically every location in the Salt Lake Valley. Mount Olympus is not the tallest peak along the Wasatch Front, but its unusual form and location make it a popular hiking destination for locals.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
The mountain is situated east of the center of the Salt Lake Valley, directly east of Holladay. Distinctive features of the mountain are its twin peaks and other outcroppings, the highest of which is called &quot;Summit Peak&quot; and which towers above the valley to an elevation of. Thus, the peak looms about above the valley floor. Hiking.

Geographic entities mentioned:
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.7516
lon: -122.448
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 43.16
lon: -109.659
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 37.589722222222
lon: -105.51916666667
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.59384
lon: -111.72104
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 36.66181
lon: -118.71414
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 45.303888888889
lon: -117.34388888889
surface_form: summit peak
instance_of: Mountain
countries: United States
coordinates: lat: 37.3506
lon: -106.697
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 39.0423585
lon: -106.4254736
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: twin peaks
instance_of: Landform
countries: United States
coordinates: lat: 37.0797
lon: -121.69
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.92892
lon: -115.84438
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.794722222222
lon: -111.84111111111
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 40.551944444444
lon: -111.65666666667
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
surface_form: twin peaks
instance_of: Mountain
countries: United States
coordinates: lat: 38.08298
lon: -119.35322
state of Utah is one of the most prominent and recognizable mountains visible from practically every location in the Salt Lake Valley. Mount Olympus is not the tallest peak along the Wasatch Front, but its unusual form and location make it a popular hiking destination for locals. The mountain is situated east of the center of the Salt Lake Valley, directly east of Holladay.

Geographic entities mentioned:
surface_form: salt lake valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Thus, the peak looms about above the valley floor. Hiking. Because of its proximity, visibility, and accessibility to a large metropolitan area, Mount Olympus has been a popular hiking destination for the residents of the Salt Lake Valley for many years. Most hikers reach the summit via the Mount Olympus Trail, which is a steep hike from the mountain base and stretches approximately to the summit.

Geographic entities mentioned:
surface_form: salt lake valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.2767785
lon: -98.6946248
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 44.965
lon: -96.443611111111
surface_form: salt lake
instance_of: Lake
countries: United States
coordinates: lat: 45.635555555556
lon: -99.9175
Mount Olympus (Utah). Mount Olympus in the U.S. state of Utah is one of the most prominent and recognizable mountains visible from practically every location in the Salt Lake Valley. Mount Olympus is not the tallest peak along the Wasatch Front, but its unusual form and location make it a popular hiking destination for locals.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus (utah)
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
state of Utah is one of the most prominent and recognizable mountains visible from practically every location in the Salt Lake Valley. Mount Olympus is not the tallest peak along the Wasatch Front, but its unusual form and location make it a popular hiking destination for locals. The mountain is situated east of the center of the Salt Lake Valley, directly east of Holladay.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
Thus, the peak looms about above the valley floor. Hiking. Because of its proximity, visibility, and accessibility to a large metropolitan area, Mount Olympus has been a popular hiking destination for the residents of the Salt Lake Valley for many years. Most hikers reach the summit via the Mount Olympus Trail, which is a steep hike from the mountain base and stretches approximately to the summit.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
This peak is also a popular winter hiking route because the terrain is not as avalanche prone as many of the surrounding peaks. Due to the trail's elevation and tree density, it remains snow-covered until May, and early spring hiking is best aided by snowshoes. Hiding near the base of Mount Olympus lies Utah's second deepest, and the United States' 13th deepest cave, known as Neffs Cave.

Geographic entities mentioned:
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 47.801305555556
lon: -123.71083333333
surface_form: mount olympus
instance_of: Mountain
countries: United States
coordinates: lat: 40.6566
lon: -111.771
The mountain is situated east of the center of the Salt Lake Valley, directly east of Holladay. Distinctive features of the mountain are its twin peaks and other outcroppings, the highest of which is called &quot;Summit Peak&quot; and which towers above the valley to an elevation of. Thus, the peak looms about above the valley floor. Hiking.

Geographic entities mentioned:
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
Matheson Island Airport. Matheson Island Airport was located on Matheson Island in Lake Winnipeg, Manitoba, Canada.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Norsketinden. Norsketinden is a mountain in the Stauning Alps, Eastern Greenland. Geography. Norsketinden is one of the highest mountains in the range. It rises roughly 12 km to the east of the shore of the Alpefjord —a branch of the Segelsällskapet Fjord, between the Vikingebrae and the Gully Glacier. Although according to available sources this mountain is a, or peak.

Geographic entities mentioned:
surface_form: norsketinden
instance_of: Mountain
countries: Greenland
coordinates: lat: 72.136302777778
lon: -25.051575
Although according to available sources this mountain is a, or peak. it appears as a peak in Google Earth. Climbing history. Norsketinden was first climbed by a Danish–Norwegian expedition on 7 August 1954. The names 'Erik Rødes Tinde' or 'Eirik Raudes Tinde' —after Erik the Red, were proposed, but the peak was finally named &quot;Norsketinden&quot;.

Geographic entities mentioned:
surface_form: norsketinden
instance_of: Mountain
countries: Greenland
coordinates: lat: 72.136302777778
lon: -25.051575
Eagle Rock (formation). Eagle Rock, L.A. Historic-Cultural Monument No. 10, is a large dome-shaped rock formation with an indentation that resembles an eagle in flight. The neighborhood of Eagle Rock, where the rock is located is named after the rock. Once known as Eagle Rock Valley, it incorporated in 1911 and was annexed by Los Angeles in 1923.

Geographic entities mentioned:
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.1075
lon: -118.571
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.143055555556
lon: -118.18277777778
10, is a large dome-shaped rock formation with an indentation that resembles an eagle in flight. The neighborhood of Eagle Rock, where the rock is located is named after the rock. Once known as Eagle Rock Valley, it incorporated in 1911 and was annexed by Los Angeles in 1923. Given its visibility from the Ventura Freeway, CA-134, Eagle Rock is a familiar sight to millions. History.

Geographic entities mentioned:
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.1075
lon: -118.571
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.143055555556
lon: -118.18277777778
The neighborhood of Eagle Rock, where the rock is located is named after the rock. Once known as Eagle Rock Valley, it incorporated in 1911 and was annexed by Los Angeles in 1923. Given its visibility from the Ventura Freeway, CA-134, Eagle Rock is a familiar sight to millions. History. Eagle Rock is a large sandstone formation created by hot springs millions of years ago.

Geographic entities mentioned:
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.1075
lon: -118.571
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.143055555556
lon: -118.18277777778
Given its visibility from the Ventura Freeway, CA-134, Eagle Rock is a familiar sight to millions. History. Eagle Rock is a large sandstone formation created by hot springs millions of years ago. Formerly known as La Piedra Gorda (Fat Rock), a name given to it by Spanish settlers, locals have been calling it Eagle Rock (or The Rock) since at least 1888.

Geographic entities mentioned:
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.1075
lon: -118.571
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.143055555556
lon: -118.18277777778
History. Eagle Rock is a large sandstone formation created by hot springs millions of years ago. Formerly known as La Piedra Gorda (Fat Rock), a name given to it by Spanish settlers, locals have been calling it Eagle Rock (or The Rock) since at least 1888. The first published illustration of La Piedra Gorda was made by Archduke of Austria, Ludwig Louis Salvator. His book was published in 1878.

Geographic entities mentioned:
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.1075
lon: -118.571
surface_form: eagle rock
instance_of: Mountain
countries: United States
coordinates: lat: 34.143055555556
lon: -118.18277777778
New farms built on the land of Hof were inhabited; however, the main farm has been abandoned since 1999. Hof's land holdings are incredibly vast, encompassing all the land between the Hofsá river in Vesturdalur and the Vestari-Jökulsá all the way south to Hofsjökull glacier, which is named for Hof.

Geographic entities mentioned:
surface_form: Vesturdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.3006217771
lon: -19.0496290206
It is divided into 12 floristic provinces according to the work of Armen Takhtajan, a Soviet-Armenian botanist who created a classification system for flowering plants. One of the main characteristics of the region is a great diversity and abundance of species, especially in the Iranian Plateau.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Many residents emigrated to escape the poverty. In the 17th and 18th centuries they went to Germany or the Swiss Plateau, while in the late 18th and 19th centuries they went to the United States and settled in the Carolinas, Pennsylvania and Kentucky. In the early 19th century mountain climbers began to come to Guttannen to explore the high peaks above the valley.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The Aare springs from glaciers in Guttannen. There are four lakes in the municipality: Lake Oberaar, Lake Grimsel, Lake Räterichsboden and Lake Gelmer. In the western part of the municipality are the mountains Schreckhorn, Lauteraarhorn, Finsteraarhorn, Agassizhorn and Sidelhorn. Guttannen also includes Finsteraar Glacier, Lauteraar Glacier, Unteraar Glacier, Grueben Glacier, and Bächli Glacier.

Geographic entities mentioned:
surface_form: Schreckhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58993
lon: 8.11816
surface_form: Lauteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.583388888889
lon: 8.1284166666667
surface_form: Finsteraarhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.537472222222
lon: 8.1260277777778
surface_form: Agassizhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.546580555556
lon: 8.1144388888889
surface_form: Sidelhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.552388888889
lon: 8.3126944444444