Sarmila/GeoWiki-Features huggingface dataset:
Currently there are five deposits used for curative mud excavation in Estonia - Lake Ermistu, Haapsalu Tagalaht Bay, Mullutu Suurlaht Bay, Värska Bay and Käina Bay (Figure Estonian curative mud deposits in use). The largest curative lake mud resource is in Värska Bay (1 066 400 t), the smallest in Lake Ermistu (63 900 t).

Geographic entities mentioned:
surface_form: Lake Ermistu
instance_of: Lake
countries: Estonia
coordinates: lat: 58.36666667
lon: 23.975
The largest curative lake mud resource is in Värska Bay (1 066 400 t), the smallest in Lake Ermistu (63 900 t). The largest marine deposit is in Mullutu Suurlaht Bay (918 800 t), followed by Käina (273 800 t) and Haapsalu Tagalaht (161 200 t). In Estonia, over 600,000 t of curative mud has excavation permit.

Geographic entities mentioned:
surface_form: Mullutu Suurlaht
instance_of: Lake
countries: Estonia
coordinates: lat: 58.24583333
lon: 22.37916667
Brighams Tomb. Brighams Tomb is a summit in San Juan County, Utah, United States. Description. Brighams Tomb is situated northeast of Oljato–Monument Valley, Utah, on Navajo Nation land. It is an iconic landform of Monument Valley and can be seen from Highway 163. Precipitation runoff from this landform's slopes drains into the San Juan River drainage basin.

Geographic entities mentioned:
surface_form: navajo
instance_of: Mountain
countries: United States
coordinates: lat: 37.034169444444
lon: -110.86888888889
surface_form: brighams tomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.045833333333
lon: -110.08388888889
Brighams Tomb. Brighams Tomb is a summit in San Juan County, Utah, United States. Description. Brighams Tomb is situated northeast of Oljato–Monument Valley, Utah, on Navajo Nation land. It is an iconic landform of Monument Valley and can be seen from Highway 163. Precipitation runoff from this landform's slopes drains into the San Juan River drainage basin.

Geographic entities mentioned:
surface_form: brighams tomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.045833333333
lon: -110.08388888889
The buttes and mesas of Monument Valley are the result of the Organ Rock Shale being more easily eroded than the overlaying sandstone. Climate. Spring and fall are the most favorable seasons to visit Brighams Tomb. According to the Köppen climate classification system, it is located in a semi-arid climate zone with cold winters and hot summers.

Geographic entities mentioned:
surface_form: brighams tomb
instance_of: Mountain
countries: United States
coordinates: lat: 37.045833333333
lon: -110.08388888889
The rock ranges in age from Permian at the bottom to Late Triassic at the top. The buttes and mesas of Monument Valley are the result of the Organ Rock Shale being more easily eroded than the overlaying sandstone. Climate. Spring and fall are the most favorable seasons to visit Brighams Tomb.

Geographic entities mentioned:
surface_form: the organ
instance_of: Mountain
countries: United States
coordinates: lat: 37.2709548
lon: -112.9435175
It is situated at a height of about, about 1.02 km long and 0.4 km at its widest point. Ch'uspiqucha lies south of the mountain Qullqip'ukru of the Paryaqaqa mountain range and north of the lakes named P'itiqucha, Parya Chaka and Ch'uspi.

Geographic entities mentioned:
surface_form: Parya Chaka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.0272
lon: -76.0106
surface_form: parya
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8056
lon: -74.625
surface_form: parya chaka
instance_of: Mountain
countries: Peru
coordinates: lat: -12.0272
lon: -76.0106
surface_form: parya
instance_of: Mountain
countries: Peru
coordinates: lat: -10.1936
lon: -76.9117
surface_form: ch'uspi
instance_of: Mountain
countries: Peru
coordinates: lat: -10.51666667
lon: -76.72333333
surface_form: p'itiqucha
instance_of: Lake
countries: Peru
coordinates: lat: -11.545
lon: -76.434166666667
surface_form: paryaqaqa
instance_of: Mountain
countries: Peru
coordinates: lat: -11.991666666666667
lon: -75.99166666666666
Ch'uspiqucha (Huarochirí). Ch'uspiqucha (Quechua &quot;ch'uspi&quot; insect, generic name of flies or two-winged insects / fly, &quot;qucha&quot; lake, lagoon, &quot;fly lake&quot; or &quot;insect lake&quot;, hispanicized spelling &quot;Chuspicocha&quot;) is a lake in Peru located in the Lima Region, Huarochirí Province, Quinti District.

Geographic entities mentioned:
surface_form: ch'uspi
instance_of: Mountain
countries: Peru
coordinates: lat: -10.51666667
lon: -76.72333333
Ch'uspiqucha (Huarochirí). Ch'uspiqucha (Quechua &quot;ch'uspi&quot; insect, generic name of flies or two-winged insects / fly, &quot;qucha&quot; lake, lagoon, &quot;fly lake&quot; or &quot;insect lake&quot;, hispanicized spelling &quot;Chuspicocha&quot;) is a lake in Peru located in the Lima Region, Huarochirí Province, Quinti District.

Geographic entities mentioned:
surface_form: ch'uspiqucha (huarochirí)
instance_of: Lake
countries: Peru
coordinates: lat: -11.99972
lon: -76.01556
Werner Werenskiold (28 April 1883 – 2 August 1961) was a Norwegian geologist and geographer. He was a son of Erik Werenskiold and visual artist Sophie Marie Stoltenberg Thomesen (1849–1926), and the brother of Dagfin Werenskiold. Werenskiold made field studies in Telemark and Gudbrandsdalen in his younger days, and later focused on studies at Svalbard and of glaciers in Jotunheimen.

Geographic entities mentioned:
surface_form: Gudbrandsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.1333
lon: 10.35
He was a professor of geography at the University of Oslo from 1925. He lived and died in Bærum, and was on the election ballot for the Liberal People's Party (formerly the Liberal Left Party) in the 1930s. The mountain of Werenskioldfjellet at Hopen, Svalbard is named after him. The glacier of Werenskioldbreen in Wedel Jarlsberg Land, Svalbard is also named after him.

Geographic entities mentioned:
surface_form: Werenskioldfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 76.499
lon: 24.962
A fence joins the summit ridge about halfway along from the direction of Tarn Crag, and then makes for Harrop Pike. The true top has a small cairn, while Harrop Pike sports a more impressive columnar beacon. The views east and south are expansive while westwards the Coniston and Scafell groups can be seen. Ascents.

Geographic entities mentioned:
surface_form: Scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
This is one of four such pillars built during the construction of the Haweswater aqueduct. Below Branstree, Tarn Crag and Great Howe is the first section of the pipeline carrying water from the reservoir toward Manchester. The tunnel, some 1,000 ft below Great Howe, required 250 tons of gelignite for blasting, and when constructed in the 1930s was the longest such pipeline in Britain.

Geographic entities mentioned:
surface_form: Branstree
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482638888889
lon: -2.8087305555556
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.463
lon: -2.787
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.473
lon: -3.076
To the north of the summit is a marshy depression, containing Greycrag Tarn. This is a series of small pools in the bed of a larger historic water body. Beyond the tarn is Grey Crag's sister fell, Tarn Crag. Summit. The top of the fell is a short ridge with the summit at the south west end. Half a mile () to the north east is a second top, Harrop Pike, only marginally lower at.

Geographic entities mentioned:
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.463
lon: -2.787
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.473
lon: -3.076
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
Summit. The top of the fell is a short ridge with the summit at the south west end. Half a mile () to the north east is a second top, Harrop Pike, only marginally lower at. A fence joins the summit ridge about halfway along from the direction of Tarn Crag, and then makes for Harrop Pike. The true top has a small cairn, while Harrop Pike sports a more impressive columnar beacon.

Geographic entities mentioned:
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.463
lon: -2.787
surface_form: tarn crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.473
lon: -3.076
Grey Crag can be climbed from Longsleddale via Great Howe, or from the vicinity of the A6 (Shap) road via any of the long eastern ridges mentioned above. Haweswater aqueduct. Great Howe carries the remains of a surveying pillar on its eastern flank. This unusual stone and concrete construction is cleft at the top to provide a sight line and was originally surrounded by a wooden frame, now decayed.

Geographic entities mentioned:
surface_form: pillar
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.497
lon: -3.282
The principal tops are Ancrow Brow, White Howe, Lords Seat, and Great Yarlside. These ridges encompass the valleys of Bannisdale, Crookdale, Wet Sleddale, Borrowdale and Wasdale, the latter two of which should not be confused with their more famous Lakeland namesakes. To the north of the summit is a marshy depression, containing Greycrag Tarn.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Grey Crag. Grey Crag is a fell in the English Lake District. It stands to the east of Longsleddale in the Far Eastern Fells. Topography. North of Sadgill, the valley of Longsleddale narrows considerably with walls of crag on either side. Grey Crag is the first fell encountered above the eastern side, although the top is not visible from below.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
Topography. North of Sadgill, the valley of Longsleddale narrows considerably with walls of crag on either side. Grey Crag is the first fell encountered above the eastern side, although the top is not visible from below. What is in sight is a short flat-topped spur at a height of around which juts out southwards from the body of the fell.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
This is Great Howe, and its steep flanks provide the east wall of Longsleddale, together with further outcrops above the side valley of Stockdale. Grey Crag proper is a second tier of crags, set back from Great Howe and just below the summit, thus giving its name to the entire fell. Grey Crag is the focus of an extensive ridge system stretching out eastwards to the distant Lune and Eden Valleys.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
Grey Crag proper is a second tier of crags, set back from Great Howe and just below the summit, thus giving its name to the entire fell. Grey Crag is the focus of an extensive ridge system stretching out eastwards to the distant Lune and Eden Valleys. Grey Crag lies on the main watershed of the Cumbrian hills, its runoff reaching the sea at both the Solway Firth and Morecambe Bay.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
Grey Crag is the focus of an extensive ridge system stretching out eastwards to the distant Lune and Eden Valleys. Grey Crag lies on the main watershed of the Cumbrian hills, its runoff reaching the sea at both the Solway Firth and Morecambe Bay. The long east ridges have a moorland character and provide easy walking in quiet conditions.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
The views east and south are expansive while westwards the Coniston and Scafell groups can be seen. Ascents. Grey Crag can be climbed from Longsleddale via Great Howe, or from the vicinity of the A6 (Shap) road via any of the long eastern ridges mentioned above. Haweswater aqueduct. Great Howe carries the remains of a surveying pillar on its eastern flank.

Geographic entities mentioned:
surface_form: grey crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.457680555556
lon: -2.7773888888889
The long east ridges have a moorland character and provide easy walking in quiet conditions. The principal tops are Ancrow Brow, White Howe, Lords Seat, and Great Yarlside. These ridges encompass the valleys of Bannisdale, Crookdale, Wet Sleddale, Borrowdale and Wasdale, the latter two of which should not be confused with their more famous Lakeland namesakes.

Geographic entities mentioned:
surface_form: yarlside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3814
lon: -2.4861
It lies south of St. Jakob in Defereggen and east of the Austro-Italian border. The immediate neighbour of the &quot;Rote Spitze&quot; to the east is the somewhat higher Weiße Spitze (2,962 m). The names of the two summits are, however, not absolutely clear. This article adopts the names used by the Federal Office of Metrology and Survey.

Geographic entities mentioned:
surface_form: Weiße Spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 46.871388888889
lon: 12.358055555556
surface_form: rote spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 46.8761
lon: 12.3442
The names of the two summits are, however, not absolutely clear. This article adopts the names used by the Federal Office of Metrology and Survey. According to the inhabitants of the Defereggen valley, however, their names are reversed: they view the &quot;Rote Spitze&quot; as the higher, eastern summit.

Geographic entities mentioned:
surface_form: Defereggen valley
instance_of: Valley
countries: Austria
coordinates: lat: 46.915555555556
lon: 12.34
surface_form: rote spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 46.8761
lon: 12.3442
surface_form: rote spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 46.8761
lon: 12.3442
The &quot;Rote Spitze&quot; (2,956 m, the westernmost summit of the two aforementioned peaks) may be climbed both from the Defereggen valley - via Brugger Alm (1,818 m), Ragötzlalm (2,115 m) and Gschrittlenke (2,738 m) -, as well as from the Villgratental valley - via the Oberstalleralm (1,883 m) and Gschrittlenke. The final 150 metres of height below the summit are of climbing grade I+.

Geographic entities mentioned:
surface_form: Defereggen valley
instance_of: Valley
countries: Austria
coordinates: lat: 46.915555555556
lon: 12.34
Rote Spitze (Villgraten Mountains). The Rote Spitze is a mountain in Austria and, at, the second highest peak in the Villgraten Mountains. It lies south of St. Jakob in Defereggen and east of the Austro-Italian border. The immediate neighbour of the &quot;Rote Spitze&quot; to the east is the somewhat higher Weiße Spitze (2,962 m). The names of the two summits are, however, not absolutely clear.

Geographic entities mentioned:
surface_form: rote spitze
instance_of: Mountain
countries: Austria
coordinates: lat: 46.8761
lon: 12.3442
However, the simultaneous attack at Anzio limited the availability of air support for the river crossings. Lieutenant General Mark Clark, commanding general of the US Fifth Army ordered a crossing of the Gari River, south of Monte Cassino, with two regiments (the 141st and the 143rd Infantry) of the US 36th Infantry Division, commanded by Major General Fred Walker.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Battle. On the night of 20 January 1944, the US 36th Infantry Division, under command of Major General Geoffrey Keyes's II Corps, fired an artillery barrage of 31,000 rounds on German positions across the Gari River, which resulted in only negligible damage. Feint attacks were conducted by the 34th Infantry Division to the north, near Monte Cassino, to divert attention from the main advance.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
They are mainly of glacial origin, as glaciers significantly reshaped the landscape in the High Tatras, much more so than in the Western Tatras. These are mostly tarns, filling cirques, such as Czarny Staw pod Rysami or. Moraine-dammed lakes tend to be smaller and shallower. They formed in depressions dammed by lateral moraines () or terminal moraines ().

Geographic entities mentioned:
surface_form: Czarny Staw pod Rysami
instance_of: Lake
countries: Poland
coordinates: lat: 49.188333333333
lon: 20.076111111111
Moraine-dammed lakes tend to be smaller and shallower. They formed in depressions dammed by lateral moraines () or terminal moraines (). Morskie Oko and are cirque-moraine lakes, located in deepened glacial valleys, closed by rock thresholds upon which terminal moraine ridges settled. There are also kettle lakes that fill depressions left by so-called dead ice blocks.

Geographic entities mentioned:
surface_form: Morskie Oko
instance_of: Lake
countries: Poland
coordinates: lat: 49.197222222222
lon: 20.070833333333
There are a few small water bodies of different origins. These include karst lakes filling sinkholes (,), overflow ponds (e.g., in the expansions of), and ponds in ridge hollows (e.g., a pond on the Kasne pass). Additionally, there are about a dozen artificial lakes created by humans. Among these are, Nowe Morskie Oko near, and water reservoirs on (below Nosal and in). Characteristics.

Geographic entities mentioned:
surface_form: Nosal
instance_of: Mountain
countries: Poland
coordinates: lat: 49.2764
lon: 19.9894
Most of the Tatra lakes are characterized by very high transparency. The highest transparency (measured by the visibility of a submerged white disk) is found in high-altitude tarns. Record transparency has been recorded in Veľké Hincovo pleso (19 meters), in Czarny Staw pod Rysami (from 16.5 to 17.5 meters), and in Morskie Oko (12 meters).

Geographic entities mentioned:
surface_form: Veľké Hincovo pleso
instance_of: Lake
countries: Slovakia
coordinates: lat: 49.179166666667
lon: 20.059722222222
Compared to the lowland lakes of Poland, Tatra lakes have a small surface area, but some of them are remarkably deep, which is rare among lowland lakes. The largest lakes by surface area are located on the Polish side of the Tatras: Morskie Oko and Wielki Staw Polski. Depending on the measurement, one or the other of these lakes may hold the surface area record.

Geographic entities mentioned:
surface_form: Morskie Oko
instance_of: Lake
countries: Poland
coordinates: lat: 49.197222222222
lon: 20.070833333333
surface_form: Wielki Staw Polski
instance_of: Lake
countries: Poland
coordinates: lat: 49.2092
lon: 20.0408
The largest lakes by surface area are located on the Polish side of the Tatras: Morskie Oko and Wielki Staw Polski. Depending on the measurement, one or the other of these lakes may hold the surface area record. The third-largest by surface area is Czarny Staw pod Rysami. The deepest lake in the Tatras is Wielki Staw Polski (79.3 meters), which is also the third-deepest lake in Poland.

Geographic entities mentioned:
surface_form: Czarny Staw pod Rysami
instance_of: Lake
countries: Poland
coordinates: lat: 49.188333333333
lon: 20.076111111111
Tatra lakes generally have a rounded shape, with short shorelines, and deeply indented bays are rare. Small islands are found in only a few lakes. These islands formed from masses of scree that slid into the lake (e.g.,) or are roche moutonnées (rock outcrops) surrounded by water (e.g., Kurtkowiec). Kurtkowiec contains Poland's highest island (1,689 m).

Geographic entities mentioned:
surface_form: Kurtkowiec
instance_of: Lake
countries: Poland
coordinates: lat: 49.2294
lon: 20.0039
According to the Suda, Delphi took its name from the Delphyne, the she-serpent (&quot;drakaina&quot;) who lived there and was killed by the god Apollo (in other accounts the serpent was the male serpent (&quot;drakon&quot;) Python). The sacred precinct occupies a delineated region on the south-western slope of Mount Parnassus.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The sacred precinct occupies a delineated region on the south-western slope of Mount Parnassus. It is now an extensive archaeological site, and since 1938 a part of Parnassos National Park.

Geographic entities mentioned:
surface_form: Parnassos National Park
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
The modern town was created after removing buildings from the sacred precinct so that the latter could be excavated. The two Delphis, old and new, are located on Greek National Road 48 between Amfissa in the west and Livadeia, capital of Boeotia, in the east. The road follows the northern slope of a pass between Mount Parnassus on the north and the mountains of the Desfina Peninsula on the south.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Temple of Apollo. Ancient tradition refers to a succession of mythical temples on the site: first one built of olive branches from Tempe, then one built of beeswax and wings by bees, and thirdly one built by Hephaestus and Athena. The first archaeologically attested structure was built in the seventh century BC and is attributed in legend to the architects Trophonios and Agamedes.

Geographic entities mentioned:
surface_form: Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
The Homeric name of the oracle is &quot;Pytho&quot; (Πυθώ). Another legend held that Apollo walked to Delphi from the north and stopped at Tempe, a city in Thessaly, to pick laurel (also known as bay tree) which he considered to be a sacred plant. In commemoration of this legend, the winners at the Pythian Games received a wreath of laurel picked in the temple. The prophetic process.

Geographic entities mentioned:
surface_form: Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
Mount Hercules. Mount Hercules () is a large, flat-topped, elevated feature between Mount Aeolus and Mount Jason in the Olympus Range of Victoria Land, Antarctica. It was named by the Victoria University of Wellington Antarctic Expedition (1958–59) for Hercules, a figure in Greek mythology. Marsh Cirque is a cirque on the southern slopes of Mount Hercules.

Geographic entities mentioned:
surface_form: Mount Jason
instance_of: Mountain
coordinates: lat: -77.4911
lon: 161.558
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
surface_form: mount hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Marsh, of the Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland. Marsh investigated basement sill at McMurdo Dry Valleys sites in seven field seasons, 1995–2005, for the United States Antarctic Program. Mount Hercules is separated from Mount Jason by the Nakai Snowfield. Harris Ledge lies to the north, and just west of it is Fritsen Valley.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: dry valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
surface_form: seven
instance_of: Mountain
coordinates: lat: -69.6833
lon: 64.7
Marsh, of the Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland. Marsh investigated basement sill at McMurdo Dry Valleys sites in seven field seasons, 1995–2005, for the United States Antarctic Program. Mount Hercules is separated from Mount Jason by the Nakai Snowfield. Harris Ledge lies to the north, and just west of it is Fritsen Valley.

Geographic entities mentioned:
surface_form: Mount Jason
instance_of: Mountain
coordinates: lat: -77.4911
lon: 161.558
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
surface_form: mount hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Marsh, of the Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland. Marsh investigated basement sill at McMurdo Dry Valleys sites in seven field seasons, 1995–2005, for the United States Antarctic Program. Mount Hercules is separated from Mount Jason by the Nakai Snowfield. Harris Ledge lies to the north, and just west of it is Fritsen Valley.

Geographic entities mentioned:
surface_form: Fritsen Valley
instance_of: Valley
coordinates: lat: -77.4667
lon: 161.417
Mount Hercules () is a large, flat-topped, elevated feature between Mount Aeolus and Mount Jason in the Olympus Range of Victoria Land, Antarctica. It was named by the Victoria University of Wellington Antarctic Expedition (1958–59) for Hercules, a figure in Greek mythology. Marsh Cirque is a cirque on the southern slopes of Mount Hercules. The cirque is wide and in part occupied by a glacier.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
surface_form: mount hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Mount Hercules. Mount Hercules () is a large, flat-topped, elevated feature between Mount Aeolus and Mount Jason in the Olympus Range of Victoria Land, Antarctica. It was named by the Victoria University of Wellington Antarctic Expedition (1958–59) for Hercules, a figure in Greek mythology. Marsh Cirque is a cirque on the southern slopes of Mount Hercules.

Geographic entities mentioned:
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
surface_form: mount hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Mount Hercules. Mount Hercules () is a large, flat-topped, elevated feature between Mount Aeolus and Mount Jason in the Olympus Range of Victoria Land, Antarctica. It was named by the Victoria University of Wellington Antarctic Expedition (1958–59) for Hercules, a figure in Greek mythology. Marsh Cirque is a cirque on the southern slopes of Mount Hercules.

Geographic entities mentioned:
surface_form: hercules
instance_of: Mountain
coordinates: lat: -77.4833
lon: 161.433
Marsh Cirque is a cirque on the southern slopes of Mount Hercules. The cirque is wide and in part occupied by a glacier. It was named by the Advisory Committee on Antarctic Names in 2004 after geologist Bruce D. Marsh, of the Department of Earth and Planetary Sciences, Johns Hopkins University, Baltimore, Maryland.

Geographic entities mentioned:
surface_form: bruce
instance_of: Mountain
coordinates: lat: -65.0833
lon: -60.25
Budshah Bridge, locally also known as Budshah Kadal, is a concrete bridge located in the Srinagar city of the Indian union territory of Jammu and Kashmir. It was first built in 1957 during the rule of Bakshi Ghulam Mohammad and is named after the 15th Century ruler of Kashmir, Zain-ul-Abidin, popularly known as &quot;Budshah&quot; (the Great King). The bridge is also known as Alamgir Bridge.

Geographic entities mentioned:
surface_form: Kashmir
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Jebel Zem-Zem. Jebel Zem-Zem () is the name given to a mountain located north of M'diq below Fnideq in northern Morocco below the Spanish enclave of Ceuta. It is south west of the tourist resort Punta Restinga on the eastern coast. On its northern lower slopes lies an abandoned and ruined fort called &quot;Fortín Negrón&quot;.

Geographic entities mentioned:
surface_form: jebel zem-zem
instance_of: Mountain
countries: Morocco
coordinates: lat: 35.69143
lon: -5.62115
The lake has a catchment area of 251 km2, surface area of 45 km2, a length 16 km east–west / 5 km north–south, and a maximum depth of 52 m. Sapanca Lake is located on a tectonic hole, which is situated between Izmit Bay and Adapazari Meadow and runs parallel to Iznik Lake.

Geographic entities mentioned:
surface_form: Iznik Lake
instance_of: Lake
countries: Turkey
coordinates: lat: 40.443611111111
lon: 29.508333333333
Lake Sapanca. Lake Sapanca () (previous Greek name: Boáne (Βοάνη)) is a fresh water lake in Turkey, between the Gulf of İzmit and the Adapazarı Meadow. The lake has a catchment area of 251 km2, surface area of 45 km2, a length 16 km east–west / 5 km north–south, and a maximum depth of 52 m.

Geographic entities mentioned:
surface_form: lake sapanca
instance_of: Lake
countries: Turkey
coordinates: lat: 40.716666666667
lon: 30.25
Lake Sapanca. Lake Sapanca () (previous Greek name: Boáne (Βοάνη)) is a fresh water lake in Turkey, between the Gulf of İzmit and the Adapazarı Meadow. The lake has a catchment area of 251 km2, surface area of 45 km2, a length 16 km east–west / 5 km north–south, and a maximum depth of 52 m.

Geographic entities mentioned:
surface_form: lake sapanca
instance_of: Lake
countries: Turkey
coordinates: lat: 40.716666666667
lon: 30.25
surface_form: βοάνη
instance_of: Lake
countries: Turkey
coordinates: lat: 40.716666666667
lon: 30.25
Sapanca Lake is located on a tectonic hole, which is situated between Izmit Bay and Adapazari Meadow and runs parallel to Iznik Lake. The catchment area of Lake Sapanca - about 251 km2 [km²] - is surrounded by mountains in the south and small hills in the north. Water is taken from the lake for domestic and industrial needs.

Geographic entities mentioned:
surface_form: lake sapanca
instance_of: Lake
countries: Turkey
coordinates: lat: 40.716666666667
lon: 30.25
Demography. The Surruque lived around the Mosquito Lagoon (called Surruque Lagoon by the Spanish), near Cape Canaveral, and along the Atlantic coast north from the Cape up to near Ponce de Leon Inlet. The northern limit of Surruque territory was Turtle Mound, which was called &quot;Surruque&quot; in the early 17th century.

Geographic entities mentioned:
surface_form: Mosquito Lagoon
instance_of: Landform
countries: United States
coordinates: lat: 28.7508
lon: -80.7503
surface_form: Ponce de Leon Inlet
instance_of: Landform
countries: United States
coordinates: lat: 29.0725
lon: -80.91861111
Umba Valley. Umba Valley (&quot;Bonde la Umb&quot;a, in Swahili) is a geographic area in Tanzania and the world's only source of Umba sapphires. The Umba River flows through the Umba Valley. Specifically, Umba Valley is located in the north of the Usambara Mountains in the Tanga Region of Tanzania Between Mkinga and Lushoto Districts.

Geographic entities mentioned:
surface_form: umba
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.5
lon: 38.5
Umba Valley. Umba Valley (&quot;Bonde la Umb&quot;a, in Swahili) is a geographic area in Tanzania and the world's only source of Umba sapphires. The Umba River flows through the Umba Valley. Specifically, Umba Valley is located in the north of the Usambara Mountains in the Tanga Region of Tanzania Between Mkinga and Lushoto Districts.

Geographic entities mentioned:
surface_form: umba
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.5
lon: 38.5
surface_form: umba
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.5
lon: 38.5
surface_form: umba
instance_of: Valley
countries: Tanzania
coordinates: lat: -4.5
lon: 38.5
Yewdale Beck. Yewdale Beck is a river in Lake District, Cumbria, England. The Yewdale Beck arises from the confluence of Henfoot Beck and Swallow Scar Beck, as well as other unnamed tributaries east of Wetherlam.

Geographic entities mentioned:
surface_form: Wetherlam
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.401
lon: -3.098
The Yewdale Beck first flows in an easterly direction before it turns south-west of the settlement of Lower Tilberthwaite, which it changes again at the northern edge of the town of Coniston to the southeast. It then flows into the Coniston Water. The Yewdale Beck is a Site of Special Scientific Interest.

Geographic entities mentioned:
surface_form: Coniston Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.35
lon: -3.0666666666667
Cross-country skiing at the 2019 European Youth Olympic Winter Festival. Cross-country skiing at the 2019 European Youth Olympic Winter Festival was held from 11 to 15 February at Veliko polje, Igman, Bosnia and Herzegovina.

Geographic entities mentioned:
surface_form: Veliko polje, Igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
A 1983–84 survey of Malawi found the species to be common in all forested habitats at elevations of 1,200 m to 1,700. Currently in Malawi, it is known from the Namizimu Range, the Mangochi Hills, the Chikala Hills, the Zomba and Malosa Mountains, the Shire Highlands, the Thyolo Mountains, and Mount Mulanje.

Geographic entities mentioned:
surface_form: Shire Highlands
instance_of: Plateau
countries: Malawi
coordinates: lat: -15.64684105
lon: 35.12557983
The species has now probably been extirpated from most of the Shire Highlands near Blantyre, and from all of the Thyolo Mountains excepting a few remaining forest fragments in tea estates. In Mozambique, the species is known from Mount Namuli, Mount Mabu, Mount Chiperone, and Mount Inago.

Geographic entities mentioned:
surface_form: Mount Namuli
instance_of: Mountain
countries: Mozambique
coordinates: lat: -15.366666666667
lon: 37.033333333333
surface_form: Mount Mabu
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.298888888889
lon: 36.395555555556
surface_form: Mount Chiperone
instance_of: Mountain
countries: Mozambique
coordinates: lat: -16.47888889
lon: 35.71333333
Geography. The mountain lies northwest of Knockaunanattin (569 m). West of Stumpa Dúloigh the Dunkerron range splits in two parts: the NE one leads to Broaghnabinnia (745 m) while the SE sub-range reaches Knocknabreeda (569 m). With an elevation of 784 metres it is the 55th highest summit in Ireland. Access to the summit.

Geographic entities mentioned:
surface_form: Broaghnabinnia
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.972
lon: -9.744
surface_form: broaghnabinnia
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.972
lon: -9.744
With an elevation of 784 metres it is the 55th highest summit in Ireland. Access to the summit. Stumpa Dúloigh's summit can be accessed from the end of the Black Valley; it is a 6 hours' walk (there and back) suitable only for experienced hikers.

Geographic entities mentioned:
surface_form: the Black Valley
instance_of: Valley
countries: Ireland
coordinates: lat: 51.9487
lon: -9.6465
Stumpa Dúloigh. Stumpa Dúloigh (Irish for &quot;stump of the black lake&quot;) also known as Maol, is the highest of the Dunkerron Mountains, part of the Mountains of the Iveragh Peninsula in County Kerry, Ireland. It has a height of and lies southwest of MacGillycuddy's Reeks. Name. The mountain is named after a small lake called &quot;Loch an Dúloigh&quot; or Lough Duff.

Geographic entities mentioned:
surface_form: stumpa dúloigh
instance_of: Mountain
countries: Ireland
coordinates: lat: 51.9538
lon: -9.76525
Fatal accident. On July 23, 1999, during the offseason after his rookie NHL campaign, Tertyshny was on a boating trip to Okanagan Lake in British Columbia with two players from the Flyers' minor-league affiliate Philadelphia Phantoms, Francis Belanger and Mikhail Chernov, when he suffered fatal injuries in a freak accident.

Geographic entities mentioned:
surface_form: Okanagan Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Krypetsky Monastery. Krypetsky Monastery () is a Russian Orthodox monastery situated 23 km from Pskov. The monastery was founded in 1485 by St. Savva Krypetsky, a Serbian monk from Mount Athos, in what was then described as an impracticable mire. Two years later, the Pskov veche supported his establishment by granting a large plot of land to the monks.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Location. Neuburg Peak is in the southwest end of the Dufek Massif, looking over the Jaburg Glacier to the south. It is west of the Worcester Summit. The Clinton Spur is south of the mountain, Aughenbaugh Peak is to the east and the Cairn Ridge is to the north. To the west are the Hannah Peak and Walker Peak around the Enchanted Valley. The Brown Nunataks are west of the Enchanted Valley.

Geographic entities mentioned:
surface_form: Worcester Summit
instance_of: Mountain
coordinates: lat: -82.6
lon: -52.3667
Enchanted Valley. A small snow-filled valley between Walker Peak and Hannah Peak in the southwest end of Dufek Massif, Pensacola Mountains. The name describes the scenic beauty of the valley and was applied by the US-IGY party from Ellsworth Station that visited the valley in December 1957. Walker Peak. A sharp peak, high, marking the southwest extremity of Dufek Massif.

Geographic entities mentioned:
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
It is west of the Worcester Summit. The Clinton Spur is south of the mountain, Aughenbaugh Peak is to the east and the Cairn Ridge is to the north. To the west are the Hannah Peak and Walker Peak around the Enchanted Valley. The Brown Nunataks are west of the Enchanted Valley. Clinton Spur. A rock spur on the south side of Dufek Massif, southeast of Neuburg Peak.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for Paul T. Walker, glaciologist at Ellsworth Station, a member of the first party to visit Dufek Massif, in December 1957. Brown Nunataks. Three nunataks lying northwest of Walker Peak at the southwest extremity of Dufek Massif. Mapped by USGS from surveys and United States Navy air photos, 1956-66.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
Walker, glaciologist at Ellsworth Station, a member of the first party to visit Dufek Massif, in December 1957. Brown Nunataks. Three nunataks lying northwest of Walker Peak at the southwest extremity of Dufek Massif. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for John B. Brown, ionospheric scientist, Ellsworth Station winter party, 1957.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
England Peak. A sharp peak about high, located south of Aughenbaugh Peak and east of Neuburg Peak. Named by US-ACAN at the suggestion of USGS field party leader Arthur B. Ford after Anthony W. England, USGS geophysicist who worked in the Dufek Massif during the 1976-77 and 1978-79 seasons. Tranquillity Valley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
Tranquillity Valley. A snow-covered valley between Hannah Peak and Cairn Ridge in the west part of Dufek Massif. The name was proposed by Arthur B. Ford, USGS geologist, leader of several USGS field parties to the Pensacola Mountains, 1965-79. Named from its typical weather conditions, the valley being protected from strong winds most of the time.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
Named from its typical weather conditions, the valley being protected from strong winds most of the time. The USGS snowmobile parties coming from cold, windy areas found welcome refuge in this valley. The name is also in accord with nearby Enchanted Valley to indicate the general beauty of this part of Dufek Massif. Cairn Ridge.

Geographic entities mentioned:
surface_form: the general
instance_of: Mountain
coordinates: lat: 44.483387
lon: -114.802816
Named from association with Tranquillity Valley; also because during the 1976-77 season, Arthur B. Ford and Willis H. Nelson, of USGS, on discovery of a Soviet Antarctic Expedition helicopter cache left here the previous summer, left a note of welcome to the Dufek Massif for the Soviet Antarctic Expedition party leader, Garrik Grikurov. Pyroxenite Promontory.

Geographic entities mentioned:
surface_form: nelson
instance_of: Body of water
coordinates: lat: -62.35
lon: -59.2833
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Tranquillity Valley. A snow-covered valley between Hannah Peak and Cairn Ridge in the west part of Dufek Massif. The name was proposed by Arthur B. Ford, USGS geologist, leader of several USGS field parties to the Pensacola Mountains, 1965-79. Named from its typical weather conditions, the valley being protected from strong winds most of the time.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
A cairn was erected on this ridge during a visit in December 1957 by the US-IGY traverse party from Ellsworth Station. Welcome Pass. A snow pass between Cairn Ridge and Czamanske Ridge, providing access to Tranquillity Valley. Named from association with Tranquillity Valley; also because during the 1976-77 season, Arthur B. Ford and Willis H.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
A promontory rising to about high near the west end of Dufek Massif. The feature is located west of Neuburg Peak and projects northwest toward Rautio Nunatak. The name was proposed by Arthur B. Ford, leader of the USGS geological party in the Pensacola Mountains, 1978-79, from the pyroxenite rock which forms a conspicuous dark layer along the cliffs of the promontory. Rautio Nunatak.

Geographic entities mentioned:
surface_form: arthur
instance_of: Mountain
coordinates: lat: -67.65
lon: 49.86667
The name was proposed by Arthur B. Ford, USGS geologist, leader of several USGS field parties to the Pensacola Mountains, 1965-79. Named from its typical weather conditions, the valley being protected from strong winds most of the time. The USGS snowmobile parties coming from cold, windy areas found welcome refuge in this valley.

Geographic entities mentioned:
surface_form: strong
instance_of: Mountain
coordinates: lat: -70.583333333333
lon: -62.75
Clinton Spur. A rock spur on the south side of Dufek Massif, southeast of Neuburg Peak. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for Lieutenant Clinton R. Smith, (MC) United States Navy, of the Ellsworth Station winter party, 1957. Aughenbaugh Peak. A sharp peak, over high, standing northeast of Neuburg Peak.

Geographic entities mentioned:
surface_form: smith
instance_of: Lake
coordinates: lat: -66.1167
lon: 101.283
Neuburg Peak. Neuburg Peak () is a jagged rock peak in Antarctica, high, rising east of Walker Peak in the southwest part of Dufek Massif, Pensacola Mountains. Mapping and name. Neuburg Peak was mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photographs from 1956 to 1966.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
surface_form: neuburg peak
instance_of: Mountain
coordinates: lat: -82.6167
lon: -52.9
Neuburg Peak is in the southwest end of the Dufek Massif, looking over the Jaburg Glacier to the south. It is west of the Worcester Summit. The Clinton Spur is south of the mountain, Aughenbaugh Peak is to the east and the Cairn Ridge is to the north. To the west are the Hannah Peak and Walker Peak around the Enchanted Valley. The Brown Nunataks are west of the Enchanted Valley. Clinton Spur.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
Named by US-ACAN after Henry Rautio, photographer, United States Navy Squadron VX-6, who obtained reconnaissance photographs of the Pensacola Mountains from LC-47 aircraft on January 22, 1964. Hannah Peak. A sharp peak at the southwest end of Dufek Massif north-northeast of Walker Peak. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for James L.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
surface_form: sharp peak
instance_of: Mountain
coordinates: lat: -62.5237
lon: -60.0692
Enchanted Valley. A small snow-filled valley between Walker Peak and Hannah Peak in the southwest end of Dufek Massif, Pensacola Mountains. The name describes the scenic beauty of the valley and was applied by the US-IGY party from Ellsworth Station that visited the valley in December 1957. Walker Peak. A sharp peak, high, marking the southwest extremity of Dufek Massif.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
Walker Peak. A sharp peak, high, marking the southwest extremity of Dufek Massif. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for Paul T. Walker, glaciologist at Ellsworth Station, a member of the first party to visit Dufek Massif, in December 1957. Brown Nunataks. Three nunataks lying northwest of Walker Peak at the southwest extremity of Dufek Massif.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
Named by US-ACAN for Paul T. Walker, glaciologist at Ellsworth Station, a member of the first party to visit Dufek Massif, in December 1957. Brown Nunataks. Three nunataks lying northwest of Walker Peak at the southwest extremity of Dufek Massif. Mapped by USGS from surveys and United States Navy air photos, 1956-66. Named by US-ACAN for John B.

Geographic entities mentioned:
surface_form: walker
instance_of: Mountain
coordinates: lat: -64.81666667
lon: -62.01666667
Neuburg Peak. Neuburg Peak () is a jagged rock peak in Antarctica, high, rising east of Walker Peak in the southwest part of Dufek Massif, Pensacola Mountains. Mapping and name. Neuburg Peak was mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photographs from 1956 to 1966.

Geographic entities mentioned:
surface_form: neuburg peak
instance_of: Mountain
coordinates: lat: -82.6167
lon: -52.9
Neuburg Peak () is a jagged rock peak in Antarctica, high, rising east of Walker Peak in the southwest part of Dufek Massif, Pensacola Mountains. Mapping and name. Neuburg Peak was mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photographs from 1956 to 1966. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Hugo A.C.

Geographic entities mentioned:
surface_form: neuburg peak
instance_of: Mountain
coordinates: lat: -82.6167
lon: -52.9
Neuburg, a glaciologist at Ellsworth Station and a member of the first party to visit Dufek Massif in December 1957. Location. Neuburg Peak is in the southwest end of the Dufek Massif, looking over the Jaburg Glacier to the south. It is west of the Worcester Summit. The Clinton Spur is south of the mountain, Aughenbaugh Peak is to the east and the Cairn Ridge is to the north.

Geographic entities mentioned:
surface_form: neuburg peak
instance_of: Mountain
coordinates: lat: -82.6167
lon: -52.9