Sarmila/GeoWiki-Features huggingface dataset:
Twin Lakes (Alaska). Twin Lakes is a complex of two large lakes in Lake Clark National Park in the U.S. state of Alaska, near the northeast corner of Lake and Peninsula Borough. It contains a upper lake and a smaller lower lake, joined by a short connecting stream. The lakes outflow westward into the Chilikadrotna River (and eventually into the Mulchatna and Nushagak Rivers and Nushagak Bay).

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes (alaska)
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Twin Lakes (Alaska). Twin Lakes is a complex of two large lakes in Lake Clark National Park in the U.S. state of Alaska, near the northeast corner of Lake and Peninsula Borough. It contains a upper lake and a smaller lower lake, joined by a short connecting stream. The lakes outflow westward into the Chilikadrotna River (and eventually into the Mulchatna and Nushagak Rivers and Nushagak Bay).

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: lake clark
instance_of: Lake
countries: United States
coordinates: lat: 60.244166666667
lon: -154.28527777778
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Lake Andrew (Douglas County, Minnesota). Lake Andrew (also called Lake Andrews) is a lake in Douglas County, in the U.S. state of Minnesota. Lake Andrew is a quiet, spring-fed lake located just south of Alexandria. With a size of, it is popular for recreational activities and a good lake for anglers. The most recent Lake Survey reports mean and maximum depths are and, respectively.

Geographic entities mentioned:
surface_form: lake andrew
instance_of: Lake
countries: United States
coordinates: lat: 45.31
lon: -95.043888888889
surface_form: lake andrew (douglas county, minnesota)
instance_of: Lake
countries: United States
coordinates: lat: 45.820833333333
lon: -95.421944444444
Lake Andrew (Douglas County, Minnesota). Lake Andrew (also called Lake Andrews) is a lake in Douglas County, in the U.S. state of Minnesota. Lake Andrew is a quiet, spring-fed lake located just south of Alexandria. With a size of, it is popular for recreational activities and a good lake for anglers. The most recent Lake Survey reports mean and maximum depths are and, respectively.

Geographic entities mentioned:
surface_form: lake andrew
instance_of: Lake
countries: United States
coordinates: lat: 45.31
lon: -95.043888888889
surface_form: lake andrew
instance_of: Lake
countries: United States
coordinates: lat: 45.820833333333
lon: -95.421944444444
The most recent Lake Survey reports mean and maximum depths are and, respectively. Water clarity is considered good. According to Warren Upham, Lake Andrews was probably named for a physician in Alexandria. Alternatively, according to Eugene Roth Family records, Lake Andrew was named for Andrew (Andreas) Roth, a prominent citizen and successful farmer of Douglas County.

Geographic entities mentioned:
surface_form: lake andrew
instance_of: Lake
countries: United States
coordinates: lat: 45.31
lon: -95.043888888889
surface_form: lake andrew
instance_of: Lake
countries: United States
coordinates: lat: 45.820833333333
lon: -95.421944444444
Overview. The Mingachevir Reservoir is the largest reservoir in the Caucasus, having a length of, a width of, maximum depth of, average depth of, maximum volume of 15.73 km3, shoreline length of, and overall area of. The reservoir's water level is maintained by the dam of the Mingachevir Hydro Power Plant, built near Mount Bozdağ from 1945 to 1953.

Geographic entities mentioned:
surface_form: Mount Bozdağ
instance_of: Mountain
countries: Azerbaijan
coordinates: lat: 40.83333333
lon: 46.75
The name translates as &quot;big mountain of Assynt&quot;, and with a height of it is the highest point in Sutherland. The mountain lies in the east of Assynt, set apart from the area's better known and more dramatic (but lower) mountains such as Suilven. It is hidden from the traveller on the A837 road by the adjacent Munro of Conival, and the best views of it are obtained from nearby summits.

Geographic entities mentioned:
surface_form: Suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
surface_form: suilven
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.115
lon: -5.1370694444444
The mountain lies in the east of Assynt, set apart from the area's better known and more dramatic (but lower) mountains such as Suilven. It is hidden from the traveller on the A837 road by the adjacent Munro of Conival, and the best views of it are obtained from nearby summits. The higher slopes of the mountain are capped by light coloured quartzite boulders, giving it a distinctive appearance.

Geographic entities mentioned:
surface_form: Conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
The mountain's eastern and southern slopes are drained by the River Oykel and its tributary, the River Cassley, which flow into the Dornoch Firth on Scotland's east coast. The River Traligill drains the western flanks through Loch Assynt to reach the Atlantic at Lochinver. The mountain is connected to the neighbouring peak of Conival to the west by a lofty ridge with a low point of.

Geographic entities mentioned:
surface_form: Loch Assynt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.176347
lon: -5.053878
surface_form: loch assynt
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.176347
lon: -5.053878
The summit is marked by a shattered lump of quartzite. The sharp arête is quite tricky to negotiate in places; according to Ralph Storer, it &quot;has been flatteringly compared to the Aonach Eagach, with several unexpectedly awkward moves across exposed slabs requiring care (especially when wet)&quot;. Wildlife and conservation. Ben More Assynt is home to many threatened species of vegetation.

Geographic entities mentioned:
surface_form: Aonach Eagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
surface_form: aonach eagach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.679497
lon: -5.012554
Ben More Assynt. Ben More Assynt () is a mountain in Assynt in the far northwest of Scotland, north-northeast of Ullapool. The name translates as &quot;big mountain of Assynt&quot;, and with a height of it is the highest point in Sutherland. The mountain lies in the east of Assynt, set apart from the area's better known and more dramatic (but lower) mountains such as Suilven.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: ben more assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
The higher slopes of the mountain are capped by light coloured quartzite boulders, giving it a distinctive appearance. Over of land around Ben More Assynt have been declared a Site of Special Scientific Interest (SSSI) because of their geological interest and rare plant species. Geography.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: ben more assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
Geology. The Assynt area lies within the Moine Thrust Belt and is a classic locality in the history of the development of theories about thrust tectonics. The mountains of Ben More Assynt and Conival sit on the Ben More thrust sheet which is bounded by the Ben More Thrust below and the Moine Thrust above.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
The thrust sheet consists of Lewisian gneiss with a cover of Torridonian sandstones and Cambrian quartzite. Lewisian gneisses are exposed to the south and southeast of the peak of Ben More Assynt and forms the ridge to the South Top, making it the highest located example of this rock type.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: ben more assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
From Inchnadamph the route of ascent follows the River Traligill to its source on the col between Conival and Beinn an Fhurain at a height of. It is then a stiff climb over shattered quartzite to reach Conival’s highest point. Ben More Assynt’s summit lies east and is a demanding walk over quartzite stones and scree, even though there is only just over 100 metres of re-ascent.

Geographic entities mentioned:
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
The future of the proposal is still in discussion. New Memorial. In April 1941, during the Second World War, all 6 of the crew on board an Avro Anson were killed when the aircraft crashed on Ben More Assynt. Due to the inaccessibility of the crash site, the crew were buried on the mountain; their final resting places marked with a cairn.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: ben more assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
In 2012, the Commonwealth War Graves Commission decided to replace the existing cairn, which had deteriorated in the harsh climate, with a 600-kilogramme granite marker to identify and protect the burial site. At an elevation of around, the burial site on Ben More Assynt is one of the Commission’s most remote grave sites in the UK and the logistics of replacing the cairn have proved challenging.

Geographic entities mentioned:
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.424829
lon: -6.014015
surface_form: ben more
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.385952
lon: -4.540087
surface_form: ben more assynt
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.138164
lon: -4.858208
Lewisian gneisses are exposed to the south and southeast of the peak of Ben More Assynt and forms the ridge to the South Top, making it the highest located example of this rock type. The peak itself consists of Cambrian quartzite, which also forms the ridge to Conival and the ground to the north and northeast of the peak. Torridonian sediments are only exposed around Conival. Ascents.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
The River Traligill drains the western flanks through Loch Assynt to reach the Atlantic at Lochinver. The mountain is connected to the neighbouring peak of Conival to the west by a lofty ridge with a low point of. Since Conival lies in the way of the ascent from Inchnadamph, the two are almost invariably ascended together.

Geographic entities mentioned:
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
Lewisian gneisses are exposed to the south and southeast of the peak of Ben More Assynt and forms the ridge to the South Top, making it the highest located example of this rock type. The peak itself consists of Cambrian quartzite, which also forms the ridge to Conival and the ground to the north and northeast of the peak. Torridonian sediments are only exposed around Conival. Ascents.

Geographic entities mentioned:
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
Torridonian sediments are only exposed around Conival. Ascents. An ascent of Ben More Assynt is usually combined with the neighbouring Munro of Conival, which if starting from the hamlet of Inchnadamph (grid reference), is climbed first. From Inchnadamph the route of ascent follows the River Traligill to its source on the col between Conival and Beinn an Fhurain at a height of.

Geographic entities mentioned:
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
An ascent of Ben More Assynt is usually combined with the neighbouring Munro of Conival, which if starting from the hamlet of Inchnadamph (grid reference), is climbed first. From Inchnadamph the route of ascent follows the River Traligill to its source on the col between Conival and Beinn an Fhurain at a height of. It is then a stiff climb over shattered quartzite to reach Conival’s highest point.

Geographic entities mentioned:
surface_form: conival
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.135689
lon: -4.883497
The Venetians feared that Doria would attack Venice next, and placed a heavy chain to bar entrance to the San Marco basin, while compulsory loan was levied, the population capable of bearing arms was assessed, and a force of 300 men was mobilized from each of the city's six districts and placed under the overall command of Paolo Loredan.

Geographic entities mentioned:
surface_form: San Marco basin
instance_of: Body of water
countries: Italy
coordinates: lat: 45.4295
lon: 12.345
Reovačka greda. Reovačka greda () is a ridge of Mount Orjen located in Krivošije, in southwestern Montenegro, separating the Bijela Gora plateau from the rest of the Orjen range. The ridge stretches for 17 kilometres from Vučji zub peak on the west, at the border of Montenegro and Bosnia and Herzegovina, and the villages of Crkvice and Malov Do on the east.

Geographic entities mentioned:
surface_form: Krivošije
instance_of: Landform
countries: Montenegro
coordinates: lat: 42.55
lon: 18.65
surface_form: Bijela Gora
instance_of: Plateau
countries: Montenegro
Bosnia and Herzegovina
coordinates: lat: 42.585
lon: 18.57
surface_form: reovačka greda
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.57694444
lon: 18.57
Reovačka greda () is a ridge of Mount Orjen located in Krivošije, in southwestern Montenegro, separating the Bijela Gora plateau from the rest of the Orjen range. The ridge stretches for 17 kilometres from Vučji zub peak on the west, at the border of Montenegro and Bosnia and Herzegovina, and the villages of Crkvice and Malov Do on the east. Its highest peak is Pazua, which is 1,769 metres high.

Geographic entities mentioned:
surface_form: Vučji zub
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.58111111
lon: 18.55361111
Reovačka greda. Reovačka greda () is a ridge of Mount Orjen located in Krivošije, in southwestern Montenegro, separating the Bijela Gora plateau from the rest of the Orjen range. The ridge stretches for 17 kilometres from Vučji zub peak on the west, at the border of Montenegro and Bosnia and Herzegovina, and the villages of Crkvice and Malov Do on the east.

Geographic entities mentioned:
surface_form: reovačka greda
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.57694444
lon: 18.57
The ridge stretches for 17 kilometres from Vučji zub peak on the west, at the border of Montenegro and Bosnia and Herzegovina, and the villages of Crkvice and Malov Do on the east. Its highest peak is Pazua, which is 1,769 metres high. Situated in the heavily karstified Orjen range, Reovačka greda consists mostly of limestone. Southern side of the ridge is used for trad climbing.

Geographic entities mentioned:
surface_form: reovačka greda
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.57694444
lon: 18.57
The river forms the border with neighbouring County Waterford for much of its journey through the barony, with the exception of a &quot;box&quot; around Carrick-on-Suir which straddles both banks. The Comeragh Mountains lie to the south while to the northeast is Slievenamon. The Lingaun River joins the Suir two miles downstream of Carrick-on-Suir. It holds good stocks of trout.

Geographic entities mentioned:
surface_form: Slievenamon
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.43
lon: -7.563
The waters of Wadi al-Hasa feed the Dead Sea; in winter they accumulate in the southern part of the Dead Sea. The area of the wadi's drainage basin is approximately. The wadi collects its waters from the desert wadis and streams whose basins reach the al-Jafr region to the east, and then flow down to the Jordan Rift Valley and into the Dead Sea. Water use.

Geographic entities mentioned:
surface_form: Jordan Rift Valley
instance_of: Valley
countries: Jordan
Lebanon
Israel
Syria
State of Palestine
coordinates: lat: 32.317222222222
lon: 35.57
Distribution. Known only from South Africa in the Cape Fold Mountains which surround the Little Karoo and the southern escarpment.

Geographic entities mentioned:
surface_form: Cape Fold Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Cobbosseecontee Lake. Lake Cobbosseecontee (, also known as Cobbossee Lake, is a lake located in the towns of Litchfield, Manchester, Monmouth, West Gardiner, and Winthrop in the U.S. state of Maine. It is the largest lake in the Winthrop Lakes Region at deep, covering about in surface area, a length of, and a shoreline of.

Geographic entities mentioned:
surface_form: cobbossee lake
instance_of: Lake
countries: United States
coordinates: lat: 44.25
lon: -69.933333333333
Cobbosseecontee Lake. Lake Cobbosseecontee (, also known as Cobbossee Lake, is a lake located in the towns of Litchfield, Manchester, Monmouth, West Gardiner, and Winthrop in the U.S. state of Maine. It is the largest lake in the Winthrop Lakes Region at deep, covering about in surface area, a length of, and a shoreline of.

Geographic entities mentioned:
surface_form: cobbosseecontee lake
instance_of: Lake
countries: United States
coordinates: lat: 44.25
lon: -69.933333333333
The archipelago of islands and exposed ledges are the visible high points of that reef. A state-owned public launch is located on the southwest shore of the lake in East Monmouth. Low hills and ridges surround the lake, and Monks Hill and Allen Hill rise a few miles north of the lake, while a gray line of hills form a barrier near Sabattus.

Geographic entities mentioned:
surface_form: allen
instance_of: Watercourse
countries: United States
coordinates: lat: 40.44452778
lon: -92.04033333
Mughal period. In the 16th century, Babur, a Timurid descendant of Timur and Genghis Khan from Fergana Valley (modern-day Uzbekistan), invaded across the Khyber Pass and founded the Mughal Empire, covering India, along with modern-day Afghanistan, Pakistan and Bangladesh
During the Mughal period, Akbar (1542–1605), Saharanpur became an administrative unit under the Province of Delhi.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Forts 5 and 6 occupy the upper slopes of the mountain and offer panoramic views of Lake Songkhla and the Gulf of Thailand. The two pagodas on the summit of Khao Daeng were built on the base of fort 10 during the 1830s to commemorate the suppression of rebellions in Kedah.

Geographic entities mentioned:
surface_form: Lake Songkhla
instance_of: Lake
countries: Thailand
coordinates: lat: 7.2
lon: 100.46666666667
New England Music Camp. The New England Music Camp (NEMC) is a summer camp for music students ages 11–18, located on in Sidney, Maine, on the eastern shore of Messalonskee Lake in the Belgrade Lakes region. It was founded in 1937 on the site of the defunct Eastern Music Camp. The camp has facilities for some 200 campers as well as faculty and staff.

Geographic entities mentioned:
surface_form: Belgrade Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.63333333333333
lon: -69.78333333333333
Dremelspitze. Dremelspitze is a mountain in the Lechtal Alps of Tyrol, Austria. The elevation at its peak is.

Geographic entities mentioned:
surface_form: dremelspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.233333333333
lon: 10.6
Dremelspitze. Dremelspitze is a mountain in the Lechtal Alps of Tyrol, Austria. The elevation at its peak is.

Geographic entities mentioned:
surface_form: dremelspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.233333333333
lon: 10.6
surface_form: lechtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.331319
lon: 10.5312967
It was established in 2001 and has a total area of. Tofua National Park. The Tofua National Park, covers the island of Tofua and the surrounding marine environment. It was established in 2001 and has a total area of. It incorporates the circular island, which is dominated by a wide caldera, containing a freshwater lake (above sea level) and is surrounded by cliffs.

Geographic entities mentioned:
surface_form: Tofua
instance_of: Mountain
countries: Tonga
coordinates: lat: -19.75
lon: -175.06666666667
The collective name, Sandefjord Peaks, was recommended by the United Kingdom Antarctic Place-Names Committee (UK-APC) following a survey of the peaks by the Falkland Islands Dependencies Survey (FIDS) in 1950. They were first climbed in September 1969 by John Edwards, Martin Pinder, Dave Rinning and Eliot Wright after 11 days man-hauling a sledge across from Signy Island

Geographic entities mentioned:
surface_form: martin
instance_of: Mountain
coordinates: lat: -69.6667
lon: -62.9833
Sandefjord Peaks. Sandefjord Peaks () is a set of three conical peaks, the highest 635 m, marking the southwest end of Pomona Plateau at the west end of Coronation Island, in the South Orkney Islands. The southernmost of these peaks was named Sandefjord Peak after nearby Sandefjord Bay by DI personnel in 1933.

Geographic entities mentioned:
surface_form: sandefjord peaks
instance_of: Mountain
coordinates: lat: -60.6167
lon: -45.9833
The southernmost of these peaks was named Sandefjord Peak after nearby Sandefjord Bay by DI personnel in 1933. The collective name, Sandefjord Peaks, was recommended by the United Kingdom Antarctic Place-Names Committee (UK-APC) following a survey of the peaks by the Falkland Islands Dependencies Survey (FIDS) in 1950.

Geographic entities mentioned:
surface_form: sandefjord peaks
instance_of: Mountain
coordinates: lat: -60.6167
lon: -45.9833
Lord Lansdowne's military secretary, Lord Melgund, later became Lord Minto and served as Governor General between 1898 and 1904. Parc Lansdowne and Lansdowne Avenue in Westmount, Montreal, next to Westmount Park, was named in his honor, as well as Lansdowne Ridge and Upper-Lansdowne, both located on Westmount's summit next to Villa Sainte-Marcelline and Saint Joseph's Oratory.

Geographic entities mentioned:
surface_form: Westmount's summit
instance_of: Mountain
countries: Canada
coordinates: lat: 45.492
lon: -73.6069
He was the brother of Iyasu I, and one of five sons of Yohannes I. Reign. Following the murder of his nephew Tekle Haymanot I, Tewoflos was brought out of captivity at Mount Wehni and made Emperor. At first he faced a rival in the person of the four-year-old son of his nephew who was supported by the Master of Horse Yohannes and Empress Malakotawit.

Geographic entities mentioned:
surface_form: Wehni
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 12.148333333333
lon: 37.766388888889
The river Figgjoelva marks the northern border of Time with the municipality of Sandnes. The large lake Frøylandsvatnet forms part of the border with the neighboring municipality of Klepp. The landlocked municipality also includes part of the &quot;Høg-Jæren&quot; (&quot;high-Jæren&quot;) area which is not flat like the rest of the district.

Geographic entities mentioned:
surface_form: Frøylandsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.749722222222
lon: 5.6758333333333
In December SUM assassinated three agents of the State Research Bureau. In the same month, a rebel boat sank on Lake Victoria; SUM member Patrick Kimumwe drowned during this accident. Over the next few months its operatives, moving across Lake Victoria from Kenya, destroyed a Kampala fuel depot, severed electricity lines, and attacked military outposts.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
It was named Ranchos el Tejon, or The Tejon Ranch. In 1915, Bear Mountain Boulevard (SR 223) was constructed, replacing the dangerous White Wolf Road to the south. An important route, it linked the southern San Joaquin Valley, to Tehachapi and industries in the Mojave Desert. It was also a part of the Midway Route, which was one of two routes connecting Bakersfield with Los Angeles.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The tall mountain is located in the Rondane mountains within Rondane National Park. The mountain sits about northeast of the town of Otta. The mountain is surrounded by several other notable mountains including Vinjeronden and Rondeslottet to the northeast, Storronden and Rondvasshøgde to the east, Simlepiggen to the southeast, Steet and Hoggbeitet to the west, and Veslesmeden to the northwest.

Geographic entities mentioned:
surface_form: Vinjeronden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.905833333333
lon: 9.8477777777778
surface_form: Rondeslottet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.914722222222
lon: 9.8511111111111
surface_form: Storronden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.891666666667
lon: 9.8619444444444
surface_form: Rondvasshøgde
instance_of: Mountain
countries: Norway
coordinates: lat: 61.88715
lon: 9.89629
surface_form: Simlepiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.86416667
lon: 9.845
surface_form: Steet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.89796
lon: 9.73208
surface_form: Hoggbeitet
instance_of: Mountain
countries: Norway
coordinates: lat: 61.8952
lon: 9.71251
surface_form: Veslesmeden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.917777777778
lon: 9.7572222222222
Svartnuten. Svartnuten is a mountain in Sel Municipality in Innlandet county, Norway. The tall mountain is located in the Rondane mountains within Rondane National Park. The mountain sits about northeast of the town of Otta.

Geographic entities mentioned:
surface_form: svartnuten
instance_of: Mountain
countries: Norway
coordinates: lat: 61.90025
lon: 9.82121
The total land area occupied by the state is. Geology. The bulk of Western Australia consists of the extremely old Yilgarn craton and Pilbara craton which merged with the Deccan Plateau of India, Madagascar and the Kaapvaal and Zimbabwe cratons of Southern Africa, in the Archean Eon to form Ur, one of the oldest supercontinents on Earth (3–3.2  billion years ago).

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Because the only mountain-building since then has been of the Stirling Range with the rifting from Antarctica, the land is extremely eroded and ancient, with no part of the state above 1,249 metres (4,098 ft) AHD (at Mount Meharry in the Hamersley Range of the Pilbara region).

Geographic entities mentioned:
surface_form: Mount Meharry
instance_of: Mountain
countries: Australia
coordinates: lat: -22.966666666667
lon: 118.58333333333
Kosovo. On 4 November 2016, Aliti decided to represent Kosovo at senior international level and he is the first player that comes from the Preševo Valley. On 7 November 2016, he received a call-up from Kosovo for a 2018 FIFA World Cup qualification match against Turkey.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
Geography. According to the United States Census Bureau, the township had a total area of 25.33 square miles (65.60 km2), including 24.72 square miles (64.03 km2) of land and 0.60 square miles (1.56 km2) of water (2.38%). The township is located in the Kittatinny Valley which is a section of the Great Appalachian Valley that stretches from Canada to Alabama.

Geographic entities mentioned:
surface_form: Great Appalachian Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.5
lon: -77.83333333333333
The township borders the Warren County municipalities of Blairstown Township, Hardwick Township, Hope Township and White Township. Demographics. The Township's economic data (as is all of Warren County) is calculated by the US Census Bureau as part of the Allentown-Bethlehem-Easton, PA-NJ Metropolitan Statistical Area. 2010 census.

Geographic entities mentioned:
surface_form: Allentown-Bethlehem-Easton, PA-NJ Metropolitan Statistical Area
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
The ant is rarely sighted in the northern regions of Western Australia. In South Australia, it is commonly found in the south-east regions of the state, frequently encountered in Mount Lofty (particularly the Adelaide Hills), Normanville, Hallett Cove and Aldgate, but it is not found in north-western regions. There are dense populations on the western seaboard of Kangaroo Island.

Geographic entities mentioned:
surface_form: Mount Lofty
instance_of: Mountain
countries: Australia
coordinates: lat: -34.966666666667
lon: 138.7
The ants are widespread in the Australian Capital Territory. In Queensland, the ants are only found along the south-eastern coastlines of the state, where populations are frequently encountered in the Bunya Mountains, Fletcher, Stanthorpe, Sunshine Coast, Tamborine Mountain and Millmerran, and have been found as far north as Atherton Tablelands.

Geographic entities mentioned:
surface_form: Tamborine Mountain
instance_of: Mountain
countries: Australia
coordinates: lat: -27.927513888889
lon: 153.19430555556
The Aberdare Times. &quot;The Aberdare Times&quot; was a weekly English-language newspaper based in south Wales. Its circulation was mainly in Merthyr Tydfil, Hirwaun, Mountain Ash, Pontypridd, Neath Valley, Rhondda and Cardiff. The paper had Labour/Liberal tendencies and its main content was local news. At its inception, Josiah Thomas Jones (1799–1873) was the owner, publisher and editor.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
King Jun of Gojoseon is reported to have fled to Jin after Wiman seized his throne and established Wiman Joseon. Some believe that Chinese mentions of Gaeguk or Gaemaguk (蓋馬國, literally means Kingdom of armored horses, located near Kaema Plateau) refers to Jin. Goguryeo is said to have conquered &quot;Gaemaguk&quot; in 26 AD, but this may refer to a different tribe in northern Korea.

Geographic entities mentioned:
surface_form: Kaema Plateau
instance_of: Plateau
countries: North Korea
coordinates: lat: 41
lon: 128
The district was created in 1925 after a new city charter was passed, which replaced the former &quot;at large&quot; voting system for a nine-member council with a district system with a 15-member council. Between 1923 and 1987, District 1 represented all, then parts, of the San Fernando Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Between 1923 and 1987, District 1 represented all, then parts, of the San Fernando Valley. Beginning its existence in the Hollywood area, it now covers much of the far eastern and southeastern portions of the San Fernando Valley and parts of the Crescenta Valley. Geography. The 2nd district stretches from the hills of Studio City to the edge of Verdugo Mountains Park in Sun Valley.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: Crescenta Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.225
lon: -118.237
In 1986, with the death of Howard Finn in the 1st district, the district was moved to near Downtown to provide for election of a Hispanic, with the 2nd and 7th districts taking over the old area. Since then, the district has been situated in San Fernando Valley, extending from Studio City on the south, through Van Nuys to Sunland-Tujunga.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Narira Creek. Narira Creek is a tributary of Wallaga Lake in southern New South Wales, Australia. The village of Cobargo is situated on its banks, and much of the land surrounding the creek is dairy farms.

Geographic entities mentioned:
surface_form: Wallaga Lake
instance_of: Lake
countries: Australia
coordinates: lat: -36.365277777778
lon: 150.05111111111
Claude Ewing Rusk. Claude Ewing Rusk (November 20, 1871 – February 3, 1931), also known as C. E. Rusk, was an American mountaineer, lawyer, and author from Washington who pioneered routes up Mount Adams, Mount Baker, and Glacier Peak. He also ascended many other peaks in Washington, Oregon, and California. Early life. Rusk was born on November 20, 1871, in Knox County, Illinois to James A.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Also in 1902, Rusk became one of the founding members of the American Alpine Club. Rusk and his wife moved to Hamilton, Washington in 1903, but only stayed there for about a year before they moved to Lake Chelan and bought a home along a remote portion of the lake. Rusk became a member of the Mazamas club in 1904. Rusk practiced law in the town of Chelan until 1910.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
In 1895, he joined the party from the Mazamas mountaineering club for the first heliograph signaling between the peaks of the Cascades which included, from north to south, Mount Baker, Mount Rainier, Mount Adams, Mount Hood, Mount Jefferson, and Diamond Peak.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
As they came around the mountain, Rusk suggested names for several of the glaciers. He wanted to name Adams Glacier as Reid Glacier in honor of Reid; however, Reid insisted that it should be named something else because he thought it improper to place his own name on the map that he was making and the Mazamas were trying to name a glacier on Mount Hood after him.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
They made use of a human toboggan to get her down the mountain. Two days later, Rusk joined the Mazamas party in their ascent. Mount Baker climb. In 1903, after the Rusks had moved to Hamilton, Rusk and his wife attempted to climb Mount Baker. They were unsuccessful because poor weather turned them away. Later that same year, Rusk made another attempt with George G. Cantwell and W. A. Alexander.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Gathering of the Mountain Clans. Rusk participated in a &quot;gathering of the mountain clans&quot; on Mount Rainier in 1905. Always a leader in the mountains, he went with a scouting party from Paradise Park around to the west side of Rainier, possibly up Kautz Cleaver, in an attempt to find a route that avoided the notorious rockfall on the normal Gibraltar route.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Because there were so many attempting the climb, the clubs divided into two parties and climbed on succeeding days. Ninety-eight people completed the ascent including Rusk who volunteered as a leader of one of the groups. Glacier Peak climb. Rusk climbed Glacier Peak in August 1906 with A. L. Cool. They were the third party to climb Glacier Peak and the first to climb the east side.

Geographic entities mentioned:
surface_form: Glacier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
Eventually, there were three others who accompanied Rusk on the expedition, A. L. Cool, Joseph Ridley, and Frank H. Rojec. Cool was a good friend of Rusk's from the area around Lake Chelan who was well known as an expert mountaineer and guide. Ridley was a forest ranger on the Mount Baker National Forest who had done much exploring and mapping in the area around Mount Baker.

Geographic entities mentioned:
surface_form: Lake Chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
Cool was a good friend of Rusk's from the area around Lake Chelan who was well known as an expert mountaineer and guide. Ridley was a forest ranger on the Mount Baker National Forest who had done much exploring and mapping in the area around Mount Baker. Rojec, the photographer for the expedition, worked for the Kiser Photography Company and was well known for his pictures of Western scenery.

Geographic entities mentioned:
surface_form: Mount Baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Mount Stuart climbs. Rusk first climbed Mount Stuart in 1920. When he first saw it in 1894, Rusk desired to climb it; however, other matters, including the McKinley expedition, prevented him from climbing it. That same year, 1920, the Cascadians mountaineering club was formed and with Rusk as a leading member, they decided that a record box should be taken to the summit.

Geographic entities mentioned:
surface_form: Mount Stuart
instance_of: Mountain
countries: United States
coordinates: lat: 47.4753
lon: -120.901
All but Whitnall made the summit. Rusk led another much larger party up Stuart on May 29, 1922. Conquest of the Great East Side. In 1921, in addition to climbing Mount Stuart, Rusk and a group from the Cascadians went on an expedition to Mount Adams. This expedition had as its primary goal to climb the &quot;Great East Side&quot; of Adams. They made their base camp in Avalanche Valley.

Geographic entities mentioned:
surface_form: Mount Stuart
instance_of: Mountain
countries: United States
coordinates: lat: 47.4753
lon: -120.901
Mount Hood climb. Mount Hood was one of the first mountains Rusk saw when he and his family came from Illinois; however, he did not get to climb it until much later, in 1922. This climb he made solo up the Cooper Spur route. Once he got to the top, he spent a long time with the fire lookout, Charles A. Phelps, who regaled him of many his adventures as the lookout.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
On the way back down, Rusk had one of his few climbing accidents, losing his footing and sliding quickly down the slope for a short distance. Mount Shasta climbs. The last major Cascade Mountain to be conquered by Rusk that he wrote about was Mount Shasta. He and four members from the Cascadians made an attempt to climb the peak in 1922.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Rusk closed his &quot;Tales&quot; by stating &quot;[m]y third of a century of mountaineering was more than rounded out, and, if this should be my last journey to the ice-bound heights, I could not complain.&quot;
Final expeditions. While Shasta was the last mountaineering adventure that Rusk wrote about, he would continue to climb peaks around his Grants Pass home including Mount Thielsen.

Geographic entities mentioned:
surface_form: Mount Thielsen
instance_of: Mountain
countries: United States
coordinates: lat: 43.152837292
lon: -122.066514283
La Frontera Formation. The La Frontera Formation (, K2F, Ksf) is a geological formation, part of the Villeta Group, of the Altiplano Cundiboyacense and neighbouring areas of the Eastern Ranges of the Colombian Andes. The sequence of limestones and lydites dates to the Late Cretaceous period; Turonian epoch and has a maximum thickness of.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
They also patrol the mouth of the Cape Fear River in Southport, North Carolina and the Intracoastal Waterway (ICW)
History. In the early 1800s, in recognition of the dangers to navigation caused by Frying Pan Shoals, Jay Bird Shoals, and Bald Head Shoals which lay south and southeast of Cape Fear, construction of a series of lighthouses and life saving stations in the area began.

Geographic entities mentioned:
surface_form: Frying Pan Shoals
instance_of: Landform
countries: United States
coordinates: lat: 33.80111111
lon: -77.94694444
Transport. Wrose is served by a number of West Yorkshire Transport's bus services. Notable residents. Wrose was home to the Yorkshire sporting family the Jowets, of which the last and most notable member was Dawson Jowet, founder of the Airedale beagles hunting pack in 1891, and its Master until his death in 1933. His monument remains on Ilkley Moor.

Geographic entities mentioned:
surface_form: Airedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.017
lon: -1.465
Cornett were killed along with pilot Cliff Hogue when their small plane crashed in stormy weather southwest of Dog Lake in Lake County, Oregon. The group left Klamath Falls about 10:00 p.m. en route to a ranch owned by Oscar Kittredge in Warner Valley near Lakeview, Oregon. A state funeral was held for Snell, Farrell and Cornett at the Capitol in Salem.

Geographic entities mentioned:
surface_form: Warner Valley
instance_of: Valley
countries: United States
coordinates: lat: 42.0777
lon: -119.925
Third Lake (Herkimer County, New York). Third Lake is located in the Town of Webb in Herkimer County, New York, by the hamlet of Old Forge. Third Lake is part of the Fulton Chain of Lakes.

Geographic entities mentioned:
surface_form: Fulton Chain of Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.75
lon: -74.866666666667
surface_form: third lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7295112
lon: -74.9001732
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
Third Lake (Herkimer County, New York). Third Lake is located in the Town of Webb in Herkimer County, New York, by the hamlet of Old Forge. Third Lake is part of the Fulton Chain of Lakes.

Geographic entities mentioned:
surface_form: third lake (herkimer county, new york)
instance_of: Lake
countries: United States
coordinates: lat: 43.7295112
lon: -74.9001732
Third Lake (Herkimer County, New York). Third Lake is located in the Town of Webb in Herkimer County, New York, by the hamlet of Old Forge. Third Lake is part of the Fulton Chain of Lakes.

Geographic entities mentioned:
surface_form: third lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7295112
lon: -74.9001732
Camp Cody (summer camp). Camp Cody in Freedom, New Hampshire, is a traditional, overnight, international, and co-ed summer camp, located along the shore of Ossipee Lake. Established in 1926 by Philip Axman in Cambridge, Maryland, Camp Cody began as a camp for boys, named after William &quot;Buffalo Bill&quot; Cody.

Geographic entities mentioned:
surface_form: Ossipee Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.791388888889
lon: -71.139722222222