Sarmila/GeoWiki-Features huggingface dataset:
Upon seeing smoke rising from the village square, and seeing only a few companies directly below them, Colonel Barrett decided to march back toward the town from their vantage point on Punkatasset Hill to a lower, closer flat hilltop about 300 yards (274 m) from the North Bridge.

Geographic entities mentioned:
surface_form: Punkatasset Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.4815
lon: -71.3467
Pangil River. The Pangil River (), also known as the Bambang Hari River, is a river system that runs through Pangil, Laguna, in the Philippines. It is one of 21 River tributaries of Laguna de Bay and is regularly monitored by the Laguna Lake Development Authority(LLDA) through one of its 15 river monitoring stations. The Pangil River sub-basin has a drainage area of.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
This area was above sea level a hundred million years ago, and was covered by temperate forests of trees related to the yellowwoods. Fossil tree trunks from some of these trees were seen from the submersible &quot;JAGO&quot; during explorations off Kleinsee in 1997. In 2014 the area was recognised as an ecologically and biologically significant area of global importance. Purpose.

Geographic entities mentioned:
surface_form: Kleinsee
instance_of: Lake
countries: Austria
coordinates: lat: 46.606111111111
lon: 14.565277777778
Barmer Spitze. The Barmer Spitze is a peak of the Rieserferner group on the border between Tyrol, Austria, and South Tyrol, Italy.

Geographic entities mentioned:
surface_form: barmer spitze
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.91586111111111
lon: 12.152119444444445
Swordale, Ross-shire. Swordale is a very small village which lies below the hill of the same name and above the River Sgitheach, in the parish of Kiltearn in eastern Ross-shire, Scottish Highlands. Swordale is connected by road to the village of Evanton, east, beyond which is the Cromarty Firth. To the west lies Ben Wyvis. The ornithologist Anne Constance Jackson was born at Swordale in 1889.

Geographic entities mentioned:
surface_form: Ben Wyvis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.679119444444
lon: -4.5792194444444
Castle Craig. Castle Craig, located on East Peak in the Hanging Hills, is constructed of trap rock and is in height and has a base in circumference. A metal interior stairway is used to ascend the observation deck on top. It stands above sea level and provides an expansive view of the greater Meriden, Connecticut area. Origin and details.

Geographic entities mentioned:
surface_form: Hanging Hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
It is named for the Linville River, which goes over the falls. Linville Falls has the highest volume of any waterfall on the Northern Edge of the Blue Ridge Mountains. Natural history. Linville Falls marks the beginning of the Linville Gorge, which is formed by the Linville River, which continues on after the falls before finally ending near Lake James.

Geographic entities mentioned:
surface_form: Lake James
instance_of: Lake
countries: United States
coordinates: lat: 35.7478
lon: -81.8785
Significant parts of the Jewish Quarter, much of it severely damaged in the war, together with synagogues such as the Hurva Synagogue, which had also been used as a military base in the conflict, were destroyed. It was said that some gravestones from the Jewish cemetery on the Mount of Olives had been used for construction, paving roads and to build latrines for a nearby Jordanian army barracks.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Monte Madonnino. Monte Madonnino is a mountain of Lombardy, Italy. It is located within the Bergamo Alps.

Geographic entities mentioned:
surface_form: monte madonnino
instance_of: Mountain
countries: Italy
coordinates: lat: 46.01166667
lon: 9.88611111
History. German missionaries originally settled in the Nundah area (known as German Station) in 1838. These missionaries were granted alongside the creek they named Kedron Brook, after Kidron Valley near Jerusalem. The suburb takes its name from the creek. The first land sales commenced in 1857. Alexander and Amelia Barron settled in the area in 1856.

Geographic entities mentioned:
surface_form: Kidron Valley
instance_of: Valley
countries: State of Palestine
coordinates: lat: 31.776972222222224
lon: 35.23897222222222
Uranium in an area could also be determined by looking at the chemical make up of certain plants to try to detect certain elements. This helped find new locations of uranium, specifically focusing on the Colorado Plateau. This was done using an indicator plant known as Astragalus pattersoni, which requires trace amounts of selenium to grow.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Examples of porphyry molybdenum deposits are the Climax, Urad, Mt. Emmons, and Henderson deposits in central Colorado; the White Pine and Pine Grove deposits in Utah; the Questa deposit in northern New Mexico; and Endako in British Columbia. The US Geological Survey has classed the Chorolque and Catavi tin deposits in Bolivia as &quot;porphyry tin deposits&quot;.

Geographic entities mentioned:
surface_form: Chorolque
instance_of: Mountain
countries: Bolivia
coordinates: lat: -20.91794
lon: -66.03619
Kaikōura Peninsula. The Kaikōura Peninsula is located in the northeast of New Zealand's South Island. It protrudes into the Pacific Ocean. The town of Kaikōura is located on the north shore of the peninsula. The peninsula has been settled by Māori for approximately 1000 years, and by Europeans since the 1800s, when whaling operations began off the Kaikōura coast.

Geographic entities mentioned:
surface_form: kaikōura peninsula
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.42333056
lon: 173.696125
Since the end of whaling in 1922 whales have been allowed to thrive and the region is now a popular whale watching destination. The Kaikōura Peninsula is made up of limestone and mudstone which have been deposited, uplifted and deformed throughout the Quaternary. The peninsula is situated in a tectonically active region bounded by the Marlborough Fault System. History.

Geographic entities mentioned:
surface_form: kaikōura peninsula
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.42333056
lon: 173.696125
History. Māori oral history and tradition describes the demi-god ancestor Māui standing on Kaikōura Peninsula where he &quot;fished up&quot; or discovered the North Island. An old name for the South Island is &quot;Te Waka a Māui&quot; (the canoe of Māui), and the name of the North Island is &quot;Te Ika a Māui&quot; (the fish of Māui).

Geographic entities mentioned:
surface_form: kaikōura peninsula
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.42333056
lon: 173.696125
Important Bird Area. The Kaikōura Peninsula is included within the Kaikōura Important Bird Area designated by BirdLife International in the Kaikōura region. The Important Bird Area (IBA) covers and includes parts of the Kaikōura coastline and all of the Kaikōura Peninsula. Hutton's shearwater colony. The endangered bird species Hutton's shearwater is endemic to the Kaikōura region.

Geographic entities mentioned:
surface_form: kaikōura peninsula
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.42333056
lon: 173.696125
Hutton's shearwater colony. The endangered bird species Hutton's shearwater is endemic to the Kaikōura region. As a conservation measure for the species, a new breeding colony (Te Rae o Atiu) was established on the Kaikōura Peninsula in 2005. First, a small transfer of 10 nestlings was sent in April 2005.

Geographic entities mentioned:
surface_form: kaikōura peninsula
instance_of: Mountain
countries: New Zealand
coordinates: lat: -42.42333056
lon: 173.696125
Lake Turkana occupies the northern end of the Great Rift Valley in Kenya. There are also volcanoes in Lake Turkana. The Suguta Valley, or Suguta Mud Flats, is an arid part of the Great Rift Valley directly south of Lake Turkana. The shield volcano Emuruangogolak straddles the valley to the south of Suguta, and further south Mount Silali and Paka rise from the valley floor.

Geographic entities mentioned:
surface_form: Suguta Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 2.0910583333333
lon: 36.513747222222
There are also volcanoes in Lake Turkana. The Suguta Valley, or Suguta Mud Flats, is an arid part of the Great Rift Valley directly south of Lake Turkana. The shield volcano Emuruangogolak straddles the valley to the south of Suguta, and further south Mount Silali and Paka rise from the valley floor. Paka is a shield volcano, with widespread geothermal activity.

Geographic entities mentioned:
surface_form: Mount Silali
instance_of: Mountain
countries: Kenya
coordinates: lat: 1.169362
lon: 36.17506
The shield volcano Emuruangogolak straddles the valley to the south of Suguta, and further south Mount Silali and Paka rise from the valley floor. Paka is a shield volcano, with widespread geothermal activity. South of Paka are Mount Korosi, Lake Baringo and Lake Bogoria. Menengai is a massive shield volcano in the floor of the rift with a caldera that formed about 8,000 years ago.

Geographic entities mentioned:
surface_form: Lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: Lake Bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
Paka is a shield volcano, with widespread geothermal activity. South of Paka are Mount Korosi, Lake Baringo and Lake Bogoria. Menengai is a massive shield volcano in the floor of the rift with a caldera that formed about 8,000 years ago. It overlooks Lake Nakuru to the south. This region also includes Lake Elementaita, Mount Kipipiri and Lake Naivasha.

Geographic entities mentioned:
surface_form: Menengai
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.2
lon: 36.066666666667
Menengai is a massive shield volcano in the floor of the rift with a caldera that formed about 8,000 years ago. It overlooks Lake Nakuru to the south. This region also includes Lake Elementaita, Mount Kipipiri and Lake Naivasha. The Hell's Gate National Park lies south of Lake Naivasha. In the early 1900s, Mount Longonot erupted, and ash can still be felt around Hell's Gate.

Geographic entities mentioned:
surface_form: Mount Kipipiri
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.437432
lon: 36.542673
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
It overlooks Lake Nakuru to the south. This region also includes Lake Elementaita, Mount Kipipiri and Lake Naivasha. The Hell's Gate National Park lies south of Lake Naivasha. In the early 1900s, Mount Longonot erupted, and ash can still be felt around Hell's Gate. Mount Longonot is a dormant stratovolcano located southeast of Lake Naivasha.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
This region also includes Lake Elementaita, Mount Kipipiri and Lake Naivasha. The Hell's Gate National Park lies south of Lake Naivasha. In the early 1900s, Mount Longonot erupted, and ash can still be felt around Hell's Gate. Mount Longonot is a dormant stratovolcano located southeast of Lake Naivasha. Mount Suswa is a shield volcano located between Narok and Nairobi.

Geographic entities mentioned:
surface_form: Mount Longonot
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.91527777777778
lon: 36.456944444444
This region also includes Lake Elementaita, Mount Kipipiri and Lake Naivasha. The Hell's Gate National Park lies south of Lake Naivasha. In the early 1900s, Mount Longonot erupted, and ash can still be felt around Hell's Gate. Mount Longonot is a dormant stratovolcano located southeast of Lake Naivasha. Mount Suswa is a shield volcano located between Narok and Nairobi.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
Mount Suswa is a shield volcano located between Narok and Nairobi. Lava flows from the most recent eruptions are still not covered by vegetation, and may be no more than one hundred years old. Lake Magadi is the most southern rift valley lake in Kenya, although the northern end of Lake Natron in Tanzania reaches into Kenya. The Elgeyo escarpment forms part of the western wall.

Geographic entities mentioned:
surface_form: Lake Magadi
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
The Elgeyo escarpment forms part of the western wall. The Kerio Valley lies between the Tugen Hills and the Elgeyo escarpment at an elevation of
There are large deposits of Fluorite in the Kerio Valley area. Further south the Mau Escarpment is a steep natural cliff approximately 1,000 m (3,300 ft) high, running along the western edge of the Great Rift Valley about Lake Naivasha.

Geographic entities mentioned:
surface_form: Kerio Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 0.6401
lon: 35.6086
surface_form: Kerio Valley
instance_of: Valley
countries: Kenya
coordinates: lat: 0.6401
lon: 35.6086
The Elgeyo escarpment forms part of the western wall. The Kerio Valley lies between the Tugen Hills and the Elgeyo escarpment at an elevation of
There are large deposits of Fluorite in the Kerio Valley area. Further south the Mau Escarpment is a steep natural cliff approximately 1,000 m (3,300 ft) high, running along the western edge of the Great Rift Valley about Lake Naivasha.

Geographic entities mentioned:
surface_form: Mau Escarpment
instance_of: Mountain
countries: Kenya
coordinates: lat: 0.61
lon: 35.74
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
Further south the Mau Escarpment is a steep natural cliff approximately 1,000 m (3,300 ft) high, running along the western edge of the Great Rift Valley about Lake Naivasha. Yet further south the Nguruman Escarpment is around 50 kilometers long and elongated in N-W direction.

Geographic entities mentioned:
surface_form: Nguruman Escarpment
instance_of: Mountain
countries: Kenya
coordinates: lat: -1.761655
lon: 36.025543
The Aberdare Range forms a section of the eastern rim of the Great Rift Valley to the north of Nairobi. Mount Satima lies at the northern end of the Aberdares and is their highest point, and Mount Kinangop at the southern end is the second highest. The mountains form a ridge between these two peaks.

Geographic entities mentioned:
surface_form: Mount Satima
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.34972222
lon: 36.61666667
surface_form: Mount Kinangop
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.62765
lon: 36.70832
Lakes. Kenya is home to 64 (9.50%) of the total lakes found within the continent of Africa. Eight of these make up the main lakes in the Kenyan Rift Valley. From north to south, the names of these lakes are Lake Turkana, Lake Logipi, Lake Baringo, Lake Bogoria, Lake Nakuru, Lake Elmenteita, Lake Naivasha, and Lake Magadi. Of those eight, only Lakes Baringo and Naivasha are fresh water.

Geographic entities mentioned:
surface_form: Lake Logipi
instance_of: Lake
countries: Kenya
coordinates: lat: 2.2333333333333
lon: 36.566666666667
surface_form: Lake Baringo
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 36.083333333333
surface_form: Lake Bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
surface_form: Lake Elmenteita
instance_of: Lake
countries: Kenya
coordinates: lat: -0.446
lon: 36.244
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
surface_form: Lake Magadi
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
Their nest mounds can also be preserved and cemented as the lake's water levels change. These form irregularities in the lakeside topography. Trona, an evaporative mineral, used for sodium carbonate production, has been mined at Lake Magadi for nearly 100 years. It produces about 250,000 metric tonnes per year.

Geographic entities mentioned:
surface_form: Lake Magadi
instance_of: Lake
countries: Kenya
coordinates: lat: -1.8666666666667
lon: 36.266666666667
In 2004, over 2 kilograms of Corundum were collected. Three shallow alkaline lakes and the surrounding lands make up the Kenya lake system: Lake Bogoria at, Lake Nakuru at and Lake Elmenteita at. This system has one of the most diverse populations of birds in the world, and is the home of thirteen globally threatened species of bird.

Geographic entities mentioned:
surface_form: Lake Bogoria
instance_of: Lake
countries: Kenya
coordinates: lat: 0.25
lon: 36.1
surface_form: Lake Elmenteita
instance_of: Lake
countries: Kenya
coordinates: lat: -0.446
lon: 36.244
The lands around the lakes include large populations of black rhino, Rothschild's giraffe, greater kudu, lion, cheetah and wild dogs. The Kenya lake system is surrounded by the steep escarpment of the Rift Valley, which provides a spectacular backdrop. Other lakes are Lake Chew Bahir, in the northeast extension. This lake lies mainly in Ethiopia but extends into Kenya in the rainy season.

Geographic entities mentioned:
surface_form: Lake Chew Bahir
instance_of: Lake
countries: Ethiopia
Kenya
coordinates: lat: 4.6866666666667
lon: 36.851666666667
The Kenya lake system is surrounded by the steep escarpment of the Rift Valley, which provides a spectacular backdrop. Other lakes are Lake Chew Bahir, in the northeast extension. This lake lies mainly in Ethiopia but extends into Kenya in the rainy season. Lake Kamnarok is another small lake.

Geographic entities mentioned:
surface_form: Lake Kamnarok
instance_of: Lake
countries: Kenya
coordinates: lat: 0.63333333333333
lon: 35.616666666667
The nunatak also has gamet amphibolite and hornblende schists. Baines Nunatak. Nunatak rising to to the east of Bernhardi Heights and northwest of Jackson Tooth, Pioneers Escarpment, in the Shackleton Range. Photographed from the air by the U.S. Navy, 1967. Surveyed by BAS, 1968-71. Named in 1977 by the UK-APC after Thomas Baines (1822–75), English explorer and joint author, with W.B.

Geographic entities mentioned:
surface_form: Bernhardi Heights
instance_of: Mountain
coordinates: lat: -80.3333
lon: -25
Vestjøkulen. roe5lxutwhwf9jqz8o4br44fcg93" xml:space="preserve">Vestjøkulen is a glacier in Sørkapp Land at Spitsbergen, Svalbard. It is a tributary glacier to Samarinbreen, and is located west of the mountain ridge Bredichinryggen (with Austjøkulen at the opposite/eastern side of the ridge).

Geographic entities mentioned:
surface_form: Bredichinryggen
instance_of: Mountain
countries: Norway
coordinates: lat: 76.9228
lon: 16.4769
Most of the population on the archipelago occurs on Angaur and Peleliu, while the species is probably already gone from Koror. In the Lake Ngardok wetlands of Babeldaob, a few dozen still occur, but the total number of common moorhens on Palau is about in the same region as the Guam population: fewer than 100 adult birds (usually fewer than 50) have been encountered in any survey.

Geographic entities mentioned:
surface_form: Lake Ngardok
instance_of: Lake
countries: Palau
coordinates: lat: 7.5125
lon: 134.60361111111
It is one of the four main rivers of Lake Eyre Basin and is thought to be the oldest riverbed in the world. It flows for only a few days a year. When this happens, its water usually disappears into the sands of the Simpson Desert, rarely if ever reaching Lake Eyre. Geography. The source of the Finke River is in the Northern Territory's MacDonnell Ranges, which flows through central Australia.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Geography. The source of the Finke River is in the Northern Territory's MacDonnell Ranges, which flows through central Australia. The name is first applied at the confluence of the Davenport and Ormiston Creeks, just north of Mount Zeil. From here, the river meanders for about to the western edge of the Simpson Desert in northern South Australia.

Geographic entities mentioned:
surface_form: Mount Zeil
instance_of: Mountain
countries: Australia
coordinates: lat: -23.401666666666667
lon: 132.39583333333334
South Aral Sea. The South Aral Sea is a lake in the basin of the former Aral Sea that formed in 1987 when that body divided in two, due to diversion of river inflow for agriculture.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
surface_form: south aral sea
instance_of: Lake
countries: Kazakhstan
Soviet Union
Uzbekistan
coordinates: lat: 45
lon: 58.5
In 2003, the South Aral Sea itself split into eastern and western basins, the &quot;Eastern Sea&quot; and the &quot;West Aral Sea&quot;, connected by a narrow channel (channel bed at an elevation of) that balanced surface levels but did not allow mixing, and in 2005 the North Aral Sea was dammed to prevent the collapse of its fisheries, cutting off the only remaining inflow to the southern lakes.

Geographic entities mentioned:
surface_form: North Aral Sea
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.5
lon: 60.7
surface_form: south aral sea
instance_of: Lake
countries: Kazakhstan
Soviet Union
Uzbekistan
coordinates: lat: 45
lon: 58.5
In 2008, the Eastern Sea split again, and in May 2009 had almost completely dried out, leaving only the small permanent Barsakelmes Lake between the Northern and Western Seas and increasing the expanse of the Aralkum desert. In 2010, it was partially filled again by meltwater, and by 2014 was once again dry. The West Aral Sea has some replenishment from groundwater in the northwest. Background.

Geographic entities mentioned:
surface_form: Barsakelmes Lake
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 46.2
lon: 59.6
Background. The Aral Sea began shrinking in the 1960s, when the Soviet Union decided that the two rivers feeding it, the Amu Darya and the Syr Darya, would be diverted in order to irrigate cotton and food crops in Kazakhstan and Uzbekistan. In 1987, due to an accelerated loss of water, the Aral Sea was split into northern and southern parts; the northern part is the current North Aral Sea.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
The Aral Sea began shrinking in the 1960s, when the Soviet Union decided that the two rivers feeding it, the Amu Darya and the Syr Darya, would be diverted in order to irrigate cotton and food crops in Kazakhstan and Uzbekistan. In 1987, due to an accelerated loss of water, the Aral Sea was split into northern and southern parts; the northern part is the current North Aral Sea. Salinity.

Geographic entities mentioned:
surface_form: North Aral Sea
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 46.5
lon: 60.7
Current situation. The West Aral Sea is expected to stabilize at, a mean depth of, and a maximum depth of, assuming groundwater discharge at the rate of per year. The Eastern Sea dried up completely in the summer of 2009, apart from the small permanent Barsakelmes Lake (between the Northern and Western seas), but it received some water from snow melt in the spring of 2010.

Geographic entities mentioned:
surface_form: Barsakelmes Lake
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 46.2
lon: 59.6
South Aral Sea. The South Aral Sea is a lake in the basin of the former Aral Sea that formed in 1987 when that body divided in two, due to diversion of river inflow for agriculture.

Geographic entities mentioned:
surface_form: south aral sea
instance_of: Lake
countries: Kazakhstan
Soviet Union
Uzbekistan
coordinates: lat: 45
lon: 58.5
By the time of the Islamic conquests in the 7th century, and possibly earlier, the term 'Kurd' was used with a socio-economic meaning to describe nomadic groups on the western edge of the Iranian plateau and, possibly, tribes aligned with Sassanian authority in Mesopotamia. Early Islamic writings mention the Kurds across a wide geographical area.

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Gunilda. &quot;Gunilda&quot; was a steel-hulled Scottish-built steam yacht in service between her construction in 1897 and her sinking in Lake Superior in 1911. Built in 1897 in Leith, Scotland by Ramage & Ferguson for J. M. or A. R. & J. M. Sladen, and became owned by F. W. Sykes in 1898; her first and second owners were all from England.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
In the summer of 1911, &quot;Gunilda&quot; owner, William L. Harkness, his family and friends were on an extended tour of northern Lake Superior. They were headed to Rossport, Ontario and then planned to head into Lake Nipigon to do some fishing for speckled trout. As she was about away from Rossport, &quot;Gunilda&quot; ran hard aground onto McGarvey Shoal on the north side of Copper Island.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Aurantiacibacter arachoides. &quot;Aurantiacibacter arachoides&quot; is a Gram-negative and rod-shaped bacteria from the genus &quot;Aurantiacibacter&quot; which has been isolated from the ice core of the East Rongbuk Glacier from the Tibetan Plateau.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Gilpin Road, an older alignment of US 40 that is designated MD 144AE, begins to parallel the eastbound side of the state highway at Town Creek Road. The two surface highways cross Town Creek and begin to climb Polish Mountain, with MD 144 following a gentle curve while Gilpin Road follows a winding alignment. MD 144 intersects Gilpin Road as the highway begins the descent from the mountain.

Geographic entities mentioned:
surface_form: Polish Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6961
lon: -78.5247
The inscribed lines are then brushed out and filled with thickly applied colour, and the excess colour is removed. Another feature of Drysdale's later oeuvre are her assemblages of asymmetrical pieces, suites of closed forms that echo geological features of Australia, such as the &quot;Devils Marbles&quot; series, inspired by the Devils Marbles Conservation Reserve in the Northern Territory.

Geographic entities mentioned:
surface_form: Devils Marbles Conservation Reserve
instance_of: Mountain
countries: Australia
coordinates: lat: -20.566666666667
lon: 134.26666666667
Lake Brownworth. 3wvnz1oun65z0l9tq3w8z46es2jy" xml:space="preserve">#redirect Lake Brownworth

Geographic entities mentioned:
surface_form: brownworth
instance_of: Lake
coordinates: lat: -77.433333333333
lon: 162.76666666667
surface_form: lake brownworth
instance_of: Lake
coordinates: lat: -77.433333333333
lon: 162.76666666667
Snag Lake. Snag Lake is a lake located in the northeastern part of Lassen Volcanic National Park in California, United States. Description. Snag Lake, a large body of water, is located to the south of Cinder Cone and the Fantastic Lava Beds at an elevation of. Water from the nearby Horseshoe Lake empties into Snag Lake via Grassy Creek.

Geographic entities mentioned:
surface_form: Cinder Cone and the Fantastic Lava Beds
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
Description. Snag Lake, a large body of water, is located to the south of Cinder Cone and the Fantastic Lava Beds at an elevation of. Water from the nearby Horseshoe Lake empties into Snag Lake via Grassy Creek. Water from Snag Lake continues to flow through the porous lava field that led to the lake's creation eventually making its way into Butte Lake. Access.

Geographic entities mentioned:
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 40.4725
lon: -121.336
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.30912222222222
lon: -122.04138333333333
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.1489
lon: -89.355
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.02805556
lon: -95.68916667
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.3087
lon: -121.569
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.59194444
lon: -93.05361111
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 37.6087742
lon: -119.0194324
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.40822
lon: -122.6643413
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 38.6994
lon: -90.085
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 46.119166666667
lon: -94.830277777778
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 47.4411
lon: -93.4733
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 45.459166666667
lon: -93.05
surface_form: horseshoe lake
instance_of: Lake
countries: United States
coordinates: lat: 44.131666666667
lon: -74.620833333333
Snag Lake, a large body of water, is located to the south of Cinder Cone and the Fantastic Lava Beds at an elevation of. Water from the nearby Horseshoe Lake empties into Snag Lake via Grassy Creek. Water from Snag Lake continues to flow through the porous lava field that led to the lake's creation eventually making its way into Butte Lake. Access. Snag Lake is accessible by hiking trail only.

Geographic entities mentioned:
surface_form: butte lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5621
lon: -121.29
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
Snag Lake. Snag Lake is a lake located in the northeastern part of Lassen Volcanic National Park in California, United States. Description. Snag Lake, a large body of water, is located to the south of Cinder Cone and the Fantastic Lava Beds at an elevation of. Water from the nearby Horseshoe Lake empties into Snag Lake via Grassy Creek.

Geographic entities mentioned:
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
Snag Lake, a large body of water, is located to the south of Cinder Cone and the Fantastic Lava Beds at an elevation of. Water from the nearby Horseshoe Lake empties into Snag Lake via Grassy Creek. Water from Snag Lake continues to flow through the porous lava field that led to the lake's creation eventually making its way into Butte Lake. Access. Snag Lake is accessible by hiking trail only.

Geographic entities mentioned:
surface_form: snag lake
instance_of: Lake
countries: United States
coordinates: lat: 40.513888888889
lon: -121.31166666667
After that, with a large gathering from Tafilalt around 600 kilometers north of Timbuktu. Venel subdued the Tuareg nomads, abolished the slave trade, and oversaw the economic growth of sedentary populations, allowing for the extraction of salt from the Taoudenni and Kaouar mines. Paul left Niamey on 15 February 1910 to return to France.

Geographic entities mentioned:
surface_form: Kaouar
instance_of: Valley
countries: Niger
coordinates: lat: 18.9
lon: 12.9
The river drains of western Georgia, flowing south from the upper Piedmont region south of Atlanta to the wetlands of the Gulf Coastal Plain in the southwestern corner of the state. Along with the Apalachicola and the Chattahoochee rivers, it forms part of the ACF basin. In its upper course through the red hills of the Piedmont, it is considered especially scenic, flowing unimpeded for over.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
One notable exception is the variety known as Malvasia di Candia which is a distinctly different sub-variety of Malvasia. Malvasia bianca is grown widely throughout the world in places like Italy; Sitges in Catalonia, with the renowned variety Malvasia de Sitges; the San Joaquin Valley of California; or the Greek Islands of Paros and Syros.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Unlike southern states extending into the Appalachian Mountains or Ozarks, or Texas with its German settlements in the Edwards Plateau, Florida completely lacked upland or German refugee whites opposed to secession.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Baegunsan (North Chungcheong and Gangwon). Baegunsan () is a mountain between the provinces of Gangwon Province and North Chungcheong Province in South Korea. Its area extends into the cities of Wonju and Jecheon. It has an elevation of.

Geographic entities mentioned:
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.07472222
lon: 127.44416667
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.838530555556
lon: 127.66387777778
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan (north chungcheong and gangwon)
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.106388888889
lon: 127.62166666667
Baegunsan (North Chungcheong and Gangwon). Baegunsan () is a mountain between the provinces of Gangwon Province and North Chungcheong Province in South Korea. Its area extends into the cities of Wonju and Jecheon. It has an elevation of.

Geographic entities mentioned:
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 38.07472222
lon: 127.44416667
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 37.838530555556
lon: 127.66387777778
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
surface_form: baegunsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.106388888889
lon: 127.62166666667
Conesus Lake is a hamlet and census-designated place (CDP) in Livingston County, New York, United States. Its population was 2,584 as of the 2010 census. The community is located in the towns of Geneseo, Livonia, Groveland, and Conesus and covers Conesus Lake, the westernmost of New York's Finger Lakes, and nearly all of the lake's shoreline communities. Geography. According to the U.S.

Geographic entities mentioned:
surface_form: Conesus Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.779722222222
lon: -77.716666666667
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Fort Ticonderoga. During a steamboat trip to Burlington, Vermont, Pell spotted the ruins of Fort Ticonderoga on Lake Champlain. In 1816, he began leasing the property from Columbia and Union colleges (whom had received the property from the state of New York in 1803), and in 1820, he purchased the entire 546-acre grounds for $6,008.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Mount Wuming. Mount Wuming () is a mountain in Xiulin Township, Hualien County, Taiwan with an elevation of.

Geographic entities mentioned:
surface_form: mount wuming
instance_of: Mountain
countries: Taiwan
coordinates: lat: 24.25861111
lon: 121.38194444
It has about 1,600 inhabitants. Chvalčov lies approximately north-east of Kroměříž, north of Zlín, and east of Prague. History. The first written mention of Chvalčov is from 1369. Sights. The Hostýn Hill, a Catholic pilgrimage site, lies in the municipal territory of Chvalčov. There is also the ruin of Obřany Castle on the eponymous hill.

Geographic entities mentioned:
surface_form: Hostýn
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 49.379722222222
lon: 17.701944444444
However, this endeavor failed and a similar bridge was built further upriver by others. In 1836, Waller sold his farm to his son Nathan P. and returned to the Wyoming Valley, where he purchased some more tracts of land. By the time of his death, he owned a considerable amount of land in the Wyoming Valley, including two or more coal mines.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Its main tributary is the Ulungur River. It is an endorheic lake, though the Irtysh River flows towards the Arctic Ocean less than 4 km away to the northeast. Lake Ulungur is divided into two sections, often viewed as two separate lakes: the Buluntuo Lake (or the Ulungur Lake proper) and the smaller Jili Lake (吉力湖,), connected by a narrow channel.

Geographic entities mentioned:
surface_form: Jili Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 46.9
lon: 87.416666666667
surface_form: ulungur lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
surface_form: ulungur
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
Fishing. Along with Bosten Lake, Ulungur Lake is one of the two most important fishing lakes in Xinjiang. The main fish species in the lake are
the common bream (&quot;Abrmais brama orientalis&quot;), Siberian dace (&quot;Leuciscus baicalensis&quot;), and the European perch (&quot;Perca fluviatilis&quot;).

Geographic entities mentioned:
surface_form: Bosten Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 42
lon: 87
surface_form: ulungur lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
Lake Ulungur is divided into two sections, often viewed as two separate lakes: the Buluntuo Lake (or the Ulungur Lake proper) and the smaller Jili Lake (吉力湖,), connected by a narrow channel. The main affluent of the Ulungur-Jili system is the Ulungur River; presently, its main channel enters the Jili Lake at around.

Geographic entities mentioned:
surface_form: jili lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 46.9
lon: 87.416666666667
surface_form: ulungur
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
surface_form: ulungur
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
Ulungur Lake. Ulungur Lake is located in Fuhai County, Xinjiang, China. With an area of 1,035 square kilometers, the lake is one of China's ten largest freshwater lakes. Its main tributary is the Ulungur River. It is an endorheic lake, though the Irtysh River flows towards the Arctic Ocean less than 4 km away to the northeast.

Geographic entities mentioned:
surface_form: ulungur
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
Between 1960 and 1987, the lake level dropped by 4.2 m, due to the increasing use of the river water for irrigation and other needs. To alleviate this problem, in 1987 a canal was built through the narrow isthmus between Lake Ulungur and the Irtysh River, diverting some of the Irtysh water into the lake. (The canal can be seen on Google Maps, starting at and ending in two outlets, at and).

Geographic entities mentioned:
surface_form: ulungur
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
Origins. Historically, Hintalo was the capital city of Enderta Province. Located on a high plateau beneath the south face of Amba Aradam, which made the town a natural fortress. With the advent of &quot;ras&quot; Wolde Selassie of Enderta to power as Governor of all Tigray, Hintalo became the political center of Tigray.

Geographic entities mentioned:
surface_form: Amba Aradam
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 13.333333333333
lon: 39.516666666667
baetica&quot; is smoked by the shepherds of la Sagra. (The geographical designation &quot;la Sagra&quot; generally refers in Spain to a part of the Submeseta Sur (a part, in turn of the Meseta central), although it is possible (given the distribution of &quot;A. baetica&quot;) that the Sierra de la Sagra (a mountain range further to the South of the Submeseta) may be intended).

Geographic entities mentioned:
surface_form: Meseta central
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
Battelle, Alabama. Battelle is an unincorporated community in DeKalb County, Alabama, United States. Battelle was once a thriving mining community which was spread in a north – south line along the foot of Lookout Mountain five miles north of Valley Head, Alabama.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
The only access traditionally was over the bounding ridges via mountain passes. Further southwest of the region are the glaciated high ridges of Himalaya, one in the west (belonging to the Kamet Group) and one in the east (belonging to the Nanda Devi Group). Between the two lies the valley of the Dhauliganga River. (Map 2)
The Barahoti pasture is a sloping plain that is said to be in area.

Geographic entities mentioned:
surface_form: Kamet
instance_of: Mountain
countries: India
coordinates: lat: 30.92
lon: 79.593333333333
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
Syväjärvi. i82e6k48btcf7vkbemoq0uxepqe2" xml:space="preserve">Syväjärvi () is a name for 108 lakes in Finland with no less surface than one hectare. The total area covered by all the Syväjärvis is 39,32 km2, on the average 0,36 km2.

Geographic entities mentioned:
surface_form: syväjärvi
instance_of: Lake
countries: Finland
surface_form: syväjärvi
instance_of: Lake
countries: Finland
Diadem Peak. Diadem Peak is a peak located in the Sunwapta River Valley of Jasper National Park, Canada. Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900.

Geographic entities mentioned:
surface_form: Mount Woolley
instance_of: Mountain
countries: Canada
coordinates: lat: 52.297222222222224
lon: -117.42527777777778
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900. The mountain was named in 1898 by the first ascent team of J. Norman Collie, Hugh Stutfield and Hermann Woolley.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900. The mountain was named in 1898 by the first ascent team of J. Norman Collie, Hugh Stutfield and Hermann Woolley.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Diadem Peak. Diadem Peak is a peak located in the Sunwapta River Valley of Jasper National Park, Canada. Diadem Peak is essentially the high point of a ridge leading down from the slightly higher Mount Woolley (). This peak was the first 11,000er north of the Columbia Icefield to be climbed and one of the few peaks in the Canadian Rockies to be climbed before 1900.

Geographic entities mentioned:
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
__NOTOC__
Climbing history. In the summer of 1898, J. Norman Collie, Hugh Stutfield and Herman Woolley, had made their way up Woolley Creek and initially had their sights on reaching the top of Mount Woolley by climbing the icefield that separates Mt. Woolley from Diadem Peak.

Geographic entities mentioned:
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
surface_form: mount woolley
instance_of: Mountain
countries: Canada
coordinates: lat: 52.297222222222224
lon: -117.42527777777778
Woolley from Diadem Peak. However, after a brief downpour which forced them to seek shelter among some rocks, they had just begun preparing the rope for ascending the icefield when a large collapse of ice from the summit made them switch their objective to Diadem Peak.

Geographic entities mentioned:
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
Collie recorded an initial elevation of using a mercurial barometer. With the use of crampons, the difficulties of the southeast ridge route are reduced by following a shallow snow gully up much of the way. In 1962, William Buckingham and Bill Hooker, ascended Diadem Peak by what is now known as the South Ridge route.

Geographic entities mentioned:
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Diadem Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: diadem peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.31055555555555
lon: -117.42083333333333
The province is also colloquially called &quot;Muangkhon&quot; () and its people &quot;Khonkhon&quot; (). Geography. The province is on the Gulf of Thailand on the east side of the Malay Peninsula. The terrain is mostly rugged hilly forest. The province is home to south Thailand's highest peak, Khao Luang, at.The total forest area is or 18.4 percent of provincial area. National parks.

Geographic entities mentioned:
surface_form: Khao Luang
instance_of: Mountain
countries: Thailand
coordinates: lat: 8.4936111111111
lon: 99.73