Sarmila/GeoWiki-Features huggingface dataset:
It is also noted that settlers in nearby Flemington had to defend against these wolves during the winter. Prior to the 1960s, when the valley surrounded by Cushetunk Mountain was dammed to form Round Valley Reservoir, the mountain was useful as a timber source. Farming use was limited due to the hard diabase rock in the mountain's soil. Geology.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 61.3833
lon: -150.25
surface_form: round valley
instance_of: Valley
countries: United States
coordinates: lat: 35.15166667
lon: -115.36194444
surface_form: the valley
instance_of: Valley
countries: United States
coordinates: lat: 47.7174
lon: -117.047423
The intrusion occurred when the Newark Basin, an aborted rift zone that formed as Pangaea began to break up, was still volcanically active. Originally, it was thought that Cushetunk Mountain was formed well after the nearby Watchung Mountains, also of volcanic origin.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
Originally, it was thought that Cushetunk Mountain was formed well after the nearby Watchung Mountains, also of volcanic origin. The theory was that the deposition of sediment into the Newark Basin was still occurring after the Watchungs were extruded, which explained how Cushetunk Mountain was able to intrude into strata above the height of the Watchungs.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
However, it is now known that Cushetunk Mountain, as well as other intrusive bodies in the Newark Basin, are at least 10 million years older than the Watchungs, which implies that erosion and/or uplift must have occurred after Cushetunk Mountain was intruded in order to allow the Watchungs to form at the surface.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
Instead, the mountain's shape seems to be the result of an intruding sheet of magma becoming dramatically flexed as it penetrated local strata. Round Mountain, just to the south of Cushetunk Mountain, formed as the intruding sheet that created Cushetunk Mountain reached a syncline.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
Round Mountain, just to the south of Cushetunk Mountain, formed as the intruding sheet that created Cushetunk Mountain reached a syncline. A unique feature of Cushetunk Mountain's geology is that the igneous intrusion forming the mountain partly overlaps Paleozoic limestone west of the Ramapo Fault.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
First, the overlap marks one of the only locations in the Newark Basin where an intrusion successfully crossed the Ramapo fault and effectively spilled over the western edge of the basin. Second, the trap rock comprising the intrusion at this location is fine grained and unlike the dense, coarse diabase common to Cushetunk Mountain.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
Ecology. While most of the mountain ridges in New Jersey run generally north to south, Cushetunk Mountain primarily has an east-west ridge orientation because of the elongated north and south prongs of its horseshoe-like ridge. This produces significantly different microclimates between the north facing and south facing slopes of the mountain.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
On south facing slopes, the air temperature near the ground is consistently higher than on the north facing slopes, which do not receive as much sunlight. In terms of ecology this creates a noticeable impact on Cushetunk Mountain's vegetation. Because the north slope of the mountain is cooler and shaded, moisture is more easily retained.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
Grasses and sedges are the most prevalent ground cover. Wildlife supported by Cushetunk Mountain includes a variety of woodland birds, including a nesting pair of bald eagles. Groundwater seeps, particularly on the northern slopes, provide habitat to amphibians, while outcrops of trap rock offer ideal environments for small reptiles.

Geographic entities mentioned:
surface_form: cushetunk mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5986
lon: -74.8247
state of New Jersey, located in Readington and Clinton Township in Hunterdon County. The Lenape Native Americans called the mountain &quot;Cushetunk&quot; meaning &quot;place of hogs&quot; after the wild hogs found there. In the 1960s, the valley at the heart of the mountain was dammed and filled with water to create Round Valley Reservoir.

Geographic entities mentioned:
surface_form: round valley
instance_of: Valley
countries: United States
coordinates: lat: 35.15166667
lon: -115.36194444
The firm &quot;Kraftwerke Vorderrhein AG&quot; has built a hydropower dam creating a reservoir, called the &quot;Lai da Curnera&quot;, into which both rivers now flow. The origin of the Rein da Maighels is the Maghels Glacier () on the &quot;Piz Ravetsch&quot; near the point where the cantons of Graubünden, Ticino and Uri meet.

Geographic entities mentioned:
surface_form: Piz Ravetsch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.58425
lon: 8.7029444444444
Features. The Heemskirk Range features steep, rugged terrain, characteristic of the West Coast Range. The area surrounding the range is largely undeveloped and remote, making it a destination for experienced bushwalkers and hikers. The range is known for its rich biodiversity and includes several rare plant species, making it an area of interest for conservationists. Mountain bike trails.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
Heemskirk Range. The Heemskirk Range is a mountain range located in the Western region of Tasmania, Australia. The main peak of the range is Mount Agnew, which reaches an elevation of above sea level. The range is named after the &quot;Heemskerk&quot;, one of the ships used by Dutch explorer Abel Tasman during his voyage to Tasmania in 1642.

Geographic entities mentioned:
surface_form: heemskirk range
instance_of: Mountain
coordinates: lat: -41.84166666666667
lon: 145.23333333333332
History. Historically this town and its municipal term were considered part of the Matarraña, but presently it is included in the Bajo Aragón-Caspe comarca. During the Battle of the Ebro some of the most bloody battles in the Spanish Civil War were fought in the Auts area, about 8 km north of Fayón.

Geographic entities mentioned:
surface_form: Auts
instance_of: Mountain
countries: Spain
coordinates: lat: 41.31666667
lon: 0.28333333
Puerto Ingeniero Ibáñez. Puerto Ibáñez is a small town in the Aisén Region in the south of Chile. It is located on a bay off the north shore of General Carrera Lake, south of Coihaique. In the 2002 census it had a population of 757. It is the capital of the commune of Río Ibáñez. History. The town was founded in 1924.

Geographic entities mentioned:
surface_form: General Carrera Lake
instance_of: Lake
countries: Chile
Argentina
coordinates: lat: -46.4375
lon: -71.715
He was educated at Newington College (1918–21), The King's School, Parramatta (1922–23) and the University of Sydney. He became a farmer at Bodalla, Wallaga Lake and Tilba Tilba. He won prizes for dairy fodder conservation at the Royal Agricultural Society show. Career. Bate became director of the Bodalla Co-operative Dairy Company from 1927, later managing the cheese co-operative.

Geographic entities mentioned:
surface_form: Wallaga Lake
instance_of: Lake
countries: Australia
coordinates: lat: -36.365277777778
lon: 150.05111111111
Byers Peak Wilderness. The Byers Peak Wilderness is a U.S. Wilderness Area that is located in the Arapaho National Forest in north central Colorado. The wilderness was established in 1993 and named after its highest point, Byers Peak. Byers Peak was named after William N. Byers, the first mayor of Hot Sulphur Springs and the founder of Colorado's first newspaper, the Rocky Mountain News.

Geographic entities mentioned:
surface_form: Byers Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.864444444444
lon: -105.94722222222
Eyumodjock. Eyumojock is a town and commune in Cameroon, and the sub-divisional headquarters of the Eyumojock sub-division in the Manyu division. The small volcanic Lake Ejagham is near the town.

Geographic entities mentioned:
surface_form: Lake Ejagham
instance_of: Lake
countries: Cameroon
coordinates: lat: 5.75121389
lon: 8.98358889
After leaving the state's highest court he returned to private practice in Eugene, Oregon. Early life. Lawrence Harris was born on September 13, 1873, in Oregon’s Willamette Valley in Albany, Oregon. He received his primary education in the local public schools before attending the University of Oregon in Eugene.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
WNNJ-FM was renamed WIXL and had an automated beautiful music format. The station played mostly easy listening instrumental cover versions of pop tunes along with a couple of soft vocals per hour. There were similarly formatted stations heard in Sussex County from the Lehigh Valley and New York City which were more popular, so WIXL had trouble competing. Country Music.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Punchana. Punchana is the capital of the Punchana District in the Maynas Province of the Loreto Region in northeastern Peru, in the Peruvian Amazon Jungle. It is a neighborhood on the outskirts of the city of Iquitos, located on the Amazon and the Nanay Rivers.

Geographic entities mentioned:
surface_form: Nanay
instance_of: Watercourse
countries: Peru
coordinates: lat: -3.70074
lon: -73.24703
It covers an area of and has an average elevation of. Avadi is one of the largest localities in Chennai, stretching from Poonamalle High Road to MTH Road. Lake. Avadi has a lake called Paruthipattu Lake. Spread over 200 acres and in length, the lake is located behind the Tamil Nadu Housing Board (TNHB) and Thirumullaivoyal. It was once a source of water for farmland irrigation.

Geographic entities mentioned:
surface_form: Paruthipattu Lake
instance_of: Lake
countries: India
coordinates: lat: 13.108
lon: 80.105
It is a common understorey shrub in forested areas where jarrah and marri trees are found in the Jarrah Forest, Swan Coastal Plain and Warren biogeographic regions. Subspecies &quot;aquifolium&quot; occurs from near Mundaring to near Margaret River and inland to Collie and Nannup, and subsp. &quot;laidlawiana&quot; from near Nannup and south to near Lake Muir. Conservation status.

Geographic entities mentioned:
surface_form: Lake Muir
instance_of: Lake
countries: Australia
coordinates: lat: -34.446944444444
lon: 116.74833333333
Romanticism also played a role in the popularization of the Kyffhäuser myth, about the Emperor Frederick Barbarossa sleeping atop the Kyffhäuser mountain and being expected to rise in a given time and save Germany) and the legend of the Lorelei (by Brentano and Heine) among others.

Geographic entities mentioned:
surface_form: Lorelei
instance_of: Mountain
countries: Germany
coordinates: lat: 50.139444444444
lon: 7.7288888888889
Giovanni Battista Landolina. 7uyawr4w895f130ox7s06iimjixsc" xml:space="preserve">Giovanni Battista Landolina, &quot;Marchese di S. Alfano&quot;, was a Sicilian landowner and intellectual (mathematician) instrumental in having the city of Noto removed from its former site on Mount Alveria and rebuilt in a more level location following the earthquake in 1693 centred on the Val di Noto.

Geographic entities mentioned:
surface_form: Mount Alveria
instance_of: Mountain
countries: Italy
coordinates: lat: 36.934444444444
lon: 15.019722222222
Maylandia hajomaylandi. &quot;Maylandia hajomaylandi&quot; is a species of cichlid endemic to Lake Malawi where it is only known from around Chisumulu Island. This species can reach a length of TL. It can also be found in the aquarium trade. The specific name honours the cichlid enthusiast and author about aquaria Hans Joachim Mayland, who died in 2004,

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
History. The district was created in 1994 by merging the two previous districts Riesa and Großenhain. In August 2008, it was incorporated into the district of Meißen. Geography. The district is situated in the plain countryside north of the virtual line connecting Leipzig and Dresden. The main river is the Elbe which runs through the district from south to northwest.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Riesco Island was considered part of this peninsula until 1904. The lake that occupies a significant part of its central portion was discovered in 1945. The peninsula is home to Monte Burney and Gran Campo Nevado. There have so far been two attempts to settle the peninsula, the first at &quot;fin de siècle&quot; and a second during the presidency of Eduardo Frei Montalva (1964–1970).

Geographic entities mentioned:
surface_form: Monte Burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
West Nyala language. West Nyala is a Bantu language of western Kenya, on the shores of Lake Victoria. It is a part of the Luhya branch of Great Lakes Bantu.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
There are several old Jain temples that draw pilgrims from Jains around the world in places such as Palitana, Taranga, Sankheshwar, Idar. History. Jains believe that their 22nd Tirthankara (propagators of the Jain religion) Neminath attained Moksha/ Nirvana on Girnar in Gujarat. Many other holy Kalyanak places are present in Gujarat like Palitana(Shatrunjaya), Girnar, etc.

Geographic entities mentioned:
surface_form: Girnar
instance_of: Mountain
countries: India
coordinates: lat: 21.516962
lon: 70.53154
History. Jains believe that their 22nd Tirthankara (propagators of the Jain religion) Neminath attained Moksha/ Nirvana on Girnar in Gujarat. Many other holy Kalyanak places are present in Gujarat like Palitana(Shatrunjaya), Girnar, etc. Many other monks have also got attained Moksha in Gujarat; especially on the holy mountains of Girnar and Shatrunjaya. The Jain councils were held in Vallabhi c.

Geographic entities mentioned:
surface_form: Shatrunjaya
instance_of: Mountain
countries: India
coordinates: lat: 21.46833333
lon: 71.8
In the folk tale as set down by Rees, a young man, son of a widow from Blaen Sawdde (near Llanddeusant) agreed to marry a beautiful girl who arose from the lake of Llyn y Fan Fach, with a promise that he would not hit her three times without cause, or she would return to her father.

Geographic entities mentioned:
surface_form: Llyn y Fan Fach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.881944444444
lon: -3.7419444444444
Most of the supplies transiting through the Persian Corridor arrived by ship at various ports in the Persian Gulf and were then carried northwards by railroad or in long truck convoys. Some goods were later reloaded on board ships to cross the Caspian Sea and others continued their journey by truck.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Statues. These are located toward the back of the museum. Sculpture. A camphor wooden carving depicting Sakyamuni Buddha teaching the Dharma at Vulture Peak to Five Hundred Arhats is visible in the lobby of the Main Hall. Art Galleries. These are located on the 1st floor and 2nd floor of the Main Hall. There are 4 permanent exhibitions on the 1st floor.

Geographic entities mentioned:
surface_form: Vulture Peak
instance_of: Mountain
countries: India
coordinates: lat: 25.001666666666665
lon: 85.44638888888889
The Fighting Bengals were the final USMC All-Weather designated F/A-18 squadron to deploy. Accidents. On 12 March 2010 an F/A-18D Hornet from the squadron crashed off the coast of Saint Helena Sound north of Beaufort due to an engine fire. The pilot and Weapons Systems Officer were able to safely eject.

Geographic entities mentioned:
surface_form: Saint Helena Sound
instance_of: Landform
countries: United States
coordinates: lat: 32.45472222
lon: -80.44027778
Division of Wakefield. The Division of Wakefield was an Australian electoral division in the state of South Australia. The seat was a hybrid rural-urban electorate that stretched from Salisbury in the outer northern suburbs of Adelaide at the south of the seat right through to the Clare Valley at the north of the seat, 135 km from Adelaide.

Geographic entities mentioned:
surface_form: Clare Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.83361111
lon: 138.61
Geisingberg. The Geisingberg is a striking basalt mountain in the eastern Ore Mountains in the German federal state of Saxony. Location and surrounding area. The Geisingberg lies in the upper Eastern Ore Mountains between the mining town of Altenberg and the village of Geising. On its northern and western slopes runs the track of the Müglitz Valley Railway.

Geographic entities mentioned:
surface_form: geisingberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.771936111111
lon: 13.773438888889
Ben Aden. Ben Aden (887m) is a mountain in the Northwest Highlands of Scotland. It lies on the Knoydart peninsula in Lochaber. Regarded as one of the finest Corbetts in Scotland and one of the toughest to climb, the mountain is steep and rocky on all sides. The nearest village is Inverie.

Geographic entities mentioned:
surface_form: ben aden
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.030502
lon: -5.4637763
Peaking as a Category 4 hurricane, the hurricane struck the Bahamas and Florida at a slightly weaker intensity. Much of the Miami metropolitan area was devastated by the storm. Inland, a storm surge on Lake Okeechobee flooded towns such as Clewiston and Moore Haven. The storm was a factor in ending the Florida land boom of the 1920s.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
However, numerous structures were completely destroyed. The storm was attributed to 372 deaths in the Southeastern United States, 114 of which took place in Miami and at least 150 at Moore Haven, where a storm surge estimated as high as overtopped portions of a levee on Lake Okeechobee.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
state of Michigan. It is a census-designated place (CDP) for statistical purposes, without legal status as a municipality. The community is located within areas of both Coloma Charter Township and Watervliet Township in the area surrounding Paw Paw Lake and Little Paw Paw Lake, excluding the cities of Watervliet and Coloma. The population of the CDP was 3,323 at the 2020 census. History.

Geographic entities mentioned:
surface_form: Paw Paw Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2078
lon: -86.26961
Resistance to harsh climates and freezing temperatures. Many breeds of Turano-Mongolian cattle show a great hardiness and tolerance towards freezing temperatures as a result of adaption to harsh Asian climates. Especially the breeds of the Asian steppe and the Tibetan plateau are able to withstand temperature fluctuations from –50 °C to 35 °C (–60 °F to 95 °F).

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Thomas Mackay. Thomas Mackay (1849 &ndash; 1912) was a British wine merchant and classical liberal. Life. Mackay, the son of a colonel, was born in Edinburgh and educated at Glenalmond. He matriculated at New College, Oxford in 1868, graduating B.A. in 1873; he entered the Inner Temple in 1871.

Geographic entities mentioned:
surface_form: Glenalmond
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.435
lon: -3.701
It is adjacent to the city of Wilkes-Barre. The population of the township was 3,219 at the 2020 census. Founding. In 1753, the Susquehanna Company was formed in Connecticut for settling the Wyoming Valley in present-day Pennsylvania. Connecticut succeeded in purchasing the land from the Native Americans; however, Pennsylvania already claimed the valley through a purchase they made in 1736.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Those who managed to escape fled back to New England. The Delaware then burned what was left of the Yankee settlement. Pennamite–Yankee Wars. In 1769, during the colonial era, the Connecticut settlers (Yankees) returned to Wyoming Valley. Five townships were established by Connecticut Colony. Each one was five square miles and divided amongst forty settlers.

Geographic entities mentioned:
surface_form: Wyoming Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.251
lon: -75.906
Two days later, Caroline Matilda departed from Harwich for Rotterdam, and three weeks later she crossed the river Elbe and arrived in Altona, in the then Danish Duchy of Holstein. There she left her British entourage and was welcomed by her appointed Danish courtiers. Twelve days later, Caroline Matilda arrived in Roskilde, where she met her future husband for the first time.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Dammträsk. Dammträsk (Swedish for &quot;Pond Swamp&quot;) is a small man made lake within the Tyresån Lake System, located in Haninge Municipality, south of central Stockholm, Sweden. The lake receives water from Övre and Nedre Rudasjön south of the lake and empties into Drevviken north of it.

Geographic entities mentioned:
surface_form: Tyresån Lake System
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 59.2333
lon: 18.1667
surface_form: tyresån lake system
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 59.2333
lon: 18.1667
surface_form: dammträsk
instance_of: Lake
countries: Sweden
coordinates: lat: 59.179722222222
lon: 18.142222222222
Dammträsk. Dammträsk (Swedish for &quot;Pond Swamp&quot;) is a small man made lake within the Tyresån Lake System, located in Haninge Municipality, south of central Stockholm, Sweden. The lake receives water from Övre and Nedre Rudasjön south of the lake and empties into Drevviken north of it.

Geographic entities mentioned:
surface_form: Övre
instance_of: Lake
countries: Sweden
coordinates: lat: 59.168333333333
lon: 18.133333333333
surface_form: Nedre Rudasjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.158333333333
lon: 18.125
surface_form: Drevviken
instance_of: Lake
countries: Sweden
coordinates: lat: 59.233333333333
lon: 18.175
surface_form: drevviken
instance_of: Lake
countries: Sweden
coordinates: lat: 59.233333333333
lon: 18.175
surface_form: nedre rudasjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.158333333333
lon: 18.125
However, while the lake system as a whole is regarded as sensitive to surface runoff, Dammträsk is already too contaminated to be regarded as vulnerable. Water has been deliberately redirected from Rudasjön to Dammträsk, which reduces contamination of the downstream lake, Drevviken, since much of the waste is sedimented into the lake. The price to pay has been the dense vegetation in the lake.

Geographic entities mentioned:
surface_form: drevviken
instance_of: Lake
countries: Sweden
coordinates: lat: 59.233333333333
lon: 18.175
surface_form: dammträsk
instance_of: Lake
countries: Sweden
coordinates: lat: 59.179722222222
lon: 18.142222222222
Dammträsk. Dammträsk (Swedish for &quot;Pond Swamp&quot;) is a small man made lake within the Tyresån Lake System, located in Haninge Municipality, south of central Stockholm, Sweden. The lake receives water from Övre and Nedre Rudasjön south of the lake and empties into Drevviken north of it.

Geographic entities mentioned:
surface_form: dammträsk
instance_of: Lake
countries: Sweden
coordinates: lat: 59.179722222222
lon: 18.142222222222
Environmental impact. The lake and the surrounding wetlands, together with local forests, are regarded as a valuable local natural resource. However, while the lake system as a whole is regarded as sensitive to surface runoff, Dammträsk is already too contaminated to be regarded as vulnerable.

Geographic entities mentioned:
surface_form: dammträsk
instance_of: Lake
countries: Sweden
coordinates: lat: 59.179722222222
lon: 18.142222222222
Ullscarf. Ullscarf is a fell in the English Lake District close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south. Topography. Ullscarf is bordered on the west by the Greenup valley, with steep but mainly grassy slopes, the chief exception being Lining Crag.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
To the north, the natural boundaries are unclear. Standing Crag provides a terminus to the summit plateau, rising above its reflecting tarn. From here the ridge continues across wet ground towards High Tove, the next Wainwright. Some guidebooks consider the intermediate Bell Crags (summit unnamed on Ordnance Survey maps) to be a separate fell.

Geographic entities mentioned:
surface_form: High Tove
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5396
lon: -3.10199
surface_form: high tove
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5396
lon: -3.10199
From here the ridge continues across wet ground towards High Tove, the next Wainwright. Some guidebooks consider the intermediate Bell Crags (summit unnamed on Ordnance Survey maps) to be a separate fell. A second subsidiary ridge extends north-north-west from the summit to Great Crag, passing over the twin tops of Coldbarrow Fell. Between these two northern ridges lies Blea Tarn.

Geographic entities mentioned:
surface_form: Great Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5223
lon: -3.13087
surface_form: great crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5223
lon: -3.13087
The summit is marked by a large cairn on a small rocky outcrop, the old fenceposts marching past (intermittently) in either direction. Views from the top are extensive, befitting the central location, with the Scafells and Helvellyn ranges being shown to particular effect. Ascents. From Wythburn to the south east a number of routes are possible.

Geographic entities mentioned:
surface_form: Scafells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
surface_form: helvellyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.527230555556
lon: -3.0160527777778
This may be a corrie tarn that has silted up over time, extensive shallows being colonised by sedge, water horsetail and yellow water lilly. These waters are joined by the Wyth Burn from the south of the fell. All water from the west of the fell reaches Greenup Gill via a number of feeders and flows to Derwentwater. Geology.

Geographic entities mentioned:
surface_form: derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
To the south of Thirlmere is its feeder valley of Wythburndale, which rises eastward to its source below Greenup Edge. Above Wythburndale Ullscarf displays a near continuous line of crags, the principal faces being Castle Crag and Nab Crags. A series of low tops crown the edge above Nab Crags, one of them bearing a prominent stone structure visible from the valley below.

Geographic entities mentioned:
surface_form: castle crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5328
lon: -3.16207
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
Ullscarf. Ullscarf is a fell in the English Lake District close to the geographical centre of the Cumbrian hills. It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south. Topography. Ullscarf is bordered on the west by the Greenup valley, with steep but mainly grassy slopes, the chief exception being Lining Crag.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
It forms part of the watershed between the Derwentwater and Thirlmere catchments, a ridge running broadly north-south. Topography. Ullscarf is bordered on the west by the Greenup valley, with steep but mainly grassy slopes, the chief exception being Lining Crag. This rock face is prominent in views up the valley, standing right beside the bridleway.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
This rock face is prominent in views up the valley, standing right beside the bridleway. From above however it is reached via a shallow grassy saddle and makes a fine viewpoint or picnic spot. A number of gills run down this western side of Ullscarf. To the east lies Thirlmere across a moorland of small hillocks. The final descent is steep, falling down conifer-clad slopes to the reservoir.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
This is marked &quot;Beacon&quot; on OS maps, but is in fact a very short length of dry stone wall. It was set up some decades ago to replace a vandalised beacon cairn. The main ridge of the Central Fells continues south from Ullscarf, dropping over a field of rocky knolls to cross the wide depression of Greenup Edge. This is the connection to High Raise, the highest of the Central Fells.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
Between these two northern ridges lies Blea Tarn. A large pool of about depth, Blea Tarn provides the main feed for the more famous beauty spot of Watendlath Tarn. Drainage to the east (and Thirlmere) is provided by Ullscarf and Launchy Gills, the former flowing via the secluded Harrop Tarn within the Thirlmere Forest.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
There are few paths on the fell itself. One track follows the watershed, being marked in places by old iron fenceposts. Bridleways cross the ridge to the north and south of Ullscarf, providing access from Wythburn, Thirlmere, Stonethwaite and Watendlath. The summit is marked by a large cairn on a small rocky outcrop, the old fenceposts marching past (intermittently) in either direction.

Geographic entities mentioned:
surface_form: ullscarf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.500161111111
lon: -3.09475
It was set up some decades ago to replace a vandalised beacon cairn. The main ridge of the Central Fells continues south from Ullscarf, dropping over a field of rocky knolls to cross the wide depression of Greenup Edge. This is the connection to High Raise, the highest of the Central Fells. To the north, the natural boundaries are unclear.

Geographic entities mentioned:
surface_form: high raise
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -2.851
surface_form: high raise
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.476
lon: -3.113
This consists of dacitic lapilli tuff with andesite sills. The eastern plateau above Thirlmere shows some outbreaks of the volcaniclastic sandstone of the Esk Pike Formation. A 16th century mine, Launchy Gill Level, was driven into the fellside below White Crags on the Thirlmere side of the fell. A scramble is required just to reach the mouth of the level. Summit.

Geographic entities mentioned:
surface_form: esk pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456219444444
lon: -3.17995
A second subsidiary ridge extends north-north-west from the summit to Great Crag, passing over the twin tops of Coldbarrow Fell. Between these two northern ridges lies Blea Tarn. A large pool of about depth, Blea Tarn provides the main feed for the more famous beauty spot of Watendlath Tarn.

Geographic entities mentioned:
surface_form: blea tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
Between these two northern ridges lies Blea Tarn. A large pool of about depth, Blea Tarn provides the main feed for the more famous beauty spot of Watendlath Tarn. Drainage to the east (and Thirlmere) is provided by Ullscarf and Launchy Gills, the former flowing via the secluded Harrop Tarn within the Thirlmere Forest.

Geographic entities mentioned:
surface_form: blea tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
The Wythburn valley (and its bogs) can be followed to reach the ridge at Greenup edge, or more direct climbs can be made via Harrop Tarn. From here either the line of tops above Nab Crags or Standing Crag will be the intermediate objective. Ullscarf can be climbed from Watendlath, gaining the north-north-east ridge above Blea Tarn, and then ascending over the tops of Coldbarrow Fell.

Geographic entities mentioned:
surface_form: blea tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
Andrés Cárdenas was a farm worker near Stockton, California, before the family relocated to Pacoima in 1954. Cárdenas graduated from San Fernando High School in the northeast San Fernando Valley. In 1986, he earned a Bachelor of Science degree in electrical engineering from the University of California, Santa Barbara. Elections.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Port Johnston Coal Docks. The Port Johnston Coal Docks were built on the Kill van Kull at Constable Hook in Bayonne, New Jersey in 1864 by the Central Railroad of New Jersey. The coal dock was named after the company's president John Taylor Johnston. (The former Johnston Yard and today's Johnston Avenue also bear his name).

Geographic entities mentioned:
surface_form: Constable Hook
instance_of: Landform
countries: United States
coordinates: lat: 40.6578
lon: -74.0994
Geographically, Lagos State is dominated by bodies of water with nearly a quarter of the state's area being lagoons, creeks, and rivers. The largest of these bodies are the Lagos and Lekki lagoons in the state's interior with the Ogun and Osun rivers flowing into them. Many other rivers and creeks flow throughout the state and serve as vital means of transportation for people and goods.

Geographic entities mentioned:
surface_form: Lagos
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
The conurbation is one of the most populous in the world. Lagos is a port which originated on islands separated by creeks, such as Lagos Island, fringing the southwest mouth of Lagos Lagoon while protected from the Atlantic Ocean by barrier islands and long sand spits such as Bar Beach, which stretch up to east and west of the mouth.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
The proposed land use master plan for the Lekki envisages the Peninsula as a &quot;Blue-Green Environment City&quot;, expected to accommodate over 3.4 million residential population and an additional non-residential population of at least 1.9 million. Ikorodu. Ikorodu is a city located north-east of the state along the Lagos Lagoon. It shares a boundary with Ogun State.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
Water Borders. Lagos State's water boundaries are defined by the Atlantic Ocean to the south and the Lagos Lagoon to the east. The state is also intersected by several rivers and creeks, including the Ogun River, which drains into the Lagoon. Major coastal areas include Victoria Island, Lekki, and Epe.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
Fourth Mainland Bridge. The Fourth Mainland Bridge is a 38 km long bridge project by the Lagos State Government, connecting Lagos Island by way of Langbasa(Lekki) and Baiyeku(Ikorodu) across the Lagos Lagoon to Itamaga, in Ikorodu. The bridge is a 2 x 4 lane carriageway cross-sectional road with permission for BRT Lane and future road contraction.

Geographic entities mentioned:
surface_form: Lagos Lagoon
instance_of: Lake
countries: Nigeria
coordinates: lat: 6.5015814
lon: 3.5224915
Ulungur River. The Ulungur River / Urungu River or Urungu (,), in its upper reaches in Mongolia known as the Bulgan River (), is a river of China and Mongolia. It rises in the Altai Mountains in western Mongolia, flows south into China's Xinjiang (Altay Prefecture), where it turns north-west to empty into the Ulungur Lake. It is about 700 km long.

Geographic entities mentioned:
surface_form: Ulungur Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 47.25
lon: 87.316666666667
The route is named for the fall line escarpment it follows, a geographical division between the coastal plain and inland hills. Muscogee County. SR 540 and the FLF begin on an unnamed bridge over the Chattahoochee River, at the Alabama state line, on the Phenix City, Alabama–Columbus city line, concurrent with U.S. Route 80 (US 80) and SR 22. The state line is also the western terminus of SR 22.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
SS Superior City. SS &quot;Superior City&quot; was considered a pioneer vessel at her launching in 1898. She was the largest vessel ever built on freshwater at that time. She sailed the Great Lakes for twenty-two years until she sank after a collision in 1920 with the steamer in Whitefish Bay of Lake Superior that resulted in the loss of 29 lives. Controversy was immediate over the collision.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Milvydai (&quot;Melvidai, Milvidai&quot;, formerly,) is a village in Kėdainiai district municipality, in Kaunas County, in central Lithuania. According to the 2011 census, the village had a population of 45 people. It is located from Krakės, by the Krakės-Grinkiškis road, nearby the Smilgaitis river sources. There are an airstrip, a milk buying post and old cemetery of the Goštautai family.

Geographic entities mentioned:
surface_form: Smilgaitis
instance_of: Watercourse
countries: Lithuania
coordinates: lat: 55.29171
lon: 23.894404
They are also adapted to thrive in a variety of environments, and as generalists, may be better able to persist in disturbed habitats than native species of those areas. Red shiners are capable of hybridizing with the blacktail shiner (&quot;Cyprinella venusta stigmatura&quot;), a native species found in the Coosa River, which serves to dilute the gene pool of this species.

Geographic entities mentioned:
surface_form: Coosa River
instance_of: Watercourse
countries: United States
coordinates: lat: 32.4862464
lon: -86.2777475
On 5 November 2,572 troops were loaded at Calcutta but the ship did not start moving down the Hooghly River until the next day. After a brief stop at Singapore the &quot;Marine Robin&quot; began the great circle voyage to Seattle passing within sight of Okinawa and glimpsing Mount Fuji before skirting the Aleutians and encountering heavy seas.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
It lies in the Oruro Department, Sajama Province, on the border of the Curahuara de Carangas Municipality and the Turco Municipality. Chunkarani is situated north-east of the volcanic complex of Asu Asuni.

Geographic entities mentioned:
surface_form: Asu Asuni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.21666667
lon: -68.51666667
surface_form: asu asuni
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.21666667
lon: -68.51666667
Chunkarani. Chunkarani (Aymara &quot;chunkara&quot; pointed mountain, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with a pointed mountain&quot;, Hispanicized spelling &quot;Chungarani&quot;) is a mountain in the Andes of Bolivia. It lies in the Oruro Department, Sajama Province, on the border of the Curahuara de Carangas Municipality and the Turco Municipality.

Geographic entities mentioned:
surface_form: chunkarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1375
lon: -68.4708
surface_form: chunkara
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.96555556
lon: -66.91777778
Chunkarani. Chunkarani (Aymara &quot;chunkara&quot; pointed mountain, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with a pointed mountain&quot;, Hispanicized spelling &quot;Chungarani&quot;) is a mountain in the Andes of Bolivia. It lies in the Oruro Department, Sajama Province, on the border of the Curahuara de Carangas Municipality and the Turco Municipality.

Geographic entities mentioned:
surface_form: chunkarani
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.1375
lon: -68.4708
Casalduni. Casalduni is a &quot;comune&quot; (municipality) in the Province of Benevento in the Italian region Campania, located about 60 km northeast of Naples and about 15 km northwest of Benevento, on the slopes of Monte Cicco on the right of the Tammaro river. History.

Geographic entities mentioned:
surface_form: Monte Cicco
instance_of: Mountain
countries: Italy
coordinates: lat: 45.25416667
lon: 11.7425
Pearl Shoal Waterfall. Pearl Shoal Waterfall () is a waterfall located in Jiuzhaigou, Aba-Ngawa Tibetan and Qiang Autonomous Prefecture in northern Sichuan Province, China. Located at an altitude of, the top of the waterfall is in width. It has a fall of. The waterfall exists on one of the tributaries of the Bailong River.

Geographic entities mentioned:
surface_form: Jiuzhaigou
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 33.2
lon: 103.9
Anagnorisma chamrani. &quot;Anagnorisma chamrani&quot; is a moth in the family Noctuidae. It was found in the Binaloud Mountains of the Razavi Khorasan Province in north-eastern Iran in 2012. Etymology. The species is named in honour of Mostafa Chamran (1932–1981). Specifics. The species has a wingspan of 34–35 mm.

Geographic entities mentioned:
surface_form: Binaloud Mountains
instance_of: Mountain
countries: Iran
coordinates: lat: 36.426388888889
lon: 58.849166666667
Lake Meshkeysor is located at the center in a trough of saline young soils and salt marshes. Karasor, a smaller lake, lies to the SSE, and a very large reddish sor to the northeast. Lake Kabyrshakty lies to the southeast. Meshkeysor freezes in November and stays under ice until April. It fills during the spring thaw with a river flowing from the north and another flowing from the southwest.

Geographic entities mentioned:
surface_form: Kabyrshakty
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48.33694444444445
lon: 69.52333333333333
Meshkeysor. Meshkeysor (;) is a salt lake in Ulytau District, Ulytau Region, Kazakhstan. Abilzhappas (), a wintering settlement &quot;(Kystau)&quot; of Kazakh herders, is located to the northeast of the northern lakeshore. Geography. Meshkeysor is an endorheic lake in the Sarysu basin. The lake has a sinuous shape stretching roughly from east to west, surrounded by salt pans.

Geographic entities mentioned:
surface_form: meshkeysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48.688888888889
lon: 68.721666666667
Geography. Meshkeysor is an endorheic lake in the Sarysu basin. The lake has a sinuous shape stretching roughly from east to west, surrounded by salt pans. The lake lies in the middle of the Meshkeysor region, a vast area characterized by flat valleys and low hills. The altitude of this region lies between and. It is limited by rivers Sary-Kengyr and Sarysu.

Geographic entities mentioned:
surface_form: meshkeysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48.688888888889
lon: 68.721666666667
Young started helping injured animals, and his collection started getting visitors. The Chiang Mai provincial administration set aside at the base of Doi Suthep, the mountain immediately adjacent to Chiang Mai, and the facility was opened to the public in 1957. When Young died in 1974, the property was taken over by Chiang Mai Province.

Geographic entities mentioned:
surface_form: Doi Suthep
instance_of: Mountain
countries: Thailand
coordinates: lat: 18.816388888889
lon: 98.893055555556
He was an assistant superintendent until 1944 when he became director. After independence he served as an advisor for fisheries development to the Government of India. Chopra collected aquatic fauna on several expeditions, particularly to Meghalaya, the Shan States and the Indawggyi Lake in Upper Burma and described a number of species, particularly decapods.

Geographic entities mentioned:
surface_form: Indawggyi Lake
instance_of: Lake
countries: Myanmar
coordinates: lat: 25.133333333333
lon: 96.333333333333
Domino lake. 6x8usn154btotxgnetm8us7r24d" xml:space="preserve">#REDIRECT Domino Lake

Geographic entities mentioned:
surface_form: domino lake
instance_of: Lake
coordinates: lat: -62.83013888888889
lon: -61.47152777777778
Begnas Lake. Begnas Lake () is a freshwater lake in Pokhara Metropolis of Kaski district of Nepal located in the south-east of the Pokhara Valley. The lake is the third largest lake of Nepal and second largest, after Phewa Lake, among the seven lakes in Pokhara Valley. Water level in the lake fluctuates seasonally due to rain, and utilization for irrigation.

Geographic entities mentioned:
surface_form: Pokhara Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 28.233333333333
lon: 83.983333333333
surface_form: begnas lake
instance_of: Lake
countries: Nepal
coordinates: lat: 28.171666666667
lon: 84.1