Sarmila/GeoWiki-Features huggingface dataset:
The trail covers 3.2 miles from an elevation of 6,000 feet at the trailhead and ends at the Mt. Ireland Fire Lookout. The summit overlooks Baldy Lake on the north slope and though the mountain peak's name was changed, the small mountain lake retained its original name. The view from the summit provides an extensive panorama of the North Fork John Day Wilderness.

Geographic entities mentioned:
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 31.69612
lon: -110.8481
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 43.1064
lon: -74.3697
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 37.36
lon: -80.5339
surface_form: mountain lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9522405
lon: -74.983331
surface_form: baldy
instance_of: Mountain
countries: United States
coordinates: lat: 42.2983
lon: -122.751
For a period of several years, this mountain peak was referred to as Bald Mountain, but in 1917 it was changed to Ireland Mountain—in commemoration of the late Henry Ireland, who for 10 years was supervisor of the Whitman National Forest in which the mountain is located—before formally becoming known as Mount Ireland.

Geographic entities mentioned:
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.655
lon: -114.409
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 46.8827026
lon: -88.0390147
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.8822
lon: -123.866
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6611024
lon: -107.4103338
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.4291
lon: -75.7503
surface_form: mount ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.6988
lon: -110.902
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.021388888889
lon: -75.190833333333
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.5344
lon: -119.115
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.423611111111
lon: -74.593888888889
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.1209
lon: -74.2001
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.902777777778
lon: -74.724444444444
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.4439
lon: -105.969
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7386
lon: -74.9129
surface_form: bald mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.294722222222
lon: -74.387777777778
Mount Ireland. Mount Ireland is a mountain in Grant County of the U.S. state of Oregon. It is about east-northeast of Granite, Oregon. It is the shortest and westernmost 8000'+ peak in the Elkhorn Range of the Blue Mountains at, and Oregon's 71st highest peak with at least a 500' clean prominence.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
Several gold mining claims were established in the area and are still identifiable on local forest maps. Some are still patented while others have long been abandoned. Mount Ireland is located in the Wallowa-Whitman National Forest and outdoor enthusiasts are welcome to hike the Mt. Ireland Lookout Trail #1604 which is open Summer and Fall.

Geographic entities mentioned:
surface_form: mt. ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
surface_form: mount ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
Mount Ireland is located in the Wallowa-Whitman National Forest and outdoor enthusiasts are welcome to hike the Mt. Ireland Lookout Trail #1604 which is open Summer and Fall. Though the trail is ranked as &quot;more difficult&quot;, there are no restrictions. The trail covers 3.2 miles from an elevation of 6,000 feet at the trailhead and ends at the Mt. Ireland Fire Lookout.

Geographic entities mentioned:
surface_form: mt. ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
Mount Ireland. Mount Ireland is a mountain in Grant County of the U.S. state of Oregon. It is about east-northeast of Granite, Oregon. It is the shortest and westernmost 8000'+ peak in the Elkhorn Range of the Blue Mountains at, and Oregon's 71st highest peak with at least a 500' clean prominence.

Geographic entities mentioned:
surface_form: mount ireland
instance_of: Mountain
countries: United States
coordinates: lat: 44.836533333333
lon: -118.32077777778
Iliwerung. Iliwerung or Illiwerung is a complex volcano forming a prominent south-facing peninsula on Lembata Island in southern Indonesia. It contains north-south and northwest-southeast trending lines of craters and lava domes, with the summit dome having formed by a VEI-3 eruption in 1870.

Geographic entities mentioned:
surface_form: iliwerung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.5322222222222
lon: 123.57333333333
It contains north-south and northwest-southeast trending lines of craters and lava domes, with the summit dome having formed by a VEI-3 eruption in 1870. Iliwerung has erupted at least 13 times since 1870, with eruptions having occurred in 1910, 1928, 1948, 1949, 1950, 1951, 1952, 1973-1974, 1976, 1983, 1993, 1999, 2013 and 2021.

Geographic entities mentioned:
surface_form: iliwerung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.5322222222222
lon: 123.57333333333
Iliwerung has erupted at least 13 times since 1870, with eruptions having occurred in 1910, 1928, 1948, 1949, 1950, 1951, 1952, 1973-1974, 1976, 1983, 1993, 1999, 2013 and 2021. Eruptions since 1973 have been confined to Hobal, a submarine parasitic vent on Iliwerung's lower east-southeastern flank. Iliwerung lies on the southern rim of the Lerek caldera.

Geographic entities mentioned:
surface_form: iliwerung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.5322222222222
lon: 123.57333333333
Eruptions since 1973 have been confined to Hobal, a submarine parasitic vent on Iliwerung's lower east-southeastern flank. Iliwerung lies on the southern rim of the Lerek caldera. A landslide from Iliwerung in 1979 produced tsunamis that resulted in more than 500 people killed. In 1983, a tsunami resulting from a submarine eruption caused few deaths.

Geographic entities mentioned:
surface_form: iliwerung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.5322222222222
lon: 123.57333333333
Its sub-basin covers around 53 km2 and is part of the Piracicaba River sub-basin, which is included in the Doce River Basin. It is bordered by the sub-basins of the Ipanema, Cocais Pequeno and Caladinho streams, covering a population of approximately 70,000 residents.

Geographic entities mentioned:
surface_form: Caladinho
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.526972222222224
lon: -42.60919444444445
Caladão Stream. The Caladão Stream (Portuguese: &quot;Ribeirão Caladão&quot;) is a watercourse that rises and flows in the Brazilian municipality of Coronel Fabriciano, in the state of Minas Gerais. The source is located in Serra dos Cocais and runs for 10 kilometers to its mouth in the Piracicaba River.

Geographic entities mentioned:
surface_form: ribeirão caladão
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
surface_form: caladão stream
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
Caladão Stream. The Caladão Stream (Portuguese: &quot;Ribeirão Caladão&quot;) is a watercourse that rises and flows in the Brazilian municipality of Coronel Fabriciano, in the state of Minas Gerais. The source is located in Serra dos Cocais and runs for 10 kilometers to its mouth in the Piracicaba River.

Geographic entities mentioned:
surface_form: caladão stream
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
Floods and drainage attempts. Overflows were already frequent during heavy rains. Between January and February 1979, the high level of the Piracicaba River caused the flooding of the Caladão Stream after about 40 consecutive days of heavy rains.

Geographic entities mentioned:
surface_form: caladão stream
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
Mayor Mariano Pires Pontes began drainage work on the basin to alleviate the flooding problems and built Sanitária Avenue (now Julita Pires Bretas Avenue) bordering a section of the basin with channeled gabions. On December 15, 2005, a flood affected all the neighborhoods bordering the Caladão Stream (except Santa Helena) and left dozens homeless.

Geographic entities mentioned:
surface_form: caladão stream
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
However, the project was suspended because residents in the area feared odors. In the following years, collection networks and interceptors were installed throughout the Caladão Stream sub-basin, even without a definitive position on the location of the sewage treatment plant.

Geographic entities mentioned:
surface_form: caladão stream
instance_of: Body of water
countries: Brazil
coordinates: lat: -19.525916666666667
lon: -42.618027777777776
The organization actively works to improve public history on Hawai‘i and Native Hawaiians. It has a substantial social media following and appears regularly in media due to its unique expertise and leadership in the Hawaiian community. In July 2019, Ritte was arrested while protesting the construction of the Thirty Meter Telescope on Mauna Kea.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Range and habitat. &quot;Gramastacus lacus&quot; is found in a number of geographically isolated populations along the Central and Mid North Coast of New South Wales, Australia. It is native to coastal lowlands from Wamberal Lagoon to Wamberal Lagoon, usually to above sea level. Populations typically occur in ephemeral wetlands such as small creeks and swamps, in depths no greater than.

Geographic entities mentioned:
surface_form: Wamberal Lagoon
instance_of: Lake
countries: Australia
coordinates: lat: -33.4333
lon: 151.45
surface_form: Wamberal Lagoon
instance_of: Lake
countries: Australia
coordinates: lat: -33.4333
lon: 151.45
The neighborhood is closed to automobile traffic on Shabbat and Jewish holidays. Sanhedria Murhevet is home to Yeshivat Tiferet Zvi, Yeshivat Kinyan Torah, Yeshiva Toras Moshe, Yeshiva Chofetz Chaim, the Jerusalem Kollel, and Kollel Meshech Chochma as well as some schools which include Hatzafon, Knesset Yehuda. The Har Hotzvim industrial complex and Yeshivat Horev are located nearby. Nahal Tzofim.

Geographic entities mentioned:
surface_form: Har Hotzvim
instance_of: Mountain
countries: Israel
coordinates: lat: 31.802527777778
lon: 35.209636111111
The Cordillera de Guanacaste, also called Guanacaste Cordillera, are a volcanic mountain range in northern Costa Rica near the border with Nicaragua. The mountain range stretches 110 km from northwest to the southeast and contains mostly complex stratovolcanoes. The range forms part of the southern region of the Continental Divide, with the highest peak is the stratovolcano Miravalles at 2,028 m.

Geographic entities mentioned:
surface_form: Miravalles
instance_of: Mountain
countries: Costa Rica
coordinates: lat: 10.747277777778
lon: -85.150944444444
Blea Tarn (Eskdale). Blea Tarn is a lake in Eskdale, Cumbria, in the English Lake District, located about half a mile north of Beckfoot. Located at an elevation of, the lake has an area of and measures, with a maximum depth of. There are other lakes called &quot;Blea Tarn&quot; in the Lake District (in Borrowdale and Little Langdale). John Taylor commented in 1905 that

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: blea tarn (eskdale)
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Blea Tarn (Eskdale). Blea Tarn is a lake in Eskdale, Cumbria, in the English Lake District, located about half a mile north of Beckfoot. Located at an elevation of, the lake has an area of and measures, with a maximum depth of. There are other lakes called &quot;Blea Tarn&quot; in the Lake District (in Borrowdale and Little Langdale). John Taylor commented in 1905 that

Geographic entities mentioned:
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
surface_form: blea tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
surface_form: eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.189
lon: -3.068
Blea Tarn (Eskdale). Blea Tarn is a lake in Eskdale, Cumbria, in the English Lake District, located about half a mile north of Beckfoot. Located at an elevation of, the lake has an area of and measures, with a maximum depth of. There are other lakes called &quot;Blea Tarn&quot; in the Lake District (in Borrowdale and Little Langdale). John Taylor commented in 1905 that

Geographic entities mentioned:
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: blea tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.398024
lon: -3.286979
surface_form: little langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.419557
lon: -3.073825
Blea Tarn (Eskdale). Blea Tarn is a lake in Eskdale, Cumbria, in the English Lake District, located about half a mile north of Beckfoot. Located at an elevation of, the lake has an area of and measures, with a maximum depth of. There are other lakes called &quot;Blea Tarn&quot; in the Lake District (in Borrowdale and Little Langdale). John Taylor commented in 1905 that

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
Magdalena Apasco. Magdalena Apasco is a town and municipality in Oaxaca in south-western Mexico. The municipality covers an area of 29.34 km2. It is part of the Etla District in the Valles Centrales region. As of 2005, the municipality had a total population of 6,148.

Geographic entities mentioned:
surface_form: Valles Centrales region
instance_of: Valley
countries: Mexico
coordinates: lat: 17.0833
lon: -96.75
It lies about north of Limavady on Aghanloo Road, the A2 coastal route between Limavady and Coleraine. It is designated as a hamlet and is situated within Causeway Coast and Glens district and in the former North Londonderry Area of Outstanding Natural Beauty, now redesignated as the Binevenagh Area of Outstanding Natural Beauty (AONB).

Geographic entities mentioned:
surface_form: Binevenagh Area of Outstanding Natural Beauty
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.11
lon: -6.92
ʻĀina Haina, Hawaii. Āina Haina is an unincorporated town of the City & County of Honolulu in the state of Hawaii of the United States. Located on the island of Oahu, Āina Haina is a residential community developed around Kalanianaole Highway east of Waikīkī and Diamond Head. Āina Haina was named after local dairyman and owner of Hind-Clarke Dairy, Robert Hind.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Joseph Ernst Seppelt. Joseph Ernst Seppelt (1813 &ndash; 29 January 1868) was a German-born Australian viticulturist and merchant who migrated to South Australia in 1849, and in 1851 settled in the Barossa Valley where he established Seppeltsfield, South Australia and the Seppelt winery. Life.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Through an agent in London, Seppelt managed to buy land in Adelaide, South Australia. After realising his tobacco was not growing, he moved to the Barossa Valley region in 1851 and purchased which he named Seppeltsfield. Here he grew wheat, farmed dairy cattle, and planted vines. He made his first wine in 1867 in his wife's small dairy.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
These right-lateral movements record significant Cenozoic deformation driven by both Alpine compression and mantle plume-related extension. In the Mid-Palaeocene, movement on the Camlough Fault helped form the Lough Neagh pull-apart basin. This focused subsidence beneath the modern lake and allowed unusually thick sequences of Palaeogene basalts and overlying Oligocene clays to accumulate.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Chawpi Tiyana. Chawpi Tiyana (Quechua &quot;chawpi&quot; central, middle, &quot;tiyana&quot; seat, &quot;central seat&quot;, hispanicized spelling &quot;Chaupitiana&quot;) is a mountain in the La Raya mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Canchis Province, Marangani District. It lies southwest of Kuntur Quta and south of Wiyachayuq.

Geographic entities mentioned:
surface_form: Kuntur Quta
instance_of: Mountain
countries: Peru
coordinates: lat: -14.3581
lon: -71.0258
Chawpi Tiyana. Chawpi Tiyana (Quechua &quot;chawpi&quot; central, middle, &quot;tiyana&quot; seat, &quot;central seat&quot;, hispanicized spelling &quot;Chaupitiana&quot;) is a mountain in the La Raya mountain range in the Andes of Peru, about high. It is located in the Cusco Region, Canchis Province, Marangani District. It lies southwest of Kuntur Quta and south of Wiyachayuq.

Geographic entities mentioned:
surface_form: chawpi tiyana
instance_of: Mountain
countries: Peru
coordinates: lat: -14.37916667
lon: -71.05027778
Victoria Falls, Wester Ross. Victoria Falls is a waterfall on the southern side of Loch Maree in Wester Ross in the north-west of Scotland. It is on the Abhainn Garbhaig, a short river that flows from Loch Garbhaig to Loch Maree. The falls are within Slattadale Forest, owned by the Forestry Commission.

Geographic entities mentioned:
surface_form: Loch Maree
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.689722222222
lon: -5.4575
Climate. Given the prevailing southwest and west winds, Dirmstein's location alee of the Palatinate Forest means that the locality must make do with at most 500 mm of precipitation yearly. Moreover, in weather out of the northwest, the massif of the Donnersberg, lying 25 km away in the North Palatine Highland and rising to 689 m, often likewise hinders any abundance of precipitation.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Text. Kurt Aland did not place the Greek text of the codex in any Category. It was not examined by the Claremont Profile Method. History. The manuscript belonged to the monastery Pantocrator at Athos peninsula. It was brought to Moscow, by the monk Arsenius, on the suggestion of the Patriarch Nikon, in the reign of Alexei Mikhailovich Romanov (1645-1676). The manuscript was collated by C. F.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
The total area of the city is. Geography. Fukutsu is located in northern Fukuoka Prefecture, approximately midway between Fukuoka City and Kitakyushu City. It is surrounded by Mt. Kohbi, Mt. Motoki, and Mt. Iimori from the east to the south, and the Genkai Sea (Sea of Japan) to the northwest. The coast has been designated as part of the Genkai Quasi-National Park, and is a scenic area. Climate.

Geographic entities mentioned:
surface_form: Genkai Sea
instance_of: Body of water
countries: Japan
coordinates: lat: 34
lon: 130
A week later, further withdrawals took them towards Elasson, where the regiment was briefly attached in support of the 6th New Zealand Brigade. On 18 April, the fighting was so intense that the regiment's guns fire over 6,000 rounds in a twenty-four-hour period as it attempted to thwart the advance of a German armoured column near Mount Olympus.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Saas im Prättigau. Saas im Prättigau is a Swiss village in the Prättigau and a former municipality in the district of Davos in the canton of Graubünden. On 1 January 2016 the former municipality of Saas im Prättigau merged into the municipality of Klosters-Serneus. History. Saas is first mentioned about 1290 as &quot;Säusch&quot;. Geography. Saas has an area, of.

Geographic entities mentioned:
surface_form: Prättigau
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9165
lon: 9.8537194444444
Of the rest of the land, 2.1% is settled (buildings or roads) and the remainder (27.7%) is non-productive (rivers, glaciers or mountains). The municipality is located in the Küblis sub-district of the Prättigau/Davos district. It consists of the linear village of Saas on a terrace over the Prättigau valley, between Küblis and Klosters. Coat of arms.

Geographic entities mentioned:
surface_form: Prättigau
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9165
lon: 9.8537194444444
The pass is located in the municipality of Ormont-Dessous in the canton of Vaud. It links Aigle, to the south in the valley of the Rhone, with Château-d'Œx, to the north in the valley of the Sarine, and is flanked to the west by the Mont d'Or and to the east by the Pic Chaussy. Road and public transports. The pass is traversed by a major road between Aigle and Château-d'Œx.

Geographic entities mentioned:
surface_form: Pic Chaussy
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.377111111111
lon: 7.1127777777778
It lies at an elevation of and covers an area of, not including occupied by islands within the lake such as Grande Île or Grosse Île. In the Innu language, &quot;ashuanipi&quot; means &quot;a place to cross.&quot; Ashuanipi River flows from the north end of the lake to the Menihek Lakes, which ultimately drain through the Churchill River system into Lake Melville and the Atlantic Ocean.

Geographic entities mentioned:
surface_form: Lake Melville
instance_of: Lake
countries: Canada
coordinates: lat: 53.68222222222222
lon: -59.74861111111111
surface_form: lake melville
instance_of: Lake
countries: Canada
coordinates: lat: 53.68222222222222
lon: -59.74861111111111
Through radiocarbon dating, evidence has been found at the lake for human habitation as far back as 1600 years ago. Along with the Moisie River, whose headwaters are nearby, the lake was part of a route used by the Innu to reach the lower north shore of the St. Lawrence River. The lake was known to the colonists of New France by the early 18th century.

Geographic entities mentioned:
surface_form: Moisie River
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.2
lon: -66.0675
Ashuanipi Lake. Ashuanipi Lake () is an irregularly shaped lake in southern Labrador, in the Canadian province of Newfoundland and Labrador. It lies at an elevation of and covers an area of, not including occupied by islands within the lake such as Grande Île or Grosse Île.

Geographic entities mentioned:
surface_form: ashuanipi lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.75
lon: -66.24944444
The Quebec North Shore and Labrador Railway runs along the lake's eastern shore, and the Trans-Labrador Highway crosses the Ashuanipi River about north of the lake's northern terminus. The lake features excellent fishing for lake trout, pike, whitefish and landlocked salmon. The Lac Joseph caribou herd can be found around Ashuanipi Lake during the summer and fall.

Geographic entities mentioned:
surface_form: ashuanipi lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.75
lon: -66.24944444
After the war of 1866 by which Austria lost Venetia, Cibrario negotiated with that government for the restitution of state papers and art treasures removed by it from Lombardy and Venetia to Vienna. Count Cibrario died near Salò on Lake Garda in autumn 1870.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Ancient authors tell that they were pirates that threatened navigation in the Adriatic Sea, but the consuls' campaign was part of a planned strategy of securing the northern border of the Republic. The previous consuls had indeed campaigned against the Celts of the Po Valley.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Discovery and naming. Ornithomimosaur body fossils and ichnofossils were reported in Thailand's Khorat Plateau as early as 1997 in a publication by Eric Buffetaut and colleagues. At the time, only two dinosaur genera, &quot;Siamotyrannus&quot; and &quot;Phuwiangosaurus&quot; had been named from the country.

Geographic entities mentioned:
surface_form: Khorat Plateau
instance_of: Plateau
countries: Thailand
coordinates: lat: 15.666666666667
lon: 103.16666666667
In the western Pacific, it can be found from the South China Sea, including waters around Singapore and Indonesia, northward to Taiwan. Its range extends westward into the Indian Ocean, where it has been recorded in the Andaman Sea off Thailand, throughout the Bay of Bengal, and along the coasts of India and Sri Lanka.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Taxonomy. &quot;Bertya polystigma&quot; was first formally described in 1913 by Georg Grüning in Engler's &quot;Das Pflanzenreich&quot; from specimens collected by Ludwig Diels on Walshs Pyramid. Distribution and habitat. This species of &quot;Bertya&quot; grows in woodland or forest between the Windsor Tablelands and Ravenshoe in north Queensland. Conservation status.

Geographic entities mentioned:
surface_form: Walshs Pyramid
instance_of: Mountain
countries: Australia
coordinates: lat: -17.130025
lon: 145.80065555556
Verf Kill. Verf Kill flows into the Mohawk River near Pattersonville, New York. Verf Kill is a name derived from Dutch meaning &quot;paint creek&quot;.

Geographic entities mentioned:
surface_form: verf kill
instance_of: Watercourse
countries: United States
coordinates: lat: 42.88583333
lon: -74.05333333
Forrest designed the Mendenhall Glacier Visitor Center, the Juneau Federal Building and, with Harold B. Foss, the nearby Chapel by the Lake. He designed the Elvey Building and the Ernest N. Patty Gymnasium (1963) at the University of Alaska, Fairbanks. Forrest came to Alaska after working in the 1930s in Oregon, where he was the lead exterior designer of Timberline Lodge on Mount Hood.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Description. A lake covered the region during the Pliocene epoch, which was gradually filled with sediments, and the surface of the basin is very flat. Slow-moving tributaries of the Congo, including the Lopori, Maringa, Ikelemba, Tshuapa, Lomela and Lokoro, drain westward. The region lies on the equator, where the climate is tropical and humid. Rainfall averages 2,000 mm annually.

Geographic entities mentioned:
surface_form: Lopori
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.236166
lon: 19.811654
surface_form: Maringa
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 1.228572
lon: 19.817963
surface_form: Ikelemba
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 0.11138888888889
lon: 18.273611111111
surface_form: Lomela
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -2.3
lon: 23.28
Despite several rumors in the Midwest being debunked, rumors circulated on internet forums in Cache Valley, Utah, about litter boxes being placed in Sky View High School, which schools officials could not corroborate.

Geographic entities mentioned:
surface_form: Cache Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.816666666667
lon: -111.93416666667
Since 1 January 2014 it has been part of the Black Forest National Park. The tarn lies around 4.5 kilometres southeast of the summit of the Schliffkopf in the Buhlbach valley and less than half a kilometre northeast of the Black Forest High Road. The lake can be reached on foot over various paths including from Kniebis, Baiersbronn-Obertal or from the Black Forest High Road.

Geographic entities mentioned:
surface_form: Schliffkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 48.535277777778
lon: 8.2152777777778
The tarn lies around 4.5 kilometres southeast of the summit of the Schliffkopf in the Buhlbach valley and less than half a kilometre northeast of the Black Forest High Road. The lake can be reached on foot over various paths including from Kniebis, Baiersbronn-Obertal or from the Black Forest High Road. The tarn is about 160 metres wide and almost circular in shape.

Geographic entities mentioned:
surface_form: Kniebis
instance_of: Mountain
countries: Germany
coordinates: lat: 48.476388888889
lon: 8.2938888888889
Buhlbachsee. The Buhlbachsee is a tarn (lake) in the northern Black Forest on the southwestern edge of the parish of Baiersbronn in the county of Freudenstadt in Baden-Württemberg. Since 1 January 2014 it has been part of the Black Forest National Park.

Geographic entities mentioned:
surface_form: buhlbachsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.500722222222
lon: 8.2446111111111
There is an island in the lake, about 0.7 hectares in area, which is covered in birch trees. Like all tarns the Buhlbachsee was formed by a glacier. After the last ice age, which ended in the Black Forest about 10,000 years ago, it was left behind.

Geographic entities mentioned:
surface_form: buhlbachsee
instance_of: Lake
countries: Germany
coordinates: lat: 48.500722222222
lon: 8.2446111111111
Veliki kabao. 53wgzls3sj9jfknrhdvmkm5o5gm" xml:space="preserve">#REDIRECT Veliki Kabao

Geographic entities mentioned:
surface_form: veliki kabao
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.56972222
lon: 18.54333333
Black Reef. Black Reef, el., is a small mountain range west of Augusta, Montana in Lewis and Clark County, Montana.

Geographic entities mentioned:
surface_form: black reef
instance_of: Landform
countries: United States
coordinates: lat: 47.5914
lon: -112.854
Wilson Gap. Wilson Gap, originally known as Gregory's Gap, is a wind gap in the Blue Ridge Mountain, located on the border of Loudoun County, Virginia and Jefferson County, West Virginia. The Appalachian Trail crosses the gap.

Geographic entities mentioned:
surface_form: Blue Ridge Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.08166667
lon: -77.86222222
Seti I ruled from to. Layout and construction. The Osireion is part of the Temple of Seti I's complex. It may have been built to resemble the tombs in the Valley of the Kings. It is located centrally behind the main part of the Temple of Seti I along an east west axis. Most of its structure would have been subterranean.

Geographic entities mentioned:
surface_form: Valley of the Kings
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358
Both are cultural sites, as determined by the organisation's selection criteria. There are two other UNESCO World Heritage Sites in Ireland, both of these being in Northern Ireland. They are the Giant's Causeway and Gracehill Moravian Settlement, both in County Antrim. __TOC__
World Heritage Sites. UNESCO lists sites under ten criteria; each entry must meet at least one of the criteria.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
British imperial officials considered the name after noting that Quebec City was the capital of Quebec, and hence Toronto should be the capital of a similarly named province. The idea had little traction and was dismissed in favour of using the same name for the province as the lake adjacent to its capital city, Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The total area of the city is. Geography. Nobeoka is located in northern Miyazaki Prefecture. It is bordered by the Hyūga Sea to the east and is surrounded by the Kyushu Mountains to the north, west and south. Many rivers flow through the city, the largest of which is the Gokase River.

Geographic entities mentioned:
surface_form: Hyūga Sea
instance_of: Body of water
countries: Japan
coordinates: lat: 32
lon: 132
Graham Lakes (Minnesota). The Graham Lakes are a pair of lakes located in the northeastern corner of Nobles County, Minnesota. The lakes are known as West Graham Lake and East Graham Lake. West Graham Lake is an oval shaped body of water that extends east-to-west slightly more than one mile (1.6 km). The north-to-south width of the lake is approximately 3/4 of a mile.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Graham Lakes (Minnesota). The Graham Lakes are a pair of lakes located in the northeastern corner of Nobles County, Minnesota. The lakes are known as West Graham Lake and East Graham Lake. West Graham Lake is an oval shaped body of water that extends east-to-west slightly more than one mile (1.6 km). The north-to-south width of the lake is approximately 3/4 of a mile.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
The lakes are known as West Graham Lake and East Graham Lake. West Graham Lake is an oval shaped body of water that extends east-to-west slightly more than one mile (1.6 km). The north-to-south width of the lake is approximately 3/4 of a mile. The area of West Graham Lake is, the average depth is, and the maximum depth is. The elevation of West Graham Lake is, or 438.52 meters.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
The north-to-south width of the lake is approximately 3/4 of a mile. The area of West Graham Lake is, the average depth is, and the maximum depth is. The elevation of West Graham Lake is, or 438.52 meters. East Graham Lake is a longer, narrower lake that extends from northeast-to-southwest for 1 miles. Its width is less than 1/2 mile.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
The area of West Graham Lake is, the average depth is, and the maximum depth is. The elevation of West Graham Lake is, or 438.52 meters. East Graham Lake is a longer, narrower lake that extends from northeast-to-southwest for 1 miles. Its width is less than 1/2 mile. The area of East Graham Lake is, the average depth is, and the maximum depth is.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
The elevation of West Graham Lake is, or 438.52 meters. East Graham Lake is a longer, narrower lake that extends from northeast-to-southwest for 1 miles. Its width is less than 1/2 mile. The area of East Graham Lake is, the average depth is, and the maximum depth is. The elevation of East Graham Lake is, or 437.41 meters. A small creek runs from West Graham Lake and empties into East Graham Lake.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Its width is less than 1/2 mile. The area of East Graham Lake is, the average depth is, and the maximum depth is. The elevation of East Graham Lake is, or 437.41 meters. A small creek runs from West Graham Lake and empties into East Graham Lake. Another creek runs from East Graham Lake, and eventually flows into the Des Moines River. History.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Its width is less than 1/2 mile. The area of East Graham Lake is, the average depth is, and the maximum depth is. The elevation of East Graham Lake is, or 437.41 meters. A small creek runs from West Graham Lake and empties into East Graham Lake. Another creek runs from East Graham Lake, and eventually flows into the Des Moines River. History.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
The elevation of East Graham Lake is, or 437.41 meters. A small creek runs from West Graham Lake and empties into East Graham Lake. Another creek runs from East Graham Lake, and eventually flows into the Des Moines River. History. In the month of May, 1867, a pioneer named Stephen Muck pushed out into the unsettled Graham Lakes region and squatted on land on the bank of West Graham Lake.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Another creek runs from East Graham Lake, and eventually flows into the Des Moines River. History. In the month of May, 1867, a pioneer named Stephen Muck pushed out into the unsettled Graham Lakes region and squatted on land on the bank of West Graham Lake. When surveyed, this land proved to be on section 22 of Graham Lakes Township.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
Stephen Muck was the first permanent resident of Nobles County. The first town to appear on any map of Nobles County was a curious place called Gretchtown. According to an 1856 map - a map drawn 11 years before the arrival of Stephen Muck - Gretchtown was located on the south bank of West Graham Lake, very near to Muck's claim.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Neither town grew beyond a few hundred residents. Thus, the Graham Lakes region has remained entirely rural, and the lake shores of both East Graham Lake and West Graham Lake remain undeveloped. These lakes were first noted on Joseph Nicollet's 1842 map based upon his explorations of the late 1830s and early 1840s. Nicollet named the lakes after Joseph Duncan Graham.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
A population assessment was conducted during the week of June 4, 2007 using 3 gill nets and 8 trap nets. Black Crappies ranged from to, and their numbers were the highest since sampling of the lake has been conducted. Northern Pike ranged from to. Walleye were also abundant, and 59% of those sampled were or greater. Most fish from East Graham Lake are safe to eat.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
A population assessment conducted on June 4, 2007 found that walleye range from 6.9 to in length. Black crappies range from to. The average black crappie swimming in West Graham Lake is thought to be nearly 1/2 pound. Channel catfish average. There are no advisories for consumption of fish from West Graham Lake. Public Access.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Black crappies range from to. The average black crappie swimming in West Graham Lake is thought to be nearly 1/2 pound. Channel catfish average. There are no advisories for consumption of fish from West Graham Lake. Public Access. Fury Island and Maka-Oicu County Parks are located on East and West Graham Lakes.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Public Access. Fury Island and Maka-Oicu County Parks are located on East and West Graham Lakes. Maka-Oicu County Park is located on the northeast shore of West Graham Lake and provides for camping, lake access, natural areas, swimming beach, picnic areas, historic site and general park activities. The park has on-site showers, a large picnic shelter for reunions and gatherings.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Maka-Oicu Park consists of of developed land. Fury's Island County Park is located on the west side of East Graham Lake, and provides for camping, natural areas, lake access, showers, a large picnic shelter for gatherings, and also has a playground for the little ones. Fury's Island Park is one mile (1.6 km) south of Maka-Oicu County Park and consists of of developed land.

Geographic entities mentioned:
surface_form: graham lake
instance_of: Lake
countries: United States
coordinates: lat: 44.6584
lon: -68.3992
Graham Lakes (Minnesota). The Graham Lakes are a pair of lakes located in the northeastern corner of Nobles County, Minnesota. The lakes are known as West Graham Lake and East Graham Lake. West Graham Lake is an oval shaped body of water that extends east-to-west slightly more than one mile (1.6 km). The north-to-south width of the lake is approximately 3/4 of a mile.

Geographic entities mentioned:
surface_form: graham lakes (minnesota)
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
Graham Lakes (Minnesota). The Graham Lakes are a pair of lakes located in the northeastern corner of Nobles County, Minnesota. The lakes are known as West Graham Lake and East Graham Lake. West Graham Lake is an oval shaped body of water that extends east-to-west slightly more than one mile (1.6 km). The north-to-south width of the lake is approximately 3/4 of a mile.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
History. In the month of May, 1867, a pioneer named Stephen Muck pushed out into the unsettled Graham Lakes region and squatted on land on the bank of West Graham Lake. When surveyed, this land proved to be on section 22 of Graham Lakes Township. There he built a log structure from timber growing near the lake, the first house of wood in the county.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
When Nobles County was formally created by the Minnesota legislature on May 23, 1857, Gretchtown was briefly designated as the county seat of Nobles County, an imaginary county seat for a county that, at that time, had no residents. When a route for the St. Paul and Sioux City Railway was surveyed in 1871, it was located far south of the Graham Lakes region.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
When a route for the St. Paul and Sioux City Railway was surveyed in 1871, it was located far south of the Graham Lakes region. No towns or villages existed in Graham Lakes Township until 1879 when Kinbrae and Dundee were established. Neither town grew beyond a few hundred residents.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
Nicollet named the lakes after Joseph Duncan Graham. Graham served as a commissioner for the survey of the northeast segment of the boundary between the United States and Canada from 1840 until 1843. Fishing. Graham Lakes are known as exceptionally good fishing lakes. East Graham is managed primarily for walleye and northern pike and secondarily for black crappie and yellow perch.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
Channel catfish average. There are no advisories for consumption of fish from West Graham Lake. Public Access. Fury Island and Maka-Oicu County Parks are located on East and West Graham Lakes. Maka-Oicu County Park is located on the northeast shore of West Graham Lake and provides for camping, lake access, natural areas, swimming beach, picnic areas, historic site and general park activities.

Geographic entities mentioned:
surface_form: graham lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 43.7931
lon: -95.5086
Ventura volcanic field. Ventura volcanic field is an extinct volcanic field located in the Mexican state of San Luis Potosí, its name is due to the town and railway crossing of the same name, which had its last activity in the Pleistocene, this volcanic field is known more for the volcanic crater known as La Joya Honda, which is currently a tourist site in San Luis Potosí.

Geographic entities mentioned:
surface_form: ventura volcanic field
instance_of: Mountain
countries: Mexico
coordinates: lat: 22.364379
lon: -100.764902
state of Nevada. The GNIS classifies it as a populated place. History. Located near Mount Tenabo, Cortez first attracted attention in 1862, when Mexican miners transported silver ore from the site to stamp mills in Austin, south. In the spring of 1863, a group of eight miners exploring the area, came across Native Americans collecting silver in gulleys southwest of the Mount Tenabo mountains.

Geographic entities mentioned:
surface_form: Mount Tenabo
instance_of: Mountain
countries: United States
coordinates: lat: 40.162977777778
lon: -116.58480555556
Geography. According to the United States Census Bureau, the city has a total area of, of which, is land and is water. The majority of Meridian lies on a flat plain, roughly in the north central part of Treasure Valley. There is a low bench along the south east edge of the city. The city is crossed by several irrigation canals that generally run from the south east to the north west.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933