Sarmila/GeoWiki-Features huggingface dataset:
Territorial extent and municipalities. Upper Mantua is bounded to the west and east by the Chiese and Mincio rivers respectively, to the north by the morainic hills of Lake Garda, while its southern borders are marked by the mid-Mantuan plain crossed by the Via Postumia.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Several minor watercourses are located between the Oglio and the Mincio, whose origin is due to the confluence of resurgence waters, which contribute with their deposits to the landscape of the river valleys. In the area corresponding to the town of Castel Goffredo there are numerous resurgences. The climate of Upper Mantua is the one typical of the Po Valley. History.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
For much of the Lombard and Frankish ages Upper Mantua was accorded a degree of independence: much of it was included in a minor district practically autonomous from neighboring duchies, centered on Lake Garda and reporting to the Benacense town of Sirmione.

Geographic entities mentioned:
surface_form: Lake Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Society. Upper Mantua has experienced good industrial development in recent decades, but it still retains many traces of the rural life to which it remained attached until not so long ago. Today in the area, as now in many others in Italy and especially in the Po Valley, society has become multiethnic, with a significant presence of foreign citizens. Demographic development.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
UNESCO World Heritage Sites. The Bronze Age pile-dwelling stations of Castellaro Lagusello and Bande di Cavriana were inscribed in the year 2011 in the list of UNESCO World Heritage Sites among the ancient alpine settlements. These are a type of Bronze Age settlements located in wet environments, such as lake, marsh or river areas (Garda littoral and alpine or intermoraine basins).

Geographic entities mentioned:
surface_form: Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Cuisine. Broadly speaking, the typical food products of the Upper Mantuan area do not differ from those of the entire Po Valley. More specifically, the local gastronomy is the result of the combination of the culinary art of Mantua, appreciated all over the world, and the more genuine traditions of the morainic hill area. Anthropogenic geography.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1958–59) for James Paton, a seaman who made at least six voyages to the Ross Sea area. He first served on the Morning, relief ship of the &quot;Discovery&quot; expedition (1901–04), and made the first landing on the island by walking to it against orders, over sea ice from the ship.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: morning
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
Paton Peak. Paton Peak () is the highest point, at 740 m, on Beaufort Island, in the Ross Archipelago. Named by the New Zealand Geological Survey Antarctic Expedition (NZGSAE) (1958–59) for James Paton, a seaman who made at least six voyages to the Ross Sea area.

Geographic entities mentioned:
surface_form: paton peak
instance_of: Mountain
coordinates: lat: -76.95
lon: 166.95
Selemnos. Selemnos (Ancient Greek: Σέλεμνος,) is a river in the northern part of Achaea, Greece. The river flows entirely in the municipal unit of Rio and empties into the Gulf of Corinth. Geography. The river begins on the northwest side of the Panachaiko mountain. It passes along the villages Ano Kastritsi and Kato Kastritsi. It empties into the Gulf of Corinth, east of the Rio-Antirrio bridge.

Geographic entities mentioned:
surface_form: Panachaiko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.2025
lon: 21.868888888889
Maoke plate. The Maoke plate is a small tectonic plate located in western New Guinea underlying the Sudirman Range from which the highest mountain on the island- Puncak Jaya rises.

Geographic entities mentioned:
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
Only one species is known, &quot;G. brancai&quot;, named in honor of German paleontologist Wilhelm von Branca, who was a driving force behind the expedition that discovered it in the Tendaguru Formation.

Geographic entities mentioned:
surface_form: Tendaguru Formation
instance_of: Mountain
countries: Tanzania
coordinates: lat: -10.05
lon: 39.11666667
Some scientists have proposed that large dinosaurs like &quot;Giraffatitan&quot; were gigantotherms. Internal organs of these giant sauropods were probably enormous. Paleoenvironment. &quot;Giraffatitan&quot; lived in what is now Tanzania in the Late Jurassic Tendaguru Formation. Since 2012, the boundary between the Kimmeridgian and Tithonian is dated at 152.1 million years ago.

Geographic entities mentioned:
surface_form: Tendaguru Formation
instance_of: Mountain
countries: Tanzania
coordinates: lat: -10.05
lon: 39.11666667
was a professor and dean at Harris-Stowe State University there. Her husband died in 1970. She lived with her son and his family in Los Angeles in her last years, and died in 1973, aged 75 years, in Culver City, California. In 2021, Portia Spennie Blackiston was among the suffragists of color featured in the Champlain Valley Suffrage Centennial Auto Tour, and the tour's accompanying booklet.

Geographic entities mentioned:
surface_form: Champlain Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
McLennon breaks into his loft apartment (above the saloon which he had owned) and attempts to kill Sarah for turning on him, but Santeek appears behind McLennon and plunges a dagger into his back. Production. Although set in the U.S. state of Alaska, the movie was shot entirely in Norway in Maridalen, Møsvatn, and Orre bach.

Geographic entities mentioned:
surface_form: Møsvatn
instance_of: Lake
countries: Norway
coordinates: lat: 59.866666666667
lon: 8.0833333333333
Sand Point, Seattle. Sand Point is a neighborhood in Seattle, Washington, United States, named after and consisting mostly of the Sand Point peninsula that juts into Lake Washington, which is itself largely given over to Magnuson Park. Its southern boundary can be said to be N.E. 65th Street, beyond which are Windermere and Hawthorne Hills; its northern boundary, N.E.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
The star HD 224693 is named Axólotl. The name was selected in the NameExoWorlds campaign by Mexico, during the 100th anniversary of the IAU. &quot;Axólotl&quot; means &quot;water animal&quot; in the native Nahuatl language and an axolotl is also a species of salamander endemic to the valley of Mexico. This is an ordinary G-type main-sequence star with a stellar classification of G2V.

Geographic entities mentioned:
surface_form: valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
From Kingston Railway Bridge the limits clockwise were: the middle of the River Thames north-east to Hammersmith Bridge and then southeast within Barnes to Barn Elms; the outer limit of Putney Common; the houses east of Hallam Road and Dyers Lane; Upper Richmond Road westwards; the Beverley Brook south to Richmond Park itself; the park walls to Robin Hood Gate on the A3 road; the Beverley Brook south, west across Malden Golf Course; Coombe Road; Coombe Vale both in New Malden; the South West Main Line west of New Malden station; the Kingston branch back to the stated start.

Geographic entities mentioned:
surface_form: Beverley Brook
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.4718
lon: -0.223
surface_form: Beverley Brook
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 51.4718
lon: -0.223
Haddon Corner is also located in the Channel Country. The Channel Country is the location for a majority of Min Min light sightings. It is also home to at least two important bird areas, Lake Yamma Yamma and the Lake Machattie Area. The Channel Country features an arid landscape with a series of ancient flood plains from rivers which only flow intermittently.

Geographic entities mentioned:
surface_form: Lake Yamma Yamma
instance_of: Lake
countries: Australia
coordinates: lat: -26.2778
lon: 141.459
surface_form: Lake Machattie Area
instance_of: Lake
countries: Australia
coordinates: lat: -24.8236
lon: 139.564
The Channel Country features an arid landscape with a series of ancient flood plains from rivers which only flow intermittently. The principal rivers are Georgina River, Cooper Creek and the Diamantina River. When there is sufficient rainfall in their catchment area these rivers flow into Lake Eyre, South Australia. In most years the flood waters are absorbed into the earth or evaporate, however.

Geographic entities mentioned:
surface_form: Lake Eyre
instance_of: Lake
countries: Australia
coordinates: lat: -28.406
lon: 137.2963
Black Diamond Coal Mining Company. The Black Diamond Coal Mining Company was formed in 1861, consolidating the Cumberland and Black Diamond coal mines in the region of Mount Diablo, in Contra Costa County, California. During its years of operation as a mining company, it established three towns: Nortonville, California, Southport, Oregon, and Black Diamond, Washington.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
New York Landing was renamed Black Diamond Landing, in recognition of the company. Black Diamond also opened a wharf at Port Costa, California. The company town of Nortonville was the largest of the coal towns around Mount Diablo, with a population of over 900. It was named for Noah Norton, who originally opened the Black Diamond mine and built the first two houses there.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Chattahoochee RiverWalk. The Chattahoochee RiverWalk is a 22-mile walking and biking area along the Chattahoochee River in Columbus, Georgia, United States. The trail is paved with asphalt, concrete, or brick. Due to the RiverWalk bike path, Columbus has been listed by the League of American Bicyclists as one of the forty most Bicycle Friendly Communities in the United States. History.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
The 14th Street bridge is also slated for major renovations to be completed in 2011. The Chattahoochee RiverWalk also connects to the Phenix City RiverWalk at the 14th Street Bridge. The Phenix City RiverWalk extends from the Dillingham Street bridge to the 14th Street bridge, but it will extend up to the City Mills Dam on the Alabama side of the Chattahoochee River. Sights.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Lake Gibson is not a natural feature, but rather an artificially created reservoir. Township maps from the latter half of the 19th century show a meandering stream flowing through this area (Beaverdams Creek) and plunging over the Niagara Escarpment at Decew Falls. This is the site of Morningstar Mill (still in existence today) which used this stream for power.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
The landscape was further altered with various channels and canals to improve flow to the generating station, and with the creation of additional reservoirs. Lake Gibson receives almost all of its water supply from Lake Erie via the Welland Canal. This reservoir also serves as the domestic water supply for the City of St Catharines.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Among these was a sawmill and a grist mill on Twelve Mile Creek owned by William Hamilton Merritt. Merritt's mills were plagued by low water conditions, especially in late summer - exactly when the grain harvest needed to be ground. He conceived of an idea to divert water from the Welland River to augment the water supply.

Geographic entities mentioned:
surface_form: Welland River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.0377
lon: -79.1798
In spite of initial plans, the water source for the canal was initially the Grand River via the Feeder Canal, as opposed to the Welland River. The modern canal receives its water directly from Lake Erie. Twelve Mile Creek was not necessarily the best route for the canal, but it was the location of Merritt's mills, so economic motivation became a factor.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Copadichromis atripinnis. &quot;Copadichromis atripinnis&quot; is a species of fish in the family Cichlidae. It is endemic to Lake Malawi in Malawi. Its natural habitat is freshwater lakes.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The many cliff-like layers on the south-western approach to the Hermannskogel clearly show the hill's geological make-up. The Kahlenberg and Leopoldsberg, behind which lie the Wiener Pforte, where the Danube breaks through the Wienerwald, are three kilometres to the east of the Hermannskogel. The Vogelsangberg stands nearby, as does the Dreimarkstein (to the southwest). History.

Geographic entities mentioned:
surface_form: Kahlenberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2761
lon: 16.3333
surface_form: Leopoldsberg
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2789
lon: 16.3453
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
In the Middle Ages, the Hermannskogel was covered in vineyards. On the side of the hill, in a depression between Sievering and Weidling, is the probable former site of the village Kogelbrunn, which lived from viticulture and which is mentioned for the first time in a document from 1237 as &quot;chogelbrunne&quot;. In 1256, Albero von Feldsberg accorded the village to the Klosterneuburg Monastery.

Geographic entities mentioned:
surface_form: kogelbrunn
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
Hermannskogel. The Hermannskogel () is a hill in Döbling, the 19th district of Vienna. At 542 metres above sea level, it is the highest natural point of Vienna. It lies on the border to Lower Austria. The Habsburgwarte, standing atop the Hermannskogel, marked the kilometre zero in cartographic measurements used in Austria-Hungary until 1918. Geography.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
The Hermannskogel () is a hill in Döbling, the 19th district of Vienna. At 542 metres above sea level, it is the highest natural point of Vienna. It lies on the border to Lower Austria. The Habsburgwarte, standing atop the Hermannskogel, marked the kilometre zero in cartographic measurements used in Austria-Hungary until 1918. Geography. The Hermannskogel is a forested ridge in the Wienerwald.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
The Habsburgwarte, standing atop the Hermannskogel, marked the kilometre zero in cartographic measurements used in Austria-Hungary until 1918. Geography. The Hermannskogel is a forested ridge in the Wienerwald. It is both the highest point in the Kahlengebirge and in the city of Vienna. The Hermannskogel is part of a north-eastern chain of foothills belonging to the eastern Alps.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
Geography. The Hermannskogel is a forested ridge in the Wienerwald. It is both the highest point in the Kahlengebirge and in the city of Vienna. The Hermannskogel is part of a north-eastern chain of foothills belonging to the eastern Alps. It is composed of flysch containing quartz, limestone, marl, and other conglomerates.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
It is composed of flysch containing quartz, limestone, marl, and other conglomerates. The many cliff-like layers on the south-western approach to the Hermannskogel clearly show the hill's geological make-up. The Kahlenberg and Leopoldsberg, behind which lie the Wiener Pforte, where the Danube breaks through the Wienerwald, are three kilometres to the east of the Hermannskogel.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
The Vogelsangberg stands nearby, as does the Dreimarkstein (to the southwest). History. The first documentary reference to the Hermannskogel can be found in the Klosterneuburg Monastery’s tithe register. It dates from 1355 and names the hill &quot;hermannschobel&quot;.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
In 1346, it was still inhabited, but it was destroyed at the end of the 15th century, probably a victim of Magyar raids. The village's demise also spelt the end of the vineyards and the Hermannskogel was reclaimed by woods. The relief army summoned from the Kingdom of Saxony and other parts of the empire that lifted the second siege of Vienna camped here in 1683.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
The village's demise also spelt the end of the vineyards and the Hermannskogel was reclaimed by woods. The relief army summoned from the Kingdom of Saxony and other parts of the empire that lifted the second siege of Vienna camped here in 1683. In the 19th century, several requests made by the Klosterneuburg Monastery to erect a watchtower on the Hermannskogel were turned down.

Geographic entities mentioned:
surface_form: hermannskogel
instance_of: Mountain
countries: Austria
coordinates: lat: 48.2707124
lon: 16.2945789
At three in the afternoon the restoration forces, plus half of the flankers and two companies under the command of Generals Ramón Castilla and Remigio Deustua (father of the Peruvian philosopher Alejandro Deustua) halted in front of the Portada de Guías. The restorative army supported its right on the Rímac river and its left on the Amancaes hill.

Geographic entities mentioned:
surface_form: Rímac river
instance_of: Watercourse
countries: Peru
coordinates: lat: -12.032222222222
lon: -77.141111111111
History and etymology. Like Kjölur and Kaldidalur, Sprengisandur is an ancient pass - during the time of the Icelandic Free State (ca. 930–1265) it was one of the several important north–south routes that connected remote regions of the island to the Plains of the Parliament, Þingvellir, where the yearly parliament, Alþingi, was held each year at midsummer.

Geographic entities mentioned:
surface_form: Kjölur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.7
lon: -19.4
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
Another example is in Ölkofra þáttr, where the chieftain Broddi, who lives in Vopnafjörður, returns home from Alþingi by taking the Kjölur route north and then going east along the northern shore of the island - a much longer road home than one through Sprengisandur, yet one going largely through inhabited regions.

Geographic entities mentioned:
surface_form: Kjölur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.7
lon: -19.4
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
The modern gravel road goes more or less parallel and a bit southeast of the ancient horse trail. A tourist bus runs over the Sprengisandur every other day from Landmannalaugar to Mývatn and back in July and August. If the weather is good, the route offers views of both glaciers and volcanoes Askja and Herðubreið.

Geographic entities mentioned:
surface_form: Mývatn
instance_of: Lake
countries: Iceland
coordinates: lat: 65.6
lon: -17
A tourist bus runs over the Sprengisandur every other day from Landmannalaugar to Mývatn and back in July and August. If the weather is good, the route offers views of both glaciers and volcanoes Askja and Herðubreið. In the middle of the track there is a hut of the Icelandic Hiking Club, &quot;Nýidalur&quot;. Transport.

Geographic entities mentioned:
surface_form: Herðubreið
instance_of: Mountain
countries: Iceland
coordinates: lat: 65.183333333333
lon: -16.35
Sprengisandur. Sprengisandur () is a highland plateau in Iceland, defined roughly as the area between the Hofsjökull and Vatnajökull glaciers. History and etymology. Like Kjölur and Kaldidalur, Sprengisandur is an ancient pass - during the time of the Icelandic Free State (ca.

Geographic entities mentioned:
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
One example is in ch. 8 of the Hrafnkels saga: the chieftain Hrafnkell, who lived in the East Fjords and rather close to the northern end of Sprengisandur, prefers to travel to the Alþingi by going south along the shore of the island - his route is much longer and slower, but it goes through inhabited regions for the entire route.

Geographic entities mentioned:
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
His enemies, living in the same neighbourhood but needing speed, decide to take the shorter yet more exhausting Sprengisandur route, so as to arrive at the Alþingi much earlier and have enough time to drum up some support for their case.

Geographic entities mentioned:
surface_form: sprengisandur
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.86666667
lon: -18.11666667
Pakistan. Pakistan has built hard and deeply buried storage and launch facilities to retain a second strike capability in a nuclear war. North Korea. North Korea built a missile silo complex south of Paektu Mountain. The silos are reportedly designed for mid- to long-range missiles, but it is not clear if all of them are operational. Iran.

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
Career. Born in Iran, brought up in the Mount Damavand area, and educated at Alborz High School in Tehran, Moayedi came to the UK in the 1958 and studied at Bradford University before becoming a site engineer at a business which was subsequently acquired by Amec. In 1983 he joined &quot;Walter Lawrence&quot;, a housebuilder, where he was appointed to establish a new division.

Geographic entities mentioned:
surface_form: Mount Damavand
instance_of: Mountain
countries: Iran
coordinates: lat: 35.955277777778
lon: 52.109166666667
The land depression likely intensified due to moisture received from the Arabian Sea and the soil soaked by previous rains. A low-pressure system formed in the northwest Bay of Bengal near West Bengal and Bangladesh on 16 August. On 24 August, a well-marked low-pressure system formed over Madhya and Uttar Pradesh.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
From then onwards, the Seehandlung gradually withdrew from its trading business. Trade in wine, flour and wool was maintained for a long time, however, and the Seehandlung also retained other commercial ventures, such as some textile factories and metalworking companies. It also continued to operate the steamboat service on the rivers Spree, Havel and Elbe. From 1904 the institute traded as.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Pihanga. Pihanga is a andesitic volcanic peak in the North Island Volcanic Plateau, located to the north of Mount Tongariro, between Tongariro and Lake Taupō. The nearest town to Pihanga is Tūrangi. Lake Rotoaira lies to the south-west of Pihanga, and the smaller Lake Rotopounamu is situated on the south-western flank of the volcano, near Te Ponanga Saddle.

Geographic entities mentioned:
surface_form: Mount Tongariro
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.12972222222222
lon: 175.63583333333332
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
The nearest town to Pihanga is Tūrangi. Lake Rotoaira lies to the south-west of Pihanga, and the smaller Lake Rotopounamu is situated on the south-western flank of the volcano, near Te Ponanga Saddle. Across the saddle to the west is the volcanic peak of Tihia. Pihanga and Lake Rotopounamu are part of the 5,129ha Pihanga Scenic Reserve, which in 1975 was added to the Tongariro National Park.

Geographic entities mentioned:
surface_form: Lake Rotoaira
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.0545
lon: 175.7143
surface_form: Lake Rotopounamu
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.027
lon: 175.738
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
The nearest town to Pihanga is Tūrangi. Lake Rotoaira lies to the south-west of Pihanga, and the smaller Lake Rotopounamu is situated on the south-western flank of the volcano, near Te Ponanga Saddle. Across the saddle to the west is the volcanic peak of Tihia. Pihanga and Lake Rotopounamu are part of the 5,129ha Pihanga Scenic Reserve, which in 1975 was added to the Tongariro National Park.

Geographic entities mentioned:
surface_form: Tihia
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.98888888888889
lon: 175.70833333333331
Pihanga. Pihanga is a andesitic volcanic peak in the North Island Volcanic Plateau, located to the north of Mount Tongariro, between Tongariro and Lake Taupō. The nearest town to Pihanga is Tūrangi. Lake Rotoaira lies to the south-west of Pihanga, and the smaller Lake Rotopounamu is situated on the south-western flank of the volcano, near Te Ponanga Saddle.

Geographic entities mentioned:
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
Across the saddle to the west is the volcanic peak of Tihia. Pihanga and Lake Rotopounamu are part of the 5,129ha Pihanga Scenic Reserve, which in 1975 was added to the Tongariro National Park. Pihanga appears to have a large crater, but this is in fact the result of erosion, and the &quot;crater&quot; quickly narrows into a steep gorge. Geology.

Geographic entities mentioned:
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
Across the saddle to the west is the volcanic peak of Tihia. Pihanga and Lake Rotopounamu are part of the 5,129ha Pihanga Scenic Reserve, which in 1975 was added to the Tongariro National Park. Pihanga appears to have a large crater, but this is in fact the result of erosion, and the &quot;crater&quot; quickly narrows into a steep gorge. Geology.

Geographic entities mentioned:
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
Pihanga appears to have a large crater, but this is in fact the result of erosion, and the &quot;crater&quot; quickly narrows into a steep gorge. Geology. Eruptions from Pihanga last occurred more than 20,000 years ago. An age of 123 ± 10 ka has been challenged and potentially redating suggests first formation greater than 180,000 years ago.

Geographic entities mentioned:
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
The Keepers of the Wai. In Māori custom, the Pihanga Maunga became the responsibility of the Matapuna people (a mix of Tuwharetoa, Tama Kopiri/Upper Whanganui whanau/Tu Hope - Descendants of Te Rere Ao, the First of Tuwharetoa) of the Tuwharetoa people, who have traditionally been the keepers of the wai (Keepers of the Water) and Maunga Kaitiaki (Protectors of the Mountain).

Geographic entities mentioned:
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
surface_form: pihanga
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.041333
lon: 175.768694
It is located downstream from Moul Falls and upstream from Grouse Creek's confluence with the Clearwater River. Grouse Creek rises from snowmelt, a lake and springs at a pass between Trophy Mountain and Table Mountain. It flows west before tumbling over Moul Falls and McDiarmid Falls. The creek drops a total of in its last as it has eroded into the escarpment of a volcanic plateau. Naming.

Geographic entities mentioned:
surface_form: Trophy Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7997
lon: -119.876
In response to the attack on his clansmen, Archibald Campbell, 1st Marquess of Argyll assembled the Campbell clansmen to repel the invaders. Montrose, finding himself trapped in the Great Glen between Argyll and Covenanters advancing from Inverness, decided on a flanking march through the wintry mountains of Lochaber and surprised Argyll at the Battle of Inverlochy (2 February 1645).

Geographic entities mentioned:
surface_form: Great Glen
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
Krakeel River. Krakeel River is a town in Sarah Baartman District Municipality in the Eastern Cape province of South Africa. Village in the Langkloof, east of Avontuur and some 200 km from Port Elizabeth. The name is taken from that of the river. The form Krakeelrivier is preferred for official purposes.

Geographic entities mentioned:
surface_form: Langkloof
instance_of: Valley
countries: South Africa
coordinates: lat: -33.825
lon: 23.857777777778
Eagle Island Camp. Eagle Island Camp, also known as Camp Eagle Island or simply EIC, is a youth summer camp and former Girl Scout camp in Franklin County, New York, located on Eagle Island on Upper Saranac Lake in New York's Adirondack region. The site is listed on the National Register of Historic Places. Adirondack Great Camp years.

Geographic entities mentioned:
surface_form: Upper Saranac Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2925
lon: -74.325555555556
Buena Vista Oil Field. 3potcvhq3529wxr742uozpj12lmmc" xml:space="preserve">The Buena Vista Oil Field, formerly the Naval Petroleum Reserve No. 2 (NPR-2'&quot;) is a large oil field in Kern County, San Joaquin Valley, California in the United States. Discovered in 1909, and having a cumulative production of approximately, it is the tenth-largest oil field in California as of 2024.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The terrain is mostly rugged dissected upland, some vegetation in the west, but somewhat barren in the east. The elevation span between the shoreline of the Dead Sea at −408 m to the highest point at Mount Nabi Yunis, at 1,030 m (3,379 ft) above sea level. The West Bank is landlocked; its highlands are the main recharge area for Israel's coastal aquifers.

Geographic entities mentioned:
surface_form: Mount Nabi Yunis
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 31.57944444
lon: 35.105
Area B, 25.2%, adds other populated rural areas, many closer to the center of the West Bank. Area C contains all the Israeli settlements (excluding settlements in East Jerusalem), roads used to access the settlements, buffer zones (near settlements, roads, strategic areas, and Israel), and almost all of the Jordan Valley and the Judean Desert.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Israeli administrative districts. The West Bank is further divided into 8 administrative regions: Menashe (Jenin area), HaBik'a (Jordan Valley), Shomron (Shechem area, known in Arabic as Nablus), Efrayim (Tulkarm area), Binyamin (Ramallah/al-Bireh area), Maccabim (Maccabim area), Etzion (Bethlehem area) and Yehuda (Hebron area). Economy.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Near Ramallah the new city of Rawabi is under construction. Jenin in the extreme north and is the capital of north of the West Bank and is on the southern edge of the Jezreel Valley. Modi'in Illit, Qalqilyah and Tulkarm are in the low foothills adjacent to the Israeli Coastal Plain, and Jericho and Tubas are situated in the Jordan Valley, north of the Dead Sea. Religion.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
Near Ramallah the new city of Rawabi is under construction. Jenin in the extreme north and is the capital of north of the West Bank and is on the southern edge of the Jezreel Valley. Modi'in Illit, Qalqilyah and Tulkarm are in the low foothills adjacent to the Israeli Coastal Plain, and Jericho and Tubas are situated in the Jordan Valley, north of the Dead Sea. Religion.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
He played a prominent role in rebuilding the PLO's military apparatus and training troops alongside Yasser Arafat, Khalil al-Wazir, Muhammad Youssef al-Najjar and others. Life and career. Sayel was born in the Kafr Ghalil village located in the eastern foot of Mount Gerizim, &quot;Jabal et Tur&quot; one of the mountains of Nablus. He spent his elementary and secondary education there.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
In spite of a grim and quiet personality, Sayel was widely respected as a tough and influential commander. Death. He was assassinated by the Abu Nidal Organization in Lebanon, near Syria border on 29 September 1982. He had gone to Beqaa Valley to visit the Popular Front and the Lebanese Joint Forces. Then he went to the hospital there for visiting someone and continued his way to Baalbek.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Geisel (river). Geisel () is a river of Saxony-Anhalt, Germany. The source of the Geisel, the Geiselquell, is located in the village of Sankt Micheln just west of Mücheln. The Geisel flows east through Geiseltal, or Geisel valley, until it flows into the in Merseburg, thats runoff, the Klia, empties into the Saale. Origin of name.

Geographic entities mentioned:
surface_form: Geisel valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.307777777778
lon: 11.869166666667
The Geisel flows east through Geiseltal, or Geisel valley, until it flows into the in Merseburg, thats runoff, the Klia, empties into the Saale. Origin of name. It is probable that the name is related to Geusa, a small village in the Geisel valley dating back to the early 9th century, but since both names date back to the days of Charlemagne, the original spelling and etymology have been lost.

Geographic entities mentioned:
surface_form: Geisel valley
instance_of: Valley
countries: Germany
coordinates: lat: 51.307777777778
lon: 11.869166666667
Corbins. Corbins () is a municipality in the &quot;comarca&quot; of the Segrià in Catalonia, Spain. It is situated at the confluence of the Segre and Noguera Ribagorçana rivers and is linked to Lleida by a local road running parallel to the Segre.

Geographic entities mentioned:
surface_form: Noguera Ribagorçana
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.6267
lon: 0.7058
Slieve Gallion () is a mountain in County Londonderry, Northern Ireland. It is the easternmost of the Sperrin Mountains. It reaches a height of and dominates the western shore of Lough Neagh. Its prominent northeastern summit has a transmitter station with a small road leading to it, and stands at a height of. By road, Slieve Gallion is from Moneymore, from Cookstown, and from Magherafelt.

Geographic entities mentioned:
surface_form: Lough Neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
surface_form: neagh
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.618333333333
lon: -6.3952777777778
Slieve Gallion. Slieve Gallion () is a mountain in County Londonderry, Northern Ireland. It is the easternmost of the Sperrin Mountains. It reaches a height of and dominates the western shore of Lough Neagh. Its prominent northeastern summit has a transmitter station with a small road leading to it, and stands at a height of.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
It reaches a height of and dominates the western shore of Lough Neagh. Its prominent northeastern summit has a transmitter station with a small road leading to it, and stands at a height of. By road, Slieve Gallion is from Moneymore, from Cookstown, and from Magherafelt. The mountain is part of the parishes of Desertmartin, Lissan and Ballinascreen. Landscape. Slieve Gallion is a volcanic plug.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
By road, Slieve Gallion is from Moneymore, from Cookstown, and from Magherafelt. The mountain is part of the parishes of Desertmartin, Lissan and Ballinascreen. Landscape. Slieve Gallion is a volcanic plug. The mountain is formed from volcanic-derived igneous rock, and also granite on the southern slopes. It is steep, and has a flat top.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
It is steep, and has a flat top. There is a telecommunications mast on the northeastern summit. To the west, the landscape consists of blanket bog and coniferous forest; most of the trees in the Slieve Gallion area are Sitka spruce. There are also lodgepole pine trees, as well as oak towards the south of the area.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
Animal species living in the area include the Irish hare (a sub-species of the mountain hare), the curlew, and the red grouse. The otter can also be found around nearby rivers. Slieve Gallion is classed by the Northern Ireland Planning Service as an area of &quot;High Scenic Value&quot;. Peat formed at Slieve Gallion in the early Holocene period, around 10,000 years ago.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
The otter can also be found around nearby rivers. Slieve Gallion is classed by the Northern Ireland Planning Service as an area of &quot;High Scenic Value&quot;. Peat formed at Slieve Gallion in the early Holocene period, around 10,000 years ago. The radiocarbon dating of pollen has shown that there were plants in the area 10,000 years ago. 7,000 ago, the number of alder trees steeply increased.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
7,000 ago, the number of alder trees steeply increased. History. The earliest reference to Slieve Gallion is from the 7th century, in the Book of Armagh, where it is called, likely meaning &quot;the height of Saint Patrick&quot;. This later became &quot;Sliabh gCallann&quot;, the first element meaning &quot;mountain&quot;.

Geographic entities mentioned:
surface_form: slieve gallion
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.73
lon: -6.76
They are separated by an aspen parkland transition zone near the North Saskatchewan River on the western side of the province, and near to south of the Saskatchewan River on the eastern side. Northern Saskatchewan is mostly covered by forest except for the Lake Athabasca Sand Dunes, the largest active sand dunes in the world north of 58°, and adjacent to the southern shore of Lake Athabasca.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
The province's highest point, at, is in the Cypress Hills less than from the provincial boundary with Alberta. The lowest point is the shore of Lake Athabasca, at. The province has 14 major drainage basins made up of various rivers and watersheds draining into the Arctic Ocean, Hudson Bay, and the Gulf of Mexico. Climate.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
Light crude is found in the Kindersley-Swift Current areas as well as the Weyburn-Estevan fields. Natural gas is found almost entirely in the western part of Saskatchewan, from the Primrose Lake area through Lloydminster, Unity, Kindersley, Leader, and around Maple Creek areas. Major companies based in Saskatchewan include Nutrien, Federated Cooperatives Ltd. and Cameco.

Geographic entities mentioned:
surface_form: Primrose Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.7875
lon: -110.0325
The Trans-Hudson orogeny and the consequent upheaval of the continental crust in the middle Proterozoic eon caused the area around the Great Lakes to become a flattened plain, which in turn led to the creation of the intracontinental basin and the interior and central plains of the United States (the Great Plains are the westernmost portion of North America's Interior Plains, which extend east to the Appalachian Plateau).

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
The Black Hills of South Dakota is one of the few remaining exposed portions of the Trans-Hudson orogenic belt. The peaks of the Black Hills are above the surrounding plains, while Black Elk Peak – the highest point in South Dakota – has an altitude of above sea level.

Geographic entities mentioned:
surface_form: Black Elk Peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.871666666667
lon: -103.53166666667
It occurs along the coastlines of the southern Western Cape and Eastern Cape, and marginally in KwaZulu-Natal, but is extinct from the vicinity of Durban, due to habitat loss. A small population of less than 40 pairs exists on the eastern slopes of Table Mountain, Cape Town, and it is present in forested valleys of the Langeberg.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
New areas would be identified later. On 30 November 2023, the city of Maceió decreed a state of emergency in the municipality for 180 days due to the &quot;imminent collapse&quot; of a mine belonging to Braskem in the area of Mundaú Lagoon, in the Mutange neighborhood. The city's civil defense authority reported the partial collapse of the mine on 10 December. Affected population.

Geographic entities mentioned:
surface_form: Mundaú Lagoon
instance_of: Lake
countries: Brazil
coordinates: lat: -9.63333
lon: -35.78333
Lusty Beg Island. Lusty Beg Island () is an island located in Lower Lough Erne, in County Fermanagh, Northern Ireland, directly adjacent to Boa Island. The island is the location of Lusty Beg Island Resort and Spa, which operates an on-demand ferry service between the island and Boa Island.

Geographic entities mentioned:
surface_form: Lough Erne
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.48262
lon: -7.80622
Taihu Reservoir. Taihu Reservoir (), also spelled as Tai-Hu Reservoir, formerly known as Huanglong Reservoir, is a reservoir located in Jinhu Township, Kinmen County, Taiwan. It is one of the main water sources of Kinmen. And the &quot;Lake Tai&quot; formed by the Reservoir is the largest artificial freshwater lake in Kinmen.

Geographic entities mentioned:
surface_form: huanglong reservoir
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.439888888888888
lon: 118.42608333333334
surface_form: taihu reservoir
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.439888888888888
lon: 118.42608333333334
Taihu Reservoir. Taihu Reservoir (), also spelled as Tai-Hu Reservoir, formerly known as Huanglong Reservoir, is a reservoir located in Jinhu Township, Kinmen County, Taiwan. It is one of the main water sources of Kinmen. And the &quot;Lake Tai&quot; formed by the Reservoir is the largest artificial freshwater lake in Kinmen.

Geographic entities mentioned:
surface_form: taihu reservoir
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.439888888888888
lon: 118.42608333333334
And the &quot;Lake Tai&quot; formed by the Reservoir is the largest artificial freshwater lake in Kinmen. The construction of the Taihu Reservoir started in October 1966 and was completed on April 10, 1967. The total storage capacity of the Reservoir is more than 1.14 million cubic meters, and the dam is 11.3 meters high and 600 meters long, making it the largest reservoir in the Kinmen region.

Geographic entities mentioned:
surface_form: taihu reservoir
instance_of: Lake
countries: Taiwan
coordinates: lat: 24.439888888888888
lon: 118.42608333333334
Geography. The municipality covers an area of in the western interior of the Overberg region. It occupies the area between the Riviersonderend Mountains to the north and the Kogelberg and Kleinrivier Mountains to the south; to the west it stretches as far as the Hottentots-Holland mountains. The western area of the municipality is the Elgin Valley, drained by the Palmiet River.

Geographic entities mentioned:
surface_form: Kleinrivier Mountains
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.3833
lon: 19.4167
Distribution and habitat. The wildflower is endemic to California, where it grows in a number of habitats in the central part of the state from the Sierra Nevada (foothills and High Sierra) to the Tehachapi Mountains, the San Joaquin Valley, and the central Inner California Coast Ranges. Description.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Caylloma province. Caylloma is the largest of eight provinces in the Arequipa Region of Peru. Points of interest. The Colca Canyon lies in the Huambo and Callalli districts.

Geographic entities mentioned:
surface_form: Colca Canyon
instance_of: Valley
countries: Peru
coordinates: lat: -15.5972
lon: -72.0559