Sarmila/GeoWiki-Features huggingface dataset:
Sankt Goar. Sankt Goar () is a town on the west bank of the Middle Rhine in the Rhein-Hunsrück-Kreis (district) in Rhineland-Palatinate, Germany. It belongs to the &quot;Verbandsgemeinde&quot; Hunsrück-Mittelrhein, whose seat is in Emmelshausen. Sankt Goar is well known for its central location in the Rhine Gorge, a UNESCO World Heritage Site since July 2002.

Geographic entities mentioned:
surface_form: Middle Rhine
instance_of: Valley
countries: Germany
coordinates: lat: 50.364166666667
lon: 7.6055555555556
Above the town stand the ruins of Burg Rheinfels, one of the castles for which the Middle Rhine is famous, and across the river lies the sister town of Sankt Goarshausen with its own castles, Katz and Maus (“Cat” and “Mouse”). The famous Lorelei rock is close by, slightly upstream on the opposite bank. Location.

Geographic entities mentioned:
surface_form: Lorelei
instance_of: Mountain
countries: Germany
coordinates: lat: 50.139444444444
lon: 7.7288888888889
Other volcanoes in the island arc are also known for their volcanic activity, including Saint Vincent's La Soufrière, Guadeloupe's La Grande Soufriere volcano, Montserrat's Soufrière Hills, and the submarine volcano Kick 'em Jenny. Geological history. Volcanologists have identified three different phases in the evolution of Mount Pelée volcano: initial, intermediate, and modern.

Geographic entities mentioned:
surface_form: Soufrière Hills
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 16.716666666667
lon: -62.183333333333
surface_form: la soufrière
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
surface_form: soufriere
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
surface_form: la grande soufriere
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
surface_form: soufrière
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
surface_form: soufrière
instance_of: Mountain
countries: France
coordinates: lat: 16.0438
lon: -61.6634
During the intermediate phase, there were several eruptions which produced pyroclastic flows like those that destroyed Saint-Pierre in the 1902 eruption. Around 25,000 years ago, a large southwest sector collapse occurred, forming a landslide. This event was similar to the eruption of Mount St. Helens in 1980.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Geological history. Volcanologists have identified three different phases in the evolution of Mount Pelée volcano: initial, intermediate, and modern. In an initial phase, called the &quot;Paléo-Pelée&quot; stage, Mount Pelee was a common stratovolcano. The cone of Paléo-Pelée was composed of many layers of lava flows and fragmented volcanic debris.

Geographic entities mentioned:
surface_form: mount pelee
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelee
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The estimated population of the Commune of Saint-Pierre in 2017 was 4,123. On 6 December 2020, The Martinique Volcano Observatory (MVO) raised Mount Pelee's alert level to Yellow [Restless] from Green [Normal] due to an increase in seismicity under the volcano beginning in April 2019, and observations of tremors the previous month.

Geographic entities mentioned:
surface_form: mount pelee
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelee
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Mount Pelée. Mount Pelée or Mont Pelée (;,;) is an active volcano at the northern end of Martinique, an island and French overseas department in the Lesser Antilles Volcanic Arc of the Caribbean. Its volcanic cone is composed of stratified layers of hardened ash and solidified lava. Its most recent eruption was in 1932.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Mount Pelée. Mount Pelée or Mont Pelée (;,;) is an active volcano at the northern end of Martinique, an island and French overseas department in the Lesser Antilles Volcanic Arc of the Caribbean. Its volcanic cone is composed of stratified layers of hardened ash and solidified lava. Its most recent eruption was in 1932.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: mont pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
In 2023, it was listed as UNESCO World heritage site. Geographical setting and description. Mount Pelée is the result of a typical subduction zone. The subduction formed the Lesser Antilles island arc, a curved chain of volcanoes approximately in length, between Puerto Rico and Venezuela, where the Caribbean Plate meets Atlantic oceanic crust belonging to the South American Plate.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Geological history. Volcanologists have identified three different phases in the evolution of Mount Pelée volcano: initial, intermediate, and modern. In an initial phase, called the &quot;Paléo-Pelée&quot; stage, Mount Pelee was a common stratovolcano. The cone of Paléo-Pelée was composed of many layers of lava flows and fragmented volcanic debris.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
This event was similar to the eruption of Mount St. Helens in 1980. The modern stage of the evolution of Mount Pelée has created most of the current cone, with deposits of pumice and the results of past pyroclastic flows. More than 30 eruptions have been identified during the last 5,000 years of the volcano's activity.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Mount Pelée continued to erupt until 4 July 1905. Thereafter, the volcano was dormant until 1929. On 16 September 1929, Mount Pelée began to erupt again. This time, there was no hesitation on the part of authorities and the danger area was immediately evacuated. The 1929 eruption formed a second dome in the Étang Sec caldera and produced pyroclastic flows emptying into the Blanche River valley.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The activity ended in late 1932. Current status. The volcano is currently active. A few volcano tectonic earthquakes occur on Martinique every year, and Mount Pelée is under continuous watch by geophysicists and volcanologists (IPGP). Before the 1902 eruption—as early as the summer of 1900—signs of increased fumarole activity were present in the Étang Sec crater.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Relatively minor phreatic (steam) eruptions that occurred in 1792 and 1851 were evidence that the volcano was active. Signs of unrest are likely to precede any future eruptive activity from Mount Pelée, and its past activity (including the violent eruptions uncovered by carbon dating) is an extremely important factor for hazard assessment.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Whether or not it is going to enter a new eruptive period is currently unknown. The increase in seismicity of superficial volcanic origin (up to below the summit) observed since April 2019, is therefore clearly above the base level characteristic for Mount Pelée. In April 2019, volcanic seismicity appeared at depth around and under Mount Pelée (more than below sea level).

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The increase in seismicity of superficial volcanic origin (up to below the summit) observed since April 2019, is therefore clearly above the base level characteristic for Mount Pelée. In April 2019, volcanic seismicity appeared at depth around and under Mount Pelée (more than below sea level). It could correspond to the arrival at depth of magmatic fluids.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Biology. The Martinique volcano frog, &quot;Allobates chalcopis&quot;, is endemic to Mount Pelée, and the only species among related frogs (family Aromobatidae) endemic to an oceanic island. Important bird area.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Protection. On September 16, 2023, the volcanoes and forests of Mount Pelée and the pitons of northern Martinique were listed as UNESCO World Heritage Site. The volcanic mountain range represents 12% of Martinique's territory. It is the 7th natural site in France to be listed as a UNESCO World Heritage site.

Geographic entities mentioned:
surface_form: mount pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
In an initial phase, called the &quot;Paléo-Pelée&quot; stage, Mount Pelee was a common stratovolcano. The cone of Paléo-Pelée was composed of many layers of lava flows and fragmented volcanic debris. Remains of the Paléo-Pelée cone are still visible at the northern view at the volcano today.

Geographic entities mentioned:
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
The cone of Paléo-Pelée was composed of many layers of lava flows and fragmented volcanic debris. Remains of the Paléo-Pelée cone are still visible at the northern view at the volcano today. A second stage, now called the intermediate phase, started around 100,000 years ago, after a long period of quiescence.

Geographic entities mentioned:
surface_form: pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Ridgway is nationally recognized for being “Mavericks”. Geography. Ridgway is situated in the Uncompahgre Valley at an elevation of. The town is located on the San Juan Skyway, cradled in the heart of some of the most photographed mountains in the world. The nearby San Juan Mountain Range has 14 of Colorado's 53 peaks over 14,000 feet. Among them, Mt. Sneffels is most prominent from Ridgway.

Geographic entities mentioned:
surface_form: Uncompahgre Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.46
lon: -107.89
Ridgway is situated in the Uncompahgre Valley at an elevation of. The town is located on the San Juan Skyway, cradled in the heart of some of the most photographed mountains in the world. The nearby San Juan Mountain Range has 14 of Colorado's 53 peaks over 14,000 feet. Among them, Mt. Sneffels is most prominent from Ridgway. The eponymous Mt. Ridgway, in height, is also nearby, west of Ouray.

Geographic entities mentioned:
surface_form: Mt. Sneffels
instance_of: Mountain
countries: United States
coordinates: lat: 38.003888888889
lon: -107.79222222222
The nearby San Juan Mountain Range has 14 of Colorado's 53 peaks over 14,000 feet. Among them, Mt. Sneffels is most prominent from Ridgway. The eponymous Mt. Ridgway, in height, is also nearby, west of Ouray. To the east of the town also lies the smaller but equally-grand Cimarron Range, with Uncompahgre Peak at.

Geographic entities mentioned:
surface_form: Mt. Ridgway
instance_of: Mountain
countries: United States
coordinates: lat: 38.013611111111
lon: -107.75305555556
Tourism and culture. Ridgway is poised on a highway that leads tourists to several other mountain towns of the San Juan region. Ridgway itself is a major tourist town. Ridgway is 37 miles east of Telluride and 10 miles north of the Ouray. The area is also set at the base of the San Juan Mountains providing excellent views especially when viewed from Log Hill Mesa. The Grammy Awards.

Geographic entities mentioned:
surface_form: Log Hill Mesa
instance_of: Landform
countries: United States
coordinates: lat: 38.2105
lon: -107.905
Schubert is a single-member electoral district for the South Australian House of Assembly covering an area of 2,017.8 km2. It is named after Max Schubert, the winemaker of Penfolds Grange Hermitage. The Barossa Valley area was first represented by the seat of Barossa. The seat of Custance was abolished and recreated as Schubert in the 1994 redistribution and first contested at the 1997 election.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
The city is also a terminus of a branch of the main railroad line which connects it to Hinthada, Letpadan and Yangon. In the 1990s, the road network along the Irrawaddy to Monywa was improved. The coastline along the Bay of Bengal is surrounded by the Arakan Mountains. In the area is Inye Lake, long and wide, which is known for its fishing.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The 2011 Goderich, Ontario tornado was an intense F3 tornado generated by an isolated supercell which unexpectedly tore across Huron County, Ontario, Canada on the afternoon of Sunday, August 21, 2011. Beginning as a tornadic waterspout over Lake Huron, the tornado ripped through the lakeside town of Goderich severely damaging the historic downtown and homes in the surrounding area.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Goderich is also located in the &quot;lake shadow&quot; of Lake Huron, which is much less likely to be hit by tornadoes than other parts of Southwestern Ontario where lake convergence fronts collide. By 11:00am that morning, showers and thunderstorms began to develop over southwestern Ontario. Initially they were weak, but began to intensify in some localized areas.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
City Council. In his first bid for City Council in 1939 in Los Angeles City Council District 1, representing the San Fernando Valley, McCloskey survived the first round of voting but was defeated by the incumbent, Jim Wilson, in the final election. In the 1941 final, though, it was McCloskey who was the winner over Wilson.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
McCloskey was responsible for rescuing twenty-five pot-bellied stoves, &quot;discarded by the Fire Department, relics of those days when outlying fire stations were without gas.&quot; The stoves were reconditioned and lent to the Red Cross &quot;so soldiers occupying isolated searchlight posts in the San Fernando Valley could keep warm on winter nights.&quot;
Since the advent of the war, many thousands of persons from other states who earn large salaries in war industries and do not own any real property have become residents...

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Hog ranch, 1944. The City Council unanimously adopted McCloskey's resolution asking federal and state authorities to investigate a report that Japanese and Japanese-American detainees at Manzanar, California, would be put to work operating a large hog ranch that might pollute Los Angeles municipal water supplies from the Owens Valley. References.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
It was the third edition of the Abu Dhabi Tour and was the third event of the 2017 UCI World Tour. It was the first time that the race was included in the UCI World Tour calendar. The race's mountain-top finish at Jebel Hafeet provided the final podium of the race, after Mark Cavendish (), Marcel Kittel () and Caleb Ewan () won the three sprint stages.

Geographic entities mentioned:
surface_form: Jebel Hafeet
instance_of: Mountain
countries: United Arab Emirates
Oman
coordinates: lat: 24.05796
lon: 55.78086
Approximately 78% of the ridge's xeric uplands had already been developed by the late 1980s. Human land use includes pasture, citrus groves, pine plantations, sand mining, and residential areas. Eastern Florida Flatwoods (75d). The Eastern Florida Flatwoods are a region extending from Lake Okeechobee in the south to the St. Johns River estuary in the north, though not quite so far as Jacksonville.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
36,37 and 38 of Dhanbad Municipal Corporation. Overview. The region shown in the map is a part of the undulating uplands bustling with coalmines in the lowest rung of the Chota Nagpur Plateau. The entire area shown in the map is under Dhanbad Municipal Corporation, except Belgaria which is under Baliapur (community development block). The places in the DMC area are marked as neighbourhoods.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Klass did not finish the race in Le Mans, but ranked fifth both in Sebring and at the Targa Florio, and came in sixth place at Nürburgring. A Porsche 904 of the Swiss team Scuderia Filipinetti carried Klass to a sixth-place finish at the Schauinsland hillclimb in Germany. In 1966, he became a European rallying champion driving a Porsche 911R.

Geographic entities mentioned:
surface_form: Schauinsland
instance_of: Mountain
countries: Germany
coordinates: lat: 47.911111111111
lon: 7.8994444444444
Moel y Gest. Moel y Gest is a hill to the west of Porthmadog in North Wales. It is a very rocky hill with high topographic prominence because of the lower land that surrounds it on all sides, and qualifies as a Marilyn. The views from the top are far ranging and include the Llŷn Peninsula, the Rhinogydd, Moelwynion, Moel Hebog, and Snowdon. Ascent.

Geographic entities mentioned:
surface_form: Moel Hebog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.000138888889
lon: -4.1398
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
View to Beinisvørð from Nes. Nes lies beside the fjord of Vágsfjørður. From Nes one gets a view towards south to two other villages, which are on the other side of the fjords of Vágsfjørður and Lopransfjørður. These villages are Akrar and Lopra. One can also see the promontory sea cliff Beinisvørð, which rises 470 metres above the sea; the top of it rises above the village of Lopra.

Geographic entities mentioned:
surface_form: Beinisvørð
instance_of: Mountain
countries: Faroe Islands
coordinates: lat: 61.426388888889
lon: -6.7672222222222
Red-faced crimsonwing. The red-faced crimsonwing (&quot;Cryptospiza reichenovii&quot;) is a common species of estrildid finch found in Africa. It has an estimated global extent of occurrence of 390,000 km2. It is native to subsaharan mountainous regions: Bioko and the Western High Plateau, the Albertine Rift montane forests and east Africa (from northern Tanzania to eastern Zimbabwe). Taxonomy.

Geographic entities mentioned:
surface_form: Western High Plateau
instance_of: Plateau
countries: Cameroon
coordinates: lat: 6.5
lon: 10.5
Bergsee (Mecklenburg). Bergsee is a lake in the Mecklenburgische Seenplatte district in Mecklenburg-Vorpommern, Germany. At an elevation of 62.8 m, its surface area is 0.55 km2.

Geographic entities mentioned:
surface_form: bergsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.575555555556
lon: 12.496388888889
Baptizing Lake (Nova Scotia). Baptizing Lake is a lake of Halifax Regional Municipality, Nova Scotia, Canada.

Geographic entities mentioned:
surface_form: baptizing lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7241
lon: -63.7672
Daykovaya Peak. Daykovaya Peak is a prominent peak, high, rising between Mount Hansen and Kare Bench in the Westliche Petermann Range, Wohlthat Mountains. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39.

Geographic entities mentioned:
surface_form: Mount Hansen
instance_of: Mountain
coordinates: lat: -71.4667
lon: 12.15
surface_form: daykovaya peak
instance_of: Mountain
coordinates: lat: -71.4667
lon: 12.1833
Daykovaya Peak. Daykovaya Peak is a prominent peak, high, rising between Mount Hansen and Kare Bench in the Westliche Petermann Range, Wohlthat Mountains. It was discovered and plotted from air photos by the Third German Antarctic Expedition, 1938–39.

Geographic entities mentioned:
surface_form: daykovaya peak
instance_of: Mountain
coordinates: lat: -71.4667
lon: 12.1833
Satovcha Peak. Satovcha Peak (,) is the mostly ice-covered peak rising to 1587 m in Havre Mountains, northern Alexander Island in Antarctica. It surmounts Bongrain Ice Piedmont to the northeast and Lennon Glacier to the southwest. Its south slopes are precipitous and partly ice-free.

Geographic entities mentioned:
surface_form: Bongrain Ice Piedmont
instance_of: Landform
coordinates: lat: -69
lon: -71.5
The feature is named after the settlement of Satovcha in Southwestern Bulgaria. Location. The peak is located at, which is 14.88 km east-southeast of Cape Vostok, 5.6 km south-southeast of Boyn Ridge, 13.23 km west by north of Mount Newman, 7.73 km northwest of Igralishte Peak and 6.54 km northeast of Nicolai Peak.

Geographic entities mentioned:
surface_form: Mount Newman
instance_of: Mountain
coordinates: lat: -69.1833
lon: -71.4333
Leucoptera lustratella. &quot;Leucoptera lustratella&quot; is a moth in the Lyonetiidae family. It is found from Fennoscandia to the Pyrenees and Italy and from France to Belarus and Romania. The larvae feed on &quot;Hypericum hirsutum&quot;, &quot;Hypericum montanum&quot; and &quot;Hypericum perforatum&quot;. They mine the leaves of their host plant.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The location Dunsinane is not accepted as historical by modern historians, resting as it does on later medieval accounts. The earliest mention of Dunsinane as the location of the battle being the early 15th-century account by Andrew of Wyntoun.

Geographic entities mentioned:
surface_form: Dunsinane
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.470634
lon: -3.277998
Anoploscelus. &quot;Anoploscelus&quot; is a genus of East African tarantulas that was first described by Reginald Innes Pocock in 1897. It was erected for the species &quot;Anoploscelus celeripes&quot;, based on a single male collected near Lake Tanganyika in modern day Tanzania. It was synonymized with &quot;Phoneyusa&quot; from 1985 to 1990. it contains two species, including &quot;A.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
This marked the first direct entry of the Mexican state into the business of public television. In 1976, the government built new facilities for XHDF in Ajusco, south of Mexico City. In April 1972, the Mexican government embarked on another television project, the creation of Televisión Rural Mexicana (Mexican Rural Television).

Geographic entities mentioned:
surface_form: Ajusco
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.2075
lon: -99.258055555556
That same year, on May 15, it signed on a new television station in Mexico City, XHIMT-TV channel 7. To give Mexico City an additional VHF channel, a frequency shuffle ensued between the Televisa channel 8 in Mexico City and two Televisa stations transmitting from Altzomoni, whose signals were targeted toward Puebla.

Geographic entities mentioned:
surface_form: Altzomoni
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.12
lon: -98.654
Salinas responded the next month, agreeing with their proposal. Channel 22 was chosen for this project, and it went off the air late in 1991. On June 23, 1993, XEIMT returned to the air from a more powerful transmitter located on Cerro del Chiquihuite, under the auspices of Conaculta and with its new cultural format.

Geographic entities mentioned:
surface_form: Cerro del Chiquihuite
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.5328
lon: -99.1306
Allocations. One of the more unusual allocations at the shed was Edward Fletcher's 4-4-0 &quot;Whitby Bogies&quot; (NER Class 492). These engines were built specifically to deal with the tight curves in Newton Dale, and the gradients on the line between and. The locomotives were built by Stephenson & Co. between 1864 and 1865.

Geographic entities mentioned:
surface_form: Newton Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35472222222222
lon: -0.7105555555555555
For Colonel Bradley, it marked a record third Kentucky Derby win. Derby favorite Tick On finished sixth but in the ensuing Preakness Stakes he provided fierce competition with Burgoo King and jockey Eugene James beating Tick On by a head. A year after his two Classic wins, James died in a drowning accident in Lake Michigan. Winning the 1932 Belmont Stakes would have made Burgoo King the third U.S.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The presence of pottery from Malvern suggests that Wychbold had strong trade links outside of its immediate area, even in the Iron Age. Wychbold is located on an old Roman road and salt road, now the A38. Romans are believed to have settled in the Wychbold area between the 1st and 4th century, shown by the presence of Severn Valley and samian pottery. Middle Ages to Early modern period.

Geographic entities mentioned:
surface_form: Severn Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 52.5
lon: -2.33333
It avoids areas with an annual rainfall below 500 mm. In southern Africa it is absent from Kalahari woodlands, and is largely replaced by the orange-breasted bushshrike in the Okavango Delta. It many areas it occurs in sympatry with the latter species, but may locally be found living in close proximity with several other bushshrike species.

Geographic entities mentioned:
surface_form: Okavango Delta
instance_of: Body of water
Watercourse
countries: Botswana
coordinates: lat: -19.4
lon: 22.9
All of them are native: there is a sound of the lullaby motif, that our mothers sing to us, children's songs, and poems about the boundless beauty of our lands and people. Aktanova notes that Chuykov portrayed ordinary people, their honesty and directness. He avoided places attractive to tourists; he came to Issyk-Kul many times, but he never painted the lake.

Geographic entities mentioned:
surface_form: Issyk-Kul
instance_of: Lake
countries: Kyrgyzstan
coordinates: lat: 42.416666666667
lon: 77.25
It was formally described as a species new to science in 1942 by Swedish lichenologist Rolf Santesson. The type specimen was collected north of Lago Fagnano (Tierra del Fuego, Argentina). The lichen is typically encountered as an epiphyte, but occasionally it has been recorded growing on rocks. &quot;Menegazzia globulifera&quot; contains usnic acid and lecanoric acid as major lichen products.

Geographic entities mentioned:
surface_form: Lago Fagnano
instance_of: Lake
countries: Chile
Argentina
coordinates: lat: -54.543333333333
lon: -67.983333333333
This was a period of Muslim conquest and repression of Hindus under the Delhi Sultanate and the Mughal Empire. The literary works not composed by Namdev, but attributed to Namdev were partly a product of this historical suffering and political situation in Deccan region of India.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The maximum water depth may have reached. A wave-cut terrace lies about elevation above the salar, and a river delta formed where the Collacagua River entered the lake. The lake highstand has been correlated to Lake Tauca on the Altiplano, and its eventual drying with the Holocene Climatic Optimum. When it evaporated, it left the salts now in Salar del Huasco. Geology and watershed.

Geographic entities mentioned:
surface_form: Lake Tauca
instance_of: Lake
countries: Peru
coordinates: lat: -20
lon: -68
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
When it evaporated, it left the salts now in Salar del Huasco. Geology and watershed. The watershed of Salar de Huasco lies in the Altiplano and Andes, covering an area of about. It is surrounded by mountain chains with volcanoes, except to the west and south where the Altos de Pica highland delimits the basin.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Animal corrals and trails have been mapped around Salar del Huasco. Later archaeological sites have been linked to the Inca presence in northern Chile; El Tojo in the Huasco basin is the reference site for Inca activities in the region, where an Inca road connected Pica with the Altiplano and was frequently used in historic times. In the 20th century, the area of the salar was used for pastures.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Salar del Huasco. Salar del Huasco is a salt flat dotted with ponds and salt marshes, and seasonally partially covered with water, in northern Chile. It is part of Ramsar Site 874, and was, for several years, a national park. The area has a significant population of flamingos.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
In the Pleistocene the salt flat was covered by a lake that was identified through its clay and diatomite sediments and which has left well preserved shorelines and terraces. Lake. Salar del Huasco is in Pica commune, Iquique Province, Tarapaca Region of northern Chile, about east of Iquique. The area is largely uninhabited owing to its harsh climate.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Lake. Salar del Huasco is in Pica commune, Iquique Province, Tarapaca Region of northern Chile, about east of Iquique. The area is largely uninhabited owing to its harsh climate. The Chilean roads A-687 and A-685 pass close to Salar del Huasco. The salt covers a surface of about with a roughly rectangular shape, the long sides extending northwest-southeast.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Salinities vary between waterbodies, ranging from freshwater to hypersaline. The lowest altitude of the salar is about. A fault may cross the western side of Salar del Huasco. The salt flat is surrounded by a mostly sandy ground and two flat plains border it to the north and east, respectively: The Pampa Sillillica and the Pampa Rinconada.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
The salt flat is surrounded by a mostly sandy ground and two flat plains border it to the north and east, respectively: The Pampa Sillillica and the Pampa Rinconada. In prehistorical times, a large lake formed at Salar del Huasco and left lake sediments, tufa deposits and shorelines. Water rose and above the present-day salar surface, forming a lake. The maximum water depth may have reached.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
The maximum water depth may have reached. A wave-cut terrace lies about elevation above the salar, and a river delta formed where the Collacagua River entered the lake. The lake highstand has been correlated to Lake Tauca on the Altiplano, and its eventual drying with the Holocene Climatic Optimum. When it evaporated, it left the salts now in Salar del Huasco. Geology and watershed.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Geology and watershed. The watershed of Salar de Huasco lies in the Altiplano and Andes, covering an area of about. It is surrounded by mountain chains with volcanoes, except to the west and south where the Altos de Pica highland delimits the basin. A valley runs north-south in the basin; the Collacagua river runs along its length and Salar del Huasco lies at its southern end.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
It is a closed basin, meaning that water does not exit it except through evaporation. Three separate aquifers have formed in the basin fill, and are hydrologically connected both to the Collacagua River and the Salar del Huasco.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Three separate aquifers have formed in the basin fill, and are hydrologically connected both to the Collacagua River and the Salar del Huasco. These aquifers are an important water source to Salar del Huasco, helping it to maintain an open water surface, and assuming lack of human interference would buffer the impacts of climate change on the salar.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
These aquifers are an important water source to Salar del Huasco, helping it to maintain an open water surface, and assuming lack of human interference would buffer the impacts of climate change on the salar. There may be connections between these aquifers and these of Pica west of Salar del Huasco.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
There may be connections between these aquifers and these of Pica west of Salar del Huasco. The Collacagua River enters Salar del Huasco on its northern shore; it is the principal watercourse of the region and one of the few to permanently carry water, but its waters do not reach the salar directly except during floods.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
The Collacagua River enters Salar del Huasco on its northern shore; it is the principal watercourse of the region and one of the few to permanently carry water, but its waters do not reach the salar directly except during floods. It is about long and forms through the union of the easterly Piga and the northern Caquina rivers, far north from Salar del Huasco.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Otherwise, clockwise from north to south the Quebrada Huallacaibo, Quebrada Rinconada, Quebrada del Corregidor, Quebrada de Huasco and Quebrada Parilca and several nameless creeks join the salar. Salar del Huasco is the principal source of water for the area. Climate, flora and fauna. The salar area has a cold desert climate with a mean annual temperature not exceeding.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Noted birds at Salar del Huasco include Andean avocets, Andean condors, Andean flamingos, Andean goose, Andean gulls, Andean lapwings, Andean negritos, Baird's sandpipers, black-crowned night herons, buff-winged cinclodes, Chilean flamingo, crested ducks, giant coots, James's flamingo, least seedsnipes, lesser yellowlegs, nandus, nuthatchers, Puna plovers, Puna teal, puna tinamous, silvery grebes, Wilson's phalaropes, yellow-billed pintail and yellow-billed teals.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
There are more than three thousand flamingos at Salar del Huasco, which is their nesting site. Salar del Huasco is a major stopover for bird migrations of American golden plovers, Baird's sandpipers, lesser yellowlegs and peregrine falcons. The ecosystem at Salar del Huasco is very diverse and is used as a stand-in for other Chilean salar ecosystems.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Both the flora and fauna include numerous endemics and some species may yet be discovered. Other species are threatened species. Humans hunt waterbirds, and overgrazing has occurred in the area, but overall human impact on Salar del Huasco's land ecosystem is small. Microbial ecosystems. Salar del Huasco has been investigated for its microbial inhabitants.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Their communities are dominated by bacteria if viruses aren't counted, with a number of unidentified genera. Environmental conditions are extreme, with the lack of water, harsh climate, high insolation, intense wind-driven mixing, lack of oxygen at high elevations and plenty of toxic arsenic, and the genomes of microbes found at Salar del Huasco show evidence of adaptations.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Various metabolic pathways have been identified in microbes from Salar del Huasco, with different prevalences in different parts of the salar; they include nitrogen fixation and different kinds of photosynthesis. Various antibiotic substances are produced by microbes from Salar del Huasco. Some bacteria form microbial mats.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Human exploitation and conservation. Numerous archeological sites are found around the salar. They go back to the last ice age, when the lake was larger and its environment drew hunter-gatherers to Salar del Huasco. Populations persisted after it dried up. Animal corrals and trails have been mapped around Salar del Huasco.

Geographic entities mentioned:
surface_form: salar del huasco
instance_of: Body of water
countries: Chile
coordinates: lat: -20.3
lon: -68.85
Lemming, voles, squirrel and hare are common, and the European otter is common near the fjords and in many rivers, especially in the north. There are approximately 150 musk oxen on Dovrefjell, having been transported from Greenland in the 1930s, as the species were extinct in Scandinavia. There is a rich bird life; most birds are migratory, but some, like the ptarmigan, stay all year.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Historically, the area around this confluence has been called Three Rivers. Muskogee lies in the Arkansas River Valley and has a low elevation (above sea level) compared to much of the rest of the state. The city is on the boundary of the oak and hickory forest region of eastern Oklahoma and the prairie, Great Plains region of northeastern Oklahoma. It is southeast of Tulsa. Climate.

Geographic entities mentioned:
surface_form: Arkansas River Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Grøndalselva. Grøndalselva is a river in Nordenskiöld Land at Spitsbergen, Svalbard. It flows from Grøndalspasset through the nineteen kilometer long valley of Grøndalen, and debouches into Grønfjorden.

Geographic entities mentioned:
surface_form: Grøndalen
instance_of: Valley
countries: Norway
coordinates: lat: 77.99666667
lon: 14.64666667
Silfrastaðir. Silfrastaðir is a farm and church site at the mouth of the Norðurárdalur valley in Skagafjörður, Iceland. The farm's property is vast, spanning from the Bóluá river in Blönduhlíð out to the Kotá river in Norðurárdalur. Most of the land is mountainous, located around Silfrastaðafjall mountain. It is now slated for reforestation.

Geographic entities mentioned:
surface_form: Norðurárdalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.4325
lon: -19.04597
12th (HAC) Regiment, RHA. The 12th (HAC) Regiment RHA took part in the Operation Torch landings and were in action at Thala in February 1943, where they halted a German advance following the Battle of the Kasserine Pass. After re-equipping with Priests, they too moved on to Italy in March 1944 and fought at Monte Cassino. 13th (HAC) Regiment, RHA.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
Its outflow is the Rio Revelli, the main source stream of the Corsaglia. To the south of the lake basin runs the mountain ridge that separates Val Corsaglia from the, particularly the section of the watershed that includes the Monte Rotondo, the Bric di Conoia, the, and the distinctive. The small basin hosts marshy vegetation dominated by &quot;Carex fusca&quot;.

Geographic entities mentioned:
surface_form: Monte Rotondo
instance_of: Mountain
countries: France
coordinates: lat: 42.21611111111111
lon: 9.058055555555555
surface_form: Bric di Conoia
instance_of: Mountain
countries: Italy
coordinates: lat: 44.163324
lon: 7.8050554
surface_form: monte rotondo
instance_of: Mountain
countries: Italy
coordinates: lat: 42.98166667
lon: 13.20277778
Lake Revelli. Lake Revelli is a small alpine lake located at 2,029 m a.s.l. in the Ligurian Alps, in the municipality of Ormea. It is situated in the upper valley of the, just north of the. Description. The water body is located in at 2,029 m elevation, at the head of the valley. It lies within a basin surrounded by various peaks ranging in height between 2,300 and 2,500 meters.

Geographic entities mentioned:
surface_form: lake revelli
instance_of: Lake
countries: Italy
coordinates: lat: 44.17363
lon: 7.8158
Russia conquered Turkestan, and Britain expanded and set the borders of British India. By the early 20th century, a line of independent states, tribes, and monarchies from the shore of the Caspian Sea to the Eastern Himalayas were made into protectorates and territories of the two empires.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
East India Company. In 1782, George Forster, a civil servant of the East India Company, undertook a journey that began in Calcutta, Bengal and passed through Kashmir, Afghanistan, Herat, Khorassan, Mazanderan, crossed the Caspian Sea by ship, and then travelled to Baku, Astrakhan, Moscow, St Petersburg and then by ship to London. Forster's detailed description of the journey was published in 1798.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Russian travelogues written between the 1870s and the turn of the 1900s seem to imply that Russian commerce had become dominant in the northern and western portions of Iran that would be officially delineated to Russia by Britain in 1907. Russia had also acquired concessions such as a monopoly on the lucrative caviar in the southern Caspian Sea, which lasted until after the First World War.

Geographic entities mentioned:
surface_form: southern Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
On 21 January 1873, Great Britain and Russia signed an agreement that stipulated that the eastern Badakhshan area as well as the Wakhan Corridor to Lake Sariqol were Afghan territory, the northern Afghan boundary was the Amu Darya (Oxus River) as far west as Khwaja Salar (near Khamyab), and a joint Russian-British commission would define the boundary from the Amu Darya to the Persian border on the Hari (Harirud) River.

Geographic entities mentioned:
surface_form: Lake Sariqol
instance_of: Lake
countries: Afghanistan
Tajikistan
coordinates: lat: 37.450332
lon: 73.725128
The agreement delineated a permanent northern Afghan frontier at the Amu Darya, with the loss of a large amount of territory, especially around Panjdeh. This left the border east of Lake Zorkul in the Wakhan region to be defined. This territory was claimed by China, Russia and Afghanistan. In the 1880s, the Afghans had advanced north of the lake to the Alichur Pamir.

Geographic entities mentioned:
surface_form: Zorkul
instance_of: Lake
countries: Afghanistan
Tajikistan
coordinates: lat: 37.450332
lon: 73.725128
In the 1880s, the Afghans had advanced north of the lake to the Alichur Pamir. In 1891, Russia sent a military force to this area and its commander, Yanov, ordered the British Captain Francis Younghusband to leave Bozai Gumbaz in the Little Pamir. The Russians claimed that because they had annexed the Khanate of Kokand they had a claim over the Pamirs.

Geographic entities mentioned:
surface_form: Little Pamir
instance_of: Valley
countries: Afghanistan
coordinates: lat: 37.26666667
lon: 74.28333333