Sarmila/GeoWiki-Features huggingface dataset:
Dudelange Castle. The ruins of Dudelange Castle (Luxembourgish: &quot;Buerg um Gehaansbierg&quot;;) are located on Mont St Jean, a forested hill to the west of Dudelange in the south of Luxembourg. The castle was completed in the early 16th century but was destroyed in 1552. History.

Geographic entities mentioned:
surface_form: Mont St Jean
instance_of: Mountain
countries: Luxembourg
coordinates: lat: 49.49029
lon: 6.05974
Dörgicse. Dörgicse is a village in Veszprém county, Hungary. It consists of three hamlets (Felsõdörgicse, Alsódörgicse and Kisdörgicse) built on separate hills 4.3 km (2.7 m) north of Lake Balaton. Dörgicse is famous for the wine production and its three medieval churches which were devastated during the Turkish wars in the 16th and 17th centuries.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
Holy Trinity Church, Geneva. Holy Trinity Church, Geneva, Switzerland, was completed in 1853. The church is located at rue du Mont-Blanc, between the Genève-Cornavin railway station and the famous hotels at the banks of Lake Geneva. The church is part of the Diocese in Europe of the Church of England and is also a Swiss monument of regional significance (class B). History.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Glammsee. Glammsee is a lake in the Nordwestmecklenburg district in Mecklenburg-Vorpommern, Germany. At an elevation of 18.4 m, its surface area is 0.66 km².

Geographic entities mentioned:
surface_form: glammsee
instance_of: Lake
countries: Germany
coordinates: lat: 53.795
lon: 11.705
Kosmos 954. Kosmos 954 () was a reconnaissance satellite launched by the Soviet Union in 1977. A malfunction prevented safe separation of its onboard nuclear reactor; when the satellite reentered the Earth's atmosphere the following year, it scattered radioactive debris over northern Canada, some of the debris landing in the Great Slave Lake next to Fort Resolution, Northwest Territories.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
At 11:53 GMT on 24 January 1978, Kosmos 954 reentered the Earth's atmosphere while travelling on a northeastward track over western Canada. At first the USSR claimed that the satellite had been completely destroyed during re-entry, but later searches showed debris from the satellite had been deposited on Canadian territory along a path from Great Slave Lake to Baker Lake.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
Geography. Armada is in northern Macomb County, north of Mount Clemens, the county seat; southwest of Port Huron, and north-northeast of downtown Detroit. According to the United States Census Bureau, the village has a total area of, of which, or 0.27%, are water. The East Branch of Coon Creek passes through the center of the village, part of the Clinton River watershed flowing to Lake St. Clair.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
and the then Soviet Union. The march started at Point Conception, Calif., and went through Texas and the Deep South to New York City. Several others, including Andy Rector, walked significant portions across the U.S. and continued in Europe to Moscow, Russia, in 1985. Ed Fallon, Miriam Kashia, Mackenzie McDonald Wilkins, Jeffrey Czerwiec, Steve Martin.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Along the way he saluted passing motorists and pedestrians, received certificates of appreciation at the Inland Empire and San Gabriel Valley, and left non-sectarian 40-day prayer guides for city and county officials.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The west peak is highest at 6,420-feet elevation, the middle peak is 6,298-feet, and the east peak is lowest, at 6,020-feet. The nearest higher peak is The West Temple, to the west. Other neighbors include The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, Bridge Mountain, The Watchman, and Mount Kinesava. Precipitation runoff from this mountain drains into the North Fork Virgin River.

Geographic entities mentioned:
surface_form: The West Temple
instance_of: Mountain
countries: United States
coordinates: lat: 37.210869
lon: -113.02071
The west peak is highest at 6,420-feet elevation, the middle peak is 6,298-feet, and the east peak is lowest, at 6,020-feet. The nearest higher peak is The West Temple, to the west. Other neighbors include The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, Bridge Mountain, The Watchman, and Mount Kinesava. Precipitation runoff from this mountain drains into the North Fork Virgin River.

Geographic entities mentioned:
surface_form: Altar of Sacrifice
instance_of: Mountain
countries: United States
coordinates: lat: 37.225934
lon: -113.019858
surface_form: Mount Kinesava
instance_of: Mountain
countries: United States
coordinates: lat: 37.19804
lon: -113.0305
Description. Three Marys is situated immediately northwest of Springdale, Utah, and west of the park headquarters. The west peak is highest at 6,420-feet elevation, the middle peak is 6,298-feet, and the east peak is lowest, at 6,020-feet. The nearest higher peak is The West Temple, to the west.

Geographic entities mentioned:
surface_form: middle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.99541
lon: -121.47736
Three Marys (Zion National Park). Three Marys are three sandstone pillars in Zion National Park in Washington County, Utah, United States. Description. Three Marys is situated immediately northwest of Springdale, Utah, and west of the park headquarters. The west peak is highest at 6,420-feet elevation, the middle peak is 6,298-feet, and the east peak is lowest, at 6,020-feet.

Geographic entities mentioned:
surface_form: three marys
instance_of: Mountain
countries: United States
coordinates: lat: 37.2083156
lon: -113.0118854
Three Marys (Zion National Park). Three Marys are three sandstone pillars in Zion National Park in Washington County, Utah, United States. Description. Three Marys is situated immediately northwest of Springdale, Utah, and west of the park headquarters. The west peak is highest at 6,420-feet elevation, the middle peak is 6,298-feet, and the east peak is lowest, at 6,020-feet.

Geographic entities mentioned:
surface_form: three marys
instance_of: Mountain
countries: United States
coordinates: lat: 37.2083156
lon: -113.0118854
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Other neighbors include The Sundial, Altar of Sacrifice, Meridian Tower, Bee Hive, Bridge Mountain, The Watchman, and Mount Kinesava. Precipitation runoff from this mountain drains into the North Fork Virgin River. This feature's name, presumably for The Three Marys, was officially adopted in 1934 by the U.S. Board on Geographic Names. Climate.

Geographic entities mentioned:
surface_form: three marys
instance_of: Mountain
countries: United States
coordinates: lat: 37.2083156
lon: -113.0118854
This fourth room is and is cool by reason of the two windows opening toward the trade-wind and one toward the sea. There is a door opposite the entrance that formerly led to a platform and stairway built between this house and the old printing office. The stairway was taken away and the doorway frames a view of Diamond Head as seen through tall coconut trees. The room was early occupied by E. O.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Results. Event was held on the Cerro Catedral on 27 August 2005. The European participants (&quot;italic&quot; in the men's ranking list below) did not count in the continental championship ranking, but appeared in the &quot;International Open&quot; ranking.

Geographic entities mentioned:
surface_form: Cerro Catedral
instance_of: Mountain
countries: Argentina
coordinates: lat: -41.183333333333
lon: -71.45
Pargo Kaling. The Pargo Kaling () was a large chorten straddling across the road leading from Drepung between the Potala's Red Hill (Marpori) and the Iron Hill (Chagpori) at Lhasa, Tibet, and containing a through-passage or archway for people and animals. It formed the &quot;Western Gate&quot; of the city and led into the village of Shol.

Geographic entities mentioned:
surface_form: Chagpori
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.652202777778
lon: 91.109472222222
Lana, South Tyrol. Lana (;) is a &quot;comune&quot; (municipality) and a village in South Tyrol in northern Italy. It is situated in the Etschtal (Etsch Valley) between Bolzano and Merano and at the entrance to the Ultental. The population rose to 12,566 in 2020.

Geographic entities mentioned:
surface_form: Ultental
instance_of: Valley
countries: Italy
coordinates: lat: 46.55
lon: 11
Willcocks suggested to use the depressions of Habbaniyah and Abu Dibis, which he had recognised during his survey, as reservoirs for the excess floodwaters of the Euphrates, as well as to reconstruct the Hindiya Barrage so that the land around Hillah could be used for irrigated agriculture. Only the Hindiya Barrage would be completed before the outbreak of World War I. Construction.

Geographic entities mentioned:
surface_form: Habbaniyah
instance_of: Lake
countries: Iraq
coordinates: lat: 32.296272222222
lon: 43.470725
Harpers Ferry is a historic town in Jefferson County, West Virginia, United States. The population was 269 at the 2020 United States census. Situated at the confluence of the Potomac and Shenandoah Rivers in the lower Shenandoah Valley, where Maryland, Virginia, and West Virginia meet, it is the easternmost town in West Virginia as well as its lowest point above sea level.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Robert Harper, from whom the town takes its name, was born in 1718 in Oxford Township, Pennsylvania, now part of Philadelphia. Since he was a builder, Harper was asked by a group of Quakers in 1747 to build a meeting house in the Shenandoah Valley near the present site of Winchester, Virginia.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Viewing &quot;the passage of the Potomac through the Blue Ridge&quot; from a rock that is now named for him as Jefferson's Rock, he called the site &quot;perhaps one of the most stupendous scenes in nature&quot; and stated, &quot;This scene is worth a voyage across the Atlantic.&quot; The town was one of his favorite retreats, and tradition holds that much of his &quot;Notes on the State of Virginia&quot; was written there.

Geographic entities mentioned:
surface_form: rock
instance_of: Landform
countries: United States
coordinates: lat: 39.32261111111111
lon: -77.73327777777777
The geographical and physical features of Harpers Ferry were the principal reasons for its settlement and eventual industrial development. It is a natural transportation hub and a major river, the Shenandoah, joins the Potomac River at Harpers Ferry. It guarded the entrance to Virginia's large Shenandoah Valley, and the Potomac provided easy access to Washington.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Jamdusan. Jamdusan () is a mountain in Pyeongchang County, Gangwon Province, South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: jamdusan
instance_of: Mountain
countries: South Korea
Evolution of boundaries. The original boundaries of Newcastle were Westmorland County on the south, a line due west from the northern tip of Portage Island on the north, and a north-south line through the mouth of Cains River on the west. In 1814 Northumberland County was completely reorganised and Newcastle took on a more recognisable shape.

Geographic entities mentioned:
surface_form: Cains River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.6653
lon: -65.7772
Distribution and habitat. This correa variety grows in forest or dense scrub, often along streams south from the Goulburn district in New South Wales to eastern Victoria where it is found n places including Buchan, Mount Buffalo, Mount Baw Baw, Warburton and Healesville then extending to the south-west of Melbourne as far as the Otway Ranges.

Geographic entities mentioned:
surface_form: Mount Buffalo
instance_of: Mountain
countries: Australia
coordinates: lat: -36.777
lon: 146.767
surface_form: Mount Baw Baw
instance_of: Mountain
countries: Australia
coordinates: lat: -37.833333333333
lon: 146.26666666667
The bay opens to the east in the southern limits of the East Siberian Sea. It is located northwest of the mouths of the Indigirka and southeast of the mouth of the Bogdashkina. Gusinaya Bay is enclosed in the northeast by the Lopatka Peninsula. Lake Mogotoyevo lies a little inland to the north. The long Gusinaya () and the long Volchya are the main rivers flowing into the head of the bay.

Geographic entities mentioned:
surface_form: Lake Mogotoyevo
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 72.023411111111
lon: 149.14341111111
Name. Ghouta is an Arabic term (&quot;ghuta&quot;) for 'garden'. Geography. The Ghouta is an oasis formed by the Barada River, as its waters flow east of Mount Qasioun, and its seven tributaries. It surrounds the city of Damascus. To the east and south of the Ghouta lies the Marj plain, which forms a narrow belt of fields, and south of that lies the Hauran plain.

Geographic entities mentioned:
surface_form: Mount Qasioun
instance_of: Mountain
countries: Syria
coordinates: lat: 33.545833333333
lon: 36.286388888889
The sediments bear traces of frequent redeposition and mass flows. Ninety–four volcanic ash layers have been emplaced in Potrok Aike during the past 80,000 years, mostly by volcanoes of the Andean Austral Volcanic Zone such as Aguilera, Lautaro (volcano)/Viedma (volcano), Monte Burney and Reclus (volcano). Monte Burney is the main source of tephra at Potrok Aike.

Geographic entities mentioned:
surface_form: Monte Burney
instance_of: Mountain
countries: Chile
coordinates: lat: -52.333333333333
lon: -73.4
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Potrok Aike. Potrok Aike is a maar (a broad volcanic crater) in the Patagonian province of Santa Cruz, Argentina, which contains a brackish lake. It has a roughly square shape and is about wide. The lake is fed by groundwater and occasional inflows through dry valleys, and its water levels have fluctuated over the course of its 770,000-year-long history between overflow and near desiccation.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The variability is driven mainly by changes in wind speed, which change the evaporation rates. Usually, cold periods correlate to higher and warm periods to lower water levels in Potrok Aike. The lake is embedded in a dry steppe region and is one of the few open water bodies there.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
These drill cores were used to reconstruct the climate (temperature, wind and precipitation) and environment of the region, including volcanic activity and changes in Earth's magnetic field. The region around Potrok Aike was periodically glaciated before the maar formed, but later glaciations did no longer reach it.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The region around Potrok Aike was periodically glaciated before the maar formed, but later glaciations did no longer reach it. Sparse volcanic activity built the Pali-Aike volcanic field, which was active until 10,000 years ago east of Potrok Aike. About 12,500 years ago humans first arrived in Patagonia.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Sparse volcanic activity built the Pali-Aike volcanic field, which was active until 10,000 years ago east of Potrok Aike. About 12,500 years ago humans first arrived in Patagonia. They used the resources around Potrok Aike, including rockshelters, to dismember animal kills. The lake itself is inhabited by algae and underwater plants. Etymology and human geography.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Etymology and human geography. The name is part-Tehuelche and part-Spanish: Spanish means &quot;foal&quot; and Tehuelche refers to a place where people stop and store resources. This may indicate that Potrok Aike was a stopping point for local people, as it has a reliable water supply. The region was inhabited by Aónikenk people, before Westerners arrived at the end of the 19th century.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The region was inhabited by Aónikenk people, before Westerners arrived at the end of the 19th century. Sheep grazing is widespread in the region. Politically, Potrok Aike is in Argentina's Santa Cruz Province. The lake can be reached from the National Route 40 between Rio Gallegos and Rio Turbio, which passes about north of Potrok Aike. The border to Chile is about south of Potrok Aike.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The lake can be reached from the National Route 40 between Rio Gallegos and Rio Turbio, which passes about north of Potrok Aike. The border to Chile is about south of Potrok Aike. The &quot;Diego Ritchie&quot; police station lies southwest of the lake, a weather station about northwest and there is a field station of Argentina's National Agricultural Technology Institute. Geography and hydrology.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Water levels fluctuate up to between seasons; interannual variability reaches. The lake is a wide and deep (from above Potrok Aike's water surface) volcanic crater embedded within flat terrain. Beaches are formed by pebbles, sand and silt; there are gravel ridges formed by longshore transport. Water currents eroded the eastern coast.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Hydrology and watershed geomorphology. The waters of the lake are well-mixed by wind, which can form waves up to high and produces a water circulation in Potrok Aike that erodes lakefloor sediments. Water temperatures range between with little differences by depth; temperatures exceeding are rare.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The watershed area covers more than and reaches into Chilean territory; the ephemeral Bandurrias Creek enters Potrok Aike from the west through an U-shaped cascade. Especially on the eastern side there are arroyos, some of which cut lake terraces and which carry water mainly during snowmelt.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Lava plateaus, maars and scoria cones are widespread. Numerous ephemeral lakes and dunes formed by lake sediments dot the landscape around Potrok Aike; unlike them, the great depth of Potrok Aike keeps it water-filled year round. Former meltwater channels from ancient glaciations, one of which passes just west of Potrok Aike and is occupied by Robles Creek and Bandurrias Creek, cross the region.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Lava plateaus, maars and scoria cones are widespread. Numerous ephemeral lakes and dunes formed by lake sediments dot the landscape around Potrok Aike; unlike them, the great depth of Potrok Aike keeps it water-filled year round. Former meltwater channels from ancient glaciations, one of which passes just west of Potrok Aike and is occupied by Robles Creek and Bandurrias Creek, cross the region.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Concretions formed perhaps by microbial activity, mollusc shells, microfossils, plant remains (including phytoliths) and infrequent vivianite concretions complete the sediment package of Potrok Aike. The cold conditions allow the precipitation of ikaite, a warmth-sensitive carbonate mineral, on objects like submerged plants and mooring lines.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Monte Burney is the main source of tephra at Potrok Aike. Cerro Hudson in the Southern Volcanic Zone also emplaced one tephra during the H1 eruption; its H2 eruption has not been identified at Potrok Aike. No tephra deposits have been attributed to the Pali-Aike volcanic field, probably because it is downwind from the lake.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
No tephra deposits have been attributed to the Pali-Aike volcanic field, probably because it is downwind from the lake. Whether peaks in tephra deposition between 72,000–38,000 and 25,000–19,000 years ago reflect an increase of volcanic activity or increased tephra arrival at Potrok Aike is unclear; for Hudson tephras decreased arrival is the likely cause.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Potrok Aike is a maar that formed 770,000 ± 240,000 years ago during a phreatomagmatic eruption, when ascending magma interacted with groundwater. Intense explosions yielded a deep diatreme, now partly filled by the sediments on the floor of Potrok Aike. Phreatomagmatic deposits of the eruption crop out east and southeast of Potrok Aike, and in gullies.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Intense explosions yielded a deep diatreme, now partly filled by the sediments on the floor of Potrok Aike. Phreatomagmatic deposits of the eruption crop out east and southeast of Potrok Aike, and in gullies. The intersection of two tectonic lineaments close to Potrok Aike may have directed magma ascent there, and plentiful groundwater in the area facilitated the development of a maar.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The intersection of two tectonic lineaments close to Potrok Aike may have directed magma ascent there, and plentiful groundwater in the area facilitated the development of a maar. If the volcanic eruption took place during a glaciation, magma–ice interaction might be responsible for Potrok Aike's large size.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
If the volcanic eruption took place during a glaciation, magma–ice interaction might be responsible for Potrok Aike's large size. After its formation, wave erosion and gravitational slumping would have expanded the water surface, explaining why Potrok Aike has no tephra ring and why it is one of the largest maars in the world.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
It is part of the Pali-Aike volcanic field in the back-arc of the Andes. Other volcanic landforms around Potrok Aike are three vents northwest of the lake, an older, 1.19 million years old basaltic lava flow at the southwestern shore of the lake, the Sombrero Mexicano and Hito XXII cones also southeast of Potrok Aike, and the Miocene &quot;Bella Vista Basalts&quot; west of the lake.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Potrok Aike is in the older, western portion of the Pali-Aike volcanic field; more recent volcanic activity took place in its eastern parts 10,000 years ago. Volcanic rocks erupted by Potrok Aike contain peridotite xenoliths derived from the mantle, whose formation began during the Paleoproterozoic 2.5 billion years ago. Geological history.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The sediments deposited by the largest of these glaciations have been named &quot;Potrok Aike Drift&quot; or &quot;Sierra de los Frailes Drift&quot; and were emplaced by a glacier propagating from the Seno Otway.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Simultaneously temperatures rose to a maximum of between 10,400–3,500 years ago. They then declined until present-day. A temporary weakening of the westerlies during the Little Ice Age drove the rise of water levels at that time. Palaeoclimate records at Potrok Aike are not always congruent with records obtained from sites closer to the Andes. Research.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Research. The lake is the subject of an international research effort known as the &quot;Potrok Aike maar lake Sediment Archive Drilling prOject&quot; (PASADO), which is part of the International Continental Scientific Drilling Program and of the &quot;South American Lake Sediment Archives and Modeling&quot; (SALSA) project.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
At its beginning, the effort involved Argentine, German and Swiss scientists, later expanding to include technical personnel and researchers from Argentina, Canada, Germany, Sweden, Switzerland and the USA. The challenges encountered at Potrok Aike led to the development of new lake sediment drilling techniques and the adoption of standards used in marine core studies.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Palaeoclimate research at Potrok Aike has an economic dimension, as the regional economy is vulnerable to short-term droughts. Apart from PASADO, earlier studies were carried out on Potrok Aike to obtain data on its past hydrology, climate and archaeology, and there have been later, independent research efforts.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Apart from PASADO, earlier studies were carried out on Potrok Aike to obtain data on its past hydrology, climate and archaeology, and there have been later, independent research efforts. Palaeoclimate research in the region's lakes began at Magallanes Maar and continued at Potrok Aike and Laguna Azul. Archaeology.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Archaeology. Numerous traces of prior human habitation have been found around Potrok Aike, especially on the uppermost terraces, and rock art is widespread in the area. Potrok Aike played a major role in the human landscape of the region, as it was an important source of water and raw materials.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The region was easily traversable and Potrok Aike accessible from other major sites like Cueva Fell or the Rio Gallegos. The lake was inhabited for a long time; the oldest dated site is about 4,800 years old and was discovered in eroding dunes on the northeastern shore. Other sites with archaeological remains lie northwest of Potrok Aike, including sophisticated rock paintings.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
Other sites with archaeological remains lie northwest of Potrok Aike, including sophisticated rock paintings. The so-called &quot;Potrok Aike type&quot; or &quot;PKA&quot;, a rock type frequently used in tools found at archaeological sites in the region, is named after the frequent findings close to Potrok Aike although it is not exclusive to that lake.

Geographic entities mentioned:
surface_form: potrok aike
instance_of: Lake
countries: Argentina
coordinates: lat: -51.963055555556
lon: -70.379444444444
The album reached number 23 on the &quot;Billboard&quot; Heatseeker Albums chart. Theme. Additionally, CD artwork is based on photographs taken in Barcelona. La Rambla appears on the CD sleeve and images of Montjuïc and El Raval in the booklet and cover.

Geographic entities mentioned:
surface_form: Montjuïc
instance_of: Mountain
countries: Spain
coordinates: lat: 41.364166666667
lon: 2.1580555555556
In September 1658 Gourselas formed a force of 600 militiamen to eliminate the last Island Caribs from the northern Capesterre region of the island. 200 were carried by sea in five ships under Laubière, 200 advanced by land around Mount Pelée and 200 by Morne des Gommiers. The Caribs were soon defeated by the overwhelming French forces and fled towards Dominica and Saint Vincent.

Geographic entities mentioned:
surface_form: Mount Pelée
instance_of: Mountain
countries: France
coordinates: lat: 14.813055555556
lon: -61.165555555556
Muriel Lake (Alberta). Muriel Lake is a closed basin lake in Alberta, Canada. Although its water level has been steadily declining since 1980, this is tied to precipitation and tends to fluctuate in water level.

Geographic entities mentioned:
surface_form: muriel lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.1333
lon: -125.617
surface_form: muriel lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1461
lon: -110.689
Muriel Lake (Alberta). Muriel Lake is a closed basin lake in Alberta, Canada. Although its water level has been steadily declining since 1980, this is tied to precipitation and tends to fluctuate in water level.

Geographic entities mentioned:
surface_form: muriel lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.1333
lon: -125.617
surface_form: muriel lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.1461
lon: -110.689
surface_form: basin lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.63336
lon: -105.28386
1980 Critérium du Dauphiné Libéré. The 1980 Critérium du Dauphiné Libéré was the 32nd edition of the cycle race and was held from 26 May to 2 June 1980. The race started in Évian-les-Bains and finished at Mont Revard. The race was won by Johan van der Velde of the TI–Raleigh team.

Geographic entities mentioned:
surface_form: Mont Revard
instance_of: Mountain
countries: France
coordinates: lat: 45.681944444444
lon: 5.9744444444444
Bowditch Crests. w73ywf8gm9q74mwk4vtybfcvspbt" xml:space="preserve">#redirect Bowditch Crests

Geographic entities mentioned:
surface_form: bowditch crests
instance_of: Mountain
coordinates: lat: -68.5
lon: -65.3667
Mount Palmer (Northern Territory). Mount Palmer is a mountain with an elevation of in the southern part of the Northern Territory of Australia. It is part of the Central Desert Region and was named by the explorer Ernest Giles. Mount Palmer is part of the Central Harts Range, and is known for being the site of mica mining in the past. Nearby settlements include Hart Range.

Geographic entities mentioned:
surface_form: mount palmer
instance_of: Mountain
countries: Australia
coordinates: lat: -23.0775
lon: 134.9425
Most species have at least one hooked spine at each areole. Less often, species may not have hooks. These plants are found in higher elevation deserts such as on the Colorado Plateau, or in the Mohave Desert or the Great Basin. They are well suited to extremes due to lack of rainfall, hot summers and below freezing winters.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
Quanchus Range. The Quanchus Range is a subrange of the Nechako Plateau in the Interior of British Columbia, Canada, located on the north end of Tweedsmuir North Provincial Park and Protected Area. It is almost completely an island after the creation of the Nechako Reservoir. Its two main summits are Michel Peak (2260m) and Tweedsmuir Peak (2194m).

Geographic entities mentioned:
surface_form: Nechako Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 54.49979
lon: -126.00334
Historical references to a village or town may actually be to a different location. For instance when the explorer David Livingstone visited Mwata Kazembe in 1867 and 1868, &quot;Casembe's town&quot;, as he wrote it, was further north at the town now called Kanyembo. Mwansabombwe is situated where the Ngona River enters the swamps of the Luapula River south of Lake Mweru.

Geographic entities mentioned:
surface_form: Lake Mweru
instance_of: Lake
countries: Zambia
Democratic Republic of the Congo
coordinates: lat: -9.1666666666667
lon: 28.5
Rocotopunta (Quechua &quot;rukutu,&quot; a plant &quot;(Capsicum pubescens)&quot; and Spanish &quot;punta,&quot; a peak or ridge) is a mountain in the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Recuay Province, Ticapampa District, northeast of Lake Querococha. Rocotopunta lies between Yanamarey Creek to the north and Conde Creek to the south.

Geographic entities mentioned:
surface_form: Lake Querococha
instance_of: Lake
countries: Peru
coordinates: lat: -9.7161111111111
lon: -77.324166666667
surface_form: querococha
instance_of: Lake
countries: Peru
coordinates: lat: -9.7161111111111
lon: -77.324166666667
surface_form: lake querococha
instance_of: Lake
countries: Peru
coordinates: lat: -9.7161111111111
lon: -77.324166666667
Rocotopunta (Recuay). Rocotopunta (Quechua &quot;rukutu,&quot; a plant &quot;(Capsicum pubescens)&quot; and Spanish &quot;punta,&quot; a peak or ridge) is a mountain in the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Recuay Province, Ticapampa District, northeast of Lake Querococha.

Geographic entities mentioned:
surface_form: rocotopunta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.03805556
lon: -77.68527778
surface_form: rocotopunta (recuay)
instance_of: Mountain
countries: Peru
coordinates: lat: -9.70556
lon: -77.3075
Rocotopunta (Recuay). Rocotopunta (Quechua &quot;rukutu,&quot; a plant &quot;(Capsicum pubescens)&quot; and Spanish &quot;punta,&quot; a peak or ridge) is a mountain in the Cordillera Blanca in the Andes of Peru, about high. It is located in the Ancash Region, Recuay Province, Ticapampa District, northeast of Lake Querococha.

Geographic entities mentioned:
surface_form: rocotopunta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.03805556
lon: -77.68527778
surface_form: rukutu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.93722222
lon: -76.22083333
surface_form: rocotopunta
instance_of: Mountain
countries: Peru
coordinates: lat: -9.70556
lon: -77.3075
Fenwick Bridge over the George Washington Memorial Parkway, the Potomac River, and Ohio Drive. At the end of the bridge, the Yellow Line re-enters a tunnel near the Jefferson Memorial and crosses under the Washington Channel. The tunnel merges with the Green Line tunnel under 7th Street Southwest just south of the L'Enfant Plaza.

Geographic entities mentioned:
surface_form: Washington Channel
instance_of: Watercourse
countries: United States
coordinates: lat: 38.8787232
lon: -77.0271988
Since the 12th century, the archaic term was gradually replaced by &quot;Lombardia&quot; (as a linguistic evolution, first appeared in the &quot;Pauli Continuatio&quot;) and in the geographic view it indicated first the area of the Langobardia Maior and then only the Po Valley, where the centre of the Lombard power was located.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The Cumberland Narrows (or simply The Narrows) is a water gap in western Maryland in the United States, just west of Cumberland. Wills Creek cuts through the central ridge of the Wills Mountain Anticline at a low elevation here between Wills Mountain to the north and Haystack Mountain to the south. Cliffs and talus of the two mountains' Tuscarora quartzite caprock are prominent within the Narrows.

Geographic entities mentioned:
surface_form: Wills Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.845555555556
lon: -78.681666666667
The geological features of the Narrows provide Cumberland a western backdrop of the two mountains with a narrow gap between them. Geography. The Cumberland Narrows serves as a western gateway from Cumberland to the Appalachian Plateau and the Ohio River Valley beyond. Nemacolin's Path, which later became Old National Road and is now Alternate U.S.

Geographic entities mentioned:
surface_form: Appalachian Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 40
lon: -78
At, it is the highest point of the Jayawijaya (Orange) Range and is included in Seven Second Summits. Following Puncak Jaya/Mount Carstensz (4884 m) 350 km to the west, Mandala is the second-highest freestanding mountain in Oceania, Australasia, New Guinea, and Indonesia. Etymology.

Geographic entities mentioned:
surface_form: Puncak Jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: carstensz
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: mount carstensz
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: jaya
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
The mountain is believed to be the center of the universe and the mythical place where &quot;Atangki&quot; resides. Geology. Mandala is one of the three high massifs of Western New Guinea, together with the Carstensz and Trikora complexes. This peak used to have an ice cap, but it was last seen in 1989 and by 2003 it was gone.

Geographic entities mentioned:
surface_form: Carstensz
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: Trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
surface_form: carstensz
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.0833333333333
lon: 137.18333333333
surface_form: trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
Geology. Mandala is one of the three high massifs of Western New Guinea, together with the Carstensz and Trikora complexes. This peak used to have an ice cap, but it was last seen in 1989 and by 2003 it was gone. Based on the Shuttle Radar Topography Mission data, this peak is likely higher than Puncak Trikora, which lost its icecap in about 1960. Ascents.

Geographic entities mentioned:
surface_form: Puncak Trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
surface_form: trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
surface_form: puncak trikora
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.35
lon: 138.65
Puncak Mandala. Puncak Mandala or Mandala Peak (until 1963 Julianatop or Juliana Peak) is a mountain located in Highland Papua, Indonesia. At, it is the highest point of the Jayawijaya (Orange) Range and is included in Seven Second Summits.

Geographic entities mentioned:
surface_form: puncak mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
Puncak Mandala. Puncak Mandala or Mandala Peak (until 1963 Julianatop or Juliana Peak) is a mountain located in Highland Papua, Indonesia. At, it is the highest point of the Jayawijaya (Orange) Range and is included in Seven Second Summits.

Geographic entities mentioned:
surface_form: puncak mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
surface_form: julianatop
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
surface_form: juliana peak
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
Etymology. Locally, the mountain peak is called &quot;Aplim Apom&quot;, a holy place where the creator &quot;Atangki&quot; created humans, &quot;Aplim Apom Sibilki&quot; (children of Aplim Apom). Under Indonesian administration, the mountain is called &quot;Mandala Peak&quot;.

Geographic entities mentioned:
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
Under Indonesian administration, the mountain is called &quot;Mandala Peak&quot;. While the reasoning was not recorded at the time, the name &quot;Mandala&quot; corresponds with the &quot;Aplim Apom&quot; creation myth. The mountain is believed to be the center of the universe and the mythical place where &quot;Atangki&quot; resides. Geology.

Geographic entities mentioned:
surface_form: mandala
instance_of: Mountain
countries: Indonesia
coordinates: lat: -4.7086111111111
lon: 140.28916666667
The South River divides a peninsula from the rest of the town, where Rexhame village and the Humarock and Fourth Cliff neighborhoods of the town of Scituate lie. The Scituate neighborhoods can be reached by land by two bridges, by boat, or by foot along Rexhame Beach.

Geographic entities mentioned:
surface_form: Humarock
instance_of: Landform
countries: United States
coordinates: lat: 42.1361
lon: -70.6906
It was opened in October 2010. Travelling from east to west, the route of the Dublin Mountains Way starts on the Main Street of Shankill and passes through Rathmichael, Carrickgollogan, Barnaslingan, Glencullen, Ballyedmonduff, Three Rock, Two Rock, Tibradden Mountain, Cruagh Wood, Featherbed Forest, Glenasmole and Kiltipper before ending at Seán Walsh Memorial Park in Tallaght.

Geographic entities mentioned:
surface_form: Carrickgollogan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.21642
lon: -6.157932
surface_form: Barnaslingan
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.21945556
lon: -6.17663889
surface_form: Two Rock
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.236194444444
lon: -6.2415555555556
surface_form: Tibradden Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.238744444444
lon: -6.2801583333333
The vision document published in 2006 by the Dublin Mountains Initiative included a proposal for a &quot;Dublin Way&quot;, similar to what has now been developed. Work commenced on the Dublin Mountains Way in September 2008 with the upgrade of the trail at Tibradden Mountain.

Geographic entities mentioned:
surface_form: Tibradden Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.238744444444
lon: -6.2801583333333
The Way originally passed through St Ann's graveyard in Glenasmole to reach the Bohernabreena Waterworks but now follows the road to Castlekelly Bridge, entering the Waterworks at its southern end. Following an agreement with a local landowner, some of trail has been taken off-road by facilitating access to Three Rock Mountain via private forestry at Ballyedmonduff.

Geographic entities mentioned:
surface_form: Three Rock Mountain
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.245277777778
lon: -6.2391666666667
A further major change occurred in 2013: originally the route included an optional looped route around Massy's Estate and the Hell Fire Club on Montpelier Hill; this part of the route was removed to comply with the international classification rules for walking trails, which require trails to be continuous and without detours or loops. Shankill and Rathmichael.

Geographic entities mentioned:
surface_form: Montpelier Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.251861111111
lon: -6.3303444444444
C. Hart who, in 1886, made, and won, a bet that he could walk from Terenure in Dublin to the summit of Lugnaquilla in Wicklow in 24 hours. Leaving Cruagh Wood, walkers have the choice of either following a circular spur route via Massy's Estate and the Hell Fire Club or to continue direct to Glenasmole via the Featherbed Forest. Glenasmole and Tallaght.

Geographic entities mentioned:
surface_form: Lugnaquilla
instance_of: Mountain
countries: Ireland
coordinates: lat: 52.966
lon: -6.463
Its distribution extends from Massachusetts to Georgia, westward to at least Alabama, and the lichen also occurs in disjunct populations at high elevations of the southern Appalachian Mountains, riparian conifer forests along the edges of the Ozarks and the Ouachita Mountains, the oceanic forests of the Canadian Maritimes, and conifer swamps of the Great Lakes Region.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
Teviotdale cheese. Teviotdale is a full fat hard cheese produced in the area of Teviotdale on the border lands between Scotland and England, within a radius of 90 km from the summit of Peel Fell in the Cheviot Hills. The cheese is produced from the milk of the Jersey cattle. There are no known current producers of this cheese. Description.

Geographic entities mentioned:
surface_form: Peel Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.28333
lon: -2.58333