Sarmila/GeoWiki-Features huggingface dataset:
In 1928, Nelson Horatio Darton of the United States Geological Survey observed: “On the east side of the Pecos Valley in southern New Mexico there are very extensive sand hills formed of deposits known as the ‘Mescalero Sands,’ which are doubtless of Quaternary age...” In places, these sands climb up and over the Mescalero Ridge and spread out over portions of the Llano Estacado.

Geographic entities mentioned:
surface_form: mescalero ridge
instance_of: Mountain
countries: United States
coordinates: lat: 33.0431
lon: -103.854
[2]
Each of the three dunes are eroding from a Pleistocene lakebed that dates to 13,000 years ago.[5]
They are located at the base of the Mescalero Ridge known locally as the &quot;Caprock&quot; on the western side of the Llano Estacado between Tatum and Roswell, New Mexico five miles south of the north sands recreational area.

Geographic entities mentioned:
surface_form: mescalero ridge
instance_of: Mountain
countries: United States
coordinates: lat: 33.0431
lon: -103.854
Gamel's birth gift to his grandson was a present Gamel had received from Nansen: the compass Nansen carried on his Greenland icecap expedition. Knuth studied building technology at Royal Danish Academy of Fine Arts, and then woodcarving at Val Gardena in Italy between 1926 and 1928.

Geographic entities mentioned:
surface_form: Val Gardena
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Assisting Dr. Roussell and Dr. Poul Nørlund during the summer of 1934, Knuth excavated old Norse ruins at Igaliko. In 1935, Dr. Helge Larsen, Ebbe Munck, and Knuth, as archaeologist, assisted on the Augustine Courtauld Expedition to East Greenland, during which Gunnbjørn Fjeld, Greenland's highest mountain, was climbed.

Geographic entities mentioned:
surface_form: Gunnbjørn Fjeld
instance_of: Mountain
countries: Greenland
coordinates: lat: 68.9195
lon: -29.898533333333
Gneiskopf Peak. Gneiskopf Peak () is a peak high rising southwest of Mount Neustruyev at the southern end of the Südliche Petermann Range, in the Wohlthat Mountains of Queen Maud Land, Antarctica. It was discovered and given the descriptive name Gneiskopf (gneiss peak) by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher.

Geographic entities mentioned:
surface_form: Mount Neustruyev
instance_of: Mountain
coordinates: lat: -71.85
lon: 12.2333
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: gneiskopf peak
instance_of: Mountain
coordinates: lat: -71.933333333333
lon: 12.116666666667
Gneiskopf Peak. Gneiskopf Peak () is a peak high rising southwest of Mount Neustruyev at the southern end of the Südliche Petermann Range, in the Wohlthat Mountains of Queen Maud Land, Antarctica. It was discovered and given the descriptive name Gneiskopf (gneiss peak) by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher.

Geographic entities mentioned:
surface_form: alfred
instance_of: Mountain
coordinates: lat: -70.31133
lon: -69.23369
surface_form: gneiskopf
instance_of: Mountain
coordinates: lat: -71.933333333333
lon: 12.116666666667
Gneiskopf Peak. Gneiskopf Peak () is a peak high rising southwest of Mount Neustruyev at the southern end of the Südliche Petermann Range, in the Wohlthat Mountains of Queen Maud Land, Antarctica. It was discovered and given the descriptive name Gneiskopf (gneiss peak) by the Third German Antarctic Expedition (1938–1939), led by Captain Alfred Ritscher.

Geographic entities mentioned:
surface_form: gneiskopf
instance_of: Mountain
coordinates: lat: -71.933333333333
lon: 12.116666666667
History. According to Scrivener the manuscript was written in the 11th century, according to C. R. Gregory it was written in the 12th century. Currently the manuscript is dated by the INTF to the 12th century. Formerly it was held in the Karakalou monastery at Athos peninsula. It was bought by Robert Curzon in 1837. C. R. Gregory saw it in 1883.

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Grønnligrotta. Grønnligrotta is a marble karst cave in Rana Municipality in Nordland county, Norway. It is located in the valley of Røvassdalen, and was first explored in 1914. It has a total depth of and explored length of. It is probably connected to the nearby Setergrotta. The cave is equipped with artificial lights and open for tourists.

Geographic entities mentioned:
surface_form: Røvassdalen
instance_of: Valley
countries: Norway
coordinates: lat: 66.41666667
lon: 14.23333333
Yatung. Yatung or Yadong, also known as Shasima (,),
is the principal town in the Chumbi Valley or Yadong County in the
Tibet Autonomous Region of China. It is also its administrative headquarters. Name. The village is known locally as Shasima (&quot;Sharsingma&quot;) to the Tibetans, believed to be a Lepcha name.

Geographic entities mentioned:
surface_form: Chumbi Valley
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.4893046
lon: 88.9050579
During the British Raj era, it was called Yatung, the name having been transferred from another location called &quot;Yatung&quot; in the valley between the Jelep La and Rinchengang. The original location later came to be called Old Yatung. The Chinese administration of Tibet uses the name Yatung/Yadong for the county, and the name Shasima for the town. Geography.

Geographic entities mentioned:
surface_form: Old Yatung
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 27.42452
lon: 88.9069
It was bordered on the west by Bugna and the Afar lowlands to the east and southeast, Ambassel to the southwest and Tigray to the north. Portuguese explorer Francisco Álvares wrote that the boundary between Angot and Tigray was the Sabalete River located north-east of Lake Ashenge. Axumite history.

Geographic entities mentioned:
surface_form: Lake Ashenge
instance_of: Lake
countries: Ethiopia
coordinates: lat: 12.580555555556
lon: 39.5
Axumite history. Under the reign of Degna Djan, during the 10th century, the empire kept expanding south, and sent troops into the modern-day region of Ennarea, while at the same time undertaking missionary activity into Angot. Emperor Dil Na'od is said to have relocated the capital to Ku'bar on the shore of Lake Hayq, south of Angot, and built the Istifanos Monastery.

Geographic entities mentioned:
surface_form: Lake Hayq
instance_of: Lake
countries: Ethiopia
coordinates: lat: 11.333333333333
lon: 39.716666666667
Poclușa (river). The Poclușa is a left tributary of the Crișul Negru in western Romania. It flows into the Crișul Negru near Șoimi. Its length is and its basin size is.

Geographic entities mentioned:
surface_form: Crișul Negru
instance_of: Watercourse
countries: Romania
Hungary
coordinates: lat: 46.700277777778
lon: 21.269166666667
If &quot;Mahavamsa&quot; is correct, Sinhapura could not have been located in today's Odisha or Andhra Pradesh, because these places lie to the south of Bengal, away from Bihar. He, therefore, concludes that the Sinhapura of &quot;Mahavamsa&quot; was different from the capital city mentioned in records of Kalinga's rulers: it was probably located in the present-day Chota Nagpur area. S.

Geographic entities mentioned:
surface_form: Chota Nagpur
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
The lakebed at Fossil Lake was formed during the post-Pleistocene period from lake sediments and alluvial materials. Pumice sands from Mount Mazama and Newberry Crater also appear in the surface soils throughout the Fossil Lake area. The surface soils are underlain by a hard calcium carbonate caliche layer several inches thick.

Geographic entities mentioned:
surface_form: Mount Mazama
instance_of: Mountain
countries: United States
coordinates: lat: 42.9165186
lon: -122.0844711
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Fossil Lake (Oregon). Fossil Lake (designated by the Bureau of Land Management as Fossil Lake Area of Critical Environmental Concern) is a dry lakebed in the remote high desert country of northern Lake County in the U.S. state of Oregon. During the Pleistocene epoch, Fossil Lake and the surrounding basin were covered by an ancient lake. Numerous animals used the lake's resources.

Geographic entities mentioned:
surface_form: fossil lake (oregon)
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Fossil Lake (Oregon). Fossil Lake (designated by the Bureau of Land Management as Fossil Lake Area of Critical Environmental Concern) is a dry lakebed in the remote high desert country of northern Lake County in the U.S. state of Oregon. During the Pleistocene epoch, Fossil Lake and the surrounding basin were covered by an ancient lake. Numerous animals used the lake's resources.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Fossil Lake (Oregon). Fossil Lake (designated by the Bureau of Land Management as Fossil Lake Area of Critical Environmental Concern) is a dry lakebed in the remote high desert country of northern Lake County in the U.S. state of Oregon. During the Pleistocene epoch, Fossil Lake and the surrounding basin were covered by an ancient lake. Numerous animals used the lake's resources.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Numerous animals used the lake's resources. Over time, the remains of many of these animals became fossilized in the lake sediments. As a result, Fossil Lake has been an important site for fossil collection and scientific study for well over a century. Over the years, paleontologists have found the fossil remains of numerous mammals as well as bird and fish species there.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Some of these fossils are 2 million years old. Location. Fossil Lake is located in a remote area of northern Lake County, Oregon. It is from the unincorporated community of Christmas Valley by road. Fossil Lake is approximately southeast of Bend and north of Lakeview by straight-line distance.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
It is from the unincorporated community of Christmas Valley by road. Fossil Lake is approximately southeast of Bend and north of Lakeview by straight-line distance. From Christmas Valley, visitors travel east on County Road 5–14 (&quot;Christmas Valley-Wagontire Road&quot;) for, then turn north on County Road 5-14D (&quot;Fossil Lake Road&quot;).

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Fossil Lake is approximately southeast of Bend and north of Lakeview by straight-line distance. From Christmas Valley, visitors travel east on County Road 5–14 (&quot;Christmas Valley-Wagontire Road&quot;) for, then turn north on County Road 5-14D (&quot;Fossil Lake Road&quot;). Travel and then turn east onto the County Road 5-14E (&quot;Lost Forest Road&quot;), a gravel road.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
After approximately, turn south onto a rough unmarked dirt road. The Fossil Lake interpretive sign is approximately from the turnoff. Vehicles are not allowed in the Fossil Lake Area of Critical Environmental Concern, so visitors must walk the last to the Fossil Lake interpretive sign. Fossil Lake itself is southwest of the sign. Geology and natural history.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
This basin filled with water during the wet climatic periods of the Pleistocene and post-Pleistocene to a depth of. Over the past 3,200 years, the surface water in the Christmas Valley basin including Fossil Lake has completely dried up, leaving a high-desert environment. The lakebed at Fossil Lake was formed during the post-Pleistocene period from lake sediments and alluvial materials.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
This locally unique water-retentive sub-surface structure has helped the ponderosa pines in nearby Lost Forest Research Natural Area survive in the high-desert environment. In 1877, there were still two small seasonal ponds at the Fossil Lake site surrounded by a large dry lakebed. The two ponds were called the &quot;Fossil Lakes&quot;. Since then, both ponds have dried up completely.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The elevation of the lakebed is above sea level. There are large moving sand dunes east of the lakebed. These dunes are made up of lacustrine sediments, aeolian deposits, and alluvial materials with large amounts of volcanic pumice and ash mixed into fine sand that have been blown off the surface of Fossil Lake. History. The first settlers arrived in the Christmas Lake Valley around 1865.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
History. The first settlers arrived in the Christmas Lake Valley around 1865. In June 1877, John Whiteaker (a former governor of Oregon) visited the Christmas Valley basin. During the trip, Whiteaker explored the Fossil Lake area, where he found a large dry lakebed with two small alkali ponds in low spots. Whiteaker named the ponds the &quot;Fossil Lakes&quot;.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Later that year, Whiteaker's son, J.C. Whiteaker, returned to Fossil Lake with professor Condon. The goal of this second expedition was to more carefully examine and record the numerous fossils scattered around the Fossil Lake site. Condon's discoveries at Fossil Lake attracted the attention of other well-known paleontologists.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The goal of this second expedition was to more carefully examine and record the numerous fossils scattered around the Fossil Lake site. Condon's discoveries at Fossil Lake attracted the attention of other well-known paleontologists. After the first site surveys in 1877, numerous paleontologists have visited Fossil Lake to collect fossils and conduct research. In 1879, Professor Edward D.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Condon's discoveries at Fossil Lake attracted the attention of other well-known paleontologists. After the first site surveys in 1877, numerous paleontologists have visited Fossil Lake to collect fossils and conduct research. In 1879, Professor Edward D. Cope of the Philadelphia Academy of Sciences visited Condon at the University of Oregon and then went to Fossil Lake to collect fossils.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Wortman of the American Museum of Natural History; and Robert W. Shufeldt, curator of the Army Medical Museum. Both Sternberg and Wortman led expeditions that collected for professor Cope. The Smithsonian Institution also began research at Fossil Lake in the late 1800s. In 1901, Annie M. Alexander visited Fossil Lake to collect fossils. She sent her specimens to University of California.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
She sent her specimens to University of California. During this period, local settlers reported that fossils were often removed by the wagon load. After 1906, the number of homesteads in the Christmas Valley basin began to increase. In that year, a post office was opened at &quot;Cliff&quot;, just north of Fossil Lake. Settlers used the Fossil Lake area for grazing sheep, cattle, and horses.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
In addition, Chester Stock and E. L. Furlong conducted summers digs at the site of 1923 and 1924. Stock and Furlong sent their finds to the University of California. In 1977, the Bureau of Land Management placed a temporary ban on vehicles in the Fossil Lake area. The restriction applied to around the dry lakebed. In 1979, the Bureau of Land Management made the vehicle ban permanent.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The restriction applied to around the dry lakebed. In 1979, the Bureau of Land Management made the vehicle ban permanent. In 1983, the Bureau of Land Management joined Fossil Lake, the neighboring Lost Forest Research Natural Area, and the Christmas Valley Sand Dunes into a single Area of Critical Environmental Concern.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Collecting fossils in the Fossil Lake Area of Critical Environmental Concern without a permit from the Bureau of Land Management is prohibited. In early 1990s, the Bureau of Land Management began working with the South Dakota School of Mines to salvage fossils and conduct paleontological research at Fossil Lake. This collaboration lasted well over a decade.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Scientists believe the tracks were made approximately 43,000 years ago. Fossils. The fossil-bearing deposits at Fossil Lake cover at least. Over the years, there have been numerous expeditions to collect fossils at the Fossil Lake site. The site has produced more Holocene fossils than any other location in the world except the La Brea Tar Pits in California.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Fish fossils include tui chub and several salmon species. Two-thirds of the fossil species collected at Fossil Lake are extinct. The extent of the fossil beds at the Fossil Lake site is still unknown; stratigraphically specific rock layers laid down at different periods each contain characteristic fossils of different animals.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Some prey may have been large mammals that are now extinct. The oldest fossils from the site date back to the Pleistocene epoch. These fossils are up to 2 million years old. The Bureau of Land Management has identified several environmental concerns with regard to the Fossil Lake site. First, the fossil deposits extend beyond the boundary of the existing restricted area.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
Environment. Based on National Weather Service data recorded at Cliff between 1908 and 1916 and other nearby weather reporting stations, the mean annual temperature in the Fossil Lake area is. The hottest and driest months are July and August, with a peak average temperature of. The coldest months are December and January. The average daily temperature in December is and in January.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
However, weather patterns in this area are very erratic. For example, there was an extremely severe drought throughout the 1920s and early 1930s. The Fossil Lake area supports a plant community dominated by big sagebrush, low sagebrush, silver sagebrush, green rabbitbrush (also called yellow rabbitbrush), rubber rabbitbrush, and greasewood.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The Fossil Lake area supports a plant community dominated by big sagebrush, low sagebrush, silver sagebrush, green rabbitbrush (also called yellow rabbitbrush), rubber rabbitbrush, and greasewood. There are a number of perennial grasses common in the Fossil Lake area, including Sandberg bluegrass, needle-and-thread grass, Indian ricegrass, creeping wildrye, and invasive cheatgrass.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
There are a number of perennial grasses common in the Fossil Lake area, including Sandberg bluegrass, needle-and-thread grass, Indian ricegrass, creeping wildrye, and invasive cheatgrass. Perennial flowering plants found in the Fossil Lake area include prickly-phlox, lemon scrufpea common wooly sunflower, and Townsend daisy, and spiny hopsage. Wildlife.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The larger mammals include pronghorn, American badger, and coyotes. Black-tailed jackrabbits, Ord's kangaroo rats, deer mice, Great Basin pocket mice, and northern grasshopper mice are among the smaller animals found in the Fossil Lake area. There also 13 bat species that live in the desert around Fossil Lake. In 1917, a diminutive bear was killed near Fossil Lake.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
The larger mammals include pronghorn, American badger, and coyotes. Black-tailed jackrabbits, Ord's kangaroo rats, deer mice, Great Basin pocket mice, and northern grasshopper mice are among the smaller animals found in the Fossil Lake area. There also 13 bat species that live in the desert around Fossil Lake. In 1917, a diminutive bear was killed near Fossil Lake.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
There are also birds of prey such as prairie falcon, red-tailed hawks, and golden eagles. There are a number of reptiles found in the Fossil Lake area, both snakes and lizards. Snakes found in the area around Fossil Lake include western rattlesnakes, gopher snakes, striped whipsnakes, and night snakes.

Geographic entities mentioned:
surface_form: fossil lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3258
lon: -120.491
These dunes are made up of lacustrine sediments, aeolian deposits, and alluvial materials with large amounts of volcanic pumice and ash mixed into fine sand that have been blown off the surface of Fossil Lake. History. The first settlers arrived in the Christmas Lake Valley around 1865. In June 1877, John Whiteaker (a former governor of Oregon) visited the Christmas Valley basin.

Geographic entities mentioned:
surface_form: lake valley
instance_of: Valley
countries: United States
coordinates: lat: 38.3189
lon: -114.607
The coastal plain is characterized by short rivers and frequent lagoons and bays, and lies within the humid tropical Serra do Mar coastal forests ecoregion. The plateau to the west of the range is drained by tributaries of the Uruguay River, including the Pelotas and Canoas, and by the Jacuí River and its tributaries, which drains south into the Lagoa dos Patos of Rio Grande do Sul.

Geographic entities mentioned:
surface_form: Lagoa dos Patos
instance_of: Lake
countries: Brazil
coordinates: lat: -31.15
lon: -51.39
Magura (Western Tatras). Magura is a peak located in the Kasprowy Wierch massif, part of the Western Tatras in Poland. The peak is located between the Uhrocie Kasprowe and the Mała Kopa Królowa in the Western Tatras. The name of the peak originates from the Vlachs, pastoral peoples which introduced grazing to the Tatra Mountains.

Geographic entities mentioned:
surface_form: Kasprowy Wierch
instance_of: Mountain
countries: Slovakia
Poland
coordinates: lat: 49.231666666667
lon: 19.981666666667
surface_form: magura
instance_of: Mountain
countries: Poland
coordinates: lat: 49.2486
lon: 20.0006
Magura (Western Tatras). Magura is a peak located in the Kasprowy Wierch massif, part of the Western Tatras in Poland. The peak is located between the Uhrocie Kasprowe and the Mała Kopa Królowa in the Western Tatras. The name of the peak originates from the Vlachs, pastoral peoples which introduced grazing to the Tatra Mountains.

Geographic entities mentioned:
surface_form: magura (western tatras)
instance_of: Mountain
countries: Poland
coordinates: lat: 49.2486
lon: 20.0006
The cave has a highest fall of about 10 metres. In the central part there is a fort wall structure which is now broken. It consists of an extremely narrow gorge formed in a conglomerate limestone area on Doon Valley's Dehra plateau. It is a natural cave formation where rivers flow inside the cave. The place is a popular tourist spot and which is now being maintained by Uttarakhand State.

Geographic entities mentioned:
surface_form: Doon Valley
instance_of: Valley
countries: India
coordinates: lat: 30.361
lon: 77.992
Tămășeni () is a commune in Neamț County, Western Moldavia, Romania. It is composed of two villages, Adjudeni (&quot;Dzsidafalva&quot;) and Tămășeni. The commune is situated on the Moldavian Plateau, at an altitude of, on the right bank of the Siret River. It is located in the eastern part of Neamț County, north of Roman and east of the county seat, Piatra Neamț, on the border with Iași County.

Geographic entities mentioned:
surface_form: Moldavian Plateau
instance_of: Plateau
countries: Romania
Moldova
Ukraine
coordinates: lat: 45.55195806
lon: 27.92844
St. George Lake. St. George Lake is the fourth largest lake in Waldo County, Maine, United States. It is in the township of Liberty, on the western side of Waldo County. Lake St. George State Park is on the northwest shore of the lake. It contains the island of Hawaii 2. The lake is populated with at least 14 species of fish, including salmon, brook trout (stocked since 1980), and smallmouth bass.

Geographic entities mentioned:
surface_form: st. george lake
instance_of: Lake
countries: United States
coordinates: lat: 44.3877634
lon: -69.336092
The fortress was founded with the permission of Bashkir Tarkhan Taymas Shaimov, who was the owner of these lands. Town status was granted to it on October 25, 1951. 2013 meteor event. In February 2013, a meteor exploded in Earth's atmosphere and a part of it fell into Lake Chebarkul causing a wide hole in the ice covering the lake. Administrative and municipal status.

Geographic entities mentioned:
surface_form: Lake Chebarkul
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54.964722222222
lon: 60.316944444444
In this, he appears to be quite successful, for one and all of his subjects seem to bear for him a real affection. Permanent representation was established soon after founding of Addis Ababa in 1896. During this period, Emperor Menelik II allotted 100 acre of land to British agency at the foot of Entoto Hills.

Geographic entities mentioned:
surface_form: Entoto
instance_of: Mountain
countries: Ethiopia
coordinates: lat: 9.1155555555556
lon: 38.772222222222
Design. It is estimated that approximately 15,000 people are buried in the cemetery. It is located on a hill in the south of the city overlooking the Caspian Sea. It is considered a shrine to those who have given their lives for Azerbaijan's independence and attracts thousands of visitors each year. Memorials.

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
Both the winged adults are preserved as inclusions in transparent chunks of yellow Burmese amber shaped and polished before study. The amber specimen was recovered from the amber deposits of Hukawng Valley, Kachin State in Myanmar. The specific origin location for the fossils is unidentified since the amber pieces were obtained from traders after mining.

Geographic entities mentioned:
surface_form: Hukawng Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 26.438333333333
lon: 96.558888888889
The most important crop is rice, while other important products are beans and maize. Services provide employment for 2% of the population. There is a tobacco planting concession in this municipality since 1930. Nowadays 4500 ha are planted. Rivers. This municipality is crossed by the Sakeny and Manambolo Rivers. Roads. In its north-west part, this municipality is crossed by the National road 34.

Geographic entities mentioned:
surface_form: Manambolo River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -19.24025
lon: 44.33283333333333
Løyndbreen. Løyndbreen (&quot;The Hidden Glacier&quot;) is a glacier in Nathorst Land at Spitsbergen, Svalbard. It has a length of about four kilometers, situated between the mountains of Bassøefjellet and Langlifjellet, and extending towards the valley of Bromelldalen.

Geographic entities mentioned:
surface_form: Bassøefjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.7
lon: 16.114
surface_form: Langlifjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.722
lon: 16.15
surface_form: Bromelldalen
instance_of: Valley
countries: Norway
coordinates: lat: 77.715
lon: 15.9
A park in the Saint Boniface area of Winnipeg is named after the poet in recognition of his poem &quot;The Red River Voyageur&quot;. Whittier Education Campus in Washington, DC, is named in his honor. SS &quot;Whittier Victory&quot; a World War II ship named after Whittier College. Whittier Peak and Mount Whittier in Washington and Mount Whittier in New Hampshire are mountains named after him.

Geographic entities mentioned:
surface_form: Whittier Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.946944444444
lon: -121.03138888889
Becca di Luseney (French: Pic de Luseney) (3,502m) is a mountain of the Pennine Alps in Aosta Valley, northwest Italy. It has a pyramidal look on all four sides, and its north face is covered with a glacier. A huge rockfall from its southwest face came down in 1952, completely destroying the village of Chamen and other settlements in the Valpelline valley. The mountain was first climbed in 1866.

Geographic entities mentioned:
surface_form: valpelline
instance_of: Valley
countries: Italy
coordinates: lat: 45.83
lon: 7.33
Becca di Luseney. Becca di Luseney (French: Pic de Luseney) (3,502m) is a mountain of the Pennine Alps in Aosta Valley, northwest Italy. It has a pyramidal look on all four sides, and its north face is covered with a glacier. A huge rockfall from its southwest face came down in 1952, completely destroying the village of Chamen and other settlements in the Valpelline valley.

Geographic entities mentioned:
surface_form: pic de luseney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8705972
lon: 7.4908648
surface_form: becca di luseney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8705972
lon: 7.4908648
Becca di Luseney. Becca di Luseney (French: Pic de Luseney) (3,502m) is a mountain of the Pennine Alps in Aosta Valley, northwest Italy. It has a pyramidal look on all four sides, and its north face is covered with a glacier. A huge rockfall from its southwest face came down in 1952, completely destroying the village of Chamen and other settlements in the Valpelline valley.

Geographic entities mentioned:
surface_form: becca di luseney
instance_of: Mountain
countries: Italy
coordinates: lat: 45.8705972
lon: 7.4908648
Starr happened to be in Japan when the 1923 Great Kantō earthquake and subsequent major fires struck the main island of Honshū. In the absence of news from the devastated area, speculation about his safety was published in the &quot;New York Times.&quot; His plans to spend several months researching the vicinity of Mount Fuji were not specific, nor was the extent of the quake area known.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The station primarily covers the western Lakes Region and southern White Mountains area, though it can be heard as far south as Manchester and as far west as Barre, Vermont. WPNH-FM originally transmitted from a hilltop in nearby Holderness until the late 1990s when the station's transmitter was moved to the top of Tenney Mountain in Plymouth by new owners.

Geographic entities mentioned:
surface_form: Tenney Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.737777777778
lon: -71.783611111111
Mourgana. Mourgana (or Όρη Τσαμαντά - &quot;Ori Tsamanta&quot;,) is a mountain range in northwestern Greece and southern Albania. Its highest elevation is 1,806 m. Geography and location. It is drained by tributaries of the river Thyamis towards the south by tributaries of the river Drinos towards the north and by the small river Pavllë to the west.

Geographic entities mentioned:
surface_form: όρη τσαμαντά
instance_of: Mountain
countries: Greece
Albania
coordinates: lat: 39.784
lon: 20.383
surface_form: mourgana
instance_of: Mountain
countries: Greece
Albania
coordinates: lat: 39.784
lon: 20.383
Mourgana. Mourgana (or Όρη Τσαμαντά - &quot;Ori Tsamanta&quot;,) is a mountain range in northwestern Greece and southern Albania. Its highest elevation is 1,806 m. Geography and location. It is drained by tributaries of the river Thyamis towards the south by tributaries of the river Drinos towards the north and by the small river Pavllë to the west.

Geographic entities mentioned:
surface_form: mourgana
instance_of: Mountain
countries: Greece
Albania
coordinates: lat: 39.784
lon: 20.383
In the relevant passage, Hathor is addressed as the “Lady of Byblos” while she is invoked as a protector of the passengers of the solar barque. This association finds parallels in instances of linking the same Egyptian goddess to various other distant areas, including Sinai, Punt, Wadi el-Hudi and Gebel el-Asr.

Geographic entities mentioned:
surface_form: Wadi el-Hudi
instance_of: Valley
countries: Egypt
coordinates: lat: 23.96152778
lon: 33.13133333
The pharaoh himself mentions her in on a stela from the temple of Amun in Jebel Barkal in Nubia, which commemorates the construction of ships for a military campaign in the north from wood from the “neighborhood of the Lady of Byblos.” A reference to her might also be present in a damaged text found in the Theban tomb of one of his officials, Senneferi, which describes an expedition to Byblos.

Geographic entities mentioned:
surface_form: Jebel Barkal
instance_of: Mountain
countries: Sudan
coordinates: lat: 18.5368
lon: 31.8276
The mountains are relatively high for a range so young and are very steep in places; Galdhøpiggen in South Norway is the highest peak in mainland Northern Europe, at; Kebnekaise is the highest peak on the Swedish side, at, whereas the slope of Halti is the highest point in Finland, at, although the peak of Halti is situated in Norway.

Geographic entities mentioned:
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
In Norwegian, it is called,, ('the Keel') or ('the North Ridge', name coined in 2013). The names and are often preferentially used for the northern part, where the mountains form a narrow range near the border region of Norway and Sweden. In South Norway, there is a broad scatter of mountain regions with individual names, such as Dovrefjell, Hardangervidda, Jotunheimen, and Rondane. Orography.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
Around Trondheim Fjord, peaks decrease in altitude to about, rising again to heights in excess of further north in Swedish Lapland and nearby areas of Norway. The southern part of the mountain range contains the highest mountain of Northern Europe, Galdhøpiggen at almost.

Geographic entities mentioned:
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
Geomorphologist Karna Lidmar-Bergström and co-workers recognize five widespread stepped surfaces. In eastern Norway, some of the stepped surfaces merge into a single surface. Dovrefjell and Jotunheimen are rises from the highest of the stepped surfaces. In south-western Norway, the plateaux and gently undulating surfaces are strongly dissected by fjords and valleys.

Geographic entities mentioned:
surface_form: Dovrefjell
instance_of: Mountain
countries: Norway
coordinates: lat: 62.1
lon: 9.41666667
The stable ground temperature at a depth of is still. The measured geothermal gradient in the drillhole of 1.17 °C /100 m allows to extrapolate a permafrost thickness of, a further proof that continuous permafrost exists in these altitudes and above, up to the top of Kebnekaise.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
Although the ages of these deposits and landforms vary, most of them were formed in connection to the Weichselian glaciation and the subsequent deglaciation. The Cenozoic glaciations that affected Fennoscandia most likely began in the Scandinavian Mountains. It is estimated that during 50% of the last 2.75 million years the Scandinavian Mountains hosted mountain-centered ice caps and ice fields.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Sweden. There are 12 peaks in Sweden that reach above, or 13 depending on how the peaks are defined. Eight of them are located in Sarek National Park and the neighbouring national park Stora Sjöfallet. The other four peaks are located in the further north region of Kebnekaise. All mountain names are in Sami but with the more common Swedish spelling of it.

Geographic entities mentioned:
surface_form: Kebnekaise
instance_of: Mountain
countries: Sweden
coordinates: lat: 67.883333333333
lon: 18.55
Lower Silesia is bordered by Greater Poland and Lubusz Land in the north, Upper Silesia in the east, Moravia in the south-east, Bohemia and Kłodzko Land in the south, and Lusatia in the west. Sudetes. The Sudetes are a geologically diverse mountain range that stretches for from the Lusatian Highlands in the west and to the Moravian Gate in the east.

Geographic entities mentioned:
surface_form: Lubusz Land
instance_of: Plateau
countries: Germany
Poland
Kingdom of Poland
Lands of the Bohemian Crown
The Lower Silesian section of the Sudetes comprises the Jizera Mountains (highest peak: Wysoka Kopa,), where the tripoint with Upper Lusatia and Bohemia is located near the Smrk summit, along with the adjacent Giant Mountains (highest: border peak of Sněžka Śnieżka – highest mountain of Czech Republic,); Rudawy Janowickie (Skalnik,); Owl Mountains (Wielka Sowa,); Stone Mountains (Waligóra); Wałbrzych Mountains (Borowa) and the Kaczawskie Mountains (Skopiec,) with Ostrzyca, - they surround the Jelenia Góra valley,; Ślęża Massif (Mount Ślęża), massive of Orlické hory, Králický Sněžník south of Kłodzko, Rychlebské hory and Jeseníky (; Praděd,).

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
surface_form: Wielka Sowa
instance_of: Mountain
countries: Poland
coordinates: lat: 50.679166666667
lon: 16.486944444444
surface_form: Jelenia Góra valley
instance_of: Valley
countries: Prussia
coordinates: lat: 50.916666666667
lon: 15.75
surface_form: Králický Sněžník
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.2075
lon: 16.846944444444
surface_form: Praděd
instance_of: Mountain
countries: Czech Republic
coordinates: lat: 50.083194444444445
lon: 17.23086111111111
The greatest rivers are Nysa Kłodzka, which is the source of drinking water for Wrocław (the water is drawn by special channel); Stobrawa, Oława, Ślęza, Bystrzyca with its tributaries—Strzegomka and Piława; Widawa, Średzka Woda, Kaczawa with Nysa Szalona and Czarna Woda. There is also the largest right-bank tributary of the area, Barycz.

Geographic entities mentioned:
surface_form: Widawa
instance_of: Watercourse
countries: Poland
coordinates: lat: 51.198888888889
lon: 16.918888888889
The primeval flora has been transformed significantly as a result of deforestation and cultivation. The largest forest complexes are Bory Dolnośląskie (), Bory Stobrawskie in Stobrawa and Widawa areas, and smaller fragments of forests in Barycz and Oder River valleys. These forests are kind of multi-species deciduous forests, occurring in fertile grounds.

Geographic entities mentioned:
surface_form: Widawa
instance_of: Watercourse
countries: Poland
coordinates: lat: 51.198888888889
lon: 16.918888888889
They were collectors, hunters, and fishers, and used weapons and other tools made of stone and wood. In the Upper Paleolithic, the oldest human remains of the nomadic people, which were 40,000 years old, were found in a tomb in Tyniec on the river Ślęża. In the Neolithic (4000–1700 BC), began the process of transformation into a settled way of life.

Geographic entities mentioned:
surface_form: Ślęża
instance_of: Mountain
countries: Poland
coordinates: lat: 50.865016944444
lon: 16.708816944444
Southern California Clean Power Alliance has a 20-year power purchase agreement for 300 megawatts from the wind farm. Geography. White Hills is in northwestern Mohave County, in the Detrital Valley and at the base of the White Hills, which rise to the east. U.S. Route 93 runs through the west side of the CDP, leading southeast to Kingman, the Mohave county seat, and northwest to Las Vegas, Nevada.

Geographic entities mentioned:
surface_form: Detrital Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.70472222
lon: -114.4775
Four rowing crews had confirmed Olympic places for their boats each in the men's lightweight four, and all small-boat classes for women (except coxless pair) at the 2015 FISA World Championships in Lac d'Aiguebelette, France, while the men's lightweight double sculls rowers had added one boat to the Chinese roster as a result of their gold medal triumph at the 2016 Asia & Oceania Continental Qualification Regatta in Chungju, South Korea.

Geographic entities mentioned:
surface_form: Lac d'Aiguebelette
instance_of: Lake
countries: France
coordinates: lat: 45.552777777778
lon: 5.7972222222222
A total of eight sailors, led by two-time Olympian and defending Laser Radial champion Xu Lijia, had been selected to the Chinese Olympic team for Rio 2016, following the completion of the ISAF World Cup meet (April 26 to May 1) in Hyères, France. M = Medal race; EL = Eliminated – did not advance into the medal race
Shooting.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Before 2017, the municipality was located in the Trins sub-district, of the Imboden district, after 2017 it was part of the Imboden Region. It is a small settlement north of the confluence of the Hinterrhein and Vorderrhein. It consists of the village of Tamins and since 1803 the village of Reichenau at the confluence of Hinterrhein and Vorderrhein and the Castle (Schloss) of Reichenau.

Geographic entities mentioned:
surface_form: Vorderrhein
instance_of: Watercourse
countries: Switzerland
coordinates: lat: 46.6325
lon: 8.6744444444444
In young ribbonfish, some of the fin-rays are prolonged to an extraordinary degree, and sometimes provided with appendages. Specimens have been taken in the Atlantic, the Mediterranean, the Bay of Bengal, at Mauritius, and in the Pacific. The species from the Atlantic has occurred chiefly on the northern coasts, Iceland, Scandinavia, Orkney, and Scotland.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Black Dome (New York). Black Dome is a mountain located in Greene County, New York. The mountain is the highest peak of the Blackhead Mountains range of the Catskills. Black Dome is flanked to the east by Blackhead, and to the west by Thomas Cole Mountain. Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay.

Geographic entities mentioned:
surface_form: Thomas Cole Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2708
lon: -74.1362
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226
Black Dome (New York). Black Dome is a mountain located in Greene County, New York. The mountain is the highest peak of the Blackhead Mountains range of the Catskills. Black Dome is flanked to the east by Blackhead, and to the west by Thomas Cole Mountain. Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay.

Geographic entities mentioned:
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226
The mountain is the highest peak of the Blackhead Mountains range of the Catskills. Black Dome is flanked to the east by Blackhead, and to the west by Thomas Cole Mountain. Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay. The south side of Black Dome drains into East Kill, and thence into Schoharie Creek.

Geographic entities mentioned:
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226
Black Dome is flanked to the east by Blackhead, and to the west by Thomas Cole Mountain. Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay. The south side of Black Dome drains into East Kill, and thence into Schoharie Creek. The north side of Black Dome drains into Batavia Kill, and thence into Schoharie Creek.

Geographic entities mentioned:
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226
Black Dome stands within the watershed of Schoharie Creek, which drains into the Mohawk River, the Hudson River, and into New York Bay. The south side of Black Dome drains into East Kill, and thence into Schoharie Creek. The north side of Black Dome drains into Batavia Kill, and thence into Schoharie Creek. Black Dome is within New York's Catskill Park.

Geographic entities mentioned:
surface_form: black dome
instance_of: Mountain
countries: United States
coordinates: lat: 42.2701
lon: -74.1226