Sarmila/GeoWiki-Features huggingface dataset:
These included the type site of Tell al-'Ubaid, Ur, and in the north, Tepe Gawra. Since then, archaeologists have discovered Ubaid material culture throughout the ancient Near East. There are now Ubaid sites in the Amuq Valley in the northwest and all the way to the Persian Gulf coast in the southeast. Important research includes the many excavations in the Hamrin area in the 1970s.

Geographic entities mentioned:
surface_form: Amuq Valley
instance_of: Valley
countries: Turkey
coordinates: lat: 36.354349
lon: 36.36153
As of the 2010 Census, the total population of the district was 42,752, with the population of Dylym accounting for 20.2% of that number. Geography. The district is in rugged terrain in the forested foothills of Degestan, 50 km west of the Caspian Sea. The average height is 500 to 1,000 meters above sea level, with higher elevations reaching 1,900 meters.

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
In the late October, the main forces of the New 22nd and 38th Divisions in Ledo Road arrived at the edge of the Hukawng Valley and the counter-offensive of the Chinese Expeditionary Force against Japanese forces in northern Burma began. After a bloody battle, the 38th Division captured Yubang in Kachin State on December 29.

Geographic entities mentioned:
surface_form: Hukawng Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 26.438333333333
lon: 96.558888888889
It was the eighth appearance of the 4 x 5 km relay in the Winter Olympics. The competition was held on Wednesday, 15 February 1984 at Veliko Polje, Igman. It was the first time since 1968 that Norway won the gold medal in the event.

Geographic entities mentioned:
surface_form: Igman
instance_of: Plateau
countries: Bosnia and Herzegovina
coordinates: lat: 43.783333333333
lon: 18.25
Waw an Namus. Waw an Namus (also spelled Wau-en-Namus,) is a volcano in Libya. Of either Pleistocene or Holocene age, it is located within the eastern Fezzan region. The origin of the volcanism there and at Al Haruj farther north is not clear.

Geographic entities mentioned:
surface_form: wau-en-namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Several small lakes and associated vegetation are located within the caldera. Name. The volcano is also known as Uaw en Namus, Uau en Namus, Wau-en-Namus and Wau Sqair. It means &quot;Oasis of mosquitoes&quot;, a reference to the small lakes around it and the numerous mosquitoes that exist at Waw an Namus, nurtured by the lakes at the volcano. Geography and geomorphology.

Geographic entities mentioned:
surface_form: wau-en-namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Waw an Namus. Waw an Namus (also spelled Wau-en-Namus,) is a volcano in Libya. Of either Pleistocene or Holocene age, it is located within the eastern Fezzan region. The origin of the volcanism there and at Al Haruj farther north is not clear.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Radiometric dating has yielded an age of about 200,000 years, but other circumstantial evidence points to a formation of the volcano during Holocene or even historical times. Waw an Namus is characterized by a caldera surrounded by an apron of dark tephra, which has a notable colour contrast to the surrounding desert terrain of the Sahara.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Waw an Namus is characterized by a caldera surrounded by an apron of dark tephra, which has a notable colour contrast to the surrounding desert terrain of the Sahara. A smaller crater lies northwest of the Waw an Namus caldera. The caldera itself contains a scoria cone. Several small lakes and associated vegetation are located within the caldera. Name.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Several small lakes and associated vegetation are located within the caldera. Name. The volcano is also known as Uaw en Namus, Uau en Namus, Wau-en-Namus and Wau Sqair. It means &quot;Oasis of mosquitoes&quot;, a reference to the small lakes around it and the numerous mosquitoes that exist at Waw an Namus, nurtured by the lakes at the volcano. Geography and geomorphology.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
The volcano lies within the Sahara, in the eastern Fezzan and was discovered by scientists a few decades before 1951. The caravan route between Kufra and Sebha passes by the volcano. Ancient graves have been found at Waw an Namus. While the oasis was probably visited by herders and hunters and may have been the source of raw materials, the place is otherwise uninhabited.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Ancient graves have been found at Waw an Namus. While the oasis was probably visited by herders and hunters and may have been the source of raw materials, the place is otherwise uninhabited. The landscape around Waw an Namus has been described as &quot;very beautiful&quot; and is reportedly a tourism target but logistical issues and the Libyan Civil War make it difficult to access the area.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Waw an Namus is a, caldera, which has a small relief outwards but a steep margin inwards. During its formation, over of rock were displaced. Another crater lies northwest from Waw an Namus. That vent was formed by overlapping craters which feature no volcanic rocks and which have produced salty mud; this may have been a site of phreatic activity and of volcanic degassing.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
The water surface reaches elevation above sea level, although seasonal variations sometimes cause the lakebodies to dry up. These lakes, some of which have red colours, give Waw an Namus a multicoloured appearance. The lakes are probably groundwater-fed, as evaporation in the area greatly exceeds precipitation, with the lakes losing about water per year. Freshwater springs nourish the lakes.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Freshwater springs nourish the lakes. At least one water body was reported to be fresh in 1951 while the others are warm and saline. Deuterium isotope ratio analysis indicates that the water at Waw an Namus is recent water, certainly more recent than 8,000 years. Geology. Waw an Namus is an isolated volcano.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Geology. Waw an Namus is an isolated volcano. About north lie lava flows of basaltic composition and the Haruj volcanic field, of which Waw an Namus is sometimes considered to be a part. These in turn are only two out of several large but little known volcanic fields in the Sahara.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
A number of theories have been proposed to explain the volcanism in the Sahara, such as the activation of ancient crustal lineaments by the collision between Africa and Europe; in the case of Waw an Namus the magmas originated in the mantle at about depth, and include both asthenosphere and lithosphere components that underwent metasomatism before melting.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
The processes at Haruj and Waw an Namus were probably different. The terrain surrounding Waw an Namus is covered by Quaternary sediments. The basement beneath the volcano is crystalline, and is in turn covered by limestone, marl and the Nubian Sandstone. Alkali basalts have been identified in the scoria, and the occurrence of foidite has been reported.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Climate. Waw an Namus is part of the Sahara desert, one of the world's largest and driest deserts although parts of it were wetter in the past. In some parts of the Sahara it has only rained a few times during a whole century; at Waw an Namus the little precipitation mostly occurs during winter.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
In some parts of the Sahara it has only rained a few times during a whole century; at Waw an Namus the little precipitation mostly occurs during winter. Wind is the most important weather factor, forming ventifacts and dunes among other structures; at Waw an Namus it mostly blows from the northeast and is sometimes accompanied by dust devils south of the volcano. Eruptive history.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
The arid climate may mislead as to its actual age, as there is little erosion in the desert. Early geological studies estimated an age of less than 800–1,000 years. Salty muds and rocks erupted by the scoria cone and the crater northwest of the main Waw an Namus caldera must have been emplaced after the last pluvial.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Salty muds and rocks erupted by the scoria cone and the crater northwest of the main Waw an Namus caldera must have been emplaced after the last pluvial. The Waw an Namus caldera cuts a Holocene drainage system in the Sahara and there is no evidence of Neolithic artifacts at Waw an Namus, further supporting a recent origin of the volcano.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Radiometric dating failed to yield a reliable age for the rocks; only an imprecise age of 690,000 ± 1,100,000 years ago was obtained. Later potassium-argon dating yielded an age of 200,000 ± 9,000 years before present for a lava bomb associated with the central cone, and the Global Volcanism Program assigns a Pleistocene age to Waw an Namus.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Later potassium-argon dating yielded an age of 200,000 ± 9,000 years before present for a lava bomb associated with the central cone, and the Global Volcanism Program assigns a Pleistocene age to Waw an Namus. Hot springs are active at Waw an Namus and produce sulfurous water. Biology.

Geographic entities mentioned:
surface_form: waw an namus
instance_of: Mountain
countries: Libya
coordinates: lat: 24.9
lon: 17.75
Cape Cornish. Cape Cornish () is a cape which forms the northern tip of Buckle Island in the Balleny Islands. It was named by personnel on the &quot;Discovery II&quot; in 1938 for A.W. Cornish, a meteorologist with the Australian Central Bureau who was an observer aboard the &quot;Discovery II&quot; during 1937–38.

Geographic entities mentioned:
surface_form: Buckle Island
instance_of: Mountain
coordinates: lat: -66.783333333333
lon: 163.25
On Friday, June 27, 1911, the first fatal accident in connection with the Tourist Trophy races happened. While practicing for the forthcoming race, Victor Surridge was taking a difficult corner on Cregwilly's Hill near Glen Helen section of the course, dashing into a hedge and breaking his neck. He was nineteen years of age. Junior TT final standings.

Geographic entities mentioned:
surface_form: Glen Helen
instance_of: Valley
countries: Isle of Man
coordinates: lat: 54.22583333
lon: -4.61722222
In 1958, he published &quot;The Cayuga Bridge&quot;, a story of New York local history. The summer home on Cayuga Lake, that Wells and his wife established in 1948, would host students, colleagues, and other friends from around the world, for decades. Wells had an important collection of early works on American and European geology. Awards and memberships.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Mountain peaks and glaciers. The highest peak in Skardu District is K2 (8,611 m), which is the highest peak in Pakistan and the second-highest in the world. The Baltoro Muztagh, the subrange of the Karakoram Mountains that includes the mighty peaks of K2 (8,611 m), Broad Peak (8,047 m), the Gasherbrums (8,000+ m), and Masherbrum (7,821 m), is located in Skardu District.

Geographic entities mentioned:
surface_form: K2
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.881111111111
lon: 76.513333333333
Mountain peaks and glaciers. The highest peak in Skardu District is K2 (8,611 m), which is the highest peak in Pakistan and the second-highest in the world. The Baltoro Muztagh, the subrange of the Karakoram Mountains that includes the mighty peaks of K2 (8,611 m), Broad Peak (8,047 m), the Gasherbrums (8,000+ m), and Masherbrum (7,821 m), is located in Skardu District.

Geographic entities mentioned:
surface_form: Broad Peak
instance_of: Mountain
countries: Pakistan
People's Republic of China
coordinates: lat: 35.810555555556
lon: 76.568055555556
surface_form: Masherbrum
instance_of: Mountain
countries: Pakistan
coordinates: lat: 35.6425
lon: 76.310833333333
News/talk (1993–2000). Under Clear Channel management, the station became WGST-FM and simulcast news/talk WGST, beginning October 1. In the mid-1990s, it again relocated its transmitter site southward, this time to the Sweat Mountain antenna farm in northeastern Cobb County (where several other stations are).

Geographic entities mentioned:
surface_form: Sweat Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.0669
lon: -84.4556
United Railways (Oregon). United Railways was a railroad in Oregon. Begun as an electric interurban railway in 1911, passenger service was never effective and the road became a freight link to the Tualatin Valley. The company was dissolved in 1944, but the railroad line remains active. History.

Geographic entities mentioned:
surface_form: Tualatin Valley
instance_of: Valley
countries: United States
coordinates: lat: 45.5106
lon: -122.989
A formal synonymization took place in 2023 along with the description of six additional species. In May 2008 Jeffebeck Arimas collected specimens from the volcanoes Kanlaon and Mandalagan on Negros Island, which were initially known as &quot;Trachyaretaon&quot; sp. 'Negros'.

Geographic entities mentioned:
surface_form: Kanlaon
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.411944444444
lon: 123.13194444444
surface_form: Mandalagan
instance_of: Mountain
countries: Philippines
coordinates: lat: 10.65
lon: 123.25
Bouteille supervised the construction du Muséum in the &quot;Jardin des plantes&quot; considerably enriched the collections. He founded &quot;la Société d'acclimatation des Alpes&quot; also the &quot;Jardin d'acclimatation de Grenoble&quot; in 1854. He was also the author of &quot;Faune de l’Oisans&quot; in Essai descriptif de l’Oisans d'Aristide Albert (1821–1903).

Geographic entities mentioned:
surface_form: l’Oisans
instance_of: Valley
countries: France
coordinates: lat: 45.05
lon: 6.03333333
Pillaka. Pillaka (Quechua for a two-colored &quot;llawt'u&quot;, also spelled &quot;Pillaca&quot;) is a mountain in the Cordillera Negra in the Andes of Peru which reaches a height of approximately. It is located in the Ancash Region, Aija Province, Succha District, and the Huarmey Province, Huayan District.

Geographic entities mentioned:
surface_form: pillaka
instance_of: Mountain
countries: Peru
coordinates: lat: -9.86083333
lon: -77.63416667
Alternatively, these two might simply be independently derived from a common ancestor in the course of these events but probably somewhat earlier, and appear similar on the molecular level due to convergent evolution. Its natural habitats are Lake Ohrid and Lake Scutari, and the adjacent Drim River and Morača River basins.

Geographic entities mentioned:
surface_form: Lake Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665
Piz Mitgel. Piz Mitgel is a mountain in the Albula Range of the Swiss Alps, overlooking Savognin, in the canton of Graubünden. Similarly to its higher neighbor, Corn da Tinizong, it has an almost vertical south face. A via ferrata (&quot;Senda Ferrada&quot;) leads to the summit.

Geographic entities mentioned:
surface_form: Corn da Tinizong
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.611472222222
lon: 9.6711388888889
Piz Mitgel. Piz Mitgel is a mountain in the Albula Range of the Swiss Alps, overlooking Savognin, in the canton of Graubünden. Similarly to its higher neighbor, Corn da Tinizong, it has an almost vertical south face. A via ferrata (&quot;Senda Ferrada&quot;) leads to the summit.

Geographic entities mentioned:
surface_form: piz mitgel
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.61425
lon: 9.6465833333333
It is the headquarters of the Kwamouth territory. The town lies at the mouth of the Kwah River, the last stretch of the Kasai River after it has been joined by the Fimi River, where it enters the Congo River. On 2 February 1961 a military Fairchild C-119G Flying Boxcar operated by Aeronautica Militare Italiana was damaged beyond repair at Kwamouth. There were no fatalities.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
surface_form: Fimi River
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: -3.013472222222222
lon: 16.954305555555557
Akalamm Abkhane. Akalamm Abkhane (also known as the Black Lake) is a lake situated approximately from the Khénifra Province. It represents a notable environmental landmark within the Khenifra Province, particularly within the Temdaghas Ait Lahcen region. The lake is home to various avian species, including geese and black chickens.

Geographic entities mentioned:
surface_form: akalamm abkhane
instance_of: Lake
countries: Morocco
coordinates: lat: 32.9058
lon: -5.34333
An international organisation, the Pangaean Economic Community, exists. Seeming to be similar to the United Nations in scope but similar to the European Union in powers, it is playing a role in forcing change by directives and boycotts. Britain is known as Albion, Africa is one country called Zafrika, and Scandinavia — known as Fenno-Scandia — is the only Nought country left.

Geographic entities mentioned:
surface_form: Fenno-Scandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Mount Ossa (Greece). Mount Ossa (), alternatively Kissavos (Κίσσαβος), is a mountain in the Larissa regional unit, in Thessaly, Greece. It is high and is located between Pelion to the south and Olympus to the north, separated from the latter by the Vale of Tempe. Etymology. The name Kissavos has been connected to Serbian &quot;kisha&quot; &quot;wet weather, rain.&quot;
Mythology.

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
surface_form: tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
surface_form: olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.479
lon: 23.865
It is high and is located between Pelion to the south and Olympus to the north, separated from the latter by the Vale of Tempe. Etymology. The name Kissavos has been connected to Serbian &quot;kisha&quot; &quot;wet weather, rain.&quot;
Mythology. In Greek mythology, the Aloadaes are said to have attempted to pile Mount Pelion on top of Mount Ossa in their attempt to scale Olympus.

Geographic entities mentioned:
surface_form: Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
surface_form: pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
surface_form: olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.479
lon: 23.865
surface_form: olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
surface_form: mount ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
surface_form: ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
Mount Ossa (Greece). Mount Ossa (), alternatively Kissavos (Κίσσαβος), is a mountain in the Larissa regional unit, in Thessaly, Greece. It is high and is located between Pelion to the south and Olympus to the north, separated from the latter by the Vale of Tempe. Etymology. The name Kissavos has been connected to Serbian &quot;kisha&quot; &quot;wet weather, rain.&quot;
Mythology.

Geographic entities mentioned:
surface_form: mount ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
surface_form: ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
Mount Ossa (Greece). Mount Ossa (), alternatively Kissavos (Κίσσαβος), is a mountain in the Larissa regional unit, in Thessaly, Greece. It is high and is located between Pelion to the south and Olympus to the north, separated from the latter by the Vale of Tempe. Etymology. The name Kissavos has been connected to Serbian &quot;kisha&quot; &quot;wet weather, rain.&quot;
Mythology.

Geographic entities mentioned:
surface_form: mount ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
surface_form: ossa
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
surface_form: κίσσαβος
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
surface_form: kissavos
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
It is high and is located between Pelion to the south and Olympus to the north, separated from the latter by the Vale of Tempe. Etymology. The name Kissavos has been connected to Serbian &quot;kisha&quot; &quot;wet weather, rain.&quot;
Mythology. In Greek mythology, the Aloadaes are said to have attempted to pile Mount Pelion on top of Mount Ossa in their attempt to scale Olympus.

Geographic entities mentioned:
surface_form: kissavos
instance_of: Mountain
countries: Greece
coordinates: lat: 39.8
lon: 22.7
It is a tributary of the East Branch of the Saco River, with its waters ultimately flowing to the Atlantic Ocean in Maine. The East Fork rises on the western slopes of North and South Baldface, two rocky summits that each stand over above sea level, in the eastern part of the White Mountain National Forest.

Geographic entities mentioned:
surface_form: North
instance_of: Mountain
countries: United States
coordinates: lat: 44.2428
lon: -71.0869
surface_form: South Baldface
instance_of: Landform
Mountain
countries: United States
coordinates: lat: 44.2306
lon: -71.0781
Guthrie's song has been subsequently covered by many recording artists. Dick Tracy's adversary Flattop Jones was based on Pretty Boy Floyd. Flattop claims to be a freelancer from the &quot;Crookston Hills&quot;, a parody of Cookson Hills in Oklahoma, and the comic strip refers to Flattop's involvement in the Kansas City Massacre. Floyd in literature.

Geographic entities mentioned:
surface_form: Cookson Hills
instance_of: Landform
countries: United States
coordinates: lat: 35.7
lon: -94.8
Stinson Lake. Stinson Lake is a water body located in the town of Rumney in Grafton County, New Hampshire, United States. The lake is in the southern part of the White Mountains and is the largest lake in the White Mountain National Forest. Water from Stinson Lake flows via Stinson Brook, the Baker River, and the Pemigewasset River to the Merrimack River. The lake is a result of glacier deposits.

Geographic entities mentioned:
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.94687
lon: -119.3096
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.040555555556
lon: -121.15305555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.5781
lon: -109.32
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.67648
lon: -123.32823
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.0030248
lon: -111.4687966
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.634166666667
lon: -118.25555555556
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9555
lon: -110.735
surface_form: white mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.57476
lon: -114.49565
Most of the lake is fronted by private property and cabins, but boating access is available next to the former Stinson Lake Store on the western side of the lake. Hiking trails lead from near Stinson Lake southeast to the summit of Stinson Mountain and north to Mount Kineo, Mount Carr, and the Three Ponds area.

Geographic entities mentioned:
surface_form: mount kineo
instance_of: Mountain
countries: United States
coordinates: lat: 45.6997
lon: -69.7339
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
Stinson Lake. Stinson Lake is a water body located in the town of Rumney in Grafton County, New Hampshire, United States. The lake is in the southern part of the White Mountains and is the largest lake in the White Mountain National Forest. Water from Stinson Lake flows via Stinson Brook, the Baker River, and the Pemigewasset River to the Merrimack River. The lake is a result of glacier deposits.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
Stinson Lake. Stinson Lake is a water body located in the town of Rumney in Grafton County, New Hampshire, United States. The lake is in the southern part of the White Mountains and is the largest lake in the White Mountain National Forest. Water from Stinson Lake flows via Stinson Brook, the Baker River, and the Pemigewasset River to the Merrimack River. The lake is a result of glacier deposits.

Geographic entities mentioned:
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
Its waters are very clear, with visibility to of depth. Stinson Lake lies in the northern corner of Rumney, just south of the town boundary with Ellsworth and northwest of Stinson Mountain. Most of the lake is fronted by private property and cabins, but boating access is available next to the former Stinson Lake Store on the western side of the lake.

Geographic entities mentioned:
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
Hiking trails lead from near Stinson Lake southeast to the summit of Stinson Mountain and north to Mount Kineo, Mount Carr, and the Three Ponds area. The village of Stinson Lake is at the lake's outlet, at the top of a long climb up the paved Stinson Lake Road from the village of Rumney.

Geographic entities mentioned:
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
The village of Stinson Lake is at the lake's outlet, at the top of a long climb up the paved Stinson Lake Road from the village of Rumney. Stinson Lake Road is open year-round, while the gravel road from Ellsworth and Campton is only open from late spring through early fall.

Geographic entities mentioned:
surface_form: stinson lake
instance_of: Lake
countries: United States
coordinates: lat: 43.866666666667
lon: -71.799166666667
It is located in the Cusco Region, Canchis Province, Pitumarca District, and in the Quispicanchi Province, Marcapata District. Istalla lies northeast of the mountain Condoriquiña.

Geographic entities mentioned:
surface_form: condoriquiña
instance_of: Mountain
countries: Peru
coordinates: lat: -13.825
lon: -70.91972222
surface_form: istalla
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8064
lon: -70.905
Istalla. Istalla (possibly from Quechua for a quadrangular, woven or knitted multi-colored piece of clothing to carry coca leaves) is a mountain in the Andes of Peru, about high, situated in the Vilcanota mountain range south east of Cusco. It is located in the Cusco Region, Canchis Province, Pitumarca District, and in the Quispicanchi Province, Marcapata District.

Geographic entities mentioned:
surface_form: istalla
instance_of: Mountain
countries: Peru
coordinates: lat: -13.8064
lon: -70.905
It had a population of 551 as of 2011. Geography. Capalbio Scalo is about 50 km from Grosseto and 9 km from Capalbio. It is in the plain of southern Maremma between the hills of Capalbio and the Tyrrhenian Sea. Capalbio Scalo lies on the shore of Lago di Burano, an important natural reserve. Transport. Capalbio Scalo is located along the Via Aurelia highway which links Grosseto to Rome.

Geographic entities mentioned:
surface_form: Lago di Burano
instance_of: Lake
countries: Italy
coordinates: lat: 42.401111111111
lon: 11.377777777778
Schynige Platte. The Schynige Platte (&quot;Scheinige Platte&quot; on the old Siegfried Map) is a small mountain ridge and a viewpoint in the Bernese Highlands and belongs to the Schwarzhorn group. The mountain range consists of three peaks: Gumihorn (), Tuba (), and the closest summit next to the viewpoint, Geiss ().

Geographic entities mentioned:
surface_form: Gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
surface_form: gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
The mountain range consists of three peaks: Gumihorn (), Tuba (), and the closest summit next to the viewpoint, Geiss (). The viewpoint lies at an altitude of about, at the western end of a prominent ridge of the Schwarzhorn group, which separates the valley of the Schwarze Lütschine from Lake Brienz.

Geographic entities mentioned:
surface_form: Lake Brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38425
lon: 7.58008333
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6861
lon: 8.07556
surface_form: lake brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7358
lon: 9.9417
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.60766667
lon: 9.10652778
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6772
lon: 9.0225
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.21694444
lon: 7.75666667
It is notable for its hotel and, since 1893, its mountain railway, one of the highest in Switzerland. In good weather conditions there are views to many surrounding mountains, including the Eiger, Mönch, Jungfrau, and others giants of the Bernese Alps. Also, the town of Interlaken and the two great lakes of Thun and Brienz are visible to the north, lower.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: Mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
surface_form: Jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: jungfrau
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.536944444444
lon: 7.9625
surface_form: eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: mönch
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.558333333333
lon: 7.9972222222222
Directly above the station and hotel, and overlooking the valleys of Lauterbrunnen and Grindelwald, is the Geiss summit (). Further north, and overlooking Interlaken and the two great lakes, are the Tuba () and Oberberghorn () summits. The highest summit in the Schynige Platte area, between the Daube and Geiss summits, the tower-like Gumihorn peak (), cannot be reached by pedestrians.

Geographic entities mentioned:
surface_form: Gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
surface_form: gumihorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6553
lon: 7.90806
The highest summit in the Schynige Platte area, between the Daube and Geiss summits, the tower-like Gumihorn peak (), cannot be reached by pedestrians. The Schynige Platte is also the starting point for the popular hiking trails to Loucherhorn, Faulhorn or First which is connected to Grindelwald by a gondola lift.

Geographic entities mentioned:
surface_form: Loucherhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.666444444444
lon: 7.9348888888889
surface_form: Faulhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.674888888889
lon: 7.9996666666667
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.50486111
lon: 7.64305556
surface_form: faulhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.674888888889
lon: 7.9996666666667
surface_form: loucherhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.666444444444
lon: 7.9348888888889
surface_form: first
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6608
lon: 8.05469
Schynige Platte. The Schynige Platte (&quot;Scheinige Platte&quot; on the old Siegfried Map) is a small mountain ridge and a viewpoint in the Bernese Highlands and belongs to the Schwarzhorn group. The mountain range consists of three peaks: Gumihorn (), Tuba (), and the closest summit next to the viewpoint, Geiss ().

Geographic entities mentioned:
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.38425
lon: 7.58008333
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6861
lon: 8.07556
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.7358
lon: 9.9417
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.60766667
lon: 9.10652778
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.6772
lon: 9.0225
surface_form: schwarzhorn
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.21694444
lon: 7.75666667
It is notable for its hotel and, since 1893, its mountain railway, one of the highest in Switzerland. In good weather conditions there are views to many surrounding mountains, including the Eiger, Mönch, Jungfrau, and others giants of the Bernese Alps. Also, the town of Interlaken and the two great lakes of Thun and Brienz are visible to the north, lower.

Geographic entities mentioned:
surface_form: brienz
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.716667
lon: 7.95
surface_form: thun
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.683333333333
lon: 7.7166666666667
Schynige Platte. The Schynige Platte (&quot;Scheinige Platte&quot; on the old Siegfried Map) is a small mountain ridge and a viewpoint in the Bernese Highlands and belongs to the Schwarzhorn group. The mountain range consists of three peaks: Gumihorn (), Tuba (), and the closest summit next to the viewpoint, Geiss ().

Geographic entities mentioned:
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
Also, the town of Interlaken and the two great lakes of Thun and Brienz are visible to the north, lower. The area is accessible via the Schynige Platte railway, which runs from Wilderswil, where connection is made with Bernese Oberland railway trains from Interlaken. The railway reaches a height of at the terminus station, on the south-facing slopes of Geiss summit.

Geographic entities mentioned:
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
Southwest of the station is a hotel and mountain restaurant, at a height of. Northeast of the station is the Schynige Platte alpine botanical garden, specialising in the display of, and research into, the high altitude flora of Switzerland. A number of short loop trails extend north from the train station, reaching several view points, all within one kilometre from each other.

Geographic entities mentioned:
surface_form: schynige platte
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.656111111111
lon: 7.9069444444444
Bola (volcano). The Bola volcano, also known as Wangore, is an andesitic stratovolcano, located south-west of the Dakataua caldera in New Britain, Papua New Guinea. It is tall and has a wide summit crater. The most recent lava flow was erupted from the summit crater and flowed to the west. This viscous flow is at least 50 m thick, thus leaving an irregularity in the profile of the volcano.

Geographic entities mentioned:
surface_form: Dakataua
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.05555556
lon: 150.10833333
surface_form: bola
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.15
lon: 150.03333333333
Bola (volcano). The Bola volcano, also known as Wangore, is an andesitic stratovolcano, located south-west of the Dakataua caldera in New Britain, Papua New Guinea. It is tall and has a wide summit crater. The most recent lava flow was erupted from the summit crater and flowed to the west. This viscous flow is at least 50 m thick, thus leaving an irregularity in the profile of the volcano.

Geographic entities mentioned:
surface_form: bola (volcano)
instance_of: Mountain
countries: Papua New Guinea
coordinates: lat: -5.15
lon: 150.03333333333
Lankaran Lowland. The Lankaran Lowland () is a narrow strip of lowland in southern Azerbaijan by the Caspian Sea. It is the southward extension of the Kura-Aras Lowland which in itself is an extension of the Aral–Caspian Depression. It is named after the city of Lankaran. Geography.

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
Dexter Marsh. Dexter Marsh is a marsh located at the eastern end of Lake Ontario in Dexter, New York. It was declared a National Natural Landmark in May 1973. The marsh is managed by the New York State Department of Environmental Conservation as the Dexter Marsh Wildlife Management Area. The marsh is a popular fishing and trapping area as well as a migratory bird layover.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
San Ramon, California. San Ramon (Spanish: &quot;San Ramón&quot;, meaning &quot;Saint Raymond&quot;) is a city in Contra Costa County, California, United States, located within the San Ramon Valley, and east of San Francisco. San Ramon's population was 84,605 per the 2020 census, making it the 4th largest city in Contra Costa County, behind Concord, Richmond and Antioch.

Geographic entities mentioned:
surface_form: San Ramon Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.75
lon: -121.95
On April 24, 2001, San Ramon was designated a Tree City USA. Geography. Mount Diablo flanks the city to the northeast and is prominently visible from almost all parts of the city. The Las Trampas Regional Wilderness borders San Ramon's extreme northwest, at the northern end of Bollinger Canyon.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
The smaller Bishop Ranch Regional Preserve straddles San Ramon's western border, located approximately between Interstate 680 and the Alameda County line. The topography of San Ramon is varied, featuring a mix of the rolling hills of the Diablo Range and the flatter basin of the San Ramon Valley.

Geographic entities mentioned:
surface_form: San Ramon Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.75
lon: -121.95
The municipality adjoins the municipalities of Aguilar de Segarra (Bages), Castellfollit del Boix (Bages), Òdena, Jorba, Copons and Els Prats de Rei. It is at the centre of the Serra de Rubió, whose highest peak is the Còpia de Palomes. North of the Serra de Rubió is the Maçana River, a tributary of the Llobregat. The Rubió river, also a tributary of the Llobregat, rises south of the mountains.

Geographic entities mentioned:
surface_form: Còpia de Palomes
instance_of: Mountain
countries: Spain
coordinates: lat: 41.6597
lon: 1.60281
The municipality adjoins the municipalities of Aguilar de Segarra (Bages), Castellfollit del Boix (Bages), Òdena, Jorba, Copons and Els Prats de Rei. It is at the centre of the Serra de Rubió, whose highest peak is the Còpia de Palomes. North of the Serra de Rubió is the Maçana River, a tributary of the Llobregat. The Rubió river, also a tributary of the Llobregat, rises south of the mountains.

Geographic entities mentioned:
surface_form: Llobregat
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.282412
lon: 2.012826
The Rani tribe emerged after the Slavic settlement of the region in the ninth century, and ranked among the most powerful of several small Slav tribes between the Elbe and lower Vistula rivers before the thirteenth century. They were among the last tribes to hold to Slavic paganism, and the influence of their religious center at Arkona reached far beyond their tribal borders.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Fachinal Airport. Fachinal Airport (, is an airstrip west of Chile Chico in the Aysén Region of Chile. The small agricultural settlement of Fachinal (es) is on a point on the south shore of General Carrera Lake west of the Argentina border. There is mountainous terrain in all quadrants. Approach and departure to either end of the runway are over the lake.

Geographic entities mentioned:
surface_form: General Carrera Lake
instance_of: Lake
countries: Chile
Argentina
coordinates: lat: -46.4375
lon: -71.715
Mount Drygalski. Mount Drygalski is an ice-free hill, high, standing southeast of Atlas Cove, near the northwest end of Heard Island in the southern Indian Ocean.

Geographic entities mentioned:
surface_form: mount drygalski
instance_of: Mountain
countries: Australia
coordinates: lat: -53.03333333333333
lon: 73.38333333333334
He uses this same explanation to argue that cart ruts in Malta may have had extraterrestrial purposes along with similar lines in Australia, Saudi Arabia, and the Aral Sea. The book also suggests that ancient artwork throughout the world can be interpreted as depicting astronauts, air and space vehicles, extraterrestrials, and complex technology.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Kanalachhina is situated at the mouth of the valley, once trade centre of yesteryears for local through ponies. Dwaj, the abode of goddess 'Jayanti' is situated in front of it on a high mountain. It is the place gateway to Eastern Himalayas. Panchchuli is well visible from here. Mt.Appi and Annapurna of Nepal are visible from here. It is a Sub Tehsil Headquarters.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
Hagwilget Peak. Hagwilget Peak is the northernmost mountain in the Rocher Déboulé Range in northern British Columbia, Canada. The mountain summit is conspicuously situated immediately south of Hazelton, British Columbia. Overlooking New Hazelton, it rises above the surrounding valley. Precipitation runoff from the mountain drains into the Skeena River and Bulkley River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: hagwilget peak
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1989
lon: -127.601
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Hagwilget Peak. Hagwilget Peak is the northernmost mountain in the Rocher Déboulé Range in northern British Columbia, Canada. The mountain summit is conspicuously situated immediately south of Hazelton, British Columbia. Overlooking New Hazelton, it rises above the surrounding valley. Precipitation runoff from the mountain drains into the Skeena River and Bulkley River.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Hagwilget Peak. Hagwilget Peak is the northernmost mountain in the Rocher Déboulé Range in northern British Columbia, Canada. The mountain summit is conspicuously situated immediately south of Hazelton, British Columbia. Overlooking New Hazelton, it rises above the surrounding valley. Precipitation runoff from the mountain drains into the Skeena River and Bulkley River.

Geographic entities mentioned:
surface_form: hagwilget peak
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1989
lon: -127.601
Overlooking New Hazelton, it rises above the surrounding valley. Precipitation runoff from the mountain drains into the Skeena River and Bulkley River. Based on the Köppen climate classification, Hagwilget Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: hagwilget peak
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1989
lon: -127.601