Sarmila/GeoWiki-Features huggingface dataset:
The southwest corner of the lake is inside the Winter Haven City limits. All of the south side of the lake is bordered by mobile home parks and housing developments. A part of the west side is bordered by a mobile home park, as is part of the north side of the lake. The rest of Lake Henry is bordered by wooded areas. The Polk County Water Atlas says Lake Henry is sometimes known as Lake Drane.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
A part of the west side is bordered by a mobile home park, as is part of the north side of the lake. The rest of Lake Henry is bordered by wooded areas. The Polk County Water Atlas says Lake Henry is sometimes known as Lake Drane. Lake Henry has no public access on its shores, although there a canal on the south side that connects it to Lake Hamilton.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
The rest of Lake Henry is bordered by wooded areas. The Polk County Water Atlas says Lake Henry is sometimes known as Lake Drane. Lake Henry has no public access on its shores, although there a canal on the south side that connects it to Lake Hamilton. Since Lake Henry is part of the northern chain of the Winter Haven Chain of Lakes, it may be reached by boat from a number of lakes in the chain.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
Lake Henry has no public access on its shores, although there a canal on the south side that connects it to Lake Hamilton. Since Lake Henry is part of the northern chain of the Winter Haven Chain of Lakes, it may be reached by boat from a number of lakes in the chain. There is no information about the types of fish found in the lake.

Geographic entities mentioned:
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.328333333333
lon: -97.485555555556
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 27.3237
lon: -81.3837
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 28.0928
lon: -81.6673
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.8532859
lon: -97.4790912
surface_form: chain of lakes
instance_of: Group of lakes
Lake
countries: United States
coordinates: lat: 44.982536
lon: -97.2713448
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 45.90222222
lon: -95.37611111
surface_form: lake henry
instance_of: Lake
countries: United States
coordinates: lat: 44.288888888889
lon: -93.815555555556
In addition, the archaeological evidence indicates that in the 2nd century BC Celts expanded from Bohemia through the Kłodzko Valley into Silesia, now part of Poland and the Czech Republic. They first appear in history in connection with the Gallic invasion of northern Italy, 390 BC, when they made the Etruscan city of Felsina their new capital, Bononia (Bologna).

Geographic entities mentioned:
surface_form: Kłodzko Valley
instance_of: Valley
countries: Czech Republic
Poland
coordinates: lat: 50.25
lon: 16.666666666667
It is a transition zone between the Central tall grasslands and Central forest-grasslands transition ecoregions to the east and the Western short grasslands to the west, while to the north lie the Northern mixed grasslands, which have a cooler temperature and a much shorter growing season. The Edwards Plateau Savannas lie to the south. Flora.

Geographic entities mentioned:
surface_form: Edwards Plateau Savannas
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Oscar von Engeln. Oskar Dietrich von Engeln (July 3, 1880 – January 25, 1965) was a geologist and professor of geology best known for his study of geomorphology and the topography of New York State's Finger Lakes region. Early life and career. Von Engeln was admitted to Cornell as an undergraduate in 1904. While there, he studied under Ralph Stockman Tarr, the noted professor of geography.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
While there, he studied under Ralph Stockman Tarr, the noted professor of geography. He was a student assistant to Tarr during a 1909 expedition to Alaska, serving as photographer to document findings. In 1911, von Engeln completed his doctoral dissertation at Cornell with a study of glacier drainage at Alaska's Mount Saint Elias and the surrounding Yakutat Bay region. Legacy. The O.D.

Geographic entities mentioned:
surface_form: Mount Saint Elias
instance_of: Mountain
countries: United States
Canada
coordinates: lat: 60.29222222222222
lon: -140.93138888888888
Stara Sela. Stara Sela (;) is a small village in the Tuhinj Valley in the Municipality of Kamnik in the Upper Carniola region of Slovenia. Name. The name of the settlement was changed from &quot;Selo&quot; to &quot;Stara sela&quot; in 1952.

Geographic entities mentioned:
surface_form: Tuhinj Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.221413888889
lon: 14.775925
As the Franco-Prussian War approached, the increasingly tense atmosphere in Paris forced Winter to move south via Marseilles and Cannes to Hyères in the Côte d'Azur, where he worked as a plant illustrator for Charles Huber Freres & Co, a prominent nursery and principal source of novelty plants during that period.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Average annual rainfall is only 500 mm, spread over about 48 days, because it is in the rain shadow region of the southern Western Ghats. The altitude ranges from at east end of the Chinnar River to at Kumarikkal Mala peak. Other major peaks in the sanctuary are Nandala Malai, Kottakombu malai (), Vellaikal malai () and Viriyoottu malai.

Geographic entities mentioned:
surface_form: Kumarikkal Mala
instance_of: Mountain
Other major peaks in the sanctuary are Nandala Malai, Kottakombu malai (), Vellaikal malai () and Viriyoottu malai. In contrast, Anamudi peak, located away in the adjacent Eravikulam National Park, is the highest peak in South India. The Chinnar and Pambar rivers are the major perennial water resources in the sanctuary.

Geographic entities mentioned:
surface_form: Anamudi
instance_of: Mountain
countries: India
coordinates: lat: 10.166666666667
lon: 77.066666666667
Iskay Ch'utu. Iskay Ch'utu (Quechua &quot;iskay&quot; two, &quot;ch'utu&quot; cone, &quot;two cones&quot;, also spelled &quot;Iskay Chuto&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, Mizque Province, Vila Vila Municipality. Iskay Ch'utu lies northeast of Jatun Urqu and southeast of Tikrasqa.

Geographic entities mentioned:
surface_form: iskay ch'utu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.89777778
lon: -65.7575
The Little Sequatchie River is a tributary of the Sequatchie River in Tennessee. Unlike its larger namesake, it does not have a spectacular large spring source but is the result of the confluence of many smaller streams in a very remote, scenic area of the Cumberland Plateau along the line between Grundy County and Marion County. It flows down a narrow valley, basically south.

Geographic entities mentioned:
surface_form: Cumberland Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36
lon: -85
The Syracuse Far Westside is bounded by Erie Blvd West on the northeast, South Geddes Street on the lower east and Rowland Street on the south. The western border runs from Velasko Road in the south, to South Avery Avenue, Salisbury Road, Myrtle Street and parallel to Charles Avenue in Westvale, a section of Geddes ending at Willis Avenue just south of Onondaga Lake at the railroad tracks.

Geographic entities mentioned:
surface_form: Onondaga Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.088888888889
lon: -76.208333333333
Geddes officially became a town in 1848. &quot;It then included the west side of Syracuse to Geddes Street, which was the eastern boundary of the town.&quot;
Local residents voted to join the city because Syracuse had a paid professional police department, a paid professional fire department and the city was about to obtain an excellent water supply from Skaneateles Lake.

Geographic entities mentioned:
surface_form: Skaneateles Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8625
lon: -76.372777777778
The force has gradually acquired more experience and an international reputation for professionalism. The MARCOS regularly undertake specialised maritime operations in Jammu and Kashmir through the Jhelum River and Wular Lake, a freshwater lake, and conduct counter-insurgency operations in the region. Some MARCOS units are a part of the tri-services Armed Forces Special Operations Division.

Geographic entities mentioned:
surface_form: Wular Lake
instance_of: Lake
countries: India
coordinates: lat: 34.35472222222222
lon: 74.54833333333333
There is however no evidence that he did so, perhaps due to his having used up all his resources on the Avon. Having failed to recover the Avon after the Restoration, Sir William Sandys and his son undertook work on the Wye and Lugg. Ferries formerly existed at Rochford, at Cotheridge and at Clifton on Teme.

Geographic entities mentioned:
surface_form: Lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Livet-et-Gavet. Livet-et-Gavet () is a commune in the Isère department in southeastern France. Geography. Livet-et-Gavet is located in Oisans on the Romanche river, halfway between Grenoble and the winter sports resorts of The Alpe d'Huez and Les Deux Alpes (25 km). The town is also midway between Vizille and Bourg d'Oisans (about 15 km).

Geographic entities mentioned:
surface_form: Oisans
instance_of: Valley
countries: France
coordinates: lat: 45.05
lon: 6.03333333
Livet-et-Gavet is located in Oisans on the Romanche river, halfway between Grenoble and the winter sports resorts of The Alpe d'Huez and Les Deux Alpes (25 km). The town is also midway between Vizille and Bourg d'Oisans (about 15 km). The Romanche valley and the town are located between the Belledonne and Taillefer mountain ranges, and are served by Provincial Road 1091 (RD 1091; previously RN91).

Geographic entities mentioned:
surface_form: Taillefer
instance_of: Mountain
countries: France
coordinates: lat: 45.03948
lon: 5.92505
The current main mountain body was completed by repeated volcanic activity from 600,000 to 850,000 years ago. Mount Funagata is made up of andesite, which is easily distinguished from the pigeonite basalt that erupted from Mout Kurohana. The crater that produced Mount Izumigatake is located on a ridge between Izumigatake and Kita-izumigatake (North Izumigatake).

Geographic entities mentioned:
surface_form: kita
instance_of: Mountain
countries: Japan
coordinates: lat: 35.67432
lon: 138.23874
This has also led to the term, which is used in the name of Funagata Renpō Prefectural Natural Park, although all five peaks are part of the same stratovolcano. The other peaks that compose the Funagata volcano include Mount Ushiroshirahige (後白髪山), Mount Mitsumine (三峰山), and Mount Izumigatake (泉ヶ岳). Izumigatake is the most famous of these mountains, with two ski resorts and several camping areas.

Geographic entities mentioned:
surface_form: funagata volcano
instance_of: Mountain
countries: Japan
coordinates: lat: 38.45548
lon: 140.61997
Mount Funagata. is a mountain within the Ōu Mountains on the border of Miyagi Prefecture and Yamagata Prefecture in the Tōhoku region of northern Japan. It is listed as one of the &quot;200 famous mountains of Japan&quot; and has a height of. The mountain is also known as when viewed from Yamagata prefecture. Name.

Geographic entities mentioned:
surface_form: mount funagata
instance_of: Mountain
countries: Japan
coordinates: lat: 38.45548
lon: 140.61997
Izumigatake is the most famous of these mountains, with two ski resorts and several camping areas. Izumigatake is also the namesake of Izumi-ku, Sendai. Mount Kurohana (黒鼻山) was traditionally considered part of Mount Funagata; however, recent research has revealed that Mount Kurohana should be considered a separate volcano. Geology.

Geographic entities mentioned:
surface_form: mount funagata
instance_of: Mountain
countries: Japan
coordinates: lat: 38.45548
lon: 140.61997
surface_form: mount funagata
instance_of: Mountain
countries: Japan
coordinates: lat: 38.45548
lon: 140.61997
The summit of this prominence has an elevation of and lies about southeast of the Grand Scenic Divide, and west of Havasupai Point. This summit lies almost level with the surface of the adjacent tableland of the South Rim, the forested Kaibab Plateau. As seen in the above photograph, Fossil Mountain exhibits a large cliff of Kaibab Limestone.

Geographic entities mentioned:
surface_form: Kaibab Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 36.1267
lon: -112.009
Fossil Mountain (Grand Canyon). Fossil Mountain is a prominence that is located on a spur in the Western Grand Canyon, in Coconino County, Arizona. The summit of this prominence has an elevation of and lies about southeast of the Grand Scenic Divide, and west of Havasupai Point. This summit lies almost level with the surface of the adjacent tableland of the South Rim, the forested Kaibab Plateau.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain (grand canyon)
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Fossil Mountain (Grand Canyon). Fossil Mountain is a prominence that is located on a spur in the Western Grand Canyon, in Coconino County, Arizona. The summit of this prominence has an elevation of and lies about southeast of the Grand Scenic Divide, and west of Havasupai Point. This summit lies almost level with the surface of the adjacent tableland of the South Rim, the forested Kaibab Plateau.

Geographic entities mentioned:
surface_form: grand canyon
instance_of: Valley
countries: United States
coordinates: lat: 38.65888889
lon: -91.10388889
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
This summit lies almost level with the surface of the adjacent tableland of the South Rim, the forested Kaibab Plateau. As seen in the above photograph, Fossil Mountain exhibits a large cliff of Kaibab Limestone. The southwest slope of Fossil Mountain is a highly vegetated (trees), and high angle slope to the prominence.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
As seen in the above photograph, Fossil Mountain exhibits a large cliff of Kaibab Limestone. The southwest slope of Fossil Mountain is a highly vegetated (trees), and high angle slope to the prominence. Below the cliff of Kaibab Limestone is about ~ of vegetated slope-forming Toroweap Formation.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
Below the cliff of Kaibab Limestone is about ~ of vegetated slope-forming Toroweap Formation. The Toroweap Formation sits upon a ~ cliff-forming, Coconino Sandstone, very vertical, and uneroded, (northeast face of Fossil Mountain, overlooking the canyon). The Coconino Sandstone sits on large slopes of vegetated Hermit Formation. Geology.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
The Coconino Sandstone sits on large slopes of vegetated Hermit Formation. Geology. At Fossil Mountain, The Kaibab Limestone consists of often fossiliferous, light-gray,
thick-bedded, chert, cherty limestone and sandy limestone. It is thick and contains the abundant fossils of shallow marine organisms including brachiopods, bryozoans, sponges, and crinoids.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
The fossils found in the Kaibab Limestone at Fossil Mountain include &quot;Productus occidentalis&quot;, &quot;Composita sp.&quot;, &quot;Avonia sp.&quot;, &quot;Lophophyllum sp.&quot;, &quot;Meekella sp.&quot;, &quot;Pugnoides sp.&quot;, &quot;Spiriferina sp.&quot;, and &quot;Productus bassi&quot;.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
The fossils of crinoids typically consist of disarticulated columnals and plates
Fossil Mountain is the type section of the Fossil Mountain Member of the Kaibab Limestone. The geology and paleontology of Fossil Mountain was first described by E. D. McKee in 1938. Later, in 1962, J. E.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
D. McKee in 1938. Later, in 1962, J. E. Sorauf informally designated the lower, uniformly cherty limestones of the Kaibab Limestone, informally known as the &quot;β member&quot;, as the &quot;Fossil Mountain member&quot;. This name is based on the description of a measured section published by E. D. McKee in 1938 at Fossil Mountain and personal communications with him. Finally, in 1991, J. E.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
D. McKee in 1938 at Fossil Mountain and personal communications with him. Finally, in 1991, J. E. Sorauf and G. H. Billingsley formally named, in accordance with the rules of the North American Stratigraphic Code, the lower, uniformly cherty limestones of the Kaibab Limestone, as the &quot;Fossil Mountain Member&quot; with Fossil Mountain as its type location.

Geographic entities mentioned:
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.875833333333
lon: -113.46944444444
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6536
lon: -110.919
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
surface_form: fossil mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.19026
lon: -112.36157
According to the U.S. Census Bureau, Greensboro has a total area of, of which is land and, or 0.99%, is water. The city is in the Oconee River watershed and is located east of Lake Oconee and southeast of Oconee National Forest. Demographics. As of the 2020 United States census, there were 3,648 people, 1,288 households, and 808 families residing in the city. Greene County School District.

Geographic entities mentioned:
surface_form: Lake Oconee
instance_of: Lake
countries: United States
coordinates: lat: 33.35
lon: -83.157
White Escarpment. White Escarpment is an escarpment in the west part of the Heritage Range, Antarctica, extending for 15 nautical miles (28 km) between the heads of the Splettstoesser and Dobbratz Glaciers. Named by the University of Minnesota Geological Party to these mountains, 1963–64, for Chief Warrant Officer Ronald B.

Geographic entities mentioned:
surface_form: white escarpment
instance_of: Landform
coordinates: lat: -79.4833
lon: -85.6167
Mount Kurikoma. Mount Kurikoma, also known as Kurikomayama and Sukawadake is an active stratovolcano in Japan that stands tall. The volcano is located in Iwate Prefecture on Honshu, the largest of the four main islands of Japan. In addition to recent eruptions, the volcano is seismically active.

Geographic entities mentioned:
surface_form: mount kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
surface_form: kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
Mount Kurikoma. Mount Kurikoma, also known as Kurikomayama and Sukawadake is an active stratovolcano in Japan that stands tall. The volcano is located in Iwate Prefecture on Honshu, the largest of the four main islands of Japan. In addition to recent eruptions, the volcano is seismically active.

Geographic entities mentioned:
surface_form: mount kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
surface_form: kurikomayama
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
surface_form: kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
Geology. Mount Kurikoma composition is mostly andesitic to dacitic which formed atop elevated Tertiary dacitic tuffs and sedimentary rocks; hence the volcano's volume is smaller than its height suggests. In the early construction phase, lava erupted 500 thousand years ago to the north and south. It was followed by the formation of Higashi-Kurikoma.

Geographic entities mentioned:
surface_form: mount kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
surface_form: kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
The volcano is located in Iwate Prefecture on Honshu, the largest of the four main islands of Japan. In addition to recent eruptions, the volcano is seismically active. It is the main feature of Kurikoma Quasi-National Park and a tourist attraction due to its hot springs, hiking trails and flora. Geology.

Geographic entities mentioned:
surface_form: kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
In the early construction phase, lava erupted 500 thousand years ago to the north and south. It was followed by the formation of Higashi-Kurikoma. The volcanic cone Magusadake was last active 100 thousand years ago. The summit features a caldera across which is breached to the north and occupied by the Tsurugi-dake cone.

Geographic entities mentioned:
surface_form: kurikoma
instance_of: Mountain
countries: Japan
coordinates: lat: 38.96111111111111
lon: 140.7888888888889
Their strategic importance stems from the airport’s proximity to the Indonesian–Philippines border. History. In 1938, anticipating the outbreak of World War II and the growing threat of Japanese expansion, the Dutch colonial government constructed three airfields in North Sulawesi: Langowan (also known as Kalawiran), Mapanget, and a seaplane base in Tasuka, on the shores of Lake Tondano.

Geographic entities mentioned:
surface_form: Lake Tondano
instance_of: Lake
countries: Indonesia
coordinates: lat: 1.225
lon: 124.9
Fluchtkogel. The Fluchtkogel is a mountain in the Weisskamm group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: ötztal
instance_of: Valley
countries: Austria
coordinates: lat: 47.136944
lon: 10.927222
surface_form: fluchtkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 46.857777777778
lon: 10.7925
Fluchtkogel. The Fluchtkogel is a mountain in the Weisskamm group of the Ötztal Alps.

Geographic entities mentioned:
surface_form: fluchtkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 46.857777777778
lon: 10.7925
On October 12, 2015, she took part in her first 10k road race at the Tufts Health Plan 10k for Women and broke the Under-23 French 10k road race record in the time of 33 min 26 s. On December 13, 2015, aged 21, she competed in the senior race at the European Cross Country Championship in Hyères, France. She finished 20th, while the French senior women team won the silver medal.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
The existence of Titan was revealed in November 2006, following its discovery on 1 January 1999 after cavers discovered connections from the James Hall Over Engine Mine to both Speedwell Cavern and Peak Cavern. Previously, the deepest known underground shaft in Britain had been Gaping Gill on the slopes of Ingleborough in the Yorkshire Dales.

Geographic entities mentioned:
surface_form: Ingleborough
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.165833333333
lon: -2.3975
Geology. The rock is an andesite intrusion that formed when magma pushed upward then cooled and hardened while remaining underground. Research published in the 1930s and 1940s suggested the andesite may have been part of the Fifes Peaks Formation which includes lava flows erupted by an extinct volcano to the northeast.

Geographic entities mentioned:
surface_form: Fifes Peaks Formation
instance_of: Landform
countries: United States
coordinates: lat: 46.9737
lon: -121.3229
This time period coincides with the growth of the Cascade Mountains, a volcanic arc formed by the subduction of the Juan de Fuca Plate under the North American Plate but is not listed as a volcanic vent in geological maps produced by the Washington State Department of Natural Resources. It predates modern Cascade volcanoes like Mount Rainier to the west.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
surface_form: rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
Kloochman Rock. Kloochman Rock is a rocky outcrop in the Cascade Range east of Rimrock Lake in Yakima County, Washington, United States. The edifice is oriented linearly northwest to southeast with its highest elevation near the southeastern edge and lies within the Okanogan–Wenatchee National Forest. Geology.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: kloochman rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.66925
lon: -123.96852
surface_form: rimrock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6553
lon: -110.846
It is estimated to have formed between the Oligocene and Pliocene epochs. This time period coincides with the growth of the Cascade Mountains, a volcanic arc formed by the subduction of the Juan de Fuca Plate under the North American Plate but is not listed as a volcanic vent in geological maps produced by the Washington State Department of Natural Resources.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Kloochman Rock. Kloochman Rock is a rocky outcrop in the Cascade Range east of Rimrock Lake in Yakima County, Washington, United States. The edifice is oriented linearly northwest to southeast with its highest elevation near the southeastern edge and lies within the Okanogan–Wenatchee National Forest. Geology.

Geographic entities mentioned:
surface_form: kloochman rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.66925
lon: -123.96852
When his people found him, the chief consulted with his father and made a sacrifice of himself and the potential brides. Legend holds that Me-ow-wah became Goose Egg Mountain to the north while one of the women became Kloochman Rock. The Yakama-Cowlitz Trail used by the Yakama and Cowlitz peoples to cross the Cascades passed near the north side of Kloochman Rock.

Geographic entities mentioned:
surface_form: kloochman rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.66925
lon: -123.96852
Legend holds that Me-ow-wah became Goose Egg Mountain to the north while one of the women became Kloochman Rock. The Yakama-Cowlitz Trail used by the Yakama and Cowlitz peoples to cross the Cascades passed near the north side of Kloochman Rock. There is evidence that this route was used as early as 9,200 years ago making it one of the oldest known cross-Cascade trails.

Geographic entities mentioned:
surface_form: kloochman rock
instance_of: Mountain
countries: United States
coordinates: lat: 47.66925
lon: -123.96852
Jean-Baptiste Nompère de Champagny, duc de Cadore. Jean-Baptiste Nompère de Champagny, 1st duc de Cadore (4 August 1756 – 3 July 1834) was a French admiral and politician. He was born in Roanne, Loire. Entering the French royal navy in 1774, he fought through the war in America and resigned in 1787.

Geographic entities mentioned:
surface_form: Cadore
instance_of: Valley
countries: Italy
coordinates: lat: 46.50916667
lon: 12.35722222
Pointer Nunatak. Pointer Nunatak () is a conspicuous nunatak, 1,245 m, immediately east of Wedge Ridge in the west part of the Shackleton Range. First mapped in 1957 by the Commonwealth Trans-Antarctic Expedition and so named because it is an important landmark on the route from Blaiklock Glacier to Stratton Glacier which provides access from the west to the east part of the Shackleton Range.

Geographic entities mentioned:
surface_form: pointer nunatak
instance_of: Mountain
coordinates: lat: -80.6167
lon: -29
Chandra Varma was succeeded as king by his eldest son Devakanta. Legend has it that it was during the lifetime of Devakanta that the river Kaveri originated in Kodagu and flowed through South India. The Kaveri Purana states that Chandra Varma's progeny levelled the land, brought it under cultivation and invited Brahmins and other castes to settle the region.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Shortly afterwards, the Garibaldi Olympic Development Association (GODA) was created in order to prepare a bid to host the Winter Games in the region of Mount Garibaldi, near Whistler.

Geographic entities mentioned:
surface_form: Mount Garibaldi
instance_of: Mountain
countries: Canada
coordinates: lat: 49.850555555556
lon: -123.00472222222
Geography. Nagullanka covers a vast portion of the delta area of the Godavari river. This village is located on the north-east coast of Andhra Pradesh. It is bounded by Amalapuram on the north and by Bay of Bengal on the south and by West Godavari district on the west. It is situated between the northern latitudes of 16* 30' and 18* and between 81* 30' and 82* 30' of the eastern longitudes.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
H. Greenwood, who was the first to describe paedophagia, defines it to be a feeding behaviour evolved among cichlid fishes. Location. Paedophagy is found in fishes from Lake Victoria in Africa which in total has 200-300 species, but in regards to paedophages it is known to contain 8 species. Lake Malawi in Africa has in total 500-1000 species, but in paedophages contains only several species.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
H. Greenwood, who was the first to describe paedophagia, defines it to be a feeding behaviour evolved among cichlid fishes. Location. Paedophagy is found in fishes from Lake Victoria in Africa which in total has 200-300 species, but in regards to paedophages it is known to contain 8 species. Lake Malawi in Africa has in total 500-1000 species, but in paedophages contains only several species.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Lake Malawi in Africa has in total 500-1000 species, but in paedophages contains only several species. Other lakes which contain paegophages include Lake Edward and Lake George, both in Africa, and each contain only one species of paedophage.

Geographic entities mentioned:
surface_form: Lake Edward
instance_of: Lake
countries: Uganda
Democratic Republic of the Congo
coordinates: lat: -0.33333333333333
lon: 29.6
From Lake Malawi there are various species of cichlid fish that exhibit paedophagia, they include fishes from the genera &quot;Caprichromis&quot;, &quot;Hemitaeniochromis&quot;, and &quot;Naevochromis&quot;. In Lake Tanganyika species of the genus &quot;Haplotaxodon&quot; and &quot;Greenwoodochromis bellcrossi&quot; may also carry out this sort of feeding strategy. Mouth brooding.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Berseba. Berseba () is a village in the ǁKaras Region of southern Namibia. It is situated near the Brukkaros Mountain, a famous tourist destination. Berseba had 992 inhabitants in 2023. Geography. Berseba is situated north-west of Keetmanshoop near the Brukkaros Mountain, a famous tourist destination. It is the district capital of the Berseba electoral constituency. History.

Geographic entities mentioned:
surface_form: Brukkaros Mountain
instance_of: Mountain
countries: Namibia
coordinates: lat: -25.867222222222
lon: 17.781388888889
Six months later, on August 16, 1963, Louis and Fred Berlanti died. The private airplane he was flying with his son was sabotaged and exploded over Lake Okeechobee, Florida, killing them both. Fragments of their bodies and their exploded airplane were found floating in Lake Okeechobee.

Geographic entities mentioned:
surface_form: Lake Okeechobee
instance_of: Lake
countries: United States
coordinates: lat: 26.933333333333
lon: -80.8
The edicts are evidence of early political regimes, urbanism, and the spread of Buddhism within the Indian subcontinent. The team used a computer model to extrapolate 121 possible sites, mostly in the Deccan Plateau, Afghanistan-Pakistan border, North West India, based on similarities, such as geological and population data, to existing sites.

Geographic entities mentioned:
surface_form: Deccan Plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
Valsesian Autonomist Movement. The Valsesian Autonomist Movement (&quot;Movimento Autonomista Valsesiano&quot;, MAV) was a regionalist political party active in Valsesia, a valley region in Piedmont, Italy. The party was founded in 1980 by three members of the local section of the Italian Democratic Socialist Party and by the local leader of the Italian Liberal Party.

Geographic entities mentioned:
surface_form: Valsesia
instance_of: Valley
countries: Italy
coordinates: lat: 45.816666666667
lon: 8.1333333333333
During his year on the &quot;Phoenix&quot;, Harris and his crew performed triangulation along the coast from Pascagoula, Mississippi, to the entrance to Lake Pontchartrain, a distance of about. With the arrival of winter, the commanders left the &quot;Phoenix&quot;; when the weather turned colder, Harris was required to lay up the vessel for the remainder of the winter. He returned to U.S.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Kamakurakōkōmae Station. is a commuter railway station on the Enoshima Electric Railway (Enoden), located in the Koshigoe neighborhood of the city of Kamakura, Kanagawa Prefecture, Japan. Though small in size, it is known for its scenery, as it commands an open view of the Pacific Ocean and Mount Fuji from the station platform. Lines.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
Its habitat is moist but well-drained sandy loam, often at high altitudes. Red spruce can be easily damaged by windthrow and acid rain. Notable red spruce forests in West Virginia can be seen at Gaudineer Scenic Area, Canaan Valley, Roaring Plains West Wilderness, Dolly Sods Wilderness, and Spruce Mountain, all sites of former extensive red spruce forest. Related species.

Geographic entities mentioned:
surface_form: Canaan Valley
instance_of: Valley
countries: United States
coordinates: lat: 39.126666666667
lon: -79.378055555556
Tartt embarked on a mission to find the lost red spruce forest that had been planted by the DAR as a memorial to the lives lost during the American Revolution. The forest, consisting of 50,000 trees was dedicated in 1940 and had until recently been forgotten until Tartt located and identified the forest near Devil's Courthouse.

Geographic entities mentioned:
surface_form: Devil's Courthouse
instance_of: Mountain
countries: United States
coordinates: lat: 35.3025
lon: -82.8956
After Storms' arrival, villagers under Karema's Chief, Yassagula, attacked the Belgian fort, prompting Becker to lead a counterattack with his askaris and destroy the village. In 1884, Becker was ordered to lead an expedition to Lake Tanganyika, to link a series of captured &quot;bomas&quot; with forts he would build further inland.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
Mahnkopf. Mahnkopf (elevation) is a summit in the Falken Group, a subgroup of the Karwendel range in the Austrian state of Tyrol. Alpinism. The Mahnkopf is the only peak in the Falken Group that can be reached as a normal alpine hike, e.g. from the hut &quot;Falkenhütte&quot;, followed by the Steinfalk (UIAA I).

Geographic entities mentioned:
surface_form: Steinfalk
instance_of: Mountain
countries: Austria
coordinates: lat: 47.4272
lon: 11.5122
surface_form: steinfalk
instance_of: Mountain
countries: Austria
coordinates: lat: 47.4272
lon: 11.5122
Mahnkopf. Mahnkopf (elevation) is a summit in the Falken Group, a subgroup of the Karwendel range in the Austrian state of Tyrol. Alpinism. The Mahnkopf is the only peak in the Falken Group that can be reached as a normal alpine hike, e.g. from the hut &quot;Falkenhütte&quot;, followed by the Steinfalk (UIAA I).

Geographic entities mentioned:
surface_form: mahnkopf
instance_of: Mountain
countries: Austria
coordinates: lat: 47.41222
lon: 11.50778
Port Talbot, Ontario. Port Talbot was the name of a community located west of Port Stanley, about one hour's drive south from London, Ontario, Canada, where Talbot Creek flows into Lake Erie. The village was the original commercial nucleus for the settlement which developed on 5,000 acres (20 km2) of land granted to Thomas Talbot in 1800 by the Crown along the northwestern shore of Lake Erie.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Etymology. is the Nahuatl term for the heartland of the Aztec Empire, namely the Valley of Mexico and surrounding territories, with its people being known as the Mexica. It is generally believed that the toponym for the valley was the origin of the primary ethnonym for the Aztec Triple Alliance, but it may have been the other way around.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
Geopolitically, Mexico is entirely considered part of North America. The majority of Mexican central and northern territories are located at high altitudes, and as such the highest elevations are found at the Trans-Mexican Volcanic Belt which crosses Mexico east to west: Pico de Orizaba (), Popocatépetl () and Iztaccihuatl () and the Nevado de Toluca ().

Geographic entities mentioned:
surface_form: Pico de Orizaba
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.03
lon: -97.27
surface_form: Nevado de Toluca
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.101666666667
lon: -99.7675
The Mexican territory is prone to volcanism. Mexico has nine distinct regions: Baja California, the Pacific Coastal Lowlands, the Mexican Plateau, the Sierra Madre Oriental, the Sierra Madre Occidental, the Cordillera Neo-Volcánica, the Gulf Coastal Plain, the Southern Highlands, and the Yucatán Peninsula.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Double Lake. Double Lake is a pair of lakes in Cottonwood County, in the U.S. state of Minnesota. Double Lake was named from the fact these twin lakes are separated only by a narrow passage.

Geographic entities mentioned:
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 27.893888888889
lon: -81.594722222222
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 43.4834018
lon: -74.9490486
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 37.6181
lon: -119.008
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 44.8079
lon: -118.0867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 40.7433
lon: -115.283
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.0183
lon: -73.3867
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.23888889
lon: -111.86472222
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 60.638888888889
lon: -153.86305555556
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 48.6494
lon: -113.718
surface_form: double lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.05
lon: -95.375
surface_form: twin lakes
instance_of: Lake
countries: United States
coordinates: lat: 45.7487796
lon: -84.4527626
surface_form: twin lakes
instance_of: Lake
countries: United States
surface_form: twin lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.6375
lon: -89.41583333333334
Double Lake. Double Lake is a pair of lakes in Cottonwood County, in the U.S. state of Minnesota. Double Lake was named from the fact these twin lakes are separated only by a narrow passage.

Geographic entities mentioned:
surface_form: double lake
instance_of: Group of lakes
countries: United States
coordinates: lat: 44.05
lon: -95.375
Binalud, Iran. Binalud () is a city in Ahmadabad District of Mashhad County, Razavi Khorasan province, Iran. Along with Golbahar, Binalud is one of the two planned cities of the province. Etymology. The city is named after Mount Binalud. Geography. It has an area of about, of which are residential. The city of Binalud is situated near the south-eastern foot of Binalud Mountain Range.

Geographic entities mentioned:
surface_form: Mount Binalud
instance_of: Mountain
countries: Iran
coordinates: lat: 36.426388888889
lon: 58.849166666667