Sarmila/GeoWiki-Features huggingface dataset:
The Blistock (also spelled &quot;Blistögg&quot;) is a mountain of the Glarus Alps, overlooking Elm in the canton of Glarus. It lies on the range between the small valley of the Garichtisee and the Sernftal, north of the Kärpf. It is composed of three summits: the &quot;Vorder Blistock&quot; (2,405 m), the &quot;Mittler Blistock&quot; (2,448 m) and the &quot;Hinter Blistock&quot; (2,446 m).

Geographic entities mentioned:
surface_form: Sernftal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.961
lon: 9.171
surface_form: Kärpf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.91674
lon: 9.09323
surface_form: kärpf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.91674
lon: 9.09323
surface_form: sernftal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.961
lon: 9.171
Blistock. The Blistock (also spelled &quot;Blistögg&quot;) is a mountain of the Glarus Alps, overlooking Elm in the canton of Glarus. It lies on the range between the small valley of the Garichtisee and the Sernftal, north of the Kärpf.

Geographic entities mentioned:
surface_form: blistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.93138889
lon: 9.12027778
The Blistock (also spelled &quot;Blistögg&quot;) is a mountain of the Glarus Alps, overlooking Elm in the canton of Glarus. It lies on the range between the small valley of the Garichtisee and the Sernftal, north of the Kärpf. It is composed of three summits: the &quot;Vorder Blistock&quot; (2,405 m), the &quot;Mittler Blistock&quot; (2,448 m) and the &quot;Hinter Blistock&quot; (2,446 m).

Geographic entities mentioned:
surface_form: blistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.93138889
lon: 9.12027778
surface_form: blistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.93138889
lon: 9.12027778
surface_form: blistock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.93138889
lon: 9.12027778
Distribution and habitat. The Mexican spiny pocket mouse is endemic to parts of Texas and Mexico. Its range extends from just north of the Rio Grande southwards to the Mexican Plateau, its southernmost limit being Zapotitlán in the state of Oaxaca. It is found in dry shrubland at altitudes of up to.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
The 34 members of the party arrived in California via the Sonora Pass and followed the Stanislaus River down hill. They reached the confluence with the San Joaquin River on November 3, and several members of the group, including the Kelsey's, stopped at Doctor Marsh's ranch at the foot of Mount Diablo on November 4, 1841. The Kelseys stayed a month with Marsh before proceeding to Sutter's Fort.

Geographic entities mentioned:
surface_form: Mount Diablo
instance_of: Mountain
countries: United States
coordinates: lat: 37.881697781
lon: -121.914154997
Life in the west. During 1842, Nancy and Ben Kelsey worked for John Sutter collecting elk hides at Clear Lake, California. In 1843, while she was pregnant, they left Sutter's employ and drove cattle north along the California–Oregon Trail east of Mount Shasta, past Klamath Lake, and on to Oregon City.

Geographic entities mentioned:
surface_form: Mount Shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Lake Hughes, California. Lake Hughes is an unincorporated community and census-designated place in northern Los Angeles County, California, United States. It is in the Sierra Pelona Mountains, northwest of Palmdale and north of the Santa Clarita Valley, in the Angeles National Forest. It is on the sag pond waters of Lake Hughes and Elizabeth Lake.

Geographic entities mentioned:
surface_form: Santa Clarita Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.398
lon: -118.522
Settlers were drawn to the area because water was more plentiful than in the drier Antelope Valley. In 1907 William Mulholland, superintendent of the Los Angeles Department of Water and Power, started work on the Elizabeth Lake Tunnel for transporting water in the Los Angeles Aqueduct from Owens Valley to Los Angeles.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
Wolziger See. Wolziger See is a lake in Heidesee, Brandenburg, Germany. At an elevation of, its surface covers.

Geographic entities mentioned:
surface_form: wolziger see
instance_of: Lake
countries: Germany
coordinates: lat: 52.256388888889
lon: 13.820833333333
Mount Tanzawa. is a mountain of the Tanzawa Mountains, with an elevation of. Its summit marks the border between Sagamihara, Kiyokawa in Aikō District, and Yamakita in Ashigarakami District.

Geographic entities mentioned:
surface_form: mount tanzawa
instance_of: Mountain
countries: Japan
coordinates: lat: 35.474166666667
lon: 139.16277777778
It flows generally east and southeast about to join the Stikine River at Tahltan, British Columbia. The lower Tahltan River marks the boundary between the Tahltan Highland and the Nahlin Plateau, both of which are part of the larger Stikine Plateau region. The Tahltan River's watershed covers, and its mean annual discharge is.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
surface_form: Stikine Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.38305555555556
lon: -129.885
After flowing north briefly the Tahltan River is joined by its main tributary, the Little Tahltan River near the Indian reserve of Tahltan Forks 5, of the Tahltan First Nation. Turning east and southeast, the Tahltan River is joined by numerous tributaries including Bear Creek, Beatty Creek, Newell Creek, Middle Creek, and Hartz Creek.

Geographic entities mentioned:
surface_form: Hartz Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.04966
lon: -131.00386
Turning east and southeast, the Tahltan River is joined by numerous tributaries including Bear Creek, Beatty Creek, Newell Creek, Middle Creek, and Hartz Creek. In its last few kilometres the Tahltan River flows south to join the Stikine River in the Grand Canyon of the Stikine, at the locality of Tahltan and the Tahltan Indian Reserve Tahltan 1. History.

Geographic entities mentioned:
surface_form: Grand Canyon of the Stikine
instance_of: Valley
countries: Canada
coordinates: lat: 58.08222222222222
lon: -130.735
Vedkosten Peak. Vedkosten Peak () is a 2,285 m tall bare peak standing 1 nautical mile (1.9 km) southeast of Hoggestabben Butte in the Muhlig-Hofmann Mountains of Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Vedkosten (the wooden broom).

Geographic entities mentioned:
surface_form: Hoggestabben Butte
instance_of: Mountain
coordinates: lat: -72
lon: 3.96667
surface_form: vedkosten
instance_of: Mountain
coordinates: lat: -72.0167
lon: 3.96667
Vedkosten Peak. Vedkosten Peak () is a 2,285 m tall bare peak standing 1 nautical mile (1.9 km) southeast of Hoggestabben Butte in the Muhlig-Hofmann Mountains of Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Vedkosten (the wooden broom).

Geographic entities mentioned:
surface_form: vedkosten peak
instance_of: Mountain
coordinates: lat: -72.0167
lon: 3.96667
Vedkosten Peak. Vedkosten Peak () is a 2,285 m tall bare peak standing 1 nautical mile (1.9 km) southeast of Hoggestabben Butte in the Muhlig-Hofmann Mountains of Queen Maud Land. It was mapped by Norwegian cartographers from surveys and air photos by the Norwegian Antarctic Expedition (1956–60) and named Vedkosten (the wooden broom).

Geographic entities mentioned:
surface_form: vedkosten
instance_of: Mountain
coordinates: lat: -72.0167
lon: 3.96667
A descent back over the Upsspitze, the 'Grünen Ups&quot; (a viewing point) and the Tuftlalm to Lermoos takes about 2½ hours. The summit offers a splendid view of the Zugspitze massif to the east and the Mieminger Range chain to the south.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Located near the villages of Ehrwald and Lermoos, it is a popular mountain with hikers. Its north face is around 200 metres high and its south face has a more schrofen-like character. With the almost equally high Upsspitze (2,332 m) it forms a double summit. To the northwest is a neighbouring peak, the &quot;Hochschrutte&quot; (2,247 m). Ascent.

Geographic entities mentioned:
surface_form: hochschrutte
instance_of: Mountain
countries: Austria
coordinates: lat: 47.445
lon: 10.84194
Daniel (mountain). The Daniel (2,340 m) is a mountain in the Austrian state of Tyrol, and the highest peak in the Ammergau Alps, a range within the Northern Limestone Alps. Located near the villages of Ehrwald and Lermoos, it is a popular mountain with hikers. Its north face is around 200 metres high and its south face has a more schrofen-like character.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.4322
lon: 10.8803
Ascent. The summit may be reached on an easy mountain tour from the south, sure-footedness only being required on the summit arête from the Daniel to the Upsspitze. The ascent on the normal route starting at Leermoos and passing over the &quot;Tuftlalm&quot; and the &quot;Upsspitze&quot; takes about 3–4 hours according to the literature.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.4322
lon: 10.8803
North Wabasca Lake. North Wabasca Lake is located in northern Alberta, Canada, north of Edmonton and is the fifteenth largest lake in Alberta. The hamlet of Wabasca is located on the southeast shore of the lake, and along the path of the river flowing north from South Wabasca Lake. Two First Nations Reserves border the lake, Wabasca 166C in the northeast, and Wabasca 166B in the south. Geography.

Geographic entities mentioned:
surface_form: north wabasca lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.0475
lon: -113.9275
Two First Nations Reserves border the lake, Wabasca 166C in the northeast, and Wabasca 166B in the south. Geography. Surface area of the lake measures and is over long and at its widest point. North Wabasca Lake averages in depth and is at its deepest. The South Wabasca Lake outlet and Willow River in the south are the primary inflows.

Geographic entities mentioned:
surface_form: north wabasca lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.0475
lon: -113.9275
Other species of fish found in the lake include Northern Cisco, White Sucker, and Longnose Sucker. Over 25 species of zooplankton are found in North Wabasca Lake and are an important indicator of the health of the lake. Some examples of species native to the lake include Rotifer, Cladocera, Calanoida Copepod, Cyclopoida Copepod, and Nauplii.

Geographic entities mentioned:
surface_form: north wabasca lake
instance_of: Lake
countries: Canada
coordinates: lat: 56.0475
lon: -113.9275
USS Growler (1812 schooner). USS &quot;Growler&quot; was a 53-ton wooden schooner of 5 guns that served in the War of 1812, changing hands three times. The United States purchased &quot;Growler&quot; as &quot;Experiment&quot; on Lake Ontario during 1812, and was first commanded by Sailing Master M.P. Mix. She was actively employed with Isaac Chauncey's squadron on Lake Ontario from 1812 to 1814.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Arctostaphylos malloryi. &quot;Arctostaphylos malloryi&quot; is a species of manzanita known by the common name Mallory's manzanita. It is endemic to California. The plant is native to the Inner North Coast Ranges west and northwest of the Sacramento Valley. It is a resident of the chaparral plant community, often on volcanic soils. Description.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
History. μετροπολιτου περγης και ατταλειας θεογνωστου, υπερτιμου και εξαρχου της κενης δευτερας παμφυλιας. εν ατταλου τη μητροπολει αμβλυωπων. Αρχιερευς νειλος. In 1547 it was presented to the Iviron monastery at Mount Athos, where it was housed until 1655. It was examined by Matthaei. It is currently housed at the State Historical Museum (V. 412, S. 5), at Moscow.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Hayden Valley. Hayden Valley is a large, sub-alpine valley within Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger. The valley is well known as one of the best locations to view wildlife in Yellowstone national park. History.

Geographic entities mentioned:
surface_form: Yellowstone Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
History. The valley was the natural route to Yellowstone Lake as trappers, explorers and natives made their way up the Yellowstone River. On August 29, 1870, when Henry D. Washburn and Gustavus Cheyney Doane ascended Mount Washburn during the Washburn-Langford-Doane Expedition, they saw the great expanse of the Hayden Valley between Yellowstone Falls and the lake.

Geographic entities mentioned:
surface_form: Mount Washburn
instance_of: Mountain
countries: United States
coordinates: lat: 44.7975
lon: -110.43333333333
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Hayden Valley. Hayden Valley is a large, sub-alpine valley within Yellowstone National Park straddling the Yellowstone River between Yellowstone Falls and Yellowstone Lake. The valley floor along the river is an ancient lake bed from a time when Yellowstone Lake was much larger. The valley is well known as one of the best locations to view wildlife in Yellowstone national park. History.

Geographic entities mentioned:
surface_form: hayden valley
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
To the south appears a broad sheet of water -- the Yellowstone Lake. Although it is clear that the valley is named in honor of Ferdinand Vandeveer Hayden and his geological surveys of the Yellowstone region (as his 1871 survey led to the creation of the park), there is little definitive evidence as to who actually named the valley.

Geographic entities mentioned:
surface_form: hayden
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Location. The Hayden valley, centrally located in Yellowstone National Park, is approximately long north to south and wide east to west and occupies about of the park. It lies mostly to the west of the Yellowstone River between Canyon and Yellowstone Lake, in Wyoming. The Canyon to Lake section of the Grand Loop Road follows the eastern side of the valley near the river. Geothermal features.

Geographic entities mentioned:
surface_form: hayden valley
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Sensitive habitat. The Hayden Valley is outstanding wildlife habitat and is frequented by buffalo, elk, grizzly bears, coyote, wolves, and a host of smaller mammals and birds. To protect this habitat and prevent disturbing wildlife, the valley is closed to off-trail foot travel. Two trails make the valley accessible for hikers—the Hayden Valley trail and the Mary Mountain trail.

Geographic entities mentioned:
surface_form: hayden valley
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
Soløyvatnet. Soløyvatnet is a lake that lies in Bodø Municipality in Nordland county, Norway. The lake is located about northeast of the town of Bodø.

Geographic entities mentioned:
surface_form: soløyvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.313611111111
lon: 14.595277777778
California State Route 209. State Route 209 (SR 209) was a state highway in the U.S. state of California, connecting Cabrillo National Monument with the interchange of Interstate 5 (I-5) and I-8 in San Diego, passing through the neighborhoods of Point Loma. The majority of the route was along Rosecrans Street; it also included Cañon Street and Catalina Boulevard leading to the tip of Point Loma.

Geographic entities mentioned:
surface_form: Point Loma
instance_of: Landform
countries: United States
coordinates: lat: 32.67
lon: -117.24194444
An early map noted the area as Campbell's Gap. In 1851, Martin McCarthy, who had leased the mill, built a toll road down to the Santa Clara Valley and founded what is now Saratoga as &quot;McCarthysville&quot;. The toll gate was located at the present-day intersection of Big Basin Way and 3rd St., giving the town its first widely used name: &quot;Toll Gate&quot;. During the Civil War.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Puyang River. The Puyang River (浦阳江) is one of the three main tributaries of the Qiantang River (钱塘江) in Zhejiang Province (浙江省), China. At present, the Puyang River is 150 kilometers long and empties into the Qiantang River northwest of Linpu (临浦镇). The gazette of Xiaoshan County (蕭山縣誌) states: &quot;The Puyang River...

Geographic entities mentioned:
surface_form: puyang river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 30.10294
lon: 120.17618
Before the mid-15th century, the river ran east of Linpu to flow in a winding, snakelike course to the south of Xiaoshan (萧山) and the northwest of Shaoxing (绍兴市), leaving numerous lakes along its course before emptying into Hangzhou Bay. The frequent flooding of the Puyang River has resulted in it being called the &quot;Little Yellow River&quot;.

Geographic entities mentioned:
surface_form: puyang river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 30.10294
lon: 120.17618
Among the scenic sites located along or near the river are Matoushan (马头山), which has the shape of a horse's head, Nanshan (南山) with many strange rock formations, Changshan (常山), and Guanyenshan (官岩山), where legend says Yu the Great (Yu (Xia dynasty ruler)) ordered the opening of a channel for the Puyang River. Some of these names appear to come from the Shanhai Jing (山海经: A Chinese Bestiary).

Geographic entities mentioned:
surface_form: puyang river
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 30.10294
lon: 120.17618
The city of Tampere, the capital of the Pirkanmaa region, is located north of Akaa. Akaa, as well as the town of Toijala and the former municipality of Viiala are situated by the lake Vanajavesi, which is the most central watercourse in the Tavastia Proper region as well as in the southern parts of the Pirkanmaa region. Demographics.

Geographic entities mentioned:
surface_form: Vanajavesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.16666667
lon: 24.25
Turó del Galutxo. Turó del Galutxo is a mountain of Catalonia, Spain. It has an elevation of 851 metres above sea level.

Geographic entities mentioned:
surface_form: turó del galutxo
instance_of: Mountain
countries: Spain
coordinates: lat: 41.555
lon: 1.380833
Mount Yakebitai. is a mountain located in Yamanouchi, Nagano, Japan. For the 1998 Winter Olympics, it hosted the alpine skiing slalom and snowboarding giant slalom events. During the 1998 games, the mountain suffered a mild earthquake that registered 5.0 on the Richter magnitude scale, but the skiing events continued.

Geographic entities mentioned:
surface_form: mount yakebitai
instance_of: Mountain
countries: Japan
coordinates: lat: 36.766666666667
lon: 138.51666666667
Näsijärvi is then used for Nordic walking, cross-country skiing, and everyday pleasure walking. There is a small, rocky island upon which a lighthouse, called, is located; it is the most popular walking destination on the lake. In the north Näsijärvi has a wide catchment area that includes among others the lakes Ruovesi, Kuorevesi, Keurusselkä, Tarjanne, Pihlajavesi, Toisvesi and Ähtärinjärvi.

Geographic entities mentioned:
surface_form: Ruovesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.004128
lon: 24.11047
surface_form: Kuorevesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.9577401
lon: 24.710365
surface_form: Keurusselkä
instance_of: Lake
countries: Finland
coordinates: lat: 62.18333333333333
lon: 24.683333333333334
surface_form: Tarjanne
instance_of: Lake
countries: Finland
coordinates: lat: 62.11384
lon: 24.076824
surface_form: Toisvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.29424
lon: 23.73058
surface_form: Ähtärinjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.69768
lon: 24.06426
surface_form: näsijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.566666666667
lon: 23.766666666667
surface_form: pihlajavesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.36057
lon: 24.27715
surface_form: pihlajavesi
instance_of: Lake
countries: Finland
coordinates: lat: 61.68081
lon: 28.67648
Näsijärvi. Näsijärvi () is a lake above sea level, in the Pirkanmaa region of southern Finland. Näsijärvi is the biggest lake in the Tampere area at in size. The city of Tampere was built along the Tammerkoski rapids, through which the lake drains into Pyhäjärvi. The water quality of the lake has improved as forest industry has decreased the amount of waste water.

Geographic entities mentioned:
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.48333333
lon: 23.66666667
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 60.9889329
lon: 22.2989207
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 62.7238
lon: 25.46206
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 63.58333333
lon: 25.95
surface_form: pyhäjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.013333
lon: 26.491667
Näsijärvi. Näsijärvi () is a lake above sea level, in the Pirkanmaa region of southern Finland. Näsijärvi is the biggest lake in the Tampere area at in size. The city of Tampere was built along the Tammerkoski rapids, through which the lake drains into Pyhäjärvi. The water quality of the lake has improved as forest industry has decreased the amount of waste water.

Geographic entities mentioned:
surface_form: näsijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.566666666667
lon: 23.766666666667
Between Koljonselkä and Vankavesi is an archipelago, to the south of which the lake is crossed by the terminal moraine of the Inner Finland. There are boat cruising services on Näsijärvi. In 1929, the steamer SS Kuru sinking in the lake, with at least 136 people drowning including the Member of the Parliament Ida Vihuri, remains the deadliest Finnish inland shipping disaster.

Geographic entities mentioned:
surface_form: näsijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.566666666667
lon: 23.766666666667
During the winter, usually during February and March, the lake is frozen in its entirety. Näsijärvi is then used for Nordic walking, cross-country skiing, and everyday pleasure walking. There is a small, rocky island upon which a lighthouse, called, is located; it is the most popular walking destination on the lake.

Geographic entities mentioned:
surface_form: näsijärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.566666666667
lon: 23.766666666667
It is located in the Graz Basin and surrounded by mountains and hills to the north, east and west. The city centre sits at an elevation of, the highest point is Plabutsch mountain with at the western border. The mountain Schöckl is just a few kilometres to the north and surmounts the city by. Climate.

Geographic entities mentioned:
surface_form: Schöckl
instance_of: Mountain
countries: Austria
coordinates: lat: 47.19838
lon: 15.46607
From the Transylvanian Plateau, with heights between, in the North and East, the heights grow abruptly through a zone of deep valleys at about on the verge of the massif where some villages are situated. The heights continue to grow slowly towards the highest peak, &quot;Cindrel Peak&quot;, at.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
Keshava starts a new life with his sister and Satyabhama. Production. &quot;Keshava&quot; was primarily filmed in Visakhapatnam, Araku, Kakinada, and Narasapuram, as the story is set in these locations. Director Sudheer Varma selected these areas due to his personal connection, having studied in Visakhapatnam and Kakinada. Some scenes were even shot at his former school.

Geographic entities mentioned:
surface_form: Araku
instance_of: Valley
countries: India
coordinates: lat: 18.3333
lon: 82.8667
Although the Knobs (peak elevation: 2,854 ft) are dwarfed by Spruce Mountain to the west (peak: 4,840 ft) and by North Fork Mountain to the east (peak: 4,588 ft), they are notable for their series of prominent &quot;razorback&quot; ridges or &quot;fins&quot;. The largest and most famous of these blade-like crags is Seneca Rocks. Geography.

Geographic entities mentioned:
surface_form: North Fork Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.405555555556
lon: -74.198888888889
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.75
lon: -79.48
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.0175
lon: -74.45
surface_form: north fork mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.6675
lon: -79.4378
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.5521
lon: -114.822
surface_form: spruce mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.33007
lon: -74.1154089
Although the Knobs (peak elevation: 2,854 ft) are dwarfed by Spruce Mountain to the west (peak: 4,840 ft) and by North Fork Mountain to the east (peak: 4,588 ft), they are notable for their series of prominent &quot;razorback&quot; ridges or &quot;fins&quot;. The largest and most famous of these blade-like crags is Seneca Rocks. Geography.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
From north to south the most prominent features are Roy Gap (with its Seneca Rocks), Harper Knob (2,820 ft), Harper Gap, Harmon Knob (2,854 ft), Hinkle Gap, Germany Knob (2,802 ft), Riverton Gap, Judy Gap (with its Judy Rocks), Nelson Gap (with its Nelson Rocks), False Gap, Lambert Gap, Pike Gap and Teter Gap.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
The Knobs are part of the same structural fold of the Earth's crust that continues to the north as Champe Knobs (with its Champe Rocks and Yellow Rocks) and to the south as River Hill and (in Virginia) Lantz Mountain. Geology.

Geographic entities mentioned:
surface_form: Champe Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
surface_form: champe rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
The tough quartzite of the western walls resisted this process, leaving the soaring &quot;fins&quot; - narrow vertical plates of exposed rock. About east, along the top of North Fork Mountain, the horizontal strata of the far slope of the Tuscarora anticline are also visible. At Champe Rocks and Nelson Rocks the outcroppings are seen as not one, but two parallel fins.

Geographic entities mentioned:
surface_form: Champe Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8914
lon: -79.3117
Nelson Rocks is considered one of the best examples of the &quot;faulted Tuscarora&quot;. Seneca Rocks is a much thicker, monolithic formation because there the rock did not fault cleanly into two layers, but rather rolled over on itself. From Roy Gap, looking north, this effect is clearly visible in the curving layers of rock surrounding the large cave in the south end of Seneca Rocks.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
Nelson Rocks is considered one of the best examples of the &quot;faulted Tuscarora&quot;. Seneca Rocks is a much thicker, monolithic formation because there the rock did not fault cleanly into two layers, but rather rolled over on itself. From Roy Gap, looking north, this effect is clearly visible in the curving layers of rock surrounding the large cave in the south end of Seneca Rocks.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
River Knobs (West Virginia). &quot;For other &quot;River Knobs&quot;, see River Knobs (disambiguation).&quot;
The River Knobs — formerly known as East Seneca Ridge — are a ridge and series of knobs in western Pendleton County, West Virginia, USA, along a stretch of the North Fork South Branch Potomac River.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
The largest and most famous of these blade-like crags is Seneca Rocks. Geography. The River Knobs stretch for about from near Cherry Grove to near Seneca Rocks and are situated in a southwest/northeast orientation. They are a minor part of the High Alleghenies of the Appalachian Mountains. Their rock outcrops are clearly visible from WV 55 and US 33.

Geographic entities mentioned:
surface_form: seneca
instance_of: Lake
countries: United States
coordinates: lat: 42.655555555556
lon: -76.8975
surface_form: seneca rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
River Knobs (West Virginia). &quot;For other &quot;River Knobs&quot;, see River Knobs (disambiguation).&quot;
The River Knobs — formerly known as East Seneca Ridge — are a ridge and series of knobs in western Pendleton County, West Virginia, USA, along a stretch of the North Fork South Branch Potomac River.

Geographic entities mentioned:
surface_form: river knobs
instance_of: Mountain
countries: United States
coordinates: lat: 38.7369
lon: -79.4347
The River Knobs trace the western wall of this arch, or anticline, where the Tuscarora was turned a full 90 degrees from horizontal to vertical. Over time, erosion stripped away the softer rock covering the arch, and finally the dome of the arch itself. The tough quartzite of the western walls resisted this process, leaving the soaring &quot;fins&quot; - narrow vertical plates of exposed rock.

Geographic entities mentioned:
surface_form: the dome
instance_of: Mountain
countries: United States
coordinates: lat: 46.307777777778
lon: -122.1575
Almere. Almere () is a planned city and municipality in the province of Flevoland, Netherlands across the IJmeer from Amsterdam.

Geographic entities mentioned:
surface_form: IJmeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.362778
lon: 5.051944
It is the most western municipality of the province Flevoland. It borders with Markermeer in the west and north, Lelystad in the northeast, Zeewolde in the east, and Gooimeer in the south. Almere consists of three boroughs and three districts (Dutch: &quot;stadsdelen&quot;), three of which are under construction. Climate.

Geographic entities mentioned:
surface_form: Markermeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.566666666667
lon: 5.2166666666667
surface_form: Gooimeer
instance_of: Lake
countries: Netherlands
coordinates: lat: 52.321389
lon: 5.206389
Scheuereckberg. Scheuereckberg is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: scheuereckberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.067777777778
lon: 13.330833333333
Verona Beach, New York. Verona Beach is a hamlet in Oneida County, New York, United States. The community is located along the eastern shore of Oneida Lake and New York State Route 13; the Erie Canal separates the community from neighboring Sylvan Beach. Verona Beach has a post office with ZIP code 13162. Verona Beach State Park is located in the community.

Geographic entities mentioned:
surface_form: Oneida Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
In 2014, its teams were mostly assimilated into the 18-team league of large eastern and northeastern Pennsylvania high schools known as the Eastern Pennsylvania Conference. History. There had been widespread discussion about high school league realignment in the Lehigh Valley starting in late 1990 and early 1991. In the fall of 1993, the Mountain Valley Conference was formed.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
BES SC 390 was collected from an oil shale at Cava di Besano of the Besano Formation (Grenzbitumenzone). These lagoonal beds are equivalent to those at Monte San Giorgio, dating to the Anisian-Ladinian boundary, probably to the latest Anisian at this location, of the early Middle Triassic, about 243 million years ago. Nicole Klein and Oliver J.

Geographic entities mentioned:
surface_form: Monte San Giorgio
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.916666666667
lon: 8.95
Batterbee Mountains. The Batterbee Mountains are a group of prominent mountains rising to, which forms part of the dissected edge of Dyer Plateau overlooking George VI Sound, on the west coast of Palmer Land.

Geographic entities mentioned:
surface_form: Dyer Plateau
instance_of: Landform
coordinates: lat: -70.5
lon: -65
Mount Kaimon. , or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small complex central lava dome – which rises to a height of 924 metres above sea level near the city of Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as &quot;the Fuji of Satsuma&quot;.

Geographic entities mentioned:
surface_form: mount kaimon
instance_of: Mountain
countries: Japan
coordinates: lat: 31.18
lon: 130.52833333333
Mount Kaimon. , or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small complex central lava dome – which rises to a height of 924 metres above sea level near the city of Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as &quot;the Fuji of Satsuma&quot;.

Geographic entities mentioned:
surface_form: mount kaimon
instance_of: Mountain
countries: Japan
coordinates: lat: 31.18
lon: 130.52833333333
surface_form: ibusuki
instance_of: Mountain
countries: Japan
coordinates: lat: 31.18
lon: 130.52833333333
Together with Mt. Noma and Mt. Kinpo, it is used by marine traffic. Geology. Part of the Ibusuki volcanic field, Mt. Kaimon defines the eastern margin of the old Ata Caldera. The total eruptive volume of tephra has been and of lava. There is a sea scarp which is 7.8 km wide and 9.3 km long, the shape is similar to a horseshoe in the seabed at the southern foot of the mountain.

Geographic entities mentioned:
surface_form: ibusuki
instance_of: Mountain
countries: Japan
coordinates: lat: 31.18
lon: 130.52833333333
Mount Kaimon. , or Mount Kaimon, is an undissected volcano – consisting of a basal stratovolcano and a small complex central lava dome – which rises to a height of 924 metres above sea level near the city of Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as &quot;the Fuji of Satsuma&quot;.

Geographic entities mentioned:
surface_form: fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
The airline will later restart the flights to Ghaziabad and Pantnagar. As of October 2024, it was reported that the IAF and MoD were in an advanced stage of talks with the State Government to take over or operate from 3 civilian airports, including the Gauchar, Pithoragarh Airport and Dharasu Airports. The IAF has plans to establish an airstrip in the Spiti region as well.

Geographic entities mentioned:
surface_form: Spiti
instance_of: Valley
countries: India
Qing dynasty
coordinates: lat: 32.246944444444445
lon: 78.05222222222223
He was promoted to lieutenant on 1 July 1881, served as adjutant to the 1st Battalion from 1885 to 1887, during which he was promoted to captain on 12 June 1886, then passed through the Staff College and entered a career of staff posts. Cavendish climbed Paektu Mountain in 1891, and published an account of his experiences in 1894.

Geographic entities mentioned:
surface_form: Paektu Mountain
instance_of: Mountain
countries: North Korea
People's Republic of China
coordinates: lat: 41.992777777778
lon: 128.07722222222
Tête de Valpelline. Tête de Valpelline is a mountain of the Pennine Alps, located on the Swiss-Italian border. It lies west of the Dent d'Hérens, between the valleys of Mattertal (Valais) and Valpelline (Aosta Valley).

Geographic entities mentioned:
surface_form: Dent d'Hérens
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.970055555556
lon: 7.6050833333333
surface_form: Mattertal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.083333333333
lon: 7.8
Tête de Valpelline. Tête de Valpelline is a mountain of the Pennine Alps, located on the Swiss-Italian border. It lies west of the Dent d'Hérens, between the valleys of Mattertal (Valais) and Valpelline (Aosta Valley).

Geographic entities mentioned:
surface_form: tête de valpelline
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.975333333333
lon: 7.5811388888889
&quot;Bloodsport&quot; is one of the few films featuring scenes filmed inside Kowloon Walled City before its demolition in 1993. Other locations included The Peninsula Hotel, Causeway Bay, Hong Kong Trail, Victoria Peak, and Stanley Fort. Soundtrack.

Geographic entities mentioned:
surface_form: Victoria Peak
instance_of: Mountain
countries: People's Republic of China
British Hong Kong
coordinates: lat: 22.275469444444
lon: 114.14382777778
Lleulleu Lake. Lleulleu Lake is a Chilean lake located in the Bío Bío Region. It is located on the western slope of the Cordillera de Nahuelbuta, administratively divided between the communes of Contulmo to the north and Tirúa to the south. It has an area of 4300 hectares. It has been declared by the Chilean authority as the purest lake in Latin America.

Geographic entities mentioned:
surface_form: lleulleu lake
instance_of: Lake
countries: Chile
coordinates: lat: -38.15
lon: -73.333333333333
Kvarnsjön, Gladö. Kvarnsjön is a lake in Stockholm County, Södermanland, Sweden. It is part of the Tyresån lake system.

Geographic entities mentioned:
surface_form: Tyresån lake system
instance_of: Group of lakes
countries: Sweden
coordinates: lat: 59.2333
lon: 18.1667
Kvarnsjön, Gladö. Kvarnsjön is a lake in Stockholm County, Södermanland, Sweden. It is part of the Tyresån lake system.

Geographic entities mentioned:
surface_form: kvarnsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.192777777778
lon: 18.080833333333
surface_form: kvarnsjön, gladö
instance_of: Lake
countries: Sweden
coordinates: lat: 59.183888888889
lon: 17.971666666667
Kvarnsjön, Gladö. Kvarnsjön is a lake in Stockholm County, Södermanland, Sweden. It is part of the Tyresån lake system.

Geographic entities mentioned:
surface_form: kvarnsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.192777777778
lon: 18.080833333333
surface_form: kvarnsjön
instance_of: Lake
countries: Sweden
coordinates: lat: 59.183888888889
lon: 17.971666666667
On July 29, 2011, after the second round of voting, it was declared 1 of 28 finalists. Mayor Edward S. Hagedorn extended his gratitude to all those who supported and voted for the PPUR. On November 11, 2011, it was provisionally chosen as one of the New7Wonders, together with the Amazon rainforest, Halong Bay, Iguazu Falls, Jeju Island, Komodo Island, and Table Mountain.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The name &quot;Lachen&quot; means &quot;big pass&quot;. The Sikkimese government promotes it as a tourist destination. The town serves as a base for visiting the Chopta Valley and Gurudongmar Lake. An annual yak race, the &quot;Thangu&quot; is held there in summer. Unlike other places in India, Lachen has a unique form of self-governance, &quot;Dzumsa&quot;.

Geographic entities mentioned:
surface_form: Chopta Valley
instance_of: Valley
countries: India
coordinates: lat: 30.4878
lon: 79.2094
surface_form: Gurudongmar Lake
instance_of: Lake
countries: India
coordinates: lat: 28.02
lon: 88.71
Tourism. The Lachen monastery and the women's handicraft centre to view the weaving of traditional blankets and carpets reveal the local way of life. Gurudongmar Lake at 17,800 ft elevation is encircled by snowy massifs.Thangu offers accommodations 30 km from Lachen. During summer and monsoon, it is dotted with flowers.

Geographic entities mentioned:
surface_form: Gurudongmar Lake
instance_of: Lake
countries: India
coordinates: lat: 28.02
lon: 88.71
The heads of the Dzumsa are known as Pipon and Gyenbos. To the north, there is the old town of Thangu where the daytime temperature varies from 4 to 12 degrees Celsius (40 to 55 °F), even in the months of June and July. Gurudongmar Lake can be reached from Lachen, a sacred lake in the Great Himalayas Region. Lachen is connected with numerous routes in India.

Geographic entities mentioned:
surface_form: Gurudongmar Lake
instance_of: Lake
countries: India
coordinates: lat: 28.02
lon: 88.71
According to the 2008 census its population is 4,251, up from 3,893 in 1998, with an annual growth rate of 0.9%. The commune covers an area of. Geography. Ouled Khoudir lies at in the Saoura valley the on banks of Oued Saoura, a wadi that separates the Grand Erg Occidental, a large area of sand dunes in the Sahara desert to the east, from the rocky hills of the Ougarta Range to the west. Climate.

Geographic entities mentioned:
surface_form: Saoura
instance_of: Valley
countries: Algeria
France
coordinates: lat: 29.45
lon: -1.4333333333333
In the ninth century the relics of Rufus of Metz were transferred to the local church in the Roman Catholic Diocese of Mainz. In 1268, the vast holdings owned by the Lords of Bolanden between the Donnersberg and the Rhine were shared out among offspring, among whom an open feud later broke out, which claimed some participants’ lives.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Production. Shooting took place in 1989 in Arizona, mostly in Phoenix. Parts of the film were also shot at Glen Canyon in Utah. Release. Hemdale shelved the film for over a year before finally giving it a limited release. It was released to home video on August 21, 1992 and on DVD and Blu-ray on February 2, 2016. Reception.

Geographic entities mentioned:
surface_form: Glen Canyon
instance_of: Valley
countries: United States
coordinates: lat: 36.86443
lon: -111.58794
1. The oldest and largest one was on the southeastern bank of the Flint River (Georgia), a few miles from its merger with the Chattahoochee to form the Apalachicola River, in southwest Georgia (modern Decatur County). European references to it begin in the late 18th century.

Geographic entities mentioned:
surface_form: Chattahoochee
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
In 1799 its population was about 59, &quot;but this number had grown to several hundred by 1813&quot;. 2. The second (1814–1816) was in Spanish Florida, on the west bank of the Chattahoochee River, across from &quot;Tocktoethla&quot; (&quot;River Junction&quot;), in modern Jackson County, Florida. 3.

Geographic entities mentioned:
surface_form: Chattahoochee River
instance_of: Watercourse
countries: United States
coordinates: lat: 30.7088028
lon: -84.8638097
Also, David Brydie Mitchell, former governor of Georgia and Creek Indian agent at the time, stated in a report to Congress that this attack on Fowltown was the start of the First Seminole War. 4. The final Fowltown was also in Spanish Florida, on the eastern shore of Lake Miccosukee, in modern Jefferson County, Florida.

Geographic entities mentioned:
surface_form: Lake Miccosukee
instance_of: Lake
countries: United States
coordinates: lat: 30.5707
lon: -83.9791
The last burial of an English monarch prior to this was 43 years earlier, for Edward VIII, who abdicated and became Duke of Windsor, in 1972. The cathedral tomb was designed by van Heyningen and Haward Architects and made by James Elliott. The tombstone features a cross deeply incised into a rectangular block of pale Swaledale fossil stone quarried in North Yorkshire.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
He was given then control of the brigade of operations of Guadalajara, and later another part of the forces of &quot;Centro&quot;, taking part in combats in Campillo de Alto Buey, Huélamo and Muela de Chert, siege and surrender of Cantavieja, Sanahuja, Montanicell, Torá, and Tremp. He took his brigade to Navarre, occupying Oteiza and Monte Esquinza.

Geographic entities mentioned:
surface_form: Muela de Chert
instance_of: Mountain
countries: Spain
coordinates: lat: 40.53166667
lon: 0.15194444
Santa Cruz Chico. Santa Cruz Chico, is a mountain in the Cordillera Blanca in the Andes of Peru; within Santa Cruz District, Huaylas Province, Ancash. It has a height of.

Geographic entities mentioned:
surface_form: santa cruz
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083
surface_form: santa cruz chico
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083
Santa Cruz Chico. Santa Cruz Chico, is a mountain in the Cordillera Blanca in the Andes of Peru; within Santa Cruz District, Huaylas Province, Ancash. It has a height of.

Geographic entities mentioned:
surface_form: santa cruz
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083
surface_form: santa cruz
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083
surface_form: santa cruz chico
instance_of: Mountain
countries: Peru
coordinates: lat: -8.89429
lon: -77.7083