Sarmila/GeoWiki-Features huggingface dataset:
Scotia River. The Scotia River is a tributary of the Skeena River in the North Coast Regional District of the province of British Columbia, Canada. It originates in the Kitimat Ranges of the Coast Mountains, and flows north about to the tidally-influenced lower Skeena River, about upriver from Port Essington, southeast of Prince Rupert, and about southwest of Terrace.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
Natural history. The Scotia River mainstem and west fork support of runs of salmonids such as coho salmon, pink salmon, and steelhead trout. Between the river's source lake and the west fork confluence a waterfall limits anadromous fish passage. Most of the Scotia River's watershed has been repeatedly logged since the 1980s.

Geographic entities mentioned:
surface_form: source lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5608
lon: -78.6503
surface_form: source lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.815
lon: -94.1475
Scotia River. The Scotia River is a tributary of the Skeena River in the North Coast Regional District of the province of British Columbia, Canada. It originates in the Kitimat Ranges of the Coast Mountains, and flows north about to the tidally-influenced lower Skeena River, about upriver from Port Essington, southeast of Prince Rupert, and about southwest of Terrace.

Geographic entities mentioned:
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
Its watershed covers, and its mean annual discharge is. Geography. The Scotia River originates in an unnamed lake fed by several small streams. The river flows north from the lake about to the Skeena River, just west of the Khtada River. Its main tributary of the West Fork Scotia River.

Geographic entities mentioned:
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
Geography. The Scotia River originates in an unnamed lake fed by several small streams. The river flows north from the lake about to the Skeena River, just west of the Khtada River. Its main tributary of the West Fork Scotia River. The Scotia River's watershed's land cover is classified as 62.5% Coniferous, 21.6% Herb, 19.3% Shrub, and 17.4% Barren. Natural history.

Geographic entities mentioned:
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
The Scotia River's watershed's land cover is classified as 62.5% Coniferous, 21.6% Herb, 19.3% Shrub, and 17.4% Barren. Natural history. The Scotia River mainstem and west fork support of runs of salmonids such as coho salmon, pink salmon, and steelhead trout. Between the river's source lake and the west fork confluence a waterfall limits anadromous fish passage.

Geographic entities mentioned:
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
Between the river's source lake and the west fork confluence a waterfall limits anadromous fish passage. Most of the Scotia River's watershed has been repeatedly logged since the 1980s. In recent decades logging has focused on upland areas, using both conventional and helicopter logging.

Geographic entities mentioned:
surface_form: scotia river
instance_of: Watercourse
countries: Canada
coordinates: lat: 54.16839
lon: -129.63619
Course. The nominal source of the Speyerbach is located near the hamlet of Speyerbrunn in the municipality of Elmstein, in the middle of the Palatinate Forest, east of the Palatine Watershed. It has an elevation of AMSL; the surrounding Frankenweide hills climbing up to in height (Eschkopf).

Geographic entities mentioned:
surface_form: Eschkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.3103
lon: 7.85361
Breakneck Hill. Breakneck Hill is a mountain in the Ridge and Valley region of the Appalachian Mountains, located in Allegany County, Maryland. The ridge is just south of Interstate 68 across from Rocky Gap State Park, approximately northwest of the town of Rush.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: breakneck hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.6768
lon: -78.6386
Breakneck Hill. Breakneck Hill is a mountain in the Ridge and Valley region of the Appalachian Mountains, located in Allegany County, Maryland. The ridge is just south of Interstate 68 across from Rocky Gap State Park, approximately northwest of the town of Rush.

Geographic entities mentioned:
surface_form: breakneck hill
instance_of: Mountain
countries: United States
coordinates: lat: 39.6768
lon: -78.6386
His story is intertwined with that of Kolbeinn Sigmundarson and the Skagafjörður region in Iceland. He established his residence in Hóf in Hjaltadalur valley, which is named for him and was previously acquired by Kolbeinn and Sleitu-Björn Hróarsson in his time. According to the &quot;Landnámabók&quot;, his two sons, Þorvaldur and Þórður, became prominent figures in the Icelandic Commonwealth.

Geographic entities mentioned:
surface_form: Hjaltadalur
instance_of: Valley
countries: Iceland
coordinates: lat: 65.73107
lon: -19.12997
Tobique First Nation. Tobique First Nation () is one of six Wolastoqiyik or Maliseet Nation band governments in New Brunswick, Canada. The Tobique Reserve is located on the north side of the Tobique River. The reserve comprises two lots (18, 4 ha; Tobique #20, 2724 ha). The Tobique Reserve, established in 1801 with nearly, was granted after a petition to the government by band members.

Geographic entities mentioned:
surface_form: Tobique River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.7667
lon: -67.7
Confrontation with New Brunswick Power Corporation. Tobique First Nation and the New Brunswick Power Corporation (NB Power) (a Crown corporation) have had a long history of confrontation over uses of the land and waters. The First Nation rejected the company's bid to construct a hydro-electric dam on the Tobique River in 1844, and in 1895.

Geographic entities mentioned:
surface_form: Tobique River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.7667
lon: -67.7
The First Nation rejected the company's bid to construct a hydro-electric dam on the Tobique River in 1844, and in 1895. By 1945, the provincial and federal Canadian governments had started development of a dam on the Tobique River, the Tobique Narrows Dam.

Geographic entities mentioned:
surface_form: Tobique River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.7667
lon: -67.7
It is situated in the La Paz Department, at the border of the Inquisivi Province, Quime Municipality, and the Loayza Province, Cairoma Municipality and Malla Municipality. Quri Ch'uma lies south of Salvador Apachita and northwest of Yaypuri.

Geographic entities mentioned:
surface_form: Yaypuri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.9083
lon: -67.4158
surface_form: yaypuri
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.9083
lon: -67.4158
Quri Ch'uma. Quri Ch'uma (Aymara &quot;quri&quot; gold, &quot;ch'uma&quot; filtering, &quot;gold filtering&quot;, also spelled &quot;Corichuma, Corri Chuma, Khori Chuma, Korichuma&quot;), also named Inmaculado, is a mountain in the Kimsa Cruz mountain range in the Bolivian Andes, about 5,312 metres (17,428 ft) high.

Geographic entities mentioned:
surface_form: khori chuma
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
surface_form: inmaculado
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
surface_form: quri ch'uma
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
surface_form: corri chuma
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
surface_form: korichuma
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
Quri Ch'uma. Quri Ch'uma (Aymara &quot;quri&quot; gold, &quot;ch'uma&quot; filtering, &quot;gold filtering&quot;, also spelled &quot;Corichuma, Corri Chuma, Khori Chuma, Korichuma&quot;), also named Inmaculado, is a mountain in the Kimsa Cruz mountain range in the Bolivian Andes, about 5,312 metres (17,428 ft) high.

Geographic entities mentioned:
surface_form: quri ch'uma
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.8958
lon: -67.4517
The Johnsons' first African expedition, from 1921 to 1922, resulted in their feature film &quot;Trailing Wild African Animals&quot; (1923). During the second and longest trip, from 1924 to 1927, the Johnsons spent much of their time in northern Kenya by a lake they dubbed Paradise, at Mount Marsabit.

Geographic entities mentioned:
surface_form: Mount Marsabit
instance_of: Mountain
countries: Kenya
coordinates: lat: 2.3166666666667
lon: 37.966666666667
On their fifth African trip, from 1933 to 1934, the Johnsons flew the length of Africa, getting now classic aerial scenes of large herds of elephants, giraffes, and other animals moving across the plains of Africa. They were the first pilots to fly over Mount Kilimanjaro and Mount Kenya in Africa and film them from the air. The 1935 feature film &quot;Baboona&quot; was made from this footage.

Geographic entities mentioned:
surface_form: Mount Kenya
instance_of: Mountain
countries: Kenya
coordinates: lat: -0.1
lon: 37.2
Crystal Lake (Pontiac, Michigan). Crystal Lake is a private lake along the main branch of the Clinton River in Pontiac in Oakland County, Michigan. Upstream from Crystal Lake lies Sylvan Lake. Downstream, the Clinton River goes underground in Pontiac near Orchard Lake Road and Bagley Avenue. The river reappears, after being piped under Pontiac for, near Union Street and E.

Geographic entities mentioned:
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64416
lon: -98.56947
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.621645
lon: -83.303091
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2745524
lon: -75.7991552
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.1603
lon: -81.6415
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.3272
lon: -71.2003
surface_form: michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4433
lon: -71.3114
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 41.163055555556
lon: -81.465277777778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.02622
lon: -81.90986
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.661644
lon: -86.172576
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.829166666667
lon: -76.126944444444
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 27.952
lon: -81.6823
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 47.62777778
lon: -96.10277778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6006
lon: -72.0889
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.33361111
lon: -93.2125
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.615
lon: -95.950555555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.002
lon: -89.613
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.650347
lon: -75.201606
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7998926
lon: -109.5141115
The river reappears, after being piped under Pontiac for, near Union Street and E. Huron Street (M-59), where it winds its way eastward to Auburn Hills and beyond. Ironically, Crystal Lake was originally named Mud Lake. Golf. There is a public golf course on Crystal Lake. Fish. Fish on Crystal Lake include Yellow Perch, Smallmouth Bass and White Perch.

Geographic entities mentioned:
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.9511
lon: -71.4083
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.051666666667
lon: -75.360833333333
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 26.049722222222
lon: -80.193055555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7227
lon: -93.2667
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.64416
lon: -98.56947
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.621645
lon: -83.303091
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.2745524
lon: -75.7991552
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.1603
lon: -81.6415
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.3272
lon: -71.2003
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4433
lon: -71.3114
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 41.163055555556
lon: -81.465277777778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 28.02622
lon: -81.90986
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.661644
lon: -86.172576
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.829166666667
lon: -76.126944444444
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 27.952
lon: -81.6823
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 47.62777778
lon: -96.10277778
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6006
lon: -72.0889
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 44.33361111
lon: -93.2125
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.615
lon: -95.950555555556
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.002
lon: -89.613
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 42.650347
lon: -75.201606
surface_form: crystal lake
instance_of: Lake
countries: United States
coordinates: lat: 46.7998926
lon: -109.5141115
Crystal Lake (Pontiac, Michigan). Crystal Lake is a private lake along the main branch of the Clinton River in Pontiac in Oakland County, Michigan. Upstream from Crystal Lake lies Sylvan Lake. Downstream, the Clinton River goes underground in Pontiac near Orchard Lake Road and Bagley Avenue. The river reappears, after being piped under Pontiac for, near Union Street and E.

Geographic entities mentioned:
surface_form: orchard lake
instance_of: Lake
countries: United States
coordinates: lat: 44.70083333
lon: -93.30944444
surface_form: orchard lake
instance_of: Lake
countries: United States
coordinates: lat: 42.588333333333
lon: -83.366944444444
Grand Canal of Versailles. The Grand Canal of Versailles is the largest basin in the park of the Palace of Versailles. Cross-shaped, it was built between 1667 and 1679, at the instigation of André Le Nôtre. Prior to this date, the park was closed by a gate and ended behind the Bassin des Cygnes. Presentation.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
Nonetheless, this monumental water feature was successfully completed, cutting through the Ru de Gally river, which was used to feed the canal. Today, the layout of the Grand Canal takes the form of a cross, the main east-west perspective of which is located in the axis of the château and measures.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
When the work was completed in 1679, the Grand Canal served as the starting point for fireworks during the sumptuous royal festivities that Louis XIV organized at Versailles. It is a common perception that every year, on 5 September, the anniversary of Louis XIV's birth (in 1638), the sun sets in line with the Grand Canal; other sources mention 25 August, Saint Louis Day.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
The history of the construction of the park at Versailles suggests that the orientation of the canal was simply determined by the topography of the site. In winter, when frost prohibited all navigation, the Grand Canal was transformed into a skating rink for skaters and sleighs.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
In winter, when frost prohibited all navigation, the Grand Canal was transformed into a skating rink for skaters and sleighs. Over and above the decorative and playful requirements of this aspect of the garden, the Grand Canal also played a practical role. Located at a low point in the park, it received water from the fountains in the upstream gardens.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
This hydraulic system operated in a closed circuit. During the French Revolution, the canal was filled in and used as a wheat field. Louis XVIII restored it to its original purpose. In 2016, Danish artist Olafur Eliasson installed &quot;Waterfall&quot; at the eastern end of the Grand Canal. Fleet.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
They were housed in purpose-built buildings known as &quot;Little Venice&quot; at the eastern end of the Grand Canal, in the immediate vicinity of the &quot;Bassin d'Apollon&quot; (Apollo's basin). In 1685, 260 men from Flanders were assigned to three companies for the frigates.

Geographic entities mentioned:
surface_form: grand canal
instance_of: Lake
countries: France
coordinates: lat: 48.81
lon: 2.10011
Ernest Peak. Ernest Peak - Lyell 3, L3 or Mt. Lyell (on maps, etc.) - is the central and highest peak of five distinct subpeaks on Mount Lyell (Canada) and is located on the border of Alberta and British Columbia.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: ernest peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9567
lon: -117.103
surface_form: mount lyell (canada)
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
Ernest Peak. Ernest Peak - Lyell 3, L3 or Mt. Lyell (on maps, etc.) - is the central and highest peak of five distinct subpeaks on Mount Lyell (Canada) and is located on the border of Alberta and British Columbia.

Geographic entities mentioned:
surface_form: ernest peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9567
lon: -117.103
Lyell (on maps, etc.) - is the central and highest peak of five distinct subpeaks on Mount Lyell (Canada) and is located on the border of Alberta and British Columbia. (There has been some dispute whether Lyell 2 or Lyell 3 is highest, but according to the recently released and corrected Climbers Guide to The Canadian Rocky Mountains - Rockies West book, the tallest is Ernest Peak).

Geographic entities mentioned:
surface_form: ernest peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9567
lon: -117.103
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
It was named in 1972 by Sydney R. Vallance after Ernest Feuz Jr. __NOTOC__
Geology and climate. Due to this peak being the central and tallest subpeak - and thus &quot;is&quot; &quot;Mount Lyell&quot; - see the Mount Lyell article for geology and climate.

Geographic entities mentioned:
surface_form: mount lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: mount lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
surface_form: lyell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.956667
lon: -117.103333
Half way up the road is the Throne Centre, a mixed-use business premises that has had a number of uses over the years. Taking its name from the Giant's Chair, a large stone on nearby Cavehill used as the throne of the O'Neill Clan, it was initially a private residence before becoming a hospital and convalescent home.

Geographic entities mentioned:
surface_form: Cavehill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.647
lon: -5.951
state of Alaska. The peak is situated east of Anchorage, northeast of Whittier, and northeast of Mount Muir, on land managed by Chugach National Forest. Although modest in elevation, relief is significant since the mountain rises up from tidewater at Harriman Fiord in Prince William Sound in less than six miles. History. The peak was named in 1908 by Ulysses Sherman Grant and Daniel F.

Geographic entities mentioned:
surface_form: mount muir
instance_of: Mountain
countries: United States
coordinates: lat: 36.564722222222
lon: -118.29111111111
surface_form: mount muir
instance_of: Mountain
countries: United States
coordinates: lat: 61.1081
lon: -148.3817
Mount Gilbert (Chugach Mountains). Mount Gilbert is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. The peak is situated east of Anchorage, northeast of Whittier, and northeast of Mount Muir, on land managed by Chugach National Forest.

Geographic entities mentioned:
surface_form: mount gilbert (chugach mountains)
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
Mount Gilbert (Chugach Mountains). Mount Gilbert is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. The peak is situated east of Anchorage, northeast of Whittier, and northeast of Mount Muir, on land managed by Chugach National Forest.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
The first ascent of the peak was made May 29, 1962, by Paul B. Crews, Hans Metz, Helga Bading, and Bob Bailey, in what was described as poor weather conditions. Climate. Based on the Köppen climate classification, Mount Gilbert is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
History. The peak was named in 1908 by Ulysses Sherman Grant and Daniel F. Higgins for Grove Karl Gilbert (1843-1918), a geologist with the United States Geological Survey who was part of the 1899 Harriman Alaska expedition that explored this area. The mountain's name was officially adopted in 1910 by the U.S. Board on Geographic Names.

Geographic entities mentioned:
surface_form: daniel
instance_of: Mountain
countries: United States
coordinates: lat: 47.5652
lon: -121.1798
It is also in the barony of Middle Third, and part of the parish of New Inn and Knockgraffon in the Roman Catholic Archdiocese of Cashel and Emly. Location and access. It is located in the Golden Vale midway between the market and tourist towns of Cahir and Cashel. Bypassed in October 2007 by the M8, the main road through the village is a section of the R639.

Geographic entities mentioned:
surface_form: Golden Vale
instance_of: Valley
countries: Ireland
coordinates: lat: 52.4
lon: -8.4
The third bridge collapsed in 1856 due to heavy use and fatigue from weathering. None of these earlier bridges were either arched or covered. All three bridges were a part of the James River and Kanawha Turnpike, a heavily used mountain road that connected the Shenandoah Valley with the Alleghany Mountains and areas further west.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Dongping Lake. The Dongping Lake () is a freshwater lake in Shandong Province of China. It is situated in Dongping County in the west of Shandong Province, south of the lower reaches of Yellow River. The lake has a total area of about 148 square kilometers. The average depth is 1.59 m, the water storage capacity is about 2.35×108m3.

Geographic entities mentioned:
surface_form: dongping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 35.96472222
lon: 116.19583333
The average depth is 1.59 m, the water storage capacity is about 2.35×108m3. The Dongping Lake is the second largest fresh-water lake in Shandong Province; it is the only extant water area of the Eight Hundred Li Liangshan Lake () described in the famous medieval novel, &quot;Water Margin&quot;, one of the Four Great Classical Novels of Chinese literature.

Geographic entities mentioned:
surface_form: dongping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 35.96472222
lon: 116.19583333
surface_form: dongping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 35.96472222
lon: 116.19583333
(The Yangtze River to Yellow River route, mostly piggybacking on, or paralleling, the Grand Canal of China.)
As the water transfer system entered its testing stage in the summer of 2013, the area's fish farmers started complaining that the polluted Yangtze River water entering the Dongping Lake is killing their fish.

Geographic entities mentioned:
surface_form: dongping lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 35.96472222
lon: 116.19583333
Kingston Peak (California). Kingston Peak is the only named peak in the Kingston Range, a small desert mountain range in San Bernardino County, California, in the Mojave Desert. The highest point in the Kingston Range's 17-mile U-shaped continuous ridgeline, the peak has an elevation of and a topographic prominence of.

Geographic entities mentioned:
surface_form: kingston peak (california)
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
Kingston Peak (California). Kingston Peak is the only named peak in the Kingston Range, a small desert mountain range in San Bernardino County, California, in the Mojave Desert. The highest point in the Kingston Range's 17-mile U-shaped continuous ridgeline, the peak has an elevation of and a topographic prominence of.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
The highest point in the Kingston Range's 17-mile U-shaped continuous ridgeline, the peak has an elevation of and a topographic prominence of. Kingston Peak's prominence makes it among the top 200 mountains by prominence in the contiguous United States, and the 23rd most prominent peak in California.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
Kingston Peak's prominence makes it among the top 200 mountains by prominence in the contiguous United States, and the 23rd most prominent peak in California. Kingston Peak and the Kingston Range lie within the Kingston Range Wilderness, administered by the Bureau of Land Management (BLM) and one of California's most botanically diverse desert regions.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
Kingston Peak and the Kingston Range lie within the Kingston Range Wilderness, administered by the Bureau of Land Management (BLM) and one of California's most botanically diverse desert regions. One of only three white fir stands in the California deserts is found on the slopes of two drainages just below the summit of Kingston Peak.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
One of only three white fir stands in the California deserts is found on the slopes of two drainages just below the summit of Kingston Peak. Kingston Peak and Range also form part of the Basin and Range Province, along with neighboring mountains and ranges, such as the Mesquite Mountains to the east, and the Nopah Range to the northwest. Naming.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
Kingston Peak and Range also form part of the Basin and Range Province, along with neighboring mountains and ranges, such as the Mesquite Mountains to the east, and the Nopah Range to the northwest. Naming. The origin of the name Kingston as applied to Kingston Peak and Range is unknown. It dates back at least to the early 1860s and possibly earlier.

Geographic entities mentioned:
surface_form: kingston peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.7269
lon: -115.9161
He captured both Spoleto and Camerino. In 962, when Adalbert returned from exile in Corsica to try to reclaim his throne. Guy and Conrad joined with him in besieging Pavia, the Italian capital. The brothers then retreated into the fortresses around Lakes Como and Garda. His lands were confiscated by the Emperor Otto I and given to Guy, Bishop of Modena. Death.

Geographic entities mentioned:
surface_form: Garda
instance_of: Lake
countries: Italy
coordinates: lat: 45.633333333333
lon: 10.666666666667
Beinn Talaidh. Beinn Talaidh (762 m) is a peak on the Isle of Mull, Scotland, located in the mountainous centre of the Island. The mountain is shaped like a symmetrical cone and can be climbed from the steep facing south side, or more gentle northern side along Glen Forsa.

Geographic entities mentioned:
surface_form: beinn talaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.44522
lon: -5.85591
The mountain is shaped like a symmetrical cone and can be climbed from the steep facing south side, or more gentle northern side along Glen Forsa. Beinn Talaidh was for many years classed as a Corbett before a resurvey found it to be slightly lower than expected, and it was thus demoted to Graham status; however it is the highest of the 219 Grahams in Scotland.

Geographic entities mentioned:
surface_form: beinn talaidh
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.44522
lon: -5.85591
Based on the 1950 novel &quot;Bend of the Snake&quot; by Bill Gulick, the film is about a tough cowboy who risks his life to deliver confiscated supplies to homesteaders after gold is discovered in the region. &quot;Bend of the River&quot; was filmed on location in and around the Sandy River, Mount Hood, the Columbia River, and Timberline, Oregon.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Adams is best known for her role as Kay Lawrence in the 1954 horror film &quot;Creature from the Black Lagoon&quot; and Nelson played the female lead role in the 1955 sequel &quot;Revenge of the Creature&quot;, which were both directed by Jack Arnold. Rock Hudson played Trey Wilson, a professional gambler. The film was filmed in Mount Hood, Sandy River and Timberline, Oregon.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
After he was defeated in battle, he sought refuge first in the Ramadanids, and from there passed into Mamluk domains. Although the Mamluks declined to offer him any military support, this act aroused the hostility of Bayezid, which was further fanned when the Mamluks seized an Ottoman ambassador who was returning from Deccan with an Indian ambassador and gifts for the Ottoman Sultan. Operations.

Geographic entities mentioned:
surface_form: Deccan
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
The Fly River Basin, the most species rich river of the island, has 105 fish species, while the Sepik River Basin has 57 species. Among New Guinea's lake systems, the most important in terms of endemic fishes are Kutubu (13 endemics), Ajamaru (4 endemics), and Sentani (4 endemics). The gudgeons &quot;Oxyeleotris caeca&quot; from the upper Kikori River system in Papua New Guinea and &quot;O.

Geographic entities mentioned:
surface_form: Kutubu
instance_of: Lake
countries: Papua New Guinea
coordinates: lat: -6.4
lon: 143.33333333333
surface_form: Ajamaru
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -1.26666667
lon: 132.2
surface_form: Sentani
instance_of: Lake
countries: Indonesia
coordinates: lat: -2.6122
lon: 140.5172
There are more than 20 species of Parastacid crayfish of the genus &quot;Cherax&quot; in New Guinea. With eight endemics, by far the greatest diversity is found in the Paniai Lakes. Insects. The New Guinea insect fauna demonstrates many principles of vicariance biogeography and New Guinea has played a strategic role in the spread of insects in various directions.

Geographic entities mentioned:
surface_form: Paniai Lakes
instance_of: Group of lakes
countries: Indonesia
coordinates: lat: -3.9022222222222
lon: 136.31777777778
Tullpacocha or Tulpacocha (possibly from Quechua &quot;tullpa&quot; rustic cooking-fire, stove, &quot;qucha&quot; lake,) is a lake in Peru located in the Ancash Region, Huaraz Province, Independencia District. Tullpacocha lies in the Cordillera Blanca, southeast of Palcaraju and Pucaranra, southwest of Chinchey and Tullparaju and northwest of Andavite, at the very end of the Quilcayhuanca gorge.

Geographic entities mentioned:
surface_form: Palcaraju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.3683333333333
lon: -77.370833333333
surface_form: Pucaranra
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39166667
lon: -77.35083333
surface_form: Chinchey
instance_of: Mountain
countries: Peru
coordinates: lat: -9.3824388888889
lon: -77.33
surface_form: Tullparaju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.4
lon: -77.3167
surface_form: Andavite
instance_of: Mountain
countries: Peru
coordinates: lat: -9.43083
lon: -77.3258
surface_form: Quilcayhuanca
instance_of: Valley
countries: Peru
surface_form: tullparaju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.0286111111111
lon: -77.665555555556
surface_form: tullparaju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.4
lon: -77.3167
surface_form: andavite
instance_of: Mountain
countries: Peru
coordinates: lat: -9.43083
lon: -77.3258
surface_form: pucaranra
instance_of: Mountain
countries: Peru
coordinates: lat: -14.694166666667
lon: -72.913055555556
surface_form: palcaraju
instance_of: Mountain
countries: Peru
coordinates: lat: -9.3683333333333
lon: -77.370833333333
surface_form: pucaranra
instance_of: Mountain
countries: Peru
coordinates: lat: -9.39166667
lon: -77.35083333
surface_form: chinchey
instance_of: Mountain
countries: Peru
coordinates: lat: -9.3824388888889
lon: -77.33
surface_form: quilcayhuanca
instance_of: Valley
countries: Peru
Tullpacocha. Tullpacocha or Tulpacocha (possibly from Quechua &quot;tullpa&quot; rustic cooking-fire, stove, &quot;qucha&quot; lake,) is a lake in Peru located in the Ancash Region, Huaraz Province, Independencia District.

Geographic entities mentioned:
surface_form: tullpacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.42083
lon: -77.3433
Tullpacocha. Tullpacocha or Tulpacocha (possibly from Quechua &quot;tullpa&quot; rustic cooking-fire, stove, &quot;qucha&quot; lake,) is a lake in Peru located in the Ancash Region, Huaraz Province, Independencia District.

Geographic entities mentioned:
surface_form: tullpacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.42083
lon: -77.3433
surface_form: tullpacocha
instance_of: Lake
countries: Peru
coordinates: lat: -9.42083
lon: -77.3433
The march from Fort Loudoun to Erie took twenty-eight days. Major William McClelland's division relieved American forces at Lake Erie and later gave a good account of themselves at the Battle of Chippewa and Battle of Lundy's Lane. Underground Railroad.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In western Pennsylvania, routes began at the Maryland–Pennsylvania border and traveled through Bedford, Pennsylvania, where the route split and converged at the Great Shamokin Path at the mouth of Anderson Creek. From there, the route led to The Big Spring near Luthersburg, Pennsylvania, and thence on Meade's Path to the Venango Path, Lake Erie and onward to Canada.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Harrison Stickle. Harrison Stickle is a fell in the central part of the English Lake District, situated above Great Langdale. The fell is one of the three (although the number is debated) fells which make up the picturesque Langdale Pikes, the others being Pike of Stickle and Loft Crag. Together they make up one of the most picturesque, and probably the best-known, mountain groups in the District.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
Harrison Stickle. Harrison Stickle is a fell in the central part of the English Lake District, situated above Great Langdale. The fell is one of the three (although the number is debated) fells which make up the picturesque Langdale Pikes, the others being Pike of Stickle and Loft Crag. Together they make up one of the most picturesque, and probably the best-known, mountain groups in the District.

Geographic entities mentioned:
surface_form: Pike of Stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
surface_form: Loft Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
A &quot;stickle&quot; is a hill with a prominent rocky top. Topography. The Langdale Pikes form a raised rocky parapet around the southern and eastern edges of a high tableland centred upon Thunacar Knott. Harrison Stickle is the high point of this system and its crags fall south and east from the summit, presenting an arresting view from the valley floor below, or from further afield.

Geographic entities mentioned:
surface_form: Thunacar Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: thunacar knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
To the north, the main ridge of the central fells passes over Thunacar Knott before climbing to High Raise. The craggy eastern face of this ridge continues north as far as Harrison's near neighbour, Pavey Ark, visually the most impressive face in the area.

Geographic entities mentioned:
surface_form: Pavey Ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451
surface_form: pavey ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451
Across the Ghyll westwards are Thorn Crag, Loft Crag and finally Pike of Stickle. Below the steep eastern face of Harrison Stickle lie Stickle Tarn and its ghyll, thus ensuring that all drainage from the fell is to Great Langdale. The tarn is a waterfilled corrie about deep, this being enhanced by a dam. The water is used for public consumption in Great Langdale. Geology and archaeology.

Geographic entities mentioned:
surface_form: Stickle Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4586
lon: -3.1025
surface_form: stickle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4586
lon: -3.1025
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
Harrison Stickle is the high point of this system and its crags fall south and east from the summit, presenting an arresting view from the valley floor below, or from further afield. To the north, the main ridge of the central fells passes over Thunacar Knott before climbing to High Raise.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: high raise
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.513
lon: -2.851
surface_form: high raise
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.476
lon: -3.113
surface_form: thunacar knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
The south-western border of Harrison Stickle is formed by the deep ravine of Dungeon Ghyll, which cuts through the parapet of the Langdale Pikes and into the lower hinterland of Harrison Combe. Across the Ghyll westwards are Thorn Crag, Loft Crag and finally Pike of Stickle.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: pike of stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
Ascents. The fell is usually climbed from New Dungeon Ghyll Hotel in Great Langdale, and there are a number of possible routes up. The simplest first follows Stickle Beck to Stickle Tarn; a path then leads up the western side of Pavey Ark to reach the summit. The fell is almost invariably combined with other nearby peaks to make a longer circular walk.

Geographic entities mentioned:
surface_form: stickle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4586
lon: -3.1025
surface_form: pavey ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451
Across the Ghyll westwards are Thorn Crag, Loft Crag and finally Pike of Stickle. Below the steep eastern face of Harrison Stickle lie Stickle Tarn and its ghyll, thus ensuring that all drainage from the fell is to Great Langdale. The tarn is a waterfilled corrie about deep, this being enhanced by a dam. The water is used for public consumption in Great Langdale. Geology and archaeology.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
The view from Harrison Stickle is as good as the view of it — a surprisingly rare occurrence — with all of the major fell groups visible. Ascents. The fell is usually climbed from New Dungeon Ghyll Hotel in Great Langdale, and there are a number of possible routes up. The simplest first follows Stickle Beck to Stickle Tarn; a path then leads up the western side of Pavey Ark to reach the summit.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Harrison Stickle. Harrison Stickle is a fell in the central part of the English Lake District, situated above Great Langdale. The fell is one of the three (although the number is debated) fells which make up the picturesque Langdale Pikes, the others being Pike of Stickle and Loft Crag. Together they make up one of the most picturesque, and probably the best-known, mountain groups in the District.

Geographic entities mentioned:
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
The craggy eastern face of this ridge continues north as far as Harrison's near neighbour, Pavey Ark, visually the most impressive face in the area. The south-western border of Harrison Stickle is formed by the deep ravine of Dungeon Ghyll, which cuts through the parapet of the Langdale Pikes and into the lower hinterland of Harrison Combe.

Geographic entities mentioned:
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
Summit. The summit is a short rocky ridge with a cairn at each end, the northern one being higher. The view from Harrison Stickle is as good as the view of it — a surprisingly rare occurrence — with all of the major fell groups visible. Ascents. The fell is usually climbed from New Dungeon Ghyll Hotel in Great Langdale, and there are a number of possible routes up.

Geographic entities mentioned:
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
The water is used for public consumption in Great Langdale. Geology and archaeology. Harrison Stickle's summit area is composed of the pebbly sandstone and breccia of the Pavey Ark Member. Several greenstone knapping sites have been found below the main peak, and following the strike of the tuff exploited at nearby Pike O'Stickle in the Neolithic period.

Geographic entities mentioned:
surface_form: pavey ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451