Sarmila/GeoWiki-Features huggingface dataset:
Oppkuven Peak. Oppkuven Peak () is a peak 2 nautical miles (3.7 km) north of Gavlen Ridge in the Roots Heights, Sverdrup Mountains, in Queen Maud Land. Photographed from the air by the German Antarctic Expedition (1938–39).

Geographic entities mentioned:
surface_form: oppkuven peak
instance_of: Mountain
coordinates: lat: -72.61666667
lon: 0.4
Photographed from the air by the German Antarctic Expedition (1938–39). Mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and air photos by the Norwegian expedition (1958–59) and named Oppkuven (the ascent peak).

Geographic entities mentioned:
surface_form: oppkuven
instance_of: Mountain
coordinates: lat: -72.61666667
lon: 0.4
Ziegler and aircraft #2 (46-675) were subsequently lost on 12 May 1953, in an inflight explosion during a captive flight intended to check the aircraft's liquid oxygen system. A B-50 crew member, Frank Wolko, was also killed during the incident. The wreckage of the aircraft fell into Lake Ontario and was not recovered. Lt. Col. Frank K.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
North Watervliet Road–Paw Paw Lake Outlet Bridge. The North Watervliet Road–Paw Paw Lake Outlet Bridge, also known as Trunk Line Bridge No. 57, was an arch bridge in Watervliet Township, Michigan, that carried North Watervliet Road over the outlet of Paw Paw Lake into the Paw Paw River. It is listed on the National Register of Historic Places. The bridge was demolished and replaced about 2008.

Geographic entities mentioned:
surface_form: Paw Paw Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2078
lon: -86.26961
__NOTOC__
Geology. Like other mountains in Banff Park, Mount Sarbach is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. A glacier shared with Kaufmann Peaks resides in the southeast cirque. Climate.

Geographic entities mentioned:
surface_form: Kaufmann Peaks
instance_of: Mountain
countries: Canada
coordinates: lat: 51.88333333333333
lon: -116.75
Mount Sarbach. Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
Mount Sarbach. Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
Norman Collie and G.P. Baker in 1897. Mount Sarbach is situated south of Saskatchewan River Crossing, where the Icefields Parkway intersects with the David Thompson Highway. __NOTOC__
Geology. Like other mountains in Banff Park, Mount Sarbach is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
__NOTOC__
Geology. Like other mountains in Banff Park, Mount Sarbach is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. A glacier shared with Kaufmann Peaks resides in the southeast cirque. Climate.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
A glacier shared with Kaufmann Peaks resides in the southeast cirque. Climate. Based on the Köppen climate classification, Mount Sarbach is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
Climate. Based on the Köppen climate classification, Mount Sarbach is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Sarbach drains into the Mistaya River and Howse River which are both tributaries of the North Saskatchewan River.

Geographic entities mentioned:
surface_form: mount sarbach
instance_of: Mountain
countries: Canada
coordinates: lat: 51.8927778
lon: -116.7680556
surface_form: mistaya
instance_of: Valley
countries: Canada
coordinates: lat: 51.9503
lon: -116.717
Mount Sarbach. Mount Sarbach is a mountain located in Banff National Park between Mistaya River and Howse River and is visible from the Icefields Parkway. The mountain is named after Peter Sarbach, a mountain guide from Switzerland, who guided the first ascent by J. Norman Collie and G.P. Baker in 1897.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
&quot;Cherry, Harry and Raquel&quot; is possibly the only narrative film ever made without a narrative.&quot;
Meyer denied that the lab lost footage but admitted to shooting new sequences. He recalled &quot;one of the leading ladies couldn't stand the rigors of Panamint Valley [the location of the film].

Geographic entities mentioned:
surface_form: Panamint Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.0592
lon: -117.244
He cites the reference in the annals to the death of Áed in 575 who is said to be killed by the Uí Briúin and to a reference in the &quot;Annals of Innisfallen&quot; that he gave Enach Dúin (Annaghdown on Lough Corrib) to Saint Brendan of Clonfert. He doubts that a ruler from the Mag nAí region would be able to make this gift.

Geographic entities mentioned:
surface_form: Lough Corrib
instance_of: Lake
countries: Ireland
coordinates: lat: 53.466666666667
lon: -9.2833333333333
In 1867, it was the fourth race track to be established in Germany, but today it only hosts a few race days every year. The Fockeberg, which is also part of the Südvorstadt locality, was created from the city's war rubble but is now covered in forest, offers a view of the entire city and is a popular place to relax. Sports (Fockeberg run) and other competitions are held on its grounds.

Geographic entities mentioned:
surface_form: Fockeberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.3175
lon: 12.362222222222
Early recognition that British Columbia's farmland would be engulfed by sprawl led to the establishment of the Agricultural Land Reserve in the 1970s. This assisted in containing and intensifying development throughout the Vancouver metropolitan area and the Fraser Valley.

Geographic entities mentioned:
surface_form: Fraser Valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.108333333333
lon: -122.29166666667
Chicago Lake Tunnel. The Chicago Lake Tunnel was the first of several tunnels built from the city of Chicago's shore on Lake Michigan two miles out into the lake to access unpolluted fresh water far from the city's sewage. Waterborne disease in early Chicago.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Chesbrough (1813–1886), the first city engineer of Boston to study the problem. In 1863, Chesbrough completed a design for a water and sewer system for the city that included a tunnel five feet wide and lined with brick that would extend through the clay bed of Lake Michigan to a distance of 10,567 feet. Work started in 1864 and the tunnel was opened in 1867. Construction.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
It is the 10th-highest summit in Custer County, and the 206th-highest in Colorado. Broken Hand Peak, 0.75 mile (1.2 km) southeast of Crestone Needle, is included within the official name &quot;Crestone Peaks&quot;. The mountain is located in the Sangre de Cristo Wilderness on land managed by San Isabel National Forest and Rio Grande National Forest.

Geographic entities mentioned:
surface_form: Crestone Needle
instance_of: Mountain
countries: United States
coordinates: lat: 37.964722222222
lon: -105.57666666667
Boxing Island. Boxing Island () is a small island lying in Charlotte Bay east of Harris Peak, off the west coast of Graham Land. It was first charted by the Belgian Antarctic Expedition under Gerlache, 1897–99, and so named by members of the Falkland Islands Dependencies Survey because they first saw it on Boxing Day 1956.

Geographic entities mentioned:
surface_form: Harris Peak
instance_of: Mountain
coordinates: lat: -64.6
lon: -61.7833
After the discovery (more precisely, the beginning of the archeological excavations of the Minusinsk &quot;Sve&quot;), the researchers drew attention to the fact that there are similar fortress structures in other mountainous regions of the north of Central Asia - in the Baikal region, in the Altai Mountains, in Tuva.

Geographic entities mentioned:
surface_form: Minusinsk
instance_of: Valley
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54
lon: 91.5
surface_form: Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
The Iyus Cherny and Iyus Bely valleys part of Khakassia adjoins the forest-steppe &quot;corridor&quot;, which for a long time was the only accessible passage to the Minusinsk basin, closed on all sides by impassable Kuznetsk Alatau mountains, Sayn mountains and Altai mountains.

Geographic entities mentioned:
surface_form: Minusinsk basin
instance_of: Valley
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54
lon: 91.5
The most expressive category of finds is the mass ceramic material of the Okunev culture. This is mainly found in the lower layers of the excavation, The Okunev ceramics from Chebaki &quot;Sve&quot;, in terms of character and ornamentation, finds analogies in the Okunev burial sites of the Minusinsk Basin.

Geographic entities mentioned:
surface_form: Minusinsk Basin
instance_of: Valley
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 54
lon: 91.5
Products from plantations in the province also include pineapples, bananas and sugarcane. Situated within Bukidnon is Mount Dulang-dulang, the 2nd highest mountain in the country, with an elevation of located in the Kitanglad Mountain Range.

Geographic entities mentioned:
surface_form: Mount Dulang-dulang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1152777777778
lon: 124.92083333333
Mount Kitanglad (2,899 m), Mount Kalatungan (2,860 m), Mount Maagnaw (2,742 m), Mount Lumuluyaw (2,612 m), and Mount Tuminungan (2,400 m), the 4th, 5th, 8th, 17th, and 30th highest mountains in the country respectively, are also found in the province.

Geographic entities mentioned:
surface_form: Mount Kitanglad
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1427777777778
lon: 124.9125
It lies between parallels 7°25' and 8°38' north latitude and meridians 124°03' and 125°16' east longitude. Malaybalay, the capital town, is about by air from Manila and by road from Cagayan de Oro. It has two important landmarks, Mount Kitanglad and Pulangi River. Mount Kitanglad has a peak of above sea level.

Geographic entities mentioned:
surface_form: Mount Kitanglad
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.1427777777778
lon: 124.9125
Lakes. Aside from the relatively important river systems, various lakes also dot the landscape of the province. Pinamaloy Lake, in Don Carlos, Bukidnon, is the largest in the province covering about 50 hectares. It was named after Barangay Pinamaloy, where the lake is located. Another lake is found in Pigtauranan, Pangantucan called the Napalit Lake.

Geographic entities mentioned:
surface_form: Pinamaloy Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 7.6736944444444
lon: 124.99608333333
Pinamaloy Lake, in Don Carlos, Bukidnon, is the largest in the province covering about 50 hectares. It was named after Barangay Pinamaloy, where the lake is located. Another lake is found in Pigtauranan, Pangantucan called the Napalit Lake. The lake covers an area of 36 hectares and is one of the tourist spots in Pangantucan, Bukidnon. There are 24 floating islets in the lake.

Geographic entities mentioned:
surface_form: Napalit Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8683333333333
lon: 124.78527777778
Another lake is found in Pigtauranan, Pangantucan called the Napalit Lake. The lake covers an area of 36 hectares and is one of the tourist spots in Pangantucan, Bukidnon. There are 24 floating islets in the lake. The third significant inland body of water in the province is Apo Lake at Guinoyoran, Valencia. It occupies an approximate area of 25 hectares.

Geographic entities mentioned:
surface_form: Apo Lake
instance_of: Lake
countries: Philippines
coordinates: lat: 7.8802777777778
lon: 125.00611111111
&quot;Rafflesia schadenbergiana&quot; has also been found on Mount Kitanglad. Mount Musuan and Mount Kalatungan, along with Mount Malindang in Misamis Occisdental, are also home to the Philippine eagle, the Mindanao wrinkled hornbill (&quot;Aceros leococephalus&quot;), and the Philippine tarsier (&quot;Tarsius syrichta&quot;).

Geographic entities mentioned:
surface_form: Mount Malindang
instance_of: Mountain
countries: Philippines
coordinates: lat: 8.2175
lon: 123.63666666667
Lepp Hollow. Lepp Hollow is a valley in Warren County in the U.S. state of Missouri. Lepp Hollow has the name of the Lepp family, original owners of the site.

Geographic entities mentioned:
surface_form: lepp hollow
instance_of: Valley
countries: United States
coordinates: lat: 38.796434
lon: -91.312935
Tessa Lynch is currently working with Collective Gallery, Edinburgh and landscape architects Harrison Stevens on elements of the redesign of the Collective landscape on Edinburgh's historic Calton Hill.

Geographic entities mentioned:
surface_form: Calton Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 55.955278
lon: -3.182222
The third peak southeast of Banff is the highest at. West of the Spray Lakes road is the East End of Rundle— locally known as EEOR—which rises above Whiteman's Gap just south of Canmore. The Rundle Peaks are part of the South Banff Ranges, along with its siblings—the Sundance Range, Sulphur Mountain and the Goat Range. Geology.

Geographic entities mentioned:
surface_form: East End of Rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.080555555555556
lon: -115.42111111111112
surface_form: east end of rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.080555555555556
lon: -115.42111111111112
It is fine-grained sandstone dating back to the Triassic Period. Scrambles. At the East End of Rundle near Canmore there is a well-known scramble, the Goat Creek hiking trail, with its starting point at parking trailhead, which starts at the Smith-Dorrien/Spray Trail just south of the Canmore Reservoir above Grassi Lakes.

Geographic entities mentioned:
surface_form: East End of Rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.080555555555556
lon: -115.42111111111112
surface_form: Grassi Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.0722221
lon: -115.4069443
surface_form: grassi lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.0722221
lon: -115.4069443
The viewpoint from which most photographs are taken, from Mount Rundle, at the end of Vermilion Lakes road, with Vermillion Lakes in the foreground. Mount Rundle and Sulphur Mountain can be seen from Mount Norquay on the north side of the Trans-Canada Highway. The Banff Springs Hotel patio and restaurants look out over Mount Rundle and Tunnel Mountain. In popular culture.

Geographic entities mentioned:
surface_form: Tunnel Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.17638888888889
lon: -115.55472222222222
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
The thrust faulting occurred during the Columbian Orogeny between late Jurassic and early Cretaceous time. At that time a collision of tectonic plates caused huge sheets of sedimentary rock in what is now British Columbia to become detached and slide eastward to northeastward over their neighbors, piling up to form the southern Canadian Rockies.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The Paleozoic &quot;sandwich&quot; is part of the Rundle thrust sheet that was moved up from the west along the Rundle thrust fault and emplaced on top of the younger rocks (the Early Cretaceous Mist Mountain Formation) that underlie Canmore and the forested slopes along the Bow River. The thrust faulting occurred during the Columbian Orogeny between late Jurassic and early Cretaceous time.

Geographic entities mentioned:
surface_form: mist mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.55416666666667
lon: -114.91
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In deep shadow in the morning, it borrows a warm glow from the setting sun at the end of the day. Its colour runs the gamut from orange to cold blue-grey, with overtones of violet and intervals of green.&quot;
From Vermilion Lakes. The viewpoint from which most photographs are taken, from Mount Rundle, at the end of Vermilion Lakes road, with Vermillion Lakes in the foreground.

Geographic entities mentioned:
surface_form: vermilion lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.178055555556
lon: -115.59888888889
surface_form: vermilion lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 51.178055555556
lon: -115.59888888889
Mount Rundle. Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was &quot;Waskahigan Watchi&quot; or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Mount Rundle. Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was &quot;Waskahigan Watchi&quot; or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The Cree name was &quot;Waskahigan Watchi&quot; or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s. He introduced syllabics there—a written language developed for the Cree, as part of his missionary work.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
He only visited the Stoney-Nakoda of the area around what is now called Mount Rundle in 1844 and 1847. Mt. Rundle could actually be considered a small mountain range as the mountain extends for over, on the south side of the Trans-Canada Highway eastward from Banff to Canmore with seven distinct peaks along the way. The third peak southeast of Banff is the highest at.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The third peak southeast of Banff is the highest at. West of the Spray Lakes road is the East End of Rundle— locally known as EEOR—which rises above Whiteman's Gap just south of Canmore. The Rundle Peaks are part of the South Banff Ranges, along with its siblings—the Sundance Range, Sulphur Mountain and the Goat Range. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: sulphur mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.123611111111
lon: -115.55555555556
Geology. Mount Rundle consists of limestones, dolomitic limestones, dolomites and shales of Paleozoic (Late Devonian to Mississippian) age. In ascending order, they belong to the Palliser, Exshaw and Banff Formations, topped by the Rundle Group, which was named after the mountain. Mount Rundle illustrates the classic limestone-shale-limestone &quot;sandwich&quot; of the front ranges.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
This left the Paleozoic strata on Mount Rundle dipping steeply to the southwest, so that the southwest-facing side of the mountain forms an extensive dip slope. Geologists consider Mount Rundle to be a classic example of a mountain cut in dipping layered rocks, with the tilted strata giving the mountain its shape.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
This left the Paleozoic strata on Mount Rundle dipping steeply to the southwest, so that the southwest-facing side of the mountain forms an extensive dip slope. Geologists consider Mount Rundle to be a classic example of a mountain cut in dipping layered rocks, with the tilted strata giving the mountain its shape.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Finally, after the glaciers retreated for the last time, a series of steep, tree-covered alluvial fans began to grow at the mouths of the deep gulches on the northeast-facing side of the mountain. Commerce. Rundle rock or Rundle stone, a natural stone, first quarried on Mount Rundle, is a common dimension stone used in southern Alberta for landscaping and building purposes.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Scenic viewpoints. In 2000 Dave Birrell described Mount Rundle as one of the most recognized Canadian mountains. Painter, print-maker and art teacher, Walter Phillips RCA (1884–1963) described Mount Rundle as his, &quot;bread and butter mountain. I never tire of painting it, for it is never the same. In deep shadow in the morning, it borrows a warm glow from the setting sun at the end of the day.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Its colour runs the gamut from orange to cold blue-grey, with overtones of violet and intervals of green.&quot;
From Vermilion Lakes. The viewpoint from which most photographs are taken, from Mount Rundle, at the end of Vermilion Lakes road, with Vermillion Lakes in the foreground. Mount Rundle and Sulphur Mountain can be seen from Mount Norquay on the north side of the Trans-Canada Highway.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
The viewpoint from which most photographs are taken, from Mount Rundle, at the end of Vermilion Lakes road, with Vermillion Lakes in the foreground. Mount Rundle and Sulphur Mountain can be seen from Mount Norquay on the north side of the Trans-Canada Highway. The Banff Springs Hotel patio and restaurants look out over Mount Rundle and Tunnel Mountain. In popular culture.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Mount Rundle. Mount Rundle is a mountain in Canada's Banff National Park overlooking the towns of Banff and Canmore, Alberta. The Cree name was &quot;Waskahigan Watchi&quot; or house mountain. In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
In 1858 John Palliser renamed the mountain after Reverend Robert Rundle, a Methodist invited by the Hudson's Bay Company to do missionary work in western Canada in the 1840s. He introduced syllabics there—a written language developed for the Cree, as part of his missionary work. He only visited the Stoney-Nakoda of the area around what is now called Mount Rundle in 1844 and 1847. Mt.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
The &quot;sandwich filling&quot; is the Banff Formation, a layer of softer, more easily eroded, dark brownish-gray to black calcareous shale with thin beds of argillaceous limestone. The top layer of the geologic sandwich is the grey limestones and dolomites of the Rundle Group that form the massive upper cliffs at the top of Mount Rundle.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Commerce. Rundle rock or Rundle stone, a natural stone, first quarried on Mount Rundle, is a common dimension stone used in southern Alberta for landscaping and building purposes. It has been used in the construction of the Banff Springs Hotel and several of the Parks Canada buildings. It is fine-grained sandstone dating back to the Triassic Period. Scrambles.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
This is also the beginning of the Mount Rundle Traverse, a demanding trek to mount all of Rundle's peaks from Goat Creek parking lot to the Banff Springs Hotel. Mount Rundle is one of the most popular scrambles in the area, and is relatively straightforward for experienced hikers.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Mount Rundle is one of the most popular scrambles in the area, and is relatively straightforward for experienced hikers. In Banff, the Spray River trailhead for the first peak taking the Mount Rundle Trail, is near the Spray River bridge on the road to the Banff Springs Golf Course.

Geographic entities mentioned:
surface_form: mount rundle
instance_of: Mountain
countries: Canada
coordinates: lat: 51.1242
lon: -115.47
Bauerntarock. Bauerntarock (&quot;farmers' tarot&quot;) also called Brixentaler Bauerntarock or Brixental Tarock, is a point-trick card game played in the Brixental, Austria. It may have originated in the 19th century either as an adaptation of 54-card Tapp Tarock onto the cheaper and smaller 36-card German pack.

Geographic entities mentioned:
surface_form: Brixental
instance_of: Valley
countries: Austria
coordinates: lat: 47.44027778
lon: 12.2225
It rises in the hilly woods along the county line dividing Carleton County, Canada from York County, Canada in the western region of the province. Its watershed is adjacent to the South Branch of the Southwest Miramichi River, the Nashwaak River, the Keswick River and the Nackawic Stream. Features.

Geographic entities mentioned:
surface_form: Nashwaak River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.965694444444
lon: -66.586194444444
surface_form: Keswick River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.9927
lon: -66.8279
surface_form: southwest miramichi river
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.519346
lon: -67.151946
The Cold Stream originates from springs on the western slope of Skedaddle Ridge and the eastern slope of Garvie Mountain in the community of Knowlesville. The North Branch originates in three tiny lakes only a short distance west of the upper reaches of the Nashwaak River: Malcolm Lake, Long Lake and Owl Lake respectively.

Geographic entities mentioned:
surface_form: Nashwaak River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.965694444444
lon: -66.586194444444
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.23417
lon: -127.14639
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.1667
lon: -105.25
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.05
lon: -123.8
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.85055555555556
lon: -80.1686111111111
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.7933
lon: -76.2461
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.433
lon: -112.755
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.5788889
lon: -113.6552778
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.3039
lon: -79.2458
surface_form: long lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.6119
lon: -79.0092
Features. Three primary branches, the North Branch Becaguimec, the South Branch Becaguimec and the Cold Stream compose the Becaguimec Stream. The Cold Stream originates from springs on the western slope of Skedaddle Ridge and the eastern slope of Garvie Mountain in the community of Knowlesville.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Becaguimec Stream. The Becaguimec Stream () is a minor tributary of the Saint John River in the Canadian Province of New Brunswick. It rises in the hilly woods along the county line dividing Carleton County, Canada from York County, Canada in the western region of the province.

Geographic entities mentioned:
surface_form: becaguimec stream
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.3014
lon: -67.5296
Features. Three primary branches, the North Branch Becaguimec, the South Branch Becaguimec and the Cold Stream compose the Becaguimec Stream. The Cold Stream originates from springs on the western slope of Skedaddle Ridge and the eastern slope of Garvie Mountain in the community of Knowlesville.

Geographic entities mentioned:
surface_form: becaguimec stream
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.3014
lon: -67.5296
Settlement of the Becaguimec Valley itself began with the establishment of the community of Rockland in 1825 and Coldstream in or about 1826. River crossings. Three covered bridges once crossed the Becaguimec Stream, though only one remains standing. The Mangrum or Stormdale Bridge (Becaguimec Stream No. 3), which was constructed in 1909, burned in 2011. The Adair Bridge (North Becaguimec No.

Geographic entities mentioned:
surface_form: becaguimec stream
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.3014
lon: -67.5296
Region. Solano County is the easternmost county of the North Bay. As such, it is sometimes reported by news agencies as being in the East Bay. Additionally, a portion of the county extends into the Sacramento Valley, geographically. Geography. According to the U.S. Census Bureau, the county has a total area of, of which, comprising 9.3%, are covered by water.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
In March and April 2008, &quot;Farley Mowat&quot; was involved in controversy related to the 2008 Canadian commercial seal hunt. On 12 April 2008, Fisheries and Oceans Canada seized &quot;Farley Mowat&quot; in the Cabot Strait after the ship came near the seal hunt without an observation permit and two collisions with a coast guard vessel occurred.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
Canby Mountain. Canby Mountain is a mountain summit in San Juan County, Colorado, United States. Description. Canby Mountain is located east of the community of Silverton, on land managed by Rio Grande National Forest. Canby Mountain is situated on the Continental Divide in the San Juan Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: canby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.799444444444
lon: -107.54583333333
Topographic relief is modest as the summit rises in one-half mile (0.8 km). Neighbors include Sheep Mountain, to the southeast and Greenhalgh Mountain, to the east-southeast. The Continental Divide Trail and Colorado Trail traverse the peak's slopes and an ascent of the summit from historic Stony Pass covers one-half mile of off-trail hiking with 890-feet of elevation gain.

Geographic entities mentioned:
surface_form: Greenhalgh Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.785
lon: -107.50444444444
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.3417
lon: -113.471
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.976944444444
lon: -120.38861111111
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 61.83444444444444
lon: -147.5125
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.785277777778
lon: -107.88611111111
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.0248432
lon: -121.418174
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.2883
lon: -117.713
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.5439
lon: -110.524
surface_form: sheep mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.064444444444
lon: -114.36027777778
Canby Mountain. Canby Mountain is a mountain summit in San Juan County, Colorado, United States. Description. Canby Mountain is located east of the community of Silverton, on land managed by Rio Grande National Forest. Canby Mountain is situated on the Continental Divide in the San Juan Mountains which are a subrange of the Rocky Mountains.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: canby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.799444444444
lon: -107.54583333333
Climate. According to the Köppen climate classification system, Canby Mountain is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: canby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.799444444444
lon: -107.54583333333
Chełmża Lake. Chełmża Lake () is a lake in north-central Poland, located near the town of Chełmża, Toruń County, Kuyavian-Pomeranian Voivodeship. The lake is up to 6 km long, has a width up to 0,5 km, is up to 27 m deep, and has an area of 2,7 km2.

Geographic entities mentioned:
surface_form: chełmża lake
instance_of: Lake
countries: Poland
coordinates: lat: 53.1766
lon: 18.6432
Lower White River Wilderness. Lower White River Wilderness is a protected wilderness in the US State of Oregon on the southern part of Mount Hood. In 2009, Congress designated the area a National Wilderness preserve. The White River rises from White River Glacier in White River Canyon.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
The alternate name short-toed lark may also be used for three other species in the genus &quot;Calandrella&quot;. Description. The Mongolian short-toed lark is darker and has a shorter bill than the greater short-toed lark. The Mongolian short-toed lark breeds on the Tibetan plateau and winters mainly in peninsular India.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Mountaineering and adventure pursuits. In 1968, Dingle and Murray Jones were the first to climb all six major European north faces and the Bonati pillar, including Eiger and Matterhorn, in one season. He has achieved over 200 mountaineering and adventure firsts worldwide, including first ascents of mountains and faces in the Himalayas, the Andes, and in New Zealand.

Geographic entities mentioned:
surface_form: Eiger
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.577607529
lon: 8.005286822
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Wachbach. Wachbach is a river of Baden-Württemberg, Germany. It flows into the Tauber in Bad Mergentheim.

Geographic entities mentioned:
surface_form: Tauber
instance_of: Watercourse
countries: Germany
coordinates: lat: 49.25
lon: 10.114861111111
The eastern end of the tunnel links to the Lacey V. Murrow Memorial Bridge and the Homer M. Hadley Memorial Bridge (collectively the I-90 floating bridge) on Lake Washington, to Mercer Island. At in diameter, it is the world's largest diameter soft earth tunnel, having been bored through clay. Original.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
At in diameter, it is the world's largest diameter soft earth tunnel, having been bored through clay. Original. When completed in 1940, the twin tunnels connected the I-90 floating bridge on Lake Washington and Rainier Avenue South in Seattle. The bridge and tunnels were part of US Highway 10, which used surface streets between the tunnels and downtown Seattle.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Jarvis. Mount Jarvis is an eroded shield volcano and stratovolcano in the Wrangell Mountains of eastern Alaska. It is located in Wrangell-Saint Elias National Park about east of the summit of Mount Wrangell. The mountain sits at the northeastern edge of the massive ice-covered shield of Wrangell, rising nearly above it in a spectacular series of cliffs and icefalls.

Geographic entities mentioned:
surface_form: Mount Wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
Mount Jarvis. Mount Jarvis is an eroded shield volcano and stratovolcano in the Wrangell Mountains of eastern Alaska. It is located in Wrangell-Saint Elias National Park about east of the summit of Mount Wrangell. The mountain sits at the northeastern edge of the massive ice-covered shield of Wrangell, rising nearly above it in a spectacular series of cliffs and icefalls.

Geographic entities mentioned:
surface_form: mount jarvis
instance_of: Mountain
countries: United States
coordinates: lat: 62.02345277777778
lon: -143.62005555555555
Mount Jarvis. Mount Jarvis is an eroded shield volcano and stratovolcano in the Wrangell Mountains of eastern Alaska. It is located in Wrangell-Saint Elias National Park about east of the summit of Mount Wrangell. The mountain sits at the northeastern edge of the massive ice-covered shield of Wrangell, rising nearly above it in a spectacular series of cliffs and icefalls.

Geographic entities mentioned:
surface_form: mount jarvis
instance_of: Mountain
countries: United States
coordinates: lat: 62.02345277777778
lon: -143.62005555555555
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
It is located in Wrangell-Saint Elias National Park about east of the summit of Mount Wrangell. The mountain sits at the northeastern edge of the massive ice-covered shield of Wrangell, rising nearly above it in a spectacular series of cliffs and icefalls. When seen from above, Mount Jarvis is distinctly dumbbell-shaped, with two prominent peaks connected by a narrower ridge.

Geographic entities mentioned:
surface_form: mount jarvis
instance_of: Mountain
countries: United States
coordinates: lat: 62.02345277777778
lon: -143.62005555555555
The entire summit area including both peaks and the ridge is covered in glacial ice. The steep, rocky eastern and western faces of Mount Jarvis form headwalls above the cirques of the Jacksina Glacier and Copper Glacier, which flow northward out of the Wrangell Mountains. Mount Jarvis was named in 1903 by F. C. Schrader, a USGS geologist, for Lt. David H. Jarvis of the U. S.

Geographic entities mentioned:
surface_form: mount jarvis
instance_of: Mountain
countries: United States
coordinates: lat: 62.02345277777778
lon: -143.62005555555555
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
The entire summit area including both peaks and the ridge is covered in glacial ice. The steep, rocky eastern and western faces of Mount Jarvis form headwalls above the cirques of the Jacksina Glacier and Copper Glacier, which flow northward out of the Wrangell Mountains. Mount Jarvis was named in 1903 by F. C. Schrader, a USGS geologist, for Lt. David H. Jarvis of the U. S.

Geographic entities mentioned:
surface_form: mount jarvis
instance_of: Mountain
countries: United States
coordinates: lat: 62.02345277777778
lon: -143.62005555555555
It is located in Wrangell-Saint Elias National Park about east of the summit of Mount Wrangell. The mountain sits at the northeastern edge of the massive ice-covered shield of Wrangell, rising nearly above it in a spectacular series of cliffs and icefalls. When seen from above, Mount Jarvis is distinctly dumbbell-shaped, with two prominent peaks connected by a narrower ridge.

Geographic entities mentioned:
surface_form: wrangell
instance_of: Mountain
countries: United States
coordinates: lat: 62.006944444444
lon: -144.01583333333
Lindores Loch. Lindores Loch is a freshwater loch, situated in North Fife in the Parish of Abdie, in the Central Belt of Scotland. The Loch has for many years been used as a fishery and is well known for its abundant fish life. A curling pond is situated on the Northern shoreline and is nominally used by the Abdie Curling Club and Abdie ladies Curling Club.

Geographic entities mentioned:
surface_form: lindores loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.3333
lon: -3.18333
The water level and shoreline have changed over time due to roads, railway, sluice gate and farmland. Natural history. Lindores Loch is a protected Site of Special Scientific Interest (SSSI) and is designated for the flora and fauna of its wetlands and open water habitats. Specifically its high diversity of pondweeds (potamogeton), large area of reed bed, wet woodland and notable birds.

Geographic entities mentioned:
surface_form: lindores loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.3333
lon: -3.18333
In 1617 armed vandals destroyed two mills belonging to Sir Michael Balfour of Denmilne by demolishing the dam. A rare mid-1860s curling house survives here, once used by the Abdie Curling Club to store its members curling stones and other equipment. Culture. 'Lindores Loch is a beautiful sheet of water, nearly a mile in length. It is frequented by wild ducks, and abounds with perch and pike.

Geographic entities mentioned:
surface_form: lindores loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.3333
lon: -3.18333
This appearance is especially prominent from U.S. Route 95, which passes by the mountain to the east. The most common route to the summit is from the North Loop Trail or Trail Canyon to Mount Charleston, starting from where it reaches close to the top of the ridge between Mummy Mountain and Mount Charleston.

Geographic entities mentioned:
surface_form: Mount Charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
surface_form: Mount Charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
surface_form: mummy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.2994
lon: -115.649
surface_form: mummy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5425
lon: -111.961
surface_form: mount charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
surface_form: mount charleston
instance_of: Mountain
countries: United States
coordinates: lat: 36.271597222222
lon: -115.69556944444
surface_form: mummy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.475
lon: -105.624
Mummy Mountain (Nevada). Mummy Mountain is the second highest peak of the Spring Mountains in Clark County, Nevada, United States. It is the twentieth highest mountain in the state. The mountain is located within the Mount Charleston Wilderness and the Humboldt-Toiyabe National Forest.

Geographic entities mentioned:
surface_form: mummy mountain (nevada)
instance_of: Mountain
countries: United States
coordinates: lat: 36.2994
lon: -115.649
surface_form: mummy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5425
lon: -111.961
surface_form: mummy mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.475
lon: -105.624