Sarmila/GeoWiki-Features huggingface dataset:
These institutions contribute to both the cultural and economic vitality of the city. Other key sectors include healthcare, retail trade, and public administration. Tourism also supports the local economy, with visitors drawn to features like the city's historic architecture, Lake Sinclair, and Andalusia, the former home of author Flannery O'Connor.

Geographic entities mentioned:
surface_form: Lake Sinclair
instance_of: Lake
countries: United States
coordinates: lat: 33.1405
lon: -83.202
Economic diversification efforts gained momentum mid-century. The creation of Lake Sinclair in 1953 by the Georgia Power Company spurred recreational tourism, and subsequent historic preservation projects in the 1980s and 1990s revitalized downtown Milledgeville.

Geographic entities mentioned:
surface_form: Lake Sinclair
instance_of: Lake
countries: United States
coordinates: lat: 33.1405
lon: -83.202
Tourism adds to the economic base as well, with visitors drawn to attractions such as the Milledgeville Historic District, Antebellum architecture, Flannery O'Connor's Andalusia Farm, and outdoor recreation at Lake Sinclair. In 2016, tourism generated $88.7 million in direct spending in Baldwin County, supported 796 jobs, and contributed over $6 million in state and local tax revenue. Government.

Geographic entities mentioned:
surface_form: Lake Sinclair
instance_of: Lake
countries: United States
coordinates: lat: 33.1405
lon: -83.202
The Canada Company. In 1826, Dunlop moved to Upper Canada to work with John Galt and the Canada Company, settling in Goderich. The Canada Company had received a grant of management and settlement for the Huron Tract, a large tract of land to the south-west of Lake Huron. Galt, a Scottish novelist, had been appointed the director of the Company's affairs.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Galt in turn appointed Dunlop as Warden of the Company's Woods and Forests by of the Canada Company. The position involved inspecting the company lands in the Huron Tract along the eastern shore of Lake Huron to protect them and the selection of land to be sold to settlers from Europe for profit. This position put Tiger Dunlop as second-in-command to Galt of the Company in Canada.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Royal Salute (whisky). Royal Salute is a blended Scotch whisky brand produced and bottled by Chivas Brothers in Strathisla Distillery in Speyside, Scotland. History. Royal Salute was launched by Chivas Brothers on 2 June 1953 by in tribute to Queen Elizabeth II on the day of her Coronation.

Geographic entities mentioned:
surface_form: Speyside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
Strathisla distillery. The brand's distillery and visitor centre are at the Strathisla distillery, located in Speyside. The distillery was founded in 1786, and it is the oldest working distillery in the Highlands of Scotland. The Strathisla distillery is owned by Chivas Brothers, and Strathisla Single Malt is one of the malt whiskies used within the Royal Salute blend. Brand collaborations.

Geographic entities mentioned:
surface_form: Speyside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
Mount Cameron (Washington). Mount Cameron is a triple-summit mountain located within Olympic National Park in Jefferson County of Washington state. Mount Cameron is situated 21 miles southwest of Sequim, and set within the Daniel J. Evans Wilderness. Topographic relief is significant as the southeast aspect rises over above the Dosewallips River in approximately one mile.

Geographic entities mentioned:
surface_form: jefferson
instance_of: Mountain
countries: United States
coordinates: lat: 44.6743006
lon: -121.799573611
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Cameron (Washington). Mount Cameron is a triple-summit mountain located within Olympic National Park in Jefferson County of Washington state. Mount Cameron is situated 21 miles southwest of Sequim, and set within the Daniel J. Evans Wilderness. Topographic relief is significant as the southeast aspect rises over above the Dosewallips River in approximately one mile.

Geographic entities mentioned:
surface_form: mount cameron (washington)
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Cameron (Washington). Mount Cameron is a triple-summit mountain located within Olympic National Park in Jefferson County of Washington state. Mount Cameron is situated 21 miles southwest of Sequim, and set within the Daniel J. Evans Wilderness. Topographic relief is significant as the southeast aspect rises over above the Dosewallips River in approximately one mile.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
He pioneered the first trail into Cameron Basin. Climate. Based on the Köppen climate classification, Mount Cameron is located in the marine west coast climate zone of western North America. Weather fronts originating in the Pacific Ocean travel northeast toward the Olympic Mountains.

Geographic entities mentioned:
surface_form: mount cameron
instance_of: Mountain
countries: United States
coordinates: lat: 47.82537
lon: -123.32851
William died in New Haven, Connecticut, on March 7, 1881, of tuberculosis. He was buried in Evergreen Cemetery in New Haven. After his death, his wife, Sarah, moved to Santa Clara Valley, California and became notable for building Llanada Villa, later known as the Winchester Mystery House. Legacy.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
In fact, Major Khurshid Anwar had already mobilised the Pashtun tribes from the Frontier for a raid on Kashmir and was poised to launch his attack on 15 October. When the tribal invasion was launched on 22 October 1947, Khurshid was still in the Valley. He was arrested on 2 November 1947 by the State Police, who recovered maps and documents from him.

Geographic entities mentioned:
surface_form: Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
History. In 1837, plans were submitted for a rail link from Riesa, a major freight hub on the Elbe river, to Chemnitz and on to Zwickau, which was significant as a coal-producing region. After the Leipzig–Dresden railway was opened, connecting the industrial city of Chemnitz to Leipzig and Dresden, even if it involved a detour via Riesa, was given the highest priority.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In the first half of the 20th century, the area was extensively covered in glass-houses and market gardens. Gravel extraction has also long been a major industry in the Lea Valley, leaving a legacy of pits now used for recreation and an important wildlife habitat. In 1959–60 all of the church's houses and land were converted to stock or bank investments.

Geographic entities mentioned:
surface_form: Lea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Veggli. Veggli is a village in the municipality of Rollag, in the county of Buskerud, Norway. Veggli is located about 66 kilometers north of Kongsberg. It is located in the traditional district and valley of Numedal. It is situated on the Numedalslågen River, near the mouth of Nørdsteåas estuary. Its population in 2005 was 292. Veggli train station was on the Numedal Line.

Geographic entities mentioned:
surface_form: Numedal
instance_of: Valley
countries: Norway
coordinates: lat: 60
lon: 9.2
The line ran from Kongsberg to Rødberg in Nore og Uvdal. The line was officially opened in 1927. Passenger traffic on the track was closed in 1988. West from Veggli, the road goes over Vegglifjell where Veggli Lodge and Veggli Skisenter are located. Further the road leads to the villages of Austbygdi and Tessungdalen in Tinn. Veggli Church (&quot;Veggli kirke&quot;) in Kongsberg deanery.

Geographic entities mentioned:
surface_form: Vegglifjell
instance_of: Mountain
countries: Norway
coordinates: lat: 60.1081
lon: 8.9244
Upland squirrel. The upland squirrel (&quot;Sundasciurus tahan&quot;), also known as the mountain slender squirrel, is a species of rodent in the family Sciuridae. Native to Peninsular Malaysia, it inhabits montane and lower montane forests including portions of the Titiwangsa Mountains and Gunung Tahan.

Geographic entities mentioned:
surface_form: Gunung Tahan
instance_of: Mountain
countries: Malaysia
coordinates: lat: 4.6311111111111
lon: 102.23444444444
The Free and Hanseatic city of Hamburg (85.5%), the State of Schleswig-Holstein (3%), the State of Lower Saxony (2%) and the Districts Herzogtum Lauenburg, Pinneberg, Segeberg, Stormarn, Harburg, Lüneburg and Stade (9.5%) are these PTAs. Ferries. HADAG Seetouristik und Fährdienst operates ferries on the Elbe river. Fares.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It is found in Querétaro, Mexico. Its common name comes from the indigenous Otomi people who are native to the Mexican Plateau region, and its scientific name was given in honour of Natasha Mhatre, a noted Indian Biologist and Professor at University of Western Ontario in Canada.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
General Butler (ship). The &quot;General Butler&quot; was a schooner-rigged sailing canal boat that plied the waters of Lake Champlain and the Champlain Canal in the United States states of Vermont and New York. Built in 1862 and named for American Civil War General Benjamin Franklin Butler, she sank after striking the Burlington Breakwater in 1876, while carrying a load of marble.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Langvatnet (Sørfold). or is a lake that lies in Sørfold Municipality in Nordland county, Norway. The lake is located about northeast of the village of Straumen, just north of Rago National Park and the border with Sweden.

Geographic entities mentioned:
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.36861111
lon: 14.0825
surface_form: langvatnet (sørfold)
instance_of: Lake
countries: Norway
coordinates: lat: 67.531944444444
lon: 16.181944444444
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 68.13316
lon: 17.04921
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 61.96136
lon: 7.3982
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 67.136111111111
lon: 16.030833333333
surface_form: langvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 66.89061
lon: 14.14796
Roque Nublo (&quot;Clouded Rock&quot;, &quot;Rock in the Clouds&quot;) is a volcanic rock on the island of Gran Canaria, Canary Islands, Spain. It is tall, and its top is above sea level. The Roque Nublo is the third highest point on the island of Gran Canaria, after the Morro de la Agujereada at, and the Pico de las Nieves at. It was formed by a volcanic eruption around 4.5 million years ago.

Geographic entities mentioned:
surface_form: Morro de la Agujereada
instance_of: Mountain
countries: Spain
coordinates: lat: 27.96081388888889
lon: -15.57118611111111
surface_form: Pico de las Nieves
instance_of: Mountain
countries: Spain
coordinates: lat: 27.961944444444
lon: -15.571666666667
surface_form: morro de la agujereada
instance_of: Mountain
countries: Spain
coordinates: lat: 27.96081388888889
lon: -15.57118611111111
surface_form: pico de las nieves
instance_of: Mountain
countries: Spain
coordinates: lat: 27.961944444444
lon: -15.571666666667
Roque Nublo. Roque Nublo (&quot;Clouded Rock&quot;, &quot;Rock in the Clouds&quot;) is a volcanic rock on the island of Gran Canaria, Canary Islands, Spain. It is tall, and its top is above sea level. The Roque Nublo is the third highest point on the island of Gran Canaria, after the Morro de la Agujereada at, and the Pico de las Nieves at.

Geographic entities mentioned:
surface_form: roque nublo
instance_of: Mountain
countries: Spain
coordinates: lat: 27.970833333333
lon: -15.6125
It was formed by a volcanic eruption around 4.5 million years ago. Location. Roque Nublo is in the, in the Tejeda municipality, near the geographical centre of Gran Canaria. Near to the Roque Nublo are other rock formations, such as the &quot;Roque del Fraile&quot; and &quot;La Rana&quot;.

Geographic entities mentioned:
surface_form: roque nublo
instance_of: Mountain
countries: Spain
coordinates: lat: 27.970833333333
lon: -15.6125
Wankarani culture. The Wankarani culture was a formative stage culture that existed from approximately 1400 BCE to 600 CE on the altiplano highlands of Bolivia's Oruro Department to the north and northeast of Lake Poopo. It is the earliest known sedentary culture in Bolivia, as after circa 1200 BCE camelid hunters of the altiplano became camelid herders and sedentary lifestyle developed.

Geographic entities mentioned:
surface_form: altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
The Alto Ramírez phase dates to 1000 BCE-400 CE. The Alto Ramirez phase seems to have been contemporaneous with Pukara and other Lake Titicaca Basin societies of the andean Early Intermediate Period, such as Qaluyu, Chiripa, Pukara, Wankarani and Early Tiwanaku.

Geographic entities mentioned:
surface_form: Qaluyu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.6275
lon: -68.6339
Porcupine Gorge. Porcupine Gorge is a gorge on Galah Creek in Porcupine, Shire of Flinders in North West Queensland, Australia. It is a protected area within the Porcupine Gorge National Park. Access to the gorge and national park is via the Kennedy Development Road. The sandstone gorge has incised up to 40 m below the adjacent plateau surface.

Geographic entities mentioned:
surface_form: porcupine gorge
instance_of: Valley
countries: Australia
coordinates: lat: -20.41104722222222
lon: 144.42857222222221
The sandstone gorge has incised up to 40 m below the adjacent plateau surface. In winter the base of the gorge is a series of waterholes while in the wet season it becomes a raging cascade which has excavated a deep chasm. There is an annual race held in the gorge called the Porcupine Gorge Challenge. It starts at the bottom of the gorge at The Pyramid.

Geographic entities mentioned:
surface_form: porcupine gorge
instance_of: Valley
countries: Australia
coordinates: lat: -20.41104722222222
lon: 144.42857222222221
Monkeys love the fruit and hence the tree is sometimes known as the monkey-bread tree. The dugong is a medium-sized marine mammal which is found in Mannar Bay, Nachchikuda, Jaffna island and near Adam's Bridge. IUCN conservation status is vulnerable because of over-hunting for food and accidental capture in fishing nets.

Geographic entities mentioned:
surface_form: Adam's Bridge
instance_of: Landform
countries: India
Sri Lanka
coordinates: lat: 9.121
lon: 79.5217
No profile was made for Luke 10. It forms a textual cluster with codex 281. History. C. R. Gregory dated the manuscript to the 12th century. Currently the manuscript is dated by the INTF to the 12th century. Formerly it was held at the Athos monastery (St. Andrew E'). C. R. Gregory saw it in 1886. The manuscript was added to the list of New Testament manuscripts by Gregory (906e).

Geographic entities mentioned:
surface_form: Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Lake Nyabikere. Lake Nyabikere is a lake located in the Kabarole district of Uganda. The lake is also known as &quot;Frog Lake&quot; since it has a variety of frog species in its waters. It is also a crater lake in the ranges of Mountain Rwenzori in western Uganda and a safari destination in Uganda. Flora and fauna.

Geographic entities mentioned:
surface_form: lake nyabikere
instance_of: Lake
countries: Uganda
coordinates: lat: 0.4972222222222222
lon: 30.328611111111112
It is also a crater lake in the ranges of Mountain Rwenzori in western Uganda and a safari destination in Uganda. Flora and fauna. The area around Lake Nyabikere has chimpanzees, a variety of bird species, and various tree species and other plant species and acts as a tourist destination for Uganda.

Geographic entities mentioned:
surface_form: lake nyabikere
instance_of: Lake
countries: Uganda
coordinates: lat: 0.4972222222222222
lon: 30.328611111111112
Antermony Loch. Antermony Loch is a lochan (small loch) in East Dunbartonshire, Scotland, at the edge of the village of Auchenreoch. Its name may be a corruption of the Scottish Gaelic elements &quot;uachdar&quot; (&quot;summit, top&quot;) + &quot;monadh&quot; (&quot;moorland&quot;), i.e. &quot;Loch of the Moorland Summit&quot;.

Geographic entities mentioned:
surface_form: antermony loch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 55.965
lon: -4.13444444
Yr Aran. Yr Aran is a mountain peak on a ridge radiating south from Snowdon, Wales' highest mountain, with views of the summit of Snowdon, Moel Hebog and the Nantlle Ridge. It has an elevation of and a prominence of. Although no paths are marked on maps, the ascent can be made as a detour from the Rhyd Ddu path or the Watkin Path up Snowdon.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: Moel Hebog
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.000138888889
lon: -4.1398
surface_form: yr aran
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.042488888889
lon: -4.0837194444444
Yr Aran. Yr Aran is a mountain peak on a ridge radiating south from Snowdon, Wales' highest mountain, with views of the summit of Snowdon, Moel Hebog and the Nantlle Ridge. It has an elevation of and a prominence of. Although no paths are marked on maps, the ascent can be made as a detour from the Rhyd Ddu path or the Watkin Path up Snowdon.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Yr Aran. Yr Aran is a mountain peak on a ridge radiating south from Snowdon, Wales' highest mountain, with views of the summit of Snowdon, Moel Hebog and the Nantlle Ridge. It has an elevation of and a prominence of. Although no paths are marked on maps, the ascent can be made as a detour from the Rhyd Ddu path or the Watkin Path up Snowdon.

Geographic entities mentioned:
surface_form: yr aran
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.042488888889
lon: -4.0837194444444
1995 World Rowing Championships. The 1995 World Rowing Championships were World Rowing Championships that were held from 20 to 28 August 1995 at Lake Kaukajärvi, Tampere, Finland. Events. The women's lightweight four (LW4-) was poorly subscribed, with only five nations entering boats; no heats were thus had. The Australian team, although present, did not start.

Geographic entities mentioned:
surface_form: Lake Kaukajärvi
instance_of: Lake
countries: Finland
coordinates: lat: 61.472221944444
lon: 23.902778055556
The Havel crossed at the East German border in Nedlitz (a part of Potsdam-Bornstedt), continuing through the Elbe-Havel Canal and then either taking the Elbe northwestwards crossing the border again at Cumlosen (E)/Schnackenburg (W) or westwards following the Mittellandkanal to Buchhorst (Oebisfelde) (E)/Rühen (W).

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Pterospoda nigrescens. &quot;Pterospoda nigrescens&quot; is a species of moth of the family Geometridae. It occurs at moderate elevations in arid scrub and open woodland habitat, ranging from south-eastern Arizona and the Edwards Plateau of west-central Texas south to at least Durango, Mexico. It is not known from New Mexico, but should occur there. The wingspan is about 24 mm.

Geographic entities mentioned:
surface_form: Edwards Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 30.3
lon: -99.6
Pizzo Ragno. Pizzo Ragno is a mountain of Piedmont, Italy, with an elevation of. It is located in the Lepontine Alps, in the Province of Verbano-Cusio-Ossola, between the Val Vigezzo and the smaller Val Loana. The peak is a renowned panoramic point and can be reached on foot starting from Druogno, Santa Maria Maggiore, or Malesco.

Geographic entities mentioned:
surface_form: ossola
instance_of: Valley
countries: Italy
coordinates: lat: 46.283333333333
lon: 8.35
surface_form: cusio
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
surface_form: val vigezzo
instance_of: Valley
countries: Italy
coordinates: lat: 46.1333
lon: 8.55
Pizzo Ragno. Pizzo Ragno is a mountain of Piedmont, Italy, with an elevation of. It is located in the Lepontine Alps, in the Province of Verbano-Cusio-Ossola, between the Val Vigezzo and the smaller Val Loana. The peak is a renowned panoramic point and can be reached on foot starting from Druogno, Santa Maria Maggiore, or Malesco.

Geographic entities mentioned:
surface_form: pizzo ragno
instance_of: Mountain
countries: Italy
coordinates: lat: 46.1013935
lon: 8.4219597
In remembrance, he named his production house Duet Movies. Saran was one of the assistant directors in the film. Although the film's storyline is set in Chennai, 90% of the film was shot predominantly in and around Bheemunipatnam, Srikakulam, Vizianagaram, Araku Valley, Rayagada and Vishakhapatnam yet the remaining 10% of portions were shot in Chennai as well. Soundtrack.

Geographic entities mentioned:
surface_form: Araku Valley
instance_of: Valley
countries: India
coordinates: lat: 18.3333
lon: 82.8667
Unlike other indigenous villages in the Great Lakes region, the Mantle Site is unique &quot;in that it represents a community that had already come together from several villages and chose to build here.&quot; During its existence, the community was the only village near the eastern Rouge trail linking Lake Ontario and Lake Simcoe and north of it.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
Soagŋojávri. Soagŋojávri is a lake in Kautokeino Municipality in Finnmark county, Norway. The lake lies on the Finnmarksvidda plateau, about west of the village of Masi.

Geographic entities mentioned:
surface_form: Finnmarksvidda
instance_of: Plateau
countries: Norway
coordinates: lat: 69.31666667
lon: 23.81666667
Soagŋojávri. Soagŋojávri is a lake in Kautokeino Municipality in Finnmark county, Norway. The lake lies on the Finnmarksvidda plateau, about west of the village of Masi.

Geographic entities mentioned:
surface_form: soagŋojávri
instance_of: Lake
countries: Norway
coordinates: lat: 69.4633
lon: 23.145
The surface of the lake is, on average, above sea level, and at its deepest it is around deep. The main inflow and outflow of the lake is the River Ach, which enters from the west and departs to the north. The northeastern part of the lake is known as &quot;Untersee&quot;, the southeastern part as &quot;Stegsee&quot; and the southwestern part as &quot;Obersee&quot; (see map below).

Geographic entities mentioned:
surface_form: obersee
instance_of: Lake
countries: Germany
coordinates: lat: 47.5161
lon: 12.9883
Staffelsee. The Staffelsee is a lake in the Garmisch-Partenkirchen district of Bavaria, Germany. The settlements of Murnau, Seehausen and Uffing lie on its shores. Within its area lie seven islands, the largest and only inhabited of which is Wörth. Wörth was the site of, a Carolingian monastery founded in the 8th century and dissolved in the 11th century.

Geographic entities mentioned:
surface_form: staffelsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.6908
lon: 11.1608
Naiset Point. Naiset Point is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. The mountain is situated southeast of Lake Magog, and at the end of the ridge extending north from Terrapin Mountain. Naiset Point is composed of sedimentary rock laid down during the Cambrian period.

Geographic entities mentioned:
surface_form: Terrapin Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.88
lon: -115.6175
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: lake magog
instance_of: Lake
countries: Canada
coordinates: lat: 45.3031
lon: -72.0431
Naiset Point. Naiset Point is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. The mountain is situated southeast of Lake Magog, and at the end of the ridge extending north from Terrapin Mountain. Naiset Point is composed of sedimentary rock laid down during the Cambrian period.

Geographic entities mentioned:
surface_form: assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: mount assiniboine
instance_of: Mountain
countries: Canada
coordinates: lat: 50.86972222222222
lon: -115.6511111111111
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. History. The mountain was named in 1913 by The Interprovincial Boundary Survey for the word &quot;naiset&quot; which translates from the First Nations word for &quot;sunset&quot;. The first ascent of Naiset Point was made in 1920 by H.E. Bulyea, N. Allen, M. Gold, D.J.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Wates. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Naiset Point is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Naiset Point drains into Lake Magog.

Geographic entities mentioned:
surface_form: lake magog
instance_of: Lake
countries: Canada
coordinates: lat: 45.3031
lon: -72.0431
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
Naiset Point. Naiset Point is a mountain summit located in Mount Assiniboine Provincial Park, in the Canadian Rockies of British Columbia, Canada. The mountain is situated southeast of Lake Magog, and at the end of the ridge extending north from Terrapin Mountain. Naiset Point is composed of sedimentary rock laid down during the Cambrian period.

Geographic entities mentioned:
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
The mountain is situated southeast of Lake Magog, and at the end of the ridge extending north from Terrapin Mountain. Naiset Point is composed of sedimentary rock laid down during the Cambrian period. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. History.

Geographic entities mentioned:
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. History. The mountain was named in 1913 by The Interprovincial Boundary Survey for the word &quot;naiset&quot; which translates from the First Nations word for &quot;sunset&quot;. The first ascent of Naiset Point was made in 1920 by H.E. Bulyea, N. Allen, M. Gold, D.J.

Geographic entities mentioned:
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
Wates. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Climate. Based on the Köppen climate classification, Naiset Point is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Naiset Point drains into Lake Magog.

Geographic entities mentioned:
surface_form: naiset point
instance_of: Mountain
countries: Canada
coordinates: lat: 50.90004
lon: -115.61877
Farndale flit. Farndale in the North York Moors is separated from its neighbour Rosedale to the east by a high but relatively level moorland promontory known as Blakey Ridge. On the east side of that ridge is a topological feature known as Hobb Crag, overlooking the village of Rosedale Abbey.

Geographic entities mentioned:
surface_form: Farndale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3463
lon: -0.965
surface_form: Rosedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35
lon: -0.88333333333333
Cow Mountain Ridge. Cow Mountain Ridge is a ridge in Lake County, California, and Mendocino County, California. It joins Cow Mountain from the south. Location. Cow Mountain Ridge is in the Mayacamas Mountains of the northern California Coast Ranges. It is in Lake and Mendocino counties. Clear Lake is to the east and the Russian River Valley and Ukiah are to the west.

Geographic entities mentioned:
surface_form: Cow Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.093055555556
lon: -123.35388888889
Ojców Castle. Ojców Castle (Polish: &quot;Zamek Ojców&quot;) - a castle located in the Kraków-Częstochowa Upland, part of a system of castles known as the &quot;Eagle's Nests&quot; (Polish: &quot;Orle Gniazda&quot;) - formerly protecting the southern border of the Kingdom of Poland; currently housing a museum dedicated to the castle in its renovated castle-tower.

Geographic entities mentioned:
surface_form: Kraków-Częstochowa Upland
instance_of: Plateau
countries: Poland
coordinates: lat: 50.2067
lon: 19.8292
Rannerdale Knotts. Rannerdale Knotts is a fell in the Lake District of Cumbria, England. Rising from the Buttermere valley, it is one of the smaller Cumbrian hills and is overlooked by a number of surrounding fells, such as Grasmoor, Whiteless Pike and, across Crummock Water, Mellbreak and the High Stile ridge.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: Whiteless Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: Mellbreak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.555438888889
lon: -3.3188888888889
surface_form: High Stile
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.521669444444
lon: -3.2838111111111
The central sector, rising between Whinlatter Pass and Newlands Pass, includes Whiteless Pike. The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike.

Geographic entities mentioned:
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: Crag Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range. It sends out a subsidiary ridge to the south west, stepping down over Wandope and Whiteless Pike toward Buttermere village. Just above the village this ridge then turns sharply north west and rises to the summit of Rannerdale Knotts.

Geographic entities mentioned:
surface_form: Wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Geology. The summit area shows outcropping of the Kirkstile Formation. These Ordovician rocks, typical of the Skiddaw massif, are composed of laminated mudstone and siltstone. Low Bank lies across the Causey Pike Fault and is part of the Buttermere Formation, an olistostrome of disrupted sheared and folded mudstone, siltstone and sandstone.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
The object appears to have been lead-bearing galena of which some traces remain. Summit. The small tidy summit on the highest rock knoll bears a cairn. The view is limited by the circle of higher fells, but the vista of Buttermere backed by Great Gable is excellent. Crummock Water can also be brought into view by taking a few paces westward. Ascents.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
There is a more direct ascent up the west face of the fell from Hause Point at Rannerdale, accessed from the B5289 road on the eastern shore of Crummock Water. A larger circuit of Rannerdale can also be made, taking in Grasmoor, Crag Hill, Wandope, Whiteless Pike and Rannerdale Knotts. Norse settlement and Norman conquest.

Geographic entities mentioned:
surface_form: wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
This section of the fell is named Low Bank on Ordnance Survey maps and is clad primarily in bracken. The final section bears a series of rocky knolls, still rising slowly north westward. A tumbling descent of crag and scree then follows as the end of the ridge drops steeply to the valley floor, halfway along the shore of Crummock Water. Rannerdale farm lies below this terminal face.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
Rannerdale farm lies below this terminal face. The south western side of Rannerdale Knotts is bounded first by Mill Beck, running through Buttermere village, and then by Crummock Water. The north eastern flank falls to Squat Beck, a feeder of Rannerdale Beck.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
The north eastern flank falls to Squat Beck, a feeder of Rannerdale Beck. High Rannerdale lies within the angle of the ridge between Whiteless Pike and Rannerdale Knotts, Rannerdale proper being a triangular patch of pasture constrained by Rannerdale Knotts, Grasmoor and Crummock Water. Geology. The summit area shows outcropping of the Kirkstile Formation.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
There are also two minor intrusions of basalt running across the ridgeline. There is a trial level in the northern crags, above Hause Point on the Crummock Water road. The opening is about square but the level extends only a little way into the fell-side. The object appears to have been lead-bearing galena of which some traces remain. Summit.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
The object appears to have been lead-bearing galena of which some traces remain. Summit. The small tidy summit on the highest rock knoll bears a cairn. The view is limited by the circle of higher fells, but the vista of Buttermere backed by Great Gable is excellent. Crummock Water can also be brought into view by taking a few paces westward. Ascents.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
Ascents. Rannerdale Knotts is often ascended from Buttermere, making use of the good path going up Whiteless Pike, before turning west north-west along Low Bank at the col at. There is a more direct ascent up the west face of the fell from Hause Point at Rannerdale, accessed from the B5289 road on the eastern shore of Crummock Water.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
The highest ground in the North Western Fells is an east-west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Ascents. Rannerdale Knotts is often ascended from Buttermere, making use of the good path going up Whiteless Pike, before turning west north-west along Low Bank at the col at. There is a more direct ascent up the west face of the fell from Hause Point at Rannerdale, accessed from the B5289 road on the eastern shore of Crummock Water.

Geographic entities mentioned:
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
In Size's version, Ranulf Meschin escaped and lived in disgrace until he succeeded a relative as Earl of Chester in 1120. (In fact, he continued as lord of Cumberland until 1120, when he was promoted to become the Earl of Chester.)
The battle is imagined to have taken place in the side valley of Rannerdale, which runs east of the summit of the fell, west of Whiteless Pike and south of Grasmoor.

Geographic entities mentioned:
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Rannerdale Knotts. Rannerdale Knotts is a fell in the Lake District of Cumbria, England. Rising from the Buttermere valley, it is one of the smaller Cumbrian hills and is overlooked by a number of surrounding fells, such as Grasmoor, Whiteless Pike and, across Crummock Water, Mellbreak and the High Stile ridge.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
Norse settlement and Norman conquest. The Buttermere area does not appear in the Domesday Book, which indicates that this part of Cumbria was not under Norman control in 1086. The central area of the Lake District is known to have been populated by the earlier Norse invaders in the early 10th century, and dale is etymologically Norse.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
These Ordovician rocks, typical of the Skiddaw massif, are composed of laminated mudstone and siltstone. Low Bank lies across the Causey Pike Fault and is part of the Buttermere Formation, an olistostrome of disrupted sheared and folded mudstone, siltstone and sandstone. There are also two minor intrusions of basalt running across the ridgeline.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
Norse settlement and Norman conquest. The Buttermere area does not appear in the Domesday Book, which indicates that this part of Cumbria was not under Norman control in 1086. The central area of the Lake District is known to have been populated by the earlier Norse invaders in the early 10th century, and dale is etymologically Norse.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Rannerdale Knotts. Rannerdale Knotts is a fell in the Lake District of Cumbria, England. Rising from the Buttermere valley, it is one of the smaller Cumbrian hills and is overlooked by a number of surrounding fells, such as Grasmoor, Whiteless Pike and, across Crummock Water, Mellbreak and the High Stile ridge.

Geographic entities mentioned:
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
Rising from the Buttermere valley, it is one of the smaller Cumbrian hills and is overlooked by a number of surrounding fells, such as Grasmoor, Whiteless Pike and, across Crummock Water, Mellbreak and the High Stile ridge. In modern legend Rannerdale Knotts is said to be the site of a battle between the native Cumbrians and Norsemen and the invading Normans in the late 11th or early 12th century.

Geographic entities mentioned:
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
It sends out a subsidiary ridge to the south west, stepping down over Wandope and Whiteless Pike toward Buttermere village. Just above the village this ridge then turns sharply north west and rises to the summit of Rannerdale Knotts. The sharp angle in the ridge is marked by a depression at, beyond which the ground climbs slowly for around a mile toward the top.

Geographic entities mentioned:
surface_form: rannerdale knotts
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5522
lon: -3.28941
The garden, located in Nayot on the southeastern edge of the Givat Ram campus of the Hebrew University of Jerusalem, opened to the public in 1985 as a successor to the National Botanic Garden of Israel on Mount Scopus, which still exists today as a separate entity. History.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
History. Plans for the first National Botanic Garden of Israel, on a plot of land purchased on Mount Scopus in 1926, were drawn up by Alexander Eig, chairman of the Botany Department of the Hebrew University, based on the flora of the Land of Israel from Mount Lebanon to the desert. Planting began in 1931. The botanical gardens on Mount Scopus were the first home of the Biblical Zoo.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
The range of the rhesus or common macaque extends from as far north as the Taihang Mountains of Shanxi and down to Hainan. Tibetan macaques are often seen at tourist sites such as Mount Emei and Huangshan. Stump-tailed macaques have distinct red faces and live throughout southern China. The Formosan rock macaque is endemic to Taiwan.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
A few Indochinese tigers were known to live in Yunnan where six nature reserves have been established for their protection. The range of the snow leopard extends across the Himalayas, Tibetan Plateau, Karakorum Mountains, and Tian Shan in western China. The clouded leopard occurs in forest regions south of the Yangtze River. It became locally extinct in Taiwan in 1972.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The clouded leopard occurs in forest regions south of the Yangtze River. It became locally extinct in Taiwan in 1972. The Chinese mountain cat is endemic to China and lives on the north-eastern edge of the Tibetan Plateau. It was recorded only in eastern Qinghai and north-western Sichuan. It was photographed by a camera-trap for the first time in 2007.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88