Sarmila/GeoWiki-Features huggingface dataset:
Ostenoteuthidae is an extinct family of cephalopods from Lower Jurassic of Italy. They had ten arms with unusual structure. Both known species are from Lower Sinemurian. The type locality for up to date known two species is near village Osteno, Lake Lugano, Province of Como, northern Italy. Eight specimens from this family are stored in Museo Civico di Storia Naturale di Milano in Milan, Italy.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
County of Frome. The County of Frome is one of the 49 cadastral counties of South Australia in straddling the Mid North and Flinders Ranges regions. It was proclaimed in 1851 by Governor Henry Young and was named for the former Surveyor-General of South Australia, Edward Charles Frome. The iconic Mount Remarkable in the Hundred of Gregory is at the centre of the county. Local government.

Geographic entities mentioned:
surface_form: Mount Remarkable
instance_of: Mountain
countries: Australia
coordinates: lat: -32.80603
lon: 138.16479
Origins. The Chiefs of Clan Grant descended from Normans who arrived in Scotland during the medieval period, bearing the French name &quot;le Grand&quot; ('the tall', 'large'). The first Grants to appear in Scotland are recorded in the 13th century when they acquired the lands of Stratherrick. Sir Laurence le Grant, son of Gregory le Grant, was Sheriff of Inverness. Wars of Scottish Independence.

Geographic entities mentioned:
surface_form: Stratherrick
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.25
lon: -4.42
Their main allies being the Clan Gordon, whose chief was the powerful Earl of Huntly. In 1535 James Grant, 3rd Laird of Freuchie was made responsible for the policing of Strathspey. In 1580 Robert Grant, champion of the Grants, defeated an English champion at a jousting tournament while on an embassy in England.

Geographic entities mentioned:
surface_form: Strathspey
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
Grant has also explained in recent interviews he also looked after William, Prince of Wales and Catherine, Princess of Wales during his time at Highgrove. His first employers were Urs Schwarzenbach and Major Christopher Hanbury on the Ben Alder estate, where he began working in private service in 1997. Based in Tetbury, Gloucestershire, Harrold now runs an etiquette and butler school.

Geographic entities mentioned:
surface_form: Ben Alder
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.813796
lon: -4.465089
Suyruqucha (Huarochirí). Suyruqucha (Quechua &quot;suyru&quot; a very long dress tracked after when worn, &quot;qucha&quot; lake, Hispanicized spelling &quot;Suerococha&quot;) is a mountain in the Cordillera Central in the Andes of Peru and the name of a little lake near the mountain.

Geographic entities mentioned:
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.70944444
lon: -75.23833333
surface_form: suyruqucha (huarochirí)
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9125
lon: -76.2189
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2864
lon: -76.9758
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9389
lon: -76.0519
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.20916667
lon: -73.05777778
Suyruqucha (Huarochirí). Suyruqucha (Quechua &quot;suyru&quot; a very long dress tracked after when worn, &quot;qucha&quot; lake, Hispanicized spelling &quot;Suerococha&quot;) is a mountain in the Cordillera Central in the Andes of Peru and the name of a little lake near the mountain.

Geographic entities mentioned:
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.70944444
lon: -75.23833333
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9125
lon: -76.2189
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2864
lon: -76.9758
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2864
lon: -76.9758
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -11.9389
lon: -76.0519
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.2972
lon: -76.9806
surface_form: suerococha
instance_of: Mountain
countries: Peru
coordinates: lat: -10.3861
lon: -76.8556
surface_form: suyruqucha
instance_of: Mountain
countries: Peru
coordinates: lat: -13.20916667
lon: -73.05777778
The peak of the mountain lies in the Lima Region, Huarochirí Province, on the border of the districts of Huarochirí, San Damian and San Mateo. It is situated southeast of Uqhu. The mountain is named after a small lake northwest of it and southeast of Uqhu. It lies in the San Mateo District at.

Geographic entities mentioned:
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.7878
lon: -76.0631
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.8958
lon: -76.2414
surface_form: uqhu
instance_of: Mountain
countries: Peru
coordinates: lat: -11.5225
lon: -76.2464
The inscription credits the influential general Shamshi-ilu with victory against Damascus and is ambiguous concerning whether it was Shamshu-ilu or Shalmaneser who negotiated with Ušpilulume. At Tell Abta, an archaeological site by Lake Tharthar, a stele has been found, written by the palace herald Bel-harran-beli-usur which describes the foundation of a new city in the desert.

Geographic entities mentioned:
surface_form: Lake Tharthar
instance_of: Lake
countries: Iraq
coordinates: lat: 33.966666666667
lon: 43.183333333333
The lake vessels generally have a 10:1 length to beam ratio, whereas ocean vessels are typically 7:1. Size. The size of a lake freighter determines where it may work. The shallow draft imposed by the St. Marys River and Lake St. Clair restrict the cargo capacity of lakers. Poe Lock at the Soo Locks is the largest deep lock at long and wide.

Geographic entities mentioned:
surface_form: Lake St. Clair
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.450265
lon: -82.67572
Most students live on the college's wooded campus located from the Lake Michigan shore; however, the population of commuting students has increased in the past few years. Lake Forest is affiliated with the Associated Colleges of the Midwest. The college has 23 varsity teams that compete in the NCAA Division III Midwest Conference. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Madambakkam lake. 7479bt18f6c1o70z2th4jviwfc7" xml:space="preserve">#REDIRECT Madambakkam Lake

Geographic entities mentioned:
surface_form: madambakkam lake
instance_of: Body of water
countries: India
coordinates: lat: 12.91
lon: 80.165
Beaver Dam Mountains Wilderness. The Beaver Dam Mountains Wilderness is a wilderness area located in northwestern Arizona and southwestern Utah, USA, within the arid Colorado Plateau region. The jagged mountains and gently sloping alluvial plain of the Beaver Dam Mountains straddle the border between the two states.

Geographic entities mentioned:
surface_form: Colorado Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37
lon: -110
At about 1500 BC the karst shifted due to small crustal movements and the islands consolidated into a peninsula. Since then the sea has risen 1.75 m but the peninsula has been surrounded by sediment from the Maeander river and is now land-locked. Sedimentation of the harbor began at about 1000 BC, and by 300 AD Lake Bafa had been created. Economy and Land Use.

Geographic entities mentioned:
surface_form: Lake Bafa
instance_of: Lake
countries: Turkey
coordinates: lat: 37.5013
lon: 27.437
Another Albanian paramilitary organization Albanian National Army (ANA, AKSh) also had former UÇPMB fighters. The group is associated with FBKSh (National Front for Reunification of Albanians), its political wing. The group participated in attacks against Macedonian forces with the NLA. After the NLA disbanded, the ANA later went and operated in the Preševo Valley.

Geographic entities mentioned:
surface_form: Preševo Valley
instance_of: Valley
countries: Serbia
coordinates: lat: 42.3
lon: 21.633333333333
Bell River is a short river in Presque Isle County in the U.S. state of Michigan. Less than long, Bell River is entirely within Presque Isle Township and flows from an unnamed lake into False Presque Isle Harbor at. on Lake Huron approximately north of the city of Alpena. Bell River, along with the unnamed lake, nearly completely separates False Presque Isle from the rest of Presque Isle Township.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
During World War II he was a member of Armia Krajowa and was a soldier during the Warsaw Uprising. Żuławski published music reviews in &quot;Ruch Muzyczny&quot;, &quot;Express Wieczorny&quot;, &quot;Nowa Kultura&quot;. He also composed orchestral, chamber, piano and vocal pieces. He was one of the leading Polish alpinists. He died on Mont Blanc during a rescue action in 1957.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
or is the capital of the Swiss canton of Fribourg and district of La Sarine. Located on both sides of the river Sarine, on the Swiss Plateau, it is a major economic, administrative and educational centre on the cultural border between German-speaking and French-speaking Switzerland. Its Old City, one of the best-maintained in Switzerland, sits on a small rocky hill above the valley of the Sarine.

Geographic entities mentioned:
surface_form: Swiss Plateau
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The sewage is released at the bottom. From 1897 to 1965 in Fribourg there was a long tram network in operation, with the trams replaced from 1949 with the Fribourg trolleybus system. The current bus network is now operated by the &quot;Transports publics fribourgeois&quot;, with connections to Bulle, Avenches, Schmitten, Schwarzenburg and in the tourist region Schwarzsee. Airport.

Geographic entities mentioned:
surface_form: Schwarzsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.665277777778
lon: 7.2805555555556
Spechtenköpfe. Spechtenköpfe is a mountain of Bavaria, Germany.

Geographic entities mentioned:
surface_form: spechtenköpfe
instance_of: Mountain
countries: Germany
coordinates: lat: 47.70395
lon: 12.88395
While Gumlau is not today used as a word to mean social system, many of the ideals described by Leach and others can be found in gumrawng gumtsa or zaw gumsa system. History. The origins of gumlau are described in Kawlu Ma Nawng's 1942 book The History of the Kachins of the Hukawng Valley which describes origin stories occurring 300–400 years before its publication.

Geographic entities mentioned:
surface_form: Hukawng Valley
instance_of: Valley
countries: Myanmar
coordinates: lat: 26.438333333333
lon: 96.558888888889
He was reflected in Durham in 1828. After being unsuccessful in gaining reelection in 1830, he attempted to start a number of businesses. During the 1830s, he also published &quot;An essay descriptive of the quadrupeds of British North America&quot; and another paper on the situation of the salmon in Lake Ontario; these works were well received but did not provide any income.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Gallen. Battle. Albert initially avoided a collision, but then on July 2, 1298 deployed his troops in a strategically favorable position on the &quot;Hasenbühl&quot;, a hill near Göllheim. Göllheim community is located south of Alzey between Kaiserslautern and Worms, near the &quot;Donnersberg&quot; massif.

Geographic entities mentioned:
surface_form: Donnersberg
instance_of: Mountain
countries: Germany
coordinates: lat: 49.625280555556
lon: 7.9147194444444
Rising to, by some counts it is the fifth-highest mountain in Scotland (and the United Kingdom). It is in the western massif of the Cairngorms, standing between Braeriach and Cairn Toul, overlooking An Garbh Choire and the Lairig Ghru pass. It was promoted to Munro status by the Scottish Mountaineering Club's 1997 revision of the tables.

Geographic entities mentioned:
surface_form: Braeriach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.078298
lon: -3.728389
surface_form: Cairn Toul
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.054406
lon: -3.710774
It was promoted to Munro status by the Scottish Mountaineering Club's 1997 revision of the tables. It is usually climbed together with other peaks: if coming from the south it may be climbed with Cairn Toul and The Devil's Point, whilst from the north one must first cross Braeriach. The mountain takes its name from An Lochan Uaine, the lochan lying in the corrie on the north-east side of the peak.

Geographic entities mentioned:
surface_form: The Devil's Point
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.035728
lon: -3.688788
surface_form: braeriach
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.078298
lon: -3.728389
surface_form: cairn toul
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.054406
lon: -3.710774
It was promoted to Munro status by the Scottish Mountaineering Club's 1997 revision of the tables. It is usually climbed together with other peaks: if coming from the south it may be climbed with Cairn Toul and The Devil's Point, whilst from the north one must first cross Braeriach. The mountain takes its name from An Lochan Uaine, the lochan lying in the corrie on the north-east side of the peak.

Geographic entities mentioned:
surface_form: the peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -7.95
lon: -14.35
surface_form: an lochan uaine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.17528
lon: -3.65433
The mountain takes its name from An Lochan Uaine, the lochan lying in the corrie on the north-east side of the peak. It is also sometimes called &quot;The Angel's Peak&quot;, a name allegedly given to it in the 19th century by Alexander Copland, a founding member of the Cairngorm Club, in contrast to the nearby Devil's Point.

Geographic entities mentioned:
surface_form: cairngorm
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.116714
lon: -3.644477
Sgòr an Lochain Uaine. is one of the Cairngorms mountains in the Scottish Highlands. Rising to, by some counts it is the fifth-highest mountain in Scotland (and the United Kingdom). It is in the western massif of the Cairngorms, standing between Braeriach and Cairn Toul, overlooking An Garbh Choire and the Lairig Ghru pass.

Geographic entities mentioned:
surface_form: sgòr an lochain uaine
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.058367
lon: -3.725896
The village and surrounds are geographically closer to Allentown and Bethlehem than to the Schuylkill County seat at Pottsville. Andreas is part of the Lehigh Valley, which has a population of 861,899 and is the 69th most populated metropolitan area in the U.S. Andreas is served by the Mantzville exchanges (386 and 818) in area code 570 and (205) in area code 272.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Gubongsan (North Jeolla). Gubongsan () is a mountain of North Jeolla Province, western South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: gubongsan (north jeolla)
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.923333333333
lon: 127.41638888889
Gubongsan (North Jeolla). Gubongsan () is a mountain of North Jeolla Province, western South Korea. It has an elevation of.

Geographic entities mentioned:
surface_form: gubongsan
instance_of: Mountain
countries: South Korea
coordinates: lat: 35.923333333333
lon: 127.41638888889
Kabiskagami Lake (Ontario). 1j0rxmma9888bplsf1yc0ga3cbr" xml:space="preserve">#REDIRECT Kabiskagami Lake

Geographic entities mentioned:
surface_form: kabiskagami lake (ontario)
instance_of: Lake
countries: Canada
coordinates: lat: 48.6931
lon: -84.5647
Lower Valley, New Jersey. Lower Valley is an unincorporated community located along County Route 513 (High Bridge-Califon Road) in Califon Borough and Lebanon Township of Hunterdon County, New Jersey. It is at the western end of Long Valley, historically known as German Valley, the valley of the South Branch Raritan River south of Schooley's Mountain. History. Settlers came here as early as 1735.

Geographic entities mentioned:
surface_form: Schooley's Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.829166666667
lon: -74.793611111111
Darnsee. Darnsee is a deep lake in Bramsche, Lower Saxony, Germany.

Geographic entities mentioned:
surface_form: darnsee
instance_of: Lake
countries: Germany
coordinates: lat: 52.421388888889
lon: 7.9997222222222
Despite Chile's narrowness, some interior regions may experience wide temperature oscillations and cities such as Lonquimay, may even experience a continental climate. In the extreme northeast and southeast the border of Chile extends beyond the Andes into the Altiplano and the Patagonian plains, giving these regions climate patterns similar to those seen in Bolivia and Argentina respectively.

Geographic entities mentioned:
surface_form: Altiplano
instance_of: Plateau
countries: Bolivia
Peru
Chile
Argentina
coordinates: lat: -16.00358
lon: -69.65332
Mount Bradley is a summit in Siskiyou County, California, in the United States. It is in the Shasta–Trinity National Forest with an elevation of. The peak rises over above City of Dunsmuir, California and the Sacramento River. Though it is entirely surrounded by private land, the summit, which is the site of Forest Service lookout tower, can be reached by way of the Castle Lake Trail.

Geographic entities mentioned:
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 41.227039
lon: -122.383789
surface_form: castle lake
instance_of: Lake
countries: United States
coordinates: lat: 40.5683
lon: -115.398
surface_form: the castle
instance_of: Mountain
countries: United States
coordinates: lat: 46.7577433
lon: -121.7283957
surface_form: the castle
instance_of: Mountain
countries: United States
coordinates: lat: 38.2986188
lon: -111.2640679
Mount Bradley (Siskiyou County, California). Mount Bradley is a summit in Siskiyou County, California, in the United States. It is in the Shasta–Trinity National Forest with an elevation of. The peak rises over above City of Dunsmuir, California and the Sacramento River.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley (siskiyou county, california)
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Mount Bradley (Siskiyou County, California). Mount Bradley is a summit in Siskiyou County, California, in the United States. It is in the Shasta–Trinity National Forest with an elevation of. The peak rises over above City of Dunsmuir, California and the Sacramento River.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Mount Bradley (Siskiyou County, California). Mount Bradley is a summit in Siskiyou County, California, in the United States. It is in the Shasta–Trinity National Forest with an elevation of. The peak rises over above City of Dunsmuir, California and the Sacramento River.

Geographic entities mentioned:
surface_form: shasta
instance_of: Mountain
countries: United States
coordinates: lat: 41.409197222222
lon: -122.19488888889
Guanaco Peak is a mountain located in the North Cascades of southwestern British Columbia, Canada. It is the highest summit of the Anderson River Group, a subset of the North Cascades. It is situated northwest of Coquihalla Summit, and northeast of Vicuna Peak. Precipitation runoff from the peak drains west into headwaters of the East Anderson River, or east into headwaters of the Coldwater River.

Geographic entities mentioned:
surface_form: Vicuna Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.64972
lon: -121.15253
Guanaco Peak. Guanaco Peak is a mountain located in the North Cascades of southwestern British Columbia, Canada. It is the highest summit of the Anderson River Group, a subset of the North Cascades. It is situated northwest of Coquihalla Summit, and northeast of Vicuna Peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: guanaco peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6623
lon: -121.1442
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It is situated northwest of Coquihalla Summit, and northeast of Vicuna Peak. Precipitation runoff from the peak drains west into headwaters of the East Anderson River, or east into headwaters of the Coldwater River. The mountain was named for the guanaco, as part of the animal names theme for several other nearby peaks that were submitted by Philip Kubik of the 1974 first ascent party.

Geographic entities mentioned:
surface_form: coldwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.735
lon: -79.6508
surface_form: coldwater river
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.4681
lon: -84.7881
Guanaco Peak. Guanaco Peak is a mountain located in the North Cascades of southwestern British Columbia, Canada. It is the highest summit of the Anderson River Group, a subset of the North Cascades. It is situated northwest of Coquihalla Summit, and northeast of Vicuna Peak.

Geographic entities mentioned:
surface_form: guanaco peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6623
lon: -121.1442
Climate. Based on the Köppen climate classification, Guanaco Peak is located in the marine west coast climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Cascade Range where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: guanaco peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6623
lon: -121.1442
As a result, the Cascade Mountains experience high precipitation, especially during the winter months in the form of snowfall. Temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Guanaco Peak.

Geographic entities mentioned:
surface_form: guanaco peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.6623
lon: -121.1442
It is situated northwest of Coquihalla Summit, and northeast of Vicuna Peak. Precipitation runoff from the peak drains west into headwaters of the East Anderson River, or east into headwaters of the Coldwater River. The mountain was named for the guanaco, as part of the animal names theme for several other nearby peaks that were submitted by Philip Kubik of the 1974 first ascent party.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain was named for the guanaco, as part of the animal names theme for several other nearby peaks that were submitted by Philip Kubik of the 1974 first ascent party. The mountain's name was officially adopted on February 5, 1976, by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Establishment in Naruohama. The origins of golf in Japan can be traced back over a century to a small private course in Kobe's Rokko mountains. During the Meiji Period, many Europeans and Americans lived in the bay-front foreign settlement in Kobe, introducing various aspects of foreign culture into Japan.

Geographic entities mentioned:
surface_form: Rokko mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 34.777777777778
lon: 135.26388888889
During the Meiji Period, many Europeans and Americans lived in the bay-front foreign settlement in Kobe, introducing various aspects of foreign culture into Japan. The British-born trading merchant Arthur Hesketh Groom (1846–1918) built a summerhouse atop Mt. Rokko, an area he chose for its peace and quiet as a perfect location for social gatherings. There he built a four-hole golf course.

Geographic entities mentioned:
surface_form: Mt. Rokko
instance_of: Mountain
countries: Japan
coordinates: lat: 34.777777777778
lon: 135.26388888889
Kibby Mountain. Kibby Mountain is a mountain located in Franklin County, Maine, about east of the Canada–United States border. Kibby Mountain is flanked to the southeast by Spencer Bale Mountain. Kibby Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
The west side of Kibby Mountain drains into Caribou Flow, then into the South Branch of the Moose River. The southwest end of Kibby Mountain drains into the Middle Branch of Kibby Stream, then into Spencer Stream and the Dead River, another tributary of the Kennebec. The southeast side of Kibby Mountain drains into the West Branch of Spencer Stream.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
The southwest end of Kibby Mountain drains into the Middle Branch of Kibby Stream, then into Spencer Stream and the Dead River, another tributary of the Kennebec. The southeast side of Kibby Mountain drains into the West Branch of Spencer Stream. The Kibby Wind Power Project is located on the mountain.

Geographic entities mentioned:
surface_form: west branch
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
Kibby Mountain. Kibby Mountain is a mountain located in Franklin County, Maine, about east of the Canada–United States border. Kibby Mountain is flanked to the southeast by Spencer Bale Mountain. Kibby Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine.

Geographic entities mentioned:
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
Kibby Mountain is flanked to the southeast by Spencer Bale Mountain. Kibby Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The north side of Kibby Mountain drains into the East Branch of the Moose River, then into the South Branch of the Moose, the Moose River, and the Kennebec River.

Geographic entities mentioned:
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
Kibby Mountain stands within the watershed of the Kennebec River, which drains into the Gulf of Maine. The north side of Kibby Mountain drains into the East Branch of the Moose River, then into the South Branch of the Moose, the Moose River, and the Kennebec River. The west side of Kibby Mountain drains into Caribou Flow, then into the South Branch of the Moose River.

Geographic entities mentioned:
surface_form: kibby mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.4187
lon: -70.5443
The A505 road is crossed as the trail makes its way through open countryside towards Harpenden. The path descends into the Lea Valley, passing under the railway lines before crossing the B653 road. The route now follows the track of a disused railway, the former Luton, Dunstable and Welwyn Junction line.

Geographic entities mentioned:
surface_form: Lea Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69
lon: -0.01
Passing under Ferry Lane A503 road bridge. Close by is the &quot;Ferry Boat Inn&quot; public house and Tottenham Hale station. The path passes under the London Overground Gospel Oak to Barking line and Lea Valley Lines railway bridges as the towpath skirts the West Warwick Reservoir further to the east are the East Warwick Reservoir and the Walthamstow Reservoirs.

Geographic entities mentioned:
surface_form: Walthamstow Reservoirs
instance_of: Group of lakes
countries: United Kingdom
coordinates: lat: 51.58165
lon: -0.05055
Its breeding and nesting habits remain almost entirely unstudied. Distribution. The blue-backed conebill is found along the Andes range from northern to central South America, its northern terminus being Cerro Pintado on the Colombia-Venezuela border and its southern terminus being Cochabamba Department in Bolivia.

Geographic entities mentioned:
surface_form: Cerro Pintado
instance_of: Mountain
countries: Venezuela
Colombia
coordinates: lat: 10.33833333
lon: -72.90416667
Military commander Fernando Rivera y Moncada led the guard, until killed during a civil resistance uprising by Quechan Indians near Yuma Crossing. Argüello and the settlers continued onward to Mission San Gabriel in today's San Gabriel Valley. They founded the Pueblo de Los Angeles beside the Los Angeles River on September 4, 1781. This became present day Los Angeles, California.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
The rocks involved in this fold system are primarily sandstones and shales, with shales from the Bokkeveld Group persisting in valley floors, while the more erosion-resistant sandstones of the Peninsula Formation form the parallel ranges of the Cape Fold Mountains. The highest peak in the range is Seweweekspoortpiek, which reaches 2,325meters.

Geographic entities mentioned:
surface_form: Seweweekspoortpiek
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.382777777778
lon: 21.358888888889
The famous Table Mountain forms part of the Cape Fold Belt, being made up of the local lowest (oldest) strata of the Cape Supergroup, composed predominantly of quartzitic sandstone which forms the impressive, almost vertical cliffs which characterize the mountain and the rest of the range which constitutes the backbone of the Cape Peninsula.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
These sandstones are very hard, and erosion resistant. They therefore form the bulk of mountains and steep cliffs and rugged crags of the Cape Fold Belt, including the upper 600 m of the 1 km high Table Mountain, below which Cape Town is situated. It contains no fossils. The Peninsula formation can be traced from 300 km north of Cape Town (i.e.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The best known defiles are: Meiringspoort, Seweweekspoort, the Tradouws Pass, Kogmanskloof, Garcia's pass, the Gourits River gorge (which does not have a road running through it), and Michell's Pass, which is, however, more V-shaped than the others, but impressive nevertheless. In addition several roads and highways crest the mountains over cols, or go through them via tunnels.

Geographic entities mentioned:
surface_form: Seweweekspoort
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.382777777778
lon: 21.358888888889
The Swartberg Mountains were uplifted along this fault, to such an extent that in the Oudtshoorn region the rocks that form the base of the Cape Supergroup are exposed. These are locally known as the &quot;Cango Group&quot;, but are probably continuous with the &quot;Malmesbury Group&quot; that forms the base of Table Mountain on the Cape Peninsula, and similar outcrops in the Western Cape.

Geographic entities mentioned:
surface_form: Table Mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table mountain
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The degree to which the original Cape Fold mountains (formed during the Carboniferous and early Permian Periods) have been eroded is attested to by the fact that the 1 km high Table Mountain on the Cape Peninsula is a syncline mountain, meaning that it formed part of the bottom of a valley when the Cape Supergroup was initially folded.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
The anticline, or highest elevation of the fold between Table Mountain and the Hottentots-Holland Mountains (1.2 to 1.6 km elevation), on the opposite side of the isthmus connecting the Peninsula to the Mainland, has been eroded away.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
These formations contain no fossils. Today the Klipheuwel Group is exposed in several small patches near Lamberts Bay, Piketberg, and to the south-west of Paarl Rock. The Natal Group, which is similar to the Table Mountain Group (see below), is found in several elongated patches near the coast of the northern Eastern Cape and KwaZulu-Natal.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
A deposit, known as the Peninsula Formation (also often referred to as Table Mountain Sandstone), consisting of thickly layered quartzitic sandstone, with a maximum thickness of 2000 m, was laid down. These sandstones are very hard, and erosion resistant.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
A small patch of Pakhuis tillite occurs on the top of Table Mountain at Maclear's Beacon, but most of the Pakhuis and Cederberg Formations are found as a thin layer (on average only about 60 m thick) in the Peninsula Formation rocks of the more inland mountains to the west of a line between Swellendam and Calvinia.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
In several locations the quartzites below the glacial horizon have been rucked into a series of folds. This is believed to have been caused by the movement of ice ploughing into the underlying unconsolidated sands. A good example of this can be seen on a ridge of rocks near Maclear's Beacon on Table Mountain, close to the edge of the plateau overlooking the Cape Town City Bowl and Table Bay.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Bokkeveld Group. About 400 million years ago (in the early Devonian Period) there was further subsidence of the rift valley floor. This brought about the deposition of deeper-water, fine grained sediments of the Bokkeveld Group. This is in marked contrast to the predominantly sandy sediments of the Table Mountain Group. The Bokkeveld Group consists predominantly mudstones.

Geographic entities mentioned:
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Cape Fold Belt. The Cape Fold Belt (CFB) is a long fold-and-thrust mountain belt along the western and southern coastlines of Western Cape, South Africa.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The Cape Fold Belt formed during the Permian period (300 to 250million years ago) in the late Paleozoic age, affecting the sequence of sedimentary rock layers of the siliciclastic Cape Supergroup with folding and faulted rocks, which were deposited in the Cape Basin in the southwestern corner of South Africa.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The Cape Fold Belt was once part of a larger orogenic belt with other mountain ranges that formed as part of the same tectonic event that originally extended from Argentina, across southern Africa, and into Antarctica.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Although the tops of the original Cape Fold Mountains were eroded away, they eroded much slower than the considerably softer Karoo deposits to the north. Thus the Cape Fold Belt &quot;erupted&quot; from the eroding African landscape to form the parallel ranges of mountains that run for 800 km along the southern and south-western Cape coastline today.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The Falkland Mountain range had probably eroded into relative insignificance by the mid-Jurassic Period, and started drifting to the south-west soon after Gondwana began to break up 150 million years ago, leaving the Cape Fold Belt to edge the southern portion of the newly formed African continent.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The bases of the mountains are usually at or near sea level. Cape Supergroup. The mountains of the Cape Fold Belt are composed of rocks belonging to the Cape Supergroup, which is more extensive than the Fold Belt. The Supergroup is divided into several distinct Groups.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Here the Stellenbosch, Franschhoek, Paarl, Durbanville, Tulbagh and Constantia vineyards have been planted on the weathered Cape Granite and Malmesbury shale soils, which form the basement rocks on which the Cape Supergroup rocks in this region rest. The Bokkeveld Group extends eastwards to Port Alfred (near Grahamstown), approximately 120 km beyond the eastern extent of the Cape Fold Belt.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
The latter forms part of the Karoo Supergroup. Therefore, the Witteberg Group forms the uppermost layer of the Cape Supergroup. It tends to form the most inland outcrops of the Cape Supergroup, and can be traced eastwards as far as the Bokkeveld Group can be traced (i.e. to Port Alfred), about 120 km beyond the Cape Fold Belt.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Their stature, with heights varying from 1000m to 2300m, is mostly due to the weather-resistant rocks of quartzitic sandstone of the Peninsula Group (see above). After the fold mountains had been formed they became buried under sediments derived from the massive Himalaya-sized Falkland Mountains to the south of the Cape Fold Belt.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
After the fold mountains had been formed they became buried under sediments derived from the massive Himalaya-sized Falkland Mountains to the south of the Cape Fold Belt. Sediments eroded from these mountains provided the bulk of the 6 km thick Beaufort sediments in the Karoo Basin, but they also covered the Cape Fold Belt, thereby protecting them from erosion.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
Rivers running off this bulging interior into the seas that were forming around South Africa as Gondwana was breaking up 150 million years ago, eventually encountered rocky ridges as the protective layer over the Cape Fold Belt eroded away, exposing their mountain tops.

Geographic entities mentioned:
surface_form: cape fold belt
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.4
lon: 22
For this reason, and its proximity to mountains (&quot;vynyd&quot; in the poem) R. G. Gruffydd proposed the Cumbrian Derwent as the identity of &quot;Derwennydd&quot;, and this view is now generally accepted. If this is the case, it seems likely that the mentioned in the text refer to Lodore Falls, not actually on the Derwent, but very close to the point where it enters Derwentwater.

Geographic entities mentioned:
surface_form: Derwentwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.583333333333
lon: -3.15
Rajbhandari. Rājbhandāri (राजभण्डारी) is a Newar Chatharīya Srēstha clan residing primarily in Kathmandu Valley and other parts of Nepal. It is said that the Malla king Jayasthiti Malla appointed treasurers to look after the wealth. The king honored them with the title of “Bhandari”. As time passed, the &quot;bhandari&quot; were replaced by the &quot;Raj-bhandari&quot;.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Its eventual area encompassed the three Scottish counties of Aberdeenshire, Banffshire and Moray, with short lengths of line in Inverness-shire and Kincardineshire. Fish from the North Sea ports and whisky from the distilleries of Speyside became important goods traffic.

Geographic entities mentioned:
surface_form: Speyside
instance_of: Valley
countries: United Kingdom
coordinates: lat: 57.45
lon: -3.3
Geography. Matelica lies in an ample valley where the Braccano creek joins the Esino river, dominated by the town from an eastern ravine. The valley, roughly in the north&ndash;south direction, is delimited on the east and west sides by Apennines sub-ranges, whose highest peaks are respectively Mount Gemmo at and Mount San Vicino at, compared to the above sea-level of the city centre.

Geographic entities mentioned:
surface_form: Mount San Vicino
instance_of: Mountain
countries: Italy
coordinates: lat: 43.3318934
lon: 13.06126
Mount Provender. Mount Provender () is a conspicuous rock mountain, 900 m, marking the northwest extremity of the Shackleton Range.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
surface_form: provender
instance_of: Mountain
coordinates: lat: -80.3833
lon: -29.9167
surface_form: mount provender
instance_of: Mountain
coordinates: lat: -80.3833
lon: -29.9167
It was first mapped in 1957 by the Commonwealth Trans-Antarctic Expedition and so named because members of the Commonwealth Trans-Antarctic Expedition established a depot of food and fuel and an airplane camp on the south side of the mountain in 1957 to support sledging parties working in the Shackleton Range.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Mount Provender. Mount Provender () is a conspicuous rock mountain, 900 m, marking the northwest extremity of the Shackleton Range.

Geographic entities mentioned:
surface_form: provender
instance_of: Mountain
coordinates: lat: -80.3833
lon: -29.9167
surface_form: mount provender
instance_of: Mountain
coordinates: lat: -80.3833
lon: -29.9167
Junction Creek. Junction Creek is a creek in southwestern Alberta. It is a tributary of the Sheep River.

Geographic entities mentioned:
surface_form: junction creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 50.60007
lon: -114.7353
The river is only known as the Meese below Aqualate Mere, but its source lies considerably higher via the stream known successively as Dawford Brook, Lynn Brook, Moreton Brook, Back Brook, and Coley Brook, which flows north from its source near the Roman Watling Street (now the A5) just to the east of Weston-under-Lizard until it reaches Aqualate Mere.

Geographic entities mentioned:
surface_form: Aqualate Mere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 52.7812
lon: -2.3392
Kranjska Gora. Kranjska Gora (;) is a town in northwestern Slovenia, on the Sava Dolinka River in the Upper Carniola region, close to the Austrian and Italian borders. It is the seat of the Municipality of Kranjska Gora. The tripoint between Austria, Italy and Slovenia lies on the mountain of Dreiländereck, known as Peč in Slovenia. Name.

Geographic entities mentioned:
surface_form: Dreiländereck
instance_of: Mountain
countries: Austria
Slovenia
Italy
coordinates: lat: 46.522986
lon: 13.714089
Recreation. Kranjska Gora is best known as a winter sports town, being situated in the Julian Alps. It annually hosts an event in the FIS Alpine Ski World Cup series, also known as the Vitranc Cup, for the slalom and giant slalom events. The well-known ski jumping hill Planica is located in the nearby Tamar Valley.

Geographic entities mentioned:
surface_form: Planica
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.476944444444
lon: 13.722222222222
Description. &quot;Codon royenii&quot; is an annual or multi-seasonal herb, reaching up to 1.3 m high. Distribution. &quot;Codon royenii&quot; is found in Namibia and the Northern Cape, from central Namibia to Gordonia through Namaqualand to Loeriesfontein, Biedouw Mountains, and the Tanqua Karoo. Conservation status. &quot;Codon royenii&quot; is classified as &quot;Least Concern&quot;.

Geographic entities mentioned:
surface_form: Biedouw Mountains
instance_of: Valley
countries: South Africa
coordinates: lat: -32.128
lon: 19.3348
The population was 427 as of the 2020 census. It is part of the Baton Rouge metropolitan statistical area. History. Springfield began in the 18th century at one of the northernmost points considered to be navigable on the Natalbany River. Between Springfield and Lake Maurepas, Ponchatoula Creek joins the Natalbany and increases its flow. The town was also connected to the Natchez Trace.

Geographic entities mentioned:
surface_form: Lake Maurepas
instance_of: Lake
countries: United States
coordinates: lat: 30.258027777778
lon: -90.498677777778