Sarmila/GeoWiki-Features huggingface dataset:
The lake and its amenities are accessed from Highway 9. Originally the lake was named &quot;Carlyle Lake&quot; by the first European settlers to the area. In the late 1970s control of the lake was handed over to the White Bear First Nations and at that time the lake was renamed to White Bear (Carlyle) Lake. Water levels. Beaver are not native to Moose Mountain.

Geographic entities mentioned:
surface_form: white bear (carlyle) lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7683
lon: -102.2665
Water levels. Beaver are not native to Moose Mountain. In 1923, two breeding pairs from Hudson Bay, Saskatchewan were brought to nearby Kenosee Lake. The beavers flourished and soon dams were blocking not just inflow creeks to Kenosee, but to White Bear (Carlyle) Lake as well. According to aerial photographs, the surface of White Bear (Carlyle) Lake in 1928 was asl. By 1945, it had dropped to.

Geographic entities mentioned:
surface_form: white bear (carlyle) lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7683
lon: -102.2665
partnered with Moose Mountain Provincial Park to control beavers in and around the park through trapping and by blasting beaver dams. Once again, lake levels began to rise. The eventual goal is to raise Kenosee Lake levels enough so that it flows into White Bear (Carlyle) Lake, which hasn't happened since 1928. Fish species. The most common fish found in the lake is the walleye.

Geographic entities mentioned:
surface_form: white bear (carlyle) lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7683
lon: -102.2665
They moved to a new Gothic cathedral that was designed by architect William H. Parkins in 1870. In 1902, the congregation sold the property to Asa Candler, where he founded the Coca-Cola Company. The current building was built in 1903 using granite from Stone Mountain for $161,000. The current name was adopted in 1968 after the Methodist Church and the Evangelical United Brethren merged.

Geographic entities mentioned:
surface_form: Stone Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.805944444444
lon: -84.145422222222
Quebec Autoroute 19. Autoroute 19, also known as Autoroute Papineau (Papineau Highway), is an autoroute in Quebec. It crosses the Rivière des Prairies via the Papineau-Leblanc Bridge, connecting the borough of Ahuntsic-Cartierville in Montreal and the Duvernay neighbourhood in Laval.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
Tempa, West Virginia. Tempa is an unincorporated community in Summers County, West Virginia, United States. Tempa is northwest of Hinton and east of Alderson. The community probably derives its name from the Vale of Tempe, in Greece.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
History. A post office called Winona has been in operation since 1888. The community was named after Winona, Minnesota, the native home of an area lumberman. The name is also a Sioux word meaning 'first born.'
Geography. Winona is located in the Ozarks of southern Missouri. The city is at the intersection of US Route 60 and Missouri Route 19. The city lies within the Mark Twain National Forest.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
History. Simpson made a preparatory exploration in 1951. A Short Sunderland flying boat landed in Seal Lake and from there Simpson walked across Storstrommen to Queen Louise Land. There he found an ice-free glacial lake that would be a suitable place for landing and he named it Britannia Lake &quot;(Britannia Sø)&quot; after the future expedition.

Geographic entities mentioned:
surface_form: Seal Lake
instance_of: Lake
countries: Greenland
coordinates: lat: 77.075
lon: -20.84
The municipality is located on the right side of the Linth valley. It includes the area from the Linth Canal and Walensee to the &quot;Schlattbach&quot; in the &quot;Netstal&quot;. It consists of the village of Mollis and the hamlets of Beglingen on the Kerenzerberg and the alpine settlement of Mullern. Demographics.

Geographic entities mentioned:
surface_form: Walensee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.116666666667
lon: 9.2
(It is now fourth, having been surpassed by Osaka (1970) and Shanghai (2010).)
Several sites were proposed as the main Expo grounds. One location that was considered was Mount Royal Park, to the north of the downtown core. But it was Drapeau's idea to create new islands in the St. Lawrence river, and to enlarge the existing Saint Helen's Island.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Mokelumne Peak. Mokelumne Peak is a peak in the Mokelumne Wilderness, Sierra Nevada, Amador County, California, consisting of metamorphic and granitic rock. Geology. Mokelumne Peak has the largest body of metamorphic rock in the region, called the Mokelumne Peak roof pendant, extending over an area of.

Geographic entities mentioned:
surface_form: mokelumne peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.53815
lon: -120.094455
Geology. Mokelumne Peak has the largest body of metamorphic rock in the region, called the Mokelumne Peak roof pendant, extending over an area of. These rocks were originally Jurassic or Cretaceous age, but were metamorphosed when plutons of the Sierra Nevada batholith intruded in the Cretaceous. The pendant may be several thousand feet thick.

Geographic entities mentioned:
surface_form: mokelumne peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.53815
lon: -120.094455
surface_form: mokelumne peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.53815
lon: -120.094455
The granite is medium- to coarse-grained porphyritic hornblende-biotite granodiorite, determined by K-Ar dating to be between 91.7 and 99.6 million years old. Thirty mining claims were staked on Mokelumne Peak between 1929 and 1934. Rocks on the east side of the peak contain arsenopyrite, chalcopyrite, and bornite. Samples contained 0.3 grams per ton of gold and 7 grams per ton of silver.

Geographic entities mentioned:
surface_form: mokelumne peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.53815
lon: -120.094455
Marial Bai. Marial Bai is a village in Northern Bahr el Ghazal state, South Sudan. Marial Bai lies between the Magadhik River and Chel or Kuru River, which converge to form the Lol River.

Geographic entities mentioned:
surface_form: Kuru River
instance_of: Watercourse
countries: South Sudan
coordinates: lat: 9.12
lon: 26.95
surface_form: Lol River
instance_of: Watercourse
countries: South Sudan
coordinates: lat: 9.19055556
lon: 29.19666667
Walton River. The Walton River is a tributary of the Cedar River on the Upper Peninsula of Michigan in the United States. It joins the Cedar River at the village of Cedar River, less than from the mouth of the Cedar River in Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The plain of Bonaduz and Rhäzüns also belongs to the Chur Rhine Valley and forms its southern end. The valley is part of the Alpine Rhine natural landscape. Climate. Climatically, the Chur Rhine Valley is one of the warmest and driest regions in the Canton of Grisons. It experiences föhn winds on a large number of days during the year. Language and population.

Geographic entities mentioned:
surface_form: Alpine Rhine
instance_of: Valley
countries: Switzerland
Austria
Liechtenstein
coordinates: lat: 47.07013888888889
lon: 9.483347222222223
Media. Regional daily newspapers in the area are the &quot;Bündner Tagblatt&quot; and &quot;Südostschweiz&quot;. In the Bündner Herrschaft, the local papers are the &quot;Prättigauer und Herrschäftler&quot; and in the southern part of the Bündner Rhine Valley, the &quot;Ruinaulta&quot; (called the &quot;Rhiiblatt&quot; until late 2013).

Geographic entities mentioned:
surface_form: ruinaulta
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.8081
lon: 9.31495
Chur Rhine Valley. The Chur Rhine Valley (, also commonly known as the &quot;Bündner Rheintal&quot;) is that part of Nordbünden through which the Rhine flows from the confluence of Anterior and Posterior Rhine near Reichenau to the cantonal border near Maienfeld and Fläsch. The plain of Bonaduz and Rhäzüns also belongs to the Chur Rhine Valley and forms its southern end.

Geographic entities mentioned:
surface_form: bündner rheintal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
surface_form: chur rhine valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
Chur Rhine Valley. The Chur Rhine Valley (, also commonly known as the &quot;Bündner Rheintal&quot;) is that part of Nordbünden through which the Rhine flows from the confluence of Anterior and Posterior Rhine near Reichenau to the cantonal border near Maienfeld and Fläsch. The plain of Bonaduz and Rhäzüns also belongs to the Chur Rhine Valley and forms its southern end.

Geographic entities mentioned:
surface_form: chur rhine valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
The plain of Bonaduz and Rhäzüns also belongs to the Chur Rhine Valley and forms its southern end. The valley is part of the Alpine Rhine natural landscape. Climate. Climatically, the Chur Rhine Valley is one of the warmest and driest regions in the Canton of Grisons. It experiences föhn winds on a large number of days during the year. Language and population.

Geographic entities mentioned:
surface_form: chur rhine valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
Most of the population speak Bündner German (in Chur the variant of Chur German). In Rhäzüns and especially in Ems they also speak Romansh. In recent years, the settlements of the Chur Rhine Valley have increasingly grown together into an urban region around the central town of Chur. Media. Regional daily newspapers in the area are the &quot;Bündner Tagblatt&quot; and &quot;Südostschweiz&quot;.

Geographic entities mentioned:
surface_form: chur rhine valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
In the Bündner Herrschaft, the local papers are the &quot;Prättigauer und Herrschäftler&quot; and in the southern part of the Bündner Rhine Valley, the &quot;Ruinaulta&quot; (called the &quot;Rhiiblatt&quot; until late 2013). The periodicals, &quot;Terra Grischuna&quot; and &quot;Rheinfluss&quot;, deal with the Chur Rhine Valley in terms of cultural and natural history.

Geographic entities mentioned:
surface_form: chur rhine valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.9774
lon: 9.55725
Distribution. The chub is distributed throughout most of northern Eurasia, it can be found in the rivers flowing into the North, Baltic, northern Black, White, Barents and Caspian Sea basins, the Atlantic basins south to Adour drainage in France and in Great Britain north to 56°, in Scandinavia in southern Finland and southern Sweden north to around Stockholm.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Wharfedale Speakers. Briggs built his first loudspeaker in the cellar of his home in Ilkley in the valley of the River Wharfe known as Wharfedale. Live concert hall demonstrations.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
Baiju returned to the vanguard at Irbil, and crossing the Tigris at Mosul with the help of its emir Badr al-Din Lu'lu', who also provided supplies, headed southwards towards Baghdad. Baiju reached the Nahr Isa canal in mid-January 1258, whereupon his deputy Sughunchaq pushed the advance party to around from the city.

Geographic entities mentioned:
surface_form: Nahr Isa canal
instance_of: Watercourse
Cross diatreme. The Cross diatreme is a diatreme in southeastern British Columbia, Canada, located east of the Rocky Mountain Trench and northeast of Elkford.

Geographic entities mentioned:
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: cross diatreme
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0903
lon: -114.825
Cross diatreme. The Cross diatreme is a diatreme in southeastern British Columbia, Canada, located east of the Rocky Mountain Trench and northeast of Elkford.

Geographic entities mentioned:
surface_form: cross diatreme
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0903
lon: -114.825
Although some of its topography has been carved into U-shaped glacial valleys, it is primarily a byproduct of geologic faulting. The Trench separates the Rocky Mountains on its east from the Columbia Mountains and the Cassiar Mountains on its west. It also skirts part of the McGregor Plateau area of the Nechako Plateau sub-area of the Interior Plateau of British Columbia.

Geographic entities mentioned:
surface_form: McGregor Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 54.3333
lon: -121
surface_form: Nechako Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 54.49979
lon: -126.00334
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
For convenience the Rocky Mountain Trench may be divided into two sections, the Northern Trench (between the Muskwa Ranges and Interior Mountains) and the Southern Trench (between the Continental Ranges and Columbia Mountains), separated by the northeastern portion of the Interior Plateau west of the Hart Ranges.

Geographic entities mentioned:
surface_form: Interior Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 52
lon: -123
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Northern Rocky Mountain Trench. The Northern Rocky Mountain Trench is closely aligned with the Tintina Trench near the British Columbia-Yukon border at 60 degrees north latitude, and the two trenches could arguably be classified as one and the same - or 'extensions' of each other. The Tintina Trench extends further north-westward through the Yukon into Alaska.

Geographic entities mentioned:
surface_form: Tintina Trench
instance_of: Valley
countries: Canada
coordinates: lat: 63.41627
lon: -137.00409
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The Tintina Fault is one of the two major fault zones paralleling the Northern Cordilleran Volcanic Province, the other being the Denali Fault in the Yukon, the U.S. state of Alaska and along the British Columbia Coast. History and accessibility. First Nations have traditionally always travelled the northern Trench.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
Geography. The southern Rocky Mountain Trench comprises approximately one half of the Trench in British Columbia and includes three regions, the Robson Valley, Columbia Valley and East Kootenay (from north to south).

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
surface_form: Columbia Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.0333
lon: -116.617
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
West of Donald BC, the Beaver river flows in from the south - but it represents the intersection of the lesser but impressive feature called the Purcell Trench. The Purcell Trench as it proceeds southward becomes the valley of the Duncan River and Duncan and Kootenay Lakes.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Rocky Mountain Trench. The Rocky Mountain Trench, also known as the Valley of a Thousand Peaks or simply the Trench, is a large valley on the western side of the northern part of North America's Rocky Mountains.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Despite differences in timing and faulting styles of the northern and southern portions, they were aligned with each other because faulting for both was controlled by a pre-existing, west-facing, deep basement ramp with over of vertical offset. Northern Rocky Mountain Trench.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Geology. Right-lateral strike-slip movement of the Tintina Fault on the Tintina-Northern Rocky Mountain Trench may have begun during the middle Jurassic. The fastest rates of slip probably occurred during two pulses in the middle Cretaceous and early Cenozoic, respectively, with the latter probably occurring during the Eocene.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
In the context of plate tectonics, strike-slip movement of the Tintina Fault on the Tintina-Northern Rocky Mountain Trench is also related to strike-slip movement along the San Andreas Fault, the extension of the Basin and Range Province, and other extensional or strike-slip fault systems in western North America.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The B route favors the Trench option. The C route following the airfields east of the Rocky Mountains and then crossing to the west near the Liard River is the chosen route. 1942 - March 28 the American government initiates a highly secret survey. It was undertaken for the purpose of assessing a military railway link up the Northern Rocky Mountain Trench. It was completed on Sept 28.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Nov 15 US General Somervell declines to proceed with a military railway. Canada's Major Charles presents drawings for the Northern Trench portion of a railway from Ware to Lower Post of, $112,000,000 cost, with 17,000 personnel over 400 days. Of the 1217 total miles of proposed railway to Alaska, 530 are on Canadian soil and lie within the Northern Rocky Mountain Trench or the Tintina Trench.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
1999 - Karsten Heuer completes the final section of the Y2Y hike (Yellowstone to Yukon) at Lower Post
2000 - Extension of the Muskwa-Kechika Management Area into the Northern Trench. Much of the Northern Rocky Mountain Trench's furthest reach is within this British Columbia Protected Area.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Discussions among feasibility experts still do not seem to favor the B Route despite it being lower, more direct, fewer major river crossings and considerably less snow. Geology. The Southern Rocky Mountain Trench was created mainly by Cenozoic-aged extension (normal faulting). What little strike-slip movement that is found in the southern trench is not considered significant.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The extensional faulting was nonetheless substantial, having extended as deep as. The southern trench also differs from the northern trench in that it is more sinuous and is asymmetrical in cross-section (perpendicular to its length). The western side of the Southern Rocky Mountain Trench is more subdued and irregular than the east side.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The western side of the Southern Rocky Mountain Trench is more subdued and irregular than the east side. During late Paleozoic to Mesozoic time, rapid sediment deposition and subsidence to the west transitioned in the area of the modern Rocky Mountain Trench into a stable continental shelf in the east.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The Nevadan Orogeny destroyed the western wedge of sedimentary rocks during Jurassic to middle Cretaceous time, thrusting them up into metamorphic fold belts. Currently, strata on either side of the Southern Rocky Mountain Trench consist mainly of Precambrian and Paleozoic metasedimentary and sedimentary rocks. Within the trench are unconsolidated Cenozoic sandstones and conglomerates.

Geographic entities mentioned:
surface_form: rocky mountain trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Lake Kipawa. Lake Kipawa (in French: &quot;Lac Kipawa&quot;) is a lake in far south-west Quebec, Canada, near the border with Ontario, north of Témiscaming, Quebec. Also see Kipawa River which is the only natural outflow of Kipawa Lake, Gordon Creek in Témiscaming on the south end being artificial.

Geographic entities mentioned:
surface_form: lake kipawa
instance_of: Lake
countries: Canada
coordinates: lat: 46.8847
lon: -78.9678
Lake Kipawa. Lake Kipawa (in French: &quot;Lac Kipawa&quot;) is a lake in far south-west Quebec, Canada, near the border with Ontario, north of Témiscaming, Quebec. Also see Kipawa River which is the only natural outflow of Kipawa Lake, Gordon Creek in Témiscaming on the south end being artificial.

Geographic entities mentioned:
surface_form: lake kipawa
instance_of: Lake
countries: Canada
coordinates: lat: 46.8847
lon: -78.9678
surface_form: lac kipawa
instance_of: Lake
countries: Canada
coordinates: lat: 46.8847
lon: -78.9678
Also see Kipawa River which is the only natural outflow of Kipawa Lake, Gordon Creek in Témiscaming on the south end being artificial. Lake Kipawa is currently the source of debate among Innergex and Hydro Quebec concerning water rights for their competing hydro electric projects.

Geographic entities mentioned:
surface_form: lake kipawa
instance_of: Lake
countries: Canada
coordinates: lat: 46.8847
lon: -78.9678
Bordering the lake are the communities of Kipawa, Laniel, and the Keboawek Reserve. The lake is popular with fishermen for its walleye and northern pike abundance, as well as a supply of trout. Various lodges (such as Kipawa Lodge which is located at Edward's Narrows and Alwaki Lodge, which is located on Thompson Island) bordering the lake offer hunting and fishing tours and accommodations.

Geographic entities mentioned:
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
From 2020 onwards she has been invoked by some citizens of Palermo to protect the city from COVID-19. Life. Rosalia was born of a Norman noble family that claimed descent from Charlemagne. Devoutly religious, she retired to live as a hermit in a cave on Mount Pellegrino, where she died alone in 1166. Tradition says that she was led to the cave by two angels.

Geographic entities mentioned:
surface_form: Mount Pellegrino
instance_of: Mountain
countries: Italy
coordinates: lat: 38.17
lon: 13.351388888889
Mont Orohena. Mont Orohena is a mountain located in the South Pacific, on the island of Tahiti. With an elevation of above sea level, it is the highest point of French Polynesia. Mont Orohena is an extinct shield volcano and ranks 7th in the world for topographic isolation.

Geographic entities mentioned:
surface_form: orohena
instance_of: Mountain
countries: France
coordinates: lat: -17.623055555556
lon: -149.47694444444
surface_form: mont orohena
instance_of: Mountain
countries: France
coordinates: lat: -17.623055555556
lon: -149.47694444444
Paula V. Welander. Paula Veronica Welander is a microbiologist and professor at Stanford University who is known for her research using lipid biomarkers to investigate how life evolved on Earth. Early life and career. Welander was born and raised in the San Fernando Valley, California. Her mother and father immigrated from Mexico to Los Angeles in the early 1970's.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Hall Peak. Hall Peak () is a peak, high, in the Heritage Range of Antarctica, surmounting the dividing ridge at the upper reaches of Rennell Glacier, Schmidt Glacier and Larson Valley. It was named by the University of Minnesota Geological Party to these mountains in 1963–64 for Walter D. M. (Mike) Hall, a geologist with the party.

Geographic entities mentioned:
surface_form: Larson Valley
instance_of: Valley
coordinates: lat: -79.5333
lon: -83.85
surface_form: hall peak
instance_of: Mountain
coordinates: lat: -79.4833
lon: -83.75
Hall Peak. Hall Peak () is a peak, high, in the Heritage Range of Antarctica, surmounting the dividing ridge at the upper reaches of Rennell Glacier, Schmidt Glacier and Larson Valley. It was named by the University of Minnesota Geological Party to these mountains in 1963–64 for Walter D. M. (Mike) Hall, a geologist with the party.

Geographic entities mentioned:
surface_form: hall peak
instance_of: Mountain
coordinates: lat: -79.4833
lon: -83.75
Thin drapes of Tapeats Sandstone of the Tonto Group now cover most of these ancient monadnocks. However, a few of these monadnocks protrude further up into the Bright Angel Shale (Isis Temple prominence example). These monadnocks served locally as sources of coarse-grained sediments that accumulated during the marine transgression to form the Tonto Group. Fossils.

Geographic entities mentioned:
surface_form: Isis Temple
instance_of: Mountain
countries: United States
coordinates: lat: 36.1408
lon: -112.138
It is a satellite lake of Lake Kyoga, which it drains into, and the two are to some extent directly connected by papyrus swamps. During the high-water rainy season, Lake Bisina can be up to deep and often directly connects with the smaller Lake Opeta, but during the dry season the two are clearly separated. Conservation and ecology.

Geographic entities mentioned:
surface_form: Lake Opeta
instance_of: Lake
countries: Uganda
coordinates: lat: 1.7
lon: 34.23333333
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
Lake Bisina. Lake Bisina, also known as Lake Salisbury and Lake Bisinia, is a freshwater lake in eastern Uganda. It is a satellite lake of Lake Kyoga, which it drains into, and the two are to some extent directly connected by papyrus swamps.

Geographic entities mentioned:
surface_form: lake salisbury
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
Lake Bisina. Lake Bisina, also known as Lake Salisbury and Lake Bisinia, is a freshwater lake in eastern Uganda. It is a satellite lake of Lake Kyoga, which it drains into, and the two are to some extent directly connected by papyrus swamps.

Geographic entities mentioned:
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
Conservation and ecology. Lake Bisina is one of Uganda's 33 Important Bird Areas and since 2006 a Ramsar-listed wetland of international importance. The lake is important for fish, notably several threatened haplochromine cichlids like &quot;Haplochromis orthostoma&quot;, &quot;H. argenteus&quot; (appears to have disappeared from its main range in Lake Victoria), &quot;H.

Geographic entities mentioned:
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
maxillaris&quot;, &quot;H. nubilus&quot;, &quot;H. parvidens&quot;, &quot;H. phytophagus&quot; and a number of undescribed species. Although Nile perch was introduced to Lake Bisina in the early 1970s, recent surveys have not detected this species, which has been implicated in the extinctions of many haplochromine cichlids elsewhere.

Geographic entities mentioned:
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
Although Nile perch was introduced to Lake Bisina in the early 1970s, recent surveys have not detected this species, which has been implicated in the extinctions of many haplochromine cichlids elsewhere. A few tilapia species have also been introduced to Lake Bisina and they are still present, along with the native Singida and Victoria tilapias.

Geographic entities mentioned:
surface_form: lake bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
surface_form: bisina
instance_of: Lake
countries: Uganda
coordinates: lat: 1.60777778
lon: 33.96194444
Little Harbor, Michigan. Little Harbor is a former settlement in Schoolcraft County, Michigan, United States, on the north shore of Lake Michigan. Little Harbor was located between Garden and Thompson on the Garden Peninsula. It was a steam powered sawmill town founded between 1885 and 1887 by Alfred Tracy and William L.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Gränna. Gränna () is a locality in Jönköping Municipality, Jönköping County, Sweden with 2,665 inhabitants in 2018. Founded in 1652 by Count Per Brahe, it is in Småland on the eastern shores of the lake Vättern, about 40 km north of Jönköping. History and academic development. The town is at the foot of Gränna mountain and is characterized by its steep streets and old wooden houses.

Geographic entities mentioned:
surface_form: Vättern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.4
lon: 14.6
Lake Vatten. Vättern(Swedish: &quot;Vatten Sjö&quot;) is a picturesque freshwater lake located in the southern part of Sweden. Known for its clear waters and serene surroundings, Lake Vatten is a popular destination for outdoor enthusiasts, offering activities such as boating, fishing, and hiking.

Geographic entities mentioned:
surface_form: Vättern
instance_of: Lake
countries: Sweden
coordinates: lat: 58.4
lon: 14.6
Etymology. The name Lower Philipstown is derived from Philipstown, the former name of Daingean. Location. Lower Philipstown is located in northeast County Offaly and contains Croghan Hill and part of the Bog of Allen. History. Lower Philipstown was roughly formed from the ancient tuaths; Tuath Rátha Droma and Tuath Cruacháin of the Uí Failge (O'Connor Faly).

Geographic entities mentioned:
surface_form: Croghan Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.2
lon: -7.16
History. Lower Philipstown was roughly formed from the ancient tuaths; Tuath Rátha Droma and Tuath Cruacháin of the Uí Failge (O'Connor Faly). Ó hAonghusa (O'Hennessy) alongside Ó hUallacháin (O'Houlihan) are cited here as chiefs of Clan Colgan, near Croghan Hill. The original Philipstown barony was split into upper and lower by 1807.

Geographic entities mentioned:
surface_form: Croghan Hill
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.2
lon: -7.16
Sengge Zangbo. Sengge Khabab () or Shiquan He () is a river in the Ngari Prefecture in the Tibet Autonomous Region, China that is the source stream of the Indus River, one of the major trans-Himalayan rivers of Central and South Asia. The river rises in the mountain springs north of the Manasarovar lake, and downstream joins the Gar Tsangpo river near the village of Tashigang.

Geographic entities mentioned:
surface_form: Gar Tsangpo
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 32.49348
lon: 79.68701
The town of Shiquanhe, the administrative headquarters of the Ngari Prefecture, is located in the lower valley of Sengge Zangbo, and is named after the river. The Sengge Zangbo drains an area of, and covers a length of. Main tributaries include Gar Tsangpo. Other tributaries include the Langqu River, the Chizuo Tsangpo River, and the Charinongqu River.

Geographic entities mentioned:
surface_form: Gar Tsangpo
instance_of: Watercourse
countries: People's Republic of China
coordinates: lat: 32.49348
lon: 79.68701
Improvised river crossings were conducted at the Blackwater and Dry Fork Rivers, among others. Both Seneca Rocks and the Blackwater Canyon were utilized for mountain climbing instruction. In July 1943 a detachment from Camp Hale, Colorado, instituted high-angle rock and assault climbing instruction at Seneca Rocks. Approximately 180 soldiers cycled through this course every 2 weeks.

Geographic entities mentioned:
surface_form: Seneca Rocks
instance_of: Landform
countries: United States
coordinates: lat: 38.8347
lon: -79.3661
The name itself means the &quot;bottom [end] of the Lysefjorden&quot;. It's a destination for over 100,000 tourists annually, and it is an access point for the Kjerag mountain, a popular Base Jumping spot. There are cruises and an express boat to Lysebotn from Skagenkaien in the city of Stavanger, Lauvvik in Sandnes, and the village of Forsand.

Geographic entities mentioned:
surface_form: Kjerag
instance_of: Mountain
countries: Norway
coordinates: lat: 59.033055555556
lon: 6.5958333333333
The road was opened in 1984 and it is open only in the summer, when it is ice free and safe. The road has its highest point at above sea level. At the top of the turns is Øygardstølen which has a parking lot, food service, and a service building for hiking trips to the nearby Kjerag mountain, Kjeragbolten boulder, and Kjeragfossen waterfall.

Geographic entities mentioned:
surface_form: Kjerag
instance_of: Mountain
countries: Norway
coordinates: lat: 59.033055555556
lon: 6.5958333333333
surface_form: Kjeragbolten
instance_of: Mountain
countries: Norway
coordinates: lat: 59.0337269
lon: 6.5932748
The area is. The lowlands surrounding the steep-sided plateau average about in elevation above sea level while the top of the massif has an average elevation of about with a maximum elevation of at Grand Veymont. Unlike a flat-topped mesa, three ridges run along the top of the massif from north to south.

Geographic entities mentioned:
surface_form: Grand Veymont
instance_of: Mountain
countries: France
coordinates: lat: 44.87
lon: 5.526944
Parququcha (Peru). Parququcha (Quechua &quot;parquy&quot; irrigation, &quot;qucha&quot; lake, &quot;irrigation lake&quot;, hispanicized spelling &quot;Parccoccocha&quot;) is a lake in Peru located in the Ayacucho Region, Parinacochas Province, Coracora District. It is situated at a height of about.

Geographic entities mentioned:
surface_form: parququcha (peru)
instance_of: Lake
countries: Peru
coordinates: lat: -14.651666666667
lon: -73.694444444444
Parququcha (Peru). Parququcha (Quechua &quot;parquy&quot; irrigation, &quot;qucha&quot; lake, &quot;irrigation lake&quot;, hispanicized spelling &quot;Parccoccocha&quot;) is a lake in Peru located in the Ayacucho Region, Parinacochas Province, Coracora District. It is situated at a height of about.

Geographic entities mentioned:
surface_form: parccoccocha
instance_of: Lake
countries: Peru
coordinates: lat: -14.651666666667
lon: -73.694444444444
surface_form: parinacochas
instance_of: Lake
countries: Peru
coordinates: lat: -15.3
lon: -73.7
They crossed the Sahara carrying a boat on the backs of camels, splitting up in 1851 with Overweg trekking by route of Zinder to Kukawa. After 18 months of exploring the Adamawa Emirate, Benue River, and finally completing his most notable feat of circumnavigating Lake Chad, he died of an unknown illness in Maduari after swimming in cold waters. Barth and Overweg were close friends.

Geographic entities mentioned:
surface_form: Benue River
instance_of: Watercourse
countries: Cameroon
Nigeria
coordinates: lat: 7.783333
lon: 6.766667
The latter's death took place after his recognition as bailiff of Loch Awe and Ardscotnish by Edward in September 1296, suggesting that he too was employed by the English against Clann Dubhghaill. Accordingly, both Alasdair Óg and Cailéan Mór appear to have succumbed to Clann Dubhghaill whilst attempting to extend Edward's authority into Argyll and bring the clan to heel.

Geographic entities mentioned:
surface_form: Loch Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291475
lon: -5.231141
Goldkenn is part of the Choco-Diffusion group since 2010. It moved from Geneva to Le Locle in 2011. In 2014, the campaign for the Save our Swiss Gold initiative, calling on the Swiss National Bank to maintain minimum gold reserves, was launched. The supporters of the initiative displayed a pile of Goldkenn bullion replicas at the press conference. The Goldkenn logo features the Matterhorn.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
Inn (river). The Inn (;;) is a river in Switzerland, Austria and Germany. The long river is a right tributary of the Danube, being the third largest tributary of the Danube by discharge. The highest point of its drainage basin is the summit of Piz Bernina at. The Engadine, the valley of the En, is the only Swiss valley whose waters end up in the Black Sea (via the Danube). Etymology.

Geographic entities mentioned:
surface_form: Piz Bernina
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.382388888889
lon: 9.9081111111111
Inn (river). The Inn (;;) is a river in Switzerland, Austria and Germany. The long river is a right tributary of the Danube, being the third largest tributary of the Danube by discharge. The highest point of its drainage basin is the summit of Piz Bernina at. The Engadine, the valley of the En, is the only Swiss valley whose waters end up in the Black Sea (via the Danube). Etymology.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
The mentions in Roman times refer to the lower course. The Tyrolean section was first called Aenus by Venantius Fortunatus in the 6th century. The name Engadin and the Romansh name &quot;En&quot; indicate that the upper reaches of the river have always been called this way.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
A connection may exist between the name Inn and the name of the French river Ain. Geography. The source of the Inn is located in the Swiss Alps, west of St. Moritz in the Engadine region, which is named after the river (Romansh &quot;Engiadina&quot;; Latin &quot;vallis Eniatina&quot;).

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
Geography. The source of the Inn is located in the Swiss Alps, west of St. Moritz in the Engadine region, which is named after the river (Romansh &quot;Engiadina&quot;; Latin &quot;vallis Eniatina&quot;). Shortly after it leaves its source, the Inn flows through the largest lakes on its course, Lake Sils and Lake Silvaplana.

Geographic entities mentioned:
surface_form: Lake Sils
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 9.7333333333333
surface_form: Lake Silvaplana
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.45
lon: 9.7944444444444
The most important crops are rice and tobacco, while other important agricultural products are peanuts and cassava. Additionally fishing employs 5% of the population. Rivers. Maevatanana lies between the Ikopa River & the Betsiboka River. Secondary rivers are the Menavava, Mandrava, Andriantoany, Nandronjia and the Isinko river. Mining.

Geographic entities mentioned:
surface_form: Ikopa River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -16.798611111111
lon: 46.855555555556
surface_form: Betsiboka River
instance_of: Watercourse
countries: Madagascar
coordinates: lat: -18.35868
lon: 47.485374
Distribution and habitat. It is native to temperate Europe. Range. It is found in Greece, on Peloponnese (a peninsula and geographic region in southern Greece), on the slopes of Ziria, Mount Saito (near Mount Oligyrtos and Mount Helmos. Habitat. It grows on the limestone rocky mountain slopes and clearings, between clumps of &quot;Abies cephalonica&quot; (or Greek Fir) forest.

Geographic entities mentioned:
surface_form: Ziria
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
surface_form: Mount Oligyrtos
instance_of: Mountain
countries: Greece
coordinates: lat: 37.807
lon: 22.387
He was very hospitable at Seton Palace, where James VI and Anne of Denmark, and ambassadors and strangers of quality were nobly entertained. Anne of Denmark came to Seton Palace in a litter in 1597 and planned to make an excursion to the Bass Rock.

Geographic entities mentioned:
surface_form: Bass Rock
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.08
lon: -2.64
Education. Welcome Bay has two state primary schools for Year 1 to 6 students: Welcome Bay School, with a roll of, and Selwyn Ridge School, with a roll of. Welcome Bay School opened in 1979 because Maungatapu School was under pressure from its growing roll. Selwyn Ridge opened in 1997. Tauranga Waldorf School is a state-integrated primary school for Year 1 to 8 students, with a roll of.

Geographic entities mentioned:
surface_form: Maungatapu
instance_of: Mountain
countries: New Zealand
coordinates: lat: -41.323
lon: 173.415
Omega Peak. Omega Peak is located on the border of Alberta and British Columbia, between the head of the Sullivan River and Columbia Icefield. It was named in 1939 because it was the last unclimbed peak over between the Thompson and Yellowhead Passes.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: omega peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1283
lon: -117.578
Omega Peak. Omega Peak is located on the border of Alberta and British Columbia, between the head of the Sullivan River and Columbia Icefield. It was named in 1939 because it was the last unclimbed peak over between the Thompson and Yellowhead Passes.

Geographic entities mentioned:
surface_form: omega peak
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1283
lon: -117.578
Matsue is the capital and largest city of Shimane Prefecture, with other major cities including Izumo, Hamada, and Masuda. Shimane Prefecture contains the majority of the Lake Shinji-Nakaumi metropolitan area centered on Matsue, and with a population of approximately 600,000 is Japan's third-largest metropolitan area on the Sea of Japan coast after Niigata and Greater Kanazawa.

Geographic entities mentioned:
surface_form: Lake Shinji
instance_of: Lake
countries: Japan
coordinates: lat: 35.45
lon: 132.96666666667
surface_form: Nakaumi
instance_of: Lake
countries: Japan
coordinates: lat: 35.466666666667
lon: 133.2
Another major landform is the Shimane peninsula. The peninsula is located across the Sea of Japan from Izumo to Sakaiminato, which is located in Tottori prefecture. Also, the peninsula created two brackish lakes, Lake Shinji and Nakaumi. The island of Daikon is located in Nakaumi. Off the main island of Honshū, the island of Oki belongs to Shimane prefecture as well.

Geographic entities mentioned:
surface_form: Lake Shinji
instance_of: Lake
countries: Japan
coordinates: lat: 35.45
lon: 132.96666666667
surface_form: Nakaumi
instance_of: Lake
countries: Japan
coordinates: lat: 35.466666666667
lon: 133.2
Morven, Georgia. Morven is a city in Brooks County, Georgia, United States. It is part of the Valdosta metropolitan statistical area. The city was named after a mountain in Scotland. The population was 565 at the 2010 census, and 506 in 2020. It was formerly known as Sharpe's Store. History. Morven is the oldest community established by Europeans in Brooks County.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 58.233888888889
lon: -3.6977777777778
Whitmer Peninsula. The Whitmer Peninsula () is a broad ice-capped peninsula, about long and wide, between Cheetham Ice Tongue and Harbord Glacier Tongue on the coast of Victoria Land, Antarctica. Location. The Whitmer Peninsula is on the west coast of the Ross Sea. Kohler Head is on its northeast coast.

Geographic entities mentioned:
surface_form: Cheetham Ice Tongue
instance_of: Landform
coordinates: lat: -75.75
lon: 162.91666667
Location. The Whitmer Peninsula is on the west coast of the Ross Sea. Kohler Head is on its northeast coast. It is south of the Cheetham Ice Tongue and Lamplugh Island, east of the Davis Glacier and north of the Harbord Glacier, which flows between Starr Nunatak and Varney Nunatak into the sea, where it forms the Harbord Glacier Tongue. Exploration and naming.

Geographic entities mentioned:
surface_form: Cheetham Ice Tongue
instance_of: Landform
coordinates: lat: -75.75
lon: 162.91666667
Kohler, United States Navy, construction electrician at McMurdo Station, 1965-66 and 1966-67. Harbord Glacier. A glacier flowing along the south side of Mount George Murray. It enters the Ross Sea south of Whitmer Peninsula where it forms Harbord Glacier Tongue. The name derives from the glacier tongue, which was named by Ernest Shackleton for A.E.

Geographic entities mentioned:
surface_form: Mount George Murray
instance_of: Mountain
coordinates: lat: -75.9
lon: 161.833
The tradition covers Alaska, and expands far into the east, west, and the Southwest Yukon Territory of Canada. The Upward Sun River site, a Late Pleistocene archaeological site associated with the Paleo-Arctic Tradition, located in the Tanana Valley, Alaska has now been dated to around 11,500 BP. Upward Sun River is the site of the oldest human remains discovered on the American side of Beringia.

Geographic entities mentioned:
surface_form: Tanana Valley
instance_of: Valley
countries: United States
coordinates: lat: 64.4
lon: -147
Background. As the main Allied contingent retreated from German forces towards the south of Greece, a holding action was determined to be needed to delay the pursuing Germans at Tempe Gorge, a site deemed suitable for the defence. The force allocated for this action was dubbed &quot;Anzac Force&quot;.

Geographic entities mentioned:
surface_form: Tempe Gorge
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667