Sarmila/GeoWiki-Features huggingface dataset:
The only other river to do so is the Kootenay, just to the north. The Rocky Mountain Trench runs across the northeast part of the watershed, through the Flathead Valley, and eventually terminating in mountains near the Clark Fork's confluence with the Flathead. Tributaries. The Pend Oreille River starts in northern Idaho, at Lake Pend Oreille, Idaho's largest lake.

Geographic entities mentioned:
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
The second one blocked the upper Pend Oreille River near Sandpoint, creating an enlarged Lake Pend Oreille that could have connected with a similarly enlarged Kootenay Lake in the north. Water pressure and glacial melt destroyed the larger of the two ice dams several times, causing massive amounts of water to rush out across eastern Washington through the upper Pend Oreille River.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Both tribes lived around the area of Lake Pend Oreille occasionally ranging lower onto the Pend Oreille River (or maybe they did have settlements along the river?) but the lower (north) basin was generally less populated than the upper (south) portion. The Flathead tribe inhabited the upper (Clark Fork) part of the basin, especially the Bitterroot Valley.

Geographic entities mentioned:
surface_form: Bitterroot Valley
instance_of: Valley
countries: United States
coordinates: lat: 46.247
lon: -114.16
Canadian explorer David Thompson saw the river in 1807, after a long and arduous journey from Saskatchewan. His primary mission was to find the source of the Columbia River (Columbia Lake), which he did. Afterwards he proceeded to establish trading posts throughout the region, including Kullyspell House on the north shore of Lake Pend Oreille.

Geographic entities mentioned:
surface_form: Columbia Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.230555555556
lon: -115.85333333333
In the 1920s, there was a proposal to divert the Pend Oreille through a gravity canal to irrigate the Grand Coulee and surrounding lands in eastern Washington as part of the tentative Columbia Basin Project. These plans were later dropped with the construction of Grand Coulee Dam and a pumping plant on the Columbia River. Names.

Geographic entities mentioned:
surface_form: Grand Coulee
instance_of: Valley
countries: United States
coordinates: lat: 47.62
lon: -119.308
Glen River (Chaudière River tributary). The Glen River (&quot;in French: rivière Glen&quot;) is a tributary of the west bank of the Chaudière River which flows north to empty onto the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
surface_form: rivière glen
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.62139
lon: -70.85639
Glen River (Chaudière River tributary). The Glen River (&quot;in French: rivière Glen&quot;) is a tributary of the west bank of the Chaudière River which flows north to empty onto the south bank of the St. Lawrence River.

Geographic entities mentioned:
surface_form: glen river (chaudière river tributary)
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.62139
lon: -70.85639
Mount Hatsuka. is a 524.0 meter high Japanese mountain in Sanda, Hyōgo, Japan. Another name of this mountain is Mount Koge. Mount Hatsuka is an independent peak in Tamba Highland. This mountain is on a popular picnic course from Dojo Station to Kozuki Bus Stop of Shinki Bus. On the top of the mountain, Hatsuka Shrine is extant. History.

Geographic entities mentioned:
surface_form: mount hatsuka
instance_of: Mountain
countries: Japan
coordinates: lat: 34.916666666667
lon: 135.26666666667
In 2008, the Long Lake Dam was rebuilt and modernized. The dam was built in 1930 and reinforced in 1968 and 2008. The Long Lake Dam allows the control of water flowing from Long Lake to Fox Lake and allows pleasure boat traffic from Long Lake to the rest of the Chain O'Lakes. Transportation. Ingleside is served by Metra commuter train's Milwaukee District North Line connecting to downtown Chicago.

Geographic entities mentioned:
surface_form: Chain O'Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.4
lon: -88.133333333333
Salmo fibreni. &quot;Salmo fibreni&quot;, or the Fibreno trout, is a freshwater salmonid fish, endemic to Lago di Posta Fibreno in central Italy. The size of Lago di Posta Fibreno is only 0.29 km². It is a narrow lake 1.1 km long, 100–300 m wide, situated 289 m above sea level. The lake is in a karstic terrain and rich in underwater springs.

Geographic entities mentioned:
surface_form: Lago di Posta Fibreno
instance_of: Lake
countries: Italy
coordinates: lat: 41.699801
lon: 13.686304
Spring Lake (Waushara County, Wisconsin). Spring Lake is a lake in Waushara County, Wisconsin, in the United States. Spring Lake was named from the many springs which flow into the lake.

Geographic entities mentioned:
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 28.0381
lon: -81.7351
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.76083333
lon: -92.96277778
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.700833333333
lon: -93.473888888889
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.719669
lon: -83.392527
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.325555555556
lon: -74.964444444444
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 44.0111458
lon: -89.1607253
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 47.43638888888889
lon: -122.08888888888889
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 45.3667276
lon: -88.9628259
surface_form: spring lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6536
lon: -73.4215
Seeweidsee. Seeweidsee is a lake in the municipality of Hombrechtikon, in the Canton of Zurich, Switzerland. Its surface area is. Lake has grass floating mat at it shores.

Geographic entities mentioned:
surface_form: seeweidsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.256944444444
lon: 8.7461111111111
Peters&quot;) is a small incorporated village located on Cape Breton Island in Richmond County, Nova Scotia, Canada. This village is located on a narrow isthmus which separates the southern end of Bras d'Or Lake, known as St. Peter's Inlet, to the north from St. Peter's Bay on the Atlantic Ocean to the south. The isthmus is crossed by the St.

Geographic entities mentioned:
surface_form: Bras d'Or Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.860277777778
lon: -60.778888888889
At the end of the 1880s, Fuchs acquired the Conservatory originally founded by Wilhelm Freudenberg and bankrupt under Otto Taubmann in Wiesbaden and moved from the &quot;Saxon Nice&quot; on the Elbe to the &quot;Nice of the North&quot; on the Main.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The term &quot;neutral ground&quot; underwent broadening in the local lexicon, and now refers to medians in general. The city was for years divided into Downtown and Uptown. Development of the low-lying Back of Town (the swamp and marsh extending northwards from the edge of development to the shores of Lake Pontchartrain) only began after 1900, as longstanding drainage issues were solved.

Geographic entities mentioned:
surface_form: Lake Pontchartrain
instance_of: Lake
countries: United States
coordinates: lat: 30.188888888889
lon: -90.101388888889
Uven Spur. Uven Spur () is a small rock spur just southwest of Tunga Spur, extending from the Kirwan Escarpment in Queen Maud Land, Antarctica. It was mapped by Norwegian cartographers from surveys and air photos by Norwegian-British-Swedish Antarctic Expedition (NBSAE) (1949–52) and additional air photos (1958–59), and named Uven.

Geographic entities mentioned:
surface_form: Kirwan Escarpment
instance_of: Landform
coordinates: lat: -73.4167
lon: -3.5
Williams was also responsible for suggesting the singing of the Welsh national anthem in a match in 1905, the first time a national anthem was sung before a sporting event. Williams was born in Llwynypia into a farming community in the Rhondda Valley and in his early years he lived in at the Tonypandy Inn. A solicitor by trade, he trained for his profession in Pontypridd, probably under Spicketts.

Geographic entities mentioned:
surface_form: Rhondda Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Ballenger Creek. Ballenger Creek is a tributary of the Monocacy River in Frederick County, Maryland. The headwaters of the creek are located on the east slope of Catoctin Mountain, about west of the city of Frederick. The stream runs roughly southeast to the Monocacy National Battlefield and the confluence with the Monocacy River, which drains to the Potomac River.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Meyers Nunatak. 9iaxfrcipkgyoej1be1yayncfsu8" xml:space="preserve">#redirect Meyers Nunatak

Geographic entities mentioned:
surface_form: meyers nunatak
instance_of: Mountain
coordinates: lat: -74.9
lon: -98.7667
Lake of the Woods 31B. Lake of the Woods 31B is a First Nations reserve on Lake of the Woods, northwestern Ontario. It is one of the reserves of the Anishnaabeg of Naongashiing.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
System implementation. The work by the RN and RCN teams was well known to the USN starting as early as 1946, and included live demonstrations of the Canadian system on Lake Ontario. They also built their own version of the Royal Navy's concept as the &quot;Electronic Data System&quot;, and 20 sets were eventually produced by Motorola.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The Sullivan Expedition of 1779 during the American Revolutionary War passed through the area, destroying Seneca villages, as the Seneca and three other Iroquois nations sided with the British. Loyalist and allied Iroquois tribes had been raiding colonial settlements in the Mohawk Valley and related areas.

Geographic entities mentioned:
surface_form: Mohawk Valley
instance_of: Valley
countries: United States
The western end of the fault appears to peter out into ductile deformation in the Bregaglia Valley or continues as the Gruf Line to the southwest; the eastern end is buried by the Ötztal tectonic block and may continue as the &quot;Inntal fault&quot;, &quot;Isar fault&quot; or &quot;Loisach fault&quot;. Total offset along the Engadine Line is about, decreasing southwest.

Geographic entities mentioned:
surface_form: Inntal
instance_of: Valley
countries: Switzerland
Germany
Austria
coordinates: lat: 47.28109
lon: 10.98633
It was originally discovered in 1896 and named &quot;Engadiner Spalte&quot;. It is a steeply dipping left-lateral strike-slip fault that cuts to a depth of. The total slip on the Engadine Line decreases from in the Lower Engadine to in the Upper Engadine and at Sils, Maloja. The towns of Bever, Maloja, Nauders, S-chanf, Samedan, Sils, St.

Geographic entities mentioned:
surface_form: Lower Engadine
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.75
lon: 10.25
surface_form: Upper Engadine
instance_of: Valley
countries: Switzerland
The Engadine Line deforms the Austroalpine and Penninic nappes and also appears in magnetic anomaly maps. It is responsible for the geologic differences between Graubünden north and south of the Engadine. The Engadine Line is sometimes considered to be a branch of the Periadriatic Fault System.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
The Engadine Line might form the northwestern border of the Scarl-Campo rock units. The combined effects of glacial erosion and slip along the Engadine Line generated the Lej da Segl, Lej da Silvaplauna, Lej da Champfèr and Lej da San Murezzan lakes which are traversed by the Inn River. The fault cuts across the Isola delta of Lake Sils.

Geographic entities mentioned:
surface_form: Lake Sils
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 9.7333333333333
The Engadine Line and other lineaments delimit a fast uplifting area of the Central Alps. In the Val Laschadura, close to Zernez, post-glacial faulting is recorded, and recent vertical offsets of more than are recorded from fluvial sands close to Piz Mundin.

Geographic entities mentioned:
surface_form: Piz Mundin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.925361111111
lon: 10.43075
Trees that drowned between 650-700 AD in Lake Sils, and around 1000 AD as well as at the beginning of the 14th century in Lake Silvaplana may indicate lake level changes or ground subsidence triggered by tectonic activity on the Engadine Line. A large earthquake in the Alps during the 6th century left traces in the Engadine lakes, but the Engadine Line is unlikely to have been its source.

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
Seismic activity in the Venosta Valley may be related to the intersection between the Engadine Line and a north-south trending fault. Some landslides in the region may have been triggered by earthquakes on the Engadine or Gruf lines. Turbidites in Lake Como and Lake Sils, dated to have occurred in AD 700, may relate to Engadine earthquakes.

Geographic entities mentioned:
surface_form: Lake Sils
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.416666666667
lon: 9.7333333333333
The Jordan Valley would continue to be occupied by the Egyptian Expeditionary Force (EEF) through the summer until the middle of September 1918 when the Battle of Megiddo began.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
Lebanon
Israel
Syria
State of Palestine
coordinates: lat: 32.317222222222
lon: 35.57
From here on, the ridge only climbs gently in a northeasterly direction and has several more subpeaks with small wind gaps. To the north the Großer Mittelberg transitions to the ridge of Auf dem Acker without any noticeable wind gap. The Großer Mittelberg is almost entirely covered in beech woods and lies within the Harz National Park.

Geographic entities mentioned:
surface_form: Auf dem Acker
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7488
lon: 10.4453
surface_form: großer mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6951
lon: 10.3649
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4097
lon: 9.91389
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5117
lon: 11.1923
surface_form: auf dem acker
instance_of: Mountain
countries: Germany
coordinates: lat: 51.7488
lon: 10.4453
Großer Mittelberg (Lonau). The Großer Mittelberg (the short form &quot;Mittelberg&quot; is also common) is a ridge in the Harz Mountains of Germany that begins immediately northeast of Lonau in the district of Göttingen in Lower Saxony. It separates the valley of &quot;Kirchtal&quot;, through which the Große Lonau flows, from the &quot;Mariental&quot; and the Kleine Lonau.

Geographic entities mentioned:
surface_form: großer mittelberg (lonau)
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6951
lon: 10.3649
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4097
lon: 9.91389
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5117
lon: 11.1923
Großer Mittelberg (Lonau). The Großer Mittelberg (the short form &quot;Mittelberg&quot; is also common) is a ridge in the Harz Mountains of Germany that begins immediately northeast of Lonau in the district of Göttingen in Lower Saxony. It separates the valley of &quot;Kirchtal&quot;, through which the Große Lonau flows, from the &quot;Mariental&quot; and the Kleine Lonau.

Geographic entities mentioned:
surface_form: großer mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6951
lon: 10.3649
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4097
lon: 9.91389
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4097
lon: 9.91389
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5117
lon: 11.1923
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5117
lon: 11.1923
It separates the valley of &quot;Kirchtal&quot;, through which the Große Lonau flows, from the &quot;Mariental&quot; and the Kleine Lonau. is Although it is the nearest subpeak to the village of Lonau, the Großer Mittelberg is, at 531 metres, not the highest point, but may be viewed as a main summit due to its prominent location.

Geographic entities mentioned:
surface_form: großer mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.6951
lon: 10.3649
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.4097
lon: 9.91389
surface_form: mittelberg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.5117
lon: 11.1923
Battle of Lookout Mountain. The Battle of Lookout Mountain, also known as the Battle Above the Clouds, was fought November 24, 1863, as part of the Chattanooga Campaign of the American Civil War. Union forces under Maj. Gen. Joseph Hooker assaulted Lookout Mountain, Chattanooga, Tennessee, and defeated Confederate forces commanded by Maj. Gen. Carter L. Stevenson.

Geographic entities mentioned:
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
Gen. William Rosecrans retreated to Chattanooga, Tennessee. Bragg's Army of Tennessee besieged the city, threatening to starve the Union forces into surrender. Bragg's troops established themselves on Missionary Ridge and Lookout Mountain, both of which had excellent views of the city, the Tennessee River flowing through the city, and the Union's supply lines.

Geographic entities mentioned:
surface_form: Missionary Ridge
instance_of: Landform
countries: United States
coordinates: lat: 34.986388888889
lon: -85.278611111111
surface_form: Lookout Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 34.863713888889
lon: -85.392452777778
1949) is a Zimbabwean-British blind adventurer. He undertakes a variety of expeditions all around the world to raise awareness and money for a charity organization, and blind people in general. His recent trips include flying from London to Sydney in a micro-light, climbing Mont Blanc and running across the Gobi Desert. Hilton-Barber grew up in Rhodesia (now Zimbabwe), where his father, Lt.-Col.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
Miranzai Valley. The Miranzai Valley, also Hangu, is a mountainous valley situated in the Kohat and Hangu districts in the North-West Frontier Province of Pakistan. It is made up of two valleys, draining from the southwest into the Kurram and northeast into the Kohat Tai. It is divided into upper and lower Miranzai. It extends from the Bangash and Orakzai hills to the Bangashs.

Geographic entities mentioned:
surface_form: miranzai valley
instance_of: Valley
countries: Pakistan
They enjoy weekends away there, although the younger Broons show some reluctance to go there. In a 1940s strip, the house is shown to be on a hillside on the east side of the River Ness and an arrow also points to Auchentoogle being located on the northern bank of Loch Ness near Dores.

Geographic entities mentioned:
surface_form: Loch Ness
instance_of: Lake
countries: United Kingdom
coordinates: lat: 57.3
lon: -4.45
White Crown Mountain. White Crown Mountain is a mountain in the Princess Margaret Range on Axel Heiberg Island, Nunavut, Canada. It is located on the southwestern edge of the Muller Icecap and is surrounded by glaciers.

Geographic entities mentioned:
surface_form: crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.945
lon: -125.813
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: white crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 79.9267
lon: -92.3217
surface_form: crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.41
lon: -123.092
White Crown Mountain. White Crown Mountain is a mountain in the Princess Margaret Range on Axel Heiberg Island, Nunavut, Canada. It is located on the southwestern edge of the Muller Icecap and is surrounded by glaciers.

Geographic entities mentioned:
surface_form: crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.945
lon: -125.813
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: white crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 79.9267
lon: -92.3217
surface_form: crown mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 49.41
lon: -123.092
Pichcacocha Lakes. Pichcacocha Lakes or Pichgacocha Lakes (possibly from Quechua &quot;pichqa&quot; five &quot;qucha&quot; lake) is a group of five lakes in Peru. They lie in the Huánuco Region, Ambo Province, Conchamarca District.

Geographic entities mentioned:
surface_form: pichcacocha lakes
instance_of: Lake
countries: Peru
coordinates: lat: -10.01944444
lon: -76.12833333
Pichcacocha Lakes. Pichcacocha Lakes or Pichgacocha Lakes (possibly from Quechua &quot;pichqa&quot; five &quot;qucha&quot; lake) is a group of five lakes in Peru. They lie in the Huánuco Region, Ambo Province, Conchamarca District.

Geographic entities mentioned:
surface_form: pichcacocha lakes
instance_of: Lake
countries: Peru
coordinates: lat: -10.01944444
lon: -76.12833333
surface_form: pichgacocha
instance_of: Lake
countries: Peru
coordinates: lat: -10.01944444
lon: -76.12833333
Leadfield, California. Leadfield was an unincorporated community, and historic mining town in Inyo County, California. It is now a ghost town. It is located in Titus Canyon in the Grapevine Mountains, east of Death Valley in Death Valley National Park. Leadfield lies at an elevation of. It is on the National Register of Historic Places. History.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
, also known as the Manshuin Monzeki, is a Tendai monastery located near the Shugakuin Imperial Villa at Sakyō-ku, Ichijo-ji, Takenouchi-cho, in northeast Kyoto, Japan. The monastery was founded by Dengyō Daishi in the 8th century. It was then located near Mount Hiei and known as Tobibo, but renamed Manshuin in 1108 or 1109. In the early Edo period the monastery moved to its current site.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Luoland. s2rd7k08zbq1ol6i5i1xz6jjmfnc3" xml:space="preserve">Luoland (historically &quot;Kavirondo&quot;) is the tribal homeland of the Kenya Luo (also called Jo-Luo or Kavirondo), a people of western Kenya, also extending into eastern Uganda and northern Tanzania. This area consists roughly of the basin surrounding Winam Gulf of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Before civil engineers rechanneled the Duwamish, the area had extensive tidelands, and had an abundance of seafoods. The people living around Lake Washington were collectively known as &quot;hah-choo-AHBSH&quot; or &quot;hah-chu-AHBSH&quot; or &quot;Xacuabš&quot;, People of &quot;HAH-choo&quot; or &quot;Xachu&quot;, &quot;People of a Large Lake&quot; or &quot;Lake People&quot;.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Mount Eboshi. is a stratovolcano located in the Daisetsuzan Volcanic Group of the Ishikari Mountains in central Hokkaido, Japan.

Geographic entities mentioned:
surface_form: mount eboshi
instance_of: Mountain
countries: Japan
coordinates: lat: 43.680555555556
lon: 142.92194444444
surface_form: mount eboshi
instance_of: Mountain
countries: Japan
coordinates: lat: 40.84044444
lon: 141.0395
It ranges from sea level up to. It also occurs in palm-vine scrub, gallery forest and along rivers. The species is mostly non-migratory, but some birds disperse to the &quot;Eucalyptus&quot; woodland in the Atherton Tableland during the winter. The species has a tiny global range, and is described as uncommon and occurring at low densities throughout its range.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Blue Hole (New Mexico). The Blue Hole of Santa Rosa, or simply the Blue Hole, is a circular, bell-shaped pool or small lake located along Route 66 east of Santa Rosa, New Mexico that is a tourist attraction and swimming venue, and one of the most popular dive destinations in the US for scuba diving and training. The Blue Hole is an artesian well and cenote that was once used as a fish hatchery.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
Blue Hole (New Mexico). The Blue Hole of Santa Rosa, or simply the Blue Hole, is a circular, bell-shaped pool or small lake located along Route 66 east of Santa Rosa, New Mexico that is a tourist attraction and swimming venue, and one of the most popular dive destinations in the US for scuba diving and training. The Blue Hole is an artesian well and cenote that was once used as a fish hatchery.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
The Blue Hole of Santa Rosa, or simply the Blue Hole, is a circular, bell-shaped pool or small lake located along Route 66 east of Santa Rosa, New Mexico that is a tourist attraction and swimming venue, and one of the most popular dive destinations in the US for scuba diving and training. The Blue Hole is an artesian well and cenote that was once used as a fish hatchery. Description.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
The Blue Hole is an artesian well and cenote that was once used as a fish hatchery. Description. The Blue Hole is a clear blue body of water with a constant temperature and constant inflow of, enough to cycle out the water every six hours. While the surface is only in diameter, it expands to a diameter of at the bottom. The depth of the main pool is more than below the surface.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
The depth of the main pool is more than below the surface. The water in the pool originates deep underground below from the western edge of the Ogallala Aquifer. The Blue Hole is an example of a natural artesian well, a type of well or spring fed by water under high pressure, and of a cenote, a collapsed cavern exposing groundwater beneath.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
Hazards in the passages include frequent cave-ins, zero visibility due to silt, and extreme restrictions. Fauna present in the Blue Hole includes goldfish, koi, carp, and crawdads. Since Santa Rosa, New Mexico is at an elevation of, it is necessary for divers to use high-altitude dive tables to compute the dive profile and decompression stops when diving in the Blue Hole.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
The pool is open for public use, including picnic, swimming, diving, and snorkeling; however, there are no lifeguards on duty. Early history. The Blue Hole was used by nomadic tribes as a reliable water source in the arid plains that surround the area. Cowboys on cattle drives across the Pecos River would also stop by the pool.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
Cowboys on cattle drives across the Pecos River would also stop by the pool. When Route 66 came through the city in the 1920s, the original alignment brought it right past the property of the Blue Hole. The pool became a popular stop and tourist attraction for motorists on the new highway. In 1932, it became a hatchery for the National Fish Hatchery.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
The pool became a popular stop and tourist attraction for motorists on the new highway. In 1932, it became a hatchery for the National Fish Hatchery. Afterward it became the Blue Hole Recreation Area in the 1970s, then the Blue Hole Dive and Conference Center. In the current era of the Interstate, the pool continues to be a popular destination with both locals and divers from around the world.

Geographic entities mentioned:
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 24.7058
lon: -81.3808
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 39.6265
lon: -74.896
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Lake
countries: United States
coordinates: lat: 34.9404
lon: -104.673
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
surface_form: blue hole
instance_of: Landform
countries: United States
coordinates: lat: 41.4059
lon: -82.8069
After taking a wrong turn in low visibility, Thompson became trapped in a dead end passage below the surface. By the time Young had located Thompson, he had already drowned. Young returned the next day to recover the body.

Geographic entities mentioned:
surface_form: dead
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
He married his master's eldest daughter Bao Gu (), who was a famous female physician in Chinese history. Bao instructed Ge in Daoist alchemy and transmitted a version of the that had been divinely revealed to him while meditating in a cave on Mount Song. Daoist legends differed over whether the was revealed to Bo He (, fl. 300) or to Bao Jing.

Geographic entities mentioned:
surface_form: Mount Song
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 34.484722222222
lon: 112.96027777778
Daoist legends differed over whether the was revealed to Bo He (, fl. 300) or to Bao Jing. The former narrative says the transcendent Wang Fangping () instructed his student Bo He to stare at the north wall of a grotto on Mount Emei (Sichuan) until he could discern the Chinese characters that ancient Daoists had engraved, which was revealed after three years of wall gazing. Ge Hong's c.

Geographic entities mentioned:
surface_form: Mount Emei
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.519722222222
lon: 103.3325
Central Switzerland. Central Switzerland is a subdivision of Switzerland as defined by the Federal Statistical Office for statistical purposes. It is classified as a NUTS-2 statistical region of Switzerland, and encompasses the cantons of Uri, Schwyz, Obwalden, Nidwalden, Lucerne and Zug. It incorporates the highlands in the central portion of the country. Sub-division.

Geographic entities mentioned:
surface_form: highlands
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The region encompasses an area of, and had a population of 718,400 inhabitants. Central Switzerland incorporates the highlands in the central portion of the country. It is flanked by the Jura and Rhine rivers in the north, and Lake Geneva and the Alps in the south. The topography consists of hills interspersed with valleys and grasslands.

Geographic entities mentioned:
surface_form: highlands
instance_of: Plateau
countries: Switzerland
coordinates: lat: 47.1167
lon: 7.36667
The region encompasses an area of, and had a population of 718,400 inhabitants. Central Switzerland incorporates the highlands in the central portion of the country. It is flanked by the Jura and Rhine rivers in the north, and Lake Geneva and the Alps in the south. The topography consists of hills interspersed with valleys and grasslands.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Chindongo heteropictus. &quot;Chindongo heteropictus&quot; is a species of cichlid endemic to Lake Malawi, where it is only known from Thumbi West Island. This species can reach a length of SL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
The southern side of the park looks over the valley below, offering scenic views of the Sierra Madre Oriental mountains: Cofre de Perote to the West and snowcapped Pico de Orizaba to the South. In 1922, the Junta de Obras Materiales de Jalapa, presided by William K.

Geographic entities mentioned:
surface_form: Cofre de Perote
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.491944444444446
lon: -97.15
surface_form: Pico de Orizaba
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.03
lon: -97.27
Blackface Mountain. Blackface Mountain is a summit in Alberta, Canada. Blackface Mountain most likely was so named on account of its appearance.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: blackface mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.90006
lon: -117.41903
Kiryas Joel–Poughkeepsie–Newburgh metropolitan area. The Kiryas Joel–Poughkeepsie–Newburgh, NY Metropolitan Statistical Area, as defined by the United States Office of Management and Budget, is an area consisting of two counties in New York's Hudson Valley, with the municipalities of Kiryas Joel, Poughkeepsie, and Newburgh as its principal cities.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Germanic tribes prior to migration. Germanic peoples moved out of southern Scandinavia and northern Germany to the adjacent lands between the Elbe and Oder after 1000 BC.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Wickwire Hill. Wickwire Hill is a summit located in Central New York Region of New York located in the Town of Florence in Oneida County, north of Camden.

Geographic entities mentioned:
surface_form: oneida
instance_of: Lake
countries: United States
coordinates: lat: 43.2
lon: -75.9
surface_form: wickwire hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.39201
lon: -75.74324
Wickwire Hill. Wickwire Hill is a summit located in Central New York Region of New York located in the Town of Florence in Oneida County, north of Camden.

Geographic entities mentioned:
surface_form: wickwire hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.39201
lon: -75.74324
Montejurra incidents. The Montejurra incidents, was a neo-fascist terrorist attack that took place on 9 May 1976, when two Carlist members were killed and another three seriously wounded by right-wing gunmen at the annual Carlist Party celebration that was held in Montejurra, Navarre, Spain. The incident.

Geographic entities mentioned:
surface_form: Montejurra
instance_of: Mountain
countries: Spain
coordinates: lat: 42.631111111111
lon: -2.0447222222222
Geography. According to the United States Census Bureau, the Indian reservation has a total area of 6.0 mi2 (15.5 km2). 5.8 mi2 (14.9 km2) of it is land and 0.2 mi2 (0.6 km2) of it (3.68%) is water. Cattaraugus Creek runs through the middle of the reservation, and Lake Erie forms part of the western boundary. Demographics.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Agno, Ticino. Agno () is a historic town and a municipality in the district of Lugano in the canton of Ticino in Switzerland. Due to its position on Lake Lugano it is popular with tourists, and hosts summer festivals, with two hotels and several camping grounds. It is served by the Lugano-Agno airport. The official language of Agno is Italian. History.

Geographic entities mentioned:
surface_form: Lake
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Following the Act of Mediation of 1803, the parish lost its political meaning entirely. Community of Agno. Because of its strategic location at the northern end of an arm of Lake Lugano and along the Varese-Ponte Tresa-Monte Ceneri road, Agno was possibly the center of a Roman Pagus. Some of the archeological finds from Roman Agno are in the local Museo plebano.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Lake Hoare. Lake Hoare is a lake about long between Lake Chad and Canada Glacier in Taylor Valley, Victoria Land, Antarctica. Its surface area measures. The lake was named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist Ray A. Hoare, a member of the VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys.

Geographic entities mentioned:
surface_form: Taylor Valley
instance_of: Valley
coordinates: lat: -77.616666666667
lon: 163
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Its surface area measures. The lake was named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist Ray A. Hoare, a member of the VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Hoare is dammed by the tongue of Canada Glacier, otherwise it would drain into Lake Fryxell, northeast across the glacier tongue.

Geographic entities mentioned:
surface_form: Wright
instance_of: Valley
coordinates: lat: -77.166666666667
lon: 161.83333333333
surface_form: Victoria
instance_of: Valley
coordinates: lat: -77.383333333333
lon: 161.93333333333
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Hoare, a member of the VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Hoare is dammed by the tongue of Canada Glacier, otherwise it would drain into Lake Fryxell, northeast across the glacier tongue. Lake Chad, only southeast of Lake Hoare, sometimes overflows into Lake Hoare.

Geographic entities mentioned:
surface_form: chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: lake chad
instance_of: Lake
coordinates: lat: -77.65
lon: 162.767
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Lake Hoare. Lake Hoare is a lake about long between Lake Chad and Canada Glacier in Taylor Valley, Victoria Land, Antarctica. Its surface area measures. The lake was named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, for physicist Ray A. Hoare, a member of the VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys.

Geographic entities mentioned:
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Hoare, a member of the VUWAE that examined lakes in Taylor, Wright, and Victoria Valleys. Lake Hoare is dammed by the tongue of Canada Glacier, otherwise it would drain into Lake Fryxell, northeast across the glacier tongue. Lake Chad, only southeast of Lake Hoare, sometimes overflows into Lake Hoare.

Geographic entities mentioned:
surface_form: hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
surface_form: lake hoare
instance_of: Lake
coordinates: lat: -77.6305561111111
lon: 162.86666694444443
Its summit elevation of above sea level is above the city center. Located between downtown Boise and the foothills, Table Rock has multiple caves and ledges and overlooks the Treasure Valley. A prominent local landmark, it is a popular spot for day hiking from the Old State Penitentiary which offers access to views of the Treasure Valley, Owyhee Mountains, and the Boise Foothills themselves.

Geographic entities mentioned:
surface_form: Treasure Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.0403
lon: -116.933
The northeast end of East Kennebago drains into Cherry Run, thence into the South Branch of the Dead River. The southwest end of East Kennebago drains into Kennebago Lake, thence into the Kennebago River, Cupsuptic Lake, through a series of lakes into the Rapid River and Umbagog Lake, the source of the Androscoggin River, which drains into Merrymeeting Bay, the estuary of the Kennebec River.

Geographic entities mentioned:
surface_form: Umbagog Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75
lon: -71.05
East Kennebago Mtn. is a monadnock, flanked by its spurs: Tim Mountain to the north, Black Spur to the west, and Blackcat Mountain to the southwest. The southeast side of East Kennebago Mountain drains into the South Branch of the Dead River, thence into Flagstaff Lake, the Dead River, and the Kennebec River, which drains into the Gulf of Maine.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: east kennebago mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.121833333333
lon: -70.599666666667
surface_form: flagstaff lake
instance_of: Lake
countries: United States
coordinates: lat: 42.5825
lon: -119.80027777778
The southeast side of East Kennebago Mountain drains into the South Branch of the Dead River, thence into Flagstaff Lake, the Dead River, and the Kennebec River, which drains into the Gulf of Maine. The northeast end of East Kennebago drains into Cherry Run, thence into the South Branch of the Dead River.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
East Kennebago Mountain. East Kennebago Mountain is a trailless mountain located in Franklin County, Maine. East Kennebago Mtn. is a monadnock, flanked by its spurs: Tim Mountain to the north, Black Spur to the west, and Blackcat Mountain to the southwest.

Geographic entities mentioned:
surface_form: east kennebago mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.121833333333
lon: -70.599666666667