Sarmila/GeoWiki-Features huggingface dataset:
It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north. The telegraph trail crosses other tributaries along the eastern side of Mess Creek, including Crayke Creek about south of Elwyn Creek.

Geographic entities mentioned:
surface_form: Crayke Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.73298
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Geography. Elwyn Creek originates in the middle of the Big Raven Plateau. From its source on the northwestern slope of Mount Edziza, Elwyn Creek flows about northwest past Tsekone Ridge and Pillow Ridge to the head of a vegetated canyon. It then continues to flow northwest through the canyon for about before flowing west inside the canyon for an additional to empty into Mess Creek.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
History. The historic Yukon Telegraph Trail crosses Elwyn Creek in Mess Creek valley. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
History. The historic Yukon Telegraph Trail crosses Elwyn Creek in Mess Creek valley. It was built to serve the nearly Yukon Telegraph Line which was constructed by the Dominion Government Telegraph Service between 1897 and 1901 to send messages from Ashcroft, British Columbia in the south to Dawson City, Yukon in the north.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
It is of Eocene age, having yielded a K–Ar date of 53.1 ± 2.4 million years. This suggests that the Elwyn Creek Pluton was formed by one of the youngest known igneous events in the Elwyn Creek area prior to the onset of volcanism of the Mount Edziza volcanic complex in the Late Miocene. History. The historic Yukon Telegraph Trail crosses Elwyn Creek in Mess Creek valley.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Elwyn Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about southwest of Dease Lake. Elwyn Creek's watershed's land cover is classified as 37.9% shrubland, 30.3% conifer forest, 15.2% barren, 7.6% snow/glacier, 7.1% herbaceous, and small amounts of other cover.

Geographic entities mentioned:
surface_form: dease lake
instance_of: Lake
countries: Canada
coordinates: lat: 58.63502
lon: -130.03761
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek's watershed's land cover is classified as 37.9% shrubland, 30.3% conifer forest, 15.2% barren, 7.6% snow/glacier, 7.1% herbaceous, and small amounts of other cover. Elwyn Creek is in Mount Edziza Provincial Park which lies within the traditional territory of the Tahltan people. Geography. Elwyn Creek originates in the middle of the Big Raven Plateau.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
It then continues to flow northwest through the canyon for about before flowing west inside the canyon for an additional to empty into Mess Creek. Elwyn Creek's only named tributary, Kadeya Creek, is about east of Elwyn Creek's confluence with Mess Creek. It is about long and flows northwest into Elwyn Creek from near the western side of Mount Edziza. Geology.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek. Elwyn Creek is a tributary of Mess Creek, which in turn is a tributary of the Stikine River in northwest part of the province of British Columbia, Canada. It flows generally west for about to join Mess Creek about north of Mess Creek's confluence with Taweh Creek. Elwyn Creek's watershed covers and its mean annual discharge is estimated at.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
It flows generally west for about to join Mess Creek about north of Mess Creek's confluence with Taweh Creek. Elwyn Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Elwyn Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about southwest of Dease Lake.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek's watershed covers and its mean annual discharge is estimated at. The mouth of Elwyn Creek is located about southeast of Telegraph Creek, about west-southwest of Iskut and about southwest of Dease Lake. Elwyn Creek's watershed's land cover is classified as 37.9% shrubland, 30.3% conifer forest, 15.2% barren, 7.6% snow/glacier, 7.1% herbaceous, and small amounts of other cover.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
It is about long and flows northwest into Elwyn Creek from near the western side of Mount Edziza. Geology. Elwyn Creek contains a group of hot springs between elevations of called the Elwyn Hot Springs. They occur near the base of the Mount Edziza volcanic complex where basalt of the Nido Formation overlies Tertiary leucogranite.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
In 1983, the springs had a maximum temperature of. Their existence may be linked to a shallow hydrothermal system driven by residual magmatic heat from the recently active Desolation Lava Field about to the east. Elwyn Creek is the namesake of the Elwyn Creek Pluton. This is a body of intrusive rock at least wide exposed in Elwyn Creek canyon.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek is the namesake of the Elwyn Creek Pluton. This is a body of intrusive rock at least wide exposed in Elwyn Creek canyon. The main intrusive rock comprising the Elwyn Creek Pluton is fine grained, slightly porphyritic leucogranite containing phenocrysts of sodic plagioclase. It is of Eocene age, having yielded a K–Ar date of 53.1 ± 2.4 million years.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
The telegraph trail crosses other tributaries along the eastern side of Mess Creek, including Crayke Creek about south of Elwyn Creek. Elwyn Creek was formerly called 14 Mile Creek which appeared on a BC Lands map published in 1929. Its current name was suggested by the BC Geographic Division to avoid duplication; it first appeared on maps in 1945.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek was formerly called 14 Mile Creek which appeared on a BC Lands map published in 1929. Its current name was suggested by the BC Geographic Division to avoid duplication; it first appeared on maps in 1945. Elwyn Creek is named after Thomas Elwyn, a government agent who accompanied a Western Union Telegraph expedition in 1866.

Geographic entities mentioned:
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Chammliberg. The Chammliberg is a mountain of the Glarus Alps, located south of the Klausen Pass in the canton of Uri. While the south side of the mountain is covered by the large Hüfi Glacier, the north-west side consists of an 800 metre high face.

Geographic entities mentioned:
surface_form: chammliberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.83666667
lon: 8.84486111
Haplochromis riponianus. &quot;Haplochromis riponianus&quot; is a species of cichlid found in Lake Victoria and possibly in the adjacent reaches of the Nile. This species can reach a length of SL.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
His acting debut was on an episode of &quot;Police Woman&quot;. Carter also made appearances on &quot;Good Times&quot;, &quot;The Sinbad Show&quot;, &quot;The Steve Harvey Show&quot;, &quot;A Different World&quot;, and in the television films &quot;Polly&quot; and its 1990 sequel. Personal life. Carter grew up in the San Gabriel Valley area of Southern California.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
After graduating from King's College, Cambridge he studied for the priesthood at Ripon College Cuddesdon. He served curacies at St Anthony of Egypt, Newcastle upon Tyne and Berwick Parish Church and incumbencies at Alwinton, Alston cum Garrigill and Glendale before his Archdeacon's appointment. He died on 31 January 2020 and is buried in St Bartholomew's Church, Whttingham, England.

Geographic entities mentioned:
surface_form: Glendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.595083
lon: -2.105
Yamuna. The Yamuna (;) is the second-largest tributary river of the Ganges by discharge and the longest tributary in India. Originating from the Yamunotri Glacier at a height of about on the southwestern slopes of Bandarpunch peaks of the Lower Himalaya in Uttarakhand, it travels and has a drainage system of, 40.2% of the entire Ganges Basin.

Geographic entities mentioned:
surface_form: Bandarpunch
instance_of: Mountain
countries: India
coordinates: lat: 30.99916667
lon: 78.54166667
The drainage system of the river stretches between Giri-Sutlej catchment in Himachal and Yamuna-Bhilangna catchment in Garhwal, also draining the ridge of Shimla. Kalanag () is the highest point of the Yamuna basin. Other tributaries in the region are the Giri, Rishi Ganga Kunta, Hanuman Ganga and Bata, which drain the upper catchment area of the Yamuna basin.

Geographic entities mentioned:
surface_form: Kalanag
instance_of: Mountain
countries: India
coordinates: lat: 31.02
lon: 78.57
Other tributaries in the region are the Giri, Rishi Ganga Kunta, Hanuman Ganga and Bata, which drain the upper catchment area of the Yamuna basin. From the upper catchment area, the river descends onto the plains of Doon Valley, at Dak Pathar near Dehradun. Flowing through the Dakpathar Barrage, the water is diverted into a canal for power generation.

Geographic entities mentioned:
surface_form: Doon Valley
instance_of: Valley
countries: India
coordinates: lat: 30.361
lon: 77.992
The main canal is long. When including its branches and many major and minor irrigation channels, it has a total length of The WYC begins at the Hathni Kund Barrage about from Dakpathar and south of Doon Valley. The canals irrigate vast tracts of land in the region in Ambala, Karnal, Sonipat, Rohtak, Jind, Hisar and Bhiwani districts. Sutlej–Yamuna Link Canal.

Geographic entities mentioned:
surface_form: Doon Valley
instance_of: Valley
countries: India
coordinates: lat: 30.361
lon: 77.992
Haplogroup I-Z63. Haplogroup I-Z63, also known as I1a3 per the International Society of Genetic Genealogy ('ISOGG), is a Y chromosome haplogroup. It is correlated with a DYS456 value inferior to 15, but there are exceptions. I-Z63 is most common in England, Scotland, Germany, Fennoscandia and Poland. Its progenitor is assumed to have lived in Jutland at around 2500 BCE.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The earliest archeological sample for I-Z63 is indeed connected to an individual from near Hjørring in Jutland, present Denmark. Within Fennoscandia, I-Z63 has a particularly strong association with Finland. To date, ancient I-Z63 has been found archeologically in historic Jutland (present Denmark and Germany) along with Poland, Hungary, Turkey and Italy. Origins.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
The Mexica people, guided by their god Huitzilopochtli, sought the place where a bird lands on the prickly pear and devours a snake. They found their sign on an island in Lake Texcoco, where they erected the city of Tenochtitlan (&quot;Place of the Prickly Pear Cactus&quot;; present-day México City) in 1325.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
Wilderness area proposal. The area has been proposed as a Wilderness area to protect its ecology. Geography. Burma Rim is near Hatch Lake, Dead Horse Lake, and World Lake. It runs along the east boundary with Sheep Rock at the south end of the unit. There are no permanent springs or streams, but several playa lake bed waterholes. The vegetative cover is primarily desert sagebrush and grassland.

Geographic entities mentioned:
surface_form: Sheep Rock
instance_of: Mountain
countries: United States
coordinates: lat: 45.1917
lon: -116.671
Pinto, Maryland. Pinto is an unincorporated community along the North Branch Potomac River in Allegany County, Maryland, United States across from Rocket Center, West Virginia. While the town was first known as Potomac, its post office is referred to as Pinto because there already exists a Potomac, Maryland. Pinto is located south of Cresaptown on Winchester Road.

Geographic entities mentioned:
surface_form: North Branch Potomac River
instance_of: Watercourse
countries: United States
coordinates: lat: 39.5284255
lon: -78.5875141
The main bodies of standing water in the department are the lakes Petén Itzá, Peténchel, Quexil, Salpetén and Macanche in the centre of the department; Yaxhá and Sacnab in the east, Petexbatún in the southwest, and Perdida, Larga, La Gloria, San Diego, Mendoza, El Repasto and Lacandón in the west. The San Pedro River flows east to west in the northwest corner of Petén. Climate.

Geographic entities mentioned:
surface_form: Petén Itzá
instance_of: Lake
countries: Guatemala
coordinates: lat: 16.983333333333
lon: -89.8
This tradition began with the importation of the Byzantine Empire's religious music when the Kievan Rus' converted to Orthodoxy in 988. Origins. When Prince Vladimir of Kiev converted to Orthodoxy, Mount Athos was the musical center of the Orthodox world. Monks from all over Eastern Europe and Byzantium traveled to Mount Athos for musical training and to learn the ways of Orthodox chant.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Little Bear Lake Airport. Little Bear Lake Airport is located adjacent to Little Bear Lake, Saskatchewan, Canada.

Geographic entities mentioned:
surface_form: Little Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.328641
lon: -104.6242189
xenbase provides limited support (BLAST, JBrowse tracks, genome download) for Nanorana parkeri. Habitat and conservation. This very common frog is found on high-altitude grasslands, forests, shrubs, lakes, ponds, marshes, streams and rivers in the Tibetan Plateau at elevations of above sea level. It an explosive breeder in streams and marshes. There are no known major threats.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
The country has 1008 lakes, 16 have an area of more than. Lake Arresø, located northwest of Copenhagen, is the largest lake. The Kingdom of Denmark includes two overseas territories, both well to the west of Denmark: Greenland, the world's largest island, and the Faroe Islands in the North Atlantic Ocean.

Geographic entities mentioned:
surface_form: Arresø
instance_of: Lake
countries: Denmark
coordinates: lat: 55.974722222222
lon: 12.104166666667
Between 1926 and 1956 he presented the children's radio show &quot;Children's Hour with Uncle Markus&quot; () on the National Radio of Finland. On his show he said Father Christmas () lived in Lapland on Ear Mountain (Korvatunturi), on the basis that this was where he could hear everything to find out who was naughty and nice.

Geographic entities mentioned:
surface_form: Korvatunturi
instance_of: Mountain
countries: Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 68.073611111111
lon: 29.315277777778
His first successful trial flight was on 24 June 2004 near Geneva, Switzerland. Rossy has made more than 30 powered flights since. In November 2006 he flew with a later version of his jet pack. On 14 May 2008 he made a successful 6-minute flight from the town of Bex near Lake Geneva. He exited a Pilatus Porter at with his jet pack. It was the first public demonstration before the world's press.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Lamprologus ornatipinnis. &quot;Lamprologus ornatipinnis&quot; is a species of cichlid endemic to Lake Tanganyika, where it prefers areas with sandy substrates or, sometimes, rocky areas. While not a shell dweller like many of its congeners, it does use shells (and possibly rock crevices) for spawning. This species can reach a length of 7.8 centimetres (3.1 in) TL.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
City of Newcastle. The City of Newcastle is a local government area in the Hunter region of New South Wales, Australia. The City of Newcastle incorporates much of the area of the Newcastle metropolitan area. The Lord Mayor of the City of Newcastle Council is Councillor Dr.

Geographic entities mentioned:
surface_form: Hunter
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
In the following decades, fur-trading companies used the Columbia as a key transportation route. Overland explorers entered the Willamette Valley through the scenic, but treacherous Columbia River Gorge, and pioneers began to settle the valley in increasing numbers.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
These developments have greatly altered river environments in the watershed, mainly through industrial pollution and barriers to fish migration. Course. The Columbia begins its journey in the southern Rocky Mountain Trench in British Columbia (BC). Columbia Lake above sea level and the adjoining Columbia Wetlands form the river's headwaters.

Geographic entities mentioned:
surface_form: Rocky Mountain Trench
instance_of: Landform
Valley
countries: Canada
United States
coordinates: lat: 54.5
lon: -122.5
Course. The Columbia begins its journey in the southern Rocky Mountain Trench in British Columbia (BC). Columbia Lake above sea level and the adjoining Columbia Wetlands form the river's headwaters. The trench is a broad, deep, and long glacial valley between the Canadian Rockies and the Columbia Mountains in BC.

Geographic entities mentioned:
surface_form: Columbia Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.230555555556
lon: -115.85333333333
The trench is a broad, deep, and long glacial valley between the Canadian Rockies and the Columbia Mountains in BC. For its first, the Columbia flows northwest along the trench through Windermere Lake and the town of Invermere, a region known in BC as the Columbia Valley, then northwest to Golden and into Kinbasket Lake.

Geographic entities mentioned:
surface_form: Columbia Valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.0333
lon: -116.617
For its first, the Columbia flows northwest along the trench through Windermere Lake and the town of Invermere, a region known in BC as the Columbia Valley, then northwest to Golden and into Kinbasket Lake. Rounding the northern end of the Selkirk Mountains, the river turns sharply south through a region known as the Big Bend Country, passing through Revelstoke Lake and the Arrow Lakes.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
This C-shaped segment of the river is also known as the &quot;Big Bend&quot;. During the Missoula Floods 1015,000 years ago, much of the floodwater took a more direct route south, forming the ancient river bed known as the Grand Coulee. After the floods, the river found its present course, and the Grand Coulee was left dry.

Geographic entities mentioned:
surface_form: Grand Coulee
instance_of: Valley
countries: United States
coordinates: lat: 47.62
lon: -119.308
The river flows past The Gorge Amphitheatre, a prominent concert venue in the Northwest, then through Priest Rapids Dam, and then through the Hanford Nuclear Reservation. Entirely within the reservation is Hanford Reach, the only U.S. stretch of the river that is completely free-flowing, unimpeded by dams, and not a tidal estuary.

Geographic entities mentioned:
surface_form: Hanford Reach
instance_of: Landform
countries: United States
coordinates: lat: 46.2794
lon: -119.268
Between 50 and 20 million years ago, from the Eocene through the Miocene eras, tremendous volcanic eruptions frequently modified much of the landscape traversed by the Columbia. The lower reaches of the ancestral river passed through a valley near where Mount Hood later arose.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Numerous flat-topped buttes with rich soil stand high above the chaotic scablands. Constrictions at several places caused the floodwaters to pool into large temporary lakes, such as Lake Lewis, in which sediments were deposited. Water depths have been estimated at at Wallula Gap and over modern Portland, Oregon.

Geographic entities mentioned:
surface_form: Lake Lewis
instance_of: Lake
countries: United States
coordinates: lat: 46.1667
lon: -119
Over the last several thousand years a series of large landslides have occurred on the north side of the Columbia River Gorge, sending massive amounts of debris south from Table Mountain and Greenleaf Peak into the gorge near the present site of Bonneville Dam. The most recent and significant is known as the Bonneville Slide, which formed a massive earthen dam, filling of the river's length.

Geographic entities mentioned:
surface_form: Greenleaf Peak
instance_of: Mountain
countries: United States
coordinates: lat: 45.7138356
lon: -121.9669576
The bridge, which aligns with geological records of the Bonneville Slide, was described in some stories as the result of a battle between gods, represented by Mount Adams and Mount Hood, in their competition for the affection of a goddess, represented by Mount St. Helens.

Geographic entities mentioned:
surface_form: Mount Hood
instance_of: Mountain
countries: United States
coordinates: lat: 45.37361111111111
lon: -121.69583333333334
Steamboats operated in several distinct stretches of the river: on its lower reaches, from the Pacific Ocean to Cascades Rapids; from the Cascades to the Dalles-Celilo Falls; from Celilo to Priests Rapids; on the Wenatchee Reach of eastern Washington; on British Columbia's Arrow Lakes; and on tributaries like the Willamette, the Snake and Kootenay Lake.

Geographic entities mentioned:
surface_form: Kootenay Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
Climate varies greatly within the watershed. Elevation ranges from sea level at the river mouth to more than in the mountains, and temperatures vary with elevation. The highest peak is Mount Rainier, at. High elevations have cold winters and short cool summers; interior regions are subject to great temperature variability and severe droughts.

Geographic entities mentioned:
surface_form: Mount Rainier
instance_of: Mountain
countries: United States
coordinates: lat: 46.85166666666667
lon: -121.76027777777777
To the northeast, mostly along the southern border between British Columbia and Alberta, the Continental Divide separates the Columbia watershed from the Nelson-Lake Winnipeg-Saskatchewan watershed, which empties into Hudson Bay.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
The Mississippi and Nelson watersheds are separated by the Laurentian Divide, which meets the Continental Divide at Triple Divide Peak near the headwaters of the Columbia's Flathead River tributary. This point marks the meeting of three of North America's main drainage patterns, to the Pacific Ocean, to Hudson Bay, and to the Atlantic Ocean via the Gulf of Mexico.

Geographic entities mentioned:
surface_form: Laurentian Divide
instance_of: Landform
countries: United States
Canada
KBPL (107.9 FM, &quot;107.9 KBPI South&quot;) is a radio station licensed to Pueblo, Colorado, and serving the Colorado Springs–Pueblo radio market. Owned by iHeartMedia, it broadcasts an active rock format. The transmitter is located on Cheyenne Mountain amid other TV and FM towers for stations in the Colorado Springs-Pueblo market. History. The station first signed on as KRYT on March 3, 1987.

Geographic entities mentioned:
surface_form: Cheyenne Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.737194444444
lon: -104.881
On July 13, 2009, Clear Channel flipped KDZA-FM to album rock and moved the studios and offices to Colorado Springs. KDZA-FM switched to classic rock as &quot;Z107.9&quot; on November 30, 2011. A few years later, KDZA-FM got a boost in its coverage area when it was allowed to relocate its tower to Cheyenne Mountain. The height above average terrain (HAAT) increased from.

Geographic entities mentioned:
surface_form: Cheyenne Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.737194444444
lon: -104.881
Holuhraun. Holuhraun () is a lava field just north of the Vatnajökull ice cap, in the Icelandic Highlands, in Suður-Þingeyjarsýsla, Northeastern Region, Iceland. The lava field was created by fissure eruptions. After a research expedition in 1880, the lava field was initially called &quot;Kvislarhraun&quot;.

Geographic entities mentioned:
surface_form: Icelandic Highlands
instance_of: Plateau
countries: Iceland
coordinates: lat: 64.84
lon: -18.11
The main volume of the Jökulsá á Fjöllum river flows from the eastern side of Holuhraun, in the Kverkfjöll area. Hrímalda, Urðarháls and Kistufell are to the west of Holuhraun, with Dyngjuháls and Trölladyngja beyond. The Dyngjujökull glacier, which is part of Vatnajökull, is to the immediate south.

Geographic entities mentioned:
surface_form: Trölladyngja
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.893055555556
lon: -17.254722222222
The Dyngjujökull glacier, which is part of Vatnajökull, is to the immediate south. Holuhraun is about south of the Askja caldera, and the Bárðarbunga volcano is to the south-west of Holuhraun. Holuhraun is traversed by an unnumbered road, which connects to the Route F910 gravel road at both the east and the west ends. Volcanism.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
Holuhraun is traversed by an unnumbered road, which connects to the Route F910 gravel road at both the east and the west ends. Volcanism. Located at the northern and southern extensions of the Bárðarbunga and Askja fissure systems respectively, the soil is mainly composed of lavas derived from these volcanoes, either in the form of flows or alluvial deposits of volcanic origin.

Geographic entities mentioned:
surface_form: Bárðarbunga
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.640833333333
lon: -17.527777777778
The geological configuration, along with the presence of nearby subglacial volcanoes such as Bárðarbunga and Grímsvötn, is responsible for the risk of jökulhlaups, which have affected Holuhraun repeatedly. Until 2014, the surface of the lava field was of an older lava flow, which was assumed to have erupted from a vent associated with Askja in 1797, but this is no longer accepted.

Geographic entities mentioned:
surface_form: Grímsvötn
instance_of: Mountain
countries: Iceland
coordinates: lat: 64.42
lon: -17.33
Also known for its good tasting spring water, &quot;Eldorado Springs&quot; bottled water is sold in stores around Colorado. Geography. The Eldorado Springs CDP has an area of, including of water. To the southwest is Eldorado Mountain. Demographics. The United States Census Bureau initially defined the for the

Geographic entities mentioned:
surface_form: Eldorado Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.914166666667
lon: -105.29472222222
The Ciguayos appear to have predated the agricultural Taíno who inhabited much of the island. The language appears to have been moribund at the time of Spanish contact, and within a century it was extinct. Ciguayo was spoken on the northeastern coast of the Roman Catholic Diocese of Magua from Nagua southward to at least the Yuna River, and throughout the Samana Peninsula. Lexicon.

Geographic entities mentioned:
surface_form: Yuna River
instance_of: Watercourse
countries: Dominican Republic
coordinates: lat: 18.787777777778
lon: -70.418055555556
Totenstein. Totenstein is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: totenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.824722222222
lon: 12.778611111111
A few miles away, further into the Black Mountains, is Partrishow or Patricio, which has an outstanding 11th-century church. Bruce Chatwin's book &quot;On the Black Hill&quot; depicts the upland livestock farming community over the past 100 years or so in the area.

Geographic entities mentioned:
surface_form: black hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.0072
lon: -3.05667
surface_form: black hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.4736
lon: -3.26833
Vale of Ewyas. The Vale of Ewyas () is the steep-sided and secluded valley of the River Honddu, in the Black Mountains of Wales and within the Brecon Beacons National Park. As well as its outstanding beauty, it is known for the ruins of Llanthony Priory, and for several noteworthy churches such as those at Capel-y-ffin and Cwmyoy.

Geographic entities mentioned:
surface_form: vale of ewyas
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.941
lon: -3.035
In 1932 he became the first recipient of the Johannes Bruehl Memorial Medal of the Asiatic Society of Bengal. Early life. Blatter was born in the canton of Appenzell Innerrhoden in northeastern Switzerland in a region near Mount Säntis. Having lost his father at an early age, he was raised by an uncle, a popular doctor in the municipality of Rebstein in the neighboring Canton of St. Gallen.

Geographic entities mentioned:
surface_form: Säntis
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.249167
lon: 9.343333
Miranda Peaks. The Miranda Peaks () are a line of about six peaks trending in a north–south direction on the south side of Uranus Glacier, in eastern Alexander Island, Antarctica. They were photographed by Lincoln Ellsworth on November 23, 1935, in the course of a trans-Antarctic flight and were plotted from the air photos by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: miranda peaks
instance_of: Mountain
coordinates: lat: -71.4667
lon: -68.6
Miranda Peaks. The Miranda Peaks () are a line of about six peaks trending in a north–south direction on the south side of Uranus Glacier, in eastern Alexander Island, Antarctica. They were photographed by Lincoln Ellsworth on November 23, 1935, in the course of a trans-Antarctic flight and were plotted from the air photos by W.L.G. Joerg.

Geographic entities mentioned:
surface_form: miranda peaks
instance_of: Mountain
coordinates: lat: -71.4667
lon: -68.6
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Korzok Monastery. Korzok, དཀོར་མཛོད་ (wylie dkor-mdzod) is a Tibetan Buddhist monastery belonging to the Drukpa Lineage. It is located in the Korzok village, on the northwestern bank of Tso Moriri, a lake in Leh District of Ladakh, a union territory of India. The gompa (monastery), at, houses a Shakyamuni Buddha and other statues. It is home to about seventy monks.

Geographic entities mentioned:
surface_form: Tso Moriri
instance_of: Lake
countries: India
coordinates: lat: 32.9
lon: 78.3
Summer temperatures in the area reach a high of and a low of. Local festival. The Korzok Gu-stor festival is held at the monastery and attracts many Chang-pa, the Tibetan plateau nomadic herdsmen. At the festival masks are worn by the dancers to represent the Dharmapalas (guardian divinities of the Buddhist pantheon), and the patron divinities of the Drukpa sect of Tibetan Buddhism.

Geographic entities mentioned:
surface_form: Tibetan plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
General Carleton escaped from Montreal, and made his way to Quebec City to prepare its defences against an anticipated attack. Background. Fort Saint-Jean guarded the entry to the province of Quebec on the Richelieu River at the northern end of Lake Champlain. When Benedict Arnold and Ethan Allen captured Fort Ticonderoga and raided Fort St.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
British defensive preparations. Fort St. Jean had been under preparations for an attack from the south ever since Arnold's raid on Fort St. Jean on May 18, in which he captured its small garrison and Lake Champlain's only large military ship. When news of that raid reached Montreal, 140 men under the command of Major Charles Preston were immediately dispatched to hold the fort.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
&quot;Constructed in 1743 by M. de Léry under orders from Governor la Galissonnière. This post was for all the military expeditions towards Lake Champlain. In August 31, 1760, Commandant de Roquemaure had it blown up in accordance with orders from the Governor de Vaudreuil in order to prevent its falling into the hands of the English. Rebuilt by Governor Carleton, in 1773.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
However, the department is largely focused on the conservation and allotment of harvests of salt water fisheries on the Atlantic, Pacific and Arctic coasts of Canada. The department works toward the conservation and protection of inland freshwater fisheries, such as on the Great Lakes and Lake Winnipeg, through cooperative agreements with various provinces.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Thomas Hodgkin, probably following Rodrigo Jiménez de Rada, placed the battle at Jerez de la Frontera. Joaquín Vallvé, studying toponymy, puts the engagement on the banks of the Guadarranque, which he says might derive from &quot;Wad al-Rinq&quot; (Roderic's river). It has recently been argued that the battle took place in a field bordering the Almodóvar River, in Province of Cádiz. Clash.

Geographic entities mentioned:
surface_form: Guadarranque
instance_of: Watercourse
countries: Spain
coordinates: lat: 36.178461111111
lon: -5.4141027777778
Violence soon followed, with the use of muskets, pistols, and cannons by the British. A number of Tsimshian were killed, wounded, and taken captive. Also during their time at Calamity Bay the British used boats to explore the complex waterways of the region, including Principe Channel, Douglas Channel, and Laredo Sound, in the process producing the first significant maps of this part of the coast.

Geographic entities mentioned:
surface_form: Douglas Channel
instance_of: Watercourse
countries: Canada
coordinates: lat: 53.666666666667
lon: -129.13333333333
Kendall is at the junction of Washington State Route 542 (the Mount Baker Highway) and State Route 547, which leads over a low pass on the northeastern flank of Sumas Mountain to connect to the town of Sumas and the border crossing with Abbotsford, British Columbia, Canada. The community of Maple Falls is three miles east along the Mount Baker Highway, which leads to the Mount Baker Ski Area.

Geographic entities mentioned:
surface_form: Sumas Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.9118
lon: -122.222
Spanish East Indies. During the Spanish colonial period, the lesser arms of the Spanish Sovereign were used. The seal of Manila was also issued under royal decree by Philip II (for whom the islands were named) in 1596. Note that the Pillars of Hercules or the Golden Fleece were not always displayed and the arms themselves were sometimes solely used. First Philippine Republic.

Geographic entities mentioned:
surface_form: Pillars of Hercules
instance_of: Landform
countries: Morocco
Spain
Gibraltar
coordinates: lat: 36
lon: -5.35
The conflict moved to some areas in the Beqaa Valley, and it reached its climax when some Druze besieged the emir in the Deir al-Qamar Palace and then stormed him and arrested the emir and mistreated him. The Ottomans seized this opportunity and dealt their final blow.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Torrgårdsvatten. Torrgårdsvatten is a lake in Lilla Edet Municipality in the province of Bohuslän and is part of the main catchment area of the Göta River.

Geographic entities mentioned:
surface_form: torrgårdsvatten
instance_of: Lake
countries: Sweden
coordinates: lat: 58.0453
lon: 12.0542
The map shows no noticeable difference from the 1750 map, except that a stream is seen connecting Torrgårdsvatten with Rödvatten (no dam was drawn, but neither was the dam at Stendammen). In 1780 Wenngren had sold the mill, which then had financial problems. This may have led to reduced maintenance of the dam, so water could once again flow to Rödvatten.

Geographic entities mentioned:
surface_form: torrgårdsvatten
instance_of: Lake
countries: Sweden
coordinates: lat: 58.0453
lon: 12.0542
Udea hamalis. &quot;Udea hamalis&quot; is a species of moth in the family Crambidae described by Carl Peter Thunberg in 1788. It is found from Fennoscandia south to Switzerland and Ukraine and from France east to Russia. The wingspan is 16–21 mm. The larvae feed on &quot;Vaccinium&quot;, &quot;Oxalis&quot; and &quot;Anemone&quot; species.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Bayankhongor contains two mountain ranges, the Khangai Mountains in the north and the Gobi Altai Mountains in the central region. Ikh Bogd, the aimag's tallest mountain at 3957 meters, is part of the Gobi Altai range and is located outside of Bogd sum.

Geographic entities mentioned:
surface_form: Ikh Bogd
instance_of: Mountain
countries: Mongolia
coordinates: lat: 44.995
lon: 100.23083333333
Ikh Bogd, the aimag's tallest mountain at 3957 meters, is part of the Gobi Altai range and is located outside of Bogd sum. The largest lakes in Bayankhongor are Orog Nuur and Böön Tsagaan Nuur, which are found in the central semi-desert region of the aimag (the Valley of Lakes between the Khangai and Gobi Altai ranges), as are several other lakes.

Geographic entities mentioned:
surface_form: Orog Nuur
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.055
lon: 100.70472222222
surface_form: Böön Tsagaan Nuur
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.5961
lon: 99.142
The Gobi bear population is estimated at less than 50 animals. On the other hand, Bayankhongor residents have been heard to say that the aimag has the most marmots out of any aimag. The middle salt lake depression plane, particularly areas like &quot;Boon Tsaagan Nuur&quot; and &quot;Orog Nuur&quot; are excellent birding areas with endangered birds such as the Dalmatian pelican and relict gull.

Geographic entities mentioned:
surface_form: Boon Tsaagan Nuur
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.5961
lon: 99.142
surface_form: Orog Nuur
instance_of: Lake
countries: Mongolia
coordinates: lat: 45.055
lon: 100.70472222222
The caravan of PLA fighters, Maoist activists and civilian &quot;volunteers&quot; marched through days and nights, across the forests, fields and snowy mountains of Dhawalagiri region, stopping for short times only at the designated rest-stops where local villagers had been &quot;volunteered&quot; to cook for them and provide shelter.

Geographic entities mentioned:
surface_form: Dhawalagiri region
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.696666666666665
lon: 83.49
Gasconade River. The Gasconade River is about long and is located in central and south-central Missouri. The Gasconade River begins in the Ozarks southwest of Hartville in Wright County and flows generally north-northeastwardly through Wright, Laclede, Pulaski, Phelps, Maries, Osage and Gasconade counties, through portions of the Mark Twain National Forest.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The river joins the Missouri River at the city of Gasconade at. The river follows a meandering course through the Ordovician age dolomite and sandstone bedrock of the Ozark Salem Plateau creating spectacular bluffs and incised meanders along the way. Numerous springs and caves occur within the drainage area and along the river course.

Geographic entities mentioned:
surface_form: Salem Plateau
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
It is situated in the Puno Region, Lampa Province, Vilavila District, and in the Melgar Province, Ayaviri District. Wisa Wisa lies near the mountains Pukarani &quot;(Pucarani)&quot; in the northwest and Wallatani &quot;(Huallatane)&quot; in the southeast, southwest of a place called Wisa Wisa &quot;(Huisa Huisa)&quot;.

Geographic entities mentioned:
surface_form: huallatane
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4039
lon: -71.9161
surface_form: wallatani
instance_of: Mountain
countries: Peru
coordinates: lat: -15.4039
lon: -71.9161
surface_form: wisa wisa
instance_of: Mountain
countries: Peru
coordinates: lat: -15.1369
lon: -70.5878
surface_form: wisa wisa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.1178
lon: -70.7881
surface_form: pucarani
instance_of: Mountain
countries: Peru
coordinates: lat: -15.24111111
lon: -70.27777778
surface_form: pukarani
instance_of: Mountain
countries: Peru
coordinates: lat: -15.24111111
lon: -70.27777778
Wisa Wisa (Lampa-Melgar). Wisa Wisa (Aymara &quot;wisa&quot; first born twin, Quechua &quot;wiksa, wisa&quot; belly, the reduplication indicates that there is a group or a complex of something, Hispanicized spelling &quot;Visa Visa&quot;) is a mountain in the Andes of Peru, about high.

Geographic entities mentioned:
surface_form: wisa wisa
instance_of: Mountain
countries: Peru
coordinates: lat: -15.1369
lon: -70.5878
surface_form: wisa wisa
instance_of: Mountain
countries: Peru
coordinates: lat: -14.1178
lon: -70.7881
Cheops Mountain, is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Cheops Mountain is situated in the Hermit Range, and the summit provides a good view of the Hermit and Sir Donald Ranges. Its nearest higher peak is Ursus Major Mountain, to the northwest. Cheops is visible from Highway 1, the Trans-Canada Highway at Rogers Pass. History.

Geographic entities mentioned:
surface_form: Ursus Major Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29991
lon: -117.60225
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
In the late afternoon of March 4, 1910, an avalanche swept down the slopes of Cheops, burying the railroad tracks in snow. The men were working to clear the tracks when shortly before midnight the deadly slide hit, coming from the opposite side of the valley down Avalanche Mountain. The mountain's current name was officially adopted in 1951 when approved by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: Avalanche Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2881
lon: -117.469
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain's current name was officially adopted in 1951 when approved by the Geographical Names Board of Canada. Prior to that it was known as Mount Cheops. The peak was named by Otto Julius Klotz for its resemblance to the Pyramid of Cheops. Climate. Based on the Köppen climate classification, Cheops Mountain has a subarctic climate with cold, snowy winters, and mild summers.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Cheops Mountain. Cheops Mountain, is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Cheops Mountain is situated in the Hermit Range, and the summit provides a good view of the Hermit and Sir Donald Ranges. Its nearest higher peak is Ursus Major Mountain, to the northwest.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: cheops mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.28321
lon: -117.55224