Sarmila/GeoWiki-Features huggingface dataset:
The fungal parasite, Hemigrapha astericus, a native of Australia and South America, was first recorded in the northern hemisphere in Derryclare Wood. In 2005, 19 Irish red squirrels were translocated from Portumna Forest Park to Derryclare Wood as part of a programme to protect the species in Ireland. Hill walking.

Geographic entities mentioned:
surface_form: derryclare
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49665
lon: -9.78599
Hill walking. Derryclare is one of the more accessible Twelve Bens, being situated near the N59 road, and a number of routes are available from the &quot;Glencoaghan Valley&quot; side in the west, or the &quot;Derryclare Nature Reserve&quot; side in the east, that climb to the summit and back.

Geographic entities mentioned:
surface_form: derryclare
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49665
lon: -9.78599
surface_form: derryclare
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49665
lon: -9.78599
Derryclare is also often climbed as part of the popular 16–kilometre 8–9 hour &quot;Glencoaghan Horseshoe&quot;, considered one of Ireland's best hill-walks. Rock climbing.

Geographic entities mentioned:
surface_form: derryclare
instance_of: Mountain
countries: Ireland
coordinates: lat: 53.49665
lon: -9.78599
Katrana. The katrana (&quot;Rheocles alaotrensis&quot;) is a species of fish in the Bedotiidae family. It is endemic to the basin of Lake Alaotra in Madagascar. Its natural habitats are rivers and freshwater lakes. It is threatened by habitat loss. This species was described by Jacques Pellegrin as &quot;Atherina alaotrensis&quot; with the type locality of Lake Aloatra.

Geographic entities mentioned:
surface_form: Lake Alaotra
instance_of: Lake
countries: Madagascar
coordinates: lat: -17.5
lon: 48.5
Treaty 5. &quot;Treaty Five&quot; is a treaty between Queen Victoria and Saulteaux and Swampy Cree non-treaty band governments and peoples around Lake Winnipeg in the District of Keewatin. Much of what is today central and northern Manitoba was covered by the treaty, as were a few small adjoining portions of the present-day provinces of Saskatchewan and Ontario.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Hakea chromatropa. &quot;Hakea chromatropa&quot; is a species of shrub found in Southwest Australia. The distribution is restricted to an area around Wongan Hills, where it is found on gravelly loam in open shrubland. The flowers are white or creamy, becoming pink, and without a scent. Description.

Geographic entities mentioned:
surface_form: Wongan Hills
instance_of: Mountain
countries: Australia
coordinates: lat: -30.8
lon: 116.617
Other outcrops of the Loma Gorda Formation have been noted east of the Magdalena River northeast of Honda, west of Nariño, west across the Magdalena River in San Luis, Tolima, between the Tetuán and Saldaña Rivers west of Coyaima and east and west of Ataco, to the east of the Prado River reservoir, north and west of Aipe, surrounding Alpujarra, Tolima, south of Palermo, Huila, displaced by the Baché Fault, east of Iquira, north of Yaguará, south of La Plata where the formation is cut by the Itaibe Fault, a small patch east of Gigante, Huila, northwest and northeast of San Agustín, and north of Timaná surrounding the Magdalena River.

Geographic entities mentioned:
surface_form: Saldaña River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 3.9933333333333
lon: -74.871944444444
Tibet Institute Rikon. The Tibet Institute Rikon is a Tibetan monastery located in Zell-Rikon im Tösstal in the Töss Valley in Switzerland. It was established as a non-profit foundation in 1968, because Swiss laws resulting from the 19th century secularization movement did not allow for the establishment of new monasteries until 1973. History.

Geographic entities mentioned:
surface_form: Töss Valley
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.350277777778
lon: 8.935
Thompson Center (Atrium Mall). Additional scenes were shot at Yerkes Observatory in Williams Bay, Wisconsin, on Geneva Lake in southern Wisconsin, interiors of the U.S. Capitol were shot at the Wisconsin State Capitol, in Madison, Wisconsin, at Inland Steel Company (now known as Cleveland-Cliffs Inc.) in East Chicago, Indiana, and at a private residence in Barrington Hills, Illinois.

Geographic entities mentioned:
surface_form: Geneva Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.59
lon: -88.435
In geographical terms, the cantref was very variable, including fertile land and rich pastures on the shore of the Menai and in the valleys, a number of woods on the slopes and mountains to the south, and the highest mountains in Wales such as Snowdon and Tryfan. Arfon comprised two commotes, which were apparently created later in its history.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
surface_form: Tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
Anchialus Glacier. Anchialus Glacier (,) is the 8.5 km long and 3.4 km wide glacier in Sostra Heights on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of lower Embree Glacier, east of Sabazios Glacier, south of lower Newcomer Glacier and northwest of Vit Ice Piedmont.

Geographic entities mentioned:
surface_form: Sostra Heights
instance_of: Plateau
coordinates: lat: -77.8833
lon: -85.4667
It is situated north of lower Embree Glacier, east of Sabazios Glacier, south of lower Newcomer Glacier and northwest of Vit Ice Piedmont. The glacier drains the northeast slopes of Mount Malone and the west slopes of Bracken Peak, flows northwards and joins Newcomer Glacier east of Mount Lanning. The glacier is named after the ancient town of Anchialus in Southeastern Bulgaria. Location.

Geographic entities mentioned:
surface_form: Mount Malone
instance_of: Mountain
coordinates: lat: -77.8667
lon: -85.6
surface_form: Bracken Peak
instance_of: Mountain
coordinates: lat: -77.85
lon: -85.4
surface_form: Mount Lanning
instance_of: Mountain
coordinates: lat: -77.783305555556
lon: -85.75
Etymology. This specific epithet ‘taborans’ refers to the Mount Tabor Ashram, Zoology Research Centre, St. Stephen's College, Pathanapuram, the Headquarters of the Institution where this research was conducted. Distribution. Known only from Munroe Island, Ashtamudi Estuary, Kerala, India.

Geographic entities mentioned:
surface_form: Ashtamudi Estuary
instance_of: Lake
countries: India
coordinates: lat: 8.9833333333333
lon: 76.6
Thief River. The Thief River is a tributary of the Red Lake River in northwestern Minnesota in the United States. Via the Red Lake River, the Red River of the North, Lake Winnipeg and the Nelson River, it is part of the watershed of Hudson Bay. Course.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Via the Red Lake River, the Red River of the North, Lake Winnipeg and the Nelson River, it is part of the watershed of Hudson Bay. Course. The Thief River flows from Thief Lake in Thief Lake Township of northeastern Marshall County and flows generally south-southwestwardly to Thief River Falls in northwestern Pennington County. The river flows through the Agassiz National Wildlife Refuge.

Geographic entities mentioned:
surface_form: Thief Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.490555555556
lon: -95.891111111111
On November 4, 1929, Gould and five companions began a grueling 2½ month, 1500-mile dog-sledge journey into the Queen Maud Mountains, with the primary purpose of providing ground support and possible emergency assistance for Byrd's historic first airplane flight over the South Pole and a secondary purpose of conducting the first geological and glaciological survey of an area that Gould called &quot;a veritable paradise for a geologist.&quot;
After the flight over the Pole in November 1929, Gould and his companions climbed Mount Fridtjof Nansen to investigate its geology.

Geographic entities mentioned:
surface_form: Mount Fridtjof Nansen
instance_of: Mountain
coordinates: lat: -85.35
lon: -167.55
The coasts rivers of Laguna give the region a quick method of transportation and make trade with foreign merchants easier. Laguna has been investigated multiple times by several archeological teams and has yielded several finds. Henry Otley Beyer had studied the shores of Laguna de Bay, particularly near the northern regions of Rizal and Manila.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Mount Bindyego was also named by Mitchell on the same day based on the name provided by Aboriginal informants. The name &quot;Brinsop&quot; comes from the village of Brinsop in Herefordshire, England, which possibly means brown valley (brun/hop). The name &quot;Ona Ona&quot; was assigned on 29 April 1915 by the Queensland Railways Department, an Aboriginal phrase, meaning &quot;boxtree flat&quot;.

Geographic entities mentioned:
surface_form: brown valley
instance_of: Landform
coordinates: lat: -75.6333
lon: -132.2
Mount Overlord. Mount Overlord is a very large mountain which is an extinct stratovolcano, situated at the northwest limit of Deception Plateau, 50 miles inland from the Ross Sea and just east of the head of Aviator Glacier in Victoria Land. Its asymmetrical cone is on the edge of a plateau above Aviator Glacier. While most of the cone is ice-covered, Mount Overlord does have a diameter caldera.

Geographic entities mentioned:
surface_form: Deception Plateau
instance_of: Landform
coordinates: lat: -73.25
lon: 164.833
The state highway runs from MD 26 in Libertytown north to Pen Mar Road in Fort Ritchie. MD 550 runs southeast&ndash;northwest across central Frederick County, connecting Fort Ritchie in the northeastern corner of Washington County and Libertytown with the towns of Thurmont and Woodsboro and the smaller communities of Creagerstown and Sabillasville. South of the highway's junction with U.S.

Geographic entities mentioned:
surface_form: Catoctin Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.6478
lon: -77.4664
Mount Eniwa. is an active volcano located in Shikotsu-Tōya National Park in Hokkaido, Japan. It sits opposite Mount Tarumae and Mount Fuppushi on the shores of Lake Shikotsu, the caldera lake that spawned the volcanoes. Mount Eniwa is the tallest of the three volcanoes. Eruptions. The last eruption occurred around the start of the 18th century (c. 1700 ±30 years).

Geographic entities mentioned:
surface_form: Mount Fuppushi
instance_of: Mountain
countries: Japan
coordinates: lat: 42.71694444
lon: 141.35888889
surface_form: Lake Shikotsu
instance_of: Lake
countries: Japan
coordinates: lat: 42.75
lon: 141.33333333333
Known for its rugged beauty and remote access, Paguekwash Point is popular among hikers and nature enthusiasts seeking a more secluded experience within the Grand Canyon's vast wilderness. It is located on the North Rim, about 4.5 miles northwest of Mount Sinyella and across the Colorado River. An excursion of the west-flowing Colorado is ~1.0 mile east, and also ~1.5 miles west.

Geographic entities mentioned:
surface_form: Mount Sinyella
instance_of: Mountain
countries: United States
coordinates: lat: 36.2997
lon: -112.70575
Jbel Bou Naceur. Mount Bou Nasser or &quot;Jbel Bou Naceur&quot; is a mountain in Sefrou Province, Fès-Meknès, Morocco. Its altitude is 3,340 meters. Geography. It is the highest peak in the Middle Atlas, located near Tirnest to the south and Tinesmet to the north.

Geographic entities mentioned:
surface_form: bou naceur
instance_of: Mountain
countries: Morocco
coordinates: lat: 33.5665
lon: -3.8896
surface_form: jbel bou naceur
instance_of: Mountain
countries: Morocco
coordinates: lat: 33.5665
lon: -3.8896
Galba, too, was in search for booty, and slaughtered a large number of Lusitanians by treachery. He, too, was not held to account. Lucullus built a temple dedicated to Fortuna in the Velabrum to celebrate his &quot;success&quot;. He adorned it with statues which Lucius Mummius Achaicus, who defeated the Achaean League in Greece, had lent him.

Geographic entities mentioned:
surface_form: Velabrum
instance_of: Valley
countries: Italy
coordinates: lat: 41.88916667
lon: 12.48194444
Kosvinsky Kamen. Mount Kosvinsky Kamen, Kosvinsky Mountain, Kosvinski Mountain, Kosvinsky Rock or Rostesnoy Rock () is a mountain in the northern Urals, Sverdlovsk Oblast, Russia. Its summit is bare of vegetation with an uneven rocky surface and small lakes fed by melting snow. The Kosva River flows from the mountain, hence the name.

Geographic entities mentioned:
surface_form: kamen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 69.133333333333
lon: 95.066666666667
surface_form: kosvinsky kamen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.516666666667
lon: 59.05
The timing of the Kosvinsky completion date is regarded as one explanation for US interest in a new nuclear bunker buster and the declaration of the deployment of the B61 Mod 11 in 1997: Kosvinsky is protected by about of granite. US analysts believe that the command post of the Perimeter system is in the bunker under Kosvinsky Kamen mountain.

Geographic entities mentioned:
surface_form: kamen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 69.133333333333
lon: 95.066666666667
surface_form: kosvinsky kamen
instance_of: Mountain
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 59.516666666667
lon: 59.05
He is married with three children and lives in the Lake Macquarie suburb of Warners Bay. State politics. In 2011, Cornwell contested the normally safe Labor seat of Charlestown in the Hunter Valley. He defeated Labor incumbent Matthew Morris with a swing of 25.2 per cent and winning the seat with 59.9 per cent of the vote on a two party preferred basis.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Aubad. The Aubad is a man-made lake in Tulln on the Danube, Austria. It is the centerpiece of a recreational park (&quot;Erholungspark&quot;) that includes facilities for swimming, as well as a area for sport and leisure activities—such as soccer, volleyball, baseball and basketball—and of woodland. The lake and park are popular summertime resorts for both townspeople and tourists.

Geographic entities mentioned:
surface_form: aubad
instance_of: Lake
countries: Austria
coordinates: lat: 48.3329
lon: 16.0768
It has a total height of 35 metres. The observation deck is 30 metres high and can be reached via a stairway with 150 steps. Walking. Several footpaths lead to the Platte. The best-known is that from the &quot;Marktredwitzer Haus&quot; to the Weißenstein Ruins and then on to the Platte. Another of the many paths leads from the &quot;Waldhaus&quot; to the Platte.

Geographic entities mentioned:
surface_form: weißenstein
instance_of: Mountain
countries: Germany
coordinates: lat: 50.13
lon: 11.6904
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 49.91
lon: 12.0531
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 50.0186
lon: 11.8906
Platte (Steinwald). At, the Platte is the highest mountain in the Steinwald, a forest in the Fichtel mountain range in central Germany. The Platte is a popular walking destination, not least because of the Upper Palatinate Tower, which is located on its summit. It is climbable and offers good views of the surrounding region. The Upper Palatinate Tower.

Geographic entities mentioned:
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 49.91
lon: 12.0531
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 50.0186
lon: 11.8906
It has a total height of 35 metres. The observation deck is 30 metres high and can be reached via a stairway with 150 steps. Walking. Several footpaths lead to the Platte. The best-known is that from the &quot;Marktredwitzer Haus&quot; to the Weißenstein Ruins and then on to the Platte. Another of the many paths leads from the &quot;Waldhaus&quot; to the Platte.

Geographic entities mentioned:
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 49.91
lon: 12.0531
surface_form: platte
instance_of: Mountain
countries: Germany
coordinates: lat: 50.0186
lon: 11.8906
On its south side the mountain drops steeply (50% slope) to Ingalls Creek, which flows about below the summit. The mountain, which lies in the Alpine Lakes Wilderness, bordered by Colchuck Peak, Little Annapurna, and Cannon Mountain, is composed of a granite formation that creates the Stuart Range.

Geographic entities mentioned:
surface_form: Colchuck Peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.476944444444
lon: -120.845
surface_form: Little Annapurna
instance_of: Mountain
countries: United States
coordinates: lat: 47.46817
lon: -120.81453
surface_form: cannon mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1565
lon: -71.6984
surface_form: little annapurna
instance_of: Mountain
countries: United States
coordinates: lat: 47.46817
lon: -120.81453
surface_form: colchuck peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.476944444444
lon: -120.845
surface_form: cannon mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5025
lon: -120.80194444444
Dragontail Peak. Dragontail Peak, also known as Dragon Tail, is a mountain in the Stuart Range, in Chelan County, Washington. While climbing an adjacent peak, Lex Maxwell, Bob McCall, and Bill Prater remarked that the needles on the crest, southwest of the summit, resembled a &quot;dragon tail&quot;. The name was officially accepted in 1955.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: dragontail peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.4787
lon: -120.833
The mountain, which lies in the Alpine Lakes Wilderness, bordered by Colchuck Peak, Little Annapurna, and Cannon Mountain, is composed of a granite formation that creates the Stuart Range. Dragontail is the second highest mountain in the range, second only to Mount Stuart which lies to the west and reaches.

Geographic entities mentioned:
surface_form: mount stuart
instance_of: Mountain
countries: United States
coordinates: lat: 47.4753
lon: -120.901
Dragontail Peak. Dragontail Peak, also known as Dragon Tail, is a mountain in the Stuart Range, in Chelan County, Washington. While climbing an adjacent peak, Lex Maxwell, Bob McCall, and Bill Prater remarked that the needles on the crest, southwest of the summit, resembled a &quot;dragon tail&quot;. The name was officially accepted in 1955.

Geographic entities mentioned:
surface_form: dragontail peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.4787
lon: -120.833
The two needles, on ridge southwest of the summit which gave rise to its name, serve as formidable alpine climbing objectives that demand more than 20 pitches of sustained climbing. The area around Dragontail Peak is dominated by wilderness and is protected from development. The Enchantments, to northeast of Dragontail, is an area of towering peaks, year-round snow, and alpine lakes.

Geographic entities mentioned:
surface_form: dragontail peak
instance_of: Mountain
countries: United States
coordinates: lat: 47.4787
lon: -120.833
Dragontail Peak. Dragontail Peak, also known as Dragon Tail, is a mountain in the Stuart Range, in Chelan County, Washington. While climbing an adjacent peak, Lex Maxwell, Bob McCall, and Bill Prater remarked that the needles on the crest, southwest of the summit, resembled a &quot;dragon tail&quot;. The name was officially accepted in 1955.

Geographic entities mentioned:
surface_form: needles
instance_of: Mountain
countries: United States
coordinates: lat: 43.8369
lon: -103.549
surface_form: the needles
instance_of: Mountain
countries: United States
coordinates: lat: 36.109
lon: -118.485
Herschel Heights. The Herschel Heights () are a complex of nunataks of which Mimas Peak on the east is the highest, located southwest of the Enceladus Nunataks and near the head of Saturn Glacier in southeastern Alexander Island, Antarctica.

Geographic entities mentioned:
surface_form: Mimas Peak
instance_of: Mountain
coordinates: lat: -71.9333
lon: -69.6
surface_form: Enceladus Nunataks
instance_of: Mountain
coordinates: lat: -71.716666666667
lon: -69.45
surface_form: herschel heights
instance_of: Mountain
coordinates: lat: -71.8833
lon: -69.6333
surface_form: alexander
instance_of: Mountain
coordinates: lat: -63.3039
lon: -55.80564
Herschel Heights. The Herschel Heights () are a complex of nunataks of which Mimas Peak on the east is the highest, located southwest of the Enceladus Nunataks and near the head of Saturn Glacier in southeastern Alexander Island, Antarctica.

Geographic entities mentioned:
surface_form: herschel heights
instance_of: Mountain
coordinates: lat: -71.8833
lon: -69.6333
Joerg. The heights were named by the UK Antarctic Place-Names Committee from association with Mimas and Enceladus, after Sir William Herschel, the British astronomer who discovered these two satellites of Saturn in 1789.

Geographic entities mentioned:
surface_form: william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833
Staff consisted of eight teachers including one head teacher, and approximately 133 students in grades 9-11 (secondary III-V). MIND currently has five teachers and 55 students. In 1999, MIND moved to its current location in the top floor of the Bancroft elementary school building at Mont Royal and St. Urbain, in the shadow of Mount Royal.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
Bride's Pool. Bride's Pool () is a small river in the northeastern New Territories, Hong Kong near Tai Mei Tuk. The river is characterized by a string of waterfalls with plunge pools. Mirror Pool is also located nearby. Legend and namesake. Legend has it that a bride was being carried in a sedan by four porters on her way to meet her groom in stormy weather.

Geographic entities mentioned:
surface_form: bride's pool
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 22.503214
lon: 114.237047
Legend has it that a bride was being carried in a sedan by four porters on her way to meet her groom in stormy weather. As they passed the pool, one of the porters slipped and the bride fell into the pool and drowned. Therefore, the pool was named Bride's Pool in memory of the bride. Transport. Bride's Pool is located in the North East Region of the New Territories in Plover Cove Country Park.

Geographic entities mentioned:
surface_form: bride's pool
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 22.503214
lon: 114.237047
Therefore, the pool was named Bride's Pool in memory of the bride. Transport. Bride's Pool is located in the North East Region of the New Territories in Plover Cove Country Park. It can be accessed either by car or by public transport. By public transport take the MTR East Rail (formerly KCR East Rail) to Tai Po Market station and board minibus 20R. The bus will terminate at Wu Kau Tang.

Geographic entities mentioned:
surface_form: bride's pool
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 22.503214
lon: 114.237047
On Sundays and public holidays, the Kowloon Motor Bus operates the route 275R from Tai Po Market station to the Pool. The Bride's Pool Trail lies past Tai Mei Tuk and shortly before Wu Kau as the bus heads north. If the bus terminates short of the Pool at Tai Mei Tuk or minibus 20C (which also terminates at Tai Mei Tuk) is taken instead, the pool can be accessed by taxi or a 2-3 hour hike.

Geographic entities mentioned:
surface_form: bride's pool
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 22.503214
lon: 114.237047
Big Raven Plateau. The Big Raven Plateau is an intermontane plateau in Cassiar Land District of northwestern British Columbia, Canada. It lies on the Tahltan Highland and is surrounded by several valleys, including those of Mess Creek, Kakiddi Creek, Chakima Creek, Walkout Creek and the Klastline River.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
surface_form: Chakima Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
The plateau is in Mount Edziza Provincial Park, which is one of the largest provincial parks in British Columbia. Access to the Big Raven Plateau is mainly by aircraft or by a network of horse trails from surrounding roads. The Big Raven Plateau is volcanic in origin, consisting mostly of basaltic lava flows of the Mount Edziza volcanic complex that were erupted in the last 7.5 million years.

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: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
These lava flows are interbedded with rhyolite and trachyte which are in the form of rock fragments produced and ejected by explosive eruptions. The dominant feature on the Big Raven Plateau is Mount Edziza, an ice-covered stratovolcano reaching an elevation of.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The Big Raven Plateau is subdivided into at least 10 geological formations, each being the product of a distinct period of volcanic activity. Location. The Big Raven Plateau is located on the Tahltan Highland east of the Zagoddetchino massif and west of the mountainous Klastline Plateau in Cassiar Land District.

Geographic entities mentioned:
surface_form: Klastline Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.95
lon: -130.083
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Between the Zagoddetchino massif and the Big Raven Plateau is Mess Creek valley, which extends more than to the south where it separates the Boundary Ranges of the Coast Mountains in the west from the Spectrum Range and Arctic Lake Plateau in the east.

Geographic entities mentioned:
surface_form: Mess Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: Arctic Lake Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.3
lon: -130.767
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Between the Big Raven and Klastline plateaus is the north–south trending Kakiddi Creek valley, which includes a number small lakes such as Nuttlude Lake, Kakiddi Lake, Mowchilla Lake and Mowdade Lake.

Geographic entities mentioned:
surface_form: Kakiddi Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.872778
lon: -130.425556
This intermontane plateau lies at the northern end of the Mount Edziza volcanic complex, which consists of a group of overlapping shield volcanoes, stratovolcanoes, lava domes and cinder cones that have formed over the last 7.5 million years.

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
Four central volcanoes occur along the north–south trending axis of the volcanic complex; the two youngest central volcanoes, Mount Edziza and Ice Peak, are on the Big Raven Plateau. In addition to the Big Raven Plateau, the volcanic complex also includes the Arctic Lake and Kitsu plateaus, as well as the Spectrum Range to the south.

Geographic entities mentioned:
surface_form: Mount Edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: Ice Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6906
lon: -130.635
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Four central volcanoes occur along the north–south trending axis of the volcanic complex; the two youngest central volcanoes, Mount Edziza and Ice Peak, are on the Big Raven Plateau. In addition to the Big Raven Plateau, the volcanic complex also includes the Arctic Lake and Kitsu plateaus, as well as the Spectrum Range to the south.

Geographic entities mentioned:
surface_form: Kitsu
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Drainage. As a part of the Mount Edziza volcanic complex, the Big Raven Plateau is drained entirely by streams within the Stikine River watershed. The northeastern portion of the Big Raven Plateau is drained by Tsecha Creek, which flows to the northeast.

Geographic entities mentioned:
surface_form: Tsecha Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.83296
lon: -130.42064
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
The northeastern portion of the Big Raven Plateau is drained by Tsecha Creek, which flows to the northeast. Draining the eastern side of the plateau are a series of east-flowing streams choked with glacial and landslide debris from rapidly eroding headwalls; from north to south these are Pyramid Creek, Tenchen Creek, Nido Creek, Tennaya Creek, Sorcery Creek and Shaman Creek.

Geographic entities mentioned:
surface_form: Tenchen Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.76636
lon: -130.43724
surface_form: Nido Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71636
lon: -130.47065
surface_form: Tennaya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
surface_form: Shaman Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: pyramid creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91673
lon: -118.05237
Nido Creek and Tennaya Creek flow into Nuttlude Lake whereas Sorcery Creek and Shaman Creek flow into Kakiddi Lake. Both lakes are expansions of Kakiddi Creek which flows north into the Klastline River, a tributary of the Stikine River. Elwyn Creek and its tributary, Kadeya Creek, drain the northwestern portion of the plateau; Elwyn Creek flows westward whereas Kadeya Creek flows to the northwest.

Geographic entities mentioned:
surface_form: Elwyn Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: Kadeya Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.79967
lon: -130.87063
surface_form: kadeya creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.79967
lon: -130.87063
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
Elwyn Creek and its tributary, Kadeya Creek, drain the northwestern portion of the plateau; Elwyn Creek flows westward whereas Kadeya Creek flows to the northwest. Northwest-flowing Taweh Creek and its tributary, the westward-flowing Sezill Creek, drain the southwestern and western portions of the plateau, respectively.

Geographic entities mentioned:
surface_form: Taweh Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: Sezill Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
The northern end of the Big Raven Plateau is drained by small, unnamed streams which flow north into the Klastline River; these streams are shallowly incised into the plateau. At the southern end of the Big Raven Plateau is a drainage divide between Chakima Creek, flowing east into the Kakiddi drainage, and Walkout Creek flowing west via Raspberry Creek into Mess Creek. Structure.

Geographic entities mentioned:
surface_form: Chakima Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.59966
lon: -130.42066
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
In contrast to the northern end of the Big Raven Plateau which is relatively smooth and uneroded, the eastern side has undergone extensive erosion, which has resulted in the creation of steep spurs with intervening valleys. A handful of these spurs are named on the southeastern side of the plateau; from north to south they are Idiji Ridge, Sorcery Ridge and Cartoona Ridge.

Geographic entities mentioned:
surface_form: Idiji Ridge
instance_of: Mountain
coordinates: lat: 57.67653055555555
lon: -130.6231527777778
surface_form: Sorcery Ridge
instance_of: Mountain
coordinates: lat: 57.65606944444444
lon: -130.61504166666666
surface_form: Cartoona Ridge
instance_of: Mountain
coordinates: lat: 57.60666666666667
lon: -130.6147222222222
Idiji Ridge extends east from the northern end of Tencho Glacier and is the namesake of Idiji Glacier, which exists to the northwest. Sorcery Ridge, which shares its name with adjacent Sorcery Creek, extends east from the southern end of Tencho Glacier. Cartoona Ridge lies between Chakima and Shaman creek valleys and shares its name with Cartoona Peak at the westernmost end of the ridge.

Geographic entities mentioned:
surface_form: Cartoona Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
Smaller features on the Big Raven Plateau include Hoia Bluff at the southwestern end of the plateau along Taweh Creek, Kaia Bluff and Cartoona Peak at the southeastern end of the plateau, Camp Hill near the southwestern edge of the plateau, Kana Cone on the extreme northern side of the plateau, Klastline Cone on the eastern side of the plateau near the head of Pyramid Creek and Tsekone Ridge at the northwestern end of the plateau near the head of Elwyn Creek canyon, as well as Ornostay and Koosick bluffs near the middle of the plateau adjacent to the head of Sezill Creek canyon.

Geographic entities mentioned:
surface_form: Tsekone Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.77
lon: -130.69
surface_form: Ornostay
instance_of: Mountain
countries: Canada
coordinates: lat: 57.699722222222
lon: -130.70388888889
surface_form: Koosick
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6739
lon: -130.725
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: sezill creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: cartoona peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.6067
lon: -130.615
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
surface_form: elwyn creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.78298
lon: -130.98722
surface_form: pyramid creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 52.91673
lon: -118.05237
Mount Edziza. Mount Edziza is a nearly symmetrical volcanic cone containing a nearly flat summit with an ice-filled, in diameter crater. The symmetry of the volcano is broken by several steep-sided lava domes, including Sphinx Dome, Glacier Dome, Triangle Dome and The Pyramid.

Geographic entities mentioned:
surface_form: Glacier Dome
instance_of: Mountain
countries: Canada
coordinates: lat: 56.4029
lon: -130.9166
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Although the eastern side of Mount Edziza has been deeply dissected by glacial erosion, less dissection has taken place on the southern and northwestern flanks of the volcano. Extending northwest from the northwestern flank of Mount Edziza is Pillow Ridge, which is named after its exposures of pillow lava. About south of the summit is Ice Peak, the southern peak of Mount Edziza.

Geographic entities mentioned:
surface_form: Pillow Ridge
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7594
lon: -130.652
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
Tennena Cone, Cocoa Crater, Coffee Crater, Keda Cone and The Saucer are the only named volcanic features in the Snowshoe Lava Field, which are in elevation.

Geographic entities mentioned:
surface_form: Tennena Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.68416666666667
lon: -130.66222222222223
surface_form: Cocoa Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.65
lon: -130.7
surface_form: Coffee Crater
instance_of: Mountain
countries: Canada
coordinates: lat: 57.63
lon: -130.67
The largest lava flow is about long and travelled to the northeast into the Kakiddi Creek and Klastline River valleys where it temporarily blocked both streams. From oldest to youngest, the cinder cones in this lava field are Sleet Cone, Storm Cone, the three Triplex Cones, Sidas Cone, Twin Cone, Moraine Cone, Eve Cone and Williams Cone, which range in elevation from.

Geographic entities mentioned:
surface_form: Sidas Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.8589
lon: -130.628
surface_form: Eve Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
surface_form: Williams Cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.78
lon: -130.599
surface_form: moraine
instance_of: Lake
countries: Canada
coordinates: lat: 51.3225
lon: -116.18555555555555
surface_form: twin
instance_of: Watercourse
countries: Canada
coordinates: lat: 56.72361111
lon: -131.21166667
The source of these lava flows was probably a cluster of vents further to the east called Sezill Volcano. In contrast, the air-fall pumice and ash flows probably originated from the more than in diameter Armadillo Peak caldera south of the Big Raven Plateau. Nido Formation. The Tenchen Member is the only stratigraphic unit of the Nido Formation comprising the Big Raven Plateau.

Geographic entities mentioned:
surface_form: Armadillo Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5383
lon: -130.56
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Williams Cone is the largest, reaching wide at its base and rising about on the northeastern side of Mount Edziza. Eve Cone contains a bowl-shaped crater at its summit and is one of the most symmetrical and best-preserved cinder cones in Canada, rising about above the central portion of the Desolation Lava Field. Stratigraphy.

Geographic entities mentioned:
surface_form: eve cone
instance_of: Mountain
countries: Canada
coordinates: lat: 57.81305555555556
lon: -130.67555555555555
Discharge at these hot springs may be linked to shallow hydrothermal systems driven by residual magmatic heat as they are adjacent to recently active volcanic centres on the plateau. Forming the southwestern edge of the Big Raven Plateau is the Mess Creek Escarpment, which extends at least to the south where it forms the western edge of the Kitsu Plateau. Landforms.

Geographic entities mentioned:
surface_form: kitsu plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.4667
lon: -130.75
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Pyramid Formation. Exposures of the 1.1-million year-old Pyramid Formation are limited only to the northeastern, eastern and southeastern ends of the Big Raven Plateau where it is in the form of rhyolite and trachyte domes, flows and pyroclastic breccia. The Pyramid at the northeastern end of the plateau consists of a roughly high trachyte dome whose base is slightly more than wide.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
The Pyramid at the northeastern end of the plateau consists of a roughly high trachyte dome whose base is slightly more than wide. Unlike other domes of the Pyramid Formation which have been either buried under younger lavas or greatly modified by erosion, The Pyramid has only been moderately eroded and is completely isolated from adjacent rocks.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Unlike other domes of the Pyramid Formation which have been either buried under younger lavas or greatly modified by erosion, The Pyramid has only been moderately eroded and is completely isolated from adjacent rocks. Sphinx Dome is a partially buried rhyolite dome adjacent to The Pyramid whose southern edge has been largely destroyed by headward stream erosion.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Isolated remnants of the rhyolitic Pharaoh Dome occur along the eastern and southeastern ends of the Big Raven Plateau between Tennaya Creek in the north and Cartoona Ridge in the south. A series of basaltic lava flows up to thick overlies a pyroclastic surge deposit of trachytic composition south and east of The Pyramid, both of which are also part of the Pyramid Formation. Ice Peak Formation.

Geographic entities mentioned:
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
surface_form: the pyramid
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7628
lon: -130.564
Northwest-flowing Taweh Creek and its tributary, the westward-flowing Sezill Creek, drain the southwestern and western portions of the plateau, respectively. Elwyn Creek and Taweh Creek are tributaries of Mess Creek, which flows northwestward into the Stikine River.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
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
Cartoona Ridge lies between Chakima and Shaman creek valleys and shares its name with Cartoona Peak at the westernmost end of the ridge. The western side of the Big Raven Plateau has been moderately dissected by stream erosion which has resulted in the formation of steep-sided canyons; Elwyn, Sezill and Taweh creek canyons are the most extensive.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Although most of the lava in the Snowshoe Lava Field ponded as thick flows on the gently sloping surface of the Big Raven Plateau, some of it flowed into the upper canyon of Sezill Creek and into the head of Taweh Creek, as well as into the narrow tributary valleys of Walkout and Shaman creeks.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: sezill creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69967
lon: -130.88724
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Lava from Camp Hill extends to the northwest along the southwestern edge of the plateau, but it is almost completely buried under colluvium deposits. Small exposures of this lava occur along the Mess Creek Escarpment and along Taweh Creek valley just south of Hoia Bluff. Pillow Ridge Formation.

Geographic entities mentioned:
surface_form: taweh creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71638
lon: -130.97063
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
Transportation of the glacial and landslide debris into Kakiddi Creek valley has resulted in the formation of several large alluvial fans behind which Nuttlude Lake, Kakiddi Lake, Mowdade Lake and Mowchilla Lake have ponded. Nido Creek and Tennaya Creek flow into Nuttlude Lake whereas Sorcery Creek and Shaman Creek flow into Kakiddi Lake.

Geographic entities mentioned:
surface_form: tennaya creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
surface_form: shaman creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.61636
lon: -130.40395
surface_form: nido creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.71636
lon: -130.47065
Sphinx Dome is a partially buried rhyolite dome adjacent to The Pyramid whose southern edge has been largely destroyed by headward stream erosion. Isolated remnants of the rhyolitic Pharaoh Dome occur along the eastern and southeastern ends of the Big Raven Plateau between Tennaya Creek in the north and Cartoona Ridge in the south.

Geographic entities mentioned:
surface_form: tennaya creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.69966
lon: -130.42065
surface_form: big raven plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 57.7167
lon: -130.75
Raspberry Formation. The Raspberry Formation is exposed at the base of prominent escarpments on the western, southwestern and southeastern sides of the Big Raven Plateau. It has an elevation of less than along the Mess Creek Escarpment and consists of flat-lying basaltic lava flows interbedded with scoria.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206
It has an elevation of less than along the Mess Creek Escarpment and consists of flat-lying basaltic lava flows interbedded with scoria. More than of Raspberry lava flows are exposed in the Mess Creek Escarpment, most of which were erupted from a shield volcano that formed on a Late Miocene erosion surface.

Geographic entities mentioned:
surface_form: mess creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.88296
lon: -131.2206