Sarmila/GeoWiki-Features huggingface dataset:
Sulamutag Feng. Sulamutag Feng is a mountain located in Xinjiang, China. It is an ultra-prominent peak and is the 193rd highest in Asia. It has an elevation of. See also. List of ultras of Tibet, East Asia and neighbouring areas

Geographic entities mentioned:
surface_form: sulamutag feng
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 37.91333333
lon: 87.38916667
The Regiment served through the Italian campaign, sometimes in support of the 5th Army, sometimes with the 8th Army (at least parof the time with 6 AGRA), and saw action in many notable battles. These included the third battle of Monte Cassino, operations against the Gustav Line and the breakthrough, operations against the Hitler Line, actions at Arezzo and the occupation of Florence and Forlì.

Geographic entities mentioned:
surface_form: Monte Cassino
instance_of: Mountain
countries: Italy
coordinates: lat: 41.49
lon: 13.813888888889
John, to watch them climbing into the sky. Mountaineering, motorsports and ballooning. In 1891, when he was 18, Santos-Dumont visited Europe. In England he spent a few months practising his English, and in France he climbed Mont Blanc. This adventure, at an altitude of almost 5,000 metres, gave him a taste for heights.

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
13, a luxurious double hot air and hydrogen balloon. On his first return to Rio de Janeiro in 1903, a group of climbers put up a banner on Sugarloaf Mountain, beside Guanabara Bay, greeting the aviator on his return by ship from Europe. On 7 September 1903, he returned as a hero and met the President of Brazil, Rodrigues Alves, at the Catete Palace.

Geographic entities mentioned:
surface_form: Sugarloaf Mountain
instance_of: Mountain
countries: Brazil
coordinates: lat: -22.949444444444445
lon: -43.156666666666666
It starts off just west of Longwood Road South and east of Highway 403 as a two-way thoroughfare up to Queen Street South, where it then switches over to a one-way collector road (eastbound) to Bay Street South and then to another two-way section from Bay Street to James Mountain Road, a mountain-access road in the city near the base of the Niagara Escarpment (mountain). History.

Geographic entities mentioned:
surface_form: Niagara Escarpment
instance_of: Mountain
countries: Canada
coordinates: lat: 43.8334
lon: -79.99966
1842 find. In 1842 the Greek manuscript collector Minoides Mynas came upon a manuscript of Babrius in the convent of Great Lavra on Mount Athos, now in the British Museum. This manuscript contained 123 fables out of the supposed original number, 160. They are arranged alphabetically, but break off at the letter O.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Desolation Peak Lookout remains an operational fire lookout staffed each summer by fire personnel. The lookout features sweeping vistas of North Cascade peaks including Hozomeen Mountain. The lookout is best known as the setting for Jack Kerouac's novel &quot;Desolation Angels&quot;. Kerouac spent the summer of 1956 manning the structure for the U.S. Forest Service.

Geographic entities mentioned:
surface_form: Hozomeen Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.9822
lon: -121.012
Umbria. Umbria (;) is a region of central Italy. It includes Lake Trasimeno and Marmore Falls, and is crossed by the Tiber. It is the only landlocked region on the Apennine Peninsula. The capital is Perugia. The region has 851,954 inhabitants as of 2025.

Geographic entities mentioned:
surface_form: Lake Trasimeno
instance_of: Lake
countries: Italy
coordinates: lat: 43.14
lon: 12.1
Geography. Umbria is bordered by Tuscany to the west and the north, Marche to the east and Lazio to the south. Partly hilly and mountainous, and partly flat and fertile owing to the valley of the Tiber, its topography includes part of the central Apennines, with the highest point in the region at Monte Vettore on the border of Marche, at; the lowest point is Attigliano.

Geographic entities mentioned:
surface_form: Monte Vettore
instance_of: Mountain
countries: Italy
coordinates: lat: 42.816666666667
lon: 13.266666666667
Contained within Umbria is the hamlet of Cospaia, which was a tiny republic from 1440 to 1826, created by accident. Umbria is crossed by two valleys: the Umbrian valley (&quot;Valle Umbra&quot;), stretching from Perugia to Spoleto, and the Tiber Valley (&quot;Val Tiberina&quot;), north and west of the first one, from Città di Castello to the border with Lazio.

Geographic entities mentioned:
surface_form: Tiber Valley
instance_of: Valley
countries: Italy
coordinates: lat: 42.133333333333
lon: 12.583333333333
The husband proposed that they take refuge on Mount Orofena, a high mountain in Tahiti, saying that it was lofty and would not be reached by the sea.

Geographic entities mentioned:
surface_form: Mount Orofena
instance_of: Mountain
countries: France
coordinates: lat: -17.623055555556
lon: -149.47694444444
His wife had objected that the sea would reach to Mount Orofena, and that they had better go to Mount O Pitohito, where they would be safe from the flood So to Mount O Pitohito they went; and she was right, for Orofena was overwhelmed by the sea, but O Pitohito rose above the waste of waters and became their abode.

Geographic entities mentioned:
surface_form: Mount O Pitohito
instance_of: Mountain
countries: France
coordinates: lat: -17.6125
lon: -149.465
The &quot;Dreiseenbahn&quot; branches southwards from the Höllentalbahn railway, from Freiburg im Breisgau to Donaueschingen, at Titisee station. Along its route it serves stations and halts at Feldberg-Bärental, Altglashütten-Falkau, Aha and Schluchsee, before terminating at Seebrugg. The line is so called because it passes by the three lakes of Titisee, Windgfällweiher and Schluchsee.

Geographic entities mentioned:
surface_form: Titisee
instance_of: Lake
countries: Germany
coordinates: lat: 47.893333333333
lon: 8.1461111111111
surface_form: Windgfällweiher
instance_of: Lake
countries: Germany
coordinates: lat: 47.851944444444
lon: 8.1258333333333
The line is so called because it passes by the three lakes of Titisee, Windgfällweiher and Schluchsee. On certain dates throughout the year historic steam trains are operated between Seebrugg, Titisee and Löffingen (Höllentalbahn) by IG 3-Seenbahn, an association of railway enthusiasts located in Seebrugg.

Geographic entities mentioned:
surface_form: Titisee
instance_of: Lake
countries: Germany
coordinates: lat: 47.893333333333
lon: 8.1461111111111
The Blonay–Chamby Museum Railway is a railway preservation group staffed entirely by volunteers who operate trains each Saturday and Sunday between May and October. Vintage steam and electric hauled trains depart from Blonay and climb over Lake Geneva and the Alps. After reversing at or just before Chamby, the trains terminate at the museum site, where visitors can explore stationary exhibits.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
It is in the Pacific Ocean drainage basin and is a right tributary of Indian Arm. Course. Percy Creek begins at unnamed slope in Mount Seymour Provincial Park at a height of just under. It heads east and empties into the west end of Goldie Lake, accessible via the park's Goldie Lake Loop Trail.

Geographic entities mentioned:
surface_form: mount seymour
instance_of: Mountain
countries: Canada
coordinates: lat: 49.393333333333
lon: -122.94444444444
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.353889
lon: -122.9075
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.635556
lon: -117.545
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.3305555
lon: -83.8519445
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.250284
lon: -77.816976
Percy Creek (Indian Arm). Percy Creek is a stream in the southeastern part of the District of North Vancouver in the Lower Mainland part of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a right tributary of Indian Arm. Course. Percy Creek begins at unnamed slope in Mount Seymour Provincial Park at a height of just under.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.353889
lon: -122.9075
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.635556
lon: -117.545
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.3305555
lon: -83.8519445
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.250284
lon: -77.816976
Percy Creek (Indian Arm). Percy Creek is a stream in the southeastern part of the District of North Vancouver in the Lower Mainland part of British Columbia, Canada. It is in the Pacific Ocean drainage basin and is a right tributary of Indian Arm. Course. Percy Creek begins at unnamed slope in Mount Seymour Provincial Park at a height of just under.

Geographic entities mentioned:
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.353889
lon: -122.9075
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 49.635556
lon: -117.545
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.3305555
lon: -83.8519445
surface_form: percy creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.250284
lon: -77.816976
Dillon Lake. Dillon Lake is a reservoir in Muskingum County, Ohio in the United States. It was completed in 1961, covers 1,736 acres of water and was constructed primarily for flood control purposes. The lake was named after Moses Dillon, who purchased the land in 1803/1804

Geographic entities mentioned:
surface_form: dillon lake
instance_of: Lake
countries: United States
coordinates: lat: 40.0026127
lon: -82.0966435
The last in the Great Lakes chain, Lake Ontario serves as the outlet to the Atlantic Ocean via the Saint Lawrence River, comprising the western end of the Saint Lawrence Seaway. Its primary inlet is the Niagara River from Lake Erie. The Long Sault control dam, primarily along with the Moses-Saunders Power Dam regulates the water level of the lake.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Major rivers draining into Lake Ontario include the Niagara River, Don River, Humber River, Rouge River, Trent River, Cataraqui River, Genesee River, Oswego River, Black River, Little Salmon River, Credit River, Ganaraska River and the Salmon River. The Welland Canal also drains into the lake. Geology.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
Navigation. The Great Lakes Waterway connects the lake sidestream to the Atlantic Ocean via the Saint Lawrence Seaway and upstream to the other rivers in the chain via the Welland Canal and to Lake Erie. The Trent-Severn Waterway for pleasure boats connects Lake Ontario at the Bay of Quinte to Georgian Bay (Lake Huron) via Lake Simcoe.

Geographic entities mentioned:
surface_form: Lake Simcoe
instance_of: Lake
countries: Canada
coordinates: lat: 44.436666666667
lon: -79.339166666667
The Trent-Severn Waterway for pleasure boats connects Lake Ontario at the Bay of Quinte to Georgian Bay (Lake Huron) via Lake Simcoe. The Oswego Canal connects the lake at Oswego to the New York State Canal System, with outlets to the Hudson River, Lake Erie, and Lake Champlain.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Many Roman ceramics and metal objects have been found in excavations near the village. Cultural and Natural sights. The Magura cave is located 6 kilometers west of the village. The Belogradchik rocks are located 18 kilometers from Kladorub. Honour. Kladorub Glacier on Nordenskjöld Coast in Graham Land, Antarctica is named after the village.

Geographic entities mentioned:
surface_form: Belogradchik rocks
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 43.62083333
lon: 22.685
Parks in Salzburg, Sankt Pölten and Vienna were closed as a precautionary measure. The following day, the institute observed wind gusts on Hinterer Brunnenkogel in Tyrol, Austria. Infrastructure damage, windthrow and transport disruption accounted for the majority of the disturbance caused by the storm.

Geographic entities mentioned:
surface_form: Hinterer Brunnenkogel
instance_of: Mountain
countries: Austria
coordinates: lat: 46.912777777778
lon: 10.861388888889
Much of the city is within the borders of the Suigo-Tsukuba Quasi-National Park. Geography. Itako is located in southern Ibaraki Prefecture, bordered by Chiba Prefecture to the south, and sandwiched between Lake Kasumigaura to the west and Lake Kitaura to the east. The Tone River also flows through the city, which has been noted since the Edo period for its network of canals.

Geographic entities mentioned:
surface_form: Lake Kasumigaura
instance_of: Lake
Group of lakes
countries: Japan
coordinates: lat: 36.040277777778
lon: 140.39416666667
Chimehuin River. The Chimehuin River is a river in the northwest of the Patagonic Province of Neuquén, Argentina. Its origin is at Lake Huechulafquen and it passes by the city of Junín de los Andes. After a course of about 53 km, it merges with the Aluminé River to form the Collón Curá River. The Chimehuin is considered a prime spot for fly fishing.

Geographic entities mentioned:
surface_form: Aluminé River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -39.088333333333
lon: -70.958333333333
surface_form: Collón Curá River
instance_of: Watercourse
countries: Argentina
coordinates: lat: -39.963333333333
lon: -71.075555555556
surface_form: aluminé
instance_of: Lake
countries: Argentina
coordinates: lat: -38.916666666667
lon: -71.133055555556
Chimehuin River. The Chimehuin River is a river in the northwest of the Patagonic Province of Neuquén, Argentina. Its origin is at Lake Huechulafquen and it passes by the city of Junín de los Andes. After a course of about 53 km, it merges with the Aluminé River to form the Collón Curá River. The Chimehuin is considered a prime spot for fly fishing.

Geographic entities mentioned:
surface_form: chimehuin river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -39.794444444444
lon: -71.208611111111
Its origin is at Lake Huechulafquen and it passes by the city of Junín de los Andes. After a course of about 53 km, it merges with the Aluminé River to form the Collón Curá River. The Chimehuin is considered a prime spot for fly fishing. It is known for its two introduced species of Salmonidae, the brown trout and the rainbow trout.

Geographic entities mentioned:
surface_form: chimehuin
instance_of: Watercourse
countries: Argentina
coordinates: lat: -39.794444444444
lon: -71.208611111111
The Chimehuin is considered a prime spot for fly fishing. It is known for its two introduced species of Salmonidae, the brown trout and the rainbow trout. The area around first part of the river's course (from the lake up to a few kilometers before Junín de los Andes) is a protected nature reserve (&quot;Área Natural Protegida Boca del Chimehuin&quot;).

Geographic entities mentioned:
surface_form: chimehuin
instance_of: Watercourse
countries: Argentina
coordinates: lat: -39.794444444444
lon: -71.208611111111
It is a part of the E33 European route. The road is also known as Autostrada della Cisa because it crosses the Northern Apennines at the Cisa Pass. The main 101-km expanse of the motorway connects the Autostrada A1 with the Autostrada A12, thus directly linking the Po Valley with the Italian Riviera and the Versilia region. The Autostrada A15 is operated by the company.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
It has been revised numerous times. Description. The female is recorded at 4mm in length. Distribution. This species is known from Nelson and Lake Tekapo in New Zealand, but is probably widespread. Conservation status. Under the New Zealand Threat Classification System, this species is listed as &quot;Not Threatened&quot; with the qualifier of &quot;Sparse&quot;.

Geographic entities mentioned:
surface_form: Lake Tekapo
instance_of: Lake
countries: New Zealand
coordinates: lat: -43.9
lon: 170.525
History. Stanley straddles the Nashwaak River 30 km north of Fredericton at the intersection of Route 107 and Route 620. The area was colonized in 1833 when a group associated with the New Brunswick and Nova Scotia Land Company became interested in the area. Early impressions of the land were not positive, with surveyors noting the rocky soil as one problem.

Geographic entities mentioned:
surface_form: Nashwaak River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.965694444444
lon: -66.586194444444
The name comes from the ancient city of Pheneus. History. In ancient times the area was considered part of Arcadia. Herodotus stated that the river Styx arises near Feneos. Feneos lies at the foot of Mount Cyllene, mythical birthplace of the god Hermes. It therefore served as an important cult centre for the god, notably during the annual festival of the Hermaea.

Geographic entities mentioned:
surface_form: Mount Cyllene
instance_of: Mountain
countries: Greece
coordinates: lat: 37.939166666667
lon: 22.396666666667
The Calf. The Calf, at an elevation of, is the highest point in the Howgill Fells, an area of high ground in north-west England. It is in the north-west of the Yorkshire Dales in Westmorland and Furness in the county of Cumbria (historically it was on the West Riding of Yorkshire/Westmorland boundary).

Geographic entities mentioned:
surface_form: the calf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.367419444444
lon: -2.5140305555556
A twenty-mile skyline of the Lakeland peaks can be seen, as well as the Yorkshire Three Peaks and many of the nearer Howgill Fells. Alfred Wainwright, in his &quot;Walks on the Howgill Fells&quot;, describes a route from Sedbergh to Calders and The Calf as &quot;the classic high-level walk on the Howgill Fells&quot;.

Geographic entities mentioned:
surface_form: the calf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.367419444444
lon: -2.5140305555556
He includes a drawing of the trig point on the summit of The Calf, discusses a &quot;reclining&quot; standing stone 400 yards to the north-east which appears on large-scale Ordnance Survey maps, and spends a column of text discussing &quot;the altitude of Calders&quot;, which he estimates as 2215 ft.

Geographic entities mentioned:
surface_form: the calf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.367419444444
lon: -2.5140305555556
He also describes ascents of the Calf from Castley (&quot;this impressive expedition&quot;, &quot;a beautiful walk&quot;), Beck Houses farm on the west of the Howgills (&quot; this high-level traverse of the plateau splendidly reveals the topographical details of the Howgills&quot;) and Bowderdale (&quot;the longest direct ascent of The Calf&quot;).

Geographic entities mentioned:
surface_form: the calf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.367419444444
lon: -2.5140305555556
surface_form: the calf
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.367419444444
lon: -2.5140305555556
Mount Rainey. Mount Rainey is a summit located in the Coast Mountains of British Columbia, Canada. It is situated southeast of Stewart, British Columbia, and east of Hyder, Alaska. The nearest higher neighbor is Mount Magee, to the east-northeast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mount rainey
instance_of: Mountain
countries: Canada
coordinates: lat: 55.90968
lon: -129.93685
Mount Rainey. Mount Rainey is a summit located in the Coast Mountains of British Columbia, Canada. It is situated southeast of Stewart, British Columbia, and east of Hyder, Alaska. The nearest higher neighbor is Mount Magee, to the east-northeast.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The nearest higher neighbor is Mount Magee, to the east-northeast. This mountain's toponym was officially adopted 4 May 1926 on Geological Survey sheet 193A, and confirmed by the Geographical Names Board of Canada in 1953 to remember Robert &quot;Bob&quot; Rainey, the first locator on this mountain who was killed on his mineral claim near Stewart.

Geographic entities mentioned:
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
This mountain's toponym was officially adopted 4 May 1926 on Geological Survey sheet 193A, and confirmed by the Geographical Names Board of Canada in 1953 to remember Robert &quot;Bob&quot; Rainey, the first locator on this mountain who was killed on his mineral claim near Stewart. Precipitation runoff from the mountain drains into the Portland Canal.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount Rainey. Mount Rainey is a summit located in the Coast Mountains of British Columbia, Canada. It is situated southeast of Stewart, British Columbia, and east of Hyder, Alaska. The nearest higher neighbor is Mount Magee, to the east-northeast.

Geographic entities mentioned:
surface_form: mount rainey
instance_of: Mountain
countries: Canada
coordinates: lat: 55.90968
lon: -129.93685
Climate. Based on the Köppen climate classification, Mount Rainey is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: mount rainey
instance_of: Mountain
countries: Canada
coordinates: lat: 55.90968
lon: -129.93685
The mouth is located between Marina di Casalvelino and Velia. The Alento has 3 tributaries: Palistro river and Badolato creek originate from the Mount Gelbison, Fiumicello creek originates from the Mount Stella. Natural environment.

Geographic entities mentioned:
surface_form: Mount Gelbison
instance_of: Mountain
countries: Italy
coordinates: lat: 40.21666667
lon: 15.31666667
Etymology. The name &quot;Tequendama&quot; means in the Muysccubun: &quot;he who precipitates downward&quot;. Background. During the time before the Spanish conquest of the Muisca, the central highlands of the Colombian Andes (Altiplano Cundiboyacense) were populated first by prehistorical indigenous groups, then by people from the Herrera Period, and finally by the Muisca.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
Description. The site of Tequendama consists of four cave and overhang locations at close distance to each other, called Tequendama I (~11,000-10,000 years BP), II (9500-8300 BP), III (7000-6000 BP) and IV (2500-450 BP). The cave sites have been inhabited probably because of the access to fresh water; the Bogotá River currently flows very close to the site and also the Funza River was nearby.

Geographic entities mentioned:
surface_form: Bogotá River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
At that time, the paleoclimate was less cold and more humid than today. Lake Fúquene was overflowing rapidly on the Bogotá savanna during this Guantivá interstadial. During the next phase, of El Abra, dated at 11,000 to 9500 years BP, the climate was colder again and the previously retreating glaciers in the Eastern Ranges of the Colombian Andes were advancing.

Geographic entities mentioned:
surface_form: Lake Fúquene
instance_of: Lake
countries: Colombia
coordinates: lat: 5.46667
lon: -73.75
Geography. Sreepur upazila is located northeast of Magura district. Rajbari District to the north of the upazila, Shailkupa Upazila of Jhenaidah on the west, Magura Sadar Upazila on the south, Madhukhali Upazila. The Gorai River and the Kumar River are notable rivers of Sreepur. Sreepur upazila has an area of 175.15 km2. Sreepur upazila is the smallest upazila in Magura district. Demographics.

Geographic entities mentioned:
surface_form: Kumar River
instance_of: Watercourse
countries: Bangladesh
coordinates: lat: 23.517777777778
lon: 89.454722222222
Lake Washington Boulevard. Lake Washington Boulevard is a scenic, approximately, road through Seattle, Washington, that hugs Lake Washington for much of the route. There are views of the lake, small sections of rainforest, meadows, and views of the Cascade mountains.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
He also made lithographs of Welsh scenery. He made caricatures of the commissioners of education sent to Wales (1846–47). Some of his sketches, including a map of North Wales under the name &quot;Dame Venedotia&quot;, &quot;Pitt's Head&quot; near Beddgelert, and others of the neighbourhood of Snowdon, were published at Caernarfon. His sketch of &quot;Pwllheli and St.

Geographic entities mentioned:
surface_form: Snowdon
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.068863888889
lon: -4.0755888888889
Describing the journey to Africa, Carscallen wrote. &quot;After an exceedingly hot trip through the Red Sea, we arrived in Mombasa nearly three weeks later.&quot;
By November 27, 1906, Carscallen and Nyambo were able to open the first British East Africa Mission station in Kenya at Gendia Hill near the eastern shore of Lake Victoria on Kendu Bay with the assistance of Abraham C.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Mt Talagabodas is just north of Galunggung volcano which attracted global attention following an eruption in 1982 that, amongst other things, caused widely reported disruption to international air travel and an emergency for British Airways Flight 9 travelling from Kuala Lumpur to Perth in June 1982.

Geographic entities mentioned:
surface_form: Galunggung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.2567315
lon: 108.0770588
surface_form: galunggung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.2567315
lon: 108.0770588
Talagabodas. Mount Talagabodas or Mount Telagabodas (which means Mount of &quot;White Lake&quot; (refer to white crater lake) in Sundanese) is a stratovolcano in West Java, Indonesia. The volcano is about 25 km to the east of the town of Garut and is built up of andesitic lavas and pyroclastics. Fumaroles, mud pots and hot springs are found around the crater lake.

Geographic entities mentioned:
surface_form: talagabodas
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.208
lon: 108.07
Talagabodas. Mount Talagabodas or Mount Telagabodas (which means Mount of &quot;White Lake&quot; (refer to white crater lake) in Sundanese) is a stratovolcano in West Java, Indonesia. The volcano is about 25 km to the east of the town of Garut and is built up of andesitic lavas and pyroclastics. Fumaroles, mud pots and hot springs are found around the crater lake.

Geographic entities mentioned:
surface_form: talagabodas
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.208
lon: 108.07
surface_form: telagabodas
instance_of: Mountain
countries: Indonesia
coordinates: lat: -7.208
lon: 108.07
Beaufortain. Beaufortain is a valley in the Savoie department in the Auvergne-Rhône-Alpes region in Southeastern France. It extends around the commune of Beaufort.

Geographic entities mentioned:
surface_form: beaufortain
instance_of: Valley
countries: France
coordinates: lat: 45.73333333
lon: 6.55
Other work. Nadel appeared as the Rangers' radio announcer in the film &quot;The Rookie&quot; in 2002. Nadel is active in animal causes and was one of the founders of the first leash-free dog park in the DFW Metroplex at White Rock Lake in Dallas.

Geographic entities mentioned:
surface_form: White Rock Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.834166666667
lon: -96.722777777778
It has an elevation of and lies within an east–west valley through which a tributary of the Tseax River flows. The volcano consists of two nested structures and was the source of four lava flows that descended into neighbouring valleys. A secondary eruptive centre lies just north of Tseax Cone on the opposite side of Melita Lake.

Geographic entities mentioned:
surface_form: Melita Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.11361
lon: -128.89861
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
It lies within a steep-sided, long, east–west valley penetrating the Nass Ranges of the Hazelton Mountains. Tseax Cone is situated at the outlet of Melita Lake, an expansion of Crater Creek which flows west into the Tseax River. Crater Creek gets its name from being in association with Tseax Cone which is located on the eastern side of the creek.

Geographic entities mentioned:
surface_form: Melita Lake
instance_of: Lake
countries: Canada
coordinates: lat: 55.11361
lon: -128.89861
surface_form: Crater Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.09955
lon: -128.97039
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Background. Tseax Cone is one of the southernmost volcanoes in the Northern Cordilleran Volcanic Province. This is a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: Northern Cordilleran Volcanic Province
instance_of: Mountain
countries: Canada
coordinates: lat: 57.7156
lon: -130.634
The Tseax River was forced to abandon its alluvial channel in favour of bedrock channels along the lava flows, although in some places one or more channels flow on the lava. Vetter Creek, a tributary of the Nass River, flows along the western side of the lava and then disappears under the lava-covered Nass River floodplain through a series of sinkholes.

Geographic entities mentioned:
surface_form: Vetter Creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 55.18284
lon: -129.1204
G. Hanson wrote in a 1923 Canada Department of Mines report that 170-year-old trees were found growing on lava from Tseax Cone; this would indicate an eruption prior to 1753. In 1935, Marius Barbeau concluded in the Canadian Geographical Journal that the latest eruption at Tseax Cone occurred in the late 18th century. In 1977, G. P. V. Akrigg and H. B.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Tseax Cone. Tseax Cone () is a small volcano in the Nass Ranges of the Hazelton Mountains in northwestern British Columbia, Canada. It has an elevation of and lies within an east–west valley through which a tributary of the Tseax River flows. The volcano consists of two nested structures and was the source of four lava flows that descended into neighbouring valleys.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Location and climate. Tseax Cone is about north of Terrace near the Nisga'a villages of Gitwinksihlkw and Gitlaxt'aamiks in Cassiar Land District of northwestern British Columbia, Canada. It lies within a steep-sided, long, east–west valley penetrating the Nass Ranges of the Hazelton Mountains.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Background. Tseax Cone is one of the southernmost volcanoes in the Northern Cordilleran Volcanic Province. This is a broad area of shield volcanoes, lava domes, cinder cones and stratovolcanoes extending from northwestern British Columbia northwards through Yukon into easternmost Alaska.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The lava was also being excavated from borrow pits and hauled to be used on forest service roads. It was not until 1992 when Nisga'a Memorial Lava Bed Provincial Park was founded to preserve the volcanic landscape and to honour the 2,000 Nisga'a people who died during the Tseax Cone eruption.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
This protected area is noteworthy for being the first provincial park in British Columbia to be managed by both BC Parks and a First Nation, as well as the first provincial park in British Columbia to combine indigenous culture and natural features. Accessibility.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Tseax Cone. Tseax Cone () is a small volcano in the Nass Ranges of the Hazelton Mountains in northwestern British Columbia, Canada. It has an elevation of and lies within an east–west valley through which a tributary of the Tseax River flows. The volcano consists of two nested structures and was the source of four lava flows that descended into neighbouring valleys.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
A secondary eruptive centre lies just north of Tseax Cone on the opposite side of Melita Lake. It probably formed simultaneously with Tseax Cone, but the timing of volcanism at the two eruptive centres is not precisely known; both were formed by volcanic activity sometime in the last 800 years.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
The exact timing of volcanism at Tseax Cone has been a subject of controversy due to there being no direct written accounts; radiocarbon dating of plants killed by lava or ejecta from the volcano has yielded ages as old as 625 ± 70 years to as young as 190 ± 15 years. There is also controversy over whether the volcano was formed during one or more distinct episodes of eruptive activity.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
The single eruptive episode hypothesis has been proposed by researchers as early as 1923 whereas a multi-eruption hypothesis was proposed in 1978. Most research suggests that Tseax Cone was formed during one episode of eruptive activity; new data supporting this hypothesis was reported in 2020. Tseax Cone is the subject of legends told by the local indigenous people.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
As many as 2,000 people are claimed to have been killed by an eruption from Tseax Cone; this would make it the deadliest geological disaster in Canada and the second-worst natural disaster in Canadian history by death toll. Tseax Cone has therefore been described as the deadliest volcano in Canada. Renewed eruptions from the volcano could start wildfires and block local streams with lava flows.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Tseax Cone has therefore been described as the deadliest volcano in Canada. Renewed eruptions from the volcano could start wildfires and block local streams with lava flows. Tseax Cone lies within an ecoregion characterized by mountainous terrain and several streams. Rainforests occur at the volcano, as well as several species of mammals.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Rainforests occur at the volcano, as well as several species of mammals. Lichens and mosses cover most of the lava flows that have issued from Tseax Cone, although rainforests and waterbodies also obscure them. After at least 20 years of pleas for protection, the volcano and lava flows were established as Nisga'a Memorial Lava Bed Provincial Park in 1992.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Lichens and mosses cover most of the lava flows that have issued from Tseax Cone, although rainforests and waterbodies also obscure them. After at least 20 years of pleas for protection, the volcano and lava flows were established as Nisga'a Memorial Lava Bed Provincial Park in 1992. Tseax Cone and its lava flows can be accessed via provincial highways and backcountry roads. Names and etymology.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Tseax Cone and its lava flows can be accessed via provincial highways and backcountry roads. Names and etymology. Tseax Cone has been variously called &quot;Aiyansh Volcano&quot;, &quot;Aiyansh River Volcano&quot;, &quot;Tseax River Cone&quot; and &quot;Tseax Volcano&quot;. &quot;Aiyansh&quot; comes from a Nisga'a word meaning or whereas &quot;Tseax&quot; comes from a Nisga'a word meaning.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
surface_form: tseax river cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
&quot;Tseax&quot; is possibly a reference to the disturbed drainage patterns of the Tseax River caused by a volcanic eruption from the cone. The well-established local name for the volcano, &quot;Tseax Cone&quot;, became official on December 13, 1991, and was adopted on the National Topographic System map 103P/2.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
The well-established local name for the volcano, &quot;Tseax Cone&quot;, became official on December 13, 1991, and was adopted on the National Topographic System map 103P/2. To the local Nisga'a people, Tseax Cone is known as; in their language it means, which is a reference to the volcanic eruption that sent lava spewing out of the volcano. Location and climate.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Olivine, plagioclase and the iron-titanium oxides are in the form of phenocrysts whereas clinopyroxene occurs as a matrix mineral. The lack of clinopyroxene phenocrysts in Tseax Cone lavas is a phenomenon commonly observed in other mafic lavas throughout the Northern Cordilleran Volcanic Province.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Tseax Cone and its eruptive products rest unconformably on sedimentary rocks of the Bowser Lake Group, a geological group of Jurassic and Cretaceous age consisting of grey sandstones and dark grey and black conglomerates, siltstones and mudstones.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Lava and tephra from Tseax Cone cover about and have a total volume of around; the volume of this volcanic material is similar to that produced during Mauna Loa's 1984 eruption and Kīlauea's fissure 8 eruption in 2018. The Tseax Cone lavas are thought to have been emplaced at high speed during a short period of time, which may have been partially due to eruption rate and topography.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Their liquidus viscosities are comparable to basalts of Mount Etna and the Hawaiian Islands, as well as the foidite lavas of Mount Nyiragongo and the tephrite lavas of Nyamuragira. It is possible that the lava erupted from Tseax Cone rose along the same faults as those at the Lakelse Hot Springs south of Terrace, which are the hottest geothermal springs in Canada. Structure.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Each structure was formed by a different style of volcanic activity; the spatter rampart was created by Hawaiian-style lava fountaining whereas the inner cone was created by low-intensity Strombolian explosions. The entire structure of Tseax Cone has been variously described as a cinder cone, a pyroclastic cone or a tephra cone.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Red oxidized tephra beneath the black tephra was deposited by lava fountaining at the larger satellite cone. Lava flows. Tseax Cone was the source of four distinct lava flows, all of which were probably erupted over a timespan of weeks to a few months. The first flow is the longest and most voluminous, accounting for about 84% of the total volume of lava erupted from Tseax Cone.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
They are among the longest lava flows in the Canadian Cordillera; lava flows more than long in this cordillera are usually basaltic in composition. The third flow accounts for less than 2% of the total volume of lava erupted from Tseax Cone, having travelled through Crater Creek valley to near Ross Lake in the Tseax River valley.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
The exact timing of volcanism at Tseax Cone has been a subject of controversy due to there being no direct written accounts. Reports of the rich oral history of the local Nisga'a people by missionaries as early as the 1910s suggest that Tseax Cone was erupting around 1770. However, the credibility of these reports has been disputed due to possible poor translation from Nisga'a to English. G.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Akrigg and H. B. Akrigg speculated in &quot;British Columbia Chronicle, 1847–1871: Gold & Colonists&quot; that the Tseax Cone eruption was witnessed by naval officer Juan Francisco de la Bodega y Quadra on August 24, 1775. However, this is extremely unlikely because Bodega y Quadra's schooner, the &quot;Sonora&quot;, was anchored more than west of Tseax Cone across mountainous terrain. Michael D.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
However, this is extremely unlikely because Bodega y Quadra's schooner, the &quot;Sonora&quot;, was anchored more than west of Tseax Cone across mountainous terrain. Michael D. Higgins proposed in a 2008 Journal of Volcanology and Geothermal Research article that the 1700 Cascadia earthquake may have caused the latest Tseax Cone eruption by destabilizing a subterranean magmatic system.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
In 2001, M. C. Roberts and S. McCuaig reported in The Canadian Geographer that a wood fragment of a lava-encased tree yielded a radiocarbon date of 220 ± 130 years; they gave a corrected date of 230 ± 50 years. These two radiocarbon dates were recalibrated by Michael D. Higgins in 2008 using calibration software and reinterpreted the age of the Tseax Cone eruption at between 1668 and 1714.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
These two radiocarbon dates were recalibrated by Michael D. Higgins in 2008 using calibration software and reinterpreted the age of the Tseax Cone eruption at between 1668 and 1714. Charred wood beneath tephra about northwest of Tseax Cone was reported by Williams-Jones &quot;et al.&quot; in 2020 to have yielded radiocarbon dates of 190 ± 15 years and 390 ± 15 years.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
These dates suggest that Tseax Cone erupted between 1675 and 1778, which correlates with the oral history of the Nisga'a, as well as reports that claim an eruption took place during the 18th century. A Common Era date of 1690 ± 150 years is provided by the Smithsonian Institution's Global Volcanism Program for the last known eruption of Tseax Cone.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
A Common Era date of 1690 ± 150 years is provided by the Smithsonian Institution's Global Volcanism Program for the last known eruption of Tseax Cone. The timing of volcanism at Tseax Cone makes it one of the youngest volcanoes in Canada, as well as the site of one of the most recent volcanic eruptions in Canada.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Hazards. The question of whether Tseax Cone formed during one or more distinct eruptive episodes has important implications for future activity and hazard mitigation efforts. Renewed activity from Tseax Cone is unlikely if the volcano is monogenetic; this is because monogenetic volcanoes are typically considered to erupt only once and to be short-lived.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
Damming of the Nass River by lava flows could negatively affect the salmon fisheries on this river. Carbon dioxide emissions from Tseax Cone could pose a threat to local inhabitants due to the gas's ability to replace oxygen in low-lying areas and poorly ventilated structures.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899
While some of the Nisga'a may have escaped the lava flow by canoe to the far side of the Nass River, many of them were caught between the river and the advancing lava flow. The average discharge rate of the Nass River is strong enough to drown anyone attempting to escape by swimming during the summer months of June, August and September; Tseax Cone is suspected to have erupted during this time.

Geographic entities mentioned:
surface_form: tseax cone
instance_of: Mountain
countries: Canada
coordinates: lat: 55.1108
lon: -128.899