Sarmila/GeoWiki-Features huggingface dataset:
Those are not reflected in the table below. Spanning the Rivière des Prairies. Although the Rivière des Prairies is much smaller than the Saint Lawrence, bridge construction there did not begin until the 1840s—when rapid construction began on three wooden toll bridges to what is now Laval, one of which, Pont des Saints-Anges, collapsed in the 1880s and was never rebuilt.

Geographic entities mentioned:
surface_form: Rivière des Prairies
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.708333333333
lon: -73.479166666667
(Another bridge across Rivière des Mille Îles, which was part of the same line, collapsed in 1882 but was immediately rebuilt.) The highway construction boom of the 1960s and 1970s led to the construction of four new freeway bridges across the river, and the upgrading of the existing Pie IX Bridge to freeway standards. Spanning the Lake of Two Mountains and the Ottawa River East Channel.

Geographic entities mentioned:
surface_form: Rivière des Mille Îles
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.69916666666667
lon: -73.52916666666667
It was not until 1925, however, that a fixed road link, formed by Galipeault Bridge and Taschereau Bridge, was built across the Ottawa River from Montreal Island. Île Perrot was the only way out of Montreal to the West before the construction of Île aux Tourtes Bridge, which goes directly to Vaudreuil across the Lake of Two Mountains.

Geographic entities mentioned:
surface_form: Lake of Two Mountains
instance_of: Lake
countries: Canada
coordinates: lat: 45.45
lon: -74.016666666667
XEUN-FM's power was increased to 50 kW when the station moved to new facilities in 1976. In 1992, the FM station moved to a new tower in Ajusco, on land that had been donated to UNAM in 1986 by the government of the Federal District; the move decreased the station's power to 35 kW, which then increased to its current 100 kW with another new transmitter in 1995. Programming.

Geographic entities mentioned:
surface_form: Ajusco
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.2075
lon: -99.258055555556
After further disruptions to his lectures, Adorno cancelled the lectures for the rest of the seminar, continuing only with his philosophy seminar. In the summer of 1969, weary from these activities, Adorno returned once again to Zermatt, Switzerland, at the foot of Matterhorn to restore his strength. On 6 August, he died of a heart attack, during a vacation in Visp. Intellectual influences.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
He was always out climbing around the bluffs, or going down to the river, or going across the river into the woods.&quot; He attended Prospect Hill Elementary, where he ranked at the top of his class, and then, the overcrowded Burlington High School. Every August, the family vacationed in Michigan on the forested Marquette Island in Lake Huron, which the children took to exploring. Schooling.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Most of these statuettes show stylized clothes. Quite often the face is depicted. They were discovered at Mal'ta, at the Angara River, near Lake Baikal in Irkutsk Oblast, Siberia by the archeologists Sergey Zamyatnin, Georgy Sosnovsky, and Mikhail Gerasimov. These figurines are on display at the Hermitage Museum, Saint Petersburg. Discovery.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
These figurines are on display at the Hermitage Museum, Saint Petersburg. Discovery. Around 30 female statuettes of varying shapes were discovered at Mal'ta, at the Angara River, and near Lake Baikal in Irkutsk Oblast in Siberia. The wide variety of forms, combined with the realism of the sculptures and the lack of repetitiveness in detail, are definite signs of developed, albeit early, art.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Both approaches have gradients of up to 1 in 10 or 10%. In snow conditions, lorries are required to fit snow chains. In the area of the pass two more mountain roads branch off; one runs north to the Feldberg mountain and another south to the National Training Centre of the DSV on the Herzogenhorn (DE-NN). In the winter of 2005/2006, the road was blocked after heavy snow for avalanche blasting.

Geographic entities mentioned:
surface_form: Herzogenhorn
instance_of: Mountain
countries: Germany
coordinates: lat: 47.835
lon: 8.0194444444444
They include 14 lifts and 16 slopes, from simple family runs to sophisticated FIS World Cup routes. Using a Feldberg Pass, cross-country skiers have access to the trails at the Herzogenhorn (about 20 km), the Köpfle (3 km), Äulemer Kreuz and the Stübenwasen track. The 32 -kilometre-long Hinterzarten to Schluchsee long-distance cross country trail runs over the Feldberg Pass.

Geographic entities mentioned:
surface_form: Herzogenhorn
instance_of: Mountain
countries: Germany
coordinates: lat: 47.835
lon: 8.0194444444444
The high level of tourist traffic in the area of the Feldberg Pass causes major problems, especially in winter, something often exacerbated by wintry road conditions. Currently, a multi-storey car park is being built at the Pass by the foot of the Seebuck, which is designed to relieve parking along the road. The Feldberg Pass has twice been a mountaintop finish on the Deutschland Tour cycle race.

Geographic entities mentioned:
surface_form: Seebuck
instance_of: Mountain
countries: Germany
coordinates: lat: 47.864444444444
lon: 8.0222222222222
Elbe Sluice. The Elbe Sluice () also known as Střekov Sluice, Masaryk Sluice or Sluice of T. G. Masaryk is a lock on the Elbe river in Ústí nad Labem, Czech Republic, located immediately below the Střekov Castle. The main purpose was to navigate the Elbe in the area of the Střekov rapids, which were often impassable.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Life. He was born in Aberdeen on 10 March 1917, the son of Kenneth Fraser and Mary Fraser (née Boyd). He studied Medicine at Aberdeen University graduating MB ChB in 1940. In 1941, he joined the Royal Army Medical Corps and given the rank of captain. He was posted to the Chin Hills in Burma. Here a combined British and Indian force fought Japanese troops.

Geographic entities mentioned:
surface_form: Chin Hills
instance_of: Mountain
countries: Myanmar
coordinates: lat: 22.5
lon: 93.5
George, Istanbul. The skull, however, having been kept at the monastery at Vatopedi on Mount Athos in northern Greece, was not among the relics that were taken by the crusaders in the 13th century. In 1655, at the request of Tsar Alexei Mikhailovich, the skull was taken to Russia, for which the monastery was compensated in the sum of 2,000 rubles.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Two sites in Italy also claim to have the saint's skull: the Basilica di Santa Maria del Fiore in Florence and the &quot;Dal Pozzo&quot; chapel in Pisa. The right hand of Saint John is preserved at Philotheou Monastery on Mount Athos, and numerous smaller relics are scattered throughout the world. Collected works.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
He founded the Village of Otsego at the foot of the lake in 1786, creating a traditional plan for the village inspired by that of Burlington. He moved his family there, arriving on November 10, 1790. The judge and other investors also founded De Kalb, New York, near the east end of Lake Ontario and the St. Lawrence River, in 1803, platting approximately 64,000 acres and selling the parcels on.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The maintenance of the trail is performed by the staff of both adjacent national parks: the Polish Karkonosze National Park and the Czech Krkonoše National Park. The start point is located on Szrenica and the end in the Okraj pass / Pomezní boudy; the length of the trail is approx. 30 km; the level of difficulty is moderate. The trail partially overlaps with ski trails.

Geographic entities mentioned:
surface_form: Szrenica
instance_of: Mountain
countries: Poland
Czech Republic
coordinates: lat: 50.791388888889
lon: 15.514166666667
Until the Middle Ages, the peak area of Karkonosze remained untouched; the first people to explore it were treasure hunters looking for gold, and shepherds. Already in the 18th century ascents to the Sněžka/Śnieżka were fairly common, albeit the forms of organised tourism appeared in the second half of 19th century, along with railway access to Jelenia Góra, Szklarska Poręba and Karpacz.

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
Being situated in the upper part of the Karkonosze range, the trail's climate is generally more varied and less favourable than in the lower levels. Both major peaks on the trail, Sněžka and Szrenica are shrouded in fog or cloud for more than half of the year: for 296 days and 264 days respectively. The annual average temperature on Mount Sniezka reaches approx +0.2 °C, for Szrenica +1.9 °C.

Geographic entities mentioned:
surface_form: Sněžka
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.736111111111
lon: 15.740277777778
surface_form: Szrenica
instance_of: Mountain
countries: Poland
Czech Republic
coordinates: lat: 50.791388888889
lon: 15.514166666667
Acid rains, frequent in years 1980 and 1990 affected the area, though their destructive effect was not as powerful as in the lower zones. In some parts, especially around Mały Szyszak mountain meadows cover the large areas, used in 19th and in the first half of the 20th centuries as mountain pasture areas.

Geographic entities mentioned:
surface_form: Mały Szyszak
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.759444444444
lon: 15.648611111111
Numerous nonvertebrates also occur in the alpine zone. From Szrenica to Przełęcz Karkonoska. The trail starts at Szrenica joining the Main Sudeten Trail, which starts in Świeradów-Zdrój in the Jizera Mountains (ending in Prudnik in the Opawskie Mountains), subsequent mountain range and runs eastwards along the main ridge to Śnieżka, the highest summit of the range.

Geographic entities mentioned:
surface_form: Szrenica
instance_of: Mountain
countries: Poland
Czech Republic
coordinates: lat: 50.791388888889
lon: 15.514166666667
After a mild descent amongst the vast mountain pine shrub, it traverses the second highest peak of the range, Wielki Szyszak, the helmet shaped peak, which it derives its Polish name from. Covered in granite rocks, it elevates distinctly over other peaks of this part of the range, being the steepest and with the most alpine features.

Geographic entities mentioned:
surface_form: Wielki Szyszak
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.7775
lon: 15.5675
Covered in granite rocks, it elevates distinctly over other peaks of this part of the range, being the steepest and with the most alpine features. Then the trail touches the upper border of Śnieżne Kotły, two glacial cirques, the nature reserve. The radio tower above has been the distinctive landmark since the moment it was built. Sniezne Kotly offer landscapes over the whole Lower Silesia region.

Geographic entities mentioned:
surface_form: Śnieżne Kotły
instance_of: Valley
countries: Poland
coordinates: lat: 50.7833
lon: 15.5667
Sniezne Kotly offer landscapes over the whole Lower Silesia region. The trail traverses Łabski szczyt hosting the sources of the Elbe River on the Czech side, then runs along the top of another post-glacial cirque, Wielki Kocioł Jagniątkowski, which precedes two mild peaks with the prominent rock formations, Czeskie Kamienie and Śląskie Kamienie (Silesian Rocks and Czech Rocks).

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The pass is accessible by car and bus from the Czech side. From there on the way to Śnieżka, the trail traverses the mild peak Smogornia and, leading through the exposed grassy slope with common mountain pine shrubs slowly descends to the standalone rock Słonecznik.

Geographic entities mentioned:
surface_form: Smogornia
instance_of: Mountain
countries: Czech Republic
Poland
coordinates: lat: 50.755
lon: 15.676388888889
From there on the way to Śnieżka, the trail traverses the mild peak Smogornia and, leading through the exposed grassy slope with common mountain pine shrubs slowly descends to the standalone rock Słonecznik. On the left, suddenly a deep cirque appears with Wielki Staw and Maly Staw at the bottom, two postglacial lakes, accessible by means of a path downhill, marked blue.

Geographic entities mentioned:
surface_form: Wielki Staw
instance_of: Lake
countries: Poland
coordinates: lat: 50.7583
lon: 15.6936
Near the lakes, there are two mountain huts: &quot;Samotnia&quot; and &quot;Strzecha Akademicka&quot;. Then the trail crosses the plateau Równia pod Śnieżką with cirques on both sides. The Friendship trail intersects here with several important paths to remarkable towns: Špindlerův Mlýn and Karpacz.

Geographic entities mentioned:
surface_form: Równia pod Śnieżką
instance_of: Plateau
countries: Poland
Czech Republic
coordinates: lat: 50.74148
lon: 15.71688
Mountain huts are available on the trail or in the vicinity, mostly with refreshments and some offering catering for organised groups. The route is secured with fences along abysses (Śnieżne Kotły, Mały Staw and Wielki Staw), other climbing aids, mostly chains, are available in the most difficult parts.

Geographic entities mentioned:
surface_form: Wielki Staw
instance_of: Lake
countries: Poland
coordinates: lat: 50.7583
lon: 15.6936
St. Lawrence River. The St. Lawrence River (,) is a large international river in the middle latitudes of North America connecting the Great Lakes to the North Atlantic Ocean. Its waters flow in a northeasterly direction from Lake Ontario to the Gulf of St. Lawrence, traversing Ontario and Quebec in Canada and New York in the United States. A section of the river demarcates the Canada–U.S. border.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
With the draining of the Champlain Sea, due to a rebounding continent from the Last Glacial Maximum, the St. Lawrence River was formed. The Champlain Sea lasted from about 13,000 years ago to about 10,000 years ago and was continuously shrinking during that time, a process that continues today. The head of the St. Lawrence River, near Lake Ontario, is home to the Thousand Islands. Today, the St.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The average discharge below the Saguenay River is. At Quebec City, it is. The average discharge at the river's source, the outflow of Lake Ontario, is. The St. Lawrence River includes Lake Saint Francis at Salaberry-de-Valleyfield, Lake Saint-Louis south of Montreal and Lake Saint Pierre east of Montreal.

Geographic entities mentioned:
surface_form: Lake Saint-Louis
instance_of: Lake
countries: Canada
coordinates: lat: 45.401388888889
lon: -73.814166666667
Pierre Archipelago (classified a biosphere world reserve by the UNESCO in 2000) and the smaller Mingan Archipelago. Other islands include Île d'Orléans near Quebec City and Anticosti Island north of the Gaspé. It is the second longest river in Canada. Lake Champlain and the Ottawa, Richelieu, Saint-Maurice, Saint-François, Chaudière and Saguenay rivers drain into the St. Lawrence. The St.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
surface_form: Chaudière
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
The faults in the area are rift-related and comprise the Saint Lawrence rift system. According to the United States Geological Survey, the St. Lawrence Valley is a physiographic province of the larger Appalachian division, containing the Champlain section. However, in Canada, where most of the valley is, it is instead considered part of a distinct St.

Geographic entities mentioned:
surface_form: Champlain
instance_of: Valley
countries: United States
coordinates: lat: 44.45868
lon: -73.42617
However, in Canada, where most of the valley is, it is instead considered part of a distinct St. Lawrence Lowlands physiographic division, and not part of the Appalachian division. Sources. The St. Lawrence River also passes through Lake Saint-Louis and Lake Saint-Pierre in Quebec. Tributaries. The St. Lawrence River and the largest tributaries of the Great Lakes. The St.

Geographic entities mentioned:
surface_form: Lake Saint-Louis
instance_of: Lake
countries: Canada
coordinates: lat: 45.401388888889
lon: -73.814166666667
Lawrence Seaway, was officially opened on 26 June 1959 by Elizabeth II (representing Canada) and President Dwight D. Eisenhower (representing the United States). The Seaway (including the Welland Canal) now permits ocean-going vessels to pass all the way to Lake Superior. Modern Canada. Alcoa, Reynolds Metals Company, and General Motors (GM) Central Foundry operated along the St.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
These facilities released toxic substances into the St. Lawrence River and the surrounding area, including PCBs, PAHs, cyanide, fluoride, and dioxins. During the Second World War, the Battle of the St. Lawrence involved submarine and anti-submarine actions throughout the lower St. Lawrence River and the entire Gulf of St.

Geographic entities mentioned:
surface_form: Cabot Strait
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.233333333333
lon: -59.716666666667
Längsee (Tyrol). Längsee is a lake of Tyrol, Austria.

Geographic entities mentioned:
surface_form: längsee
instance_of: Lake
countries: Austria
coordinates: lat: 46.7894
lon: 14.4242
surface_form: längsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.5994
lon: 12.1547
Imperial Resort Beach Hotel. Imperial Resort Beach Hotel is a hotel in Entebbe, Uganda. Location. It is located on the shores of Lake Victoria, Africa's largest fresh-water lake, not far from Uganda's largest airport, Entebbe International Airport. This location is approximately, by road, south of Kampala, Uganda's capital city.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
During the monsoon months, the subtropical ridge moves northward due to the development of a thermal low from the intense solar radiation. The low develops over the Mexican Plateau and gradually moves northward towards the Four Corners region.

Geographic entities mentioned:
surface_form: Mexican Plateau
instance_of: Plateau
countries: Mexico
coordinates: lat: 24
lon: -103
Glenshesk. Glenshesk (Irish: &quot;Gleann Seisce&quot;,) is one of the nine Glens of Antrim in County Antrim, Northern Ireland. It was shaped by glacial erosion. The glen lies on the eastern side of Knocklayde mountain and flows out to the sea at Ballycastle. At the foot of the glen is the ruins of the Friary of Bunamargy built in 1485.

Geographic entities mentioned:
surface_form: Glens of Antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
surface_form: gleann seisce
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.1717
lon: -6.21611
surface_form: glenshesk
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.1717
lon: -6.21611
surface_form: glens of antrim
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.16
lon: -6.1
Glenshesk. Glenshesk (Irish: &quot;Gleann Seisce&quot;,) is one of the nine Glens of Antrim in County Antrim, Northern Ireland. It was shaped by glacial erosion. The glen lies on the eastern side of Knocklayde mountain and flows out to the sea at Ballycastle. At the foot of the glen is the ruins of the Friary of Bunamargy built in 1485.

Geographic entities mentioned:
surface_form: glenshesk
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.1717
lon: -6.21611
Pike of Stickle. Pike of Stickle, also known as Pike o’ Stickle, is a fell in the English Lake District. It reaches a height of and is situated in the central part of the national park in the valley of Great Langdale. The fell is one of three fells which make up the picturesque Langdale Pikes (the others being Harrison Stickle and Loft Crag), one of the best-known areas in Lakeland.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Pike of Stickle. Pike of Stickle, also known as Pike o’ Stickle, is a fell in the English Lake District. It reaches a height of and is situated in the central part of the national park in the valley of Great Langdale. The fell is one of three fells which make up the picturesque Langdale Pikes (the others being Harrison Stickle and Loft Crag), one of the best-known areas in Lakeland.

Geographic entities mentioned:
surface_form: Harrison Stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
surface_form: Loft Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
Topography. The Langdale Pikes form a raised rocky parapet around the southern and eastern edges of a high tableland centred upon Thunacar Knott. Pike of Stickle stands at the western end of this system and its crags fall south from the summit, presenting an arresting view from the valley floor below, or from further afield.

Geographic entities mentioned:
surface_form: Thunacar Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: thunacar knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
Pike of Stickle stands at the western end of this system and its crags fall south from the summit, presenting an arresting view from the valley floor below, or from further afield. Loft Crag stands next along the rampart, with Thorn Crag and Harrison Stickle further to the east.

Geographic entities mentioned:
surface_form: Loft Crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: Harrison Stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
Westward the height of the land gradually falls away to Martcrag Moor, a wide plateau with a few small tarns near the summit. Martcrag Moor represents the end of the Central Fells as defined by Alfred Wainwright, providing a high-level connection to Rossett Pike in the Southern Fells. Geology. The rearward slopes show evidence of the Pavey Ark Member, pebbly sandstone and breccia.

Geographic entities mentioned:
surface_form: Rossett Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.458211111111
lon: -3.1599611111111
surface_form: rossett pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.458211111111
lon: -3.1599611111111
Summit. Despite the peaked profile the summit is wide enough for a sizeable cairn surrounded by a small level area. Loft Crag and Gimmer Crag steal the attention in the foreground while Bowfell impresses across Langdale. A wide swathe of the Southern Fells is in view, whilst even distant Skiddaw puts in an appearance. Ascents.

Geographic entities mentioned:
surface_form: Bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
surface_form: bowfell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
Summit. Despite the peaked profile the summit is wide enough for a sizeable cairn surrounded by a small level area. Loft Crag and Gimmer Crag steal the attention in the foreground while Bowfell impresses across Langdale. A wide swathe of the Southern Fells is in view, whilst even distant Skiddaw puts in an appearance. Ascents.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
surface_form: skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
Loft Crag stands next along the rampart, with Thorn Crag and Harrison Stickle further to the east. 'Behind' Pike of Stickle to the north is the depression of Harrison Combe, beyond which are the twin tops of Thunacar Knott. Westward the height of the land gradually falls away to Martcrag Moor, a wide plateau with a few small tarns near the summit.

Geographic entities mentioned:
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
surface_form: thunacar knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
Ascents. Pike of Stickle rises steeply from Langdale, culminating in a narrow tapering summit which gives excellent views of the head of the valley, the fells of Bow Fell and Crinkle Crags showing well. The fell is usually climbed from Great Langdale with either the New or Old Dungeon Ghyll Hotels as the starting points.

Geographic entities mentioned:
surface_form: bow fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.447369444444
lon: -3.1658194444444
Ascents. Pike of Stickle rises steeply from Langdale, culminating in a narrow tapering summit which gives excellent views of the head of the valley, the fells of Bow Fell and Crinkle Crags showing well. The fell is usually climbed from Great Langdale with either the New or Old Dungeon Ghyll Hotels as the starting points.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
The factory was set up here because of a vein of greenstone, a very hard volcanic rock, which comes to the surface around the head of the valley. Evidence of axe manufacture have been found in many areas of Great Langdale but it is the screes of Pike of Stickle which have yielded the most discoveries.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: pike of stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
Geology. The rearward slopes show evidence of the Pavey Ark Member, pebbly sandstone and breccia. The Langdale face displays several strata: from the top The Lingmell Formation, Crinkle Member and Bad Step Tuff. These are composed, respectively, of tuff, lapilli tuff and breccia; rhyolitic tuff and breccia; and rhyolitic lava-like tuff. Summit.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Pike of Stickle. Pike of Stickle, also known as Pike o’ Stickle, is a fell in the English Lake District. It reaches a height of and is situated in the central part of the national park in the valley of Great Langdale. The fell is one of three fells which make up the picturesque Langdale Pikes (the others being Harrison Stickle and Loft Crag), one of the best-known areas in Lakeland.

Geographic entities mentioned:
surface_form: pike of stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
Martcrag Moor represents the end of the Central Fells as defined by Alfred Wainwright, providing a high-level connection to Rossett Pike in the Southern Fells. Geology. The rearward slopes show evidence of the Pavey Ark Member, pebbly sandstone and breccia. The Langdale face displays several strata: from the top The Lingmell Formation, Crinkle Member and Bad Step Tuff.

Geographic entities mentioned:
surface_form: pavey ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451
WAEB (AM). WAEB (790 kHz) is a commercial AM radio station licensed to Allentown, Pennsylvania, and serving the Lehigh Valley region of eastern Pennsylvania. It airs a news-talk radio format and is owned by iHeartMedia, Inc. The studios and offices are on Alta Drive in Whitehall. By day, WAEB is powered at 3,600 watts.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
He won &quot;Badge Golden Safavid&quot; in Iran for promoting Persian Language and Literature. Early life. In 1965, Bayrami was born near the Sabalan mountain in Ardabil, Azerbaijan province, Iran, and emigrated with his parents to Tehran & Karaj in 1962, where he is currently living. In 1987, he became a conscript soldier for the Iranian army and served his country in the war with Iraq.

Geographic entities mentioned:
surface_form: Sabalan
instance_of: Mountain
countries: Iran
coordinates: lat: 38.266944444444
lon: 47.836944444444
Parks. The neighborhood includes two parks: Cowen Park, in the southeast corner (contiguous with the larger Ravenna Park of Ravenna); and Froula Playground, in the northeast corner, adjacent to the Green Lake Reservoir. The source of Ravenna Creek has been reduced to Cowen Park; since completion of the partial daylighting in 2006, the creek has been reconnected to Lake Washington. Transportation.

Geographic entities mentioned:
surface_form: Lake Washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
A year later, on January 4, 2018, Densmore accepted a second proclamation from Los Angeles Council member Paul Koretz at the junction of Densmore Avenue and Morrison Street in Encino, Los Angeles in the San Fernando Valley in which honorary street signs were unveiled. Personal life. Densmore has married four times.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
In Mono County, California, they evaluated strontium and lead isotopic data, finding that the obsidian from Glass Mountain was the result of fractional crystallization. Noble and Korringa continued their research by studying calcium variations in whole-rock and glass samples from Quaternary lavas in Crater Lake, Oregon.

Geographic entities mentioned:
surface_form: Crater Lake, Oregon
instance_of: Lake
countries: United States
coordinates: lat: 42.943611111111
lon: -122.10666666667
The term forms part of some toponyms of Kazakhstan, such as Altybaysor, Aralsor, Atansor, Azhibeksor, Bauzhansor, Karasor, Koksengirsor, Mangisor, Maysor, Meshkeysor, Shandaksor, Sholaksor, Shureksor, Sorasha, Sorkol, Sormoildy, Tuzdysor, Zhaltyrsor, Zhyngyldysor and Sor Tuzbair. Description. A sor forms in the flatland of arid areas or deserts.

Geographic entities mentioned:
surface_form: Altybaysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.57722
lon: 76.60528
surface_form: Aralsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.04
lon: 48.2347222
surface_form: Bauzhansor
instance_of: Lake
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 52.753055555556
lon: 79.461388888889
surface_form: Karasor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.84889
lon: 75.35222
surface_form: Koksengirsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 53.03944
lon: 71.765
surface_form: Maysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 51.9075
lon: 74.43222222222222
surface_form: Meshkeysor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 48.688888888889
lon: 68.721666666667
surface_form: Sholaksor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.48369
lon: 74.02649
surface_form: Shureksor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 52.24261
lon: 75.79811
surface_form: Zhaltyrsor
instance_of: Lake
countries: Kazakhstan
coordinates: lat: 49.876388888889
lon: 64.979722222222
In the dry flat expanse the groundwater is located close to the surface. Although usually a sor is located away from the seashore, an inlet in the southern coast of the Dead Kultuk had the characteristics of a sor and was known as &quot;Sor Kaydak&quot;. However, in recent decades it lost its distinct shoreline owing to the rise of the level of the Caspian Sea and has become a salt marsh. Flora.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Doi Phi Pan Nam. Doi Phi Pan Nam, is a 1,745 m high mountain of the Luang Prabang Range (ทิวเขาหลวงพระบาง) in Southeast Asia. It is at the east end of the Thai highlands, on the Laos-Thailand border. The Wa River has its source beneath this mountain.

Geographic entities mentioned:
surface_form: doi phi pan nam
instance_of: Mountain
countries: Thailand
Laos
coordinates: lat: 19.12583333
lon: 101.25611111
The mean annual runoff is per year. The headwaters of the rivers rise on the northern edge of the Barkly Tableland. Tributaries of the McArthur River include Tooganginie Creek, and the Kilgour and Clyde rivers. The river has a long tidal estuary which extends inland to the town of Borroloola.

Geographic entities mentioned:
surface_form: Barkly Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -19
lon: 138
The division subsequently attacked across the Roer, pierced the Siegfried Line, reached the Rhine at Wesel on March 10, and crossed March 25–26. It destroyed the enemy's defenses across the Herne Canal and reached the Ruhr River early in April, when it was ordered to move to the Elbe April 12.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Rehabilitation of the Pasig River. The Pasig River is a river in the Philippines running through the heart of Manila. It flows from Laguna de Bay to Manila Bay for. Its average width is and average depth around. The river runs through some of the most populated areas in the Philippines.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Plans are being implemented for a dike to be built at the entrance to the Pasig River at Laguna de Bay to keep flood waters out during rainy season to prevent major areas of the city from flooding; this is coming under great controversy as the people living around Laguna de Bay would have to deal with flooding.

Geographic entities mentioned:
surface_form: Laguna de Bay
instance_of: Lake
countries: Philippines
coordinates: lat: 14.508888888889
lon: 121.11888888889
Spruce was born to William Everett and Fannie May Spruce, as the oldest of six, in Holland, Arkansas, a small town near Conway. When he was three, his family moved to Adams Mountain, where his father grew apples and peaches. Spending time atop the mountain in rural Arkansas sparked his curiosity for the natural world and he claimed that sketching landscapes was his way of “understanding things”.

Geographic entities mentioned:
surface_form: Adams Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9311
lon: -81.7244
Bath County, Virginia. Bath County is a United States county located in the Shenandoah Valley on the central western edge of the Commonwealth of Virginia. As of the 2020 census, the population was 4,209, making it the second-least populous county in Virginia. Bath's county seat is Warm Springs, while the largest community is Hot Springs.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Like much of the Shenandoah Valley region, Bath had a relatively large share of residents descended from Scots-Irish immigrants and German farmers, both of whom were moving southward from Pennsylvania. By 1800, Bath County's population was mostly subsistence farmers, though some were also artisans and smaller amounts were shopkeepers. Economy.

Geographic entities mentioned:
surface_form: Shenandoah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.5
lon: -78.85
Vaughn Pond (Massachusetts). Vaughn Pond is a pond in Carver, Massachusetts near the center of the town.

Geographic entities mentioned:
surface_form: vaughn pond (massachusetts)
instance_of: Lake
countries: United States
coordinates: lat: 41.8908
lon: -70.7797
Vaughn Pond (Massachusetts). Vaughn Pond is a pond in Carver, Massachusetts near the center of the town.

Geographic entities mentioned:
surface_form: vaughn pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8908
lon: -70.7797
Savio (river). The Savio is a river in the Emilia-Romagna region of northern Italy. Its source is in the province of Forlì-Cesena near Montecoronaro on Mount Castelvecchio which is near the western side of Mount Fumaiolo. The source is at an elevation of and is marked by an iron monument.

Geographic entities mentioned:
surface_form: Mount Castelvecchio
instance_of: Mountain
countries: Italy
coordinates: lat: 43.8001
lon: 12.0502
surface_form: Mount Fumaiolo
instance_of: Mountain
countries: Italy
coordinates: lat: 43.78755555555556
lon: 12.076097222222222
Distribution and habitat. This species is distributed from Fennoscandia to eastern Siberia; in addition, isolated mountain populations occur in the Alps, Scotland, the Baltics, northeastern Poland, and Hokkaidō. In Ireland, the Irish hare (&quot;L. t. hibernicus&quot;) lives on lowland pastures, coastal grasslands, and salt marshes, not just in the mountains.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Kose Valgjärv. Kose Valgjärv is a lake of Estonia.

Geographic entities mentioned:
surface_form: valgjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 58.08916855
lon: 26.63861084
surface_form: valgjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.9
lon: 25.87
surface_form: valgjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.7240274
lon: 26.9314221
surface_form: kose valgjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.812225
lon: 27.039098
surface_form: valgjärv
instance_of: Lake
countries: Estonia
coordinates: lat: 57.812225
lon: 27.039098
Description. The range is bounded by Pine Valley to the west, Wah Wah Valley to the east, the Escalante Desert to the south, and on trend with the Confusion Range to the north. The Wah Wah Mountains are located in Beaver and Millard counties. State Route 21 bisects the range, crossing over Wah Wah Summit at about above sea level.

Geographic entities mentioned:
surface_form: Wah Wah Valley
instance_of: Valley
countries: United States
coordinates: lat: 38.7222
lon: -113.26
Christensenfjella. Christensenfjella is a mountain in Nordenskiöld Land at Spitsbergen, Svalbard. It is named after Norwegian shipowner Christen Christensen. The mountain has several peaks, the highest is 682 m.a.s.l. It is located east of Systemafjellet and north of Orustdalen, and is proximate to the glaciers of Aldegondabreen and Linnébreen.

Geographic entities mentioned:
surface_form: Systemafjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 77.9482
lon: 13.8956
surface_form: Orustdalen
instance_of: Valley
countries: Norway
coordinates: lat: 77.936
lon: 13.96
Christensenfjella. Christensenfjella is a mountain in Nordenskiöld Land at Spitsbergen, Svalbard. It is named after Norwegian shipowner Christen Christensen. The mountain has several peaks, the highest is 682 m.a.s.l. It is located east of Systemafjellet and north of Orustdalen, and is proximate to the glaciers of Aldegondabreen and Linnébreen.

Geographic entities mentioned:
surface_form: christensenfjella
instance_of: Mountain
countries: Norway
coordinates: lat: 77.963
lon: 13.973
Under Bernese rule. Much of the region that would become the Canton of Léman was conquered in 1538 by Bern and had been jointly administered by Bern and Fribourg for the following two and a half centuries. As the doctrines of the French Revolution spread, they found a warm reception from the citizens of the French-speaking towns around Lake Geneva () which was known as Pays de Vaud.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The largely untouched, forested landscape of the park was the result of a 1891 visit from famed landscape architect Frederick Law Olmsted, who refused to develop a plan for it due to his belief that it &quot;should not be marred by the intrusion of artificial objects.&quot;
The park. Presque Isle Park is located in the Upper Peninsula of Michigan on the coast of Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Lake Yankton (South Dakota). Lake Yankton, also called Cottonwood Lake, is an artificial lake that was originally part of the main channel of the Missouri River on the border of the U.S. States of Nebraska and South Dakota, near Yankton, South Dakota. The lake has an approximate surface area of and has a maximum depth of.

Geographic entities mentioned:
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 45.109357
lon: -97.2247008
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 44.835574
lon: -99.9058888
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 45.7325
lon: -97.426944444444
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 44.1927927
lon: -98.7571033
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 44.7899106
lon: -98.6745112
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 45.761111111111
lon: -96.019722222222
surface_form: cottonwood lake
instance_of: Lake
countries: United States
coordinates: lat: 45.1276426
lon: -97.6994205
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
States of Nebraska and South Dakota, near Yankton, South Dakota. The lake has an approximate surface area of and has a maximum depth of. The lake is located immediately downstream (east) of Gavins Point Dam and Lewis and Clark Lake, located just north of the current location of the main channel of the Missouri River. History.

Geographic entities mentioned:
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 48.2238736
lon: -118.1367659
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 60.244166666667
lon: -154.28527777778
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 42.1206
lon: -84.3264
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 47.383333333333
lon: -122.175
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 44.9375
lon: -87.204
surface_form: clark lake
instance_of: Lake
countries: United States
coordinates: lat: 46.225188
lon: -89.320288
Lake Yankton (South Dakota). Lake Yankton, also called Cottonwood Lake, is an artificial lake that was originally part of the main channel of the Missouri River on the border of the U.S. States of Nebraska and South Dakota, near Yankton, South Dakota. The lake has an approximate surface area of and has a maximum depth of.

Geographic entities mentioned:
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: lake yankton (south dakota)
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
The lake is located immediately downstream (east) of Gavins Point Dam and Lewis and Clark Lake, located just north of the current location of the main channel of the Missouri River. History. Originally the area now known as Lake Yankton was part of the main channel of the Missouri River. During the construction of Gavins Point Dam (1952-1957), the U.S.

Geographic entities mentioned:
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
After dam construction completion a dike, called the Training Dike, was constructed by the Corps to &quot;train&quot; the river to its current location and flow, thus creating a land barrier separating Lake Yankton from the Missouri River. The lake was then impounded in order to control the lake level for fish and wildlife enhancement, along with recreational opportunities.

Geographic entities mentioned:
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
Camping, hiking, biking, bird watching, fishing and hunting are popular activities around the lake. Lake Yankton Beach, located within Training Dike Day-Use Area is a popular swimming beach in summer months. Lake Yankton Island is located within the lake and is approximately in size. This Cottonwood-dominated island was originally a sandbar in the Missouri River.

Geographic entities mentioned:
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
2011 Flood and fisheries restoration. During the 2011 Missouri River Floods the Missouri River water rose high enough that the river had backed into Lake Yankton, as a result the lake was infiltrated with Asian Carp, an aquatic invasive species not native to South Dakota/Nebraska that are well-established in the Missouri River below Gavins Point Dam.

Geographic entities mentioned:
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 44.246111111111
lon: -95.865833333333
surface_form: lake yankton
instance_of: Lake
countries: United States
coordinates: lat: 42.855509
lon: -97.472443
The line is the oldest one on the metro system, having been opened as a light railway in 1898 by the Holmenkolbanen company. Originally it ran for from Majorstuen Station to Besserud. In 1916, the line was extended to Tryvann, with the last being used for freight only. In 1928, the city terminus was moved to the underground Nationaltheatret Station. Operations.

Geographic entities mentioned:
surface_form: Tryvann
instance_of: Lake
countries: Norway
coordinates: lat: 59.997222222222
lon: 10.668888888889