Sarmila/GeoWiki-Features huggingface dataset:
Monte Emilius. Monte Emilius () (3,559 m) is a mountain of the Graian Alps in Aosta Valley, north-western Italy. Located just above the town of Aosta, from where it is visible looking southwards behind the lower Becca di Nona, it is usually climbed starting from the ski resort of Pila, at a height of 1,870 m. History.

Geographic entities mentioned:
surface_form: Becca di Nona
instance_of: Mountain
countries: Italy
coordinates: lat: 45.687
lon: 7.366
Aostan canons thought about naming it &quot;Pic Pie&quot; in honour of Pope Pius IX, but decided against it as &quot;Pie&quot; in French also means magpie. Ascent. A marked path from Pila usually takes one to the summit, past various lakes, with a bit of scrambling involved. The view from the top includes famous peaks such as Mont Blanc, Monte Rosa, the Matterhorn and Grand Combin

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
surface_form: Grand Combin
instance_of: Mountain
countries: Switzerland
coordinates: lat: 45.9375
lon: 7.2991666666667
Monte Emilius. Monte Emilius () (3,559 m) is a mountain of the Graian Alps in Aosta Valley, north-western Italy. Located just above the town of Aosta, from where it is visible looking southwards behind the lower Becca di Nona, it is usually climbed starting from the ski resort of Pila, at a height of 1,870 m. History.

Geographic entities mentioned:
surface_form: monte emilius
instance_of: Mountain
countries: Italy
coordinates: lat: 45.676944444444
lon: 7.3827777777778
The arils are mature 6–9 months after pollination. Age. Japanese yew is a long-lived tree. Individual trees from Sikhote-Alin are known to have been 1,000 years old. One specimen in Tottori, Japan, known as &quot;Sentsūzan-no-Ichii&quot; (&quot;Yew of Mount Sentsū&quot;) is estimated at 2,000 years old. Toxicity.

Geographic entities mentioned:
surface_form: Mount Sentsū
instance_of: Mountain
countries: Japan
coordinates: lat: 35.15583333
lon: 133.17861111
Annie Powell. Annie Powell (8 September 1906 – 29 August 1986) was a Welsh Communist politician, teacher, and trade unionist who served as Mayor of Rhondda from 1979 to 1980, making her the first Communist mayor in Wales and widely recognised as the first female Communist mayor in Britain.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Born into a Welsh-speaking family in Ystrad, Rhondda, Powell witnessed the poverty of the Great Depression during her early teaching career, which led her to join the Labour Party and subsequently the Communist Party of Great Britain (CPGB) in 1938. A dedicated educator for four decades, Powell taught in Welsh throughout her career and was active in the National Union of Teachers.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Early life and education. Annie Powell was born on 8 September 1906 in Ystrad, Rhondda, Glamorgan. She was educated at Pentre Grammar School before attending Glamorgan Training College, Barry, in the 1920s to train as a teacher. Political awakening. Powell became interested in politics while at Glamorgan Training College during the period of the 1926 General Strike.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Imperial Valley Transit. Imperial Valley Transit (IVT), also known as IV Transit, is the provider of mass transportation in California's Imperial Valley, serving the cities of El Centro, Calexico, Brawley, and Imperial. Formed in 1989 with just 3 buses and serving close to 3000 passengers per month, the agency currently serves more than 73,000 passengers per month with over 20 buses in operation.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Each village has a fortified church. Geography. The commune lies within the southern reaches of the Transylvanian Plateau. The river Hârtibaciu flows through the village of Bărcuț; its left tributary, Valea Morii, flows through the village of Seliștat. Șoarș is located in the northwestern part of the county, north of Făgăraș, on the border with Sibiu County.

Geographic entities mentioned:
surface_form: Transylvanian Plateau
instance_of: Plateau
countries: Romania
coordinates: lat: 46.5
lon: 24.5
In the mountainous regions in the south and southwest of the state, the tropical climate is strongly influenced by altitude, and the average temperatures are lower. Lakes. One of the most important lake districts in Brazil lies on the banks of the Doce River. The area contains some 26 large lakes, the biggest of which is called Juparanã Lagoon. Topography.

Geographic entities mentioned:
surface_form: Juparanã Lagoon
instance_of: Lake
countries: Brazil
coordinates: lat: -19.34916667
lon: -40.09722222
The area contains some 26 large lakes, the biggest of which is called Juparanã Lagoon. Topography. The state can be divided into two areas: the low lying coastline and the highland area known as &quot;Serra&quot; (where one can find the  Pico da Bandeira), which is part of the larger Serra do Caparaó range. Demographics. According to the 2022 census, 3,833,712 people were residing in the state.

Geographic entities mentioned:
surface_form: Pico da Bandeira
instance_of: Mountain
countries: Brazil
coordinates: lat: -20.435151
lon: -41.7963
Hut Point Peninsula to the south helps deflect icebergs propelled by prevailing southerly winds. The long, narrow Erebus ice stream drains from the western slope of Mount Erebus, an active volcano rising in elevation. The mountain constantly replenishes the glacial ice stream, as annual snow fall exceeds annual snow melt.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
Portions of the glacier tongue become unstable, rupture, and calve icebergs. Such instability in part comes from the flexing and tension the ice beam undergoes from being cantilevered over the sea. Moreover, the river of ice carries with it weaknesses introduced by earlier fractures experienced during its journey down the slopes of Mount Erebus. Effects on the ocean.

Geographic entities mentioned:
surface_form: Mount Erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Erebus Glacier Tongue. The Erebus Glacier Tongue is a mountain outlet glacier and the seaward extension of Erebus Glacier from Ross Island. It projects into McMurdo Sound from the Ross Island coastline near Cape Evans, Antarctica. The glacier tongue varies in thickness from at the snout to at the point where it is grounded on the shoreline. Explorers from Robert F.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Erebus Glacier Tongue. The Erebus Glacier Tongue is a mountain outlet glacier and the seaward extension of Erebus Glacier from Ross Island. It projects into McMurdo Sound from the Ross Island coastline near Cape Evans, Antarctica. The glacier tongue varies in thickness from at the snout to at the point where it is grounded on the shoreline. Explorers from Robert F.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Explorers from Robert F. Scott's Discovery Expedition (1901–1904) named and charted the glacier tongue. Erebus Glacier Tongue is about high and is centred upon 77.6 degrees south latitude, 166.75 degrees east longitude. The portion of the glacier tongue extending beyond the shoreline or grounding line floats upon the water.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Ice tongues emerge when a glacier ice stream flows rapidly (relative to surrounding ice) into the sea or a lake, usually in a protected area. For instance, Capes Evans and Royds extending from Ross Island protect the Erebus Glacier Tongue from the open waters of the Ross Sea. Hut Point Peninsula to the south helps deflect icebergs propelled by prevailing southerly winds.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
The long, narrow Erebus ice stream drains from the western slope of Mount Erebus, an active volcano rising in elevation. The mountain constantly replenishes the glacial ice stream, as annual snow fall exceeds annual snow melt. The Erebus Glacier Tongue is a dynamic structure subject to a host of internal and external stresses which affect its shape, size, and durability. Harbors.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
The Erebus Glacier Tongue is a dynamic structure subject to a host of internal and external stresses which affect its shape, size, and durability. Harbors. The frozen sea ice of Erebus Bay surrounding the Erebus Glacier Tongue typically breaks out during the summer. This exposes the glacier tongue to pounding waves from McMurdo Sound.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Breaking off pieces of ice, 10 or 20,000 years old, we melt it in our mouths and savour the taste of pure, uncontaminated water. Scientists funded by a National Science Foundation grant have retrieved rare underwater views of the Erebus Glacier Tongue caves by mounting cameras on Weddell seals. Images revealed rocks and dead fish frozen into the ice.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Video also depicted other Weddell seals that appeared to use the underwater caves as hiding places from predators such as the orca (or killer whale) and the leopard seal. Weddell seals are commonly sighted by visitors to the Erebus Glacier Tongue. Each year 300 to 400 Weddell seal pups are born to a colony of seals that live in adjoining Erebus Bay.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Weddell seals are commonly sighted by visitors to the Erebus Glacier Tongue. Each year 300 to 400 Weddell seal pups are born to a colony of seals that live in adjoining Erebus Bay. The seals have been distinctively marked and re-sighted since 1969. The nearly 40-year study represents one of the longest field investigations of its type, according to a Montana State University report.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
The seals have been distinctively marked and re-sighted since 1969. The nearly 40-year study represents one of the longest field investigations of its type, according to a Montana State University report. Emperor and Adelie penguins are also found in the vicinity of the Erebus Glacier Tongue. Adelie are particularly noted for their rookeries on Erebus Bay's rocky north shore at nearby Cape Royds.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Emperor and Adelie penguins are also found in the vicinity of the Erebus Glacier Tongue. Adelie are particularly noted for their rookeries on Erebus Bay's rocky north shore at nearby Cape Royds. Penguins, like the Weddell seal, are preyed upon by orcas and leopard seals. The presence of penguins also attracts the predatory skua seabird. On January 2 thick weather caused party to lay up.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
The party then proceeded round the Tongue to Tent Island, which was also searched, a complete tour of the island being made. Dynamics. The dynamics within floating ice streams such as the Erebus Glacier Tongue are complex. For instance, typically ice streams such as the Erebus Glacier Tongue, which ranges from 50 to 300 meters thick, contain smaller streams of ice.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Dynamics. The dynamics within floating ice streams such as the Erebus Glacier Tongue are complex. For instance, typically ice streams such as the Erebus Glacier Tongue, which ranges from 50 to 300 meters thick, contain smaller streams of ice. Each ice flow produces its own set of stress fields. Thus, throughout the glacier tongue, different flow rates and tensions are present.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Each ice flow produces its own set of stress fields. Thus, throughout the glacier tongue, different flow rates and tensions are present. Stress and friction increase along the flanks of ice streams such as the Erebus Glacier Tongue. Stress appears as crevasses as the ice flow rate is slowed. Friction created by the Earth's topography at the bottom of the glacier also slows the ice stream.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Such sliding features the glacier jerking forward due to lubrication from bottom melt-water. Ice streams such as the Erebus Glacier Tongue wax and wane like the moon. Indeed, British researchers in 2006 discovered a correlation between lunar tides (caused by gravitational pull) and variances in flow speed of the Rutland Ice Stream in Antarctica. Previously a team of U.S.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Such surges may occur over a period of months or years. Then the movement stops. Scientists have measured Erebus Glacier Tongue's length as growing about 160 meters yearly. The Erebus Glacier Tongue flow pushes the glacier into Erebus Bay where it butts against seasonal ice pack. This massive but gradual collision of ice against ice creates pressure ridges in the glacier.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Then the movement stops. Scientists have measured Erebus Glacier Tongue's length as growing about 160 meters yearly. The Erebus Glacier Tongue flow pushes the glacier into Erebus Bay where it butts against seasonal ice pack. This massive but gradual collision of ice against ice creates pressure ridges in the glacier. Portions of the glacier tongue become unstable, rupture, and calve icebergs.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Iceberg calving. The forces of wave action from McMurdo Sound, tides, and internal stresses exploit the glacier tongue's weaknesses. Subsequently, small icebergs and bergy bits typically calf from the Erebus Glacier Tongue but only when the sea ice has broken up. Subsequently, iceberg calving is seasonal and periodic, as open water is needed to release the bergs into Erebus Bay.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Subsequently, small icebergs and bergy bits typically calf from the Erebus Glacier Tongue but only when the sea ice has broken up. Subsequently, iceberg calving is seasonal and periodic, as open water is needed to release the bergs into Erebus Bay. Waters at the glacier tongue that receive the icebergs vary in depth from a minimum of. Members of Robert F.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
Such calving along the glacier snout naturally leads to shortening, while icebergs released from the glacier tongue sides contribute to the glacier's narrowing. The Erebus Glacier Tongue produces flat-topped or tabular icebergs. It calved most recently in 2013, around a decade earlier than expected.

Geographic entities mentioned:
surface_form: erebus
instance_of: Mountain
coordinates: lat: -77.533333333333
lon: 167.28333333333
surface_form: erebus glacier tongue
instance_of: Landform
coordinates: lat: -77.7341
lon: 166.528
Waters at the glacier tongue that receive the icebergs vary in depth from a minimum of. Members of Robert F. Scott's Terra Nova Expedition first observed the glacier tongue calving in March 1911 when a 4 km section broke off during a gale. A similar event in March 1990 produced a 100-million ton iceberg, 3.5 km long, from the glacier tongue.

Geographic entities mentioned:
surface_form: terra nova
instance_of: Mountain
coordinates: lat: -77.5167
lon: 167.95
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The ice caves are a popular attraction for residents from nearby the McMurdo Station and Scott Base research stations. Visitors report observing stalactite-like icicles on the cave ceilings, as well as intricate ice crystals. Sunlight filtering through ice into the caves bathes the interiors with diffuse blue light. Sitting quietly we absorb the natural beauty.

Geographic entities mentioned:
surface_form: light
instance_of: Mountain
coordinates: lat: -74.2667
lon: -61.9833
Each year 300 to 400 Weddell seal pups are born to a colony of seals that live in adjoining Erebus Bay. The seals have been distinctively marked and re-sighted since 1969. The nearly 40-year study represents one of the longest field investigations of its type, according to a Montana State University report. Emperor and Adelie penguins are also found in the vicinity of the Erebus Glacier Tongue.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
The glacier tongue varies in thickness from at the snout to at the point where it is grounded on the shoreline. Explorers from Robert F. Scott's Discovery Expedition (1901–1904) named and charted the glacier tongue. Erebus Glacier Tongue is about high and is centred upon 77.6 degrees south latitude, 166.75 degrees east longitude.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The ice caves include inter-locked crevasses covered by snow bridges. The ice caves are a popular attraction for residents from nearby the McMurdo Station and Scott Base research stations. Visitors report observing stalactite-like icicles on the cave ceilings, as well as intricate ice crystals. Sunlight filtering through ice into the caves bathes the interiors with diffuse blue light.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The floating glacier has a major effect on the local ocean. Its melting has been thought to create Double diffusive convection effects. A 2010 expedition funded by the Marsden Fund supported deployment of Timothy Haskell's sea ice camp right next to the tongue. Observations from the camp showed how the tide flowed beneath and along the tongue and was affected by submarine topography.

Geographic entities mentioned:
surface_form: haskell
instance_of: Mountain
coordinates: lat: -66.75
lon: -64.2667
surface_form: marsden
instance_of: Mountain
coordinates: lat: -67.8667
lon: 66.05
On January 2 thick weather caused party to lay up. On 3rd, glacier was further examined, and several slopes formed by snow led to top of glacier, but crevasses between slope and the tongue prevented crossing. The party then proceeded round the Tongue to Tent Island, which was also searched, a complete tour of the island being made. Dynamics.

Geographic entities mentioned:
surface_form: tent
instance_of: Mountain
coordinates: lat: -67.6
lon: -65.35
These sites represent both indigenous peoples and early European settlers. Projectile points of &quot;Hi-Lo&quot; style have been discovered at four Late Paleo-Indian (10000-7000 BCE) sites in the Duffins Creek watershed. Around Lake Ontario, the indigenous peoples have been commonly associated with the lake shore, which fluctuated because of the melting glaciers.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
The first mill in the new settlement was established in 1810 by Timothy Rogers on the banks of Duffins Creek. At the time of Rogers's arrival, thousands of salmon from Lake Ontario came to the Duffins Creek. By the time of his death in 1834, the salmon had practically disappeared from the stream.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Course. The headwaters of the Duffins Creek are located in the Oak Ridges Moraine area, within the boundaries of Uxbridge, Pickering, Markham, and Whitchurch-Stouffville. The mouth of the stream is located in Ajax. The Duffins Creek drains an area of 283 sq. km., much of which is owned by the government. The federal government owns around 75 sq.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
The federal government owns around 75 sq. km., the provincial government of Ontario owns around 28 sq. km., and the Toronto and Region Conservation Authority (TRCA) owns around 23 sq. km. List of tributaries. Although Duffins Creek is a single waterway entering Lake Ontario at Duffins Marsh in Ajax, there are 12 other waterways that branches off Duffins towards the Oak Ridges Moraine.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
Duffins Creek. Duffins Creek is a waterway in the eastern end of the Greater Toronto Area in Ontario, Canada. The watershed of the Duffins Creek is part of the Durham Region (Uxbridge, Pickering and Ajax) and the York Region (Markham and Whitchurch-Stouffville). Etymology and names.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
These sites represent both indigenous peoples and early European settlers. Projectile points of &quot;Hi-Lo&quot; style have been discovered at four Late Paleo-Indian (10000-7000 BCE) sites in the Duffins Creek watershed. Around Lake Ontario, the indigenous peoples have been commonly associated with the lake shore, which fluctuated because of the melting glaciers.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
Around Lake Ontario, the indigenous peoples have been commonly associated with the lake shore, which fluctuated because of the melting glaciers. At the end of the Last Glacial Period, the Duffins Creek met Lake Ontario at a point located 10-20 m below the present surface level. So, any evidence of indigenous activity at the mouth of the Duffins Creek would be under water now.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
Detailed excavations have not been carried out at these sites, so little information is available about the pre-historic residents of the area. Several sites dated to the early and middle Woodland period (1000 BCE-700 CE) exist along the Duffins Creek, but not much research has been done on them.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
This family lived at the east edge of the Duffins Creek marshes until the mid-19th century. Unlike the Rouge River watershed, where a well-established trail ran along the stream, the Duffins Creek watershed remained largely ignored by the early European visitors in the area. In 1670, French missionaries from Ganatsekwyagon reached the Duffins Creek, but did not settle there.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
In 1670, French missionaries from Ganatsekwyagon reached the Duffins Creek, but did not settle there. In the 1770s, Mike Duffin, an Irish fur trader, became the first person of European descent to settle in the Duffins Creek area. He built a cabin on the east side of the Creek, north of a trail that later became the Kingston Road.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
The dams also cut off the salmon from their spawning grounds. Pickering Village, a settlement initially known as &quot;Duffins Creek&quot;, developed along the stream, in what is now Ajax. The first mill in the new settlement was established in 1810 by Timothy Rogers on the banks of Duffins Creek. At the time of Rogers's arrival, thousands of salmon from Lake Ontario came to the Duffins Creek.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
The community around the DIL munitions plant evolved into the town of Ajax in the mid-20th century. The northern part of the Duffins Creek watershed did not develop as rapidly as other watersheds in the Greater Toronto area, because the Government of Canada marked a large portion of land for the proposed Pickering Airport. Course.

Geographic entities mentioned:
surface_form: duffins creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.81652
lon: -79.04128
Fossli Provincial Park. Fossli Provincial Park is a provincial park in British Columbia, Canada, located on Stirling Arm of Sproat Lake on Vancouver Island. The 52-hectare park, west of Port Alberni, is accessible by water or private logging road. It has few services, but has a 30-minute hiking trail to an old homestead site.

Geographic entities mentioned:
surface_form: Sproat Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.2667
lon: -125.033
It is a poetry of scenic wonders, a poetry of officials exiled for their views and beliefs, and a poetry of dissent against submitting to government control. Xiaoxiang poetry is geographically associated with the Xiaoxiang region, around and south of Dongting Lake. The Xiaoxiang genre of literature is often associated with similarly themed Chinese calligraphy and Chinese painting.

Geographic entities mentioned:
surface_form: Dongting Lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 29.316666666667
lon: 112.95
Lake Uspaccocha. Lake Uspaccocha or Uspaycocha (possibly from Quechua &quot;uspha, uchpha&quot; ash, rest of combustion, &quot;qucha&quot; lake, lagoon, &quot;ash lake&quot;) is a lake in the Andes of Peru located in the Apurímac Region, Abancay Province, Abancay District. It is situated in the Ampay National Sanctuary, at 3750 meters above sea level, north of the city of Abancay.

Geographic entities mentioned:
surface_form: uspaccocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.5744
lon: -72.8883
surface_form: lake uspaccocha
instance_of: Lake
countries: Peru
coordinates: lat: -13.5744
lon: -72.8883
The hat has been adopted as a part of Nepali national dress for men, as an alternative to the Palpali Dhaka topi. History. The hat is said to be in used since Malla era in Nepal, according to historians. However, the hat was only limited to Kathmandu Valley then. The hat became famous nationwide after King Tribhuvan and his son Mahendra started wearing it.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Tarahi (volcano). Tarahi is a high andesite volcano, in the Kaikohe-Bay of Islands volcanic field in New Zealand. Northwest of Tarahi is a smaller, basaltic scoria cone, Haruru pā, before the higher cone of Te Ahuahu. To its immediate east is Putahi and the location of a famous battle of the Flagstaff War adjacent to Lake Ōmāpere.

Geographic entities mentioned:
surface_form: Lake Ōmāpere
instance_of: Lake
countries: New Zealand
coordinates: lat: -35.347056
lon: 173.789111
Its nearest higher neighbor is Mount Ben Stewart, to the northwest. History. This geographic feature's name was originally published as &quot;Jumbo Mountain&quot; by U.S. Geological Survey in 1904, likely from the Jumbo Mine at its base. &quot;Mount Jumbo&quot; is another variant name still in common use.

Geographic entities mentioned:
surface_form: jumbo mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.195654
lon: -121.59959
surface_form: jumbo mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.395833333333
lon: -113.165
Mount Bradley (Mount Jumbo). Mount Bradley is a elevation mountain summit located on Douglas Island in the Alexander Archipelago, in the U.S. state of Alaska. It is the third-highest peak on the island, and is situated south of Juneau, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount jumbo
instance_of: Mountain
countries: United States
coordinates: lat: 46.8792
lon: -113.956
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley (mount jumbo)
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Mount Bradley (Mount Jumbo). Mount Bradley is a elevation mountain summit located on Douglas Island in the Alexander Archipelago, in the U.S. state of Alaska. It is the third-highest peak on the island, and is situated south of Juneau, on land managed by Tongass National Forest.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
&quot;Mount Jumbo&quot; is another variant name still in common use. It was officially renamed Mount Bradley in 1939 in honor of Frederick Worthen Bradley (1863–1933), world-famous mining engineer. He was president of the American Mining Institute, and in 1931 was awarded the Saunder Gold Medal for outstanding achievement in mining.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Board on Geographic Names. Climate. Based on the Köppen climate classification, Mount Bradley has a subarctic climate with cold, snowy winters, and mild summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Coast Mountains (orographic lift), causing heavy precipitation in the form of rainfall and snowfall.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Juneau Icefield to the mountain's northeast. The month of July offers the most favorable weather for viewing and climbing Mount Bradley.

Geographic entities mentioned:
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 62.92472222222222
lon: -150.7263888888889
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 48.1687464
lon: -113.4593874
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 41.22184755
lon: -122.3089186
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 36.7285453
lon: -118.3384294
surface_form: mount bradley
instance_of: Mountain
countries: United States
coordinates: lat: 58.2478
lon: -134.4142
Pelion, South Carolina. Pelion is a town in Lexington County, South Carolina, United States. The population was 674 at the 2010 census. It is part of the Columbia, South Carolina Metropolitan Statistical Area. History. A post office called Pelion has been in operation since 1900. The town was named after Mt Pelion in Greece. Geography. Pelion is located at (33.765562, -81.246472).

Geographic entities mentioned:
surface_form: Pelion
instance_of: Mountain
countries: Greece
coordinates: lat: 39.433333333333
lon: 23.05
When he lost one of these skirmishes he left northern Thessaly and returned to Macedon. As winter was approaching he sent his troops to winter camps. After Perseus left, Publius Licinius tried to take a town in the Vale of Tempe, a gorge between Thessaly and Macedon which was the passage between the two states. However, he gave up because it was well fortified.

Geographic entities mentioned:
surface_form: Vale of Tempe
instance_of: Valley
countries: Greece
coordinates: lat: 39.872778
lon: 22.546667
Vale do Anhangabaú. Vale do Anhangabaú (Anhangabaú Valley) is a region in the city center of São Paulo, located between the viaducts do Chá and Santa Ifigênia. It is a public space commonly characterized as park, where events have traditionally been organized, such as public demonstrations, political rallies, presentations and popular shows.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Vale do Anhangabaú. Vale do Anhangabaú (Anhangabaú Valley) is a region in the city center of São Paulo, located between the viaducts do Chá and Santa Ifigênia. It is a public space commonly characterized as park, where events have traditionally been organized, such as public demonstrations, political rallies, presentations and popular shows.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
It is considered the point that separates the Old City Center from the New City Center. Currently, the 43 thousand square meters of the Anhangabaú Valley are used as a crossing point for people wishing to transit between the east and west regions of the center, and can be defined as an extensive boardwalk under a road junction.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
With gardens, works of art and three fountains, Vale do Anhangabaú is today a postcard of the City Center of São Paulo, from where it is possible to glimpse buildings such as the Martinelli, Altino Arantes, Teatro Municipal, and the Matarazzo Building, headquarters of city hall.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
In addition to being in a region that houses all the places mentioned above, the Vale do Anhangabaú is also located near the Dramatic and Musical Conservatory of São Paulo, which is called the School of Dance of São Paulo, also known as the School of Dance of the Municipal Theater of São Paulo (EDTMSP). Basically, it is a university campus that concentrates classes on public dance in the city.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Origins and first occupations. The Anhangabaú River, which gave origin to the Valley, is born as Saracura Stream, which runs through Avenida 9 de Julho and goes through the Anhangabaú Valley, reaching its mouth at Tamanduateí River, at the47 edge of Municipal Market. Thus, the Tamanduateí constitutes a kind of delta with its main tributary, Anhangabaú.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Origins and first occupations. The Anhangabaú River, which gave origin to the Valley, is born as Saracura Stream, which runs through Avenida 9 de Julho and goes through the Anhangabaú Valley, reaching its mouth at Tamanduateí River, at the47 edge of Municipal Market. Thus, the Tamanduateí constitutes a kind of delta with its main tributary, Anhangabaú.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Thus, the Tamanduateí constitutes a kind of delta with its main tributary, Anhangabaú. The name Anhangabaú possibly derives from the fact that its waters are very ferreous and acidic - in Tupi, it means &quot;poisonous water&quot;.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Because of its size, the Valley was the scene of historical facts of great national importance, such as the inauguration of the Viaduto do Chá in 1892, the channeling of Anhangabaú River in 1906, and the replacement of the park's gardens by avenues, in 1940, following the architectural changes of the city. Landscaping and reurbanisation.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
He proposed to create a circular boulevard around the central area, so that it would comprise a gigantic avenue full of trees, from Brás to Ipiranga, in the clean and drained floodplain of the Tamanduateí River, which, in turn, would connect to other avenues and even the Anhangabaú Stream — which was being rectified at the time.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Even with so many suggestions for urban improvement, despite their proposals, the complexity of elaborating the works was greater than what monarchic governments could act at that moment, so they were not carried out. In 1910, a great afforestation of the Anhangabaú Valley was carried out, resulting in the formation of the Anhangabaú Park.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
This project took shape from a combination of three projects, including &quot;Grandes Avenidas&quot;, by the architect Alexandre Albuquerque, which resulted in the urbanization of the valley with the insertion of buildings. Between 1920 and 1930, Vale do Anhangabaú served as an important center for socialization and encounters between homosexuals.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
The intersection between Anhangabaú Avenue and Avenida São João gained a different height in 1951, with the construction of Buraco do Ademar, which remained there for 37 years, being subsequently replaced by two homonymous tunnels (Papa João Paulo II).

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
The main focus was to transform the Valley into a large boulevard, to resume the original function of its construction at the beginning of the 20th century. Since 2019, Vale do Anhangabaú has undergone a renovation, which was completed in 2022. Political manifestations.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Since 2019, Vale do Anhangabaú has undergone a renovation, which was completed in 2022. Political manifestations. In addition to its importance for the city's architectural history, the Anhangabaú Valley played a very influential role in the social history of São Paulo residents. A milestone in the history of the Valley was the event that became known as &quot;Diretas Já&quot;.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
The demonstration of April 16, 1984, however, is worth mentioning, as more than a million people gathered in Vale do Anhangabaú to continue the &quot;Diretas Já!&quot; demonstrations.

Geographic entities mentioned:
surface_form: anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
surface_form: vale do anhangabaú
instance_of: Valley
countries: Brazil
coordinates: lat: -23.545975
lon: -46.63703611
Second marriage. Biden met teacher Jill Tracy Jacobs in 1975 on a blind date. They married at the United Nations chapel in New York on June 17, 1977, and spent their honeymoon at Lake Balaton in the Hungarian People's Republic. Biden credits her with the renewal of his interest in politics and life.

Geographic entities mentioned:
surface_form: Lake Balaton
instance_of: Lake
countries: Hungary
coordinates: lat: 46.85
lon: 17.72
History. In 1841, Richard Barton purchased of land in the upper Hutt Valley. He modeled his development of his estate on that of Trentham in England, where he had been a supervisor of the estate. This meant part of the land was cleared for farming and settlement while some of it was left as natural bush land.

Geographic entities mentioned:
surface_form: Hutt Valley
instance_of: Valley
countries: New Zealand
coordinates: lat: -41.1657
lon: 174.973
Stadt Wehlen station. Stadt Wehlen is a station on the Dresden to Děčín line that serves the town of Stadt Wehlen in the German state of Saxony. The station is located on the south bank of the Elbe and is connected to the town, which lies on the north bank, by the Stadt Wehlen passenger ferry. The station is served by the Dresden S-Bahn S1 service.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
1986 Kashmir riots. The 1986 Kashmir Riots, also commonly referred to as the 1986 Anantnag Riots, were a series of attacks targeting Kashmiri Hindus in the Kashmir Valley of Jammu and Kashmir, India, particularly in Anantnag district. Background.

Geographic entities mentioned:
surface_form: Kashmir Valley
instance_of: Valley
countries: India
coordinates: lat: 34.0333
lon: 74.6667
Ilave River. lgkp90vkl3qaxoyotiw3o03j2ocjp" xml:space="preserve">Ilave River or Río Ilave is a stream in Peru, located in the Puno Region, on the Titicaca slope. It flows into Lake Titicaca. It has an elevation of 3,815 metres. Iiave River has a hydrographic basin that covers 7705 km2. It has a length of 163 km. Río Ilave is situated nearby the localities Jullani and Huayllata.

Geographic entities mentioned:
surface_form: Lake Titicaca
instance_of: Lake
countries: Peru
Bolivia
coordinates: lat: -15.825
lon: -69.325