Sarmila/GeoWiki-Features huggingface dataset:
This same day, the state of emergency for the entire state was extended to June 13. On May 15, five regions, Finger Lakes, Mohawk Valley, Southern Tier, North Country, and Central New York, were allowed to begin Phase 1 of the reopening plan.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
On May 19, Cuomo allowed Western New York to begin Phase 1 of reopening. On May 20, Cuomo allowed the Capital Region to begin Phase 1 of reopening. On May 23, Cuomo modified an executive order to allow gatherings of up to 10 people as long as social distancing is practiced. On May 26, the Hudson Valley region began Phase 1 of reopening, followed by Long Island on May 27. June.

Geographic entities mentioned:
surface_form: Hudson Valley
instance_of: Valley
countries: United States
coordinates: lat: 41.9209
lon: -73.9613
Sülzetal. Sülzetal is a municipality in the Börde district in Saxony-Anhalt, Germany. It is situated on the creek Sülze, a tributary of the Elbe, about southwest of Magdeburg. Sülzetal was established on 1 April 2001 by the merger of the former municipalities &quot;Altenweddingen, Bahrendorf, Dodendorf, Langenweddingen, Osterweddingen, Schwaneberg, Stemmern&quot; and &quot;Sülldorf&quot;.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
The usual form of the legend is that Shem and Melchizedek retrieved the body of Adam from the resting place of Noah's ark on Mount Ararat and were led by angels to Golgotha, a skull-shaped hill at the center of the earth where Adam had previously crushed the serpent's head following the Fall of Man.

Geographic entities mentioned:
surface_form: Mount Ararat
instance_of: Mountain
countries: Turkey
coordinates: lat: 39.70194444444444
lon: 44.29833333333333
The Northern Forum is located north of the Temple Mount, on the junction of the Via Dolorosa and the Eastern Cardo (the Tyropoeon), adjacent to the Temple of Jupiter Capitolinus, intentionally built atop the Temple Mount.

Geographic entities mentioned:
surface_form: Tyropoeon
instance_of: Valley
countries: State of Palestine
Israel
coordinates: lat: 31.776947222222
lon: 35.234238888889
Superior (proposed U.S. state). The State of Superior (or State of Ontonagon) is a proposed &quot;51st state&quot; that would be created by the secession of the Upper Peninsula from the rest of Michigan, named for adjacent Lake Superior. Some proposals would also incorporate territory from the northern Lower Peninsula, northern Wisconsin, and even Minnesota.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
It is not to be confused with another Crag Hill lying on the border of North Yorkshire. It overlooks the valleys of Rannerdale on the west, and Coledale on the east. It is the second highest fell in the area of high ground between the passes of Whinlatter and Newlands, second to Grasmoor. It is high, and has a relative height of. Topography.

Geographic entities mentioned:
surface_form: Grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The central sector, rising between Whinlatter and Newlands passes, includes Crag Hill. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range.

Geographic entities mentioned:
surface_form: Crummock Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: Scar Crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: Causey Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
In plan it appears as a cross with ridges running to the four points of the compass. To the north of Crag Hill is the col of Coledale Hause, the high level connection to Hopegill Head, focal point of a parallel but slightly lower ridge. Valleys descend from either side of Coledale Hause, running between these two ridges.

Geographic entities mentioned:
surface_form: Hopegill Head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Guarding the way up from the Hause to Crag Hill is Eel Crag, the face which gave the fell its former name. Crag Hill also has a southern ridge which steps down toward Buttermere over Wandope and Whiteless Pike. The valley of Rannerdale forms the western boundary with Sail Beck on the other side. Both empty into Crummock Water.

Geographic entities mentioned:
surface_form: Buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: Wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: Whiteless Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
Geology. The summit areas of Crag Hill are composed of the Ordovician Kirkstile Formation. This is the typical rock of the Skiddaw fells and is composed of laminated mudstone and siltstone. Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation. The Causey Pike Fault runs across the southern flanks of the fell, beyond which are the rocks of the Buttermere Formation.

Geographic entities mentioned:
surface_form: Skiddaw
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.651388888889
lon: -3.1477777777778
All of the major fell groups can be seen with the Scafells particularly fine. Although a higher neighbour, Grasmoor detracts little from the view to the west. Ascents. From the shore of Crummock Water, Rannerdale Beck can be followed to its source, gaining the ridge between Crag Hill and Wandope. The alternative western route follows Gasgale Gill up to its birthplace on Coledale Hause.

Geographic entities mentioned:
surface_form: wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
Many ascents of Crag Hill are made indirectly as part of a full traverse of the Grasmoor to Causey Pike ridge. Climbs from Buttermere via Whiteless Pike and Wandope are also practicable. Finally, rounds of either Coledale or Gasgale Gill, crossing to or from Hopegill Head via Coledale Hause, provide fine horseshoe walks for those needing to return to their starting point. Protection.

Geographic entities mentioned:
surface_form: wandope
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.565980555556
lon: -3.2573611111111
surface_form: whiteless pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.558669444444
lon: -3.2695111111111
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Crag Hill also has a southern ridge which steps down toward Buttermere over Wandope and Whiteless Pike. The valley of Rannerdale forms the western boundary with Sail Beck on the other side. Both empty into Crummock Water. The highest part of Crag Hill is near the 'cross' where the four ridges meet. Moving further east towards Sail, the ridge tapers down with crags on either side.

Geographic entities mentioned:
surface_form: crummock water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.55
lon: -3.3
Geology. The summit areas of Crag Hill are composed of the Ordovician Kirkstile Formation. This is the typical rock of the Skiddaw fells and is composed of laminated mudstone and siltstone. Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation. The Causey Pike Fault runs across the southern flanks of the fell, beyond which are the rocks of the Buttermere Formation.

Geographic entities mentioned:
surface_form: loweswater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.5825
lon: -3.355277777777778
Crag Hill. Crag Hill is a mountain in the North Western part of the English Lake District. It was formerly known as Eel Crag; however, the Ordnance Survey now marks Eel Crag as referring to the northern crags of the fell. It is not to be confused with another Crag Hill lying on the border of North Yorkshire. It overlooks the valleys of Rannerdale on the west, and Coledale on the east.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
Two roads cross from east to west, dividing the fells into three convenient groups. The central sector, rising between Whinlatter and Newlands passes, includes Crag Hill. The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: whinlatter
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.614
lon: -3.252
The highest ground in the North Western Fells is an east–west ridge in this central sector, beginning with Grasmoor above Crummock Water and then gradually descending eastwards over Crag Hill, Sail, Scar Crags and Causey Pike. Grasmoor has the greatest elevation, but Crag Hill stands at the hub of the range. In plan it appears as a cross with ridges running to the four points of the compass.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Gasgale Gill (or Liza Beck on OS maps) flows westward to the River Cocker, while Coledale Beck runs eastwards to the Derwent. Guarding the way up from the Hause to Crag Hill is Eel Crag, the face which gave the fell its former name. Crag Hill also has a southern ridge which steps down toward Buttermere over Wandope and Whiteless Pike.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
The valley of Rannerdale forms the western boundary with Sail Beck on the other side. Both empty into Crummock Water. The highest part of Crag Hill is near the 'cross' where the four ridges meet. Moving further east towards Sail, the ridge tapers down with crags on either side. Scott Crags stands over Coledale and Scar Crag (not to be confused with Scar Crags) looks down on Sail Beck.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
By contrast to the west of the summit the slopes are smooth and wide, although still steep. Geology. The summit areas of Crag Hill are composed of the Ordovician Kirkstile Formation. This is the typical rock of the Skiddaw fells and is composed of laminated mudstone and siltstone. Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation. The Causey Pike Fault runs across the southern flanks of the fell, beyond which are the rocks of the Buttermere Formation. Although there is much evidence of mining activity in the surrounding fells, Crag Hill itself has remained untouched. Summit.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
From here a simple ascent turns Eel Crag to the west, although Wainwright listed more interesting alternatives on the eastern side of the crag. Many ascents of Crag Hill are made indirectly as part of a full traverse of the Grasmoor to Causey Pike ridge. Climbs from Buttermere via Whiteless Pike and Wandope are also practicable.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Finally, rounds of either Coledale or Gasgale Gill, crossing to or from Hopegill Head via Coledale Hause, provide fine horseshoe walks for those needing to return to their starting point. Protection. Crag Hill is within Buttermere Fells Site of Special Scientific Interest. The land surface of Crag Hill mountain is owned by the National Trust.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
Finally, rounds of either Coledale or Gasgale Gill, crossing to or from Hopegill Head via Coledale Hause, provide fine horseshoe walks for those needing to return to their starting point. Protection. Crag Hill is within Buttermere Fells Site of Special Scientific Interest. The land surface of Crag Hill mountain is owned by the National Trust.

Geographic entities mentioned:
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.2445
lon: -2.47413
surface_form: crag hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.572
lon: -3.25
Guarding the way up from the Hause to Crag Hill is Eel Crag, the face which gave the fell its former name. Crag Hill also has a southern ridge which steps down toward Buttermere over Wandope and Whiteless Pike. The valley of Rannerdale forms the western boundary with Sail Beck on the other side. Both empty into Crummock Water.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
Both empty into Crummock Water. The highest part of Crag Hill is near the 'cross' where the four ridges meet. Moving further east towards Sail, the ridge tapers down with crags on either side. Scott Crags stands over Coledale and Scar Crag (not to be confused with Scar Crags) looks down on Sail Beck. Beneath Scar Crag is Addacomb Hole, a deep corrie without a tarn.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
Both empty into Crummock Water. The highest part of Crag Hill is near the 'cross' where the four ridges meet. Moving further east towards Sail, the ridge tapers down with crags on either side. Scott Crags stands over Coledale and Scar Crag (not to be confused with Scar Crags) looks down on Sail Beck. Beneath Scar Crag is Addacomb Hole, a deep corrie without a tarn.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: scar crags
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.574388888889
lon: -3.2266805555556
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Beneath this are the Greywacke sandstone turbidites of the Loweswater Formation. The Causey Pike Fault runs across the southern flanks of the fell, beyond which are the rocks of the Buttermere Formation. Although there is much evidence of mining activity in the surrounding fells, Crag Hill itself has remained untouched. Summit.

Geographic entities mentioned:
surface_form: buttermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.533333333333
lon: -3.2666666666667
surface_form: causey pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.576338888889
lon: -3.2112694444444
The view is excellent, although robbed of some foreground by the flat expanse of the top. All of the major fell groups can be seen with the Scafells particularly fine. Although a higher neighbour, Grasmoor detracts little from the view to the west. Ascents. From the shore of Crummock Water, Rannerdale Beck can be followed to its source, gaining the ridge between Crag Hill and Wandope.

Geographic entities mentioned:
surface_form: grasmoor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.57115
lon: -3.2791805555556
Many ascents of Crag Hill are made indirectly as part of a full traverse of the Grasmoor to Causey Pike ridge. Climbs from Buttermere via Whiteless Pike and Wandope are also practicable. Finally, rounds of either Coledale or Gasgale Gill, crossing to or from Hopegill Head via Coledale Hause, provide fine horseshoe walks for those needing to return to their starting point. Protection.

Geographic entities mentioned:
surface_form: hopegill head
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.5875
lon: -3.2626694444444
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
It is not to be confused with another Crag Hill lying on the border of North Yorkshire. It overlooks the valleys of Rannerdale on the west, and Coledale on the east. It is the second highest fell in the area of high ground between the passes of Whinlatter and Newlands, second to Grasmoor. It is high, and has a relative height of. Topography.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
To the north of Crag Hill is the col of Coledale Hause, the high level connection to Hopegill Head, focal point of a parallel but slightly lower ridge. Valleys descend from either side of Coledale Hause, running between these two ridges. Gasgale Gill (or Liza Beck on OS maps) flows westward to the River Cocker, while Coledale Beck runs eastwards to the Derwent.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Valleys descend from either side of Coledale Hause, running between these two ridges. Gasgale Gill (or Liza Beck on OS maps) flows westward to the River Cocker, while Coledale Beck runs eastwards to the Derwent. Guarding the way up from the Hause to Crag Hill is Eel Crag, the face which gave the fell its former name.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
Ascents. From the shore of Crummock Water, Rannerdale Beck can be followed to its source, gaining the ridge between Crag Hill and Wandope. The alternative western route follows Gasgale Gill up to its birthplace on Coledale Hause. From Braithwaite near Keswick at the opposite end of the ridge, Coledale Hause is also the first objective.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
The alternative western route follows Gasgale Gill up to its birthplace on Coledale Hause. From Braithwaite near Keswick at the opposite end of the ridge, Coledale Hause is also the first objective. From here a simple ascent turns Eel Crag to the west, although Wainwright listed more interesting alternatives on the eastern side of the crag.

Geographic entities mentioned:
surface_form: coledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.65
lon: -3.23333
During the day, the elevated trough and surface low crossed the Mississippi Valley, reaching South-central Indiana before midnight on January 27 and deepening to 997 mb. Dew points of, or more, in the warm sector of the surface low brought significant humidity from the Gulf of Mexico while the high pressure moved to the Lake Superior, keeping cold and dry air over the Great Lakes.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The strong pressure gradient between the latter and the low pressure center caused strong winds over Lake Michigan, causing widespread blowing snow while heavy snowfall affected the Chicago area. On January 27, the low occluded. Its central pressure reached 990 mb while passing over Lake Erie and Southern Ontario, Canada.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
On January 27, the low occluded. Its central pressure reached 990 mb while passing over Lake Erie and Southern Ontario, Canada. Snow stopped in the evening in Chicago and strong winds moved north-northwest out of the region. Forecast. The weather forecast on January 25 for the 26th was for rain or snow because the cold front was forecast to stall in the Chicago area.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The tradition of Gassire's lute mentions Wagadu's fall. The traditions of the Moors, Hassaniya Arabs and Berbers in Mauritania maintain that the earliest occupants of areas such as the Adrar and Tagant were Black. These regions, part of the core of Wagadu, remained largely Soninke until at least the 16th century. Medieval Arab writers and a Berber origin.

Geographic entities mentioned:
surface_form: Adrar
instance_of: Plateau
countries: Mauritania
coordinates: lat: 20.405277777778
lon: -13.111111111111
Niger Bend theory. Historian Dierk Lange has argued that the core of Wagadou was not Koumbi Saleh but in fact lay near Lake Faguibine, on the Niger Bend. This area was historically more fertile than the Tichitt zone, and Lange draws on oral traditions to support his argument, contending that dynastic struggles in the 11th century pushed the capital west. Rise of the Empire.

Geographic entities mentioned:
surface_form: Lake Faguibine
instance_of: Lake
countries: Mali
coordinates: lat: 16.75
lon: -4
Fusch an der Großglocknerstraße. Fusch an der Großglocknerstraße is a municipality, at the foot of Grossglockner mountain, in the district of Zell am See (Pinzgau region), in the state of Salzburg in Austria. The Fusch valley lies north of the main chain of the Alps. The population (as of December 2008) is 697.

Geographic entities mentioned:
surface_form: Grossglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Bergsmoen. Bergsmoen is a village in Grong Municipality in Trøndelag county, Norway. The village is located about west of Medjå, the municipal center of Grong. The village lies close to the river Namsen in the Namdalen valley and less than southeast from Eidsvatnet. It has a single bus stop in the village center. The village had a population (2023) of 213 and a population density of.

Geographic entities mentioned:
surface_form: Eidsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 64.5348
lon: 12.1143
With a land area of, it had a population density of in 2016. Attractions. The municipality of Lac Ste. Anne maintains the Lessard Lake Campground, the Lessard Lake Outdoor Ed Centre, the Riverside Campground, and the Paddle River Dam Campground. Many summer villages are established, especially on lake shores (such as Lac Ste. Anne, Lac la Nonne, Nakamun Lake, and Lake Isle).

Geographic entities mentioned:
surface_form: Lac la Nonne
instance_of: Lake
countries: Canada
coordinates: lat: 53.9372
lon: -114.32
History. Archaeological surveying in the area of the Snow Lakes shows evidence that the occupation of indigenous groups dated to at least 12,000 years before the present era. Klonaqua Lake is within the traditional territory of the Wenatchi People, one of the Confederated Tribes of the Colville Reservation and within the ceded lands of the Yakama Nation.

Geographic entities mentioned:
surface_form: Snow Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
The lake captures water runoff at the far southeast of a 3,800-acre drainage basin which gives the lake a high potential for refill, even during dry years. Between Eightmile Lake, Colchuck Lake and Klonaqua Lake, the total average usable storage volume is 6,600 acre-feet. Additional usage storage volume of approximately 12,730 acre-feet is available from Snow Lakes.

Geographic entities mentioned:
surface_form: Eightmile Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.520277777778
lon: -120.86527777778
The lake captures water runoff at the far southeast of a 3,800-acre drainage basin which gives the lake a high potential for refill, even during dry years. Between Eightmile Lake, Colchuck Lake and Klonaqua Lake, the total average usable storage volume is 6,600 acre-feet. Additional usage storage volume of approximately 12,730 acre-feet is available from Snow Lakes.

Geographic entities mentioned:
surface_form: Snow Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
surface_form: snow lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.483116
lon: -120.7586572
2017 fire. On August 11, 2017 lightning caused by a cold frontal passage that tracked through the Alpine Lakes Wilderness started a fire about 15 miles southwest of Leavenworth, Washington. The fire expanded into the Eightmile Lake, Stuart Lake and Klonaqua drainages burning to the shoreline and damaging a large percentage of the lake's watershed.

Geographic entities mentioned:
surface_form: Eightmile Lake
instance_of: Lake
countries: United States
coordinates: lat: 47.520277777778
lon: -120.86527777778
surface_form: Stuart Lake
instance_of: Lake
countries: Canada
coordinates: lat: 54.55
lon: -124.58333333333
Klonaqua Lakes. Klonaqua Lakes are a set of freshwater reservoir lakes located on the western slope of The Enchantments, in Chelan County, Washington. A self-issued Alpine Lake Wilderness permit is required for transit within the Klonaqua Lakes area. Name.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: chelan
instance_of: Lake
countries: United States
coordinates: lat: 47.841111111111
lon: -120.04638888889
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
2017 fire. On August 11, 2017 lightning caused by a cold frontal passage that tracked through the Alpine Lakes Wilderness started a fire about 15 miles southwest of Leavenworth, Washington. The fire expanded into the Eightmile Lake, Stuart Lake and Klonaqua drainages burning to the shoreline and damaging a large percentage of the lake's watershed.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
Klonaqua Lakes. Klonaqua Lakes are a set of freshwater reservoir lakes located on the western slope of The Enchantments, in Chelan County, Washington. A self-issued Alpine Lake Wilderness permit is required for transit within the Klonaqua Lakes area. Name.

Geographic entities mentioned:
surface_form: alpine lake
instance_of: Lake
countries: United States
coordinates: lat: 37.9622
lon: -119.304
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
surface_form: lake wilderness
instance_of: Lake
countries: United States
coordinates: lat: 47.3746
lon: -122.036
Klonaqua Lakes. Klonaqua Lakes are a set of freshwater reservoir lakes located on the western slope of The Enchantments, in Chelan County, Washington. A self-issued Alpine Lake Wilderness permit is required for transit within the Klonaqua Lakes area. Name.

Geographic entities mentioned:
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
Name. Along with neighboring lakes, Klonaqua Lakes was given its name by Albert Hale Sylvester, a topographer for the United States Geological Survey working throughout the North Cascades National Park Complex in the 1900s. Sylvester compounded the word from the Chinook Jargon &quot;klone&quot; with the Wenatchi language word &quot;aqua&quot; to mean &quot;three waters&quot;. History.

Geographic entities mentioned:
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
Klonaqua Lake is within the traditional territory of the Wenatchi People, one of the Confederated Tribes of the Colville Reservation and within the ceded lands of the Yakama Nation. Icicle Irrigation District applied in 1926 for the right to divert water from Klonaqua Lakes at approximately 25 cfs (cubic feet per second) for seasonal irrigation purposes.

Geographic entities mentioned:
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
Access. Access to Klonaqua Lakes is through Klonaqua trail which spins off French Creek Trail. The trail ascends steeply and splits at Bobs Lake () in order to access both main lakes. Camping sites are dotted along Klonaqua Lakes. Bobs Lakes is also lined with campsites as overflow and is stocked with trout. 2017 fire.

Geographic entities mentioned:
surface_form: klonaqua lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 47.594444444444
lon: -121.06972222222
Geography. Klonaqua Lake sits in a basin consisting of rocky soils and igneous tonalite geology. The bedrock is about 3 feet from the surface and mapped as granites of the Mount Stuart Batholith (Mesozoic intrusive rocks) and ultramafic/metamorphic of the Ingalls Tectonic Complex (Mesozoic-Paleozoic ultramafic rocks).

Geographic entities mentioned:
surface_form: mount stuart
instance_of: Mountain
countries: United States
coordinates: lat: 47.4753
lon: -120.901
On the morning of 7 December 1941, the soldiers of the 16th Coast Artillery manned their anti-aircraft guns, bringing down six of the attacking Japanese aircraft. Fort Ruger. Fort Ruger was located in and around Diamond Head. The interior of the volcanic cone was accessible through two tunnels large enough for trucks. The administrative buildings were on the north side of the cone.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
The crossed spears are taken from Hawaiian history, they were formerly placed at the King's tent, and are shown conventionally in the Hawaiian arms by a saltire cross placed on an inescutcheon. The motto, probably the best known Hawaiian word, is used extensively as a sign against trespassers. The batteries at Diamond Head constitute the principal element of these defenses. Background.

Geographic entities mentioned:
surface_form: Diamond Head
instance_of: Mountain
countries: United States
coordinates: lat: 21.259722222222
lon: -157.81175
Alberni Valley. Alberni Valley is a broad valley located at the head of Alberni Inlet on Vancouver Island in British Columbia, Canada. It is home to Port Alberni, Sproat Lake and other outlining areas. The term is largely used as a synonym for Greater Port Alberni and adjoining communities but is used in a larger regional sense as well.

Geographic entities mentioned:
surface_form: Sproat Lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.2667
lon: -125.033
Alberni Valley. Alberni Valley is a broad valley located at the head of Alberni Inlet on Vancouver Island in British Columbia, Canada. It is home to Port Alberni, Sproat Lake and other outlining areas. The term is largely used as a synonym for Greater Port Alberni and adjoining communities but is used in a larger regional sense as well.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Alberni Valley. Alberni Valley is a broad valley located at the head of Alberni Inlet on Vancouver Island in British Columbia, Canada. It is home to Port Alberni, Sproat Lake and other outlining areas. The term is largely used as a synonym for Greater Port Alberni and adjoining communities but is used in a larger regional sense as well.

Geographic entities mentioned:
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
It is home to Port Alberni, Sproat Lake and other outlining areas. The term is largely used as a synonym for Greater Port Alberni and adjoining communities but is used in a larger regional sense as well. Various local organizations and companies use the term &quot;Alberni Valley&quot; in their name, e.g.

Geographic entities mentioned:
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
Various local organizations and companies use the term &quot;Alberni Valley&quot; in their name, e.g. the &quot;Alberni Valley Times&quot; and &quot;Alberni Valley News&quot; newspapers the Alberni Valley Chamber of Commerce and the Alberni Valley Bulldogs minor hockey team. The Canadian pioneer, Joe Drinkwater lived in Alberni Valley during the late nineteenth and early twentieth centuries.

Geographic entities mentioned:
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
the &quot;Alberni Valley Times&quot; and &quot;Alberni Valley News&quot; newspapers the Alberni Valley Chamber of Commerce and the Alberni Valley Bulldogs minor hockey team. The Canadian pioneer, Joe Drinkwater lived in Alberni Valley during the late nineteenth and early twentieth centuries. First Nations. First Nations cultures are an essential part of the Alberni Valley's makeup.

Geographic entities mentioned:
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
The Canadian pioneer, Joe Drinkwater lived in Alberni Valley during the late nineteenth and early twentieth centuries. First Nations. First Nations cultures are an essential part of the Alberni Valley's makeup. The Tseshaht and the Hupacasath are two of the tribes that make up the Nuu-chah-nulth Tribal Council.

Geographic entities mentioned:
surface_form: alberni valley
instance_of: Valley
countries: Canada
coordinates: lat: 49.25
lon: -124.8
Ylä-Rieveli. Ylä-Rieveli (also called &quot;Ylä-Rääveli&quot;) is a medium-sized lake in Finland. It is a lake in the Kymijoki main catchment area, located in the regions Southern Savonia and Päijänne Tavastia. It is connected with another lake, Enonvesi, by the Pirtinsalmi strait.

Geographic entities mentioned:
surface_form: Enonvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.116666666667
lon: 28.9
surface_form: enonvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.061
lon: 29.003
surface_form: enonvesi
instance_of: Lake
countries: Finland
coordinates: lat: 62.116666666667
lon: 28.9
Ylä-Rieveli. Ylä-Rieveli (also called &quot;Ylä-Rääveli&quot;) is a medium-sized lake in Finland. It is a lake in the Kymijoki main catchment area, located in the regions Southern Savonia and Päijänne Tavastia. It is connected with another lake, Enonvesi, by the Pirtinsalmi strait.

Geographic entities mentioned:
surface_form: ylä-rieveli
instance_of: Lake
countries: Finland
coordinates: lat: 61.41666667
lon: 26.48333333
Mount Maslen. Mount Maslen is a mountain, high, standing west of Mount Currie in the Raggatt Mountains of Enderby Land, Antarctica. It was plotted from air photos taken from Australian National Antarctic Research Expeditions aircraft in 1956 and was named by the Antarctic Names Committee of Australia for A.W.G. Maslen, the officer-in-charge at Mawson Station in 1961.

Geographic entities mentioned:
surface_form: mount maslen
instance_of: Mountain
coordinates: lat: -67.7
lon: 49.1167
surface_form: maslen
instance_of: Mountain
coordinates: lat: -67.7
lon: 49.1167
Mount Maslen. Mount Maslen is a mountain, high, standing west of Mount Currie in the Raggatt Mountains of Enderby Land, Antarctica. It was plotted from air photos taken from Australian National Antarctic Research Expeditions aircraft in 1956 and was named by the Antarctic Names Committee of Australia for A.W.G. Maslen, the officer-in-charge at Mawson Station in 1961.

Geographic entities mentioned:
surface_form: maslen
instance_of: Mountain
coordinates: lat: -67.7
lon: 49.1167
40&quot; plays from speakers near the waiting room. Izukyū Corporation. On the Izu Kyūkō Line, since March 26, 2015, by Sayuri Ishikawa, a song of Mount Amagi nearby, has been used at Kawazu Station. Fuji Kyūkō (Fujikyū). On the Fuji Kyūkō Line, the traditional students' song is used at Ōtsuki, Mt. Fuji, and Kawaguchiko Stations. Izuhakone Railway.

Geographic entities mentioned:
surface_form: Mount Amagi
instance_of: Mountain
countries: Japan
coordinates: lat: 34.862777777778
lon: 139.00166666667
For example, at six stations including Toyama and Takaoka, the arrival melody, which was composed by Joe Hisaishi as a hometown song for Toyama Prefecture, is used. At Toyama Station, the departure melody is &quot;The Four Seasons&quot; by Vivaldi, which was used as background music in the film &quot;Mt. Tsurugidake&quot;, set in the Tateyama mountain range. Manyōsen.

Geographic entities mentioned:
surface_form: Tateyama mountain range
instance_of: Mountain
countries: Japan
coordinates: lat: 36.575833333333
lon: 137.61972222222
The district was established in 2019 from the surrounding districts. Abala Abaya is bordered on the south by Lake Abaya, on the west by the Humbo district, on the north by the Sodo Zuria district, on the east by Hobicha district. The administrative center of this district is Paracho Town. Population. The total population of the district is about 56,812.

Geographic entities mentioned:
surface_form: Lake Abaya
instance_of: Lake
countries: Ethiopia
coordinates: lat: 6.236
lon: 37.832
TTA started construction in 1977 on its first toll bridge, the Mountain Creek Lake Bridge, which opened in 1979. The bridge spans Mountain Creek Lake in the southwestern Dallas County city of Grand Prairie. Construction was started on TTA's only project outside the area, the Jesse Jones Memorial Bridge across the Houston Ship Channel, in 1979, with the bridge opening in 1982.

Geographic entities mentioned:
surface_form: Mountain Creek Lake
instance_of: Lake
countries: United States
coordinates: lat: 32.719269444444
lon: -96.960894444444
Toconce. Toconce is a small Chilean village located on the south rim of the Toconce River Canyon at 3,350 m above sea level. To the north, the landscape is dominated by the volcanoes Cerro Paniri, Cerro del León and Toconce.

Geographic entities mentioned:
surface_form: Cerro del León
instance_of: Mountain
countries: Chile
coordinates: lat: -22.15
lon: -68.116666666667
Durham School Services. Durham School Services is a school bus operator providing contracted student transportation throughout the United States, based in Lisle, Illinois, and currently operating in 32 states. Founded in 1917 with three buses in the San Gabriel Valley, it became a subsidiary of National Express in 1999. In July 2025 it was sold to I Squared Capital.

Geographic entities mentioned:
surface_form: San Gabriel Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.101944444444
lon: -118.10277777778
Grosmont, North Yorkshire. Grosmont (; archaically spelt &quot;Growmond&quot;) is a village and civil parish situated in Eskdale in the North York Moors National Park, within the boundaries of the county of North Yorkshire, England. From 1974 to 2023 it was part of the Borough of Scarborough, it is now administered by the unitary North Yorkshire Council.

Geographic entities mentioned:
surface_form: Eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
Grosmont Priory. Grosmont Priory was a Grandmontine religious house, one of three in England. It was established around 1200 when Joan Fossard and her husband gifted about of land in the Forest of Egton (Eskdale) to the order. A fire destroyed most of the priory in 1360. In 1394 the Abbot of Grandimont gained permission to sell the priory, which was acquired by John Hewitt.

Geographic entities mentioned:
surface_form: Eskdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.478
lon: -0.786
The priory was located on the banks of the Esk. An unrelated chapel on the banks of the Esk about south-west of the priory was dedicated to St Leonard or St Lawrence and possibly connected with the Abbey of Melsa. Tunnel, or Grosmont village. A canal was surveyed in 1793 from Ruswarp near Whitby passing through Grosmont, Beck Hole and Newton Dale to Pickering, but was not pursued.

Geographic entities mentioned:
surface_form: Newton Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.35472222222222
lon: -0.7105555555555555
In 2015, he became the world's first reigning monarch to visit Antarctica, specifically the Norwegian dependency Queen Maud Land. In 2016, King Harald V competed with a team for the sailing World Championships on Lake Ontario, Toronto. The king came second in the classic fleet category.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Ipswich Museum and the promotion of science. Packard took Dr. Taylor to inspect his phosphate mines in southern France, in the area of the Puy de Dôme, in 1876, and Taylor responded with deep interest. Packard resigned his Chairmanship of the Museum Committee (making way for his son) when Taylor's ill health led to his enforced retirement in 1893.

Geographic entities mentioned:
surface_form: Puy de Dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
Bridges Creek. Bridges Creek is a stream in southeast Ozark County in the Ozarks of southern Missouri. It is a tributary of the North Fork River. The stream begins at the junction of North Bridges Creek with South Bridges Creek. The north branch has headwaters in Howell County just west of Caulfield and south of U. S. Route 160 and it flows southwest into Ozark County and past Elijah.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
McCarthy Cook & Co currently own and manage the property. Location. China Basin Landing is located on one city block bounded by 3rd Street, 4th Street, Berry Street, and the China Basin Canal. It is across from AT&T Park and it overlooks McCovey Cove. China Landing is one block from the Caltrain depot. It is about from the University of California San Francisco Mission Bay campus.

Geographic entities mentioned:
surface_form: McCovey Cove
instance_of: Body of water
countries: United States
coordinates: lat: 37.7772
lon: -122.388
Founded in June 1887, the city takes its name from Imperial County, California, a desert climate east. Farmers and land owners from the Imperial Valley came to the area in the late 1880s seeking cooler weather during summer months. In March 1887, over 2,000 laborers descended upon nearby Coronado, California to construct the Hotel del Coronado, the largest resort in the world at the time.

Geographic entities mentioned:
surface_form: Imperial Valley
instance_of: Valley
countries: United States
coordinates: lat: 33.1
lon: -115.5
Mount Chelidona. Mount Chelidona is a mountain in Central Greece in the regional unit of Evritania. It has a maximum elevation of 1'975 meters. It is connected with the Panaitoliko mountain range in the South, the Kaliakouda East and Tymfristos North, while in the West it ends at the artificial lake of Kremasta.

Geographic entities mentioned:
surface_form: Kaliakouda
instance_of: Mountain
countries: Greece
coordinates: lat: 38.79596
lon: 21.75887
surface_form: Tymfristos
instance_of: Mountain
countries: Greece
coordinates: lat: 38.95
lon: 21.816666666667
surface_form: panaitoliko
instance_of: Mountain
countries: Greece
coordinates: lat: 38.69305556
lon: 21.575
Mount Chelidona. Mount Chelidona is a mountain in Central Greece in the regional unit of Evritania. It has a maximum elevation of 1'975 meters. It is connected with the Panaitoliko mountain range in the South, the Kaliakouda East and Tymfristos North, while in the West it ends at the artificial lake of Kremasta.

Geographic entities mentioned:
surface_form: mount chelidona
instance_of: Mountain
countries: Greece
coordinates: lat: 38.866
lon: 21.57