Sarmila/GeoWiki-Features huggingface dataset:
It is also noted as being a tough bicycle ride for cyclists going up the valley. The Pennine Way skirts to the west of the summit of Dodd Fell and traverses the high ground separating Widdale from Sleddale. The walk then enters Sleddale in its lower reaches, going through Gayle and then Hawes.

Geographic entities mentioned:
surface_form: Widdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3
lon: -2.245
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
The spoil heaps from these workings, which consist largely of shale and iron nodules, still scar the upper valley landscape. The dale was also used to produce peat for people in Appersett, Gayle, Hawes and Snaizeholme, who held turbary rights at Ten End peat ground ().

Geographic entities mentioned:
surface_form: Snaizeholme
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.262
lon: -2.269
The dale was also used to produce peat for people in Appersett, Gayle, Hawes and Snaizeholme, who held turbary rights at Ten End peat ground (). Along with the adjacent south to north valleys of Mid-Wensleydale (Snaizeholme, Widdale and Raydale), Sleddale lacks the mineral deposits on the northern side of the main valley (lead, barytes etc).

Geographic entities mentioned:
surface_form: Raydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.286
lon: -2.126
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
Sleddale is &quot;hemmed in by the lofty hills of Dodd Fell, and Drumaldrace (Wether Fell).&quot;
Geology. The underlying rock in the valley is from the Yoredale Series and mainly consists of limestone, shale and sandstone. Just below the Middle Limestone formation lies a narrow coal seam which was exploited in Sleddale (and nearby Cotterdale too).

Geographic entities mentioned:
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
The Pennine Way skirts to the west of the summit of Dodd Fell and traverses the high ground separating Widdale from Sleddale. The walk then enters Sleddale in its lower reaches, going through Gayle and then Hawes. Sleddale is &quot;hemmed in by the lofty hills of Dodd Fell, and Drumaldrace (Wether Fell).&quot;
Geology.

Geographic entities mentioned:
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
The walk then enters Sleddale in its lower reaches, going through Gayle and then Hawes. Sleddale is &quot;hemmed in by the lofty hills of Dodd Fell, and Drumaldrace (Wether Fell).&quot;
Geology. The underlying rock in the valley is from the Yoredale Series and mainly consists of limestone, shale and sandstone.

Geographic entities mentioned:
surface_form: fell
instance_of: Mountain
coordinates: lat: -73.4333
lon: -62.2667
The beck drains the land between Dodd Fell in the west, and Wether Fell in the east. At the lower end of the valley, the beck is shown on OS Mapping as &quot;Gayle Beck&quot;, and before it reaches the hamlet of Gayle at the southern end of the valley, it drops over Aysgill Force. White-clawed crayfish (austropotamobius pallipes) have been observed in Duerley beck in the 1980s and 1990s.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Sleddale. Sleddale is a short, narrow valley to the south of Wensleydale in North Yorkshire, England. The waters draining down the valley feed into the River Ure and form part of the Humber Catchment. The valley has only one settlement, Gayle, although Hawes lies at the mouth of the beck where it runs into the River Ure.

Geographic entities mentioned:
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
The dale is characterised by upland farming and historical mine workings, and is between the slopes of Dodd Fell to the west, and Wether Fell to the east. History. The name Sleddale first appears in documents in 1280 as &quot;Seldalegile&quot;. The name is a combination of the Old English words of &quot;slæd&quot; and &quot;dæl&quot;, meaning &quot;slow-dale&quot;.

Geographic entities mentioned:
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
The name of the beck which flows down the valley (Duerley Beck), has not influenced the name of the dale (or vice versa), which does occur in the Yorkshire Dales, but is uncommon. Occasionally, the name for the water down the valley was referred to as &quot;Sleddale Beck&quot;.

Geographic entities mentioned:
surface_form: sleddale
instance_of: Valley
coordinates: lat: 54.27
lon: -2.21
The thin layer of coal is attributed to small swamps which developed here rather than the extensive bogs that led to deeper and better coalfields elsewhere in Yorkshire and the North of England. Four mines are known to have existed in the upper dale; West Duerley, Storth, Scar Head and Bank Gill Colliery.

Geographic entities mentioned:
surface_form: scar
instance_of: Mountain
coordinates: lat: -63.4167
lon: -57.0167
The collieries in the dale worked a very poor seam of coal, but in the absence of good transportation, they survived largely until the Wensleydale Railway was opened, and better quality coal could be railed into Wensleydale. The spoil heaps from these workings, which consist largely of shale and iron nodules, still scar the upper valley landscape.

Geographic entities mentioned:
surface_form: scar
instance_of: Mountain
coordinates: lat: -63.4167
lon: -57.0167
Four mines are known to have existed in the upper dale; West Duerley, Storth, Scar Head and Bank Gill Colliery. The collieries in the dale worked a very poor seam of coal, but in the absence of good transportation, they survived largely until the Wensleydale Railway was opened, and better quality coal could be railed into Wensleydale.

Geographic entities mentioned:
surface_form: coal
instance_of: Mountain
coordinates: lat: -72.1167
lon: -68.5333
Hazar (name). Hazar is a unisex Turkish given name and it is a Turkic tribe's name who lived around the Caspian Sea between the 7th and 11th centuries.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
Samalayuca Dune Fields. The Samalayuca Dune Fields, more traditionally known as Los Médanos (the dunes), or more recently referenced as Médanos de Samalayuca, are a series of large but separated fields of sand dunes located in the northern part of the Mexican state of Chihuahua. The dune fields are scattered over a wide expanse of desert to the south, southwest and southeast of Ciudad Juárez.

Geographic entities mentioned:
surface_form: médanos de samalayuca
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
surface_form: los médanos
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
The name Samalayuca Dune Fields is of more recent origin. The name &quot;Los Médanos&quot; is more commonly used, particularly in historical accounts. Recently, the dune fields have been increasingly referred to even by non-Spanish speakers as Médanos de Samalayuca. Name origin. The field and the desert gets its name from the town of Samalayuca, Chihuahua.

Geographic entities mentioned:
surface_form: médanos de samalayuca
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
Samalayuca Dune Fields. The Samalayuca Dune Fields, more traditionally known as Los Médanos (the dunes), or more recently referenced as Médanos de Samalayuca, are a series of large but separated fields of sand dunes located in the northern part of the Mexican state of Chihuahua. The dune fields are scattered over a wide expanse of desert to the south, southwest and southeast of Ciudad Juárez.

Geographic entities mentioned:
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
The Samalayuca Desert and its dune fields are part of the much larger Chihuahua Desert region. The best known portion of the Samalayuca Dune Fields lie in and around the village of Samalayuca. These dune fields lay across the much traveled north–south route between Chihuahua City and &quot;The Pass of the North&quot; at the site of the border cities of Ciudad Juárez and El Paso.

Geographic entities mentioned:
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
The high silica content of the sands has also attracted industrial interest. Historical name. The sand dune area has traditionally been referred to as &quot;Los Médanos&quot; or simply, the dunes. The name Samalayuca Dune Fields is of more recent origin. The name &quot;Los Médanos&quot; is more commonly used, particularly in historical accounts.

Geographic entities mentioned:
surface_form: los médanos
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
Location. The most dramatic portion of the Samalayuca dune fields lie east and west of Mexican Federal Highway 45 and the parallel Mexican Railway in an area 30 to 60 miles south of Juárez. This major north-south highway and railroad, between Ciudad Juárez and the city of Chihuahua crosses through this dune area, and low dunes are visible for many kilometers on each side of the highway.

Geographic entities mentioned:
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
The original Mexican community of El Paso del Norte south of the river changed its name to Ciudad Juárez in 1865. However, in the segment of the Chihuahua trail from Chihuahua City and El Paso del Norte, where the trail reached a point some 45 miles south of the Pass of the North, the trail encountered a 15-mile stretch of the Samalayuca dune fields.

Geographic entities mentioned:
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
Tourists hike in the dunes, ride over them in various vehicles, and slide down the dunes on sand boards. Government protection. On June 5 of 2009, the Mexican federal government created a protected area of 63,182 hectares (631.82 km2, or 156,126.12 acres) in Samalayuca dune fields. Movie setting. The Samalayuca Dunes were used to film many of the exterior shots in the 1984 movie &quot;Dune&quot;.

Geographic entities mentioned:
surface_form: samalayuca dune fields
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
Even as late as 1882 travelers were &quot;warned to avoid this point [Los Médanos] of all others while traveling through Chihuahua&quot;, and to take the alternative route around the dunes area, though some 60 miles longer, because &quot;This place is attended by great danger from the attacks of the Apaches, who well know the helpless condition of animals passing and take the opportunity to attack parties.&quot;
While animals and persons found footing and traction to be difficult in the loose sands of the dunes, what was most dreaded was the difficulty of hauling loaded wagons or carts through the sand.

Geographic entities mentioned:
surface_form: los médanos
instance_of: Mountain
countries: Mexico
coordinates: lat: 31.14
lon: -106.9
Production and character. Glengoyne Distillery is situated at Dumgoyne, on the south-western edge of the Scottish Highlands, close to Loch Lomond and to the north of Glasgow. Although distilled in the Highlands, making Glengoyne a Highland single malt, the whisky is matured in the Lowlands.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Glengoyne and Bruichladdich, is one of only two distilleries remaining today that uses Golden Promise barley, which is low in yield but high in quality. The distillery's water supply comes from the Glengoyne Burn which flows from the nearby Dumgoyne hill into the distillery grounds before continuing on to Loch Lomond.

Geographic entities mentioned:
surface_form: Loch Lomond
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.1482
lon: -4.6515
Crater Rings (Idaho). Crater Rings are adjacent, symmetrical volcanic pit craters in the Western Snake River Plain about eight miles northwest of Mountain Home, Idaho. They are one of few examples of volcanic craters in the continental United States. The craters are at the summit of a broad shield volcano. The eastern crater is about 3000 ft across and 350 ft deep.

Geographic entities mentioned:
surface_form: crater rings
instance_of: Mountain
countries: United States
coordinates: lat: 43.1907
lon: -115.86
The volcano is the youngest of the shield volcanoes near Mountain Home and is estimated to be less than two million years old. Crater Rings are a National Natural Landmark designated in 1980. The site is owned by the Bureau of Land Management as part of the Morley Nelson Snake River Birds of Prey National Conservation Area.

Geographic entities mentioned:
surface_form: crater rings
instance_of: Mountain
countries: United States
coordinates: lat: 43.1907
lon: -115.86
Hestebottnuten. Hestebottnuten is a mountain of Ål municipality, Buskerud, in southern Norway.

Geographic entities mentioned:
surface_form: hestebottnuten
instance_of: Mountain
countries: Norway
coordinates: lat: 60.87178
lon: 8.11733
Mythology. One account related that during the reign of King Cranaus, Deucalion, who founded and ruled over Lycoreia in Mt. Parnassus, was said to have fled from his kingdom during the great flood with his sons Hellen and Amphictyon, and seek refuge to Athens.

Geographic entities mentioned:
surface_form: Mt. Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Amfreville is understood to be the ancestral home of the Umfraville family of Anglo-Norman nobles who occupied England under William the Conqueror and his successors, and went on to become British nobility under the titles &quot;the Barons of Prudhoe&quot; and the &quot;Lords of Redesdale&quot;, and later also gained Scottish lands and the title &quot;Earl of Angus&quot;.

Geographic entities mentioned:
surface_form: Redesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 55.229
lon: -2.186
Comanche Point. Comanche Point is the northwestern headland and prominence of the Tejon Hills, notably extending westward into the southern San Joaquin Valley, west of the Tehachapi Mountains. It is approximately south of Arvin, in Kern County, California. Ecology. Comanche Point and the rest of the Tejon Hills are on the Tejon Ranch, in the section managed by the Tejon Ranch Conservancy.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
surface_form: comanche point
instance_of: Mountain
countries: United States
coordinates: lat: 35.1216
lon: -118.825
Comanche Point. Comanche Point is the northwestern headland and prominence of the Tejon Hills, notably extending westward into the southern San Joaquin Valley, west of the Tehachapi Mountains. It is approximately south of Arvin, in Kern County, California. Ecology. Comanche Point and the rest of the Tejon Hills are on the Tejon Ranch, in the section managed by the Tejon Ranch Conservancy.

Geographic entities mentioned:
surface_form: comanche point
instance_of: Mountain
countries: United States
coordinates: lat: 35.1216
lon: -118.825
Ecology. Comanche Point and the rest of the Tejon Hills are on the Tejon Ranch, in the section managed by the Tejon Ranch Conservancy. There are natural alkali springs and marshes on Comanche Point and the alkaline uplifted marine sediment deposits that form it, which support locally and regionally endemic and rare California native plants (flora).

Geographic entities mentioned:
surface_form: comanche point
instance_of: Mountain
countries: United States
coordinates: lat: 35.1216
lon: -118.825
Texqa'kallt. The Texqa'kallt or Xexka'llt (Shuswap: &quot;people of the upper reaches&quot;) are a division of the Shuswap people of British Columbia that are historically cited as living in and around the North Thompson, through to the Robson Valley. Historic accounts record them as being a mixed peoples speaking Cree and Shuswap, and ethnically of Iroquois, Cree and Shuswap origin.

Geographic entities mentioned:
surface_form: Robson Valley
instance_of: Valley
countries: Canada
coordinates: lat: 53.25
lon: -120
was discontinued on June 30, 1977. The last route with a railway post office title was actually a boat run that lasted a year longer. This boat railway post office was the Lake Winnipesaukee RPO operating between The Weirs, New Hampshire, and Bear Island on Lake Winnipesaukee. The final date it operated with a postmark was September 30, 1978. Preservation.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
Belize was important in the commerce of the whole Bay of Honduras. In 1802 Bennett acted as convener for a succession debate in the Kingdom of Mosquitia after the 1801 death of George II Frederic, when at Cabo Gracias a Dios George Frederic Augustus II was declared heir apparent.

Geographic entities mentioned:
surface_form: Cabo Gracias a Dios
instance_of: Landform
countries: Honduras
coordinates: lat: 15.0064851
lon: -83.1301235
The Verapaz grant was on the north side of Lake Izabal (the Golfo Dulce), and the deal involved Thomas Gould, whom Bennett had diverted from his original purpose of making something of the former Poyais grant. On the south side, Bennett received, in the same year 1834, a grant in Chiquimula on the Motagua River.

Geographic entities mentioned:
surface_form: Lake Izabal
instance_of: Lake
countries: Guatemala
coordinates: lat: 15.5
lon: -89.166666666667
The Dirt Track at Genesee. The Dirt Track at Genesee, is a dirt oval raceway located in the Finger Lakes Region of New York State. Overview. In 1960, the Genesee Valley Agricultural Society moved its annual fair from what is now the Batavia Downs to its present location on East Main Street in Batavia, New York.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Long Pond Ridge. Long Pond Ridge is a ridge located in Adirondack Mountains of New York located in the Town of Indian Lake south of Indian Lake.

Geographic entities mentioned:
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 42.2980198
lon: -71.8120781
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.7
lon: -74.3167
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 44.329722222222
lon: -68.363611111111
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.81402
lon: -89.30162
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.5937
lon: -75.1133
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.4793
lon: -71.4684
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9947
lon: -86.2042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 44.114166666667
lon: -93.786666666667
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.640555555556
lon: -74.289444444444
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 42.419444444444
lon: -75.845277777778
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7667
lon: -70.8558
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5083
lon: -95.5028
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.669742
lon: -70.197151
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8
lon: -70.9494
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8583
lon: -70.6042
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: indian lake
instance_of: Lake
countries: United States
coordinates: lat: 45.988888888889
lon: -86.332222222222
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.4058
lon: -73.3841
surface_form: long pond ridge
instance_of: Mountain
countries: United States
coordinates: lat: 43.64
lon: -74.301388888889
Long Pond Ridge. Long Pond Ridge is a ridge located in Adirondack Mountains of New York located in the Town of Indian Lake south of Indian Lake.

Geographic entities mentioned:
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 44.329722222222
lon: -68.363611111111
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.5937
lon: -75.1133
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.640555555556
lon: -74.289444444444
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 42.419444444444
lon: -75.845277777778
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.7667
lon: -70.8558
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.669742
lon: -70.197151
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8
lon: -70.9494
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 41.8583
lon: -70.6042
surface_form: long pond
instance_of: Lake
countries: United States
coordinates: lat: 43.4058
lon: -73.3841
surface_form: long pond ridge
instance_of: Mountain
countries: United States
coordinates: lat: 43.64
lon: -74.301388888889
However, the schedules of the two systems are not aligned in any way. History. The Vermont Central Railroad was chartered to build a line along the Connecticut River to Lake Champlain, which was to include service to Randolph. The original station was not built until 1848, by which time the VCRR was acquired by the Central Vermont Railway.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Lawrence River to the north. History of tourism. In 1634, Samuel de Champlain sent Sieur de Laviolette to establish a new fort that was also used as a fur trading post. The term &quot;Mauricie&quot; is used for the first time in 1933 by Bishop Albert Tessier to denote the region since Trois-Rivières to the gates of Lac Saint-Jean. Before that date, it was simply called the Valley of Saint-Maurice.

Geographic entities mentioned:
surface_form: Lac Saint-Jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
He served under Asaf Jah III. In 1800, as part of his ongoing rivalry with his predecessor Arastu Jah, the latter enticed Mir Alam to discredit James A. Kirkpatrick and demanded his execution. The Mir Alam tank in Hyderabad is named after him. Mir Alam headed the Hyderabad army in support of British East India company during the siege of Srirangapatnam against Tipu Sultan.

Geographic entities mentioned:
surface_form: Mir Alam tank
instance_of: Lake
countries: India
coordinates: lat: 17.35
lon: 78.433333333333
Takasu Snow Park. The is a ski area on Mount Dainichi in Gifu Prefecture, Japan. The resort opened in 1999, developed by Tōwa Kankō. J Mountains Group acquired the resort in 2006, and is the current operator. The resort is known for its gondola and 3 half-pipes. Gondola lift. The only gondola lift in the resort is called.

Geographic entities mentioned:
surface_form: Mount Dainichi
instance_of: Mountain
countries: Japan
coordinates: lat: 36.001388888889
lon: 136.83777777778
Topography. To the north is Froswick, a strikingly similar lesser copy, while the adjoining fell to the south is Yoke. Ill Bell appears from some directions to be a perfectly symmetrical bell-shaped peak, and 'Hill Bell' is one possible derivation of the name, quoted by Alfred Wainwright.

Geographic entities mentioned:
surface_form: Froswick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.468711111111
lon: -2.8732611111111
surface_form: yoke
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.451
lon: -2.869
These are big enough to enable easy recognition of the fell from a distance. The view of the Scafells is good and Ill Bell also gives a fine view of Windermere. All the fells making up the Kentmere Horseshoe can be seen clearly, while Cross Fell and the Dun Fells in the Pennines are in sight above Nan Bield Pass.

Geographic entities mentioned:
surface_form: Scafells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: Windermere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.358333333333
lon: -2.9361111111111
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
These are big enough to enable easy recognition of the fell from a distance. The view of the Scafells is good and Ill Bell also gives a fine view of Windermere. All the fells making up the Kentmere Horseshoe can be seen clearly, while Cross Fell and the Dun Fells in the Pennines are in sight above Nan Bield Pass.

Geographic entities mentioned:
surface_form: Cross Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.702777777778
lon: -2.4872222222222
surface_form: Dun Fells
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.683111111111
lon: -2.4513194444444
To the north is Froswick, a strikingly similar lesser copy, while the adjoining fell to the south is Yoke. Ill Bell appears from some directions to be a perfectly symmetrical bell-shaped peak, and 'Hill Bell' is one possible derivation of the name, quoted by Alfred Wainwright. With this form aped by Froswick, the ridge assumes an unmistakable 'roller-coaster' appearance when viewed in profile.

Geographic entities mentioned:
surface_form: froswick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.468711111111
lon: -2.8732611111111
There is the hint of a ridge to the north-east over Leads Howe. North and south of Ill Bell the Kentmere face is gouged out by Over and Rainsborrow Coves respectively. These features have created the narrow ridges to Froswick and Yoke. Ascents. The ridge is followed by a good path, and is the most usual route of ascent.

Geographic entities mentioned:
surface_form: froswick
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.468711111111
lon: -2.8732611111111
surface_form: yoke
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.451
lon: -2.869
These features have created the narrow ridges to Froswick and Yoke. Ascents. The ridge is followed by a good path, and is the most usual route of ascent. Yoke and Ill Bell form the start of the popular Kentmere Horseshoe, returning ultimately down the ridge on the opposite side of Kentmere valley. The ridge is also commonly ascended from Troutbeck valley, via the Garburn Road.

Geographic entities mentioned:
surface_form: yoke
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.451
lon: -2.869
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
Ill Bell. Ill Bell is a fell in the English Lake District, in the county of Cumbria, standing on the narrow ridge between the valleys of Kentmere and Troutbeck. Topography. To the north is Froswick, a strikingly similar lesser copy, while the adjoining fell to the south is Yoke.

Geographic entities mentioned:
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
To the north is Froswick, a strikingly similar lesser copy, while the adjoining fell to the south is Yoke. Ill Bell appears from some directions to be a perfectly symmetrical bell-shaped peak, and 'Hill Bell' is one possible derivation of the name, quoted by Alfred Wainwright. With this form aped by Froswick, the ridge assumes an unmistakable 'roller-coaster' appearance when viewed in profile.

Geographic entities mentioned:
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
The eastern Kentmere flank is rougher and steeper, falling in a great tumble of scree to the shore of Kentmere Reservoir. There is the hint of a ridge to the north-east over Leads Howe. North and south of Ill Bell the Kentmere face is gouged out by Over and Rainsborrow Coves respectively. These features have created the narrow ridges to Froswick and Yoke. Ascents.

Geographic entities mentioned:
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
Direct ascents are also possible from the valley of Hagg Gill via the northernmost quarry, or striking up over Lead Howes from the reservoir in Kentmere. Summit. The top of Ill Bell is small, peaked, and unusually stony for the Far Eastern Fells. A number of columnar cairns have been built at the summit and at various points close by.

Geographic entities mentioned:
surface_form: ill bell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462430555556
lon: -2.8715805555556
Distribution and habitat. Coast grey box occurs in New South Wales and Victoria from as far north as the Wolgan Valley, west of Sydney and as far south as eastern Gippsland. It is found near streams in lowland areas on better quality soils, particularly over limestone, although it may also appear on the tablelands up to above sea level, near Goulburn and Bungonia.

Geographic entities mentioned:
surface_form: Wolgan Valley
instance_of: Valley
countries: Australia
coordinates: lat: -33.24638888888889
lon: 150.1597222
Niaqornarsuaq. Niaqornarsuaq is a mountain of Greenland. It is located in the Upernavik Archipelago.

Geographic entities mentioned:
surface_form: niaqornarsuaq
instance_of: Mountain
countries: Greenland
coordinates: lat: 69.91666666666667
lon: -50.416666666666664
The Horn (or Saddleback Horn) is a mountain located in Franklin County, Maine. The Horn is flanked to the southwest by the main summit of Saddleback Mountain, to the northeast by Saddleback Junior, and to the northwest by Potato Nubble. The Horn drains to the northeast into Redington Stream, then into the South Branch of the Dead River, the Kennebec River, and into the Gulf of Maine.

Geographic entities mentioned:
surface_form: Saddleback Junior
instance_of: Mountain
countries: United States
coordinates: lat: 44.95815
lon: -70.457783333333
surface_form: saddleback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.5095
lon: -69.136
surface_form: saddleback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.9367
lon: -70.5031
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
surface_form: saddleback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.1267
lon: -73.8752
Saddleback Horn. The Horn (or Saddleback Horn) is a mountain located in Franklin County, Maine. The Horn is flanked to the southwest by the main summit of Saddleback Mountain, to the northeast by Saddleback Junior, and to the northwest by Potato Nubble.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: saddleback horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.951333333333
lon: -70.487166666667
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
Saddleback Horn. The Horn (or Saddleback Horn) is a mountain located in Franklin County, Maine. The Horn is flanked to the southwest by the main summit of Saddleback Mountain, to the northeast by Saddleback Junior, and to the northwest by Potato Nubble.

Geographic entities mentioned:
surface_form: saddleback horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.951333333333
lon: -70.487166666667
The Horn is flanked to the southwest by the main summit of Saddleback Mountain, to the northeast by Saddleback Junior, and to the northwest by Potato Nubble. The Horn drains to the northeast into Redington Stream, then into the South Branch of the Dead River, the Kennebec River, and into the Gulf of Maine. The Horn drains to the west into Saddleback Lake, then into Redington Stream.

Geographic entities mentioned:
surface_form: dead river
instance_of: Watercourse
countries: United States
coordinates: lat: 45.3333
lon: -69.9697
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
The Horn drains to the northeast into Redington Stream, then into the South Branch of the Dead River, the Kennebec River, and into the Gulf of Maine. The Horn drains to the west into Saddleback Lake, then into Redington Stream. The Horn drains to the south into Winship Stream, then into Conant Stream, Orbeton Stream, and the Sandy River, another tributary of the Kennebec.

Geographic entities mentioned:
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
The Horn drains to the west into Saddleback Lake, then into Redington Stream. The Horn drains to the south into Winship Stream, then into Conant Stream, Orbeton Stream, and the Sandy River, another tributary of the Kennebec. The Horn drains to the southeast into Hardy Stream, then into Orbeton Stream.

Geographic entities mentioned:
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
The Horn drains to the south into Winship Stream, then into Conant Stream, Orbeton Stream, and the Sandy River, another tributary of the Kennebec. The Horn drains to the southeast into Hardy Stream, then into Orbeton Stream. The Appalachian Trail, a National Scenic Trail from Georgia to Maine, runs along the ridge of Saddleback, including the summit of The Horn.

Geographic entities mentioned:
surface_form: the horn
instance_of: Mountain
countries: United States
coordinates: lat: 44.518
lon: -71.4002
Bonnington (sternwheeler). &quot;Bonnington&quot; was a sternwheel steamboat that ran on the Arrow Lakes in British Columbia from 1911 to 1931. &quot;Bonnington&quot; and two sisterships were the largest sternwheelers ever built in British Columbia. &quot;Bonnington&quot; was partially dismantled in the 1950s, and later sank, making the vessel the largest freshwater wreck site in British Columbia.

Geographic entities mentioned:
surface_form: Arrow Lakes
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
Need for construction. Steam navigation on the inland lakes of British Columbia was dominated by the River and Lake Service of the Canadian Pacific Railway. Since the early 1890s the River and Lake Service had maintained steamboat service on Okanagan, Arrow and Kootenay lakes.

Geographic entities mentioned:
surface_form: Okanagan
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
surface_form: Arrow
instance_of: Group of lakes
countries: Canada
coordinates: lat: 50
lon: -118
surface_form: Kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
had done with Banff
Similar vessels built at same time. &quot;Bonnington&quot; was a near twin of the steamers &quot;Naskookin&quot; and &quot;Sicamous&quot; built shortly afterwards on Kootenay and Okanagan lakes respectively. Unusually for a sternwheeler, &quot;Bonnington&quot; was equipped with compound steam engines, which were manufactured by Polson Iron Works of Toronto, Ontario.

Geographic entities mentioned:
surface_form: Kootenay
instance_of: Lake
countries: Canada
coordinates: lat: 49.3
lon: -116.75
surface_form: Okanagan
instance_of: Lake
countries: Canada
coordinates: lat: 49.920833333333
lon: -119.5
Chumbu (mountain). Chumbu is a mountain in the Nepal Himalayas near the border of the Tibet Autonomous Region of China. It falls under Eastern Development Region Solukhumbu Nepal. Climbing history. On November 3, 2022 a Czech team, led by Piolet d'Or winner Zdenek Hak summited the unclimbed Chumbu peak for the first time accompanied by Radek Groh, Jaroslav Bánsky and Petr Kejklíček.

Geographic entities mentioned:
surface_form: chumbu (mountain)
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.01393318
lon: 86.788414
Chumbu (mountain). Chumbu is a mountain in the Nepal Himalayas near the border of the Tibet Autonomous Region of China. It falls under Eastern Development Region Solukhumbu Nepal. Climbing history. On November 3, 2022 a Czech team, led by Piolet d'Or winner Zdenek Hak summited the unclimbed Chumbu peak for the first time accompanied by Radek Groh, Jaroslav Bánsky and Petr Kejklíček.

Geographic entities mentioned:
surface_form: chumbu
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.01393318
lon: 86.788414
Climbing history. On November 3, 2022 a Czech team, led by Piolet d'Or winner Zdenek Hak summited the unclimbed Chumbu peak for the first time accompanied by Radek Groh, Jaroslav Bánsky and Petr Kejklíček. A fifth member, Juraj Koren of Slovakia, planned to paraglide from the summit but was fallen ill by dengue and could not start the climb.

Geographic entities mentioned:
surface_form: chumbu
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.01393318
lon: 86.788414
Schwarzer Berg (Jauernick). Schwarzer Berg is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: schwarzer berg (jauernick)
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0942
lon: 14.8975
surface_form: schwarzer berg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1925
lon: 9.43017
Schwarzer Berg (Jauernick). Schwarzer Berg is a mountain of Saxony, southeastern Germany.

Geographic entities mentioned:
surface_form: schwarzer berg
instance_of: Mountain
countries: Germany
coordinates: lat: 51.0942
lon: 14.8975
surface_form: schwarzer berg
instance_of: Mountain
countries: Germany
coordinates: lat: 50.1925
lon: 9.43017
(4:21) Tent pegs have also been used as murder weapons in recent history, for example in the murder of Billie-Jo Jenkins. Other uses of tent pegs are as improvised climbing pitons, for example in the siege of the Sogdian Rock and Jean-Christophe Lafaille's self rescue on Annapurna.

Geographic entities mentioned:
surface_form: Annapurna
instance_of: Mountain
countries: Nepal
coordinates: lat: 28.5958
lon: 83.82
A total of 36 were ordered (most on 29 and 31 July 1940, but &quot;KM1&quot; to &quot;KM4&quot; were ordered on 26 August, and &quot;KM25&quot; and &quot;KM26&quot; on 11 October 1940), but as their engines proved unreliable, they were not used in their intended role and instead most were employed in lakes and rivers, being attached to the Peipusee Flotilla (&quot;KM3&quot; to the Ladogasee Flotilla).

Geographic entities mentioned:
surface_form: Peipusee
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
surface_form: Ladogasee
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 60.842777777777776
lon: 31.459722222222222
In June and July 1951, due to heavy rains, rivers and streams flooded numerous cities in Kansas, including Clements. Many reservoirs and levees were built in Kansas as part of a response to the Great Flood of 1951. Geography. Clements is located in the Flint Hills of the Great Plains. The Cottonwood River runs through the southern part of the community. Area attractions.

Geographic entities mentioned:
surface_form: Flint Hills
instance_of: Landform
countries: United States
coordinates: lat: 37.2833
lon: -96.6753
Robert G. Beattie was named president of the company in January 1956. KBCH was the second radio station, after KNPT (1310 AM, Newport), established in Lincoln County, Oregon. The station requested the call sign KBCH to represent the &quot;20 Miracle Miles&quot; of beaches in Lincoln County, including Moolack Beach and Beverly Beach State Park. Move to 1380.

Geographic entities mentioned:
surface_form: Moolack Beach
instance_of: Landform
countries: United States
coordinates: lat: 44.6998382
lon: -124.0653945
History. On July 1, 1586, Charles IX of Sweden issued a letter for the first priest elected, Olaus Gestricius – also Olavus Johannis, Olof Hansson and «herr Olaf på Möckelnsbodar» – (by the late 1500s) where he addressed the need for a church by Lake Möckeln. The residents were ordered to erect the church and completed it at the beginning of the 1600s.

Geographic entities mentioned:
surface_form: Lake Möckeln
instance_of: Lake
countries: Sweden
coordinates: lat: 59.3083
lon: 14.55
A secret annex to the treaty of the alliance considered the contested and non-contested zones in Slavic Macedonia, with the contested zone of northwestern Macedonia (the region between the Šar Mountain and Lake Ohrid) left up to the arbitration of the Russian Emperor, and the uncontested southeastern zone (east of the Lake Ohrid–Kriva Palanka line) intended to become part of Bulgaria, free of any Serbian claims.

Geographic entities mentioned:
surface_form: Lake Ohrid
instance_of: Lake
countries: North Macedonia
Albania
coordinates: lat: 41.03333333333333
lon: 20.716666666666665
From route 138, the forest road “Chemin de la Rivière des Cèdres” goes up the valley of the Portneuf river to the mouth of the Rivière des Cèdres. From there, a secondary forest road goes north-west to the peninsula south of the mouth of the Portneuf East river. The mountainous topography of the Portneuf East River hinders the development of a forest road for this valley.

Geographic entities mentioned:
surface_form: rivière des cèdres
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.238333333333
lon: -70.824444444444
surface_form: rivière des cèdres
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.238333333333
lon: -70.824444444444
The toponym &quot;Rivière Portneuf Est&quot; was formalized on December 5, 1968, at the Place Names Bank of the Commission de toponymie du Québec.

Geographic entities mentioned:
surface_form: rivière portneuf est
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.811666666667
lon: -69.776388888889
Portneuf River East. The Portneuf East River is a tributary of the Portneuf River, flowing on the northwest shore of the Saint Lawrence River, in the territory from Lac-au-Brochet, in the La Haute-Côte-Nord Regional County Municipality, in the administrative region of Côte-Nord, Quebec, Canada.

Geographic entities mentioned:
surface_form: portneuf river east
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.811666666667
lon: -69.776388888889
Portneuf River East. The Portneuf East River is a tributary of the Portneuf River, flowing on the northwest shore of the Saint Lawrence River, in the territory from Lac-au-Brochet, in the La Haute-Côte-Nord Regional County Municipality, in the administrative region of Côte-Nord, Quebec, Canada.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
From route 138, the forest road “Chemin de la Rivière des Cèdres” goes up the valley of the Portneuf river to the mouth of the Rivière des Cèdres. From there, a secondary forest road goes north-west to the peninsula south of the mouth of the Portneuf East river. The mountainous topography of the Portneuf East River hinders the development of a forest road for this valley.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
From there, a secondary forest road goes north-west to the peninsula south of the mouth of the Portneuf East river. The mountainous topography of the Portneuf East River hinders the development of a forest road for this valley. Forestry is the main economic activity in the sector; recreational tourism, second.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Forestry is the main economic activity in the sector; recreational tourism, second. The surface of the Portneuf East River is usually frozen from the end of November to the beginning of April; however, safe circulation on the ice is generally made from mid-December to the end of March. Geography.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Geography. The Portneuf East River rises at the mouth of Lake Emilien (length:; altitude:) surrounded by mountains. The mouth of this lake is located East of Lake Daniel; North-West of the mouth of the Portneuf East river.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Upper course of the Portneuf East river (segment of
altitude:) over its full length and Lake Ale (length:; altitude:) over its full length, as well as by forming a curve towards the South, up to the discharge (coming from the North) of a set of lakes including Éric, Garant, Noir, Épinette, Cameo and Élie;
Note: Lac Charles receives the outlet (coming from the Southwest) from Lac du Chicot;
Lower course of the Portneuf East river (segment of
Toponymy.

Geographic entities mentioned:
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Location and size. Pamban Island is situated between 9°11' N and 9°19' N latitude and 79°12' E to 79°23' E longitudes. The chain formed by Pamban Island, the shoals of Adam's Bridge, and Mannar Island of Sri Lanka separate Palk Bay and the Palk Strait in the northeast from the Gulf of Mannar in the southwest.

Geographic entities mentioned:
surface_form: Adam's Bridge
instance_of: Landform
countries: India
Sri Lanka
coordinates: lat: 9.121
lon: 79.5217
Eklutna River. The Eklutna River () is approximately long and is located in the Southcentral region of the U.S. state of Alaska. A portion of the river flows through a canyon up to deep, emptying into the Knik Arm of Cook Inlet approximately northeast of Anchorage. This degraded anadromous stream historically originated from Eklutna Lake, which itself is fed by Eklutna Glacier.

Geographic entities mentioned:
surface_form: Knik Arm
instance_of: Body of water
countries: United States
coordinates: lat: 61.2
lon: -150.217
Pioneering phase at Wasserkuppe Mountain. After testing at Wasserkuppe, in June 1928, Fritz von Opel had purchased an Alexander Lippisch-designed sailplane, the Ente, and fitted it with rockets. Fritz Stamer was the pilot during the OPEL RAK experimentations with Lippisch's design.

Geographic entities mentioned:
surface_form: Wasserkuppe
instance_of: Mountain
countries: Germany
coordinates: lat: 50.498055555556
lon: 9.9377777777778