Sarmila/GeoWiki-Features huggingface dataset:
The largely undeveloped shores and adjacent wetlands of Lake Altaussee provide habitats for numerous animal and plant species and have been under nature conservation since 1959. The Austrian Federal Forests own Lake Altaussee, which is a popular excursion destination due to its beautiful location. Every third year, the lake hosts the Daffodil Festival, Austria's largest flower festival. Geography.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Every third year, the lake hosts the Daffodil Festival, Austria's largest flower festival. Geography. The Totes Gebirge surround Lake Altaussee in a horseshoe shape. The Loser (1873m above sea level) lies to the north, with steep flanks that drop sharply to the lakeshore. To the east, the Trisselwand (1754m sea level) features a rock face that rises approximately 600 meters high.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
The lake is surrounded by a 7.4 km long circular hiking trail Uferpromenade. Hydrology. The hydrological catchment area of Lake Altaussee encompasses a total area of 54 km2, entirely located within the Totes Gebirge. The lake's primary source of water is from karst springs located at the lake's bottom, which receive underground flow from debris and rock crevices.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Additionally, there are a few small spring outlets along the shores with a combined discharge of approximately 20 L/s. Lake Altaussee demonstrates typical fluctuations in discharge commonly associated with karst springs. In the northeast, there is a small dead ice hole called Lake Osterseen, which is filled by groundwater corresponding to the water level of Lake Altaussee.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Lake Altaussee demonstrates typical fluctuations in discharge commonly associated with karst springs. In the northeast, there is a small dead ice hole called Lake Osterseen, which is filled by groundwater corresponding to the water level of Lake Altaussee. The Altaussee Traun, the lake's outlet, exits in the southwest at the Seeklause, where a bridge spans the outflow.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
The Altaussee Traun, the lake's outlet, exits in the southwest at the Seeklause, where a bridge spans the outflow. It carves its path between the rock barrier of the Plattenkogel and the alluvial fan of the Augstbach, which acts as a natural dam for the lake. Originally, the Augstbach stream flowed into Lake Altaussee 250m north of the lake outlet.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
However, due to the issue of saline water from the nearby salt mine repeatedly reaching the lake through this stream, the stream bed was artificially relocated before 1530. Since then, the Augstbach has been redirected to flow westward, past Lake Altaussee, and into the Traun River approximately 150m downstream from the lake outlet.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Within the western part of the Totes Gebirge, lies the Schönberg group, which is geologically distinct from the Priel group due to a deep incursion furrow. The Wildensee line is a geological structure that stretches from Lake Altaussee, traverses the Hochklapfsattel, extends to Wildensandee Lake, and continues over the Rinnerboden to Offensee Lake.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
During the ice ages, the Altaussee glacier flowed from the Totes Gebirge plateau, flowing over the Aussee basin and reaching the Traun glacier near Bad Goisern. The glacier's movement was instrumental in sculpting the valley's over-deepened basin of Lake Altaussee. About 16,000 years ago, a powerful readvance of the glacier occurred and filled the basin once again, giving it its current form.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Simultaneously, as the over-deepened basin was being freed from the ice, a lake began to form at the edge of the ice body. This phase, marked by the presence of a high debris formation around Lake Altaussee's basin, indicates the interaction between the ice body and the lake basin. As the ice eventually disappeared entirely, the alluvial cone adjusted to accommodate the present lake level.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
In spring after the ice melts, the water body mixes and brings oxygen-rich water into the depths. In the summer half-year, a distinct thermocline forms, and only the surface layer warms up, in autumn mixing occurs again, followed by ice formation. Strict stratification conditions are present in Lake Altaussee. The epilimnion has only a very small thickness of about two meters.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Due to the low phytoplankton concentration and low algae growth, the average summer visibility depth is 8.9 meters. Plankton. According to chlorophyll studies, algae growth in Lake Altaussee is relatively low. Cryptophyceae and diatoms are the principal phytoplankton community components, with species from the genus Cyclotella standing out.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Fishing in the lake is still conducted professionally to this day. Lake Altaussee is renowned for its large char and trout populations, with Arctic char accounting for approximately 90% of the total catch. The shallow and flowing water on the lake side of the Seeklause serves as a crucial spawning area for lake trout, which spawn from October to December.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
One method involves placing submerged spruce branches, where the perch lay their eggs, and then removing the branches to destroy the fish eggs. Shipping. The company Stern Schifffahrt GmbH, based in Gmunden, operates shipping on Lake Altaussee. Boats run regularly between the Madlmaier landing stage in Altaussee and the Seewiese landing stage on the northeast shore.

Geographic entities mentioned:
surface_form: lake altaussee
instance_of: Lake
countries: Austria
coordinates: lat: 47.6417
lon: 13.7861
Every third year, the lake hosts the Daffodil Festival, Austria's largest flower festival. Geography. The Totes Gebirge surround Lake Altaussee in a horseshoe shape. The Loser (1873m above sea level) lies to the north, with steep flanks that drop sharply to the lakeshore. To the east, the Trisselwand (1754m sea level) features a rock face that rises approximately 600 meters high.

Geographic entities mentioned:
surface_form: loser
instance_of: Mountain
countries: Austria
coordinates: lat: 47.660833333333
lon: 13.771111111111
The Wildensee line is a geological structure that stretches from Lake Altaussee, traverses the Hochklapfsattel, extends to Wildensandee Lake, and continues over the Rinnerboden to Offensee Lake. The base of the Loser mountain is composed predominantly of Dachstein limestone, while the Plattenkogel showcases Pedata limestone or dolomite formations, both originating from the Triassic period.

Geographic entities mentioned:
surface_form: loser
instance_of: Mountain
countries: Austria
coordinates: lat: 47.660833333333
lon: 13.771111111111
surface_form: dachstein
instance_of: Mountain
countries: Austria
coordinates: lat: 47.475168
lon: 13.605735
They were later assimilated by the Germanic conquerors. Under Augustus, the Roman Empire began to invade lands inhabited by the Germanic tribes, creating a short-lived Roman province of Germania between the Rhine and Elbe rivers. In 9 AD, three Roman legions were defeated by Arminius in the Battle of the Teutoburg Forest.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Germany is also bordered by the North Sea and, at the north-northeast, by the Baltic Sea. German territory covers. Elevation ranges from the mountains of the Alps (highest point: the Zugspitze at) in the south to the shores of the North Sea () in the northwest and the Baltic Sea () in the northeast.

Geographic entities mentioned:
surface_form: Zugspitze
instance_of: Mountain
countries: Germany
Austria
coordinates: lat: 47.421217
lon: 10.986314
Perosa Argentina. Perosa Argentina (French: Pérouse) is a &quot;comune&quot; (municipality) in the Metropolitan City of Turin in the Italian region Piedmont, located about northwest of Turin, in the val Chisone. The population of the village is 3061 (30 June 2023).

Geographic entities mentioned:
surface_form: val Chisone
instance_of: Valley
countries: Italy
coordinates: lat: 45.033
lon: 7.05
Geography. The wilderness area encompasses immediately east of the Continental Divide in Gilpin County and Clear Creek County. The wilderness is named after its second tallest mountain, James Peak. Within its boundaries are 30 miles (48 km) of trails. Parry Peak is the highest peak in the James Peak Wilderness, at. History. The wilderness was established by H.R.1576 in the 107th Congress (2001).

Geographic entities mentioned:
surface_form: James Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.851944444444
lon: -105.69027777778
Geography. The wilderness area encompasses immediately east of the Continental Divide in Gilpin County and Clear Creek County. The wilderness is named after its second tallest mountain, James Peak. Within its boundaries are 30 miles (48 km) of trails. Parry Peak is the highest peak in the James Peak Wilderness, at. History. The wilderness was established by H.R.1576 in the 107th Congress (2001).

Geographic entities mentioned:
surface_form: Parry Peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.838055555556
lon: -105.71333333333
Parry Peak is the highest peak in the James Peak Wilderness, at. History. The wilderness was established by H.R.1576 in the 107th Congress (2001). James Peak was named after Edwin James, pioneer and botanist. Originally Pikes Peak was named James Peak prior to Pike's exploration journey. After the renaming to Pikes Peak, the current James Peak was named.

Geographic entities mentioned:
surface_form: Pikes Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.840555555556
lon: -105.04416666667
Plane project. In the 1960s, Gachamba became friends with an English tourist he would go out fishing with. The tourist owned a small plane and took Gachamba out for a short trip around Lake Naivasha. Gachamba became enamored with flying and soon wanted to build his own. Come the 1970s, he became the first Kenyan to build an airplane. Education.

Geographic entities mentioned:
surface_form: Lake Naivasha
instance_of: Lake
countries: Kenya
coordinates: lat: -0.76852777777778
lon: 36.350644444444
The densely paniculate, long, inflorescences bear masses of small white flowers. The spheroidal, brown capsule is long. The main flowering season is in January. Distribution and habitat. The tree is endemic to Australia's subtropical Lord Howe Island in the Tasman Sea, where it is found in mountain forests from the Goat House and Erskine Valley to the tops of Mounts Erskine and Gower. Etymology.

Geographic entities mentioned:
surface_form: Gower
instance_of: Mountain
countries: Australia
coordinates: lat: -31.5903
lon: 159.072
It runs north from Glover through Barton, Brownington, Coventry and drains through Newport into Lake Memphremagog's South Bay. Course. The Barton River arises from the fountains of the former Runaway Pond in Glover. The stretch of river from Vermont Route 16 north of Glover village to Lake Memphremagog is long and is rated by American Whitewater as a class I-III section.

Geographic entities mentioned:
surface_form: Runaway Pond
instance_of: Lake
countries: United States
coordinates: lat: 44.634722222222
lon: -72.211666666667
Humber. Yorkshire is drained by several rivers. In western and central Yorkshire, the many rivers empty their waters into the River Ouse, which reaches the North Sea via the Humber Estuary. The most northerly of the rivers in the Ouse system is the River Swale, which drains Swaledale before passing through Richmond and meandering across the Vale of Mowbray.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
surface_form: Vale of Mowbray
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.342
lon: -1.435
The most northerly of the rivers in the Ouse system is the River Swale, which drains Swaledale before passing through Richmond and meandering across the Vale of Mowbray. Next in the Ouse system, draining in Wensleydale, is the River Ure, which joins the Swale east of Boroughbridge.

Geographic entities mentioned:
surface_form: Wensleydale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3056
lon: -2.16667
Next in the Ouse system, draining in Wensleydale, is the River Ure, which joins the Swale east of Boroughbridge. The River Nidd rises on the edge of the Yorkshire Dales National Park and flows along Nidderdale before reaching the Vale of York. The Ouse is the name given to the river after its confluence with the Ure at Ouse Gill Beck.

Geographic entities mentioned:
surface_form: Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
surface_form: Vale of York
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.95
lon: -1.0833333333333333
The River Nidd rises on the edge of the Yorkshire Dales National Park and flows along Nidderdale before reaching the Vale of York. The Ouse is the name given to the river after its confluence with the Ure at Ouse Gill Beck. The River Wharfe, which drains Wharfedale, joins the Ouse upstream of Cawood. The Rivers Aire and Calder are more southerly contributors to the River Ouse.

Geographic entities mentioned:
surface_form: Wharfedale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.88333
lon: -1.45
The most southerly Yorkshire tributary is the River Don, which flows northwards to join the main river at Goole. The River Derwent rises on the North York Moors, flows south then westwards through the Vale of Pickering, then turns south again to drain the eastern part of the Vale of York. It empties into the River Ouse at Barmby on the Marsh.

Geographic entities mentioned:
surface_form: Vale of Pickering
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.2
lon: -0.7
It empties into the River Ouse at Barmby on the Marsh. To the east of the Yorkshire Wolds, the River Hull flows southwards to join the Humber Estuary at Kingston upon Hull. The western Pennines are served by the River Ribble, which drains westwards into the Irish Sea close to Lytham St Annes.The largest freshwater lake in the region is Hornsea Mere in the East Riding of Yorkshire. Esk and Tees.

Geographic entities mentioned:
surface_form: Hornsea Mere
instance_of: Lake
countries: United Kingdom
coordinates: lat: 53.905555555556
lon: -0.18611111111111
Esk and Tees. In the far north of the county, the River Tees flows eastwards through Teesdale and empties its waters into the North Sea downstream of Middlesbrough. The smaller River Esk flows from west to east at the northern foot of the North York Moors to reach the sea at Whitby. Natural Areas.

Geographic entities mentioned:
surface_form: Teesdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.545
lon: -1.927
Pilsdon Pen. Pilsdon Pen is a 277-metre (909 ft) hill in Dorset in South West England, situated at the north end of the Marshwood Vale, approximately west of Beaminster. It is Dorset's second highest point and has panoramic views extending for many miles. It was bequeathed to the National Trust by the Pinney family in 1982.

Geographic entities mentioned:
surface_form: Marshwood Vale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 50.78
lon: -2.83
Landscape. Other notable high points in the vicinity are Lewesdon Hill (279 m), Dorset's highest point some 4 kilometres to the east, and Blackdown Hill (215 m), about 2 kilometres northwest. Though using the spelling Pillesdon, it was the central triangulation point for the area between 12 April and 1 June 1845 for the Principal Triangulation of Great Britain. Dorothy and William Wordsworth.

Geographic entities mentioned:
surface_form: Blackdown Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 50.83057
lon: -2.86057
Distribution and habitat. This species of &quot;Hypocalymma&quot; is found in swamps, often in Jarrah woodland or Myrtaceae-rich shrubland from the Scott River plain to Lake Jasper and between Walpole and the Two Peoples Bay Nature Reserve in the Jarrah Forest and Warren bioregions of southern Western Australia.

Geographic entities mentioned:
surface_form: Lake Jasper
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
Ontario Highway 18A. King's Highway 18A, commonly referred to as Highway 18A, was a provincially maintained highway in the Canadian province of Ontario. The route began and ended at Highway 18, travelling along the Lake Erie shoreline and through Colchester. It was the southernmost highway to ever exist in Canada, as the only one to travel south of the 42nd parallel.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
The west junction was at the community of Malden Centre, while the east junction was located on the western edge of Kingsville. The route itself was long, detouring to the south along the shore of Lake Erie and passing through Colchester. Highway18A was the southernmost highway in Canada, and the only one to travel south of the 42ndparallel. History.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Lake Eva. Lake Eva, located west of Polk County Road 557, is on the north side of the city of Lake Alfred, Florida. This lake is somewhat kidney-shaped and has a surface area of. Lake Eva in inside the Lake Alfred city limits and is west of Polk County Road 557. Its east shore is bordered by some homes with large lots. The northeast, north and west shores are bordered by citrus groves.

Geographic entities mentioned:
surface_form: lake eva
instance_of: Lake
countries: United States
coordinates: lat: 28.1133
lon: -81.7334
Its east shore is bordered by some homes with large lots. The northeast, north and west shores are bordered by citrus groves. A swampy area is on the south shore and a grassy area is along the southeast shore. Lake Eva is completely surrounded by private property. There is no public access to Lake Eva other than a canal on the lake's southwest that connects to nearby Lake Alfred.

Geographic entities mentioned:
surface_form: lake eva
instance_of: Lake
countries: United States
coordinates: lat: 28.1133
lon: -81.7334
A swampy area is on the south shore and a grassy area is along the southeast shore. Lake Eva is completely surrounded by private property. There is no public access to Lake Eva other than a canal on the lake's southwest that connects to nearby Lake Alfred. However, this canal is too shallow to be navigated by any boats and it is sometimes dry.

Geographic entities mentioned:
surface_form: lake eva
instance_of: Lake
countries: United States
coordinates: lat: 28.1133
lon: -81.7334
Godwin believed that Fanny had been in love with Shelley, and Shelley himself suffered depression and guilt over her death, writing: &quot;Friend had I known thy secret grief / Should we have parted so.&quot; Further tragedy followed in December when Shelley's estranged wife Harriet drowned herself in the Serpentine.

Geographic entities mentioned:
surface_form: Serpentine
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.505277777778
lon: -0.16944444444444
Wolseley sent Indian paddlers back to the other flotillas to assist in their journey across the lake. The difficulties were overcome, and the force arrived at Winnipeg in August. The expedition travelled to Georgian Bay, then by steamer across Lake Huron to the U.S. Sault Canal where men and materiel had to be transported on the Canadian side of the river.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Wolseley then arranged the portage of the soldiers and materials upriver on the Canadian side of the river to be loaded back onto the awaiting &quot;Algoma&quot;. The expedition then proceeded across Lake Superior to the Department of Public Works station at Thunder Bay, which Wolseley named Prince Arthur's Landing on May 25, in honour of Queen Victoria's third son.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Travelling further westwards, they passed through Fort Frances, arriving on August 4. Wolseley made it to Lake of the Woods; however, he lost his way. On August 15 he finally made Rat Portage with his flotilla and sent Iroquois guides back to help the remaining brigades cross the river.

Geographic entities mentioned:
surface_form: Lake of the Woods
instance_of: Lake
countries: Canada
United States
coordinates: lat: 49.09027777777778
lon: -95.2388888888889
On August 15 he finally made Rat Portage with his flotilla and sent Iroquois guides back to help the remaining brigades cross the river. They proceeded down the Winnipeg River and across the south basin of Lake Winnipeg to the Red River finally arriving at Fort Garry in late August. Wolseley formed up his troops and immediately began his advance on Upper Fort Garry.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Towards the north-west, the country was very marshy and nothing was to be seen for miles but swamps and rice fields, with a few huts scattered here and there raised on mounds of earth. In the south of the district, along the coast of the Bay of Bengal, were the forest tracts of the Sundarbans where tigers and leopards used to live.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Location. The peak is located at which is 480 m southwest of Melnik Peak, 2.46 km northwest of Atanasoff Nunatak, 930 m north of Asparuh Peak, 3.18 km east of Hemus Peak and 4.66 km southeast of Leslie Hill (Bulgarian topographic survey 05, and mapping in 2005 and 2009).

Geographic entities mentioned:
surface_form: Melnik Peak
instance_of: Mountain
coordinates: lat: -62.601777777778
lon: -60.153111111111
surface_form: Hemus Peak
instance_of: Mountain
coordinates: lat: -62.606111111111
lon: -60.220555555556
Samokov Knoll. Samokov Knoll (Samokovska Mogila \'sa-mo-kov-ska mo-'gi-la\) is a peak of elevation 602 m in Yankov Gap area, Livingston Island in the South Shetland Islands, Antarctica. Surmounting Kaliakra Glacier to the northwest and Struma Glacier to the southeast.

Geographic entities mentioned:
surface_form: samokov knoll
instance_of: Mountain
coordinates: lat: -62.605
lon: -60.1587
Kepler-5b's initial discovery by Kepler was re-examined by scientists at the W.M. Keck Observatory at Mauna Kea, Hawaii; the McDonald Observatory in west Texas; the Palomar and Lick Observatories in California; the MMT, WIYN, and Whipple Observatories in Arizona; and the Roque de los Muchachos Observatory in the Canary Islands. Characteristics.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
It is located in the La Paz Department, Murillo Province, La Paz Municipality. Tilata is situated south of the mountain Llamp'u, north-west of Qala Uyu &quot;(Khala Huyo)&quot; and north-east of Wayna Potosí. Tilata Lake lies east of the mountain.

Geographic entities mentioned:
surface_form: Wayna Potosí
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.261944444444
lon: -68.148888888889
surface_form: llamp'u
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.2014
lon: -68.0933
surface_form: wayna potosí
instance_of: Mountain
countries: Bolivia
coordinates: lat: -18.0483
lon: -68.1558
surface_form: tilata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.25
lon: -68.09
surface_form: wayna potosí
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.261944444444
lon: -68.148888888889
Tilata. Tilata (Aymara &quot;tilaña&quot; light, light ray, to set in row, &quot;-ta&quot; a suffix, &quot;set in row&quot;, also spelled &quot;Telata&quot;) is a mountain in the Cordillera Real in the Bolivian Andes. It is located in the La Paz Department, Murillo Province, La Paz Municipality.

Geographic entities mentioned:
surface_form: tilata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -16.25
lon: -68.09
Wedgemount Lake. Wedgemount Lake is a turquoise-coloured alpine lake located in Garibaldi Provincial Park of British Columbia, Canada. It is situated below Wedge Mountain, Parkhurst Mountain, Rethel Mountain, and Mount Weart. Meltwater from Wedgemount Glacier and Armchair Glacier feeds the lake, whereas Wedgemount Creek is the outflow from the lake.

Geographic entities mentioned:
surface_form: Wedge Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.13305555555556
lon: -122.79333333333334
surface_form: Parkhurst Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.14666666666667
lon: -122.80722222222222
surface_form: Rethel Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1497
lon: -122.81943
surface_form: Mount Weart
instance_of: Mountain
countries: Canada
coordinates: lat: 50.1664
lon: -122.78602
Wedgemount Lake. Wedgemount Lake is a turquoise-coloured alpine lake located in Garibaldi Provincial Park of British Columbia, Canada. It is situated below Wedge Mountain, Parkhurst Mountain, Rethel Mountain, and Mount Weart. Meltwater from Wedgemount Glacier and Armchair Glacier feeds the lake, whereas Wedgemount Creek is the outflow from the lake.

Geographic entities mentioned:
surface_form: wedgemount lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
Wedgemount Lake. Wedgemount Lake is a turquoise-coloured alpine lake located in Garibaldi Provincial Park of British Columbia, Canada. It is situated below Wedge Mountain, Parkhurst Mountain, Rethel Mountain, and Mount Weart. Meltwater from Wedgemount Glacier and Armchair Glacier feeds the lake, whereas Wedgemount Creek is the outflow from the lake.

Geographic entities mentioned:
surface_form: wedgemount lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.159444444444
lon: -122.81527777778
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The total area of the city is. Geography. Kyōtanabe is located in southern Kyoto Prefecture, bordered by Osaka Prefecture and Nara Prefecture. It is one of the three &quot;Kansai Cultural and Academic Research City municipalities&quot;. The city is sandwiched between the Kizugawa River, which runs north–south on the east side of the city, and the Ikoma Mountains on the west. Climate.

Geographic entities mentioned:
surface_form: Ikoma Mountains
instance_of: Mountain
countries: Japan
coordinates: lat: 34.678452777778
lon: 135.67896944444
Pearce, Arizona. Pearce, Arizona, and Sunsites, Arizona, are adjacent unincorporated communities in the Sulphur Springs Valley of Cochise County, Arizona, United States. The two communities are often referred to as Pearce–Sunsites, Pearce/Sunsites, or Pearce Sunsites.

Geographic entities mentioned:
surface_form: Sulphur Springs Valley
instance_of: Valley
countries: United States
coordinates: lat: 32.4987
lon: -110.031
Cerro Beltrán. Cerro Beltrán is an andesitic-dacitic volcano in the Andes. It erupted andesitic-dacitic lava flows between 14.1 and 7.7 mya. Based on geochemical considerations, the volcano formed from granite and plagioclase bearing, thick crust. Part of the volcano was later covered by ignimbrites coming from the Galán caldera eruption. The volcano is located next to the Salar de Antofalla.

Geographic entities mentioned:
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
Based on geochemical considerations, the volcano formed from granite and plagioclase bearing, thick crust. Part of the volcano was later covered by ignimbrites coming from the Galán caldera eruption. The volcano is located next to the Salar de Antofalla. It is one of the large long-lived volcanoes forming the Archibarca-Galan volcanic alignment, along with Tebenquicho, Galán and Antofalla.

Geographic entities mentioned:
surface_form: Tebenquicho
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.33333
lon: -67.68333
surface_form: Galán
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.933333333333
lon: -66.916666666667
surface_form: Antofalla
instance_of: Mountain
countries: Argentina
coordinates: lat: -25.5625
lon: -67.88083333333333
Geography. Satkhira District has an area of. It is bordered to the north by Jessore District, on the south by the Bay of Bengal, to the east by Khulna District, and to the west by North 24 Parganas and South 24 Parganas districts of West Bengal, India. The annual average maximum temperature reaches 35.5 °C (95.9 °F); minimum temperature is 12.5 °C (54.5 °F). The annual rainfall is 1710 mm (67 in).

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
High pressure causes lava to ooze and spatter out. The lava builds up on the surface and solidifies creating the initial structure. Hornitos can grow and exceed 10 meters in height. Some classic examples of hornitos have been described, or depicted, from volcanoes including El Jorullo, Mexico which was visited by Alexander von Humboldt in 1803; Kilauea Hawaii; and Oldoinyo Lengai, Tanzania.

Geographic entities mentioned:
surface_form: El Jorullo
instance_of: Mountain
countries: Mexico
coordinates: lat: 18.972
lon: -101.718
Pre-History and Roman era. Bellinzona has always occupied an important geographic location in the Alps. To the south, the Po Valley is accessible by a lowland route down the valley of the river Ticino and by Lake Maggiore. To the north, the valley of the Ticino leads to the high alpine passes of Nufenen, St. Gotthard, Lukmanier and San Bernardino.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
Milan attacked the town three years later in 1422 after an offer to buy the town was rejected by the Swiss Confederation. The troops from Uri and Obwalden were quickly driven from the town and later defeated at the Battle of Arbedo on 30 June 1422. This defeat discouraged the expansionist intentions of Uri and its allies towards Lake Maggiore for a time.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
In 1874, the first sections of the Gotthard railway opened, linking Bellinzona to Biasca and Locarno. By 1882, the whole line was open, extending northwards to northern Switzerland via the Gotthard Tunnel, southwards to Lugano and Milan via the Monte Ceneri Pass, and down the east shore of Lake Maggiore to Luino.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
The town is located at a point at which the river Ticino, which has been flowing in a generally southerly direction, makes a turn to the west, to flow through the wide Pionoa di Magadino before entering the Lake Maggiore, and after it finally reaches to the Italian Po Valley and Lombardy.

Geographic entities mentioned:
surface_form: Lake Maggiore
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46.098055555555554
lon: 8.714722222222223
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
The river Moesa, running down the Valle Mesolcina from the San Bernardino Pass with access to the Gresionian valley &quot;Rheinwald&quot; of the Posterior Rhine, joins the Ticino on the northern boundary of the town.

Geographic entities mentioned:
surface_form: Valle Mesolcina
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.385
lon: 9.235
To the south the Monte Ceneri Pass crosses the Lugano Prealps to give access to Lake Lugano and an alternate route to Lombardy, whilst the San Jorio Pass provides a possible route east to the upper Lake Como. The town Bellinzona has an area, of. Of this area, or 22.0% is used for agricultural purposes, while or 62.5% is forested.

Geographic entities mentioned:
surface_form: Lake Lugano
instance_of: Lake
countries: Switzerland
Italy
coordinates: lat: 46
lon: 9
Arch of Janus. The Arch of Janus is the only quadrifrons triumphal arch preserved in Rome. It was set up in the early 4th century AD at a crossroads at the northeastern limit of the Forum Boarium, close to the Velabrum, over the Cloaca Maxima drain that went from the Forum to the River Tiber.

Geographic entities mentioned:
surface_form: Velabrum
instance_of: Valley
countries: Italy
coordinates: lat: 41.88916667
lon: 12.48194444
Alaska Route 1 (the Glenn Highway) runs through the pass, connecting the Copper River Valley with the Alaska Highway. Mentasta Pass is notable as the key col between Mount Logan (highpoint of Canada and the Saint Elias Mountains) and Denali (highpoint of the United States and the Alaska Range).

Geographic entities mentioned:
surface_form: Mount Logan
instance_of: Mountain
countries: Canada
coordinates: lat: 60.567222222222
lon: -140.40277777778
surface_form: Denali
instance_of: Mountain
countries: United States
coordinates: lat: 63.06916666666667
lon: -151.0063888888889
It is located in the Cochabamba Department, at the border of the Arani Province, Vacas Municipality, and the Carrasco Province, Pocona Municipality. Iskay Wasi lies northeast of Qucha Quchayuq Urqu. The Iskay Wasi Mayu originates at the mountain. It flows to Misk'i Mayu.

Geographic entities mentioned:
surface_form: Qucha Quchayuq Urqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.5483
lon: -65.5258
surface_form: iskay wasi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.54
lon: -65.52305556
Iskay Wasi. Iskay Wasi (Quechua &quot;iskay&quot; two, &quot;wasi&quot; house, &quot;two houses&quot;, also spelled &quot;Iscay Huasi&quot;) is a mountain in the Bolivian Andes which reaches a height of approximately. It is located in the Cochabamba Department, at the border of the Arani Province, Vacas Municipality, and the Carrasco Province, Pocona Municipality.

Geographic entities mentioned:
surface_form: iskay wasi
instance_of: Mountain
countries: Bolivia
coordinates: lat: -17.54
lon: -65.52305556
Rookery Lake. Rookery Lake is an almost circular lake, just cut off from the sea, at the western end of Long Peninsula in the Vestfold Hills of Princess Elizabeth Land, Antarctica. It was so named because of its proximity to an Adélie penguin colony. The nearest permanent research station is Australia's Davis, 10 km to the south-west on Broad Peninsula. Important Bird Area.

Geographic entities mentioned:
surface_form: elizabeth
instance_of: Mountain
coordinates: lat: -83.9
lon: 168.383
surface_form: rookery lake
instance_of: Lake
coordinates: lat: -68.49806
lon: 78.07306
Rookery Lake. Rookery Lake is an almost circular lake, just cut off from the sea, at the western end of Long Peninsula in the Vestfold Hills of Princess Elizabeth Land, Antarctica. It was so named because of its proximity to an Adélie penguin colony. The nearest permanent research station is Australia's Davis, 10 km to the south-west on Broad Peninsula. Important Bird Area.

Geographic entities mentioned:
surface_form: rookery lake
instance_of: Lake
coordinates: lat: -68.49806
lon: 78.07306
Important Bird Area. A 741 ha site comprising the western part of Long Peninsula and extending 6 km from Rookery Lake in the south-west to Bulatnaya Bay in the north-west, has been designated an Important Bird Area (IBA) by BirdLife International, because it supports some 45,000 breeding pairs of Adélie Penguins.

Geographic entities mentioned:
surface_form: rookery lake
instance_of: Lake
coordinates: lat: -68.49806
lon: 78.07306
Rookery Lake. Rookery Lake is an almost circular lake, just cut off from the sea, at the western end of Long Peninsula in the Vestfold Hills of Princess Elizabeth Land, Antarctica. It was so named because of its proximity to an Adélie penguin colony. The nearest permanent research station is Australia's Davis, 10 km to the south-west on Broad Peninsula. Important Bird Area.

Geographic entities mentioned:
surface_form: davis
instance_of: Mountain
coordinates: lat: -78.1
lon: -86.25
Wilkniss Mountains. The Wilkniss Mountains () form a prominent group of conical peaks and mountains, long running north–south, located east-southeast of Mount Feather in the Quartermain Mountains, Victoria Land, Antarctica. The mountains are wide in the north portion where Mount Blackwelder, high, and Pivot Peak high, rise above ice-free valleys.

Geographic entities mentioned:
surface_form: Mount Feather
instance_of: Mountain
coordinates: lat: -77.95
lon: 160.35
Location. The Wilkniss Mountains are south of the Knobhead massif, the southeastern part of the Quartermain Mountains. They are separated from Knobhead by the Ferrar Glacier, which flows east from its head near Mount Blackwelder. The Palais Glacier () is a broad glacier, about long, that flows north between Wilkniss Mountains and the Colwell Massif to enter Ferrar Glacier near its head.

Geographic entities mentioned:
surface_form: Knobhead
instance_of: Mountain
coordinates: lat: -77.9167
lon: 161.567
They are separated from Knobhead by the Ferrar Glacier, which flows east from its head near Mount Blackwelder. The Palais Glacier () is a broad glacier, about long, that flows north between Wilkniss Mountains and the Colwell Massif to enter Ferrar Glacier near its head. The Wilkniss Mountains are east of The Portal and Portal Mountain. Rampart Ridge is to the south. Glaciology.

Geographic entities mentioned:
surface_form: Portal Mountain
instance_of: Mountain
coordinates: lat: -78.1
lon: 159.16666944444
The Ferrar drifts have ages around 4.0–3.4 million years, 1.2 million years, 700 thousand years and 50 thousand years. This stability of ice surface elevation suggests that over the last 4 million years the upland regions of the McMurdo Dry Valleys have experienced minimal climatic amelioration. Vernier Valley.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
Since 1910, the hut has been a popular destination for winter sports as well. Major expansions were finished in 1963 and again in 1979. Heidelberger hut is easily accessible from Ischgl, Austria, by a road through the Fimbatal, which south of the Austrian-Swiss border is named Val Fenga.

Geographic entities mentioned:
surface_form: Fimbatal
instance_of: Valley
countries: Switzerland
Austria
coordinates: lat: 46.9633
lon: 10.2839
Bear Creek (Tahltan River tributary). Bear Creek is a tributary of the Tahltan River in northwest part of the province of British Columbia, Canada. It flows generally south through the Nahlin Plateau about to join the Tahltan River just downstream from the Tahltan and Little Tahltan River confluence. Bear Creek's watershed covers, and its mean annual discharge is an estimated.

Geographic entities mentioned:
surface_form: Nahlin Plateau
instance_of: Plateau
countries: Canada
coordinates: lat: 58.44972222222222
lon: -131.41833333333332
Bear Creek is in the traditional territory of the Tahltan people. Geography. Bear Creek originates on the south flank of the massive Level Mountain shield volcano, about south of Meszah Peak, the highest peak of the Level Mountain Range, a cluster of bare peaks on the summit of Level Mountain. The creek flows south through Level Mountain's high and relatively barren lava plateau.

Geographic entities mentioned:
surface_form: Meszah Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 58.4786
lon: -131.437
Llusk'a. Llusk'a (Quechua for polished, slippery, also spelled &quot;Lluskha&quot;) is a mountain in the Bolivian Andes. It is located in the Chuquisaca Department, Azurduy Province, Tarvita Municipality.

Geographic entities mentioned:
surface_form: llusk'a
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.7627
lon: -64.5908
Course. The Karenga is a right tributary of the Vitim. Its sources are in the Chingikhan Saddle, located between the Yablonoi Mountains and the Chersky Range. Kontalaksky Golets, the highest peak of the Yablonoi rises to the NW of the river valley, near Tungokochen. It flows in a mainly northeastern direction within a winding channel.

Geographic entities mentioned:
surface_form: Kontalaksky Golets
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 53.91305555555555
lon: 115.69305555555556
Prospect Hill (Kirkland, New York). Prospect Hill is a summit located in Central New York Region of New York located in the Town of Kirkland, west of Clinton.

Geographic entities mentioned:
surface_form: prospect hill (kirkland, new york)
instance_of: Mountain
countries: United States
coordinates: lat: 43.0375
lon: -75.444166666667
Prospect Hill (Kirkland, New York). Prospect Hill is a summit located in Central New York Region of New York located in the Town of Kirkland, west of Clinton.

Geographic entities mentioned:
surface_form: prospect hill
instance_of: Mountain
countries: United States
coordinates: lat: 43.0375
lon: -75.444166666667
Chalet Reynard. Chalet Reynard is a former refuge turned into a restaurant at the foot of a ski resort, at an altitude of, on the southern face of Mont Ventoux, in the department of Vaucluse, France. The station was created in February 1927 by. Access. Chalet Reynard is located at the intersection of the RD 974 road, connecting Bédoin to the summit of Mount Ventoux, and RD 164 joining Sault.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
The team flew from Bari on 12 August 1944 aboard an RAF Dakota, landing behind enemy lines in partisan-held territory. Despite these setbacks, Woods was instrumental in successful sabotage efforts targeting key road and rail lines prior to the Allied breakthrough into the Po Valley in April 1945. For his actions, he was awarded the Military Cross.

Geographic entities mentioned:
surface_form: Po Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
He has been teaching at Bar-Ilan University since 1992. Archaeology and academic career. He has participated in, and directed, numerous archaeological excavations in Israel, including at the following sites: Jerusalem, Hazor, Yoqneam, Tell Qasile, Beth-Shean, and since 1996, at Tell es-Safi/Gath. He is married to Adina (née Hartman), and they have three sons and four grandchildren.

Geographic entities mentioned:
surface_form: Yoqneam
instance_of: Mountain
countries: Israel
coordinates: lat: 32.6640988
lon: 35.1082661
They reached and camped at Tower Creek on July 25, 1871. The survey team spent three days traveling around Mount Washburn and along the western edge of the Yellowstone River in Hayden Valley to reach its source at Yellowstone Lake on July 28, 1871. It was here that Lt. Gustavus C. Doane replaced Captain Tyler as commander of the military escort.

Geographic entities mentioned:
surface_form: Mount Washburn
instance_of: Mountain
countries: United States
coordinates: lat: 44.7975
lon: -110.43333333333
surface_form: Hayden Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.6439
lon: -110.456
surface_form: Yellowstone Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.466666666667
lon: -110.36666666667
James Wood, writing of his 'Books of the Year' in &quot;The New Yorker&quot;, described it as a &quot;brief and brilliant book&quot; that he read &quot;with huge pleasure&quot;. In 2016 Narayan published &quot;Everyday Creativity: Singing Goddesses in the Himalayan Foothills&quot;, about women's traditions of singing in the Kangra Valley.

Geographic entities mentioned:
surface_form: Kangra Valley
instance_of: Valley
countries: India
coordinates: lat: 32.08638888888889
lon: 76.25333333333333
The ring of hills that include Tabernacle Hill is approximately 1 km in diameter, and it sits somewhat off center to the southeast of a lava field approximately 5 km in diameter. Geology. Tabernacle Hill is part of the Black Rock Desert volcanic field. The lava of Tabernacle Hill is basalt and tuff of late Pleistocene age.

Geographic entities mentioned:
surface_form: black rock
instance_of: Mountain
countries: United States
coordinates: lat: 39.343055555556
lon: -79.110555555556
surface_form: tabernacle hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778
Tabernacle Hill. Tabernacle Hill is a butte formed by a dormant volcano in the west-central portion of Utah, United States. Description. The butte is located in the Sevier Desert in the Pahvant Valley southwest of Fillmore.

Geographic entities mentioned:
surface_form: tabernacle hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778
Description. The butte is located in the Sevier Desert in the Pahvant Valley southwest of Fillmore. The ring of hills that include Tabernacle Hill is approximately 1 km in diameter, and it sits somewhat off center to the southeast of a lava field approximately 5 km in diameter. Geology. Tabernacle Hill is part of the Black Rock Desert volcanic field.

Geographic entities mentioned:
surface_form: tabernacle hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778
Geology. Tabernacle Hill is part of the Black Rock Desert volcanic field. The lava of Tabernacle Hill is basalt and tuff of late Pleistocene age. The basalt erupted from the vent at Tabernacle Hill into Lake Bonneville when it was at the Provo level. Tabernacle Hill lies south of The Cinders, the youngest lava flow in Utah.

Geographic entities mentioned:
surface_form: tabernacle hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778
The lava of Tabernacle Hill is basalt and tuff of late Pleistocene age. The basalt erupted from the vent at Tabernacle Hill into Lake Bonneville when it was at the Provo level. Tabernacle Hill lies south of The Cinders, the youngest lava flow in Utah. The basalt of the Cinders and Tabernacle hill was first mapped by geologists Grove Karl Gilbert and Israel Russell in 1890 (see map below).

Geographic entities mentioned:
surface_form: tabernacle hill
instance_of: Mountain
countries: United States
coordinates: lat: 38.91
lon: -112.53027777778