Sarmila/GeoWiki-Features huggingface dataset:
La Garma A. the entrance to the cave system leads through La Garma A, as the only entrance into the cave system. It lies at above sea level and has an extensive stratigraphy, containing Aurignacian, Gravettian, Solutrean, and Magdalenian layers, as well as Mesolithic, Neolithic, Chalcolithic, Bronze Age, and Middle Ages layers. La Garma B.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
It lies at above sea level and has an extensive stratigraphy, containing Aurignacian, Gravettian, Solutrean, and Magdalenian layers, as well as Mesolithic, Neolithic, Chalcolithic, Bronze Age, and Middle Ages layers. La Garma B. La Garma B lies at above sea level and is situated between La Garma A and the Lower Gallery. La Garma B contains Chacolithic and Bronze Age layers.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
It lies at above sea level and has an extensive stratigraphy, containing Aurignacian, Gravettian, Solutrean, and Magdalenian layers, as well as Mesolithic, Neolithic, Chalcolithic, Bronze Age, and Middle Ages layers. La Garma B. La Garma B lies at above sea level and is situated between La Garma A and the Lower Gallery. La Garma B contains Chacolithic and Bronze Age layers.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
La Garma B. La Garma B lies at above sea level and is situated between La Garma A and the Lower Gallery. La Garma B contains Chacolithic and Bronze Age layers. La Garma B leads into the Intermediate Gallery, which contains Paleolithic cave paintings and deposits. Lower Gallery. The Lower Gallery of La Garma is situated at above sea level and is around in length. It was discovered in November 1995.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
La Garma B leads into the Intermediate Gallery, which contains Paleolithic cave paintings and deposits. Lower Gallery. The Lower Gallery of La Garma is situated at above sea level and is around in length. It was discovered in November 1995. Its original entrance was sealed during the Pleistocene by a rockslide about 16,000 years ago, preserving the cave floor in a pristine manner.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
The Middle Magdalenian paintings and remains of residential structures were found near the entrance to this section of the cave. A vertical bison representation from Zone IX was directly dated to around 16,512-17,238 BP. La Garma C and D. La Garma C and D are situated above La Garma A and contain burials from the Chacolithic. El Truchiro Cave.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
Other portable art elements found at the cave complex include perforated batons&quot;, &quot;, decorated stone plaquettes, and undecorated pendants. Mortuary practices. During the Neolithic, La Garma was less and less used as a residential site. From the Chalcolithic through the Bronze Age, it was used primarily as a collective burial site.

Geographic entities mentioned:
surface_form: la garma
instance_of: Mountain
countries: Spain
coordinates: lat: 43.43055556
lon: -3.66583333
Tyrrau Mawr. Tyrrau Mawr or Craig-las is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the west of Cyfrwy, and can be climbed by taking a west bearing from the Pony Path at Rhiw Gwredydd. Its north face is a crag, known as Craig-las. Below the crags lies Llyn Cregennen with its small island.

Geographic entities mentioned:
surface_form: Cadair Idris
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.699827777778
lon: -3.9086944444444
surface_form: tyrrau mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.70349
lon: -3.95941
surface_form: craig-las
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.70349
lon: -3.95941
Its north face is a crag, known as Craig-las. Below the crags lies Llyn Cregennen with its small island. The reflection of Craig-las from this lake is one of the famous images associated with Snowdonia. The summit is grassy and marked by a few stones. To the east of the summit lies the large ancient cairn, Carnedd Lwyd. It is often climbed in combination with Craig-y-llyn.

Geographic entities mentioned:
surface_form: Craig-y-llyn
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.689102
lon: -3.976073
Tyrrau Mawr. Tyrrau Mawr or Craig-las is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the west of Cyfrwy, and can be climbed by taking a west bearing from the Pony Path at Rhiw Gwredydd. Its north face is a crag, known as Craig-las. Below the crags lies Llyn Cregennen with its small island.

Geographic entities mentioned:
surface_form: tyrrau mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.70349
lon: -3.95941
Tyrrau Mawr. Tyrrau Mawr or Craig-las is a subsidiary summit of Cadair Idris in the Snowdonia National Park, in Gwynedd, northwest Wales. It lies to the west of Cyfrwy, and can be climbed by taking a west bearing from the Pony Path at Rhiw Gwredydd. Its north face is a crag, known as Craig-las. Below the crags lies Llyn Cregennen with its small island.

Geographic entities mentioned:
surface_form: craig-las
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.70349
lon: -3.95941
Its north face is a crag, known as Craig-las. Below the crags lies Llyn Cregennen with its small island. The reflection of Craig-las from this lake is one of the famous images associated with Snowdonia. The summit is grassy and marked by a few stones. To the east of the summit lies the large ancient cairn, Carnedd Lwyd. It is often climbed in combination with Craig-y-llyn.

Geographic entities mentioned:
surface_form: craig-las
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.70349
lon: -3.95941
A flood watch was also issued for parts of Guam and the Northern Marianas. In the Philippines, PAGASA raised Tropical Cyclone Wind Signals in several areas, while PHIVOLCS issued warnings about potential lahar flows from the Taal, Pinatubo, and Mayon volcanoes.

Geographic entities mentioned:
surface_form: Mayon
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.256666666667
lon: 123.685
PAGASA issued gale warnings for the eastern and southern seaboards of Luzon and eastern Visayas and also warned of storm surges with a height of up to affecting Cagayan Valley, Central Luzon, Calabarzon, Mimaropa, the Bicol Region and Eastern Visayas. PHIVOLCS warned of possible lahar flows from the Taal, Pinatubo, and Mayon volcanoes.

Geographic entities mentioned:
surface_form: Mayon
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.256666666667
lon: 123.685
Sub-Balkan Valley. The Sub-Balkan Valleys () are row of 11 valleys running from the Bulgarian border with Serbia east to the Black Sea. They are separating the Balkan Mountains from a chain of other mountains known as Srednogorie which includes Vitosha and Sredna Gora. There is great abundance of mineral waters. They are divided into two parts: Western (higher) and Eastern (lower).

Geographic entities mentioned:
surface_form: Vitosha
instance_of: Mountain
countries: Bulgaria
coordinates: lat: 42.566666666667
lon: 23.283333333333
Rivière à Idas. The rivière à Idas (&quot;English: Idas River&quot;) is a tributary of the north bank of the upper part of the Bras du Nord-Ouest, flowing entirely in the town of Baie-Saint-Paul, in the Charlevoix Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: bras du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.562777777778
lon: -70.995555555556
surface_form: rivière à idas
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.403333333333336
lon: -70.63583333333334
surface_form: bras du nord-ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.446666111111114
lon: -70.50722194444444
The water level of the river varies with the seasons and the precipitation; the spring flood generally occurs in April. Geography. From the mouth of the Idas river, the current descends on following the course of the Bras du Nord-Ouest; then on with a drop of following the course of the rivière du Gouffre which flows into Baie-Saint-Paul in the St. Lawrence River. Toponymy.

Geographic entities mentioned:
surface_form: bras du nord
instance_of: Watercourse
countries: Canada
coordinates: lat: 48.562777777778
lon: -70.995555555556
surface_form: bras du nord-ouest
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.446666111111114
lon: -70.50722194444444
Rivière à Idas. The rivière à Idas (&quot;English: Idas River&quot;) is a tributary of the north bank of the upper part of the Bras du Nord-Ouest, flowing entirely in the town of Baie-Saint-Paul, in the Charlevoix Regional County Municipality, in the administrative region of Capitale-Nationale, in the province of Quebec, in Canada.

Geographic entities mentioned:
surface_form: rivière à idas
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.403333333333336
lon: -70.63583333333334
Lawrence River. Toponymy. This toponymic designation appears on the map &quot;Domaine forestier du Séminaire de Québec&quot;, 1955–01. It also appears on the cards of the Ruisseau du Pied du Mont number 309 and Lac des Fourches number 308 clubs of the Séminaire de Québec. This toponym evokes the memory of a hunter who once frequented the area.

Geographic entities mentioned:
surface_form: ruisseau du pied du mont
instance_of: Watercourse
countries: Canada
coordinates: lat: 47.484999
lon: -70.623332
Sir Henry Fane, of Basildon, KB, (1650–1705/06), by his wife Elizabeth, daughter of Thomas Southcott of Exeter. Family. His elder brother's death made him eventual heir to the Bourchier estates; the manors of Lough Gur and Glenogra in county Limerick and of Clare, near Tandragee, in county Armagh; to the Fane estate at Basildon in Berkshire; and to the Southcott estate at Calwoodley in Devon.

Geographic entities mentioned:
surface_form: Lough Gur
instance_of: Lake
countries: Ireland
coordinates: lat: 52.516380555556
lon: -8.5332777777778
Political career. Fane was appointed Deputy Lieutenant (DL) for Berkshire, 21 September 1715. He was Member of the Irish Parliament (MP) for Killybegs in county Donegal, a seat controlled by the Conygham family, from 1715 to 1719. On 22 April 1718 he was created Baron of Loughguyre, in the county of Limerick, and Viscount Fane, both in the Peerage of Ireland, and number 264 on the roll.

Geographic entities mentioned:
surface_form: Loughguyre
instance_of: Lake
countries: Ireland
coordinates: lat: 52.516380555556
lon: -8.5332777777778
The river reaches a length of. The Laudach is a left and the main tributary of the Alm. The longer Äußere (outer) Laudach is the output of the Laudachsee in Gmunden. It passes the areas of the municipalities Sankt Konrad, Gschwandt, Kirchham and Vorchdorf from the south. The smaller tributary, the Innere (inner) or Dürre Laudach, has its source in Kirchham.

Geographic entities mentioned:
surface_form: Laudachsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.878888888889
lon: 13.852777777778
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
Laudach. Laudach is a river in the Austrian state of Upper Austria. The river reaches a length of. The Laudach is a left and the main tributary of the Alm. The longer Äußere (outer) Laudach is the output of the Laudachsee in Gmunden. It passes the areas of the municipalities Sankt Konrad, Gschwandt, Kirchham and Vorchdorf from the south.

Geographic entities mentioned:
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
The Laudach is a left and the main tributary of the Alm. The longer Äußere (outer) Laudach is the output of the Laudachsee in Gmunden. It passes the areas of the municipalities Sankt Konrad, Gschwandt, Kirchham and Vorchdorf from the south. The smaller tributary, the Innere (inner) or Dürre Laudach, has its source in Kirchham. It is formed by two sources, the Platzbach and the Edlbach.

Geographic entities mentioned:
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
The smaller tributary, the Innere (inner) or Dürre Laudach, has its source in Kirchham. It is formed by two sources, the Platzbach and the Edlbach. The water stems from three hills (Wiesberg, Hacklberg and Feichtenberghills) that lay like a horseshoe around the district Hagenmühle of Kirchham. This right tributary discharges from the south into the Äußere Laudach north of Vorchdorf.

Geographic entities mentioned:
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
surface_form: äußere laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
This right tributary discharges from the south into the Äußere Laudach north of Vorchdorf. The Laudach empties into the Alm about after the junction of the Äußere and Innere Laudach, several times interrupted by small weirs, in the southern area of the city of Bad Wimsbach. There are a couple of artificial ponds along the Laudach.

Geographic entities mentioned:
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
This right tributary discharges from the south into the Äußere Laudach north of Vorchdorf. The Laudach empties into the Alm about after the junction of the Äußere and Innere Laudach, several times interrupted by small weirs, in the southern area of the city of Bad Wimsbach. There are a couple of artificial ponds along the Laudach.

Geographic entities mentioned:
surface_form: laudach
instance_of: Watercourse
countries: Austria
coordinates: lat: 48.0392
lon: 13.9208
Farming and fishery are the main sources of livelihood for the residents. However, Toubul is also one of the most affected villages due to the hydroelectric power generation plant from Loktak lake, which happens to be the biggest freshwater lake in north-east India. The village is located at 24.6213°N 93.7934°E.

Geographic entities mentioned:
surface_form: Loktak lake
instance_of: Lake
countries: India
coordinates: lat: 24.55
lon: 93.783333333333
Lying on the transition zone between the Central Asian steppes and the Iranian Plateau, the region was characterized by a mixture of sedentary, urban populations in the fertile river valleys, alongside nomad tribes engaged in pastoralism, which is singled out as the region's main source of wealth by medieval geographers.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
It lies in Benton and Polk counties. Route description. OR 223 begins at an intersection with U.S. Route 20 in Wren northwest of Philomath. It continues north from there, through the western edge of the Willamette Valley. In the town of Bridgeport, it intersects with OR 194. The only major city on the route is Dallas, Oregon; north of Dallas, it ends at an intersection with OR 22. Covered bridge.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Lake Văcărești. Lake Văcărești is a lake in the south of Bucharest, Sector 4. The lake has a surface of. It is now part of the &quot;Văcărești Nature Park&quot;, a protected zone of nature. Over 100 species of wild birds and animals live in this area. The area is nicknamed &quot;Bucharest Delta&quot;. History.

Geographic entities mentioned:
surface_form: lake văcărești
instance_of: Lake
countries: Romania
coordinates: lat: 44.401411
lon: 26.13123889
Rágesjávri. Rágesjávri is a lake in Kautokeino Municipality in Finnmark county, Norway. The lake lies on the Finnmarksvidda plateau, about northeast of the village of Máze and about south of the large lake of Iešjávri.

Geographic entities mentioned:
surface_form: Finnmarksvidda
instance_of: Plateau
countries: Norway
coordinates: lat: 69.31666667
lon: 23.81666667
surface_form: Iešjávri
instance_of: Lake
countries: Norway
coordinates: lat: 69.6654
lon: 24.209
Rágesjávri. Rágesjávri is a lake in Kautokeino Municipality in Finnmark county, Norway. The lake lies on the Finnmarksvidda plateau, about northeast of the village of Máze and about south of the large lake of Iešjávri.

Geographic entities mentioned:
surface_form: rágesjávri
instance_of: Lake
countries: Norway
coordinates: lat: 69.5411
lon: 24.171
Dunseverick. Dunseverick () is a hamlet near the Giant's Causeway in County Antrim, Northern Ireland. The name is also the alias for the townland of Feigh. It is most notable for Dunseverick Castle.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
By 09:00 the entire division of Lorge was on the right side of the Limmat with 8,000 men and a total of 26 guns. Masséna aimed to prevent the Russian right wing under Durasov joining their left at Zürich, and now quickly sent Bontemps with his brigade to gain the slopes of the mountains of the Glatt and cut the communications between Regensberg and Zürich.

Geographic entities mentioned:
surface_form: Glatt
instance_of: Valley
countries: Switzerland
coordinates: lat: 47.416666666667
lon: 8.5666666666667
His right under Drouet drove the Russians from Wollishofen, but were soon counter-attacked by Gorchakov's six battalions, assisted by William's flotilla of gunboats, and pushed back towards the Uetli. Gorchakov however, not satisfied with merely repulsing the enemy attack, pursued the French to the Uetliberg and succeeded in capturing some batteries.

Geographic entities mentioned:
surface_form: Uetliberg
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.349722222222
lon: 8.4902777777778
Encouraged by the defeat of Hotze, Molitor's men drove Jellacic's Austrians back towards Walenstadt. On the 25th, Linken's column appeared in the Sernftal, surprising and capturing two battalions of the French 76th Line Infantry. Linken's troops, which consisted of Joseph Anton von Simbschen's brigade, soon found themselves opposed by a battalion of the 84th Line.

Geographic entities mentioned:
surface_form: Sernftal
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.961
lon: 9.171
Description. The three glacial diamictite-bearing units of the Huronian are, from the oldest to youngest, the Ramsay Lake, Bruce, and Gowganda formations. Although there are other glacial deposits recognized throughout the world at this time, the Huronian is restricted to the region north of Lake Huron, between Sault Ste. Marie, Ontario, and Rouyn-Noranda, Quebec.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Mickey's Spire. Mickey's Spire, at above sea level is the fourth highest peak in the Sawtooth Range of Idaho. The peak is located in the Sawtooth Wilderness of Sawtooth National Recreation Area in Custer County. The peak is located south-southwest of Thompson Peak, its line parent. It is the 206th highest peak in Idaho.

Geographic entities mentioned:
surface_form: the sawtooth
instance_of: Mountain
countries: United States
coordinates: lat: 39.590833333333
lon: -105.66416666667
surface_form: mickey's spire
instance_of: Mountain
countries: United States
coordinates: lat: 44.1384
lon: -115.012
Mickey's Spire. Mickey's Spire, at above sea level is the fourth highest peak in the Sawtooth Range of Idaho. The peak is located in the Sawtooth Wilderness of Sawtooth National Recreation Area in Custer County. The peak is located south-southwest of Thompson Peak, its line parent. It is the 206th highest peak in Idaho.

Geographic entities mentioned:
surface_form: the sawtooth
instance_of: Mountain
countries: United States
coordinates: lat: 39.590833333333
lon: -105.66416666667
Mickey's Spire. Mickey's Spire, at above sea level is the fourth highest peak in the Sawtooth Range of Idaho. The peak is located in the Sawtooth Wilderness of Sawtooth National Recreation Area in Custer County. The peak is located south-southwest of Thompson Peak, its line parent. It is the 206th highest peak in Idaho.

Geographic entities mentioned:
surface_form: thompson peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.141666666667
lon: -115.01
surface_form: thompson peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.6443
lon: -111.812
surface_form: thompson peak
instance_of: Mountain
countries: United States
coordinates: lat: 41.0005
lon: -123.048
surface_form: thompson peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.261388888889
lon: -120.55777777778
Mickey's Spire. Mickey's Spire, at above sea level is the fourth highest peak in the Sawtooth Range of Idaho. The peak is located in the Sawtooth Wilderness of Sawtooth National Recreation Area in Custer County. The peak is located south-southwest of Thompson Peak, its line parent. It is the 206th highest peak in Idaho.

Geographic entities mentioned:
surface_form: mickey's spire
instance_of: Mountain
countries: United States
coordinates: lat: 44.1384
lon: -115.012
In the Late Cretaceous, at the end of the Maastrichtian stage, near Mount Rushmore in South Dakota (specifically Bone Butte), &quot;Anatotitan&quot; and &quot;Triceratops&quot; browse on a rolling grassland bordered by tropical jungle, while &quot;Ornithomimus&quot; peck at roots and other plants in the area.

Geographic entities mentioned:
surface_form: Mount Rushmore
instance_of: Mountain
countries: United States
coordinates: lat: 43.878947222222
lon: -103.459825
Moolock Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher neighbor is line parent Bessemer Mountain, to the northeast, and Green Mountain is 2.5 miles to the southwest. Precipitation runoff from this mountain drains into tributaries of the North and Middle Forks of the Snoqualmie River.

Geographic entities mentioned:
surface_form: Bessemer Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.56
lon: -121.60805555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3053
lon: -105.3
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5175
lon: -121.67305555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.563333333333
lon: -122.80694444444
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.700833333333
lon: -105.17805555556
Moolock Mountain. Moolock Mountain is a summit located in King County of Washington state. It is situated at the western edge of the Cascade Range, on land managed by Mount Baker-Snoqualmie National Forest. Moolock Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: moolock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.547367
lon: -121.641897
Moolock Mountain. Moolock Mountain is a summit located in King County of Washington state. It is situated at the western edge of the Cascade Range, on land managed by Mount Baker-Snoqualmie National Forest. Moolock Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
surface_form: mount baker
instance_of: Mountain
countries: United States
coordinates: lat: 48.7773426
lon: -121.8132008
Moolock Mountain. Moolock Mountain is a summit located in King County of Washington state. It is situated at the western edge of the Cascade Range, on land managed by Mount Baker-Snoqualmie National Forest. Moolock Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation.

Geographic entities mentioned:
surface_form: moolock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.547367
lon: -121.641897
It is situated at the western edge of the Cascade Range, on land managed by Mount Baker-Snoqualmie National Forest. Moolock Mountain is more notable for its large, steep rise above local terrain than for its absolute elevation. The nearest higher neighbor is line parent Bessemer Mountain, to the northeast, and Green Mountain is 2.5 miles to the southwest.

Geographic entities mentioned:
surface_form: moolock mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.547367
lon: -121.641897
Kwoiek Needle. Kwoiek Needle is a mountain summit located in the Lillooet Ranges of southwestern British Columbia, Canada. It is situated southwest of Lytton, and its nearest higher peak is Kumkan Peak, to the west. The mountain was named in association with Kwoiek Creek, Kwoiek Lake, and Kwoiek Peak.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: kwoiek needle
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0847
lon: -121.8076
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Kwoiek Needle. Kwoiek Needle is a mountain summit located in the Lillooet Ranges of southwestern British Columbia, Canada. It is situated southwest of Lytton, and its nearest higher peak is Kumkan Peak, to the west. The mountain was named in association with Kwoiek Creek, Kwoiek Lake, and Kwoiek Peak.

Geographic entities mentioned:
surface_form: kumkan peak
instance_of: Mountain
countries: Canada
coordinates: lat: 50.08301
lon: -121.93593
Kwoiek Needle. Kwoiek Needle is a mountain summit located in the Lillooet Ranges of southwestern British Columbia, Canada. It is situated southwest of Lytton, and its nearest higher peak is Kumkan Peak, to the west. The mountain was named in association with Kwoiek Creek, Kwoiek Lake, and Kwoiek Peak.

Geographic entities mentioned:
surface_form: kwoiek needle
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0847
lon: -121.8076
Climate. Based on the Köppen climate classification, Kwoiek Needle is located in a subarctic climate zone of western North America. Most weather fronts originate in the Pacific Ocean, and travel east toward the Coast Mountains where they are forced upward by the range (Orographic lift), causing them to drop their moisture in the form of rain or snowfall.

Geographic entities mentioned:
surface_form: kwoiek needle
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0847
lon: -121.8076
As a result, the Coast Mountains experience high precipitation, especially during the winter months in the form of snowfall. Winter temperatures can drop below −20 °C with wind chill factors below −30 °C. The months July through September offer the most favorable weather for climbing Kwoiek Needle.

Geographic entities mentioned:
surface_form: kwoiek needle
instance_of: Mountain
countries: Canada
coordinates: lat: 50.0847
lon: -121.8076
It is situated southwest of Lytton, and its nearest higher peak is Kumkan Peak, to the west. The mountain was named in association with Kwoiek Creek, Kwoiek Lake, and Kwoiek Peak. &quot;Kwoiek&quot; is a Thompson Indian word meaning &quot;gouged out,&quot; referring to a large chunk missing from the canyon wall.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
It was among the first fossils found by the American paleontologist Charles D. Walcott in 1909. He described it in 1912 and named it after two mountains near the discovery site – Wapta Mountain and Mount Field. Although it bears a remarkable resemblance to modern crustaceans, its taxonomic affinities were long unclear.

Geographic entities mentioned:
surface_form: Wapta Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4513
lon: -116.478
A formal description for the species was published by Walcott in 1912. The species was named after the two mountains connected by the Fossil Ridge containing the Burgess Shale locality, Wapta Mountain and Mount Field of Yoho National Park, British Columbia, Canada.

Geographic entities mentioned:
surface_form: Wapta Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4513
lon: -116.478
Geography. The town is located on the northern shore of the Ottawa River, the Rivière des Mille Îles, and the Lake of Two Mountains, all of which join the Saint Lawrence River, to its south, near the West Island of Montreal Island. Pointe-Calumet is accessible from the Montreal area and points east from Quebec Autoroute 640, which runs from Laval, Saint-Eustache, Terrebonne, and Repentigny.

Geographic entities mentioned:
surface_form: Rivière des Mille Îles
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.69916666666667
lon: -73.52916666666667
surface_form: Lake of Two Mountains
instance_of: Lake
countries: Canada
coordinates: lat: 45.45
lon: -74.016666666667
In Uttarakhand, the Byangsi area extends from Budi () in the south to Kuti village () in the north. The area is located in Dharchula and Munsiyari tehsils of the Pithoragarh district, and the majority of it is in the Kuthi valley near the Tibet and Nepal borders. Other villages of the area include Nabi, Gunji, Napalchyu, Rongkang, and Garbyang.

Geographic entities mentioned:
surface_form: Kuthi valley
instance_of: Valley
countries: India
coordinates: lat: 30.3064016
lon: 80.7557186
On the other hand, the East Antarctic Ice Sheet is far more stable and may only cause - of sea level rise from the current level of warming, which is a small fraction of the contained in the full ice sheet. Around, vulnerable locations like Wilkes Basin and Aurora Basin may collapse over a period of around 2,000 years, which would add up to to sea levels.

Geographic entities mentioned:
surface_form: Wilkes Basin
instance_of: Landform
coordinates: lat: -75
lon: 145
Collectively, these ice sheets have an average thickness of around, Even the Transantarctic Mountains are largely covered by ice, with only some mountain summits and the McMurdo Dry Valleys being ice-free in the present. Some coastal areas also have exposed bedrock that is not covered by ice. During the Late Cenozoic Ice Age, many of those areas had been covered by ice as well.

Geographic entities mentioned:
surface_form: McMurdo Dry Valleys
instance_of: Valley
coordinates: lat: -77.466666666667
lon: 162.51666666667
James Cathedral, which is the oldest Episcopal congregation in the city of Chicago. The Diocese of Chicago covers twenty-two counties located in the northern third of the state of Illinois, stretching from the shores of Lake Michigan on the east, to the banks of the Mississippi River on the west. Its northern boundary is the state of Wisconsin; the southernmost city is Watseka, Illinois. History.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
The police officer who made the stop searched the vehicle and found more than of marijuana. Way was arrested and released on bond the same day. On January 22, 2014, Way was a passenger in his vehicle when the driver ran a stop sign in the San Fernando Valley, California, and police discovered a loaded handgun in the car. Way was arrested immediately and taken to jail.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Description. Congo is a traditional name for the equatorial Middle Africa that lies between the Gulf of Guinea and the African Great Lakes. The basin begins in the highlands of the East African Rift system with input from the Chambeshi, the Uele and Ubangi rivers in the upper reaches and the Lualaba River draining wetlands in the middle reaches.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Geographic range. The greater short-horned lizard is the most widely distributed horned lizard in North America and occurs in the widest range of habitats: West into central Nevada, east into North and South Dakota, north to southern Saskatchewan and Alberta, and then south into eastern New Mexico to central Mexico, with a few pockets in Trans-Pecos Texas.

Geographic entities mentioned:
surface_form: Trans-Pecos
instance_of: Valley
countries: United States
coordinates: lat: 30.56
lon: -103.79
state of Michigan. long, it is the largest tributary of Little Traverse Bay in the northwest of the lower peninsula. Traverse Bay is on Lake Michigan. The river is formed as the outflow of Walloon Lake on the boundary between Charlevoix County and Emmet County, draining from the southeast end of the lake at near the community of Walloon Lake in Melrose Township.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Traverse Bay is on Lake Michigan. The river is formed as the outflow of Walloon Lake on the boundary between Charlevoix County and Emmet County, draining from the southeast end of the lake at near the community of Walloon Lake in Melrose Township. M-75 has its northern terminus in a junction with US 131 nearby.

Geographic entities mentioned:
surface_form: Walloon Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.285833333333
lon: -85.018333333333
In 1995, he became president of Exxon Yemen Inc. and Esso Exploration and Production Khorat Inc. In 1998, he became a vice president of Exxon Ventures (CIS) and president of Exxon Neftegas Limited with responsibility for Exxon's holdings in Russia and the Caspian Sea. He then entered Exxon into the Sakhalin-I consortium with Rosneft.

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
1979 Yugoslav Mount Everest expedition. The 1979 Yugoslav Mount Everest expedition () was the first successful summit of Mount Everest (8,848m) using the entirety of the West Ridge route (the West Ridge Direct) in the North Face of Everest. It was the seventh expedition in the Himalayas by the Yugoslav alpinist team, and their first and only ascent to the highest peak of Mount Everest.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The Archipelago Division was tasked with supporting the French towards Davidovo. As the Bulgarian retreat began on 8 September, the division crossed the trenches on 9 September, and advanced through Strumica to Plačkovica.

Geographic entities mentioned:
surface_form: Plačkovica
instance_of: Mountain
countries: North Macedonia
coordinates: lat: 41.766666666667
lon: 22.533333333333
Ghana is well endowed with water resources. The Volta River system basin, consisting of the Oti River, Daka River, Pru River, Sene River and Afram River as well as the White Volta and Black Volta rivers, covers 70% of Ghana's total land area. Another 22% of Ghana is covered by the southwestern river system watershed comprising the Bia River, Tano River, Ankobra River and Pra River.

Geographic entities mentioned:
surface_form: Bia River
instance_of: Watercourse
countries: Ivory Coast
Ghana
coordinates: lat: 6.0966666666667
lon: -3.095
Wind Creek Bethlehem. The Wind Creek Bethlehem, formerly Sands Casino Resort Bethlehem, is a casino hotel located in the Bethlehem Works development site in Bethlehem, Pennsylvania, in the Lehigh Valley region of eastern Pennsylvania. It is owned and operated by Wind Creek Hospitality, an entity of the Poarch Band of Creek Indians. History.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
History. It was first proposed to make the Ngiri triangle, the area between the Ubangi, Congo and Ngiri rivers, into a reserve in 1975, but the project could not be completed. The project was revived by the WWF in the context of Lake Tele - Lake Tumba landscape project, of which the Tumba-Ngiri-Maindombe wetland is the DRC portion. It was proposed that the new reserve should be IUCN category VI.

Geographic entities mentioned:
surface_form: Ngiri
instance_of: Watercourse
countries: Democratic Republic of the Congo
coordinates: lat: 0.31694444444444
lon: 17.936111111111
History. It was first proposed to make the Ngiri triangle, the area between the Ubangi, Congo and Ngiri rivers, into a reserve in 1975, but the project could not be completed. The project was revived by the WWF in the context of Lake Tele - Lake Tumba landscape project, of which the Tumba-Ngiri-Maindombe wetland is the DRC portion. It was proposed that the new reserve should be IUCN category VI.

Geographic entities mentioned:
surface_form: Lake Tele
instance_of: Lake
countries: Republic of the Congo
coordinates: lat: 1.3333333333333
lon: 17.15
surface_form: Lake Tumba
instance_of: Lake
countries: Democratic Republic of the Congo
coordinates: lat: -0.83333333333333
lon: 18
Despite this, a large number of households worked in private industry; scholars have estimated that 10% of Tang China's population lived in cities. The height of Tang prosperity came during the Kaiyuan Era of Emperor Xuanzong of Tang, who expanded Tang influence westward to the Aral Sea.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Leirvogsvatn. Leirvogsvatn () is a small lake, located about northeast of Reykjavík, Iceland. It lies along Route 36. Located at above sea level, it has an area of with a maximum depth of. Fed by the, the lake is the subject of a legend in the form of a horse-shaped monster. The lake is known to contain populations of &quot;Gasterosteus islandicus&quot;.

Geographic entities mentioned:
surface_form: leirvogsvatn
instance_of: Lake
countries: Iceland
coordinates: lat: 64.19666667
lon: -21.45388889
He used this time in exile to travel and to set up a private network to create periodical publications to oppose the anticlerical press coming from his archdiocese. He was later allowed to return and carried out his duties, such as aiding victims of two cholera epidemics and the 1861 eruption of Mount Vesuvius.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
In 1855 he refused the pope's offer to become the newest Archbishop of Bologna. Sforza distinguished himself in the two cholera epidemics in 1854-55 and 1873 in tending to the ill while tending to victims of the 1861 eruption of Mount Vesuvius. Sforza became titled &quot;Borromeo redivivo&quot; since people associated his pastoral qualities as reminiscent to those of Saint Carlo Borromeo.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556
He returned to Naples on 30 November 1860 with the aid of Saint Ludovico of Casoria. Sforza was exiled once again on 31 July 1861 until 6 December 1866. During his exile he lived in Genoa and Marseille (where he resided with the bishop Patrice-François-Marie Cruice) for a time before moving to Hyères and Civitavecchia before settling in Rome.

Geographic entities mentioned:
surface_form: Hyères
instance_of: Mountain
countries: France
coordinates: lat: 43.118888888889
lon: 6.1286111111111
Snowshoe Lake (Cripple Creek, Ontario). Snowshoe Lake is a lake in the Lake Huron drainage basin in Kearney, Almaguin Highlands, Parry Sound, Ontario, Canada. The lake is east of the community of Ravenscroft, just south of the access road to Rain Lake in Algonquin Provincial Park, and west of the park boundary. It is about long and wide, and lies at an elevation of.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5617
lon: -78.8036
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7317
lon: -80.1856
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5753
lon: -95.1192
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0689
lon: -88.8917
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1356
lon: -76.9278
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4417
lon: -77.8686
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7992
lon: -79.8253
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5886
lon: -79.0361
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.9803
lon: -79.9083
It is about long and wide, and lies at an elevation of. The primary inflow is an unnamed creek from Ink Lake, and the primary outflow is an unnamed creek to Cripple Lake, which flows via Cripple Creek, the Big East River, the Muskoka River and the Moon and Musquash rivers into Lake Huron. A second Snowshoe Lake in the Big East River system, Snowshoe Lake (West Harry Lake, Ontario), lies southeast.

Geographic entities mentioned:
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5617
lon: -78.8036
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5617
lon: -78.8036
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7317
lon: -80.1856
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7317
lon: -80.1856
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5753
lon: -95.1192
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5753
lon: -95.1192
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0689
lon: -88.8917
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0689
lon: -88.8917
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1356
lon: -76.9278
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1356
lon: -76.9278
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4417
lon: -77.8686
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4417
lon: -77.8686
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7992
lon: -79.8253
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7992
lon: -79.8253
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5886
lon: -79.0361
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5886
lon: -79.0361
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.9803
lon: -79.9083
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.9803
lon: -79.9083
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Snowshoe Lake (Cripple Creek, Ontario). Snowshoe Lake is a lake in the Lake Huron drainage basin in Kearney, Almaguin Highlands, Parry Sound, Ontario, Canada. The lake is east of the community of Ravenscroft, just south of the access road to Rain Lake in Algonquin Provincial Park, and west of the park boundary. It is about long and wide, and lies at an elevation of.

Geographic entities mentioned:
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5617
lon: -78.8036
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7317
lon: -80.1856
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.5753
lon: -95.1192
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0689
lon: -88.8917
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1356
lon: -76.9278
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.4417
lon: -77.8686
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.7992
lon: -79.8253
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.5886
lon: -79.0361
surface_form: snowshoe lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.9803
lon: -79.9083
It is about long and wide, and lies at an elevation of. The primary inflow is an unnamed creek from Ink Lake, and the primary outflow is an unnamed creek to Cripple Lake, which flows via Cripple Creek, the Big East River, the Muskoka River and the Moon and Musquash rivers into Lake Huron. A second Snowshoe Lake in the Big East River system, Snowshoe Lake (West Harry Lake, Ontario), lies southeast.

Geographic entities mentioned:
surface_form: musquash
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.9594
lon: -79.8811
surface_form: east river
instance_of: Watercourse
countries: Canada
coordinates: lat: 44.5529
lon: -62.3032
Rush Lake (Pakistan). Rush Lake () is a high-altitude lake located in Nagar Valley, Gilgit-Baltistan, Pakistan near Rush Peak. At, Rush is one of the highest alpine lakes in the world. It is located about north of Miar Peak and Spantik (Golden Peak) in the Nagar Valley. It is one of the highest lakes in Pakistan and the 27th-highest lake in the world.

Geographic entities mentioned:
surface_form: Nagar Valley
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.4
lon: 73.8
surface_form: Rush Peak
instance_of: Mountain
countries: Pakistan
coordinates: lat: 36.170638888889
lon: 74.88975
surface_form: rush lake
instance_of: Lake
countries: Pakistan
coordinates: lat: 36.174491
lon: 74.88251