Sarmila/GeoWiki-Features huggingface dataset:
Mount Falconer. Mount Falconer () is a mountain, high, surmounting Lake Fryxell on the north wall of Taylor Valley, between Mount McLennan and Commonwealth Glacier in Antarctica. It was named by the Western Journey Party, led by Thomas Griffith Taylor, of the British Antarctic Expedition, 1910–13. Location. Mount Falconer is in the southeast of the Asgard Range.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
It was named by the Western Journey Party, led by Thomas Griffith Taylor, of the British Antarctic Expedition, 1910–13. Location. Mount Falconer is in the southeast of the Asgard Range. The Commonwealth Glacier forms to its north and flows east and then south into the Taylor Valley.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Location. Mount Falconer is in the southeast of the Asgard Range. The Commonwealth Glacier forms to its north and flows east and then south into the Taylor Valley. Lake Fryxell in the Taylor Valley is to the south of the mountain, and Canada Glacier flows southeast into Taylor Valley to the west of Mount Falconer. Mount McLennan is to the northwest. Perk Summit.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Huey Gully. A high, deeply incised gully between Mount Keohane and Mount Falconer in the north wall of Taylor Valley. Containing some glacial ice from Commonwealth Glacier, the gully provides meltwater to Huey Creek, which descends south to Lake Fryxell, Taylor Valley. Scholars Peak. A peak rising to high west of Mount Falconer.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Scholars Peak. A peak rising to high west of Mount Falconer. The peak stands at the southwest end of Tarn Valley and was named by New Zealand Geographic Board (NZGB) (1998) in association with the prominent universities for which nearby tarns are named. Tarn Valley.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Tarn Valley. An elevated ice-free valley, long, containing four tarns named after American universities, Yale, Harvard, Princeton, and Penn (Pennsylvania), located at the north side of lower Taylor Valley, north of Mount Falconer. This valley was visited in the 1965-66 field season by Victoria University of Wellington Antarctic Expedition (VUWAE) (Edward D. Ghent, leader) which named the tarns.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Ghent, leader) which named the tarns. The valley was named in association with the tarns by Advisory Committee on Antarctic Names (US-ACAN) in 1997. Princeton Tarn. A tarn at the northwest side of Mount Falconer and south of Penn Tarn in the southwest part of Tarn Valley. The feature is one of four tarns in the valley named after American universities by the VUWAE 1965-66. Penn Tarn.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
The feature is one of four tarns in the valley named after American universities by the VUWAE, 1965-66. Ghent Ridge. A ridge that parallels the south flank of Commonwealth Glacier, north of Mount Falconer. The VUWAE 1965-66, called this feature &quot;Smith Ridge,&quot; presumably after I. Smith, a member of the VUWAE field party, but that toponym is already in use for other features.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Ghent, leader of the 1965-66 VUWAE, later with the Department of Geology, University of Calgary, Alberta, Canada. Henderson Hill. An ice free summit northeast of Mount Falconer, rising to high on the north side of Taylor Valley. The name Henderson Hill appears in a 1968 report and geologic sketch map of the area prepared by the VUWAE, 1965-66, and is presumably named after Robert A.

Geographic entities mentioned:
surface_form: falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
surface_form: mount falconer
instance_of: Mountain
coordinates: lat: -77.5833
lon: 163.133
Brosno dragon. The Brosno Dragon, also known as &quot;Brosnya&quot; (Russian: Бросня), is a supposed lake monster which in Russian folklore is said to inhabit Lake Brosno near Andreapol in western Russia. It is described as resembling a dragon and is the subject of a number of regional legends, some which are said to date back to the 13th century. Theories.

Geographic entities mentioned:
surface_form: Lake Brosno
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 56.825555555556
lon: 31.941666666667
1997–2010: The Borough of Tewkesbury wards of Ashchurch, Bishop's Cleeve East, Bishop's Cleeve North, Bishop's Cleeve South, Brockworth Glebe, Brockworth Moorfield, Brockworth Westfield, Churchdown Brookfield, Churchdown Parton, Churchdown Pirton, Cleeve Hill, Coombe Hill, Crickley, De Winton, Dumbleton, Gotherington, Horsbere, Innsworth, Shurdington, Tewkesbury Mitton, Tewkesbury Newtown, Tewkesbury Prior's Park, Tewkesbury Town, Twyning, and Winchcombe, and the Borough of Cheltenham wards of Leckhampton with Up Hatherley, Prestbury, and Swindon.

Geographic entities mentioned:
surface_form: Cleeve Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.92
lon: -2.007
Between 1898 and 1909, the Borsdorf–Großbothen and Döbeln–Coswig sections were duplicated. Duplication was also later started between Großbothen and Döbeln, but only the Großbothen–Tanndorf section was completed because of the outbreak of the Second World War in 1939. One of the largest construction projects of the interwar period was the rebuilding of the bridge over the Elbe in Meißen.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
Castellfollit de la Roca. Castellfollit de la Roca () is a municipality in the &quot;comarca&quot; of Garrotxa, in the Province of Girona, Catalonia, Spain. The urban area is bordered by the confluence of the Fluvià and Toronell rivers, between which the town's basalt cliff rises. The basalt cliff. Castellfollit de la Roca is part of La Garrotxa Volcanic Zone Natural Park.

Geographic entities mentioned:
surface_form: Fluvià
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.0934
lon: 2.4591
A bulkhead was built along Mill Island's shore in the late 1890s. It was later connected to the uplands of nearby Bergen Beach, creating the continuous embankment between Mill and Paerdegat basins later used for the construction of the Belt Parkway. Most of the earliest filling operations along the island were private; the city government took over later.

Geographic entities mentioned:
surface_form: Paerdegat
instance_of: Landform
countries: United States
coordinates: lat: 40.6271
lon: -73.9077
There are also populations of white-tailed eagles at the reservoir. These do not migrate south for the winter, instead they stay at Lokka to feed on fish left by local fishermen. Lokka is connected to the Porttipahta Reservoir through the Vuotso Canal. Climate. Lokka has a Subarctic climate (Köppen: Dfc) with long, severely cold winters and short, mild summers.

Geographic entities mentioned:
surface_form: Porttipahta Reservoir
instance_of: Lake
countries: Finland
coordinates: lat: 68.116666666667
lon: 26.5
Ridge Hill (Massachusetts). Ridge Hill is a mountain in Dukes County, Massachusetts. It is on Martha's Vineyard, northeast of Chilmark in the Town of Chilmark. Abel Hill is located southwest and Peaked Hill is located west-northwest of Ridge Hill.

Geographic entities mentioned:
surface_form: Abel Hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.3515066
lon: -70.7086672
surface_form: ridge hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.3643
lon: -70.7053
surface_form: peaked hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.3582
lon: -70.7364
Ridge Hill (Massachusetts). Ridge Hill is a mountain in Dukes County, Massachusetts. It is on Martha's Vineyard, northeast of Chilmark in the Town of Chilmark. Abel Hill is located southwest and Peaked Hill is located west-northwest of Ridge Hill.

Geographic entities mentioned:
surface_form: ridge hill (massachusetts)
instance_of: Mountain
countries: United States
coordinates: lat: 41.3643
lon: -70.7053
Ridge Hill (Massachusetts). Ridge Hill is a mountain in Dukes County, Massachusetts. It is on Martha's Vineyard, northeast of Chilmark in the Town of Chilmark. Abel Hill is located southwest and Peaked Hill is located west-northwest of Ridge Hill.

Geographic entities mentioned:
surface_form: ridge hill
instance_of: Mountain
countries: United States
coordinates: lat: 41.3643
lon: -70.7053
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
As mentioned above, Michael Panaretos never mentions David, so he provides no help answering that question. More recently the truth of his fate was rediscovered: a marginal note written at Mount Athos records David died as a monk of Vatopedi monastery on 13 December 1212. But this evidence raises more questions than it answers, such as how he came to reside there.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
It is believed that the trappers who built Fort Bridger were aware of the well; however, its first published description appeared in an 1848 guidebook written by a W. Clayton, who accompanied the initial Mormon expedition that had settled the Salt Lake Valley in the previous year. Oil is comparatively plentiful in the immediate vicinity of the Young Oil Well.

Geographic entities mentioned:
surface_form: Salt Lake Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.6839
lon: -111.978
Ursprung Buam. Ursprung Buam is an Austrian folk music trio from Zillertal, Tyrol. One of the most popular touring groups in Austria, Ursprung Buam often tours Germany, many places across the European Union, as well as the Tirolean festival scene. They have had over twenty releases since 1998. Most of these albums have held strong positions on the Austrian popular music charts.

Geographic entities mentioned:
surface_form: Zillertal
instance_of: Valley
countries: Austria
coordinates: lat: 47.333333333333
lon: 11.866666666667
The old Lake Rotomakariri was only long. There were several other small ponds or lakes to the east of Lake Rotomakariri towards Mount Tarawera, with Hochstetter showing an unnamed one to the east and to the south east a Lake Rangarua Tapu. European accounts gave a lake to the east, the name Green Lake, which, as many have had the same name in the locality over time, is almost meaningless.

Geographic entities mentioned:
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.7958
lon: 167.396
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.284896
lon: 176.267218
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -29.264857
lon: -177.919092
European accounts gave a lake to the east, the name Green Lake, which, as many have had the same name in the locality over time, is almost meaningless. The present Green Lake to the east, occupying an explosion crater near the south-east shore of Lake Rotomahana did not exist prior to 1886.

Geographic entities mentioned:
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.7958
lon: 167.396
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -37.284896
lon: 176.267218
surface_form: green lake
instance_of: Lake
countries: New Zealand
coordinates: lat: -29.264857
lon: -177.919092
Lake Rotomakariri. Lake Rotomakariri (From Māori: ', meaning lake, and ', meaning cold) was a lake which formerly existed in the basin that is now occupied by Lake Rotomahana, in the Bay of Plenty region of New Zealand's North Island. The lake's name was in contrast to the nearby Lake Rotomahana, which prior to the 1886 eruption of Mount Tarawera, was a shallower warm water lake.

Geographic entities mentioned:
surface_form: mount tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
The eruption of Mount Tarawera initially destroyed Lake Rotomakariri and its lakeside village with the loss of 19 lives, though water entering the new crater gradually refilled Lake Rotomakariri after volcanic activity subsided.

Geographic entities mentioned:
surface_form: mount tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
This expansion has drowned the positions occupied by both the old and new Lake Rotomakariri, as the present Lake Rotomahana is above the old Lake Rotomahana according to one source, and according to another. Geography. The old Lake Rotomakariri had swampy surrounds and was to the east of the White Terrace and the old Lake Rotomahana, between Lake Rotomahana and Mount Tarawera.

Geographic entities mentioned:
surface_form: mount tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
The old Lake Rotomakariri was only long. There were several other small ponds or lakes to the east of Lake Rotomakariri towards Mount Tarawera, with Hochstetter showing an unnamed one to the east and to the south east a Lake Rangarua Tapu. European accounts gave a lake to the east, the name Green Lake, which, as many have had the same name in the locality over time, is almost meaningless.

Geographic entities mentioned:
surface_form: mount tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
The lake's name was in contrast to the nearby Lake Rotomahana, which prior to the 1886 eruption of Mount Tarawera, was a shallower warm water lake. Prior to this eruption, Lake Rotomakariri sat in a shallow basin surrounded by marshes, draining into Lake Tarawera by Awapurohe Creek and Rotomahana's outflow of Kaiwaka Stream.

Geographic entities mentioned:
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
It drained via a creek called into the Kaiwaka Stream. This stream drained mainly Lake Rotomahana and was quite swift, so canoes had to be poled up it from Lake Tarawera. It had a fall of in. On the north-eastern lake shore was the village of Waingōngongo. The old Lake Rotomakariri was only long.

Geographic entities mentioned:
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
The eruption accordingly likely both destroyed features, but could have covered them in eruptives which are meters thick. The depth of some of these eruptives is such that the present Lake Rotomahana has now no surface drainage to Lake Tarawera and is separated from it by a ridge rather than the former stream bed which all agree is buried by them.

Geographic entities mentioned:
surface_form: tarawera
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.229
lon: 176.498
Lake Rotomakariri. Lake Rotomakariri (From Māori: ', meaning lake, and ', meaning cold) was a lake which formerly existed in the basin that is now occupied by Lake Rotomahana, in the Bay of Plenty region of New Zealand's North Island. The lake's name was in contrast to the nearby Lake Rotomahana, which prior to the 1886 eruption of Mount Tarawera, was a shallower warm water lake.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
As water accumulated over the decade after the eruption, Lake Rotomakariri was absorbed by the larger Lake Rotomahana, which eventually rose to about above its pre-eruption level due to the previous outflow of the basin being blocked by ashfall. History. The Māori name Rotomakariri means cold water lake, and was first used by Hochstetter.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
High quality pictures of the then Lake Rotomahana and associated tourist attractions were widely available in Europe by 1875. The first Lake Rotomakariri was in a swampy vegetated location and the village of Waingōngongo on the lake shore was destroyed in the 1886 eruption with the loss of 19 lives.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
The first official survey was done in 1887 after the eruption and this mapping showed a new cold water lake, also called Rotomakariri well to the east of the previous lake, in a new Rotomahana crater. Pictures of this new and temporary Lake Rotomakariri in a rather desolate landscape of the fresh eruptives exist.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
In due course Lake Rotomahana expanded again to ten times its previous area to occupy much of a crater produced by the 1886 eruption. This expansion has drowned the positions occupied by both the old and new Lake Rotomakariri, as the present Lake Rotomahana is above the old Lake Rotomahana according to one source, and according to another. Geography.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
The shape of the lake varies from the original 1859 map in later versions of the same map, and it seems most likely that the old Lake Rotomakariri was an ovoid orientated north-south as this was how it was sketched in 1859 and immediately after the eruption. It drained via a creek called into the Kaiwaka Stream.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
The present Green Lake to the east, occupying an explosion crater near the south-east shore of Lake Rotomahana did not exist prior to 1886. After the eruption which totally destroyed the old lake, a new lake formed in the most western part of the new Rotomahana crater, and this larger lake was called during its roughly decade of existence, the new Lake Rotomakariri. Geology.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
Geology. The area of the lake and the old Lake Rotomahana were volcanic as part of the Ōkataina Caldera and occupied an area that later became a vent of the 1886 eruption. There were some sinter cones near the lake. As the deepest part of the post eruption crater (and lake) is where the old Lake Rotomakariri was, part of the vent is likely to have been under it.

Geographic entities mentioned:
surface_form: lake rotomakariri
instance_of: Mountain
countries: New Zealand
coordinates: lat: -38.26
lon: 176.445
Areas of Outstanding Natural Beauty. Five Areas of Outstanding Natural Beauty (AONB) have been designated in Wales, one of which, the Wye Valley AONB, straddles the Anglo-Welsh border. The Gower () is a peninsula on the south west coast of Wales, on the north side of the Bristol Channel in the southwest of the historic county of Glamorgan.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
The AONB covers around, about a third of the county, making it Wales' largest AONB. The Wye Valley AONB (), designated in 1971, is an internationally important protected landscape straddling the border between England and Wales. It is one of the most dramatic and scenic landscape areas in southern Britain. The River Wye () is the fifth-longest river in the United Kingdom.

Geographic entities mentioned:
surface_form: Wye Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.69255
lon: -2.66283
Tropheus moorii. &quot;Tropheus moorii&quot; (blunthead cichlid) is a species of cichlid endemic to Lake Tanganyika in Africa. Over 40 different color morphs of this species are dispersed throughout the lake, ranging from dark green to flame red and yellow. They mostly feed on filamentous algae on the rocky shallows they inhabit. &quot;T.

Geographic entities mentioned:
surface_form: Lake Tanganyika
instance_of: Lake
countries: Tanzania
Democratic Republic of the Congo
Burundi
Zambia
coordinates: lat: -6.1
lon: 29.5
After conquering his enemies he would travel to Jerusalem and relinquish his power on the Mount of Olives. The Last Emperor was further developed in the writings of Adso of Montier-en-Der, whose &quot;Libellus de Antichristo&quot; (ca.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Bochica. Bochica (also alluded to as Nemquetaha, Nemqueteba and Sadigua) is a mythical figure in the religion of the Muisca, who inhabited the &quot;Altiplano Cundiboyacense&quot; before the Spanish invasion by conquistadors in the central Andean highlands of present-day Colombia. There is little documentation concerning Bochica, who was mentioned by name in records from 1563 from Ubaque.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
The sanjak was centered in Lajjun and later Jenin. Its territory consisted of the part of northern Palestine spanning the Jezreel Valley (then known as 'Marj ibn Amir'), Mount Carmel, and the coastland between Haifa and Atlit. From its establishment through the late 17th century, it was dominated by the Turabay dynasty, whose members served as its governors for most of this period. History.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
History. The Lajjun Sanjak was formed out of the area referred to in the Ottoman sources as the &quot;Iqta&quot; of Turabay. This iqta consisted of the nahiyas (subdistricts) of Atlit and Marj Bani Amir (the modern Jezreel Valley). Both nahiyas had been part of the Mamluk province of Safed but were administratively detached from Safed after the Ottomans conquered the region in 1516–1517.

Geographic entities mentioned:
surface_form: Jezreel Valley
instance_of: Valley
countries: Israel
coordinates: lat: 32.596388888889
lon: 35.241944444444
It has signed but not ratified the Paris Agreement on climate change. Ecosystems. Much of Iran's territory suffers from overgrazing, desertification and or deforestation. Wetlands and bodies of fresh water increasingly are being destroyed as industry and agriculture expand, and oil and chemical spills have harmed aquatic life in the Persian Gulf and the Caspian Sea.

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
The rector at that time, the Reverend Raymond Bowers, had friends in Norway, and it was he who suggested the name. A guide to the church and the Wasdale valley, &quot;The Vikings: Wasdale Head and Their Church&quot;, is available in the Barn Door Shop at Wasdale Head. The church has long been associated with British climbers.

Geographic entities mentioned:
surface_form: Wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
A guide to the church and the Wasdale valley, &quot;The Vikings: Wasdale Head and Their Church&quot;, is available in the Barn Door Shop at Wasdale Head. The church has long been associated with British climbers. The south window has a small pane within it with an etching of Napes Needle on Great Gable. A well-attended silence is kept every year on Remembrance Sunday at 11 am.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Austrepollen. Austrepollen is a village in the Mauranger area of Kvinnherad municipality in Vestland county, Norway. The village is located at the end of the Maurangsfjorden, about east of the village of Gjetingsdalen and about northeast of the village of Sunndal.

Geographic entities mentioned:
surface_form: Gjetingsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 60.134722222222
lon: 6.2319444444444
Many of these camps disappeared after the gold rush or became ghost towns. Downieville had reached a peak population of over 5,000 people in 1851, but by 1865 had significantly declined. It survived due to its status as the county seat of government in Sierra County, and from its geographic location between Sacramento Valley and Tahoe region/Nevada destinations. Demographics.

Geographic entities mentioned:
surface_form: Sacramento Valley
instance_of: Valley
countries: United States
coordinates: lat: 39
lon: -121.5
Geography. Hungerford is on the River Dun. It is the westernmost town in Berkshire, on the border with Wiltshire. It is in the North Wessex Downs. The highest point in the entire South East England region is the summit of Walbury Hill, from the town centre. The Kennet and Avon Canal separates Hungerford from what might be described as the town's only suburb, the village of Eddington.

Geographic entities mentioned:
surface_form: Walbury Hill
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.352261111111
lon: -1.4657694444444
Dongkha La. The Dongkha la or Donkia Pass() (el.) is a high mountain pass in the Himalaya connecting Sikkim in India with Tibet. Located in North Sikkim, the pass offers a view of the Tibetan Plateau. The nearby Tso Lhamo Lake is long and wide, and is the source of the Teesta River. Gurudongmar Lake, some to west-northwest, also feeds the Teesta.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Dongkha La. The Dongkha la or Donkia Pass() (el.) is a high mountain pass in the Himalaya connecting Sikkim in India with Tibet. Located in North Sikkim, the pass offers a view of the Tibetan Plateau. The nearby Tso Lhamo Lake is long and wide, and is the source of the Teesta River. Gurudongmar Lake, some to west-northwest, also feeds the Teesta.

Geographic entities mentioned:
surface_form: Tso Lhamo Lake
instance_of: Lake
countries: India
coordinates: lat: 28.011
lon: 88.756
Located in North Sikkim, the pass offers a view of the Tibetan Plateau. The nearby Tso Lhamo Lake is long and wide, and is the source of the Teesta River. Gurudongmar Lake, some to west-northwest, also feeds the Teesta. The first observer to record the pass in western literature was botanist Joseph Dalton Hooker, who crossed the pass on 7September 1849.

Geographic entities mentioned:
surface_form: Gurudongmar Lake
instance_of: Lake
countries: India
coordinates: lat: 28.02
lon: 88.71
In April 1943, under instructions from London, they set up a Free Corps in the region of Montagne Noire. Supplies are weapons start being sent from Algiers, the drop off is on the plateau of Pic de Nore. They divided the group into 5 camps: Plo Del May, Fonbruno, Le Rietgé, Co de David, La Galaube. The Corps Franc de la Montagne Noire had at some point 21 nationalities represented.

Geographic entities mentioned:
surface_form: Pic de Nore
instance_of: Mountain
countries: France
coordinates: lat: 43.42416667
lon: 2.46277778
Serranía del Aguaragüe. 4x9ii5gn3uhnu90cgo0dtc0bxsu3r" xml:space="preserve">Serranía del Aguaragüe is the easternmost range of Bolivia's Cordillera Oriental. Serranía del Aguaragüe stretches out in a north–south fashion from the latitude of crossing the Bolivian departments of Tarija, Chuquisaca and Santa Cruz.

Geographic entities mentioned:
surface_form: serranía del aguaragüe
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.383333333333
lon: -63.6
4x9ii5gn3uhnu90cgo0dtc0bxsu3r" xml:space="preserve">Serranía del Aguaragüe is the easternmost range of Bolivia's Cordillera Oriental. Serranía del Aguaragüe stretches out in a north–south fashion from the latitude of crossing the Bolivian departments of Tarija, Chuquisaca and Santa Cruz. Geologically it corresponds to the thrust front where the Andes meets the Bolivian Chaco.

Geographic entities mentioned:
surface_form: serranía del aguaragüe
instance_of: Mountain
countries: Bolivia
coordinates: lat: -21.383333333333
lon: -63.6
The father was a French-Canadian explorer and fur-trader intent on finding an overland water route to the Western Ocean. Between 1731 and 1737 he built several trading posts between Lake Superior and Lake Winnipeg, assisted by his four sons and a nephew.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Many of the homes were constructed in the early 1900s, but few date from before 1906 because of the 1906 San Francisco earthquake. These houses were built for many early Santa Clara Valley professionals and are historically significant. The Naglee Terrace Subdivision is bounded by East William Street, East Margaret Street, Coyote Creek (William Street Park), and South 11th Street.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
The Kanalla Falls, a waterfall on the Edeowie Creek, is located in the Flinders Ranges in South Australia. Situated within the Ikara-Flinders Ranges National Park approximately north of the village of and north of Adelaide, the waterfalls descend from below St Mary Peak and a range of other mountains at an elevation of above sea level; falling in the range of into the Wilpena Pound valley below.

Geographic entities mentioned:
surface_form: St Mary Peak
instance_of: Mountain
countries: Australia
coordinates: lat: -31.503888888889
lon: 138.55111111111
After winning the World Cup overall title in 1978, Wenzel's best year came in 1980. At the 1980 Winter Olympics in Lake Placid, she won gold medals in the slalom and giant slalom, and just missed out on a sweep by taking the silver in the downhill at Whiteface Mountain.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
Williamson Lake. Williamson Lake is a small mountain lake located below Welch Peak, near Chilliwack, British Columbia, Canada. It can be accessed by two different hiking trails, one 4 kilometers and the other 13 kilometers in length.

Geographic entities mentioned:
surface_form: Welch Peak
instance_of: Mountain
countries: Canada
coordinates: lat: 49.16
lon: -121.601
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.94479
lon: -84.7596
surface_form: williamson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.1505
lon: -121.596
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Williamson Lake. Williamson Lake is a small mountain lake located below Welch Peak, near Chilliwack, British Columbia, Canada. It can be accessed by two different hiking trails, one 4 kilometers and the other 13 kilometers in length.

Geographic entities mentioned:
surface_form: williamson lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.1505
lon: -121.596
Geography. Trumansburg is located at (42.540447, -76.660121). According to the United States Census Bureau, the village has a total area of, of which, of it is land and 0.83% is water. The village is located on the Trumansburg Creek (also known as Frontenac Creek) which arises on the ridge west of the village and empties into Cayuga Lake at Frontenac Point.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
San Luis provides water mainly for irrigation in the San Joaquin Valley, where it augments the supply for more than 1 million acres (400,000 ha) of agricultural land, although some water is also used for urban and environmental uses. The dam was built between 1963 and 1968, and filled for the first time in 1969.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
The storage capacity of San Luis Reservoir is divided with 55 percent belonging to the state and 45 percent to the federal government. The Delta-Mendota Canal, originally built in 1951, carries irrigation water for the federal Central Valley Project (CVP) operated by the U.S. Bureau of Reclamation to supply San Joaquin Valley farms.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
transferred to the CVP and SWP supplies. In addition to supplying the main CVP and SWP canals, San Luis Reservoir also supplies water to the Santa Clara Valley via the Pacheco Tunnel and Hollister Conduit, which travel under the Diablo Range. At the western end of the tunnel, the water is stored behind San Justo Dam, an earthfill dam completed in 1986.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Both the bank and the library were constructed by Gilbert in the Neoclassical style. Paine also had Flat Rock Camp, his summer retreat on the shores of Lake Champlain, constructed for his family. After the Second World War, the paper industry started to decline, and when the paper mill closed in the 1960s the town faced economic difficulties.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
Geography. According to the United States Census Bureau, the town has a total area of, of which is land and, or 41.80%, is water. The eastern town line, marked by Lake Champlain, is the border of Vermont. The Boquet River enters Lake Champlain in the town, east of Willsboro village. New York State Route 22 is a north–south highway which passes through Willsboro. Demographics.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
In 2001 the parish had a population of 103. The parish includes parts of Monsal Dale and the hamlet of Monsal Head, and lies wholly within the Peak District National Park. The Monsal Trail, a popular cycleway and footpath following a section of the former Manchester, Buxton, Matlock and Midlands Junction Railway, runs just south of the village.

Geographic entities mentioned:
surface_form: Monsal Dale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.244719444444
lon: -1.7317194444444
Etymology. The name derives from the fact that the Detroit River, after running more or less west along the banks of Detroit and Windsor, Ontario, then bends to flow largely south before emptying into Lake Erie. Communities to the south of the city can thus be accessed by traveling downriver (as opposed to upriver) along the waterway.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
Watkins Glen State Park. Watkins Glen State Park is in the village of Watkins Glen, south of Seneca Lake in Schuyler County in New York's Finger Lakes region. The park's lower part is near the village, while the upper part is open woodland. It was opened to the public in 1863 and was privately run as a tourist resort until 1906, when it was purchased by New York State.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
Geology. During the Pleistocene era, a vast area was covered by ice during the maximum extent of glacial ice in the north polar area. The movement of glaciers from the Laurentide and Wisconsin ice sheets shaped the Finger Lakes region. The lakes originated as a series of northward-flowing streams.

Geographic entities mentioned:
surface_form: Finger Lakes
instance_of: Group of lakes
countries: United States
coordinates: lat: 42.666666666667
lon: -76.833333333333
There are concentrations of lunar domes near the craters Hortensius, and T. Mayer, across the top of Mons Rümker, and in Mare Fecunditatis. Solitary lunar domes are also found, including Kies Pi (π), Milichius Pi (π), Mons Gruithuisen Gamma (γ) and Delta (δ), and domes near the craters Gambart C, Beer, and Capuanus. Omega Cauchy (ω) and Tau Cauchy (τ) form a pair of domes near the crater Cauchy.

Geographic entities mentioned:
surface_form: Mons Rümker
instance_of: Mountain
coordinates: lat: 40.76
lon: -58.38
There are concentrations of lunar domes near the craters Hortensius, and T. Mayer, across the top of Mons Rümker, and in Mare Fecunditatis. Solitary lunar domes are also found, including Kies Pi (π), Milichius Pi (π), Mons Gruithuisen Gamma (γ) and Delta (δ), and domes near the craters Gambart C, Beer, and Capuanus. Omega Cauchy (ω) and Tau Cauchy (τ) form a pair of domes near the crater Cauchy.

Geographic entities mentioned:
surface_form: Mons Gruithuisen Gamma
instance_of: Mountain
coordinates: lat: 36.56
lon: -40.72
Likewise near Arago are the domes Arago Alpha (α) and Arago Beta (β). There are two domes south of Mons Esam. The IAU does not currently have rules that establish the naming of lunar domes, but the practice in the professional literature and in lunar sciences is to name the dome with the name of the nearest crater followed by a number that denotes the order of discovery.

Geographic entities mentioned:
surface_form: Mons Esam
instance_of: Mountain
coordinates: lat: 14.61
lon: 35.71
Neuhofen an der Ybbs. Neuhofen an der Ybbs is a municipality in the district of Amstetten in Lower Austria in Austria. Geography. Neuhofen an der Ybbs lies in the Mostviertel in the hills north of the Hochkogel at the foot of the Kornberg. Despite its name, it does not lie directly on the river Ybbs. About 20 percent of the municipality is forested.

Geographic entities mentioned:
surface_form: Ybbs
instance_of: Watercourse
countries: Austria
coordinates: lat: 47.7603
lon: 15.2053
Dajt. Dajt is a former municipality in the Tirana County, central Albania. At the 2015 local government reform it became a subdivision of the municipality Tirana. The population as of the 2023 census is 35,170. The municipal unit took its name from the Mount Dajt. Seal. The seal of the municipality derives from the coat of arms of the medieval Albanian noble family of Skurra.

Geographic entities mentioned:
surface_form: Mount Dajt
instance_of: Mountain
countries: Albania
coordinates: lat: 41.365833333333
lon: 19.925555555556
The town's residents were unharmed. On 29 November they left Monterey, passed Point Conception, and anchored off of Refugio Canyon, about twenty miles west of Santa Barbara, where they went to the hacienda of the Ortega family rancho. Bouchard was told the family had strongly supported the Spanish cause.

Geographic entities mentioned:
surface_form: Point Conception
instance_of: Landform
countries: United States
coordinates: lat: 34.448113
lon: -120.471439
Wrangler Lake. Wrangler Lake is a lake located in Yellowstone National Park in the U.S. state of Wyoming. It is a few miles from the Wapiti Lake Trailhead. Description. &quot;The Yellowstone Fly-Fishing Guide&quot; describes the lake as fishless. There is a roundtrip trail which starts at Sour Creek in Yellowstone National Park and ends at Wrangler Lake.

Geographic entities mentioned:
surface_form: wrangler lake
instance_of: Lake
countries: United States
coordinates: lat: 44.683333333333
lon: -110.43472222222
state of Wyoming. It is a few miles from the Wapiti Lake Trailhead. Description. &quot;The Yellowstone Fly-Fishing Guide&quot; describes the lake as fishless. There is a roundtrip trail which starts at Sour Creek in Yellowstone National Park and ends at Wrangler Lake. Bill Schneider notes that Wrangler Lake has many mosquitos in June and July, and so recommends hiking later in the season.

Geographic entities mentioned:
surface_form: wrangler lake
instance_of: Lake
countries: United States
coordinates: lat: 44.683333333333
lon: -110.43472222222
Chi-Rho ⳩ is the Greek monogram for Christ. Formed by superimposing the first two letters of the Greek word &quot;ΧΡ'&quot;ΙΣΤΟΣ&quot; meaning Christ. The three chevrons represent the North Shore Mountains that overlook Vancouver. The mountains depicted are intended to represent the Hollyburn, Grouse and Seymour mountaintops. The Barque of St. Peter, the ship, symbolises the church.

Geographic entities mentioned:
surface_form: Grouse
instance_of: Mountain
countries: Canada
coordinates: lat: 49.38611111
lon: -123.07638889
surface_form: Seymour
instance_of: Mountain
countries: Canada
coordinates: lat: 49.393333333333
lon: -122.94444444444
Moel Tryfan. Moel Tryfan (429 m / 1407 ft) is a small mountain near the villages of Rhosgadfan, Y Fron and Betws Garmon, in northern Gwynedd. The higher and more famous peak of Tryfan above Dyffryn Ogwen has also sometimes been referred to as &quot;Moel Tryfan&quot; in the past. Moel Tryfan could be regarded as the westerly outlier of the larger Mynydd Mawr.

Geographic entities mentioned:
surface_form: Tryfan
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.114938888889
lon: -3.9975305555556
The higher and more famous peak of Tryfan above Dyffryn Ogwen has also sometimes been referred to as &quot;Moel Tryfan&quot; in the past. Moel Tryfan could be regarded as the westerly outlier of the larger Mynydd Mawr. The southern and eastern flanks of the mountain were heavily quarried in the past, particularly at Moel Tryfran Quarry and Cilgwyn quarry.

Geographic entities mentioned:
surface_form: Mynydd Mawr
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 53.0686
lon: -4.182
Ogulin. Ogulin () is a town in central Croatia, in Karlovac County. It has a population of 7,389 (2021) (it was 8,216 in 2011), and a total municipal population of 12,251 (2021). Ogulin is known for its historic stone castle, known as Kula, and the nearby mountain of Klek. Toponymy. There are several proposed etymologies for the name of Ogulin.

Geographic entities mentioned:
surface_form: Klek
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.26033333
lon: 15.14547222
One Partisan was killed and one captured and taken to Ogulin for questioning. When the German and Italian Zones of Influence were revised on 24 June 1942, Ogulin fell in, administered civilly by Croatia but militarily by Italy. On 2–3 July, the Italian garrison in Ogulin repelled a Partisan attack on Ogulin itself, following which the Partisans retreated to Klek.

Geographic entities mentioned:
surface_form: Klek
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.26033333
lon: 15.14547222
This is a kind of transitional micro-region neighbouring the larger regions of Croatia - Gorski Kotar, Lika, Kordun and Gornje Pokuplje. The Ogulin-Modruš valley is the northern section of the Ogulin-Plaški valley, which finishes towards the south where the Modruš hills pass into the second largest field of the area under Kapela-Plaški Polje.

Geographic entities mentioned:
surface_form: Ogulin-Plaški valley
instance_of: Valley
countries: Croatia
coordinates: lat: 45.188624
lon: 15.284755
The Ogulin-Modruš valley is the northern section of the Ogulin-Plaški valley, which finishes towards the south where the Modruš hills pass into the second largest field of the area under Kapela-Plaški Polje. This comprises a completed geographical whole border on the western side by the mountain massif of Velika Kapela dominated by Klek (1181 m).

Geographic entities mentioned:
surface_form: Klek
instance_of: Mountain
countries: Croatia
coordinates: lat: 45.26033333
lon: 15.14547222
Its distribution is centered on the Rocky Mountains. It is less frequent to the east of the Rockies in the Great Plains, but is found in many places in the Driftless Area and the Ozarks. A few populations are found as far east as Kentucky, Virginia, and North Carolina. In Mexico, it is known from the northernmost states, Chihuahua and Coahuila, and more recently from Sonora.

Geographic entities mentioned:
surface_form: Ozarks
instance_of: Plateau
countries: United States
coordinates: lat: 37.1822
lon: -92.5159
The settlement is mentioned in the &quot;Domesday Book&quot; as being in the Hundred of Cutestornes and having eight villagers and five slaves. The name derives from Old English &quot;Mōr-tūn&quot; (town by a fen), and its proximity to the River Lugg. In medieval times, the village was listed as &quot;Morton Juxta Logge&quot;.

Geographic entities mentioned:
surface_form: River Lugg
instance_of: Watercourse
countries: United Kingdom
coordinates: lat: 52.0311
lon: -2.63611
Tai Ho was originally a rural area. To the northern part there is a shoal extend and to the southern part is the foot of Lin Fa Shan. Slopes are covered with grassland and shrub forests. There are monsoonal nature of swamps, as well as a stream named Tai Ho Stream which flows into the Tai Ho Bay. Villages. Villages in the area include Pak Mong, Ngau Kwu Long, Tai Ho Village aka.

Geographic entities mentioned:
surface_form: Lin Fa Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.2737
lon: 113.972
Before the 2011 local government reform it was an independent community. The community of Karya covers an area of 74.964 km2 while the municipal unit covers 158.685 km2. Geography and climate. It is close to Mount Olympus, encouraging tourists' visits. The area has moderate temperatures year round, though in winter snow falls over the upper elevations. Morias Cave.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35
Morias Cave. In the midst of World War II in 1941, a Nazi brigade stormed the village of Karya. A local hero, Aléxandros Yiannis Morias discovered a cave in Mount Olympus to hide the town from the Nazi invaders. The villagers were unharmed thanks to the discovery of the cave. In honor of the heroics of Aléxandros, the cave has since been named Morias Cave.

Geographic entities mentioned:
surface_form: Mount Olympus
instance_of: Mountain
countries: Greece
coordinates: lat: 40.083333333333336
lon: 22.35