Sarmila/GeoWiki-Features huggingface dataset:
Darial Gorge. The Darial Gorge is a river gorge on the border between Russia and Georgia. It is at the east base of Mount Kazbek, south of present-day Vladikavkaz. The gorge was carved by the river Terek, and is approximately long. The steep granite walls of the gorge can be as much as tall in some places. The Georgian Military Road runs through the gorge. History.

Geographic entities mentioned:
surface_form: Mount Kazbek
instance_of: Mountain
countries: Georgia
Russia
Russian Empire
Soviet Union
coordinates: lat: 42.69694444444445
lon: 44.51888888888889
The pass is mentioned in the Georgian annals under the names of Darialani; Strabo calls it &quot;Porta Caucasica&quot; and &quot;Porta Cumana&quot;; Ptolemy, &quot;Fortes Sarmatica&quot;; it was sometimes known as &quot;Porta Caucasica&quot; and &quot;Portae Caspiae&quot; (a name bestowed also on the &quot;gate&quot; or pass beside the Caspian Sea at Derbent); and the Tatars call it Darioly.

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
Location. Hoang Lien National Park is Vietnam's mountainous Northwest and includes Fansipan, the highest mountain in Vietnam and on the Indochinese Peninsula. The total area of the core national park is, which includes a strict protected area of 11,875 ha; a &quot;forest rehabilitation area&quot; of 17,900 ha; and an administration services area of 70 ha.

Geographic entities mentioned:
surface_form: Fansipan
instance_of: Mountain
countries: Vietnam
coordinates: lat: 22.303333333333
lon: 103.775
The route required that participants drive from New York to Montreal, attend a party and drive back to NYC. In 2010, the event launched in Los Angeles. Teams have traveled from LA to Tombstone, Las Vegas, Lake Tahoe, the Grand Canyon, and Death Valley. 2008 NYC to Montreal. The inaugural rally featured 74 cars and 189 participants, and traveled from Long Island City, Queens to Montreal, Canada.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Loch Garry (Dalnaspidal). Loch Garry is a large upland freshwater loch located in Perth and Kinross in Scotland, within the Forest of Atholl just to the south of the Cairngorms National Park. Loch Garry Project.

Geographic entities mentioned:
surface_form: loch garry
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.805765
lon: -4.246576
Loch Garry Project. A study of the arctic char population of the loch conducted by Ron Greer between 1972 and 1974 concluded that it had become ecologically impoverished as a result of the loss of living and dead plant material from the shallow littoral zone. In 1986, the Loch Garry Project was established to undertake a programme of tree-planting around the loch.

Geographic entities mentioned:
surface_form: loch garry
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.805765
lon: -4.246576
These specimens were collected by the British naturalist Henry R. Hogg, who found them in and on decaying wood on Mount Macedon in the state of Victoria in Australia at an elevation of 1,001 meters above sea level. Two syntypes are deposited in the Museum National d’Histoire Naturelle in Paris, France. Taxonomy.

Geographic entities mentioned:
surface_form: Mount Macedon
instance_of: Mountain
countries: Australia
coordinates: lat: -37.38291
lon: 144.57625
Specimens assigned to this species have been collected elsewhere, not only in New Zealand and Tasmania, where such specimens are now assigned to other species, but also in other localities in Victoria. For example, this velvet worm has been recorded in Kinglake National Park, Emerald, Elmhurst, Ferntree Gully, and Gembrook, as well as on Mount Donna Buang.

Geographic entities mentioned:
surface_form: Mount Donna Buang
instance_of: Mountain
countries: Australia
coordinates: lat: -37.706388888889
lon: 145.68111111111
While this was to be the first penetration by an aircraft over the Antarctic Plateau, the route itself was generally familiar to Byrd and his men, because they flew close to the pathway used by Roald Amundsen in his successful ground-level expedition to the South Pole in late 1911. Those on board the &quot;Floyd Bennett&quot; for the historic flight were Commander Richard E.

Geographic entities mentioned:
surface_form: Antarctic Plateau
instance_of: Plateau
coordinates: lat: -90
lon: 0
June's polar papers were donated, with the Byrd archive, to Ohio State University. The June Nunatak, an Antarctic rocky outcropping of the Liv Glacier, was named in honor of co-pilot June in 1961-62, three decades after the successful flight by the &quot;Floyd Bennett&quot; up and over the same glacier in 1929.

Geographic entities mentioned:
surface_form: June Nunatak
instance_of: Mountain
coordinates: lat: -85.2333
lon: -169.483
It was also given a 10-year option to buy of land. The company was to plant of guayule (&quot;Parthenium argentatum&quot;) for every of rubber extracted. It planned to conduct experiments on different varieties of rubber plants. The region was along the Congo River up to the confluence of the Kasai River. Leopold was to receive half the profits of the company. History.

Geographic entities mentioned:
surface_form: Kasai River
instance_of: Watercourse
countries: Angola
Democratic Republic of the Congo
coordinates: lat: -10.9603
lon: 19.3156
History. Originally a single farm in the Rhondda, in 1857 David Davis and his partners took a mineral rights lease in the area, and went exploring for high quality steam coal. In 1862, after many difficulties, the 4 feet seam was struck below the farm.

Geographic entities mentioned:
surface_form: Rhondda
instance_of: Valley
countries: United Kingdom
coordinates: lat: 51.615938888889
lon: -3.4175222222222
Saint Joseph's Oratory. Saint Joseph's Oratory of Mount Royal (French: &quot;Oratoire Saint-Joseph-du-Mont-Royal&quot;) is a Roman Catholic minor basilica and national shrine located at 3800 Queen Mary Road in the Côte-des-Neiges neighborhood on Mount Royal's Westmount Summit in Montreal, Quebec.

Geographic entities mentioned:
surface_form: Mount Royal
instance_of: Mountain
countries: Canada
coordinates: lat: 45.506388888889
lon: -73.588888888889
surface_form: Westmount Summit
instance_of: Mountain
countries: Canada
coordinates: lat: 45.492
lon: -73.6069
With its monumental scale, Renaissance Revival facade and contrasting Art Deco interior, the Oratory is recognizable not just in Montreal but around the world, attracting more than 2 million visitors and pilgrims to its steps each year. The Oratory is the highest building in Montreal, rising more than 30 metres above Mount Royal's summit, allowing it to be seen from many kilometres away.

Geographic entities mentioned:
surface_form: Mount Royal's summit
instance_of: Mountain
countries: Canada
coordinates: lat: 45.492
lon: -73.6069
Karbonkelberg. Karbonkelberg is a small peak forming part of the Table Mountain National Park in Cape Town, South Africa. Geography. It forms a prominent landmark overlooking the harbour at Hout Bay. An unusual feature is that sand has been blown up it by the wind, causing a dune-like feature. This has been popular with local residents to surf down it on polished boards or sheets.

Geographic entities mentioned:
surface_form: table mountain national park
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: karbonkelberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.033333333333
lon: 18.316666666667
This has been popular with local residents to surf down it on polished boards or sheets. Its cliff on the southern side is also a famous climbing spot. In the North it is bordered by Table Mountain National Park, comprising the Orangekloof Nature reserve and the lower slopes of Table Mountain beyond. It is bordered by the Atlantic and Little Lions Head, Kapteins Peak and The Sentinel.

Geographic entities mentioned:
surface_form: table mountain national park
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
surface_form: table
instance_of: Mountain
countries: South Africa
coordinates: lat: -33.96216
lon: 18.41352
Karbonkelberg. Karbonkelberg is a small peak forming part of the Table Mountain National Park in Cape Town, South Africa. Geography. It forms a prominent landmark overlooking the harbour at Hout Bay. An unusual feature is that sand has been blown up it by the wind, causing a dune-like feature. This has been popular with local residents to surf down it on polished boards or sheets.

Geographic entities mentioned:
surface_form: karbonkelberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -34.033333333333
lon: 18.316666666667
Kodumudi Magudeswarar Temple. The Magudeswarar Temple in Kodumudi is a large Hindu temple dedicated to Shiva in Erode district of Tamil Nadu, India. This is the sixth temple in Kongu, the region praised in the Thevaram hymns. it is situated on the banks of the river Kaveri. The sage Agastya is associated with this temple. Location.

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
The army protected the settlers and travelers from the attacks of the resident Paiute, Mojave, and Chemehuevi Native Americans until 1871. This also opened the way for large mining development in the Mojave Desert region of San Bernardino County and agricultural development in the Victor Valley area. In 1826, American trapper Jedediah Smith used the Mojave Road to come to California.

Geographic entities mentioned:
surface_form: Victor Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5
lon: -117.3
Upon reaching the San Bernardino Valley of California, Smith and Abraham LaPlant (who spoke some Spanish) borrowed horses from a rancher and rode to the San Gabriel Mission on November 27, 1826, to present themselves to its director, Father José Bernardo Sánchez, who received them warmly. Camp Cady (1860–1861, 1866–1871) was a U.S.

Geographic entities mentioned:
surface_form: San Bernardino Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.066666666667
lon: -117.28333333333
Comephorus dybowskii. &quot;Comephorus dybowskii&quot;, the little Baikal oilfish, is a species of freshwater ray-finned fish belonging to the family Cottidae, the typical sculpins. This fish is endemic to Lake Baikal in Russia. Etymology.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Access. The trail to the top of Pyramid Mountain starts at Pyramid Campground. It is to the summit. The view is mostly southward to Trophy Mountain, Battle Mountain and Dunn Peak. The Murtle River flows along the east and south sides of Pyramid. In some weather conditions, the plume of spray over Helmcken Falls can be seen to the west.

Geographic entities mentioned:
surface_form: Trophy Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.7997
lon: -119.876
surface_form: battle mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9525
lon: -119.85472222222222
surface_form: dunn peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.43694444444444
lon: -119.95444444444445
Pyramid Mountain (Wells Gray-Clearwater). Pyramid Mountain is a subglacial mound located on the Murtle Plateau in Wells Gray Provincial Park, east-central British Columbia, Canada. Formation. Pyramid Mountain erupted about 12,000 years ago. It was once mistaken for a cinder cone and is now known to have erupted underneath about of glacial ice.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
Pyramid Mountain (Wells Gray-Clearwater). Pyramid Mountain is a subglacial mound located on the Murtle Plateau in Wells Gray Provincial Park, east-central British Columbia, Canada. Formation. Pyramid Mountain erupted about 12,000 years ago. It was once mistaken for a cinder cone and is now known to have erupted underneath about of glacial ice.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
The result was a cement-like surface with smoothed cobbles of granite, schist, phyllite and other non-volcanic pebbles which were carried by the ice from many kilometers distant. As a result of this type of eruption, Pyramid Mountain has no crater and no lava flows stretching away from its base.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
The secondary cone to the east (best seen from Clearwater Valley Road near Hemp Creek) was not formed by a separate eruption, but was simply a slump when the ice melted away from Pyramid, releasing the pressure against its slopes. Access. The trail to the top of Pyramid Mountain starts at Pyramid Campground. It is to the summit.

Geographic entities mentioned:
surface_form: pyramid mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.9944
lon: -120.104
Xieng Khouang Airport. Xieng Khouang Airport is an airport in Phonsavan, Laos. Its name is derived from the Xiangkhoang Plateau, which gives name to the Xiangkhouang Province on which it is located. It is the main access gateway for tourists visiting the nearby Plain of Jars.

Geographic entities mentioned:
surface_form: Xiangkhoang Plateau
instance_of: Plateau
countries: Laos
coordinates: lat: 19.4
lon: 103.033
Christoph Nunatak. tn37kydt967uyxb14kwzqqh6q7o" xml:space="preserve">#redirect Christoph Nunatak

Geographic entities mentioned:
surface_form: christoph nunatak
instance_of: Mountain
coordinates: lat: -74.8167
lon: -73.7833
It is endemic to the Amargosa River drainage of the southwestern United States. The small (1.5–2.7 mm high) snail is known to occur in several near-brackish springs, including the type locality of Saratoga Springs in Death Valley. Members of this order are primarily gonochoric and show a broadcast spawning reproductive strategy.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
Early life and education. Jost was born on June 29, 1982, in New York City. He was raised in a Catholic household in the Grymes Hill neighborhood of Staten Island. His mother, Kerry J. Kelly, was the chief medical officer for the New York City Fire Department, and his father, Daniel A. Jost, was a teacher at Staten Island Technical High School.

Geographic entities mentioned:
surface_form: Grymes Hill
instance_of: Mountain
countries: United States
coordinates: lat: 40.618888888889
lon: -74.093611111111
Asiak River. The Asiak River is a waterway in the Kitikmeot Region of Nunavut in Canada. It flows generally north to Coronation Gulf, an arm of the Arctic Ocean. It runs parallel to the Coppermine River, to the west. The Inuit community of Kugluktuk (formerly Coppermine) is located at the mouth of the Coppermine River, approximately to the west.

Geographic entities mentioned:
surface_form: Coppermine River
instance_of: Watercourse
countries: Canada
coordinates: lat: 67.816666666667
lon: -115.06666666667
Tourism. Many tourists come from the Kathmandu Valley, about an hour's drive away. Pollution in the Sundarijal reservoir has increased due to the number of tourists. In addition, the VDC is a starting point for hikers along the Langtang Range. Various trekking routes also lie in Sundarijal, among them the Sundarijal-to-Chisapani trek, almost 22 km long. Culture.

Geographic entities mentioned:
surface_form: Langtang Range
instance_of: Valley
countries: Nepal
coordinates: lat: 28.25
lon: 85.5
From this period, numerous monumental works of his can be seen in public spaces. The sculptures are located in Australia, Germany, and the United States. In 1996 Metzler exhibited in the Baths of Caracalla in Rome, in 1997 in Sienna, and in 2003 in Milan. In 2006, a selection of his works were exhibited at the Park Hotel on the Bürgenstock were displayed at Lake Lucerne as well.

Geographic entities mentioned:
surface_form: Bürgenstock
instance_of: Mountain
countries: Switzerland
coordinates: lat: 47.000305555556
lon: 8.3983888888889
surface_form: Lake Lucerne
instance_of: Lake
countries: Switzerland
coordinates: lat: 47.0194
lon: 8.4011
Labour's slogan was &quot;It's Time – Time for a change, time for Labour&quot;, which expertly captured the national mood. A deciding election issue was the proposed raising of the levels of lakes Manapouri and Te Anau as part of the construction of the Manapouri Power Station to supply the aluminium smelter in Bluff with electricity.

Geographic entities mentioned:
surface_form: Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
surface_form: Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
Lizumer Hütte. The Lizumer Hütte is an Alpine club hut of the Hall in Tirol section of the Austrian Alpine Club in the Tux Alps in the Austrian state of Tyrol. The hut is located in the rear Wattental in the middle of the extensive ski touring and hiking area of the Wattentaler Lizum. Due to its location and size, the hut is also used for a wide variety of alpine courses and seminars. History.

Geographic entities mentioned:
surface_form: Wattental
instance_of: Valley
countries: Austria
coordinates: lat: 47.23
lon: 11.618611111111
As a way to the Lizumer Hütte there are also some yoke crossings, namely the Klammjoch from the Navistal, the Torjoch from the Tuxer Tal and the Grafensjoch from Weerberg. The transition from the Lizumer Hütte to the Glungezerhütte via the Navisjoch and the Rosenjoch takes seven to nine hours of walking. It takes about five hours to walk to the Weidener Hütte.

Geographic entities mentioned:
surface_form: Rosenjoch
instance_of: Mountain
countries: Austria
coordinates: lat: 47.1799
lon: 11.54325
Aiguille de Chambeyron. Aiguille de Chambeyron (3,412m) is a mountain of the Cottian Alps and is the highest mountain of Alpes-de-Haute-Provence in southeast France. Together with its neighbour Brec de Chambeyron, it is the dominant peak of the upper Ubaye Valley. The mountain is located near the border with Italy, just west of the Main chain of the Alps.

Geographic entities mentioned:
surface_form: Brec de Chambeyron
instance_of: Mountain
countries: France
coordinates: lat: 44.52694444
lon: 6.85277778
surface_form: Ubaye Valley
instance_of: Valley
countries: France
coordinates: lat: 44.433780555556
lon: 6.6563416666667
Together with its neighbour Brec de Chambeyron, it is the dominant peak of the upper Ubaye Valley. The mountain is located near the border with Italy, just west of the Main chain of the Alps. It is the culminating point of the Massif du Chambeyron and is also the highest peak in the Alps south of Monte Viso. Aiguille de Chambeyron has two summits, with the west one being the slightly higher.

Geographic entities mentioned:
surface_form: Monte Viso
instance_of: Mountain
countries: Italy
coordinates: lat: 44.6675
lon: 7.0916666666667
Aiguille de Chambeyron. Aiguille de Chambeyron (3,412m) is a mountain of the Cottian Alps and is the highest mountain of Alpes-de-Haute-Provence in southeast France. Together with its neighbour Brec de Chambeyron, it is the dominant peak of the upper Ubaye Valley. The mountain is located near the border with Italy, just west of the Main chain of the Alps.

Geographic entities mentioned:
surface_form: aiguille de chambeyron
instance_of: Mountain
countries: France
coordinates: lat: 44.54722222
lon: 6.85611111
The mountain is located near the border with Italy, just west of the Main chain of the Alps. It is the culminating point of the Massif du Chambeyron and is also the highest peak in the Alps south of Monte Viso. Aiguille de Chambeyron has two summits, with the west one being the slightly higher. Two small glaciers existed on its north side, although they have now all but vanished. W.A.B.

Geographic entities mentioned:
surface_form: aiguille de chambeyron
instance_of: Mountain
countries: France
coordinates: lat: 44.54722222
lon: 6.85611111
History. The area around Suratgarh was called 'Sodhawati' and south-east of Bhatner was once occupied by the Sodha Rajputs before being evicted from these regions by Bhati Rajputs, after which they moved their base to Thar desert. A branch of Parmaras left Abu and settled in Radhanpur led by Bahar Parmar.

Geographic entities mentioned:
surface_form: Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
The mountains are primarily composed of Triassic marble. Geography. The Jinping Mountains are rugged and rise almost above the Yalong River on either side. The Jinping are located in the complicated grouping of mountains called the Hengduan Mountains that transition between the Tibetan Plateau in the northwest to the Yungui Plateau in the southeast.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Features. It is located on the main alpine watershed, at an important geographic junction: in fact, the secondary alpine ridge that separates the Varaita Valley from the Maira Valley departs from its summit. The main alpine ridge has a fairly irregular course in this area.

Geographic entities mentioned:
surface_form: Varaita Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
surface_form: Maira Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.50194444
lon: 7.13777778
Bellino. The eastern slope dominates the wide basin at the base of the Autaret pass, in the upper Bellino Valley; the wall on this side is very steep. In contrast, the southern slope, which dominates the Maurin valley in the upper Maira Valley, consists of a scree slope with a constant gradient.

Geographic entities mentioned:
surface_form: Bellino Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.58
lon: 7.1
The eastern slope dominates the wide basin at the base of the Autaret pass, in the upper Bellino Valley; the wall on this side is very steep. In contrast, the southern slope, which dominates the Maurin valley in the upper Maira Valley, consists of a scree slope with a constant gradient. The northwestern slope descends with steep rock walls on the Vallon de Mary, a side valley of the Ubaye Valley.

Geographic entities mentioned:
surface_form: Maira Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.50194444
lon: 7.13777778
The eastern slope dominates the wide basin at the base of the Autaret pass, in the upper Bellino Valley; the wall on this side is very steep. In contrast, the southern slope, which dominates the Maurin valley in the upper Maira Valley, consists of a scree slope with a constant gradient. The northwestern slope descends with steep rock walls on the Vallon de Mary, a side valley of the Ubaye Valley.

Geographic entities mentioned:
surface_form: Ubaye Valley
instance_of: Valley
countries: France
coordinates: lat: 44.433780555556
lon: 6.6563416666667
From there, one ascends to the right along a trail that, part on the ridge, part just below, leads to the summit. The itinerary has a difficulty rating of EE. The low Terrarossa can also be reached from the Maira Valley, starting from the Collet grange. From there a marked path leads to the pass, from where the itinerary previously described is followed.

Geographic entities mentioned:
surface_form: Maira Valley
instance_of: Valley
countries: Italy
coordinates: lat: 44.50194444
lon: 7.13777778
Monte Maniglia. Monte Maniglia (French: &quot;Mont de Maniglia&quot;) is a mountain in the Cottian Alps, located on the border between Italy and France, between Piedmont and the Alpes-de-Haute-Provence. Features.

Geographic entities mentioned:
surface_form: monte maniglia
instance_of: Mountain
countries: Italy
France
coordinates: lat: 44.5618
lon: 6.91644
Werleys Corner, Pennsylvania. Werleys Corner is an unincorporated community in Weisenberg Township in Lehigh County, Pennsylvania. It is part of the Lehigh Valley, which has a population of 861,899 and is the 68th-most populated metropolitan area in the U.S. as of the 2020 census.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Van Buren State Park (Michigan). Van Buren State Park is a public recreation area on Lake Michigan south of South Haven, Michigan, United States. The state park, which is maintained and operated by the Michigan Department of Natural Resources, is located in the southwest corner of South Haven Township and the northwest corner of Covert Township, just north of the Palisades Nuclear Power Plant.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
Distelsee. Distelsee is a high alpine lake in the canton of Valais, Switzerland. It is located at an elevation of 2587 m, below Brudelhorn. Its surface area is 4.8 ha.

Geographic entities mentioned:
surface_form: distelsee
instance_of: Lake
countries: Switzerland
coordinates: lat: 46.463055555555556
lon: 8.323055555555555
Lingmell. Lingmell is a fell in the English Lake District, standing above the village of Wasdale Head. It is an outlier on the north-west flank of Scafell Pike, England’s highest mountain. Topography. Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects.

Geographic entities mentioned:
surface_form: Scafell Pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
The northern crag drops for toward the valley floor, with a further of scree below. The connection to Scafell Pike is via Lingmell Col, a grassy depression at. Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells.

Geographic entities mentioned:
surface_form: Wast Water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Summit. The summit of Lingmell is directly above the crags on the eastern side, a fine cairn having been constructed to replace the thin column described by Wainwright in the 1960s. This is one of the finest vantage points for Great Gable, a little over a mile to the north. Particularly impressive is the view of the Great Napes, one of the nurseries of the sport of rock climbing.

Geographic entities mentioned:
surface_form: Great Gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Alfred Wainwright wrote in his Pictorial Guide to the Lakeland Fells of: ‘…the surprising aspect of Great Gable across the deep gulf of Lingmell Beck…the eye being deceived into seeing its half-mile of height as quite perpendicular’. From the summit of Goat Crags to the south is an equally astounding view of Scafell Crag, another early climbers’ playground on Scafell. Ascents.

Geographic entities mentioned:
surface_form: Scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
There are two ascent routes from Wasdale Head, via Brown Tongue or Piers Gill, but the latter route provides better walking and impressive views of the Piers Gill ravine and Great Gable. The ascent from Borrowdale and Styhead Tarn is made by the Corridor Route.

Geographic entities mentioned:
surface_form: Styhead Tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.478055555556
lon: -3.2027777777778
surface_form: borrowdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.42
lon: -2.665
Lingmell. Lingmell is a fell in the English Lake District, standing above the village of Wasdale Head. It is an outlier on the north-west flank of Scafell Pike, England’s highest mountain. Topography. Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects.

Geographic entities mentioned:
surface_form: wasdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Ascents. Lingmell is often bypassed by walkers aiming for Scafell Pike and Scafell, but it is a rewarding ascent in its own right, or as part of a circuit of the Scafell range. There are two ascent routes from Wasdale Head, via Brown Tongue or Piers Gill, but the latter route provides better walking and impressive views of the Piers Gill ravine and Great Gable.

Geographic entities mentioned:
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instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.425
lon: -3.35
surface_form: great gable
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells. This flows right around the northern perimeter of Lingmell, finally entering Wast Water as Lingmell Beck, only a short distance from the entry point of Lingmell Gill.

Geographic entities mentioned:
surface_form: wast water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.441666666667
lon: -3.2916666666667
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Particularly impressive is the view of the Great Napes, one of the nurseries of the sport of rock climbing. Alfred Wainwright wrote in his Pictorial Guide to the Lakeland Fells of: ‘…the surprising aspect of Great Gable across the deep gulf of Lingmell Beck…the eye being deceived into seeing its half-mile of height as quite perpendicular’.

Geographic entities mentioned:
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instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.482
lon: -3.219
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
The northern crag drops for toward the valley floor, with a further of scree below. The connection to Scafell Pike is via Lingmell Col, a grassy depression at. Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells.

Geographic entities mentioned:
surface_form: scafell pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Averaging about, but much deeper in places, it pursues an L-shaped course down the fellside before emerging from its cutting to merge with Greta Gill. The scenery of Piers Gill and Lingmell from the Corridor Route ascent of Scafell Pike is remarkable and a faint path follows the eastern bank of the gill giving even more intimate views.

Geographic entities mentioned:
surface_form: scafell pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Ascents. Lingmell is often bypassed by walkers aiming for Scafell Pike and Scafell, but it is a rewarding ascent in its own right, or as part of a circuit of the Scafell range. There are two ascent routes from Wasdale Head, via Brown Tongue or Piers Gill, but the latter route provides better walking and impressive views of the Piers Gill ravine and Great Gable.

Geographic entities mentioned:
surface_form: scafell pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.454166666667
lon: -3.2115277777778
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Lingmell. Lingmell is a fell in the English Lake District, standing above the village of Wasdale Head. It is an outlier on the north-west flank of Scafell Pike, England’s highest mountain. Topography. Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells. This flows right around the northern perimeter of Lingmell, finally entering Wast Water as Lingmell Beck, only a short distance from the entry point of Lingmell Gill.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
These two streams which girdle the fell both run through wide boulder strewn courses, evidence of flash flooding and the endless fall of rocks from the upper slopes. Lingmell sends out a long shoulder westward between the two streams. The southern face of this, riven with scree on its slow tumbling journey into Lingmell Gill is named Lingmell Scars.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Lingmell sends out a long shoulder westward between the two streams. The southern face of this, riven with scree on its slow tumbling journey into Lingmell Gill is named Lingmell Scars. At the top of the shoulder are the many outcrops of Goat Crags. Piers Gill runs below the eastern crags of Lingmell in a deep ravine, one of the finest in the District.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
At the top of the shoulder are the many outcrops of Goat Crags. Piers Gill runs below the eastern crags of Lingmell in a deep ravine, one of the finest in the District. Averaging about, but much deeper in places, it pursues an L-shaped course down the fellside before emerging from its cutting to merge with Greta Gill.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Geology. Lava flows of Scafell Dacite cross the fell, interspersed with andesite and hybridized andesite porphyry. Summit. The summit of Lingmell is directly above the crags on the eastern side, a fine cairn having been constructed to replace the thin column described by Wainwright in the 1960s. This is one of the finest vantage points for Great Gable, a little over a mile to the north.

Geographic entities mentioned:
surface_form: lingmell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.462088888889
lon: -3.2217805555556
Crossings of the ravine should also be considered impossible for the average hiker. Geology. Lava flows of Scafell Dacite cross the fell, interspersed with andesite and hybridized andesite porphyry. Summit. The summit of Lingmell is directly above the crags on the eastern side, a fine cairn having been constructed to replace the thin column described by Wainwright in the 1960s.

Geographic entities mentioned:
surface_form: scafell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.448
lon: -3.225
Its chief geographical features are Slieve Rushen mountain on whose western slope it lies, three small mountain lakes including Miles' Lough, mountain streams, mountain bogs and forestry plantations. It forms part of the Slieve Rushen Bog Natural Heritage Area. Gortnavreeghan is traversed by minor roads and rural lanes. The townland covers 383 statute acres. History.

Geographic entities mentioned:
surface_form: Slieve Rushen
instance_of: Mountain
countries: United Kingdom
Ireland
coordinates: lat: 54.151925
lon: -7.6426416666667
Bautaen Peak. 9qy3d6ysjtstygt1sh98wj1a1bh1" xml:space="preserve">#REDIRECT Sør Rondane Mountains

Geographic entities mentioned:
surface_form: bautaen peak
instance_of: Mountain
coordinates: lat: -71.9667
lon: 25.95
Lattin is surrounded by pasture land, much of which is used for dairy farming. It is situated in an area of south Tipperary known as the Golden Vale, an area in which the land is particularly suitable for grass growing and dairy farming. Lattin's local GAA club, Lattin–Cullen GAA, is affiliated to the West Division Board of Tipperary GAA. The club is historically associated with Gaelic football.

Geographic entities mentioned:
surface_form: Golden Vale
instance_of: Valley
countries: Ireland
coordinates: lat: 52.4
lon: -8.4
Hjuksebø is a village in Notodden Municipality in V
Telemark county, Norway. The village is located just south of Hjuksevelta, roughly half-way between the town of Notodden and the village of Nordagutu (in Midt-Telemark Municipality. This village is located on the hills overlooking the eastern shore of the lake Heddalsvatnet. In 2020, the Hjuksebø area became part of Notodden Municipality.

Geographic entities mentioned:
surface_form: Heddalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.55805556
lon: 9.2175
Lake George (Michigan–Ontario). Lake George is a lake in Chippewa County, Michigan, United States, and Algoma District, Northwestern Ontario, Canada, that lies between Sugar Island in Michigan on the west and the Ontario mainland on the east. The lake is in the Great Lakes Basin and is part of Lake Huron and the St. Marys River.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
surface_form: huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
Lake George (Michigan–Ontario). Lake George is a lake in Chippewa County, Michigan, United States, and Algoma District, Northwestern Ontario, Canada, that lies between Sugar Island in Michigan on the west and the Ontario mainland on the east. The lake is in the Great Lakes Basin and is part of Lake Huron and the St. Marys River.

Geographic entities mentioned:
surface_form: ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: lake george
instance_of: Lake
countries: Canada
United States
coordinates: lat: 46.45002
lon: -84.13336
Lake George (Michigan–Ontario). Lake George is a lake in Chippewa County, Michigan, United States, and Algoma District, Northwestern Ontario, Canada, that lies between Sugar Island in Michigan on the west and the Ontario mainland on the east. The lake is in the Great Lakes Basin and is part of Lake Huron and the St. Marys River.

Geographic entities mentioned:
surface_form: ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
surface_form: lake george
instance_of: Lake
countries: Canada
United States
coordinates: lat: 46.45002
lon: -84.13336
The lake is in the Great Lakes Basin and is part of Lake Huron and the St. Marys River. The primary inflow is the river arriving from Little Lake George at the north, and the primary outflow is the East Neebish Channel to the St. Joseph Channel at the south.

Geographic entities mentioned:
surface_form: lake george
instance_of: Lake
countries: Canada
United States
coordinates: lat: 46.45002
lon: -84.13336
Tectonic setting. The earthquake was located close to the northern margin of the Tibetan Plateau. This area of thickened crust is a result of the ongoing collision of the Indo-Australian plate with the Eurasian plate. The way in which this zone accommodates the collision remains unclear with two end-member models being proposed.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
History. Some people believe the city was named after Donnacona, a 16th-century St. Lawrence Iroquois chief who was taken to France. The chieftain lived further down-river in Stadacona. It was actually named after the first paper mill erected at the mouth of the Jacques-Cartier River, The Donnacona Paper Ltd. It was located where the Jacques-Cartier River meets the St. Lawrence River.

Geographic entities mentioned:
surface_form: Jacques-Cartier River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
A New France Seigneurie existed under the name of Les Écureuils as a surrounding rural parish municipality prior to its final merge with Donnacona in 1967. Geography. The Jacques-Cartier River forms the north-western boundary of the municipality, flowing south-west to its mouth in the estuary of St. Lawrence.

Geographic entities mentioned:
surface_form: Jacques-Cartier River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.671388888889
lon: -71.747222222222
Cunningtonia. &quot;Cunningtonia longiventralis&quot; is a species of cichlid endemic to Lake Tanganyika in East Africa where it is found near rocky shores. It eats floating plankton. This species reaches a length of TL. It can also be found in the aquarium trade. it is the only known member of its genus.

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
An attraction close to the village is &quot;Kirkjugólf&quot; (&quot;Church floor&quot;), a natural pavement of basalt. These are basalt columns in the earth, the visible tops of which have the appearance of a paved church floor. This lava formation has similar origins to the Giant's Causeway in Ireland. History.

Geographic entities mentioned:
surface_form: Giant's Causeway
instance_of: Landform
countries: United Kingdom
coordinates: lat: 55.240833333333
lon: -6.5116666666667
Category V manuscripts are those &quot;with a purely or predominantly Byzantine text.&quot;
History. The manuscript was brought by clergyman and scientist John Covel from Mount Sinai (Egypt) to England (along with minuscule 65). Covel marked it as codex 5, but afterwards gave it the name of &quot;the Sinai manuscript&quot;.

Geographic entities mentioned:
surface_form: Mount Sinai
instance_of: Mountain
countries: Egypt
coordinates: lat: 28.5384
lon: 33.9752
Bridge End, County Durham. Bridge End is a hamlet in the civil parish of Stanhope, in County Durham, England. It is situated on the south bank of the River Wear, on the other side of Weardale from Frosterley, and near Hill End and White Kirkley.

Geographic entities mentioned:
surface_form: Weardale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.716
lon: -1.925
St. Kilian, Minnesota. St. Kilian is an unincorporated community in Nobles County, Minnesota, United States. Geography. St. Kilian is an unincorporated community in section 27 of Wilmont Township. The village sits atop the Buffalo Ridge, the drainage divide between the Mississippi River and Missouri River systems. By elevation, St. Kilian is the highest population center in Nobles County. St.

Geographic entities mentioned:
surface_form: Buffalo Ridge
instance_of: Landform
countries: United States
coordinates: lat: 43.9802
lon: -96.0106
Mount Tuve. fxonj6zcnpgrli2e9uy7vhsr9kg" xml:space="preserve">#redirect Mount Tuve

Geographic entities mentioned:
surface_form: mount tuve
instance_of: Mountain
coordinates: lat: -73.783333333333
lon: -80.133333333333
surface_form: tuve
instance_of: Mountain
coordinates: lat: -73.783333333333
lon: -80.133333333333
The trip ended with a return to California in 1912. Return to the US and marriage. After Thompson returned to Fresno, she spent July and August in the mountains to the north-east of Fresno around Big Creek and Shaver Lake. The lower Sierra Nevada mountains appealed to her because of their immensity and natural beauty.

Geographic entities mentioned:
surface_form: Shaver Lake
instance_of: Lake
countries: United States
coordinates: lat: 37.125969444444
lon: -119.29075
Marguerite also served as the president of the modernist New York Society of Women Artists in the mid-1920s. Summer in Yosemite. One of Marguerite and William's most influential summers was in 1920 when they spent the summer in Yosemite Valley, painting the landscape. The couple, with their family, hiked, sketched, and painted the beautiful national park in the Fauvist style.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Most of Vojvodina is a flat terrain, but there are several mountain areas such are Fruška Gora, Vršac Mountains, Titelski Breg, and Zagajička Brda, as well as sandy areas such are Deliblatska Peščara (nicknamed &quot;the European Sahara&quot;), and Subotička Peščara.

Geographic entities mentioned:
surface_form: Titelski Breg
instance_of: Mountain
countries: Serbia
coordinates: lat: 45.2472
lon: 20.2397
Main agricultural hunting grounds in Vojvodina are located near Bečej, Senta, Kanjiža, Novi Kneževac, Ečka, Novo Miloševo, Padej, Kikinda, Ada, and Sombor. Main forest hunting grounds are located in Posavina (near river Sava), Podunavlje (near river Danube), Fruška Gora, Vršac Mountains, Deliblatska Peščara, and Subotička Peščara.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
Vermilion River (Minnesota). The Vermilion River is located in Saint Louis County of northeast Minnesota, flowing between Crane Lake and Dago Bay of Lake Vermilion near Vermilion Dam. The Vermilion River's width varies considerably, being the size of a large creek in places and looking like a large lake in another. The Vermilion River passes through the community of Buyck in Portage Township.

Geographic entities mentioned:
surface_form: Dago Bay of Lake Vermilion
instance_of: Lake
countries: United States
coordinates: lat: 47.857908333333
lon: -92.299611111111