Sarmila/GeoWiki-Features huggingface dataset:
Further south Rebuff Glacier joins from the west. It continues south past Wood Ridge to the east and the Deep Freeze Range to the west. Capsize Glacier joins it from the west below Mount Cavaney. Styx Glacier joins from the east past the end of Wood Ridge. Further south Bates Glacier joins from the west to the north of Mills Peak.

Geographic entities mentioned:
surface_form: Mount Cavaney
instance_of: Mountain
coordinates: lat: -74.05
lon: 163.05
Capsize Glacier joins it from the west below Mount Cavaney. Styx Glacier joins from the east past the end of Wood Ridge. Further south Bates Glacier joins from the west to the north of Mills Peak. The glacier flows past Mount Melbourne to the east and Miller Nunatak to the west, and forms the Campbell Glacier Tongue where it disgorges into Terra Nova Bay past Shield Nunatak. Exploration and name.

Geographic entities mentioned:
surface_form: Mills Peak
instance_of: Mountain
coordinates: lat: -74.23333333
lon: 163.9
Capsize Glacier joins it from the west below Mount Cavaney. Styx Glacier joins from the east past the end of Wood Ridge. Further south Bates Glacier joins from the west to the north of Mills Peak. The glacier flows past Mount Melbourne to the east and Miller Nunatak to the west, and forms the Campbell Glacier Tongue where it disgorges into Terra Nova Bay past Shield Nunatak. Exploration and name.

Geographic entities mentioned:
surface_form: Mount Melbourne
instance_of: Mountain
coordinates: lat: -74.333333333333
lon: 164.7
surface_form: Shield Nunatak
instance_of: Mountain
coordinates: lat: -74.55
lon: 164.5
Recoil Glacier. A tributary glacier descending from the Deep Freeze Range, south of Mount Pollock, to the Campbell Glacier. Named by the northern party of NZGSAE, 1962-63, because the geologist was said to have &quot;recoiled in disgust&quot; on finding little of geological interest there and not what he expected. Harper Glacier.

Geographic entities mentioned:
surface_form: Mount Pollock
instance_of: Mountain
coordinates: lat: -73.75
lon: 162.78333333
Harper Glacier. A small tributary glacier which descends northeast between Mount Gibbs and Mount Adamson of the Deep Freeze Range to enter Campbell Glacier. Mapped by the United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960-64. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Wayne M.

Geographic entities mentioned:
surface_form: Mount Gibbs
instance_of: Mountain
countries: United States
coordinates: lat: 37.8771
lon: -119.212
surface_form: Mount Adamson
instance_of: Mountain
coordinates: lat: -73.91667
lon: 163
Harper, satellite geodesist at McMurdo Station, 1964-65. Rebuff Glacier. A tributary glacier descending from the Deep Freeze Range and entering Campbell Glacier southeast of the summit of Mount Mankinen. Named by the northern party of NZGSAE, 1962-63, because the party was prevented from getting access to it. Capsize Glacier.

Geographic entities mentioned:
surface_form: Mount Mankinen
instance_of: Mountain
coordinates: lat: -73.9
lon: 163.1
Named by the northern party of NZGSAE, 1962-63, because the party was prevented from getting access to it. Capsize Glacier. A tributary glacier in Deep Freeze Range, draining the slopes between Mount Cavaney and Mount Levick and flowing northeast to enter the Campbell Glacier. So named by the Northern Party of NZGSAE, 1965-66, because of the spectacular spill which the party had there.

Geographic entities mentioned:
surface_form: Mount Cavaney
instance_of: Mountain
coordinates: lat: -74.05
lon: 163.05
surface_form: Mount Levick
instance_of: Mountain
coordinates: lat: -74.13333333
lon: 163.16666667
So named by the Northern Party of NZGSAE, 1965-66, because of the spectacular spill which the party had there. Bates Glacier. A small tributary glacier flowing north from the west side of Mount Queensland, and entering the west side of Campbell Glacier just north of Mills Peak. Named by the Northern Party of the NZGSAE, 1965-66, for D.R. Bates, field assistant with that party. Mericle Rock.

Geographic entities mentioned:
surface_form: Mount Queensland
instance_of: Mountain
coordinates: lat: -74.26667
lon: 163.93333
surface_form: Mills Peak
instance_of: Mountain
coordinates: lat: -74.23333333
lon: 163.9
Named by US-ACAN for Lieutenant John L. Archambault, United States Navy, medical officer at McMurdo Station, 1967. Miller Nunatak. A sharp pointed nunatak rising above the ice at the lower end of Campbell Glacier, ESE of Mount Dickason. Mapped by USGS from surveys and United States Navy air photos, 1955-63. Named by US-ACAN for Herman T. Miller, biologist at McMurdo Station, 1965-66 season.

Geographic entities mentioned:
surface_form: Mount Dickason
instance_of: Mountain
coordinates: lat: -74.4
lon: 163.96667
They are one of the Anishinaabeg, related to but distinct from the Ojibwe and Potawatomi peoples. After migrating from the East Coast in ancient times, they settled on Manitoulin Island, near the northern shores of Lake Huron, and the Bruce Peninsula in the present-day province of Ontario, Canada. They considered this their original homeland.

Geographic entities mentioned:
surface_form: Lake Huron
instance_of: Lake
countries: Canada
United States
coordinates: lat: 44.592584
lon: -82.756293
In 1763, after the British had defeated France, Pontiac led a rebellion against the British, but he was unable to prevent British colonial settlement of the region. A decade later, Chief Egushawa (also spelled Agushawa), who had a village at the mouth of the Maumee River on Lake Erie (where Toledo later developed), led the Odawa as an ally of the British in the American Revolutionary War.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
In 1755, 3,000 Haudenosaunee lived at Fort La Galette. After the attack against Montreal, he surveyed the regions surrounding Lake Ontario for several years, producing both military maps and artistic landscapes. He painted a series of waterfalls, including views of Great Seneca Falls and Niagara Falls.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Dereše. Dereše (, 2,004 m) is the third highest peak of the Low Tatra range, in central Slovakia. It is located on the way between the highest mountains of the range, Ďumbier and Chopok in the east, and Chabenec in the west. Dereše is a popular destination among alpine skiers despite a high risk of avalanches. The scenic trail on the top of Dereše is surrounded by hundreds of cairns.

Geographic entities mentioned:
surface_form: Ďumbier
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.936611111111
lon: 19.640169444444
surface_form: Chopok
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.943055555556
lon: 19.593055555556
Dereše. Dereše (, 2,004 m) is the third highest peak of the Low Tatra range, in central Slovakia. It is located on the way between the highest mountains of the range, Ďumbier and Chopok in the east, and Chabenec in the west. Dereše is a popular destination among alpine skiers despite a high risk of avalanches. The scenic trail on the top of Dereše is surrounded by hundreds of cairns.

Geographic entities mentioned:
surface_form: dereše
instance_of: Mountain
countries: Slovakia
coordinates: lat: 48.940277777778
lon: 19.573611111111
History. Chalan Beel, (a &quot;beel&quot; in Bengali denotes a large lake or marsh that fills up with water during the monsoons) was spread over a part of what is now Natore District. Legend has it that Raja (zamindar) Ramjivan Moitra was once travelling by boat searching for a suitable place to build his principal residence.

Geographic entities mentioned:
surface_form: Chalan Beel
instance_of: Lake
countries: Bangladesh
coordinates: lat: 24.52
lon: 89.01
398, Saskatchewan, Canada. It previously held the status of a village until April 30, 1973. The hamlet is located on the north shore of Kipabiskau Lake about east of the village of Pleasantdale on highway 773. Demographics. Prior to April 30, 1973, Kipabiskau was incorporated as a village, and was restructured as a hamlet under the jurisdiction of the RM of Pleasantdale on that date.

Geographic entities mentioned:
surface_form: Kipabiskau Lake
instance_of: Lake
countries: Canada
coordinates: lat: 52.56667
lon: -104.15049
Description. Located on the northern tip of the cape is Dominguez Butte. Formerly an island in the reservoir, but at lower water levels, Padres Butte is located near the tip of Padre Point. Nearly all of the cape is located on the Navajo Nation, including Dominguez Butte, but not Padres Butte (which is located within Glen Canyon National Recreation Area).

Geographic entities mentioned:
surface_form: Padres Butte
instance_of: Mountain
countries: United States
coordinates: lat: 37.048611111111
lon: -111.28277777778
Spafford Valley, New York. Spafford Valley is a hamlet in Onondaga County, New York, United States, in the Otisco Valley south of Otisco Lake. The hamlet is noted for &quot;The Bucktail,&quot; a picturesque gorge with waterfalls.

Geographic entities mentioned:
surface_form: Otisco Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.8652
lon: -76.2868
The valley is a regular trough, or basin, from the coast to the interior. The dendrism is mainly right-bank. On the left is the long ridge of Mount Lykaion, relatively uneroded, suggesting that different types of rock occur on either side. After a divide the ridge continues as Mount Taygetus, and the valley as the Eurotas River valley, which extends south to the Gulf of Lakonia.

Geographic entities mentioned:
surface_form: Mount Lykaion
instance_of: Mountain
countries: Greece
coordinates: lat: 37.4569
lon: 21.975
The dendritic terrain of the upper Alpheios ascends to central Arcadia by steps. The plateau of Megalopoli is intermediate between the lowlands and the capital of Arcadia, modern Tripoli at. Between the two are the Tsemperou and Mainalo mountains, which are well over. Unsupported speculation throughout the ages wishes to connect the Alpheios of Megalopoli to Tripoli.

Geographic entities mentioned:
surface_form: Tsemperou
instance_of: Mountain
countries: Greece
coordinates: lat: 37.348
lon: 22.248
surface_form: Mainalo
instance_of: Mountain
countries: Greece
coordinates: lat: 37.6583
lon: 22.2517
Kallaste. Kallaste is a town in Peipsiääre Parish, Tartu County, in eastern Estonia. It is located on the western shore of Lake Peipus. History. Kallaste was founded in the 18th century as a village of Russian Old Believers. It became a small borough (&quot;alevik&quot;) in 1921 and a town 1 May 1938.

Geographic entities mentioned:
surface_form: Lake Peipus
instance_of: Lake
countries: Estonia
Russia
Russian Empire
Soviet Union
coordinates: lat: 58.676666666667
lon: 27.491666666667
Vatapi, associated with the sage &quot;Agastya&quot;, is identified with Badami in Bagalkot district. Karnataka is situated on the western edge of the Deccan plateau. It neighbours Maharashtra and Goa to the north, Andhra Pradesh to the east, Telangana to the northeast, and Tamil Nadu and Kerala to the south. On the west, it opens out on the Arabian sea. Prehistory.

Geographic entities mentioned:
surface_form: Deccan plateau
instance_of: Plateau
countries: India
coordinates: lat: 15
lon: 77
His grandmother Daisy inherited the Maynard estates in 1865 from her grandfather, Henry Maynard, 3rd Viscount Maynard, and reportedly was a long-term mistress to the Prince of Wales, who later became King Edward VII. Greville was educated at Eton and at Chillon College, Lake Geneva in Switzerland.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Nike Missile Site SF-88. SF-88 is a former Nike Missile launch site at Fort Barry, in the Marin Headlands to the north of San Francisco, California, United States. Opened in 1954, the site was intended to protect the population and military installations of the San Francisco Bay Area during the Cold War, specifically from attack by Soviet bomber aircraft.

Geographic entities mentioned:
surface_form: Marin Headlands
instance_of: Landform
countries: United States
coordinates: lat: 37.827777777778
lon: -122.50611111111
Several hours later, TCWC Jakarta upgraded the system to a tropical cyclone, giving the name &quot;Cempaka&quot;. Winds from the cyclone also blew ash from nearby Mount Agung on Bali westwards to its popular beaches and far eastern Java. On 30 November, Cempaka weakened into a tropical low, while turning to the southwest. TCWC Perth last mentioned Cempaka on 1 December.

Geographic entities mentioned:
surface_form: Mount Agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
It has a range of on campus subjects and also provides online learning for long distance students. Boarding. The ALC provides accommodation for up to 96 tertiary boarders (and single students studying at ALC), the majority coming from the surrounding areas such as the Barossa Valley, Mid North, Riverland, Eyre Peninsula, Murray Mallee and South East.

Geographic entities mentioned:
surface_form: Barossa Valley
instance_of: Valley
countries: Australia
coordinates: lat: -34.533333333333
lon: 138.95
Ganslernhang. Ganslernhang (short: Ganslern) is a men's classic slalom World Cup ski course in Kitzbühel, Austria, competing for Hahnenkamm Races since 1937. It is located on the Hahnenkamm mountain (Kitzbühel Alps) in Kitzbühel, Tyrol, right next to even more famous &quot;Streif&quot; downhill course.

Geographic entities mentioned:
surface_form: Hahnenkamm
instance_of: Mountain
countries: Austria
coordinates: lat: 47.424166666667
lon: 12.365277777778
In 2009, before relatively short course, was lengthened by moving start higher up in the hill, at the same time new lift was built, with more comfortable standing area. Club5+. In 1986, elite Club5 was originally founded by prestigious classic downhill organizers: Kitzbühel, Wengen, Garmisch, Val d’Isère and Gröden, with goal to bring alpine ski sport on the highest levels possible.

Geographic entities mentioned:
surface_form: Gröden
instance_of: Valley
countries: Italy
coordinates: lat: 46.56
lon: 11.704722
Another proposed location for Rephidim is in northwestern Saudi Arabia north of the town of al-Bad, the ancient city of Midian. Some researchers suggest that Mount Sinai was not in the Sinai Peninsula, but in Midian, which is modern-day Saudi Arabia, and subsequently place Rephidim here as well. Jabal Maqla has been the subject of several explorations since the early 1980s.

Geographic entities mentioned:
surface_form: Jabal Maqla
instance_of: Mountain
countries: Saudi Arabia
coordinates: lat: 28.65416667
lon: 35.30583333
He died on 26 December 2021 in Athens at the age of 92. The Greek government announced three days of national mourning on December 27–29 with flags down to half-mast. His state funeral took place on 29 December at the church of Agios Spyridon in Pagrati and was attended by the country's highest authorities. The following day he was buried on the island of Lake Ioannina.

Geographic entities mentioned:
surface_form: Lake Ioannina
instance_of: Lake
countries: Greece
coordinates: lat: 39.6625
lon: 20.885
Powell Lake. Powell Lake is a lake in the northern Sunshine Coast region of British Columbia, Canada, adjacent to the city of Powell River, which sits on the low rise of land forming a natural dam between the lake and the Strait of Georgia at 46 metres above sea level. The lake flows to the ocean through Powell River and features Goat Island, a large mountainous island.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: powell lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0833
lon: -124.417
Powell Lake. Powell Lake is a lake in the northern Sunshine Coast region of British Columbia, Canada, adjacent to the city of Powell River, which sits on the low rise of land forming a natural dam between the lake and the Strait of Georgia at 46 metres above sea level. The lake flows to the ocean through Powell River and features Goat Island, a large mountainous island.

Geographic entities mentioned:
surface_form: powell lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0833
lon: -124.417
Tonstad. Tonstad is the administrative centre of the municipality of Sirdal in Agder county, Norway. The village is located at the northern end of the lake Sirdalsvatnet in the Sirdalen valley. The village has a population (2015) of 874, giving the village a population density of. Tonstad Hydroelectric Power Station and the Tonstad ski center are both located in and around this village.

Geographic entities mentioned:
surface_form: Sirdalsvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 58.4675
lon: 6.67638889
The district is named after the town. Location. Mpigi is an important transit town located approximately southwest of Kampala, Uganda's capital and largest city, along the Kampala–Masaka Road. The location of Mpigi town makes it an access point to the districts of Mpigi, Wakiso, Butambala, Gomba, Mityana, Kalungu and Kalangala, through various fishing landing sites on the shores of Lake Victoria.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
It is located at the head of the Coppermines Valley, above Coniston village. To its south-west is Raven Tor, a spur of Brim Fell, and to its north-west are Little How Crags and Great How Crags, on the eastern side of the north–south ridge leading to Swirl How. A dam built in 1717 enlarged the existing tarn to provide water for the mines and for the village below.

Geographic entities mentioned:
surface_form: Brim Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.3777
lon: -3.12381
surface_form: Swirl How
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.395661111111
lon: -3.1212305555556
Levers Water. Levers Water is a small lake in the English Lake District. It is located at the head of the Coppermines Valley, above Coniston village. To its south-west is Raven Tor, a spur of Brim Fell, and to its north-west are Little How Crags and Great How Crags, on the eastern side of the north–south ridge leading to Swirl How.

Geographic entities mentioned:
surface_form: levers water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.384134
lon: -3.11098
It is in the Spanish province of Huesca, the northernmost of three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif. Aneto is located in the Posets-Maladeta Natural Park, in the municipality of Benasque, Huesca province, an autonomous community of Aragon, Spain. It is part of the Maladeta massif and is located in the Benasque valley.

Geographic entities mentioned:
surface_form: Maladeta
instance_of: Mountain
countries: Spain
coordinates: lat: 42.64722222
lon: 0.63944444
Only when Friedrich von Parrot reached the top of the Maladeta in 1817, came the realisation that both Aneto as well as its neighbours the Pico del Medio, the Punta de Astorg, the Pico Maldito and la Aguja Schmidt Endell towered higher. Until then, the Monte Perdido had been considered the highest.

Geographic entities mentioned:
surface_form: Punta de Astorg
instance_of: Mountain
countries: Spain
coordinates: lat: 42.6404
lon: 0.644672
surface_form: Pico Maldito
instance_of: Mountain
countries: Spain
coordinates: lat: 42.639687
lon: 0.6401
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Only when Friedrich von Parrot reached the top of the Maladeta in 1817, came the realisation that both Aneto as well as its neighbours the Pico del Medio, the Punta de Astorg, the Pico Maldito and la Aguja Schmidt Endell towered higher. Until then, the Monte Perdido had been considered the highest.

Geographic entities mentioned:
surface_form: Monte Perdido
instance_of: Mountain
countries: Spain
coordinates: lat: 42.673888888889
lon: 0.033333333333333
There are three glaciers on the slopes of the mountain: the oldest, Aneto glacier on the north side; the Barrancos, alongside the Las Tempestades on the north-east side; and the Maladetas glacier on the north side (under the Maladeta peak). The rest cannot truly be defined as glaciers without contention, as they have lost all mobility and do not behave as such.

Geographic entities mentioned:
surface_form: Maladeta
instance_of: Mountain
countries: Spain
coordinates: lat: 42.64722222
lon: 0.63944444
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Thereafter Aneto entered into the dynamics of dissemination and popularization of the Pyrenees peaks. In France, its ascension became a great classic and every spring tourist to Bagneres de Luchon had to try it. Henry Spont wrote a book reflecting on this experience, simply titled Le Néthou, describing the trip, the schedule and recommended equipment. First winter ascent.

Geographic entities mentioned:
surface_form: néthou
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Aneto. Aneto is the highest mountain in the Pyrenees and in Aragon, Spain's third-highest mountain, reaching a height of. It is in the Spanish province of Huesca, the northernmost of three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
It is in the Spanish province of Huesca, the northernmost of three Aragonese provinces, south of the France–Spain border. It forms the southernmost part of the Maladeta massif. Aneto is located in the Posets-Maladeta Natural Park, in the municipality of Benasque, Huesca province, an autonomous community of Aragon, Spain. It is part of the Maladeta massif and is located in the Benasque valley.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
surface_form: posets
instance_of: Mountain
countries: Spain
coordinates: lat: 42.654481
lon: 0.4352
It was also previously known as La Malahite. The first traveller who is recorded as having seen it from the port (or pass) of Benasque, Louis Ramond de Carbonnières, simply described its appearance as &quot;needles of ice&quot; in 1787. The highest point of the Pyrenees eventually inherited the name of a village on its south-eastern side: Aneto.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
The highest point of the Pyrenees eventually inherited the name of a village on its south-eastern side: Aneto. The French, on hearing the Aragonese pronunciation of &quot;Aneto&quot;, retained the last two clearly accentuated phonetic syllables, &quot;ne&quot; and &quot;tu&quot;, ignoring the first syllable &quot;a&quot;.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
So these names were the toponyms that were then used. It took Émile Belloc's renowned work on the Pyrenees (notably on its hydrology, glaciology and etymology) to establish the name of Aneto as the official toponym; by 1898, he referred to it only by this name. History.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
It lies entirely in Spain, just south of the main ridge of the Pyrenees and the border between France and Spain. The peak lies in the north-east of the province of Huesca above the town of Benasque. Aneto occupies the eastern end of the Malditos Massif which primarily consists of a 6 km long ridge, running from north-west to south east at over 3000 m.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Although the valley to the north is the source of the Ésera river, which flows west and then south, the northern slopes of Aneto and its glacier drain into a sinkhole called Forau de Aigualluts in the Plan de Aigualluts and flows underground to the east where it resurfaces to empty into the Aran Valley and the Garonne river, flowing north into France and the Atlantic Ocean.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
The waters on the western and southern sides, flow into the Coronas and Llosas lakes respectively before draining separately into the river Ballibierna, which flows into the Esera, then the Cinca before joining the Ebro and flowing to the Mediterranean. Thus although Aneto does not lie on the main ridge of the Pyrenees, it does lie on the watershed between the Atlantic and the Mediterranean.

Geographic entities mentioned:
surface_form: cinca
instance_of: Watercourse
countries: Spain
coordinates: lat: 42.695649
lon: 0.040951
Today, global warming has reduced the portentous mass to eleven glaciers that total only three hundred acres. No one knows for sure when the melting process began but despite a slight advance in the '50s it has now accelerated rapidly, and it is expected that the Aneto permafrost and the glaciers of the Pyrenees could disappear around the middle of the 21st century.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
The high number of people who come to climb Aneto each year makes a significant contribution to the local economy. The vast majority of the people staying at the Renclusa Refuge are there solely to climb Aneto. By comparison many of the adjacent peaks, which are arguably finer climbs, see relatively few ascents and are comparatively quiet. First ascent.

Geographic entities mentioned:
surface_form: aneto
instance_of: Mountain
countries: Spain
coordinates: lat: 42.63099166666667
lon: 0.6566861111111112
Many of the animals can be found on protected land in Tunisia, but this is not the case in Morocco and Algeria, where many of the animals are still being outcompeted for food from livestock. One of the most important refuges is Djebel Chambi National Park, which holds the largest population in Tunisia.

Geographic entities mentioned:
surface_form: Djebel Chambi National Park
instance_of: Mountain
countries: Tunisia
coordinates: lat: 35.206666666667
lon: 8.6830555555556
The Forest Reserve covers a total of or of both public and privately owned land, one of the largest blocks of core forest in the state. Camel's Hump Forest Reserve wholly contains Camel's Hump State Park, which is home to Camel's Hump, the third highest mountain in Vermont.

Geographic entities mentioned:
surface_form: Camel's Hump
instance_of: Mountain
countries: United States
coordinates: lat: 44.319722222222225
lon: -72.8861111111111
95% of these rocks were eventually removed by uplifted-accelerated erosion. Most of the remaining rocks are exposed as 'roof pendants' in the eastern metamorphic zone. Mount Dana and Mount Gibbs are made of these metavolcanic rocks. Only 5% of the rocks exposed in Yosemite National Park are metamorphic. Pluton emplacement.

Geographic entities mentioned:
surface_form: Mount Dana
instance_of: Mountain
countries: United States
coordinates: lat: 37.8999
lon: -119.221
surface_form: Mount Gibbs
instance_of: Mountain
countries: United States
coordinates: lat: 37.8771
lon: -119.212
In the late Cenozoic, extensive volcanism occurred east of the park area. Within the Yosemite region, andesitic lava flows and lahars flowed north of the Grand Canyon of the Tuolumne and volcanic dikes and plugs developed from faults on the flanks of Mount Dana. There is also evidence for a great deal of rhyolitic ash covering the northern part of the Yosemite region 30 million years ago.

Geographic entities mentioned:
surface_form: Grand Canyon of the Tuolumne
instance_of: Valley
countries: United States
coordinates: lat: 37.9263
lon: -119.601
There is also evidence for a great deal of rhyolitic ash covering the northern part of the Yosemite region 30 million years ago. This and later ash deposits have been almost completely eroded away (especially during the ice ages). Volcanic activity persisted past 5 million years BP east of the current park borders in the Mono Lake and Long Valley areas.

Geographic entities mentioned:
surface_form: Long Valley
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
Volcanic activity persisted past 5 million years BP east of the current park borders in the Mono Lake and Long Valley areas. The most significant activity was the creation of the Long Valley Caldera about 700,000 years ago in which about 600 times as much material was erupted than in the 1980 eruption of Mt. Saint Helens.

Geographic entities mentioned:
surface_form: Long Valley Caldera
instance_of: Landform
countries: United States
coordinates: lat: 37.716666666667
lon: -118.88416666667
The results were hanging valleys and cascading waterfalls where the tributaries met the main streams. Additional uplift occurred when major faults developed to the east, especially the creation of Owens Valley from Basin and Range-associated extensional forces. Uplift of the Sierra accelerated again about two million years ago during the Pleistocene.

Geographic entities mentioned:
surface_form: Owens Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.8025
lon: -118.199722
(Example of a graben valley is Death Valley in California)
The uplifting and increased erosion exposed granitic rocks in the area to surface pressures, resulting in exfoliation (responsible for the rounded shape of the many granite domes in the park) and mass wasting following the numerous fracture joint planes (cracks; especially vertical ones) in the now solidified plutons.

Geographic entities mentioned:
surface_form: Death Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.45693888888889
lon: -116.86528055555556
In fact, only 10% of its widening and 12% of its excavation are thought to be the result of glaciation. Large, relatively unjointed volumes of granite form domes such as Half Dome and monoliths like the high El Capitan. Closely spaced joints lead to the creation of columns, pillars, and pinnacles such as Washington Column, Cathedral Spires, and Split Pinnacle. Glaciations.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
They are common in north-facing cirques and below modern glaciers in the High Sierra and are typically fresh, unstable, and often ice-cored. Good examples of Matthes moraines can be found below the Palisade Glacier (the largest glacier in the range), Lyell and Maclure glaciers in southern Yosemite N.P., and the smaller glaciers below Mount Dana, Kuna Peak, Mount Conness, and Matterhorn Peak.

Geographic entities mentioned:
surface_form: Mount Dana
instance_of: Mountain
countries: United States
coordinates: lat: 37.8999
lon: -119.221
surface_form: Matterhorn Peak
instance_of: Mountain
countries: United States
coordinates: lat: 38.093333333333
lon: -119.38277777778
Lee Vining Glacier carved Lee Vining Canyon and emptied into Lake Russell (the much enlarged ice age version of Mono Lake). Only the highest peaks, such as Mount Dana and Mount Conness, were not covered by glaciers. Retreating glaciers often left recessional moraines that impounded lakes such as Lake Yosemite (a shallow lake that periodically covered much of the floor of Yosemite Valley).

Geographic entities mentioned:
surface_form: Mount Dana
instance_of: Mountain
countries: United States
coordinates: lat: 37.8999
lon: -119.221
surface_form: Mount Conness
instance_of: Mountain
countries: United States
coordinates: lat: 37.967
lon: -119.321
The rounded side was where the glacier flowed over the dome and the steep side is where the glacier flowed away from it. The steepness is caused by glacial plucking of rock along fracture joints. Good examples in the park are Liberty Cap, Lembert Dome, and Mount Broderick. Half Dome was created by a different process, but erosion acting on jointing planes was still the major factor. Controversy.

Geographic entities mentioned:
surface_form: Mount Broderick
instance_of: Mountain
countries: United States
coordinates: lat: 37.73354
lon: -119.53516
The steepness is caused by glacial plucking of rock along fracture joints. Good examples in the park are Liberty Cap, Lembert Dome, and Mount Broderick. Half Dome was created by a different process, but erosion acting on jointing planes was still the major factor. Controversy. The origin of the geological landscapes of the park have been under debate since 1865.

Geographic entities mentioned:
surface_form: Half Dome
instance_of: Mountain
countries: United States
coordinates: lat: 37.746
lon: -119.53316666667
Controversy. The origin of the geological landscapes of the park have been under debate since 1865. At that time, Josiah Whitney, then chief geologist of California, proposed that Yosemite Valley is a graben: a downdropped block of land surrounded by faults. John Muir proposed that Yosemite Valley and Hetch Hetchy Valley were formed purely by glacial action. In 1930, François E.

Geographic entities mentioned:
surface_form: Yosemite Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.721694444444445
lon: -119.646
Stormberg Mountains. The Stormberg is a range of mountains situated in the Eastern Cape province of South Africa, are an easterly extension of the Bamboesberge and form an outlier of the greater Drakensberg mountain range. They form part of the 'Amatola and Stormberg' region which includes major towns like Grahamstown, East London and Port Alfred.

Geographic entities mentioned:
surface_form: stormberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -31.4475
lon: 26.7175
They form part of the 'Amatola and Stormberg' region which includes major towns like Grahamstown, East London and Port Alfred. Towns in the Stormberg Mountains include Sterkstroom, Jamestown, Molteno, Dordrecht, Barkly East, Rhodes and Steynsburg. South Africa's only ski resort, Tiffindell, is also situated in these mountains. Geology.

Geographic entities mentioned:
surface_form: stormberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -31.4475
lon: 26.7175
South Africa's only ski resort, Tiffindell, is also situated in these mountains. Geology. Geologically, the mountains form part of the Stormberg Series of the Karoo System where some of the only workable coal seams in the Cape are to be found. These coal fields are being explored for possible coal bed methane extraction. History.

Geographic entities mentioned:
surface_form: stormberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -31.4475
lon: 26.7175
The Nguni migrations saw the arrival of the Xhosa herders from the north and the displacement of the Khoisan. The subsequent arrival of the Cape colonists in the area resulted in a series of 'frontier wars' which led to the region's incorporation into the Cape Colony. During the Second Boer War, this was the site of the Battle of Stormberg, fought on 9 December 1899.

Geographic entities mentioned:
surface_form: stormberg
instance_of: Mountain
countries: South Africa
coordinates: lat: -31.4475
lon: 26.7175
Miche Wabun Peak. Miche Wabun Peak () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Miche Wabun Peak is in the northeastern section of Glacier National Park and is north of Miche Wabun Lake.

Geographic entities mentioned:
surface_form: Miche Wabun Lake
instance_of: Lake
countries: United States
coordinates: lat: 48.9575
lon: -113.82
surface_form: miche wabun peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.9697
lon: -113.831
Miche Wabun Peak. Miche Wabun Peak () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Miche Wabun Peak is in the northeastern section of Glacier National Park and is north of Miche Wabun Lake.

Geographic entities mentioned:
surface_form: miche wabun peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.9697
lon: -113.831
Montagnes du Cibao. The Montagnes du Cibao (&quot;Mountains of Cibao&quot;) are located in Haiti. The highest point of the range, Morne du Cibao, is 2,280 meters (7,480 feet) above sea level, making it the third highest peak in Haiti, behind Pic la Selle and Pic Macaya.

Geographic entities mentioned:
surface_form: Morne du Cibao
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.357
lon: -72.259
surface_form: Pic la Selle
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.366666666667
lon: -71.983333333333
surface_form: Pic Macaya
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.3825
lon: -74.025
surface_form: morne du cibao
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.357
lon: -72.259
surface_form: pic macaya
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.3825
lon: -74.025
surface_form: pic la selle
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.366666666667
lon: -71.983333333333
Montagnes du Cibao. The Montagnes du Cibao (&quot;Mountains of Cibao&quot;) are located in Haiti. The highest point of the range, Morne du Cibao, is 2,280 meters (7,480 feet) above sea level, making it the third highest peak in Haiti, behind Pic la Selle and Pic Macaya.

Geographic entities mentioned:
surface_form: montagnes du cibao
instance_of: Mountain
countries: Haiti
coordinates: lat: 18.216666666667
lon: -71.966666666667
Big Pasture Plateau. The Big Pasture Plateau () is a karstified mountain plateau in the Kamnik–Savinja Alps northeast of Kamnik, Slovenia. It measures and has an average elevation of above sea level. Its highest point is Mount Gradišče, at.

Geographic entities mentioned:
surface_form: big pasture plateau
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.2955
lon: 14.6535
It measures and has an average elevation of above sea level. Its highest point is Mount Gradišče, at. There are numerous herders' dwellings that comprise several settlement areas: &quot;Velika Planina&quot; 'Big Pasture', &quot;Mala Planina&quot; 'Little Pasture', &quot;Gojška Planina&quot; 'Gozd Pasture' (named for the village of Gozd), &quot;Tiha Dolina&quot; 'Quiet Valley', and others.

Geographic entities mentioned:
surface_form: velika planina
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.2955
lon: 14.6535
The Big Pasture Plateau is a tourist destination both in winter as a ski resort and in summer as a place for relaxation. History. There is evidence that man has been present on the Big Pasture Plateau since prehistoric times. In Medieval times the plateau was used for pasturing. The oldest huts, which date from the 16th century, are nearly identical to the present Preskar Hut ().

Geographic entities mentioned:
surface_form: big pasture plateau
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.2955
lon: 14.6535
During his three decades at the helm of the Hadassah HMO, he was credited with the renovation of the hospital campus on Mount Scopus after the Six-Day War, and the construction of a new Hadassah medical center at Ein Kerem. He also sat on 14 different government committees, influencing Israeli health-care legislation.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
7 May 1994 — Zaragoza to Pamplona,
Stage 14. 8 May 1994 — Pamplona to Sierra de la Demanda,
Stage 15. 9 May 1994 — Santo Domingo de la Calzada to Santander,
Stage 16. 10 May 1994 — Santander to Lakes of Covadonga,
Stage 17. 11 May 1994 — Cangas de Onís to Monte Naranco,
Stage 18. 12 May 1994 — Ávila to Ávila,
Stage 19. 13 May 1994 — Ávila to Palazuelos de Eresma,
Stage 20.

Geographic entities mentioned:
surface_form: Lakes of Covadonga
instance_of: Group of lakes
countries: Spain
coordinates: lat: 43.26829288409789
lon: -4.985873734085007
8 May 1994 — Pamplona to Sierra de la Demanda,
Stage 15. 9 May 1994 — Santo Domingo de la Calzada to Santander,
Stage 16. 10 May 1994 — Santander to Lakes of Covadonga,
Stage 17. 11 May 1994 — Cangas de Onís to Monte Naranco,
Stage 18. 12 May 1994 — Ávila to Ávila,
Stage 19. 13 May 1994 — Ávila to Palazuelos de Eresma,
Stage 20. 14 May 1994 — Segovia to Palazuelos de Eresma, (ITT)
Stage 21.

Geographic entities mentioned:
surface_form: Monte Naranco
instance_of: Mountain
countries: Spain
coordinates: lat: 43.38333333
lon: -5.86666667
Origin. Dhimsa originated in Koraput district in the Odisha State, but has almost become an official dance of Visakhapatnam. Dhimsa means &quot;sound of the foot steps&quot;. Dhimsa is in the groove with the culture of this region, especially with places near Araku Valley and Borra Caves. Earlier unmarried youth used to dance. There is no discrimination as to who gets to join in the dance.

Geographic entities mentioned:
surface_form: Araku Valley
instance_of: Valley
countries: India
coordinates: lat: 18.3333
lon: 82.8667
Archaeological interactions with neighbouring cultures. BMAC materials have been found in the Indus Valley civilisation, on the Iranian Plateau, and in the Persian Gulf. Finds within BMAC sites provide further evidence of trade and cultural contacts. They include an Elamite-type cylinder seal and a Harappan seal stamped with an elephant and Indus script found at Gonur-depe.

Geographic entities mentioned:
surface_form: Iranian Plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
There is evidence of sustained contact between the BMAC and the Eurasian steppes to the north, intensifying. In the delta of the Amu Darya where it reaches the Aral Sea, its waters were channelled for irrigation agriculture by people whose remains resemble those of the nomads of the Andronovo culture.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
Genetics. In 2019, Narasimhan and co-authors analysed BMAC skeletons from the Bronze Age sites of Bustan, Dzharkutan, Gonur Tepe, and Sappali Tepe. The BMAC population largely derived from preceding local Copper Age peoples who were in turn related to Neolithic farmers from the Iranian plateau and to a lesser extent early Anatolian farmers, as well as hunter-gatherers from Western Siberia (WSHG).

Geographic entities mentioned:
surface_form: Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Geography. The Roc from the ridge in the section between Montcorvé Pass (3,875 m) and the &quot;Fenêtre de Montcorvé&quot; Pass (3,998 m), the culmination of the Orco - Dora watershed from where the long Valsavarenche-Cogne Valley ridge begins towards the north, including the summit of the Gran Paradiso (4,061 m) and other important peaks of the group, ending with the Grivola (3,969 m)

Geographic entities mentioned:
surface_form: Cogne Valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.625
lon: 7.325
surface_form: Grivola
instance_of: Mountain
countries: Italy
coordinates: lat: 45.596666666667
lon: 7.2644444444444
surface_form: cogne valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.625
lon: 7.325
surface_form: gran paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
surface_form: grivola
instance_of: Mountain
countries: Italy
coordinates: lat: 45.596666666667
lon: 7.2644444444444
Roc (Gran Paradiso). The Roc (IPA [ʁok]) is a mountain of the Gran Paradiso massif, in the Graian Alps in Italy. It is located between the Aosta Valley and Piedmont regions and is the highest point in the Metropolitan City of Turin. Geography.

Geographic entities mentioned:
surface_form: roc (gran paradiso)
instance_of: Mountain
countries: Italy
coordinates: lat: 45.5156
lon: 7.26861
surface_form: gran paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
Roc (Gran Paradiso). The Roc (IPA [ʁok]) is a mountain of the Gran Paradiso massif, in the Graian Alps in Italy. It is located between the Aosta Valley and Piedmont regions and is the highest point in the Metropolitan City of Turin. Geography.

Geographic entities mentioned:
surface_form: gran paradiso
instance_of: Mountain
countries: Italy
coordinates: lat: 45.533333333333
lon: 7.2666666666667
It is endemic to Australia. It was described in 1994 by Australian arachnologists Robert Raven and Tracey Churchill. The specific epithet &quot;nuganuga&quot; refers to the type locality. Distribution and habitat. The species occurs in Central Queensland. The type locality is Lake Nuga Nuga in the Central Highlands region.

Geographic entities mentioned:
surface_form: Lake Nuga Nuga
instance_of: Lake
countries: Australia
coordinates: lat: -24.995
lon: 148.679
It is situated in the Lakes Region of central New Hampshire, in the towns of Alexandria, Bridgewater, Bristol, and Hebron. Its area of places it behind only Lake Winnipesaukee and Squam Lake among lakes located entirely within New Hampshire, and fourth in the state overall, when Umbagog Lake on the Maine border is included. Geography. Newfound Lake has of shoreline.

Geographic entities mentioned:
surface_form: Lake Winnipesaukee
instance_of: Lake
countries: United States
coordinates: lat: 43.598888888889
lon: -71.323055555556
surface_form: Squam Lake
instance_of: Lake
countries: United States
coordinates: lat: 43.745277777778
lon: -71.526111111111
surface_form: Umbagog Lake
instance_of: Lake
countries: United States
coordinates: lat: 44.75
lon: -71.05
Two thirds of the lake was incorporated as Bristol on June 24, 1819. Fish. In 1890, the New Hampshire Fish and Game Commissioner stocked 15,000 landlocked salmon into the Fowler River, and in 1898, the NH Fish and Game Commission stocked 40,000 whitefish from Lake Superior.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The first, the &quot;Pioneer&quot; owned by Capt. George W. Dow, was placed in the lake in 1865. It was destroyed by fire. In 1878, Edward M. Drake put the &quot;Cardigan&quot; on the lake, which plied until 1883. That same year, the &quot;Lady Helen&quot; joined it, but was also destroyed in a fire. In May 1900, the &quot;Stella-Marion&quot; was launched at Kimball's beach.

Geographic entities mentioned:
surface_form: Cardigan
instance_of: Mountain
countries: United States
coordinates: lat: 43.649794444444
lon: -71.914805555556
Newfound Lake. Newfound Lake is located in Grafton County, New Hampshire, United States. It is situated in the Lakes Region of central New Hampshire, in the towns of Alexandria, Bridgewater, Bristol, and Hebron.

Geographic entities mentioned:
surface_form: newfound lake
instance_of: Lake
countries: United States
coordinates: lat: 43.662778
lon: -71.775278
Its area of places it behind only Lake Winnipesaukee and Squam Lake among lakes located entirely within New Hampshire, and fourth in the state overall, when Umbagog Lake on the Maine border is included. Geography. Newfound Lake has of shoreline. The lake is about wide and long. The deepest point is. Major tributaries include the Fowler River and the Cockermouth River.

Geographic entities mentioned:
surface_form: newfound lake
instance_of: Lake
countries: United States
coordinates: lat: 43.662778
lon: -71.775278