Sarmila/GeoWiki-Features huggingface dataset:
Description. Jello Tower is located within the Park Avenue section of Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: jello tower
instance_of: Mountain
coordinates: lat: 38.62978
lon: -109.60187
surface_form: dewey
instance_of: Mountain
coordinates: lat: -65.9
lon: -64.3167
Description. Jello Tower is located within the Park Avenue section of Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member. Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
surface_form: trail
instance_of: Mountain
coordinates: lat: -67.2
lon: 50.85
Climate. According to the Köppen climate classification system, Jello Tower is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average. Summer temperatures often exceed. Winters are cold, with highs averaging, and lows averaging.

Geographic entities mentioned:
surface_form: park
instance_of: Mountain
coordinates: lat: -67.2333
lon: 51
Jello Tower. Jello Tower is a pillar in Grand County, Utah, United States. Description. Jello Tower is located within the Park Avenue section of Arches National Park and like many of the rock formations in the park, it is composed of Entrada Sandstone, specifically the Slick Rock Member overlaying the Dewey Bridge Member.

Geographic entities mentioned:
surface_form: jello tower
instance_of: Mountain
coordinates: lat: 38.62978
lon: -109.60187
Topographic relief is significant as the summit rises above the Park Avenue Trail in laterally. Precipitation runoff from Jello Tower drains to the Colorado River via Courthouse Wash. The first ascent of the summit was made in November 1986 by Charlie Fowler and Sue Wint via &quot;Soft Parade&quot; rock-climbing route.

Geographic entities mentioned:
surface_form: jello tower
instance_of: Mountain
coordinates: lat: 38.62978
lon: -109.60187
Climate. According to the Köppen climate classification system, Jello Tower is located in a cold semi-arid climate zone with cold winters and hot summers. Spring and fall are the most favorable seasons to experience Arches National Park, when highs average and lows average. Summer temperatures often exceed. Winters are cold, with highs averaging, and lows averaging.

Geographic entities mentioned:
surface_form: jello tower
instance_of: Mountain
coordinates: lat: 38.62978
lon: -109.60187
Alison Des Forges. Alison Des Forges (née Liebhafsky; August 20, 1942 – February 12, 2009) was an American historian and human rights activist who specialized in the African Great Lakes region, particularly the 1994 Rwandan genocide. At the time of her death, she was a senior advisor for the African continent at Human Rights Watch. She died in a plane crash on 12 February 2009. Life.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Describing the politics of the court during the reign of Yuhi Musinga, it shows how divisions among different groups in Rwanda shaped their responses to colonial governments, missionaries and traders. She specialized in the African Great Lakes region and studied the Rwandan genocide. She was also an authority on human rights violations in the Democratic Republic of Congo and in Burundi.

Geographic entities mentioned:
surface_form: African Great Lakes
instance_of: Group of lakes
countries: Burundi
Zambia
Kenya
Democratic Republic of the Congo
Malawi
Mozambique
Rwanda
Tanzania
Uganda
Ethiopia
coordinates: lat: -8
lon: 35
Little Ball Lake. Little Ball Lake is a small lake in Cassiar Land District of northwestern British Columbia, Canada. It lies at the head of the Little Iskut River just south of Kounugu Mountain at the southeastern end of the Spectrum Range in Mount Edziza Provincial Park. The lake contains one island and Ball Creek flows in its vicinity.

Geographic entities mentioned:
surface_form: Little Iskut River
instance_of: Watercourse
countries: Canada
coordinates: lat: 57.448889
lon: -130.268611
surface_form: Kounugu Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 57.3647
lon: -130.5973
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The lake contains one island and Ball Creek flows in its vicinity. Little Ball Lake was referred to as Kounugu Lake by Canadian volcanologist Jack Souther who studied the Mount Edziza volcanic complex in detail for many years. Kounugu was the guardian of fresh water in Tahltan folklore &quot;who slept throughout the day on top of the well that contained his treasure&quot;.

Geographic entities mentioned:
surface_form: Mount Edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
surface_form: little ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
It lies at the head of the Little Iskut River just south of Kounugu Mountain at the southeastern end of the Spectrum Range in Mount Edziza Provincial Park. The lake contains one island and Ball Creek flows in its vicinity. Little Ball Lake was referred to as Kounugu Lake by Canadian volcanologist Jack Souther who studied the Mount Edziza volcanic complex in detail for many years.

Geographic entities mentioned:
surface_form: ball creek
instance_of: Watercourse
countries: Canada
coordinates: lat: 58.38284
lon: -129.18684
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
Little Ball Lake. Little Ball Lake is a small lake in Cassiar Land District of northwestern British Columbia, Canada. It lies at the head of the Little Iskut River just south of Kounugu Mountain at the southeastern end of the Spectrum Range in Mount Edziza Provincial Park. The lake contains one island and Ball Creek flows in its vicinity.

Geographic entities mentioned:
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
surface_form: little ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
Little Ball Lake. Little Ball Lake is a small lake in Cassiar Land District of northwestern British Columbia, Canada. It lies at the head of the Little Iskut River just south of Kounugu Mountain at the southeastern end of the Spectrum Range in Mount Edziza Provincial Park. The lake contains one island and Ball Creek flows in its vicinity.

Geographic entities mentioned:
surface_form: ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 49.7
lon: -125.317
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: little ball lake
instance_of: Lake
countries: Canada
coordinates: lat: 57.34889
lon: -130.58917
Little Ball Lake's mean annual discharge is estimated at. Its watershed covers which is entirely within Mount Edziza Provincial Park. The watershed drains parts of the Mount Edziza volcanic complex. The watershed's land cover is classified as 43% barren, 25.4% herbaceous, 20.4% shrubland, 10.1% water, 0.7% snow/glacier and 0.5% conifer forest.

Geographic entities mentioned:
surface_form: mount edziza volcanic complex
instance_of: Mountain
countries: Canada
coordinates: lat: 57.5
lon: -130.6
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Kounugu was the guardian of fresh water in Tahltan folklore &quot;who slept throughout the day on top of the well that contained his treasure&quot;. Little Ball Lake is one of several lakes that are large enough to be used by float-equipped aircraft to gain access to Mount Edziza Provincial Park.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
However, landing on the lake with a private aircraft requires a letter of authorization from the BC Parks Stikine Senior Park Ranger. Little Ball Lake's mean annual discharge is estimated at. Its watershed covers which is entirely within Mount Edziza Provincial Park. The watershed drains parts of the Mount Edziza volcanic complex.

Geographic entities mentioned:
surface_form: edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
surface_form: mount edziza
instance_of: Mountain
countries: Canada
coordinates: lat: 57.715555555555554
lon: -130.63472222222222
Great Fergana Canal. The Great Fergana Canal (,,) is an irrigation canal located on the Fergana Valley between Uzbekistan and Tajikistan in Central Asia. The project was constructed in 1939 by 160,000 Uzbek and Tajik (mainly uzbek) collective farm workers from the former Soviet Union and was completed in forty-five days.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
A negative ecological change caused by the Great Fergana Canal created was the desiccation of the Aral Sea as a result of poor water management and overuse. Uses.

Geographic entities mentioned:
surface_form: Aral Sea
instance_of: Lake
countries: Kazakhstan
Uzbekistan
Russian Empire
Soviet Union
coordinates: lat: 45
lon: 60
He made multiple first ascents. On August 26, 1921, he completed the first ascent of Middle Palisade by the south-west chute with Ansel Hall. He was the author of numerous articles for the Sierra Club and the California Historical Society, some of which were reprinted in book form. In 1956-59 he was editor of the &quot;American Alpine Journal&quot; published by the American Alpine Club.

Geographic entities mentioned:
surface_form: Middle Palisade
instance_of: Mountain
countries: United States
coordinates: lat: 37.0705
lon: -118.4682
His half brother was the Los Angeles architect Robert D. Farquhar, who moved in with the Farquhars in Berkeley in 1953. Marjorie Bridge Farquhar died in 1999 in San Francisco. Legacy. Mount Farquhar (12,893'), located northwest of Mount Brewer in Kings Canyon National Park, was named in his honor. Since 1970, the Sierra Club has given the Francis P. Farquhar Mountaineering Award in his honor.

Geographic entities mentioned:
surface_form: Mount Farquhar
instance_of: Mountain
countries: United States
coordinates: lat: 36.7286
lon: -118.499
surface_form: Mount Brewer
instance_of: Mountain
countries: United States
coordinates: lat: 36.7085
lon: -118.485
The Ganges – navigable throughout the year – was the principal river highway across the vast Indo-Gangetic Plain. Vessels capable of accommodating five hundred merchants were known to ply this river in the ancient period; it served as a major trade route, as goods were transported from Pataliputra to the Bay of Bengal and further, to ports in Sri Lanka and Southeast Asia.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Various tales and stories are told through oral tradition, such as, among many more, the legends of the &quot;Bogeyman&quot;, the &quot;Chasse-galerie&quot;, the &quot;Black Horse of Trois-Pistoles&quot;, the &quot;Complainte de Cadieux&quot;, the &quot;Corriveau&quot;, the &quot;dancing devil of Saint-Ambroise&quot;, the &quot;Giant Beaupré&quot;, the &quot;monsters of the lakes Pohénégamook&quot; and &quot;Memphremagog&quot;, of &quot;Quebec Bridge&quot; (called the Devil's Bridge), the &quot;Rocher Percé&quot; and of &quot;Rose Latulipe&quot;, for example.

Geographic entities mentioned:
surface_form: Pohénégamook
instance_of: Lake
countries: Canada
coordinates: lat: 47.488055555556
lon: -69.268055555556
He is the first Iranian man to climb Vinson Massif in Antarctica, and the first Iranian man to complete the mountaineering challenge of the Seven Summits, climbing the highest peaks on seven continents. Life and career. Andrew was born and raised in Iran (Iranian name: Amin), but moved to Canada at age of 25 for PhD studies.

Geographic entities mentioned:
surface_form: Vinson Massif
instance_of: Mountain
coordinates: lat: -78.52555555555556
lon: -85.61722222222222
Nechako Canyon Protected Area. Nechako Canyon Protected Area is a protected area of the BC Parks system, located on the Nechako River between Knewstubb Lake (formed by the Kenny Dam of the Nechako Diversion) and Cheslatta Falls at the mouth of the Cheslatta River.

Geographic entities mentioned:
surface_form: Knewstubb Lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.5167
lon: -124.817
The Nechako Canyon, also known as the Grand Canyon of the Nechako, is carved into a lava plateau and features erosive formations such as rock walls, overhanging cliffs, pinnacles and other formations, and the protected area includes Cheslatta Falls.

Geographic entities mentioned:
surface_form: Nechako Canyon
instance_of: Valley
countries: Canada
coordinates: lat: 53.6
lon: -124.933
Cerro de la Gloria. The &quot;Cerro de la Gloria&quot; (&quot;Glory Hill&quot;) is a small mount located in the city of Mendoza, Argentina, at the General San Martín Park. It features a huge memorial monument to the Army of the Andes at the top.

Geographic entities mentioned:
surface_form: mendoza
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.35
lon: -68.3
surface_form: cerro de la gloria
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.8886
lon: -68.8858
Cerro de la Gloria. The &quot;Cerro de la Gloria&quot; (&quot;Glory Hill&quot;) is a small mount located in the city of Mendoza, Argentina, at the General San Martín Park. It features a huge memorial monument to the Army of the Andes at the top.

Geographic entities mentioned:
surface_form: cerro de la gloria
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.8886
lon: -68.8858
Trekking in Paithalmala can be challenging due to frequent rain, leeches, and occasional elephant visits. Monsoon is followed by a cool climate in Paithalmala and the grass surrounding the hills grow to their fullest size, making it difficult to walk through. As they grow above seven feet, finding the regular way becomes a difficult task.

Geographic entities mentioned:
surface_form: hills
instance_of: Mountain
countries: India
coordinates: lat: 23.166666666667
lon: 92.833333333333
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
Paithalmala. Paithalmala is a hill station in the Kannur district of Kerala in India, located near Pottenplave. At a height of 4500 ft above from sea level, it is the highest geographic peak in Kannur. It is located 40 km from Taliparamba and 65 km from Kannur. Nestled in the Kerala Karnataka border near to Kodagu forests, it lies in the Western Ghats. Trekking at Paithalmala.

Geographic entities mentioned:
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
At a height of 4500 ft above from sea level, it is the highest geographic peak in Kannur. It is located 40 km from Taliparamba and 65 km from Kannur. Nestled in the Kerala Karnataka border near to Kodagu forests, it lies in the Western Ghats. Trekking at Paithalmala. Paithalmala is a popular trekking destination. There are two trekking seasons at Paithalmala: monsoon and summer.

Geographic entities mentioned:
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
It is located 40 km from Taliparamba and 65 km from Kannur. Nestled in the Kerala Karnataka border near to Kodagu forests, it lies in the Western Ghats. Trekking at Paithalmala. Paithalmala is a popular trekking destination. There are two trekking seasons at Paithalmala: monsoon and summer. Trekking in Paithalmala can be challenging due to frequent rain, leeches, and occasional elephant visits.

Geographic entities mentioned:
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
Trekking at Paithalmala. Paithalmala is a popular trekking destination. There are two trekking seasons at Paithalmala: monsoon and summer. Trekking in Paithalmala can be challenging due to frequent rain, leeches, and occasional elephant visits. Monsoon is followed by a cool climate in Paithalmala and the grass surrounding the hills grow to their fullest size, making it difficult to walk through.

Geographic entities mentioned:
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
Mobile networks other than BSNL are not available in the vicinity. Problems with Pollution. Since accessibility to it is limited, Paithalmala is one of the few places in Kerala where nature is largely unaffected by human invasion. Recently however, visitors have increasingly tended to use it as a drinking spot.

Geographic entities mentioned:
surface_form: paithalmala
instance_of: Mountain
countries: India
coordinates: lat: 12.19273611
lon: 75.58614444
They are:, and. Libra Dohko. is the last living former-generation Saint, one of the two survivors from the previous Holy War along with Shion. Athena charged him with the secret mission to keep watch over a sealed evil and so, for the past 236 years, he has never left his post at the Five Old Peaks in Rozan, China, not even to answer the Pope's summon to an urgent meeting, the.

Geographic entities mentioned:
surface_form: Rozan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.5725
lon: 115.97333333333
Geographically, &quot;Coppinsiella&quot; is predominantly found across Eurasia, ranging from Scotland, Southern Scandinavia, and Estonia in the north to the Mediterranean regions, extending from Spain to the Caspian Sea coast in the east, and reaching as far south as Israel.

Geographic entities mentioned:
surface_form: Caspian Sea
instance_of: Body of water
Lake
countries: Iran
Russia
Kazakhstan
Azerbaijan
Turkmenistan
Russian Empire
Soviet Union
coordinates: lat: 42
lon: 50.5
The columns, statues and large decorations were executed in the quarry that the Jesuits had in the &quot;Hacienda de Yurac&quot;, in the nearby parish of Píntag; the rest of the material was brought from a quarry on the western slope of El Panecillo hill, next to the city.

Geographic entities mentioned:
surface_form: El Panecillo
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.22861111111111
lon: -78.518611111111
Feudalism was abolished, the monastery was closed and fell into ruin and many of its assets were plundered. Fortunately, the remains of the founder, William of Montevergine, were moved to Montevergine. The village actively participated in the Carbonari uprisings, but the dreams of its citizens were shattered.

Geographic entities mentioned:
surface_form: Montevergine
instance_of: Mountain
countries: Italy
coordinates: lat: 40.9393747
lon: 14.7244325
Cheakamus River. The Cheakamus River (pron. CHEEK-a-mus) is a tributary of the Squamish River, beginning at the terminus of McBride Glacier on Mount Sir Richard in Garibaldi Provincial Park upstream from Cheakamus Lake on the southeastern outskirts of the resort area of Whistler. The river flows into Cheakamus Lake before exiting it and flowing northwest until it turns south and enters Daisy Lake.

Geographic entities mentioned:
surface_form: Mount Sir Richard
instance_of: Mountain
countries: Canada
coordinates: lat: 49.9639
lon: -122.7018
surface_form: Cheakamus Lake
instance_of: Lake
countries: Canada
coordinates: lat: 50.0081
lon: -122.92
He took part as a volunteer in the First World War, and after the war he joined the National Fascist Party; during the Fascist period he was President of the National Marble Federation from 1928 to 1934 (his family owned a granite quarry near Lake Orta) and a member of the board of directors of Confindustria from 1934 to 1943. In 1939, he became a member of the Chamber of Fasces and Corporations.

Geographic entities mentioned:
surface_form: Lake Orta
instance_of: Lake
countries: Italy
coordinates: lat: 45.8098
lon: 8.3963
Gibson Lake (Frontenac County). Gibson Lake is an endorheic lake in the municipality of South Frontenac, Frontenac County in Eastern Ontario, Canada. It lies within Frontenac Provincial Park.

Geographic entities mentioned:
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 45.8789
lon: -78.9194
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 46.7325
lon: -82.2014
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.53277777777778
lon: -84.80722222222222
surface_form: gibson lake (frontenac county)
instance_of: Lake
countries: Canada
coordinates: lat: 44.5772
lon: -76.4894
surface_form: gibson lake
instance_of: Body of water
Lake
countries: Canada
coordinates: lat: 46.8819
lon: -80.9928
surface_form: gibson lake
instance_of: Body of water
Lake
countries: Canada
coordinates: lat: 50.40224
lon: -89.25457
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 48.4489
lon: -80.8108
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 43.9553
lon: -79.8253
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.96611111111111
lon: -79.74916666666667
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.33972222222222
lon: -85.33305555555556
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 46.2444
lon: -78.1831
Gibson Lake (Frontenac County). Gibson Lake is an endorheic lake in the municipality of South Frontenac, Frontenac County in Eastern Ontario, Canada. It lies within Frontenac Provincial Park.

Geographic entities mentioned:
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 45.8789
lon: -78.9194
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 46.7325
lon: -82.2014
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 47.53277777777778
lon: -84.80722222222222
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.5772
lon: -76.4894
surface_form: gibson lake
instance_of: Body of water
Lake
countries: Canada
coordinates: lat: 46.8819
lon: -80.9928
surface_form: gibson lake
instance_of: Body of water
Lake
countries: Canada
coordinates: lat: 50.40224
lon: -89.25457
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 48.4489
lon: -80.8108
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 43.9553
lon: -79.8253
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.96611111111111
lon: -79.74916666666667
surface_form: gibson lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.33972222222222
lon: -85.33305555555556
surface_form: gibson lake
instance_of: Body of water
countries: Canada
coordinates: lat: 46.2444
lon: -78.1831
Mont Blanc Tunnel. The Mont Blanc Tunnel (,) is a highway tunnel between France and Italy, under Mont Blanc in the Alps. It links Chamonix, Haute-Savoie, France with Courmayeur, Aosta Valley, Italy, via the French Route Nationale 205 and the Italian Traforo T1 (forming the European route E25), in particular the motorways serving Geneva (A40 of France) and Turin (A5 of Italy).

Geographic entities mentioned:
surface_form: Mont Blanc
instance_of: Mountain
countries: France
Italy
coordinates: lat: 45.83277777777778
lon: 6.865
It reduces the route from France to Turin by and to Milan by. Northeast of Mont Blanc's summit, the tunnel is about southwest of the tripoint with Switzerland, near Mont Dolent. The agreement between France and Italy on building a tunnel was signed in 1949.

Geographic entities mentioned:
surface_form: Mont Dolent
instance_of: Mountain
countries: Switzerland
Italy
France
coordinates: lat: 45.9225
lon: 7.0461111111111
The tunnel consists of a single gallery with a two-lane dual direction road. At the time of its construction, it was twice as long as any existing highway tunnel. The tunnel passes almost exactly under the summit of the Aiguille du Midi. At this spot, it lies beneath the surface, making it the world's second deepest operational tunnel after the Gotthard Base Tunnel.

Geographic entities mentioned:
surface_form: Aiguille du Midi
instance_of: Mountain
countries: France
coordinates: lat: 45.878888888889
lon: 6.8875
At the time, the area was still Menominee territory and required special permission from the United States War Department. His lumber interest in Menominee territory made him an important participant in the 1827 treaty negotiations at Lake Butte des Morts, as his boats transported all of the American delegates and his lumber supplies were used for the construction of all of the site facilities.

Geographic entities mentioned:
surface_form: Lake Butte des Morts
instance_of: Lake
countries: United States
coordinates: lat: 44.073055555556
lon: -88.641944444444
In addition, the temple of Sennyu-ji houses the tombs of the emperors from Shijō to Kōmei. Other sites in Kyoto include Arashiyama, the Gion and Ponto-chō geisha quarters, the Philosopher's Walk, and the canals that line some of the older streets. The &quot;Historic Monuments of Ancient Kyoto&quot; are listed by the UNESCO as a World Heritage Site.

Geographic entities mentioned:
surface_form: Arashiyama
instance_of: Mountain
countries: Japan
coordinates: lat: 35.00958333333333
lon: 135.6663888888889
Background. Nicaea, located on the eastern shore of Lake Askania, had been captured from the Byzantine Empire by the Seljuk Turks in 1081, and formed the capital of the Sultanate of Rûm. In 1096, the People's Crusade, the first stage of the First Crusade, had plundered the land surrounding the city, before being destroyed by the Turks.

Geographic entities mentioned:
surface_form: Lake Askania
instance_of: Lake
countries: Turkey
coordinates: lat: 40.443611111111
lon: 29.508333333333
It was composed of Dani Christmas, Anna Plichta, Sara Olsson, Vita Heine and Silvia Valsecchi. Twenty kilometers away, they were joined by Kiesenhofer. In the descent of the pass of Murs, the groups were seven minutes and twenty-five seconds ahead. After Blavac, Anna Plichta went off alone and she had a lead of a minute thirty at the foot of Mont Ventoux. On the ascent, Kiesenhofer joined her.

Geographic entities mentioned:
surface_form: Mont Ventoux
instance_of: Mountain
countries: France
coordinates: lat: 44.166666666667
lon: 5.2833333333333
Salgó Castle. Salgó Castle is a Hungarian stronghold near Salgótarján, Nógrád county, 120 km from Budapest. Originally built as a tower by the Kacsics clan in the 13th century to withstand the Mongol invasions of the 13th century, it was later renovated into a fortress by King Béla IV.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
Ownership of the castle eventually passed to Bálint Balassi and his family, one member of the family neglected the castle and left it in ruins. Today Salgó Castle is a well-known tourist spot. Salgó Castle is visible from the towers of nearby Šomoška Castle, across the border in Slovakia. History. In the beginning it was only a square-shaped stone tower.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
15th century. In 1460 the Hussites captured the small fortress of Salgó. King Mathias recaptured it in the same year and gave it to Imre Szapolyai. This period commenced the golden age of Salgó castle. The lower castle-yard was further built and the upper castle-yard became roofed-over and became a living space.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
He made his soldiers lay tree trunks on to gun carriages and push them under the fortress. The soldiers in the tower thought that the trunks were real cannons as they could not see well in the fog. They then handed over Salgó Castle. In reality the fortress was shelled to ruins by the Ottoman army.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
History. In the beginning it was only a square-shaped stone tower. The meaning behind &quot;Salgó&quot; is 'shine', however it is still not clear whether the name Salgó was the name of the volcanic peak which the castle sits on, or that they started to call the place by this name after the tower was erected. A fortified tower at first stood on the site of the present-day castle.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
This castle had two cisterns and the water was essential, not only for drinking but also fire fighting. 15th century. In 1460 the Hussites captured the small fortress of Salgó. King Mathias recaptured it in the same year and gave it to Imre Szapolyai. This period commenced the golden age of Salgó castle.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
They then handed over Salgó Castle. In reality the fortress was shelled to ruins by the Ottoman army. They set the artillery on the top of the neighbouring hill, opposite to Salgó called Kis-Salgó (Small-Salgó) or Boszorkánykő (cliff of witches). Bálint Balassi, the great Hungarian poet, got into the fortress, while the Ottoman army was still stationed in the castle.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
Modern. The ruins became overgrown with grass and shrubs up until the 19th century when Sándor Petőfi another famous Hungarian poet climbed into the ruins of the castle in 1845 the atmosphere of the ruins made him write his romantic poetry called &quot;Salgó&quot;. This is a tragic story about the Kompolti clan, the lords of Salgó, who tyrannized the region, which were under their power.

Geographic entities mentioned:
surface_form: salgó
instance_of: Mountain
countries: Hungary
coordinates: lat: 48.14472222
lon: 19.84722222
Ślesińskie Lake. Ślesińskie Lake is a lake in central Poland known as Jezioro Ślesińskie in Polish. It is located in Konin County in Gmina Ślesin, near the town of Licheń Stary. It is a post-glacial ribbon lake with a strongly developed shoreline. To the south it is connected to Mikorzyńskie Lake. It is part of the 32-kilometer navigable Ślesińskie Canal.

Geographic entities mentioned:
surface_form: Mikorzyńskie Lake
instance_of: Lake
countries: Poland
coordinates: lat: 52.3486
lon: 18.3033
To the south it is connected to Mikorzyńskie Lake. It is part of the 32-kilometer navigable Ślesińskie Canal. It is one of several lakes known collectively as the heated Konin Lakes because the water temperature is raised as a result of the outflow received from two power stations. The lake is a tourist attraction and is used for water sports including water-skiing and wakeboarding.

Geographic entities mentioned:
surface_form: Konin Lakes
instance_of: Group of lakes
countries: Poland
coordinates: lat: 52.33
lon: 18.31
Ślesińskie Lake. Ślesińskie Lake is a lake in central Poland known as Jezioro Ślesińskie in Polish. It is located in Konin County in Gmina Ślesin, near the town of Licheń Stary. It is a post-glacial ribbon lake with a strongly developed shoreline. To the south it is connected to Mikorzyńskie Lake. It is part of the 32-kilometer navigable Ślesińskie Canal.

Geographic entities mentioned:
surface_form: ślesińskie lake
instance_of: Lake
countries: Poland
coordinates: lat: 52.3878
lon: 18.3283
Ślesińskie Lake. Ślesińskie Lake is a lake in central Poland known as Jezioro Ślesińskie in Polish. It is located in Konin County in Gmina Ślesin, near the town of Licheń Stary. It is a post-glacial ribbon lake with a strongly developed shoreline. To the south it is connected to Mikorzyńskie Lake. It is part of the 32-kilometer navigable Ślesińskie Canal.

Geographic entities mentioned:
surface_form: ślesińskie lake
instance_of: Lake
countries: Poland
coordinates: lat: 52.3878
lon: 18.3283
surface_form: jezioro ślesińskie
instance_of: Lake
countries: Poland
coordinates: lat: 52.3878
lon: 18.3283
Normandin Lake. Normandin Lake is a freshwater body of the unorganized territory of Lac-Ashuapmushuan, Quebec, in the western part of the Regional County Municipality (MRC) Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in the province of Quebec, in Canada. This lake is entirely located in the canton of Ventadour which is at the end
West of the MRC Le Domaine-du-Roy.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
surface_form: normandin lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.960833333333
lon: -74.280277777778
The name of the lake evokes the work of the life of the surveyor Joseph-Laurent Normandin. The latter had traveled the region of Saguenay-Lac-Saint-Jean in 1732 to draw a detailed map of the place by locating the lakes, large and small, and to fix the boundaries of the Domaine du Roi.

Geographic entities mentioned:
surface_form: saint-jean
instance_of: Lake
countries: Canada
coordinates: lat: 48.594444444444
lon: -72.03
Normandin Lake. Normandin Lake is a freshwater body of the unorganized territory of Lac-Ashuapmushuan, Quebec, in the western part of the Regional County Municipality (MRC) Le Domaine-du-Roy, in the administrative region of Saguenay-Lac-Saint-Jean, in the province of Quebec, in Canada. This lake is entirely located in the canton of Ventadour which is at the end
West of the MRC Le Domaine-du-Roy.

Geographic entities mentioned:
surface_form: normandin lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.960833333333
lon: -74.280277777778
This lake is entirely located in the canton of Ventadour which is at the end
West of the MRC Le Domaine-du-Roy. Forestry is the main economic activity of the sector. Recreational tourism activities come second. The forest road route 212 linking Obedjiwan, Quebec and La Tuque pass south of Dubois Lake and Normandin Lake. Other secondary forest roads serve the vicinity of the lake.

Geographic entities mentioned:
surface_form: normandin lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.960833333333
lon: -74.280277777778
Recreational tourism activities come second. The forest road route 212 linking Obedjiwan, Quebec and La Tuque pass south of Dubois Lake and Normandin Lake. Other secondary forest roads serve the vicinity of the lake. The surface of Normandin Lake is usually frozen from early November to mid-May, however safe ice circulation is generally from mid-November to mid-April. Toponymy.

Geographic entities mentioned:
surface_form: normandin lake
instance_of: Lake
countries: Canada
coordinates: lat: 48.960833333333
lon: -74.280277777778
Marine air exits the San Francisco Bay (without having experienced the normal drying and heating effects associated with over-land travel) in several directions. The predominant outflow is carried by the onshore northwesterly winds toward the south through the Santa Clara Valley to Morgan Hill and to the east via the Hayward Pass and Niles Canyon.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Livermore Valley temperatures show this phenomenon. Ocean air flows across San Francisco Bay, through the Hayward Pass and Niles Canyon, and into the Livermore Valley, causing a cooling effect in summer and a warming effect in winter.

Geographic entities mentioned:
surface_form: Livermore Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.6886
lon: -121.736
Nugget Falls. Nugget Falls, also known as Nugget Creek Falls or Mendenhall Glacier Falls, is a waterfall downstream of the Nugget Glacier, at the base of Bullard Mountain, in the U.S. state of Alaska. Formed by the creek from the Nugget Glacier, the waterfall drops in two tiers of and onto a sandbar in Mendenhall Lake, which is the freshwater pool at the face of the Mendenhall Glacier.

Geographic entities mentioned:
surface_form: Bullard Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 58.434444444444
lon: -134.49861111111
state of Alaska. Formed by the creek from the Nugget Glacier, the waterfall drops in two tiers of and onto a sandbar in Mendenhall Lake, which is the freshwater pool at the face of the Mendenhall Glacier. The lake then drains via Mendenhall River into the Inside Passage.

Geographic entities mentioned:
surface_form: Mendenhall Lake
instance_of: Lake
countries: United States
coordinates: lat: 58.4233
lon: -134.569
Divis. Divis (;) is a hill and area of sprawling moorland north-west of Belfast in County Antrim, Northern Ireland. With a height of 1,568 ft (478 m), it is the highest of the Belfast Hills. It is joined with the neighbouring Black Mountain, and in the past they may have been seen as one. Divis transmitting station is on the summit.

Geographic entities mentioned:
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 51.8814
lon: -3.70848
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6
lon: -5.98
surface_form: black mountain
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 52.008333333333
lon: -3.0847222222222
Divis. Divis (;) is a hill and area of sprawling moorland north-west of Belfast in County Antrim, Northern Ireland. With a height of 1,568 ft (478 m), it is the highest of the Belfast Hills. It is joined with the neighbouring Black Mountain, and in the past they may have been seen as one. Divis transmitting station is on the summit.

Geographic entities mentioned:
surface_form: divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
With a height of 1,568 ft (478 m), it is the highest of the Belfast Hills. It is joined with the neighbouring Black Mountain, and in the past they may have been seen as one. Divis transmitting station is on the summit. The mountain extends north to the Antrim Plateau and shares its geology; consisting of a basaltic cover underlain by limestone and lias clay.

Geographic entities mentioned:
surface_form: divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Divis transmitting station is on the summit. The mountain extends north to the Antrim Plateau and shares its geology; consisting of a basaltic cover underlain by limestone and lias clay. In 2004 the Divis area and its surrounding mountains were handed over to the National Trust; having been under the control of the Ministry of Defence since 1953.

Geographic entities mentioned:
surface_form: divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Wildlife. Among the most common birds to be seen on Divis are: snipe, curlew, meadow pipit, skylark, red grouse, greenfinch, cuckoo, owls and peregrines. Less common are buzzards whose appearance is often recorded online to preserve valuable environmental data. The site is also home to badgers and hares. A View to the Future.

Geographic entities mentioned:
surface_form: divis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.6075
lon: -6.0094444444444
Many of his pieces featured his talents on the piano. Death. Kee died on 23 November 2007 as the result of a boating accident that claimed the lives of several contestants, including four of his teammates in the 2007 Cambodia Tonlé Sap competition.

Geographic entities mentioned:
surface_form: Tonlé Sap
instance_of: Lake
countries: Cambodia
coordinates: lat: 12.883333333333
lon: 104.06666666667
It is found throughout the Albertine Rift montane forests, including the Itombwe Mountain, Kahuzi-Biéga National Park and mountains at the west of Lake Kivu in Democratic Republic of Congo, Nyungwe Forest, Gishwati, Makwa and Mukura Forest in Rwanda, Bururi Forest and elsewhere in Burundi, the Rwenzori Mountains and Bwindi Impenetrable Forest in Uganda, as well as the Virunga Mountain.

Geographic entities mentioned:
surface_form: Lake Kivu
instance_of: Lake
countries: Democratic Republic of the Congo
Rwanda
coordinates: lat: -1.8530555555556
lon: 29.135277777778
Duggleby Howe. Duggleby Howe (also known as Howe Hill, Duggleby) is one of the largest round barrows in Britain, located on the southern side of the Great Wold Valley in the county of North Yorkshire (historically the East Riding of Yorkshire), and is one of four such monuments in this area, known collectively as the Great barrows of East Yorkshire.

Geographic entities mentioned:
surface_form: Great Wold Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.1385
lon: -0.3835
Created in 1997, it is made up of three ski resorts, hence the name of the area: the first two are Campo Felice, with the two slopes of Lucoli and Rocca di Cambio, and Ovindoli, both included between Monte Velino, Monte Magnola and Monte Sirente, within the Sirente-Velino Regional Park, while the third is the more distant station of Campo Imperatore, on the Gran Sasso. Ski slopes and circuits.

Geographic entities mentioned:
surface_form: Campo Felice
instance_of: Plateau
countries: Italy
coordinates: lat: 42.21583333
lon: 13.44805556
surface_form: Monte Velino
instance_of: Mountain
countries: Italy
coordinates: lat: 42.15
lon: 13.366666666667
surface_form: Monte Sirente
instance_of: Mountain
countries: Italy
coordinates: lat: 42.146111111111
lon: 13.611111111111
surface_form: Campo Imperatore
instance_of: Plateau
countries: Italy
coordinates: lat: 42.443698
lon: 13.558333
Ski slopes and circuits. The district has 30 kilometers of slopes in Campo Felice, 15 kilometers of slopes in Campo Imperatore, 60 for cross-country skiing and 30 kilometers of slopes in Ovindoli served by important and varied infrastructures. Both in Campo Felice and in Ovindoli there are also ring tracks for cross-country skiing.

Geographic entities mentioned:
surface_form: Campo Felice
instance_of: Plateau
countries: Italy
coordinates: lat: 42.21583333
lon: 13.44805556
The village was formerly known as Raeburn's Corners, Charlestown, Charleston, and (simply) Caledon (although the former township in which the community had been located was always named &quot;Caledon&quot;). The area flourished with industries like sawmills and gristmills, powered by the nearby Credit River. The main form of economic activity ties to agriculture and poultry.

Geographic entities mentioned:
surface_form: Credit River
instance_of: Watercourse
countries: Canada
coordinates: lat: 43.5478
lon: -79.5808
&quot;Prophalangopsis&quot; is a South Asian insect genus, in the family Prophalangopsidae, distantly related to crickets and other Ensifera, erected by Francis Walker in 1869. There is one species: &quot;Prophalangopsis obscura&quot;, which is a winged insect species found in North India and the Tibetan Plateau. It is one of only a few surviving species in the family Prophalangopsidae. F.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
North Fork Snake River. The North Fork Snake River is a tributary of the Snake River in central Colorado in the United States. It flows from a source near Loveland Pass to a confluence with the Snake River in Keystone. Pass Lake is a secondary source of the river.

Geographic entities mentioned:
surface_form: Pass Lake
instance_of: Lake
countries: United States
coordinates: lat: 39.6547459
lon: -105.8789146
Through various mergers the district now consists of only three municipalities. Geography. Hino District stretches from roughly Mount Sentsū to the upper and middle reaches of the Hino River. The small plains in the valleys around the Hino River have been developed for rice production.

Geographic entities mentioned:
surface_form: Mount Sentsū
instance_of: Mountain
countries: Japan
coordinates: lat: 35.15583333
lon: 133.17861111
Filming in Wai took the entire month of March 2013. A 10-day shooting schedule in Munnar, Kerala, began in mid-April 2013; scenes were filmed at Devikulam Lake, Meesapulimala, Wagavara and Kannimala. Filming was stopped for several days because of heavy rainfall, resulting in the schedule being slightly extended until end of the same month. A press conference was held in Munnar.

Geographic entities mentioned:
surface_form: Meesapulimala
instance_of: Mountain
countries: India
coordinates: lat: 10.097403
lon: 77.203417
Stage 1. 17 May 1997 — Venice to Venice,
Stage 2. 18 May 1997 — Mestre to Cervia,
Stage 3. 19 May 1997 — Santarcangelo di Romagna to San Marino, (ITT)
Stage 4. 20 May 1997 — San Marino to Arezzo,
Stage 5. 21 May 1997 — Arezzo to Monte Terminillo,
Stage 6. 22 May 1997 — Rieti to Lanciano,
Stage 7. 23 May 1997 — Lanciano to Mondragone,
Stage 8. 24 May 1997 — Mondragone to Cava de' Tirreni,
Stage 9.

Geographic entities mentioned:
surface_form: Monte Terminillo
instance_of: Mountain
countries: Italy
coordinates: lat: 42.47327
lon: 12.99732
The Konayev Canal (or Big Almaty Canal) passes through the district. Hydroelectric power stations are built on some of the rivers. In addition to the rivers, the district has lakes, including Issyk, Jasylkol and others. The non-mountainous part of the region is mostly semi-desert.

Geographic entities mentioned:
surface_form: Issyk
instance_of: Lake
countries: Kazakhstan
Russian Empire
Soviet Union
coordinates: lat: 43.253055555556
lon: 77.484444444444
History. In 1928, hill located at 1258 meters above sea and designed by Adolf Badrutt, a Swiss ski jumper and world record holder, in the last town of the Val Camonica valley was completed. On 24 February 1929, hill was officially opened in front of 20,000 spectators by Edda Mussolini, daughther of Italian prime minister Benito Mussolini.

Geographic entities mentioned:
surface_form: Val Camonica
instance_of: Valley
countries: Italy
coordinates: lat: 46.0075
lon: 10.3475