Sarmila/GeoWiki-Features huggingface dataset:
The ECT includes the entire Appalachian Trail to Mount Katahdin, Maine, then continues on the International Appalachian Trail through Maine, New Brunswick, and Quebec. The hiking trail ends at the Gulf of St. Lawrence; the hiker can then travel to Newfoundland by other means and complete the next section of the ECT across that island.

Geographic entities mentioned:
surface_form: Mount Katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
Orontes II, who was the satrap of Armenia and led the Armenian contingent (together with Mithrenes) at the Battle of Gaugamela in 331 BC, was either a son or grandson of Orontes. Orontes is mentioned in one of the &quot;stelae&quot; (monument containing information) of Mount Nemrut, erected by his descendant Antiochus I of Commagene ().

Geographic entities mentioned:
surface_form: Mount Nemrut
instance_of: Mountain
countries: Turkey
coordinates: lat: 37.98073888888889
lon: 38.740830555555554
After this time both Berwick and the Isle of Man were lost to England, and Orkney and Shetland were gained from Norway in the fifteenth century. The area that became Scotland in this period is divided by geology into five major regions: the Southern Uplands, Central Lowlands, the Highlands, the North-east coastal plain and the Islands.

Geographic entities mentioned:
surface_form: Central Lowlands
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.408
lon: -4.044
Neighbouring independent kings became subject to Alba and eventually disappeared from the records. In the ninth century the term &quot;mormaer&quot;, meaning &quot;great steward&quot;, began to appear in the records to describe the rulers of Moray, Strathearn, Buchan, Angus and Mearns, who may have acted as &quot;marcher lords&quot; for the kingdom to counter the Viking threat.

Geographic entities mentioned:
surface_form: Strathearn
instance_of: Valley
countries: United Kingdom
coordinates: lat: 56.3325
lon: -3.6825
He was chairman of the Judiciary Committee, which considered appointments to Vermont's state courts as well as review of and updates to Vermont's statutes. While serving in the senate, Wilson also carried out a gubernatorial appointment as chairman of a commission that developed plans for construction of a bridge over Lake Champlain. In addition, Wilson carried out with Hale K.

Geographic entities mentioned:
surface_form: Lake Champlain
instance_of: Lake
countries: United States
Canada
coordinates: lat: 44.53
lon: -73.33
History. Tai Om was historically a single-clan Hakka village, settled by the Cheung family (). The founding ancestors had moved from Wuhua in Guangdong province to Tai Mo Shan, and later settled in Tai Om around 1800. (other sources mention that the village was founded in the 17th century)
At the time of the 1911 census, the population of Tai Om was 162. The number of males was 74. Conservation.

Geographic entities mentioned:
surface_form: Tai Mo Shan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 22.4118
lon: 114.123
Wilderness areas include Mkhomazi, Upper Mkhomazi, Mlambonja, Mdedelelo, and Mzimkhulu. Mkhomazi Wilderness Area is a region of deserted badlands in the Drakensberg, lying between the Giant's Castle and the Sani Pass.

Geographic entities mentioned:
surface_form: Giant's Castle
instance_of: Mountain
countries: South Africa
coordinates: lat: -29.34608
lon: 29.48364
while parks, green belts and sports fields made up 8.6%. Out of the forested land, 1.6% of the total land area is heavily forested and 1.6% is covered with orchards or small clusters of trees. Of the agricultural land, 7.0% is used for growing crops. The municipality is located on the left bank of Lake Geneva and the Seymaz river. It is partly surrounded by the municipality of Thônex.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
The current director is Susan Thornton. The Starfire Optical Range at Kirtland AFB, North Oscura Peak on White Sands Missile Range, and the Air Force Maui Optical and Supercomputing observatory (AMOS) are also operated by divisions of the Directed Energy Directorate in addition to their facilities at the Directorate's headquarters at Kirtland AFB.

Geographic entities mentioned:
surface_form: North Oscura Peak
instance_of: Mountain
countries: United States
coordinates: lat: 33.7522
lon: -106.372
In May 2025, a trilateral meeting involving the Coptic Orthodox Church, the Syriac Orthodox Church, and the Armenian Apostolic Church (of the Great House of Cilicia) took place at the Monastery of Saint Pishoy in Wadi El Natrun, Egypt to commemorate the 1700th anniversary of the Council of Nicaea.

Geographic entities mentioned:
surface_form: Wadi El Natrun
instance_of: Valley
countries: Egypt
coordinates: lat: 30.416666666667
lon: 30.333333333333
As Mao was unwilling to read the 60-article draft, which had 7,000 words, the draft was further compressed to 30 articles, with more than 4,000 words with the hope it could be reduced to 3,000 to 3,500 words. On the evening of August 22, the Central Constitution Revision Drafting Committee held its last meeting in Lushan, Jiangxi. Zhou presided over the meeting with Mao and Lin not attending.

Geographic entities mentioned:
surface_form: Lushan
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 29.5725
lon: 115.97333333333
Led by local guides from Mittenwald (Bavaria was on the side of Napoléon Bonaparte), the French were able to deploy to a flank along a mountain track that ran from the Lautersee and Ferchensee past the Grünkopf (1,587 m) and attack the Austrians stationed at the Leutascher Schanz fortifications unexpectedly from the rear on 4 November 1805.

Geographic entities mentioned:
surface_form: Lautersee
instance_of: Lake
countries: Germany
coordinates: lat: 47.438611111111
lon: 11.235277777778
surface_form: Ferchensee
instance_of: Lake
countries: Germany
coordinates: lat: 47.439166666667
lon: 11.214722222222
Charles was crowned in Bonn on 26 November 1346, and Duke Rudolf I was the only elector who was present at this solemn ceremony. His close ties to Charles IV were rewarded when he received the Altmark territory in 1347, whereby the Elbe river became the boundary between Saxony and Brandenburg.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
He was professor emeritus at Johns Hopkins University in the United States. He researched the mating of Antarctic birds and received the Polar Medal. Two mountains on the continent, Mount Sladen and Sladen Summit, are named in his honour. His discovery in the 1960s that DDT residues could be found in adelie penguins contributed to the banning of DDT in the U.S.

Geographic entities mentioned:
surface_form: Mount Sladen
instance_of: Mountain
coordinates: lat: -60.6833
lon: -45.2833
surface_form: Sladen Summit
instance_of: Mountain
coordinates: lat: -78.11666667
lon: 162.38333333
Marathon Large Igneous Province. uka6r0aityixgubb8ultwvwx2en92" xml:space="preserve">The Marathon Large Igneous Province is a Paleoproterozoic large igneous province along the southern Superior craton of Ontario, Canada, located around the northern margin of Lake Superior. It consists of three diabase dike swarms known as Marathon, Kapuskasing and Fort Frances.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
Of the agricultural land, 23.0% is used for growing crops and 15.4% is pastures, while 2.1% is used for orchards or vine crops. It is situated along the northern shores of Lake Geneva and has grown substantially within the past two decades due to the housing shortage in Geneva proper. Mainly families have moved to Bellevue.

Geographic entities mentioned:
surface_form: Lake Geneva
instance_of: Lake
countries: Switzerland
France
coordinates: lat: 46.45
lon: 6.55
Distribution. &quot;Ficus pleurocarpa&quot; is an Australian endemic. It is found in north-east Queensland, from Cape Tribulation south to the Atherton Tableland. It grows in lowland and upland wet tropical rainforests from sea level up to above sea level. Ecology.

Geographic entities mentioned:
surface_form: Atherton Tableland
instance_of: Plateau
countries: Australia
coordinates: lat: -17.16666667
lon: 145.53333333
Monte Kronio. Monte Kronio, or &quot;Monte San Calogero&quot;, is a hill about 7 km from Sciacca, a comune of the province of Agrigento in Sicily. Description. With a height of 395.48 metres, the hill is composed mostly of limestone. It is a nature reserve administered by the state forestry agency of the Regione Siciliana.

Geographic entities mentioned:
surface_form: monte san calogero
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
Monte Kronio. Monte Kronio, or &quot;Monte San Calogero&quot;, is a hill about 7 km from Sciacca, a comune of the province of Agrigento in Sicily. Description. With a height of 395.48 metres, the hill is composed mostly of limestone. It is a nature reserve administered by the state forestry agency of the Regione Siciliana.

Geographic entities mentioned:
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
On the mountain is the &quot;Sanctuary of San Calogero,&quot; from the 16th century, the Antiquarium and various natural caves which emit geothermal gas, the most well-known of which is the so-called &quot;Stove of San Calogero.&quot;
The vast area behind the settlement of Sciacca, which culminates in Monte Kronio, may be the site of an ancient volcano, which even today shows some activity, however slight, through the emission of sulphur vapours.

Geographic entities mentioned:
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
This theory is supported by the presence of Graham Island off the coast, a volcanic island forming part of a wider &quot;Empedoclean&quot; system, so it cannot be ruled out that Monte Kronio was a vent of a larger volcanic system in the distant past. Antiquarium of Monte Kronio. On the mountain there is the &quot;Antiquarium di Monte Kronio - Stufe di S.

Geographic entities mentioned:
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
Antiquarium of Monte Kronio. On the mountain there is the &quot;Antiquarium di Monte Kronio - Stufe di S. Calogero&quot; museum, a thermal complex and a series of karst caves which were used for health purposes in antiquity. The antiquarium was established in the 1980s and contains discoveries from local excavations. The site is managed by the Soprintendenza of cultural heritage for Agrigento.

Geographic entities mentioned:
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
Pope John Paul II raised it to the status of a minor basilica in 1979. It contains a statue of the saint, made by Antonello Gagini. Ancient winemaking. In 2012 Copper Age jars dating from the fourth millennium BC were found in a cave on Monte Kronio. Organic samples taken from the jars proved to contain tartaric acid and its salt, confirming the use of the vessel as wine containers.

Geographic entities mentioned:
surface_form: monte kronio
instance_of: Mountain
countries: Italy
coordinates: lat: 37.518927
lon: 13.113868
Among the pilots who took part in the attack was Ilan Ramon, later Israel's first astronaut. 1982 Lebanon War and aftermath. Prior to the 1982 Lebanon War, Syria, with the help of the Soviet Union, had built up an overlapping network of surface-to-air missiles in Lebanon's Beqaa Valley. On June 9, 1982, the IAF carried out Operation Mole Cricket 19, crippling the Syrian air defence array.

Geographic entities mentioned:
surface_form: Beqaa Valley
instance_of: Valley
countries: Lebanon
coordinates: lat: 34.008888888889
lon: 36.145277777778
Eupatorium benguetense. &quot;Eupatorium benguetense&quot; is a plant species in the family Asteraceae. Taxonomy. &quot;Eupatorium benguetense&quot; was described by Charles Budd Robinson in 1908, based on material collected on Mount Santo Tomas. All of the other specimens he cited also came from the province of Benguet, giving it its name.

Geographic entities mentioned:
surface_form: Mount Santo Tomas
instance_of: Mountain
countries: Philippines
coordinates: lat: 16.335
lon: 120.56111111111
Climate. The areas of the town near Lake Saroma do not experience a large temperature range compared to inland areas, which have colder winters and hotter summers. Saroma’s record of 39.5 °C (103.1 °F) on 26 May 2019 is both Japan’s highest temperature recorded in May and the highest temperature recorded in Hokkaido. Healthcare.

Geographic entities mentioned:
surface_form: Lake Saroma
instance_of: Lake
countries: Japan
coordinates: lat: 44.166666666667
lon: 143.71666666667
Consolation Valley. Consolation Valley is a valley in Alberta, Canada. It is situated within Banff National Park, and adjacent to Valley of the Ten Peaks. Consolation Valley was so named on account of its fine appearance. The landform's toponym was officially adopted on July 2, 1959, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: Valley of the Ten Peaks
instance_of: Valley
countries: Canada
coordinates: lat: 51.3494444
lon: -116.1597222
Consolation Valley was so named on account of its fine appearance. The landform's toponym was officially adopted on July 2, 1959, by the Geographical Names Board of Canada. The valley is bound by Mount Babel, Mount Fay, Quadra Mountain, Bident Mountain, Mount Bell, and Panorama Ridge. Two lakes officially named Consolation Lakes occupy the valley and are drained by Babel Creek.

Geographic entities mentioned:
surface_form: Mount Fay
instance_of: Mountain
countries: Canada
coordinates: lat: 51.29944444444445
lon: -116.16194444444444
surface_form: Quadra Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.286944444444444
lon: -116.15333333333334
surface_form: Bident Mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.2875
lon: -116.14111111111112
surface_form: mount bell
instance_of: Mountain
countries: Canada
coordinates: lat: 51.284166666666664
lon: -116.10111111111111
surface_form: mount babel
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4411
lon: -68.6919
surface_form: mount babel
instance_of: Mountain
countries: Canada
coordinates: lat: 51.30638888888889
lon: -116.16333333333333
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Consolation Valley. Consolation Valley is a valley in Alberta, Canada. It is situated within Banff National Park, and adjacent to Valley of the Ten Peaks. Consolation Valley was so named on account of its fine appearance. The landform's toponym was officially adopted on July 2, 1959, by the Geographical Names Board of Canada.

Geographic entities mentioned:
surface_form: consolation valley
instance_of: Valley
countries: Canada
coordinates: lat: 51.31669
lon: -116.15217
Geography. Pattamundai is located at 20.57°N 86.57°E. Pattamundai is located 22 km from the Bay of Bengal in the Utkal Plains, at an elevation of 6 m from sea level. Pattamundai is a flat, low-lying delta region in the Lower Mahanadi River basin. The Brahmani river divides it from the Aali Block.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The temperature around this season is 35 °C to 40 °C Thunderstorms are common at the height of the summer. Rains brought by the Bay of Bengal branch of the south west summer monsoon lash Pattamundai between June and September, supplying it with most of its annual rainfall of. The highest monthly rainfall total, occurs in August. from the South West Monsoon.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Temperatures may exceed 45 °C at the height of summer and may fall below 10 °C in winter. Floods. Due to the proximity to coast and being located near the delta of some great river systems, cyclones and floods are a permanent feature of this region from the Bay of Bengal. The rivers that flood Pattamundai are Brahmani, Kani and Gobari.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
The station has two platforms with a second track as a siding loop. All the trains that run on the Main Line, including the Podi Menike and Udarata Menike express trains stop at the station. The railway station was constructed to service the Great Western Estate, a tea plantation in the foothills of the Great Western Mountain. The estate was originally established by J. A. Rossiter in 1866.

Geographic entities mentioned:
surface_form: Great Western Mountain
instance_of: Mountain
countries: Sri Lanka
coordinates: lat: 6.96666667
lon: 80.69388889
Life. Dietrich was the ancestor of a comital branch named after the residence of Haldensleben in Eastphalia. He may have been a son of Count Wichmann the Elder and Frederuna, sister of Queen Matilda, and held large estates along the Elbe and Saale rivers. A henchman of the royal Ottonian dynasty, Dietrich in 953 supported King Otto I of Germany against his revolting son Duke Liudolf of Swabia.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
It is located in the state of Mexico, adjacent to the east side of Mexico City. The municipality comprises its own intrastate region, Region IX (Mexico State). It was named after Nezahualcoyotl, the Acolhua poet and king of nearby Texcoco, which was built on the drained bed of Lake Texcoco. The name &quot;Nezahualcóyotl&quot; comes from Nahuatl, meaning &quot;fasting coyote&quot;.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
The current coat of arms, which includes the glyph, was authorized by the municipality in the 1990s. Until the 20th century, the land on which Ciudad Neza sits was under Lake Texcoco and uninhabited. Successful draining of the lake in the early 20th century created new land, which the government eventually sold into private hands.

Geographic entities mentioned:
surface_form: Lake Texcoco
instance_of: Lake
countries: Mexico
coordinates: lat: 19.5
lon: -98.99
In 1933, the Mexico City–Puebla highway was built through this area. The first settlements in what is now the municipality were extensions of the municipalities of Chimalhuacán, La Paz and Ecatepec. The area was known for a bird species called the chichicuilote-atziztizuilotl, which inhabited the lakes and ponds of the Valley of Mexico. Today it is nearly extinct.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
The mountain is covered by Sierra palm trees. Various plants, including some endangered species are found here, such as the endangered fern &quot;Elaphoglossum serpens&quot; which is found only on this mountain and nowhere else in the world, and Cook's holly (&quot;Ilex cookii&quot;) or &quot;planta de te&quot;, which is only found here and in neighboring Mount Jayuya. Nearby roads.

Geographic entities mentioned:
surface_form: Mount Jayuya
instance_of: Mountain
countries: United States
coordinates: lat: 18.167777777778
lon: -66.574722222222
Geology. Unlike many Caribbean mountains, Cerro de Punta is not a volcano but simply the highest point in the Cordillera Central. Cordillera Central is the central mountain range that divides the island by running in an east–west fashion. Best view. The view from atop Cerro de Punta is said to be &quot;the best view in all of Puerto Rico&quot;.

Geographic entities mentioned:
surface_form: central mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.3
lon: -76.3463
Cerro de Punta. Cerro de Punta or Cerro Punta is the highest peak in Puerto Rico, rising to above sea level. The mountain is part of the Cordillera Central and is located on the town boundary between the municipalities of Ponce and Jayuya in the central region of the main island of Puerto Rico. Location.

Geographic entities mentioned:
surface_form: cerro de punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
The mountain is just north of east-to-westbound Route 143. It is located at coordinates 18.172458 and -66.591839W. The nearest populated place to Cerro de Punta is &quot;Urbanización Vega Linda&quot;, located 3.3 miles (5.3 km) away. Geology. Unlike many Caribbean mountains, Cerro de Punta is not a volcano but simply the highest point in the Cordillera Central.

Geographic entities mentioned:
surface_form: cerro de punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
The nearest populated place to Cerro de Punta is &quot;Urbanización Vega Linda&quot;, located 3.3 miles (5.3 km) away. Geology. Unlike many Caribbean mountains, Cerro de Punta is not a volcano but simply the highest point in the Cordillera Central. Cordillera Central is the central mountain range that divides the island by running in an east–west fashion. Best view.

Geographic entities mentioned:
surface_form: cerro de punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
The inn operates under a contract with the Government of Puerto Rico. The trails, however, are not well marked and often suffer damage from storms. While people can hike their way to the top of the mountain, there is a paved road that leads to the very summit. The Toro Negro State Forest has 12 miles (19 km) of hiking trails some of which lead to the top of Cerro de Punta.

Geographic entities mentioned:
surface_form: cerro de punta
instance_of: Mountain
countries: United States
coordinates: lat: 18.1725
lon: -66.591944444444
Loft Crag. Loft Crag is a fell in the English Lake District, situated west of Ambleside in the valley of Great Langdale. Along with the neighbouring fells of Harrison Stickle and Pike of Stickle it forms the picturesque Langdale Pikes, which when viewed from the area around Elterwater village gives one of the best-known views in the National Park. Topography.

Geographic entities mentioned:
surface_form: Great Langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
Loft Crag. Loft Crag is a fell in the English Lake District, situated west of Ambleside in the valley of Great Langdale. Along with the neighbouring fells of Harrison Stickle and Pike of Stickle it forms the picturesque Langdale Pikes, which when viewed from the area around Elterwater village gives one of the best-known views in the National Park. Topography.

Geographic entities mentioned:
surface_form: Harrison Stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
surface_form: Pike of Stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
surface_form: elterwater
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.427469444444
lon: -3.025875
From there it is a straightforward climb to the summit. A more circuitous ascent can be undertaken from the same starting point but taking the well trodden (and repaired) path up Stickle Ghyll to Stickle Tarn. From here the fells of Pavey Ark and Thunacar Knott can be climbed before tackling the three Langdale Pikes. Summit and Gimmer Crag.

Geographic entities mentioned:
surface_form: Pavey Ark
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4614
lon: -3.10451
surface_form: Thunacar Knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4613
lon: -3.11376
surface_form: knott
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.686211111111
lon: -3.0935388888889
Loft Crag. Loft Crag is a fell in the English Lake District, situated west of Ambleside in the valley of Great Langdale. Along with the neighbouring fells of Harrison Stickle and Pike of Stickle it forms the picturesque Langdale Pikes, which when viewed from the area around Elterwater village gives one of the best-known views in the National Park. Topography.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
The Langdale Pikes form a parapet to the lower hinterland to their north. From 'behind' they are unimpressive, but their southern faces fall full length over crags to the floor of Langdale, nearly below. Loft Crag has a peaked summit which apes in lesser proportion the fine knoll of Pike of Stickle. To the east, between Loft Crag and Harrison Stickle is the subsidiary top of Thorn Crag.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: pike of stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.455861111111
lon: -3.1228694444444
Loft Crag has a peaked summit which apes in lesser proportion the fine knoll of Pike of Stickle. To the east, between Loft Crag and Harrison Stickle is the subsidiary top of Thorn Crag. This is sometimes counted as a Langdale Pike in its own right, but only Birkett amongst the major guidebooks takes this view. Ascents. Loft Crag has a summit elevation of.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
This is sometimes counted as a Langdale Pike in its own right, but only Birkett amongst the major guidebooks takes this view. Ascents. Loft Crag has a summit elevation of. It lies between Harrison Stickle and Pike o' Stickle and is usually climbed in conjunction with these two peaks. The starting place for the direct ascent of the fell is The New Dungeon Ghyll Hotel in Great Langdale.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
The starting place for the direct ascent of the fell is The New Dungeon Ghyll Hotel in Great Langdale. A path leads north-westerly across the hillside passing Dungeon Ghyll Force waterfall and going between Thorn Crag and Gimmer Crag to a col between Loft Crag and Harrison Stickle. From there it is a straightforward climb to the summit.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
From here the fells of Pavey Ark and Thunacar Knott can be climbed before tackling the three Langdale Pikes. Summit and Gimmer Crag. Loft Crag is a fine viewpoint which gives an attractive vista of the fells around Great Langdale. Because the fell juts further out into the valley than the other two Langdale Pikes, it gives a more impressive and full view of the valley.

Geographic entities mentioned:
surface_form: loft crag
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.4541
lon: -3.11665
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
Because the fell juts further out into the valley than the other two Langdale Pikes, it gives a more impressive and full view of the valley. The fell has a small sharp summit below which rises Gimmer Crag, which is one of the top rock climbing venues in the Lake District. The crag is made of volcaniclastic siltstone and mudstone.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
The fell has a small sharp summit below which rises Gimmer Crag, which is one of the top rock climbing venues in the Lake District. The crag is made of volcaniclastic siltstone and mudstone. Climbing in the Lake District was pioneered in the early 1880s by Walter Parry Haskett Smith.

Geographic entities mentioned:
surface_form: the lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.07
lon: -0.62
From there it is a straightforward climb to the summit. A more circuitous ascent can be undertaken from the same starting point but taking the well trodden (and repaired) path up Stickle Ghyll to Stickle Tarn. From here the fells of Pavey Ark and Thunacar Knott can be climbed before tackling the three Langdale Pikes. Summit and Gimmer Crag.

Geographic entities mentioned:
surface_form: stickle tarn
instance_of: Lake
countries: United Kingdom
coordinates: lat: 54.4586
lon: -3.1025
It lies between Harrison Stickle and Pike o' Stickle and is usually climbed in conjunction with these two peaks. The starting place for the direct ascent of the fell is The New Dungeon Ghyll Hotel in Great Langdale. A path leads north-westerly across the hillside passing Dungeon Ghyll Force waterfall and going between Thorn Crag and Gimmer Crag to a col between Loft Crag and Harrison Stickle.

Geographic entities mentioned:
surface_form: great langdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.449119444444
lon: -3.0733305555556
This is sometimes counted as a Langdale Pike in its own right, but only Birkett amongst the major guidebooks takes this view. Ascents. Loft Crag has a summit elevation of. It lies between Harrison Stickle and Pike o' Stickle and is usually climbed in conjunction with these two peaks. The starting place for the direct ascent of the fell is The New Dungeon Ghyll Hotel in Great Langdale.

Geographic entities mentioned:
surface_form: harrison stickle
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.456869444444
lon: -3.1105611111111
The race was decided on the race's queen stage, with the top-three stage placings taking the final podium positions. Rafał Majka () won both the general and mountains classification, by taking first place at the summit finish in Rogla.

Geographic entities mentioned:
surface_form: Rogla
instance_of: Mountain
countries: Slovenia
coordinates: lat: 46.4525
lon: 15.333611
Rajgir. The Rajgir Vishwa Shanti Stupa/World Peace Pagoda () was completed in 1969 at Rajgir hills near Rajgir, near the Vulture's Peak where the Buddha is believed to have preached the Lotus Sutra. The dedication coincided with the 100th anniversary of the birth of Mahatma Gandhi. The site also includes a Nipponzan Myohoji temple. Darjeeling.

Geographic entities mentioned:
surface_form: Vulture's Peak
instance_of: Mountain
countries: India
coordinates: lat: 25.001666666666665
lon: 85.44638888888889
In Hakodate, Blakiston made a large collection of birds, which is currently located at the museum of Hakodate. The distributions of many bird species observe the Blakiston line, since many birds do not cross even the shortest stretches of open ocean water. For his discovery of Blakiston's Line, a monument was erected in his honor on Mount Hakodate.

Geographic entities mentioned:
surface_form: Mount Hakodate
instance_of: Mountain
countries: Japan
coordinates: lat: 41.758888888889
lon: 140.70444444444
Geology. The steep slopes of Epidote Peak expose two distinct geologic units, the Greenlee and Taylor formations. Metasedimentary strata of Greenlee Formation only outcrop on the northern end of Mount Greenlee and the lower eastern slopes of Epidote Peak. The remainder of the exposed bedrock of Epidote Peak consists of metavolcanic rocks of the Taylor Formation.

Geographic entities mentioned:
surface_form: Mount Greenlee
instance_of: Mountain
coordinates: lat: -84.85
lon: -177
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
The foliation in these strata has developed parallel to bedding. At the base of the slopes of Epdiote Peak that are adjacent ot Shackleton Glacier, the micaceous quartzites and argillites are intruded by granitic migmatitic gneisses. The quartzites are dark gray to brown and occur in beds that range in thickness from. Many of the beds exhibit fine laminations.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
surface_form: gray
instance_of: Mountain
coordinates: lat: -65.1
lon: -60.0833
Within the ridge crest west of Epidote Peak, the Taylor Formation consists of highly sheared silicic volcanic rocks, typically porphyritic felsite. These rocks exhibit shades of brown and gray and may be porphyritic or non-porphyritic. Considerable amounts non-porphyritic felsite or, alternatively, chert is also present within these silicic volcanic rocks.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
surface_form: gray
instance_of: Mountain
coordinates: lat: -65.1
lon: -60.0833
Local concentrations of this mineral gives the peak a spotted appearance. The name was approved by US-ACAN in 1966. Geology. The steep slopes of Epidote Peak expose two distinct geologic units, the Greenlee and Taylor formations. Metasedimentary strata of Greenlee Formation only outcrop on the northern end of Mount Greenlee and the lower eastern slopes of Epidote Peak.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
Metasedimentary strata of Greenlee Formation only outcrop on the northern end of Mount Greenlee and the lower eastern slopes of Epidote Peak. The remainder of the exposed bedrock of Epidote Peak consists of metavolcanic rocks of the Taylor Formation. A ridge crest west of Epidote Peak exposes a third geologic unit composed of highly sheared undifferentiated marble and metasedimentary rocks.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
The strata within the Greenlee Formation strike northwest-southeast to north-south and dip southwest-west. Overlying the Greenlee Formation at Epidote Peak is the Taylor Formation. It consists of a series of highly metamorphosed and sheared basaltic lava flows interbedded with graywackes and felsitic volcanic rocks.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
Plagioclase is sometimes observed as phenocrysts in what might be intermediate-mafic lava flows. Within the ridge crest west of Epidote Peak, the Taylor Formation consists of highly sheared silicic volcanic rocks, typically porphyritic felsite. These rocks exhibit shades of brown and gray and may be porphyritic or non-porphyritic.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
East of the outcrop of this deformed marble bed, several other thick marble beds are exposed. The relationship of the marble beds to each other and the Taylor and Greenlee formations is completely obscured by intense cataclasis and shearing of them and enclosing strata. A similar bed of white marble crops out on the summit of Epidote Peak.

Geographic entities mentioned:
surface_form: taylor
instance_of: Mountain
coordinates: lat: -63.4333
lon: -57.1333
Metasedimentary strata of Greenlee Formation only outcrop on the northern end of Mount Greenlee and the lower eastern slopes of Epidote Peak. The remainder of the exposed bedrock of Epidote Peak consists of metavolcanic rocks of the Taylor Formation. A ridge crest west of Epidote Peak exposes a third geologic unit composed of highly sheared undifferentiated marble and metasedimentary rocks.

Geographic entities mentioned:
surface_form: crest
instance_of: Mountain
coordinates: lat: -63.40636
lon: -56.99204
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
Epidote Peak. Epidote Peak () is a prominent rock peak just north of the mouth of Held Glacier, lying along the west side of Shackleton Glacier in the Queen Maud Mountains of Antarctica. The Texas Tech Shackleton Glacier Expedition, 1964–65, named it for the abundance of the mineral epidote. Local concentrations of this mineral gives the peak a spotted appearance.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
Epidote Peak. Epidote Peak () is a prominent rock peak just north of the mouth of Held Glacier, lying along the west side of Shackleton Glacier in the Queen Maud Mountains of Antarctica. The Texas Tech Shackleton Glacier Expedition, 1964–65, named it for the abundance of the mineral epidote. Local concentrations of this mineral gives the peak a spotted appearance.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
A ridge crest west of Epidote Peak exposes a third geologic unit composed of highly sheared undifferentiated marble and metasedimentary rocks. The Greenlee Formation consists of beds of fine-grained, micaceous quartzite and argillite that form the eastern slopes of Epidote Peak on the west side of Shackleton Glacier.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
Epidote is common as vein filling in cracks. At the western ends of ridges associated with Epidote Peak, thick beds of white, coarsely crystalline marble are exposed. On one ridge, a bed of marble that is tectonically pinched from a thickness of between massive felsite in a distance of. Thin, circa thick, beds of quartzite within the marble are ripped apart and disharmonically folded.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
The relationship of the marble beds to each other and the Taylor and Greenlee formations is completely obscured by intense cataclasis and shearing of them and enclosing strata. A similar bed of white marble crops out on the summit of Epidote Peak. These marble beds are currently correlated with the early Cambrian Shackleton Limestone of the Holyoake and Churchill mountains.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
These marble beds are currently correlated with the early Cambrian Shackleton Limestone of the Holyoake and Churchill mountains. The strata that form Epidote Peak and associated ridges are metamorphic rocks and intrusive granitic rocks that are part of the Ross orogenic belt, which is exposed throughout the Transantarctic Mountains.

Geographic entities mentioned:
surface_form: epidote peak
instance_of: Mountain
coordinates: lat: -84.7667
lon: -176.933
Epidote Peak. Epidote Peak () is a prominent rock peak just north of the mouth of Held Glacier, lying along the west side of Shackleton Glacier in the Queen Maud Mountains of Antarctica. The Texas Tech Shackleton Glacier Expedition, 1964–65, named it for the abundance of the mineral epidote. Local concentrations of this mineral gives the peak a spotted appearance.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
The foliation in these strata has developed parallel to bedding. At the base of the slopes of Epdiote Peak that are adjacent ot Shackleton Glacier, the micaceous quartzites and argillites are intruded by granitic migmatitic gneisses. The quartzites are dark gray to brown and occur in beds that range in thickness from. Many of the beds exhibit fine laminations.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
The relationship of the marble beds to each other and the Taylor and Greenlee formations is completely obscured by intense cataclasis and shearing of them and enclosing strata. A similar bed of white marble crops out on the summit of Epidote Peak. These marble beds are currently correlated with the early Cambrian Shackleton Limestone of the Holyoake and Churchill mountains.

Geographic entities mentioned:
surface_form: shackleton
instance_of: Mountain
coordinates: lat: -65.216666666667
lon: -63.933333333333
It consists of a series of highly metamorphosed and sheared basaltic lava flows interbedded with graywackes and felsitic volcanic rocks. Some of the basaltic lava flows are amygdaloidal and some are brecciated along with the interbedded graywacke in shear zones. Plagioclase is sometimes observed as phenocrysts in what might be intermediate-mafic lava flows.

Geographic entities mentioned:
surface_form: shear
instance_of: Mountain
coordinates: lat: -78.3333
lon: -86.1333
Rainy Lake (Snake Creek drainage basin). Rainy Lake is a small lake in the Ottawa River and St. Lawrence River drainage basins in Addington Highlands, Lennox and Addington County, Ontario, Canada. The lake is about long and wide and lies at an elevation of about northwest of the community of Denbigh and northeast of Ontario Highway 28.

Geographic entities mentioned:
surface_form: rainy lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.8989
lon: -77.3297
surface_form: rainy lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.1664
lon: -77.3297
Gunnerside. Gunnerside is a village in North Yorkshire, England. It is situated in Swaledale, on the B6270 road, east of Muker and west of Grinton. The village lies between the River Swale and its tributary, Gunnerside Beck, and is within the Yorkshire Dales National Park. History.

Geographic entities mentioned:
surface_form: Swaledale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.361
lon: -1.838
History. The name of the village derives from an Old Norse personal name &quot;Gunnar&quot; and &quot;sætr&quot; meaning hill or pasture. Gunnerside Ghyll (or Gunnerside Gill), a smaller valley running northwards, at right angles to the Swale valley (Swaledale), was the site of a major lead mining industry in Swaledale from the 17th century to the late 19th century.

Geographic entities mentioned:
surface_form: Gunnerside Ghyll
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.3994
lon: -2.09222
The beck that runs through the narrow valley, also called Gunnerside Gill, or Gunnerside Beck, rises between Rogan's Seat and Water Crag, and runs for emptying into the River Swale at the site of Gunnerside New Bridge. The bridge carries the B6270 over the River Swale south of the village; it was rebuilt several times during the 19th century due to flooding.

Geographic entities mentioned:
surface_form: Rogan's Seat
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.422939
lon: -2.125914
Lake Seppings. Lake Seppings (Noongar: &quot;Tjuirtgellong&quot;) is a freshwater lake located within the city of in the Great Southern region of Western Australia. Description. The lake is east-north-east of the Albany city centre.

Geographic entities mentioned:
surface_form: freshwater lake
instance_of: Lake
countries: Canada
coordinates: lat: 46.6453
lon: -60.3967
surface_form: tjuirtgellong
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
Dreamtime. The local indigenous Australians are the Noongar people whose name for the lake is &quot;Tjuirtgellong&quot; which means &quot;The place of the long-necked tortoise&quot;. The lake has a special significance to the Noongar who believe it to be the footprint of the spirit Djrat who created the south coast of Western Australia.

Geographic entities mentioned:
surface_form: tjuirtgellong
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
Lake Seppings. Lake Seppings (Noongar: &quot;Tjuirtgellong&quot;) is a freshwater lake located within the city of in the Great Southern region of Western Australia. Description. The lake is east-north-east of the Albany city centre.

Geographic entities mentioned:
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
Description. The lake is east-north-east of the Albany city centre. The main bitumen roads that border Lake Seppings are Golf Links Road to the east, Troode Street to the north, Collingwood Road, Drew Street/Sleeman Avenue to west and Lake Seppings Drive to the south. The lake is nearly completely surrounded by a compacted gravel footpath and wooden walkways.

Geographic entities mentioned:
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
A car park for access to the path is located along Golf Links Road. Lake Seppings is approximately in length (from north to south) and the north end is approximately in width. The lake narrows toward the southern end and the path crosses the lake approximately before the southern tip. The lake is situated in the Lake Seppings nature reserve that has a total area of. Fauna.

Geographic entities mentioned:
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
The sea level then rose and the lake was a shallow basin in the sea floor. This explains why cockle shells can be found preserved in the soil. Sea levels then fell to current levels about 8000 years ago leaving Lake Seppings from the coast line. The lake itself received its English name in 1827 by Major Edmund Lockyer, who named it after his cousins, Robert and John Milligen Seppings.

Geographic entities mentioned:
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
Lands along the eastern shore of the lake once were part of an estate belonging to Joseph Spencer of Balgarrup near Kojonup in 1884. In 1887 it was proposed to the Albany Municipal Council by Councillor Robert Andrew Muir that the Council apply to the Government to grant the land surrounding Lake Seppings as a
Commonage for the Municipality.

Geographic entities mentioned:
surface_form: lake seppings
instance_of: Lake
countries: Australia
coordinates: lat: -35.013333333333
lon: 117.91333333333
Riebeckite granite was used for the facing stones of the Canton Viaduct from Moyles Quarry (a.k.a. Canton Viaduct Quarry) now part of Borderland State Park in Massachusetts, US. The commonwealth's name is even taken from an Algonquian word for the Great Blue Hill, which got its color from this form of granite. Crocidolite (fibrous riebeckite).

Geographic entities mentioned:
surface_form: Great Blue Hill
instance_of: Mountain
countries: United States
coordinates: lat: 42.212044444444
lon: -71.115605555556