Sarmila/GeoWiki-Features huggingface dataset:
The agreements also resulted in the Russian Empire losing control of most Afghan territory it conquered, with the exception of Panjdeh. The Pamir Mountains were demarcated as a border line between the Russian Empire and Afghanistan as well. The Taghdumbash would be the subject of a later Afghan-China agreement. To conclude their agreement, one peak was named Mount Concord.

Geographic entities mentioned:
surface_form: Taghdumbash
instance_of: Valley
countries: People's Republic of China
coordinates: lat: 37.2
lon: 75.4
Maskut. The Maskut (also known as Mazkut, Muskur'&quot;) were a group of Massagetaen-Sarmato-Alanian tribes located in the eastern part of the Caucasus, along the western coast of the Caspian Sea. They lived between Derbent and Shaporan, which corresponds to present-day northeast Azerbaijan and southeast Dagestan (Russia).

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
Mount O'Beirne. Mount O'Beirne is a mountain in the Continental Ranges on the border of Alberta and British Columbia. It is Alberta's 59th most prominent mountain.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount o'beirne
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9286
lon: -118.619
Mount O'Beirne. Mount O'Beirne is a mountain in the Continental Ranges on the border of Alberta and British Columbia. It is Alberta's 59th most prominent mountain.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Mount O'Beirne. Mount O'Beirne is a mountain in the Continental Ranges on the border of Alberta and British Columbia. It is Alberta's 59th most prominent mountain.

Geographic entities mentioned:
surface_form: mount o'beirne
instance_of: Mountain
countries: Canada
coordinates: lat: 52.9286
lon: -118.619
The county comprises the upper valley of the Bum-chu or Arun River, with the valleys of its tributaries, the valleys of the Rongshar Tsangpo and the Lapchi Gang Tsanpo which flow south into Nepal. It is bordered on the south by the main range of the Himalayas, including Mount Everest (Tib. Jomolangma), Makalu and Cho Oyu.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
It is bordered on the south by the main range of the Himalayas, including Mount Everest (Tib. Jomolangma), Makalu and Cho Oyu. The present county administration is located at Shelkar, about east of Tingri (town).

Geographic entities mentioned:
surface_form: Makalu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.889166666667
lon: 87.088611111111
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
It is long from east to west and wide from north to south, with a total area of about. Tingri County is located at the northern foot of the middle section of the Himalayas, and at the northern foot of Mount Everest. The county's landscape is extremely mountainous, with an average altitude of more than above sea level, and the county seat situated at an altitude of above sea level.

Geographic entities mentioned:
surface_form: Mount Everest
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 27.988055555555555
lon: 86.925
The county's landscape is extremely mountainous, with an average altitude of more than above sea level, and the county seat situated at an altitude of above sea level. The world's highest peak, Mount Everest, and the world's sixth-highest mountain, Cho Oyu, are located in the county. The Arun River flows eastward out of the country. Climate.

Geographic entities mentioned:
surface_form: Cho Oyu
instance_of: Mountain
countries: Nepal
People's Republic of China
coordinates: lat: 28.094166666667
lon: 86.660833333333
Samuli Paulaharju has also recorded a memoir of a typical the case of &quot;Salkko-from the south of Lake Inari in his book &quot;Memoirs of Lapland&quot; (&quot;Lapin muisteluksia&quot;). The story has also been published in the collection of &quot;Mythical Stories&quot; (&quot;Myytillisiä tarinoita&quot;) edited by Lauri Simonsuuri.

Geographic entities mentioned:
surface_form: Lake Inari
instance_of: Lake
countries: Finland
coordinates: lat: 68.9596511
lon: 27.6017069
The closest peak to Fernow is Copper Peak, to the north, and the nearest higher peak is Bonanza Peak, to the north. Mount Fernow is flanked by several glaciers. Other large glaciated peaks are nearby, such as Seven Fingered Jack to the south. The headwaters of the Entiat River rise from the south slopes of Mount Fernow and the east slopes of Seven Fingered Jack. History.

Geographic entities mentioned:
surface_form: Seven Fingered Jack
instance_of: Mountain
countries: United States
coordinates: lat: 48.1503921
lon: -120.8143813
It is also the highest peak of the Entiat Mountains, a sub-range of the Cascades. Mount Fernow's prominence is, making it the sixtieth-most-prominent peak in Washington. The closest peak to Fernow is Copper Peak, to the north, and the nearest higher peak is Bonanza Peak, to the north. Mount Fernow is flanked by several glaciers.

Geographic entities mentioned:
surface_form: bonanza peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.2378
lon: -120.866
Mount Fernow. Mount Fernow is a tall peak in the North Cascades in the U.S. state of Washington and within the Glacier Peak Wilderness of the Wenatchee National Forest. At in elevation it is the eighth-highest peak in Washington and the state's third-highest non-volcanic peak. It is also the highest peak of the Entiat Mountains, a sub-range of the Cascades.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: glacier peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.11194444444445
lon: -121.11416666666666
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Mount Fernow. Mount Fernow is a tall peak in the North Cascades in the U.S. state of Washington and within the Glacier Peak Wilderness of the Wenatchee National Forest. At in elevation it is the eighth-highest peak in Washington and the state's third-highest non-volcanic peak. It is also the highest peak of the Entiat Mountains, a sub-range of the Cascades.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
At in elevation it is the eighth-highest peak in Washington and the state's third-highest non-volcanic peak. It is also the highest peak of the Entiat Mountains, a sub-range of the Cascades. Mount Fernow's prominence is, making it the sixtieth-most-prominent peak in Washington. The closest peak to Fernow is Copper Peak, to the north, and the nearest higher peak is Bonanza Peak, to the north.

Geographic entities mentioned:
surface_form: washington
instance_of: Lake
countries: United States
coordinates: lat: 47.616666666667
lon: -122.26472222222
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Mount Fernow. Mount Fernow is a tall peak in the North Cascades in the U.S. state of Washington and within the Glacier Peak Wilderness of the Wenatchee National Forest. At in elevation it is the eighth-highest peak in Washington and the state's third-highest non-volcanic peak. It is also the highest peak of the Entiat Mountains, a sub-range of the Cascades.

Geographic entities mentioned:
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Mount Fernow's prominence is, making it the sixtieth-most-prominent peak in Washington. The closest peak to Fernow is Copper Peak, to the north, and the nearest higher peak is Bonanza Peak, to the north. Mount Fernow is flanked by several glaciers. Other large glaciated peaks are nearby, such as Seven Fingered Jack to the south.

Geographic entities mentioned:
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Mount Fernow is flanked by several glaciers. Other large glaciated peaks are nearby, such as Seven Fingered Jack to the south. The headwaters of the Entiat River rise from the south slopes of Mount Fernow and the east slopes of Seven Fingered Jack. History. Mount Fernow was named by Albert H.

Geographic entities mentioned:
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
The headwaters of the Entiat River rise from the south slopes of Mount Fernow and the east slopes of Seven Fingered Jack. History. Mount Fernow was named by Albert H. Sylvester in honor of Bernhard Fernow, a German forester who moved to the United States and worked for the Division of Forestry in the United States Department of Agriculture in the late 19th century.

Geographic entities mentioned:
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Mount Fernow was named by Albert H. Sylvester in honor of Bernhard Fernow, a German forester who moved to the United States and worked for the Division of Forestry in the United States Department of Agriculture in the late 19th century. Mount Fernow was first summited in 1932 by a party including Oscar Pennington and Hermann Ulrichs. A small unnamed lake sits on the northwestern slopes of Fernow.

Geographic entities mentioned:
surface_form: mount fernow
instance_of: Mountain
countries: United States
coordinates: lat: 48.1619
lon: -120.808
Anif Palace. Anif Palace (), also known as the Water Palace Anif, is located beside an artificial pond in Anif on the southern edge of Salzburg, Austria. The palace was once the seat of the bishops of Chiemsee, and then later was used as a court until the nineteenth century. It was remodeled between 1838 and 1848 in the neo-Gothic style.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
From 1530 the water palace is mentioned regularly as a fief given by the respective Archbishop of Salzburg. It was so given to the bishops of Chiemsee after a restoration by Johann Ernst von Thun in 1693; from then on the bishops used it as a summer residence. It consisted simply of a plain four-story dwelling with a two-story building connecting it to a chapel.

Geographic entities mentioned:
surface_form: Chiemsee
instance_of: Lake
countries: Germany
coordinates: lat: 47.89
lon: 12.47
Bacatá was the main seat of the &quot;zipa&quot;, the ruler of the Bogotá savanna and adjacent areas. The name of the Colombian capital, Bogotá, is derived from Bacatá, but founded as Santafe de Bogotá in the western foothills of the Eastern Hills in a different location than the original settlement Bacatá, west of the Bogotá River, eventually named after Bacatá as well.

Geographic entities mentioned:
surface_form: Bogotá River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Etymology. The word Bacatá is Chibcha, the language of the indigenous Muisca, who inhabited the Altiplano Cundiboyacense before the Spanish conquest. The word is a combination of or, and, meaning &quot;outside&quot;, &quot;enclosure&quot; and &quot;farmfield(s)&quot; respectively. The name is translated as &quot;(enclosure) outside the farmfields&quot;, or &quot;limit of the farmfields&quot;.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
The many lakes, wetlands and rivers, remainders of Lake Humboldt, on the Bogotá savanna were cherished as products of their gods. An important lake for the Muisca was Lake Guatavita, a circular lake at an altitude of to the northeast of present-day Guatavita. This lake formed the basis for the -not so much- legend of &quot;El Dorado&quot;; the &quot;city or man of gold&quot;.

Geographic entities mentioned:
surface_form: Lake Guatavita
instance_of: Lake
countries: Colombia
coordinates: lat: 4.9772222222222
lon: -73.775555555556
The people constructed temples to honour their main deities; Sué (the Sun) and his wife Chía, the Moon. Another important deity for the Muisca was Bochica, who according to their mythology prevented the main river of the Bogotá savanna, the Bogotá River, from frequent overflowings by creating the Tequendama Falls.

Geographic entities mentioned:
surface_form: Bogotá River
instance_of: Watercourse
countries: Colombia
coordinates: lat: 5.25
lon: -73.666666666667
Analysis of the top soils surrounding the Bogotá River in proximity to Bacatá revealed several raised terrains used for agriculture. Muisca Confederation. The name Muisca Confederation has been given to the loose collection of &quot;caciques&quot; who governed several small settlements on the Altiplano Cundiboyacense in the times before the Spanish conquest.

Geographic entities mentioned:
surface_form: Altiplano Cundiboyacense
instance_of: Plateau
countries: Colombia
coordinates: lat: 5.532209
lon: -73.362877
The Spanish chroniclers describe a system of tributes or subordinate &quot;cacicazgos&quot; on the Bogotá savanna; dependencies of the &quot;zipa&quot; of Bacatá. The villages of Simijaca, Guachetá, Ubaté, Chocontá, Nemocón, Zipaquirá, Guatavita, Suba, Ubaqué, Tibacuy, Fusagasugá, Pasca, Cáqueza, Teusacá, Tosca, Guasca, and Pacho are described as part of the Bacatá rule.

Geographic entities mentioned:
surface_form: Teusacá
instance_of: Watercourse
countries: Colombia
coordinates: lat: 4.56313889
lon: -74.02869444
Lake Jasper. Lake Jasper is a permanent freshwater lake in the locality of Lake Jasper, in the South West area of Western Australia. It has evidence of ancient Aboriginal activity beneath its waters. The lake is located on a flat sandy plain, the Scott Coastal Plain, with a high dune ridge to the west and the Donnelly River to the east.

Geographic entities mentioned:
surface_form: lake jasper
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
Lake Jasper. Lake Jasper is a permanent freshwater lake in the locality of Lake Jasper, in the South West area of Western Australia. It has evidence of ancient Aboriginal activity beneath its waters. The lake is located on a flat sandy plain, the Scott Coastal Plain, with a high dune ridge to the west and the Donnelly River to the east.

Geographic entities mentioned:
surface_form: lake jasper
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
surface_form: lake jasper
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
The lake is contained within the boundaries of the D'Entrecasteaux National Park. The camp site has seating facilities on the eastern side of the lake, but is subject to a complete fire ban and forbids vehicle access to the shoreline; the camp site is only accessible by four-wheel drive vehicles. Lake Jasper has two smaller lakes located to the east: Lake Wilson and Lake Smith.

Geographic entities mentioned:
surface_form: lake jasper
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
The lake has significant floristic value as it supports an extensive area of tall sedgeland. The area is also an important habitat for fish, waterbirds, invertebrates and frogs. The lake is known as a &quot;White Water Lake&quot; as the lack of tannic acid in the water allows good light dispersion. The lake water is of a high quality and high quality artesian water also exists in the area.

Geographic entities mentioned:
surface_form: white water lake
instance_of: Lake
countries: Australia
coordinates: lat: -34.410555555556
lon: 115.68222222222
Tourism. There are a few cottages in the area around Loch Dionard, and the river southward has fishing and tourist destinations. There are also a few heritage paths and trails in the area but, due to its isolation and the much more accessible Loch Awe (25 miles away on the A837), Loch Dionard remains isolated.

Geographic entities mentioned:
surface_form: Loch Awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.083333333333
lon: -4.9666666666667
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
surface_form: loch awe
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.291475
lon: -5.231141
The most notable river flowing into Loch Dionard is the Allt an Eassain Ghil which provides water, from An Dubh-Loch and Lochan Ulbha which themselves bring in water from the mountain peaks of Sabhal Mor, Meall Horn, Creagan Meall Horn, Coire Lochan Ulbha. Other rivers include Allt Creag Urbhard, from An t-Sail Mhor, Allt Horn and Allt Eilidh a' Chleirich.

Geographic entities mentioned:
surface_form: sail
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.571
lon: -3.242
surface_form: sail mhor
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.844525
lon: -5.315659
Loch Dionard. Loch Dionard is a medium-sized loch in the Durness Parish, in Sutherland, Highland Council Area, Northern Scotland. It is in the North-Western Highlands about four miles south of Polla. Access. Loch Dionard is away from the settlements of Eriboll, Rhiconich, Achriesgill and Alltnacaillich, that don't have direct road access to the loch.

Geographic entities mentioned:
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
It is in the North-Western Highlands about four miles south of Polla. Access. Loch Dionard is away from the settlements of Eriboll, Rhiconich, Achriesgill and Alltnacaillich, that don't have direct road access to the loch. There are two small roads connecting tourist cottages and mountain trains/portages in the area, to the rest of Scotland.

Geographic entities mentioned:
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
It follows the banks of the River Dionard to Gualin House and the A838 away, with access to Durness further north. Geography. Loch Dionard is above standard sea level, which is relatively high for a loch, but far from any mountain peaks. As a result, it is a consolidation point for many rivers and streams that run from the mountains into the Atlantic Ocean.

Geographic entities mentioned:
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
As a result, it is a consolidation point for many rivers and streams that run from the mountains into the Atlantic Ocean. The most notable river flowing into Loch Dionard is the Allt an Eassain Ghil which provides water, from An Dubh-Loch and Lochan Ulbha which themselves bring in water from the mountain peaks of Sabhal Mor, Meall Horn, Creagan Meall Horn, Coire Lochan Ulbha.

Geographic entities mentioned:
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
Tourism. There are a few cottages in the area around Loch Dionard, and the river southward has fishing and tourist destinations. There are also a few heritage paths and trails in the area but, due to its isolation and the much more accessible Loch Awe (25 miles away on the A837), Loch Dionard remains isolated.

Geographic entities mentioned:
surface_form: loch dionard
instance_of: Lake
countries: United Kingdom
coordinates: lat: 58.39897
lon: -4.8133
Keene maintained a country home at Monkton, Maryland, and a home in England with a stable at Melton Mowbray where he kept up to ten field hunters for fox hunting. In addition, he had a seasonal residence at Ayer's Cliff, Quebec, on Lake Massawippi. In strained financial circumstances later in life, he retired to Quebec to be close to his sister. In 1938, he published a memoir, 'Full Tilt.

Geographic entities mentioned:
surface_form: Lake Massawippi
instance_of: Lake
countries: Canada
coordinates: lat: 45.2158
lon: -71.9994
This post was indeed abandoned after this season, and the company had no permanent presence in the district for many years. Manitoba House, which was intended to serve a large area, between Riding Mountain and Lake Winnipeg, was established on the west side of Lake Manitoba, about 15 miles south of the Narrows, in the 1820s. Treaty 2 was signed on August 21, 1871, at Manitoba House.

Geographic entities mentioned:
surface_form: Lake Winnipeg
instance_of: Lake
countries: Canada
coordinates: lat: 52.116666666667
lon: -97.25
Rainbow Bridge & Veterans Memorial Bridge (Texas). The Rainbow Bridge and Veterans Memorial Bridge are two bridges that cross the Neches River in Southeast Texas just upstream from Sabine Lake. It allows State Highway 87 and State Highway 73 to connect Port Arthur in Jefferson County on the southwest bank of the river. Bridge City in Orange County is on the northeast bank. Rainbow Bridge.

Geographic entities mentioned:
surface_form: Sabine Lake
instance_of: Lake
countries: United States
coordinates: lat: 29.875
lon: -93.8475
A cave discovered on the north side of Camelback Mountain indicates that it was used as a sacred site by the prehistoric Hohokam culture before they abandoned the area in the 14th century. In January 1879, United States President Rutherford B. Hayes included Camelback Mountain as part of a one million acre (4,000 km2) reservation for the Salt River Pima and Maricopa American Indian tribes.

Geographic entities mentioned:
surface_form: hayes
instance_of: Mountain
countries: United States
coordinates: lat: 61.6403
lon: -152.411
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
Camelback Mountain. Camelback Mountain is a mountain in Phoenix, Arizona, United States. The name is derived from its shape, which resembles the hump and head of a kneeling camel. The mountain, a prominent landmark, is the highest peak in the Phoenix metropolitan area and located between the Arcadia neighborhood of Phoenix and the town of Paradise Valley.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
History. A cave discovered on the north side of Camelback Mountain indicates that it was used as a sacred site by the prehistoric Hohokam culture before they abandoned the area in the 14th century. In January 1879, United States President Rutherford B.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
Six months later, at the behest of Charles Poston, the Arizona Territorial Legislature reversed the decision in order to ensure the primacy of the 5000 non-Indian area residents as well as their continued access to Salt River water. Efforts to protect Camelback Mountain as a natural preserve began in the early 1910s. However, by the 1960s, nearly all of the area had been sold to private interests.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
The area became a Phoenix city park in 1968. The peak lends its name to a major east-west street in the Phoenix area called Camelback Road that runs about starting from the eastern border of Scottsdale through the Phoenix metropolitan area to the westside suburb of Litchfield Park. Camelback Mountain is designated as a Phoenix Point of Pride. Geology.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
25 million years old). Recreation. The Echo Canyon Recreation Area is a public park for Camelback Mountain trails and facilities maintained by the City of Phoenix Parks and Recreation Department. Facilities include a parking area, restrooms and some water. In 2024, the city approved closure of park trails between 8 a.m. and 5 p.m. during extreme hear conditions.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
In 2024, the city approved closure of park trails between 8 a.m. and 5 p.m. during extreme hear conditions. Two hiking trails ascend to the peak of Camelback Mountain. The Echo Canyon Trail is 1.14 miles (1900 m) and the Cholla Trail is 1.4 mi (2300 m). Both trails are considered strenuous with steep grades. The hiking path has dirt, gravel, boulders, and some handrail-assisted sections.

Geographic entities mentioned:
surface_form: camelback mountain
instance_of: Mountain
countries: United States
coordinates: lat: 33.5144875
lon: -111.9618124
Agriculture and forestry are the main industries in the area, and there is significant grain and milk production. The landscape in the west is relatively flat, with well-cultivated fields and some marshland (Høstadmyra), while in the east it is heavily hilly with forests and mountains. The highest peak is Storheia at above sea level. History.

Geographic entities mentioned:
surface_form: Storheia
instance_of: Mountain
countries: Norway
coordinates: lat: 63.403333333333
lon: 10.200555555556
Since 1 July 2009, it is part of the town Thale. Geography. Treseburg lies at the confluence of the Luppbode stream with the River Bode in the Bode Gorge, southwest of Thale, at an average height of. Below Treseburg (downstream) lies the nature reserve of the Bode Gorge, through which a footpath, roughly 10 kilometres long, runs to Thale and the &quot;Rosstrappe&quot;.

Geographic entities mentioned:
surface_form: Bode Gorge
instance_of: Valley
countries: Germany
coordinates: lat: 51.735555555556
lon: 11.009722222222
Geography. Treseburg lies at the confluence of the Luppbode stream with the River Bode in the Bode Gorge, southwest of Thale, at an average height of. Below Treseburg (downstream) lies the nature reserve of the Bode Gorge, through which a footpath, roughly 10 kilometres long, runs to Thale and the &quot;Rosstrappe&quot;. This footpath is closed during the winter due to the danger of rockfalls.

Geographic entities mentioned:
surface_form: Bode Gorge
instance_of: Valley
countries: Germany
coordinates: lat: 51.735555555556
lon: 11.009722222222
He was prevailed upon to undertake the government of a monastery in the area, but being unsuccessful in attempting to reform the monks tepidity and indolence, he retired first to Monte Pruno, and finally in 1155 in the desert valley of &quot;Stabulum Rodis&quot;, later known as Maleval, in the territory of Castiglione della Pescaia, Diocese of Grosseto, where he was joined by Albert.

Geographic entities mentioned:
surface_form: Monte Pruno
instance_of: Mountain
countries: Italy
coordinates: lat: 40.4118309
lon: 15.3628179
The lake's location directly south of the Port Said Airport restricts the city's capacity for growth. Suez Canal. Lake Manzala is the northernmost of three natural lakes intersected by the Suez Canal, the other two being Lake Timsah and the Great Bitter Lake. Construction of the canal proceeded from north to south, reaching Manzala first.

Geographic entities mentioned:
surface_form: Lake Timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
surface_form: Great Bitter Lake
instance_of: Lake
countries: Egypt
coordinates: lat: 30.3225
lon: 32.3825
surface_form: timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
surface_form: lake timsah
instance_of: Lake
countries: Egypt
coordinates: lat: 30.577777777778
lon: 32.288888888889
surface_form: great bitter lake
instance_of: Lake
countries: Egypt
coordinates: lat: 30.3225
lon: 32.3825
Lake Manzala. Lake Manzala (&quot;baḥīrat manzala&quot;), also Manzaleh, is a brackish lake, sometimes called a lagoon, in northeastern Egypt on the Nile Delta near Port Said and a few miles from the ancient ruins at Tanis. It is the largest of the northern deltaic lakes of Egypt. As of 2008 it is long and wide. Etymology. The lake's name derives from.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
surface_form: lake manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
Lake Manzala. Lake Manzala (&quot;baḥīrat manzala&quot;), also Manzaleh, is a brackish lake, sometimes called a lagoon, in northeastern Egypt on the Nile Delta near Port Said and a few miles from the ancient ruins at Tanis. It is the largest of the northern deltaic lakes of Egypt. As of 2008 it is long and wide. Etymology. The lake's name derives from.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
surface_form: lake manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
Geography. Lake Manzala is long but quite shallow. Though Lake Manzala's unaltered depth is only, alterations to the depth were made during the construction of the Suez Canal to allow the Canal to extend lengthwise along the lake. Its bed is soft clay. Before construction of the Suez Canal, Lake Manzala was separated from the Mediterranean Sea by a strip of sand wide.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
Its bed is soft clay. Before construction of the Suez Canal, Lake Manzala was separated from the Mediterranean Sea by a strip of sand wide. Port Said was established adjacent to Lake Manzala during the nineteenth century to support canal construction and related travel. The lake's location directly south of the Port Said Airport restricts the city's capacity for growth. Suez Canal.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
surface_form: lake manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
Suez Canal. Lake Manzala is the northernmost of three natural lakes intersected by the Suez Canal, the other two being Lake Timsah and the Great Bitter Lake. Construction of the canal proceeded from north to south, reaching Manzala first. Due to the lake's shallowness, it was necessary to dig a banked channel for ships to pass. Ecology.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
The project was unprofitable: crops did not grow well in the salty soil and the value of resulting produce was less than the market value of the fish that the reclaimed land had formerly yielded. By 2001, Lake Manzala had lost approximately 80 percent of its former area through the effects of drainage efforts.

Geographic entities mentioned:
surface_form: manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
Geography. Lake Manzala is long but quite shallow. Though Lake Manzala's unaltered depth is only, alterations to the depth were made during the construction of the Suez Canal to allow the Canal to extend lengthwise along the lake. Its bed is soft clay. Before construction of the Suez Canal, Lake Manzala was separated from the Mediterranean Sea by a strip of sand wide.

Geographic entities mentioned:
surface_form: lake manzala
instance_of: Lake
countries: Egypt
coordinates: lat: 31.291
lon: 32.018
List of rivers of West Bengal. Most of the rivers of West Bengal originate from the Himalayan in the north or from the Chota Nagpur plateau in the west and flow south or southeast over the state. Due to the rivers in the western plains, the water is very scarce or bare at any other time of the year, especially in the fall of the Falgun-Chaitra, except during the monsoon.

Geographic entities mentioned:
surface_form: Chota Nagpur plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
Batova. The Batova reka () is a 39 km long river in northeastern Bulgaria. The river takes its source under the name Kavakdere from a karst spring at an altitude of 309 m in the Frangen Plateau some 1.2 km southwest of the village of Kumanovo. Throughout its whole course the Batova reka flows in a canyon-like valley with forest slopes prone to landslides.

Geographic entities mentioned:
surface_form: Frangen Plateau
instance_of: Plateau
countries: Bulgaria
coordinates: lat: 43.291
lon: 27.824
Snowline Joint Unified School District. The Snowline Joint Unified School District (SJUSD) is the school district for part of the Victor Valley in the Mojave Desert and northeastern San Gabriel Mountains, located within San Bernardino County, California. The district extends into Los Angeles County.

Geographic entities mentioned:
surface_form: Victor Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.5
lon: -117.3
Shelley in 1993 based on samples collected by Dr. Shelley in 1991 as well as museum type specimens collected by K. Goeden in 1968. The genus is found in the Cascade mountains on the Washington/Oregon border as well as down into the Willamette Valley. Description. &quot;Thrinaphe&quot; is a robust Xystodesmid with an overall brown ground color and slight blueish tinge to the tergites.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
Tramitichromis trilineatus. &quot;Tramitichromis trilineatus&quot; is a species of cichlid endemic to Lake Malawi where it occurs in the southeastern portion of the lake, preferring shallow waters with sandy substrates. It can reach a length of TL. It can also be found in the aquarium trade.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
A number of summer camps are located nearby. Facility. Deerhurst offers accommodations for 1,000 people in 400 rooms and suites, many of which are privately owned or blocked by timeshares. Rates for suites overlooking Peninsula Lake can exceed $650 a night in peak summer season. The career of singer Shania Twain took off when she was one of the performers at the resort. History.

Geographic entities mentioned:
surface_form: Peninsula Lake
instance_of: Lake
countries: Canada
coordinates: lat: 45.3333
lon: -79.1167
His given name was Houjing (后敬). Reign. Fa was a son of the King Gao of Xia and thus a grandson of Kong Jia. During his inaugural celebration, all of his vassals gathered at his palace. The first earthquake ever recorded took place in the 7th year of his rule at Mount Tai in modern Shandong during his reign. The event has been dated to 1740 BC as the Mount Tai earthquake.

Geographic entities mentioned:
surface_form: Mount Tai
instance_of: Mountain
countries: People's Republic of China
coordinates: lat: 36.266666666667
lon: 117.1
Kleinglockner. At the height of the Kleinglockner is the third highest mountain summit in Austria. However, with a prominence of only 17 metres it is arguable whether it can be counted as an independent mountain, or just as a subpeak of the Großglockner. It lies in the Glockner Group of Austria's Central Alps, the middle section of the Hohe Tauern.

Geographic entities mentioned:
surface_form: kleinglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.073888888889
lon: 12.696111111111
Its peak forms part of the Glockner crest or ridge (&quot;Glocknerkamm&quot;) and lies exactly on the border between the Austrian state of Carinthia and Lienz District in the East Tyrol.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The Kleinglockner has the shape of a sharp edge, covered with the so-called Glockner Cornice (&quot;Glocknerwechte&quot;) and, depending on the conditions, can make the ascent of the mountain dangerous to almost impossible. The climbing history of the Kleinglockner is closely linked to that of the Großglockner, because the first climbers, coming from the south and east, had to cross it.

Geographic entities mentioned:
surface_form: kleinglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.073888888889
lon: 12.696111111111
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Kleinglockner. At the height of the Kleinglockner is the third highest mountain summit in Austria. However, with a prominence of only 17 metres it is arguable whether it can be counted as an independent mountain, or just as a subpeak of the Großglockner. It lies in the Glockner Group of Austria's Central Alps, the middle section of the Hohe Tauern.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
The Kleinglockner has the shape of a sharp edge, covered with the so-called Glockner Cornice (&quot;Glocknerwechte&quot;) and, depending on the conditions, can make the ascent of the mountain dangerous to almost impossible. The climbing history of the Kleinglockner is closely linked to that of the Großglockner, because the first climbers, coming from the south and east, had to cross it.

Geographic entities mentioned:
surface_form: glockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Kleinglockner. At the height of the Kleinglockner is the third highest mountain summit in Austria. However, with a prominence of only 17 metres it is arguable whether it can be counted as an independent mountain, or just as a subpeak of the Großglockner. It lies in the Glockner Group of Austria's Central Alps, the middle section of the Hohe Tauern.

Geographic entities mentioned:
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
It lies in the Glockner Group of Austria's Central Alps, the middle section of the Hohe Tauern. Geographically and geologically speaking, it is viewed a secondary summit of the neighbouring Großglockner, but in the literature, in view of its importance to mountaineering, it is in some cases treated as separate.

Geographic entities mentioned:
surface_form: großglockner
instance_of: Mountain
countries: Austria
coordinates: lat: 47.074528
lon: 12.69385
Tocal, New South Wales. Tocal (meaning 'plenty' in the local Aboriginal language) is a locality situated in the lower Hunter Valley, of New South Wales, Australia. Located approximately north of Maitland, and about north of Sydney it is located at the junction of the Paterson River and Webbers Creek. Prior to European exploration, Tocal was home to the Gringai clan of the Wonnarua people.

Geographic entities mentioned:
surface_form: Hunter Valley
instance_of: Valley
countries: Australia
coordinates: lat: -32.56
lon: 151.17083333333332
Signal. As with almost every local FM station in the area, the broadcasting tower is located south of town on Casper Mountain. With its 2,700 watt effective radiated power, the station is audible throughout most of Natrona County, and into Converse County, Wyoming.

Geographic entities mentioned:
surface_form: Casper Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.732944
lon: -106.324167
Bhim Sen Singhal (also known as B. S. Singhal) is the director of neurology at Bombay Hospital Institute of Medical Sciences in Mumbai, India. Early life and education. Singhal was born at Mount Abu on 23 January 1933. After schooling at Mount Abu and premedical studies at Maharaja's College in Jaipur, he studied medicine at the Grant Medical College and Sir J. J. Group of Hospitals in Mumbai.

Geographic entities mentioned:
surface_form: Mount Abu
instance_of: Mountain
countries: India
coordinates: lat: 24.5925
lon: 72.708333333333
Mount Carnarvon. Mount Carnarvon is a mountain summit located in the Kiwetinok River Valley of Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
Then in 1874, he effected the settlement of difficulties between Canada and British Columbia on the &quot;Carnarvon Terms&quot;. The first ascent of the mountain was made in 1904 by members of the Dominion Topographic Survey. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Its nearest higher peak is The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains. Mount Carnarvon is situated five kilometers northwest of Emerald Lake, but is hidden from view behind Emerald Peak. However, Carnarvon is visible from Highway 1, the Trans-Canada Highway.

Geographic entities mentioned:
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 53.18338
lon: -106.96724
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 60.2663
lon: -134.7507
surface_form: emerald peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.459722222222226
lon: -116.57027777777778
surface_form: emerald lake
instance_of: Lake
countries: Canada
coordinates: lat: 51.444
lon: -116.531
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
History. Originally known as &quot;Emerald Mountain&quot;, the mountain was named in 1900 by Alexander MacKinnon Burgess (Commissioner of Public Lands) after Henry Herbert, 4th Earl of Carnarvon (1831-1890), who in 1867 authored the British North America Act which conferred self-government on Canada.

Geographic entities mentioned:
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
Then in 1874, he effected the settlement of difficulties between Canada and British Columbia on the &quot;Carnarvon Terms&quot;. The first ascent of the mountain was made in 1904 by members of the Dominion Topographic Survey. The mountain's name was officially adopted in 1924 when approved by the Geographical Names Board of Canada. Geology.

Geographic entities mentioned:
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
Mount Carnarvon. Mount Carnarvon is a mountain summit located in the Kiwetinok River Valley of Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains.

Geographic entities mentioned:
surface_form: the president
instance_of: Mountain
countries: Canada
coordinates: lat: 51.50083333333333
lon: -116.56194444444445
Its nearest higher peak is The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains. Mount Carnarvon is situated five kilometers northwest of Emerald Lake, but is hidden from view behind Emerald Peak. However, Carnarvon is visible from Highway 1, the Trans-Canada Highway.

Geographic entities mentioned:
surface_form: the president
instance_of: Mountain
countries: Canada
coordinates: lat: 51.50083333333333
lon: -116.56194444444445
Mount Carnarvon. Mount Carnarvon is a mountain summit located in the Kiwetinok River Valley of Yoho National Park, in the Canadian Rockies of British Columbia, Canada. Its nearest higher peak is The President, to the north-northeast. Both are part of the President Range which is a subset of the Waputik Mountains.

Geographic entities mentioned:
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
Both are part of the President Range which is a subset of the Waputik Mountains. Mount Carnarvon is situated five kilometers northwest of Emerald Lake, but is hidden from view behind Emerald Peak. However, Carnarvon is visible from Highway 1, the Trans-Canada Highway. The months July through September offer the most favorable weather for viewing or climbing Mount Carnarvon. History.

Geographic entities mentioned:
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Mount Carnarvon is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
Climate. Based on the Köppen climate classification, Mount Carnarvon is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. Precipitation runoff from Mount Carnarvon drains into tributaries of the Kicking Horse River.

Geographic entities mentioned:
surface_form: mount carnarvon
instance_of: Mountain
countries: Canada
coordinates: lat: 51.47027777777778
lon: -116.58888888888889
Initially, the Aller flows rather like a canalised brook in a northwestern direction through low hills and intensively farmed arable fields. As it does, it passes the Flechtingen Hills to the east and another range of hills to the west that stretches from the Lappwald over the Hohes Holz as far as Oschersleben (Bode). The river passes the villages of Eilsleben and Weferlingen.

Geographic entities mentioned:
surface_form: Flechtingen Hills
instance_of: Mountain
countries: Germany
coordinates: lat: 52.2833
lon: 11.2167
In the upper courses the Aller filled the flat, swampy basin of the Drömling from which the water drained only slowly. In addition the Ohre river flowed diffusely through the Drömling. Because the watershed between Weser and Elbe lay in the middle of the Drömling, the river could even change its course so that the waters of the Aller flowed into the Elbe.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
surface_form: aller
instance_of: Watercourse
countries: Germany
coordinates: lat: 52.945825
lon: 9.18561389
Aller (Germany). The Aller () is a river in the states of Saxony-Anhalt and Lower Saxony in Germany. It is a right-hand, and hence eastern, tributary of the Weser and is also its largest tributary. Its last form the Lower Aller federal waterway (). The Aller was extensively straightened, widened and, in places, dyked during the 1960s to provide flood control of the river.

Geographic entities mentioned:
surface_form: aller (germany)
instance_of: Watercourse
countries: Germany
coordinates: lat: 52.945825
lon: 9.18561389