Sarmila/GeoWiki-Features huggingface dataset:
Dore Head can also be reached from Mosedale if starting from Wasdale Head, although a long climb up scree is involved. It is possible instead to ascend Black Comb on easier slopes and then return to the summit. Red Pike is often the start of the Mosedale Horseshoe, a ridgewalk also visiting Scoat Fell and Pillar. Depending upon the strength of the walker Yewbarrow and Kirk Fell may also be added.

Geographic entities mentioned:
surface_form: Scoat Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.490038888889
lon: -3.2998
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
Dore Head can also be reached from Mosedale if starting from Wasdale Head, although a long climb up scree is involved. It is possible instead to ascend Black Comb on easier slopes and then return to the summit. Red Pike is often the start of the Mosedale Horseshoe, a ridgewalk also visiting Scoat Fell and Pillar. Depending upon the strength of the walker Yewbarrow and Kirk Fell may also be added.

Geographic entities mentioned:
surface_form: Yewbarrow
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.464211111111
lon: -3.2773805555556
surface_form: Kirk Fell
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.242
Red Pike (Wasdale). Red Pike is a fell in the English Lake District. It is high and lies due north of Wast Water. It is often climbed as part of the Mosedale Horseshoe, a walk which also includes Pillar. The fell can be confused with Red Pike (Buttermere), not least because its namesake is only away, so according to Alfred Wainwright it is conventional to call it Wasdale Red Pike. Topography.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
Red Pike (Wasdale). Red Pike is a fell in the English Lake District. It is high and lies due north of Wast Water. It is often climbed as part of the Mosedale Horseshoe, a walk which also includes Pillar. The fell can be confused with Red Pike (Buttermere), not least because its namesake is only away, so according to Alfred Wainwright it is conventional to call it Wasdale Red Pike. Topography.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
At the central hub of the high country are Great Gable and its satellites, while two principal ridges fan out on either flank of Ennerdale, the western fells in effect being a great horseshoe around this long wild valley. Red Pike is an outlier of the southern arm. The main watershed runs broadly westwards from Great Gable, dividing the headwaters of Ennerdale and Wasdale.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
Scoat Fell throws out a long southern ridge terminating in Yewbarrow and Red Pike stands part way along. The Red Pike ridge occupies a broad area of high country between Nether Beck in the west and Mosedale in the east. The Mosedale face is steeper with considerable areas of Crag, whilst the western slopes descend slowly over around.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
This narrow depression is squeezed between Black Comb, the birthplace of Mosedale Beck, and Scoat Tarn, the primary feeder of Nether Beck. From the depression it is only a short climb to the summit of Red Pike, the majority of the ridge lying beyond on the long south easterly descent to Dore Head. At this col the watershed turns south west, rising to the twin summits of Yewbarrow.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
At this col the watershed turns south west, rising to the twin summits of Yewbarrow. Dore Head is the source of Over Beck, the stream separating Yewbarrow from the long western flanks of Red Pike. Red Pike presents an almost continuous wall of crags above Mosedale, particularly above Black Comb. Bull and Black Crags meanwhile guard the southern section.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
This whole area is unfrequented with few paths amongst the grassy hillocks and low crags. Scoat Tarn at the head of Nether Beck is by contrast a corrie tarn, held in place by grassy moraines. Its depth is around. Red Pike has a subsidiary southern top with a height of. Geology. The fell is mainly composed of the plagioclase-phyric andesite lavas of the Birker Fell Formation.

Geographic entities mentioned:
surface_form: red pike
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.483
lon: -3.29
KAPP's studios are located in the Liberty Building on North 3rd Street in downtown Yakima, and its transmitter is atop Ahtanum Ridge; KVEW maintains its own studios on North Edison Street in Kennewick, with transmitter on Jump Off Joe Butte. KVEW operates as a semi-satellite of KAPP, serving the Tri-Cities area.

Geographic entities mentioned:
surface_form: Ahtanum Ridge
instance_of: Landform
countries: United States
coordinates: lat: 46.5069
lon: -120.816
The nearest population centre is Riverside-Albert with a population of about 320. The Trans Canada Trail passes across part of Shepody Marsh. Major streams feeding into the bay are the Shepody River, Petitcodiac River and Memramcook River. These three rivers gave the area its name under Acadian occupation in the seventeenth and eighteenth century, Trois Rivieres.

Geographic entities mentioned:
surface_form: Petitcodiac River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.926944444444
lon: -65.188888888889
surface_form: Memramcook River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.867
lon: -64.552
Geography. Toutle is located east of Castle Rock along Washington State Route 504, which is also known as the Spirit Lake Memorial Highway. Toutle is near Mount St. Helens and the Mount St. Helens National Volcanic Monument, which lies at the end of the Spirit Lake Memorial Highway. Education.

Geographic entities mentioned:
surface_form: Mount St. Helens
instance_of: Mountain
countries: United States
coordinates: lat: 46.200277777778
lon: -122.18944444444
Some toponomastic traces of that period exist in the area: Bosco Marengo stems from &quot;Lucus Maricum&quot; and Pietra Marazzi from &quot;Petra Maricorum or Mariciorum&quot;. In the 6th century BC the Po valley was occupied by Celtic peoples coming from the north and realistically also Bassignana had contacts and compenetrations with these peoples.

Geographic entities mentioned:
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
There was no direct translation for &quot;China &quot;proper&quot; in the Chinese language at the time due to differences in terminology used by the Qing to refer to the regions. Outer China usually includes the geographical regions of Dzungaria, Tarim Basin, Gobi Desert, Tibetan Plateau, and Northeast China. Etymology. According to Harry Harding, the concept can date back to 1827.

Geographic entities mentioned:
surface_form: Tibetan Plateau
instance_of: Plateau
countries: People's Republic of China
coordinates: lat: 33
lon: 88
Sand Bay, Wisconsin. Sand Bay is an unincorporated community in the town of Russell, Bayfield County, Wisconsin, United States. The community is located within the Red Cliff Indian Reservation. Sand Bay is located on the South Shore of Lake Superior, north-northwest of the city of Bayfield. The community is also located 37 miles north-northwest of the city of Ashland.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445
The hotel opened to guests in the Spring of 1906, offering 120 beds in 85 rooms. It was hoped that Bergün's altitude and remote location would make it attractive as an acclimatisation location for guests preparing to stay higher up in the Engadin and as a health resort in its own right, based on the air quality.

Geographic entities mentioned:
surface_form: Engadin
instance_of: Valley
countries: Switzerland
coordinates: lat: 46.5497
lon: 9.8959
In 1941, the Jerusalem Biblical Zoo, initially a small children's zoo on Harav Kook Street in central Jerusalem, was moved to a tract at the eastern end of Shmuel HaNavi Street before relocating to the campus of the Hebrew University on Mount Scopus in 1947.

Geographic entities mentioned:
surface_form: Mount Scopus
instance_of: Mountain
countries: Israel
coordinates: lat: 31.7925
lon: 35.244166666667
After defeating the Huron in 1649, the Iroquois conducted a December 1649 attack against the Tabacco people, who fell in 1650–1651. The Iroquois continued to campaign westwards along the north shores of Lake Ontario.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
While the terminal southern and western end of this range is unknowable, the extent along the southern shore of Lake Ontario from Rochester to Buffalo) is about.

Geographic entities mentioned:
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Derventa. Derventa () is a city in Republika Srpska, Bosnia and Herzegovina. It is situated in the Posavina region, northwest of the city of Doboj. As of 2013, the town has a total of 11,631 inhabitants, while the municipality has 27,404 inhabitants. Geography. The Derventa municipality borders Brod, Modriča, Doboj, Stanari, Prnjavor and Srbac, as well as Croatia across the Sava river.

Geographic entities mentioned:
surface_form: Posavina
instance_of: Valley
countries: Croatia
Bosnia and Herzegovina
Serbia
coordinates: lat: 45.16667
lon: 17.33333
AHCA sees about 120,000 visitors each year, who visit the conservation area for mountain biking, camping, swimming, special events, cross-country skiing and more. With over 446 hectares (1,200 acres) of largely forested land located completely within the Humber River Watershed in the headwaters of the Oak Ridges Moraine, AHCA is recognized as a key natural heritage site.

Geographic entities mentioned:
surface_form: Oak Ridges Moraine
instance_of: Mountain
countries: Canada
coordinates: lat: 44.05
lon: -78.86666667
The descriptive passages mix whimsical, often alliterative language with phonetically-spelled dialogue and a strong poetic sensibility (&quot;Agathla, centuries aslumber, shivers in its sleep with splenetic splendor, and spreads abroad a seismic spasm with the supreme suavity of a vagabond volcano&quot;).

Geographic entities mentioned:
surface_form: Agathla
instance_of: Mountain
countries: United States
coordinates: lat: 36.826666666667
lon: -110.22555555556
Baxter State Park. Baxter's history is intertwined with Baxter State Park, which bears his name, and with Mount Katahdin, Maine's highest point (the highest knob on Katahdin is called Baxter Peak). In 1903 Baxter went on a fishing trip to the area around Katahdin for the first time.

Geographic entities mentioned:
surface_form: Mount Katahdin
instance_of: Mountain
countries: United States
coordinates: lat: 45.904355555556
lon: -68.921275
Malargüe River. The Malargüe River (in Spanish: &quot;Río Malargüe&quot;) is a river located in the southern zone of the Mendoza Province, in the west of Argentina. It originates in the Malargüe lake in the Andes range, at 2,500 m above mean sea level, flows into the Malargüe Department and ends in the Llancanelo Lake, being its main tributary.

Geographic entities mentioned:
surface_form: Llancanelo Lake
instance_of: Lake
countries: Argentina
coordinates: lat: -35.622222222222
lon: -69.1425
surface_form: llancanelo lake
instance_of: Lake
countries: Argentina
coordinates: lat: -35.622222222222
lon: -69.1425
Malargüe River. The Malargüe River (in Spanish: &quot;Río Malargüe&quot;) is a river located in the southern zone of the Mendoza Province, in the west of Argentina. It originates in the Malargüe lake in the Andes range, at 2,500 m above mean sea level, flows into the Malargüe Department and ends in the Llancanelo Lake, being its main tributary.

Geographic entities mentioned:
surface_form: mendoza
instance_of: Watercourse
countries: Argentina
coordinates: lat: -32.35
lon: -68.3
surface_form: malargüe river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -35.5
lon: -70
surface_form: río malargüe
instance_of: Watercourse
countries: Argentina
coordinates: lat: -35.5
lon: -70
Malargüe River. The Malargüe River (in Spanish: &quot;Río Malargüe&quot;) is a river located in the southern zone of the Mendoza Province, in the west of Argentina. It originates in the Malargüe lake in the Andes range, at 2,500 m above mean sea level, flows into the Malargüe Department and ends in the Llancanelo Lake, being its main tributary.

Geographic entities mentioned:
surface_form: malargüe river
instance_of: Watercourse
countries: Argentina
coordinates: lat: -35.5
lon: -70
Pizzo di Rodes. Pizzo di Rodes is a mountain of Lombardy, Italy. It has an elevation of 2,831 metres above sea level.

Geographic entities mentioned:
surface_form: pizzo di rodes
instance_of: Mountain
countries: Italy
coordinates: lat: 46.09583333
lon: 9.96027778
Crescent Spire. Crescent Spire is a peak in the Purcell Mountains of the Columbia Mountains in southeastern British Columbia, Canada. Crescent Spire was named in 1933 by James Monroe Thorington because he was impressed with its shape.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: crescent spire
instance_of: Mountain
countries: Canada
coordinates: lat: 50.74989
lon: -116.78549
Crescent Spire. Crescent Spire is a peak in the Purcell Mountains of the Columbia Mountains in southeastern British Columbia, Canada. Crescent Spire was named in 1933 by James Monroe Thorington because he was impressed with its shape.

Geographic entities mentioned:
surface_form: crescent spire
instance_of: Mountain
countries: Canada
coordinates: lat: 50.74989
lon: -116.78549
Santa Clara Valley Athletic League. Santa Clara Valley Athletic League (SCVAL) is a high school athletic conference and part of the CIF Central Coast Section of the California Interscholastic Federation. Its 14+ member schools are in the northern part of the Santa Clara Valley. Each sport is divided into two leagues based on strength.

Geographic entities mentioned:
surface_form: Santa Clara Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.366944444444
lon: -121.98388888889
Establishment. Motivated by nuclear power plants around Lake Michigan and threats to Indiana's sand dunes, an editor of Hyde Park Herald and Openlands Project staff member Lee Botts gathered activists from the four-state region at a conference on April 12, 1969. This was where the participants recommended forming an organization to propose policy solutions for Lake Michigan.

Geographic entities mentioned:
surface_form: Lake Michigan
instance_of: Lake
countries: United States
coordinates: lat: 44.007874
lon: -86.756451
This rendered the taxon invalid. Occasionally, grey-blue or steel-blue walleye are caught in Lake Erie, Lake Ontario, and the Ohio River drainage. Dark blue yellow perch are also sometimes caught in the same areas. A turquoise-colored walleye exists in some waters of the Canadian Shield.

Geographic entities mentioned:
surface_form: Lake Erie
instance_of: Lake
countries: Canada
United States
coordinates: lat: 42.25
lon: -80.99972222222222
surface_form: Lake Ontario
instance_of: Lake
countries: Canada
United States
coordinates: lat: 43.72888888888889
lon: -78.10638888888889
Roanoke metropolitan area. The Roanoke Metropolitan Statistical Area is a Metropolitan Statistical Area (MSA) in Virginia as defined by the United States Office of Management and Budget (OMB). The Roanoke MSA is sometimes referred to as the Roanoke Valley, even though the Roanoke MSA occupies a larger area than the Roanoke Valley.

Geographic entities mentioned:
surface_form: Roanoke Valley
instance_of: Valley
countries: United States
coordinates: lat: 37.266
lon: -79.933
Covering an area of approximately 12,298 square kilometres, it is bordered by the Indian states of Meghalaya, Assam and Tripura to the north, east and south respectively, while domestically it adjoins Chattogram to the southwest and Dhaka and Mymensingh to the west. Prior to Partition in 1947, it included Karimganj subdivision (presently in Barak Valley, Assam, India).

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
From Waterways to Fort Fitzgerald on the Athabasca/Slave River, it used the motor tugboat &quot;Mabel&quot; with three barges; from Fort Smith to Aklavik on the Slave/Mackenzie Rivers, it used a 90-foot twin diesel powered barge with two barges carrying 300-tons per trip; from Fort Smith to Fort Rae (now Behchokǫ̀) on the north end of Great Slave Lake it used a power barge with 100-ton capacity.

Geographic entities mentioned:
surface_form: Great Slave Lake
instance_of: Lake
countries: Canada
coordinates: lat: 61.666666666667
lon: -114
On the Bear River route into Great Bear Lake, where significant silver and uranium mineral exploration was underway in 1934, the company used a series of boats and barges. The tugboat &quot;Norman&quot; operated from Fort Norman (now Tulita) to the head of the first rapids with a 50-ton barge.

Geographic entities mentioned:
surface_form: Great Bear Lake
instance_of: Lake
countries: Canada
coordinates: lat: 66
lon: -121
Port Radium on Great Bear Lake, a mine that supplied much of the uranium used by the Manhattan Project, and later the uranium mines on Lake Athabasca in northern Saskatchewan, were key destinations for the fleet. All of the tugs had extremely shallow draft, and mounted their propellers in cavities under their hull.

Geographic entities mentioned:
surface_form: Lake Athabasca
instance_of: Lake
countries: Canada
coordinates: lat: 59.266666666667
lon: -109.45
Following their heavy casualties, the three RWF battalions of 158th Bde were split up across the division, with 6th RWF transferring on 4 August to 160th Bde. When the breakout from the Normandy beachhead began in early August, XII Corps began pushing south, with 53rd (W) Division clearing the east bank of the River Orne, while XXX Corps captured Mont Pinçon.

Geographic entities mentioned:
surface_form: Mont Pinçon
instance_of: Mountain
countries: France
coordinates: lat: 48.971388888889
lon: -0.62666666666667
According to Al-Fāriqī, Ilghazi selected the route from Kars to Javakheti and Trialeti to reach Tbilisi, where he could camp, rest, and then act against the Georgians. The Muslim army under the overall command of Ilghazi entered the valley of Trialeti in eastern Georgia and encamped in the vicinities of Didgori and Manglisi in 10 August 1121, about a day's march from Tbilisi.

Geographic entities mentioned:
surface_form: vicinities of Didgori
instance_of: Mountain
countries: Georgia
coordinates: lat: 41.760555555555555
lon: 44.50694444444444
Grand Galibier. Grand Galibier (3,228 m) is a mountain of the Cottian Alps in Savoie, France. It is the highest mountain of the Massif des Cerces, a small chain of mountains located about 20 km northwest of Briançon, deep in the heart of the French Alps.

Geographic entities mentioned:
surface_form: cerces
instance_of: Mountain
countries: France
coordinates: lat: 45.0655706
lon: 6.4889393
Grand Galibier. Grand Galibier (3,228 m) is a mountain of the Cottian Alps in Savoie, France. It is the highest mountain of the Massif des Cerces, a small chain of mountains located about 20 km northwest of Briançon, deep in the heart of the French Alps.

Geographic entities mentioned:
surface_form: grand galibier
instance_of: Mountain
countries: France
coordinates: lat: 45.0642
lon: 6.43389
Tschudi was mostly active with buying and selling land in Aker, now a part of Oslo. In 1898 he bought the 400-acre farm Øvre Høybråten, which was parceled out in 1905. Solemskogen near Maridalsvannet was bought in 1897 and parceled out in 1903, in addition he parceled out Økern as well. Tschudi was also active in Bærum. In 1912 he bought Vestre Haslum, which soon was split in 360 lots and sold.

Geographic entities mentioned:
surface_form: Maridalsvannet
instance_of: Lake
countries: Norway
coordinates: lat: 59.98444444
lon: 10.77833333
Hawaii's high volcanoes, Mauna Kea and Mauna Loa, are home to some rare tropical montane grasslands and shrublands. Flora and fauna.

Geographic entities mentioned:
surface_form: Mauna Kea
instance_of: Mountain
countries: United States
coordinates: lat: 19.820555555555554
lon: -155.46805555555557
Lattice Cottage. The Lattice Cottage is a historic summer house on the slopes of Mount Monadnock in Dublin, New Hampshire, United States. Built as an estate guest house in 1929 to a design by Harry Little of Boston, Massachusetts, it is a distinctive example of Arts and Crafts architecture. Description and history.

Geographic entities mentioned:
surface_form: Mount Monadnock
instance_of: Mountain
countries: United States
coordinates: lat: 42.860833333333
lon: -72.108055555556
Description and history. The Lattice Cottage is located on the grounds of the former Amory country estate, a large tract of land rising on the northern slope of Mount Monadnock between Old Troy Road to the west and the mountain's Pumpelly Ridge to the east. It is accessed via a private road that snakes across the historic estate.

Geographic entities mentioned:
surface_form: Mount Monadnock
instance_of: Mountain
countries: United States
coordinates: lat: 42.860833333333
lon: -72.108055555556
Ruby Peak (South Georgia Island). Ruby Peak () is a peak rising on the east side of Olsen Valley to the southwest of Jason Peak, South Georgia. The name appears to be first used on a 1930 British Admiralty chart.

Geographic entities mentioned:
surface_form: Olsen Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: -54.2
lon: -36.6833
surface_form: Jason Peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.183333333333
lon: -36.616666666667
surface_form: ruby peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.2
lon: -36.6667
Ruby Peak (South Georgia Island). Ruby Peak () is a peak rising on the east side of Olsen Valley to the southwest of Jason Peak, South Georgia. The name appears to be first used on a 1930 British Admiralty chart.

Geographic entities mentioned:
surface_form: ruby peak
instance_of: Mountain
countries: United Kingdom
coordinates: lat: -54.2
lon: -36.6667
The park is located in the city center, near Yunnan University, Yuantong Hill, and Wuhua Hill. Cuihu Park is surrounded by a ring road, and along the edge of that road are restaurants and tea houses (some with rooftop dining), shops, and hotels, including the upscale Green Lake Hotel and Grand Park Hotel (formerly the Harbour Plaza Hotel). Cuihu's gulls.

Geographic entities mentioned:
surface_form: cuihu
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
surface_form: green lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
The park is located in the city center, near Yunnan University, Yuantong Hill, and Wuhua Hill. Cuihu Park is surrounded by a ring road, and along the edge of that road are restaurants and tea houses (some with rooftop dining), shops, and hotels, including the upscale Green Lake Hotel and Grand Park Hotel (formerly the Harbour Plaza Hotel). Cuihu's gulls.

Geographic entities mentioned:
surface_form: cuihu
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
Cuihu's gulls. During the winter months, black-headed gulls from Siberia migrate to Kunming, settling in bodies of water around the city and causing Cuihu to become a very popular gull-feeding area. Local vendors sell bread in and around the park, which visitors throw in the air or into the water to feed the gulls. In popular culture.

Geographic entities mentioned:
surface_form: cuihu
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
Green Lake (Kunming). Green Lake Park, or Cui Hu Park (), is an urban park in Kunming, Yunnan Province, China. It was established in the 20th century. The park consists of a group of 4 small sub-lakes linked by bridges built in traditional Chinese architecture. The lake was originally a water reservoir for the city.

Geographic entities mentioned:
surface_form: green lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
Local vendors sell bread in and around the park, which visitors throw in the air or into the water to feed the gulls. In popular culture. Green Lake Park was visited during &quot;The Amazing Race 18&quot; when the park was featured as the &quot;Pit Stop&quot; of the 5th leg.

Geographic entities mentioned:
surface_form: green lake
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 25.05041944
lon: 102.70227778
Baikalian Research Centre. o1m8ymwk3gijswqdoamzu4eukvr6w" xml:space="preserve">The Baikal Research Centre is an independent research organization focused on scientific and educational environmental studies in Lake Baikal and its area. Centre was established in 2003 as nonprofit research, technology transfer, and educational organization.

Geographic entities mentioned:
surface_form: Lake Baikal
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 53.30277778
lon: 108.00472222
Tangra Yumco. Tangra Yumco (,) is a salt lake in Tibet, China. It is in the southwest of Nyima County. Tangra Yumco is, with a drainage area of, an elevation of, length and mean width (maximum width). It is the holy lake of the

Geographic entities mentioned:
surface_form: tangra yumco
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 31
lon: 86.566666666667
Early life. Aïcha Haddad was born in 1937 in Bordj Bou Arréridj, Algeria. Her life and work were marked by the history of her family, who hailed from the Hachem tribe in Medjana. She was deeply tied to Algeria's Hautes Plaines, where she would spend her childhood and adolescence. Algerian War.

Geographic entities mentioned:
surface_form: Hautes Plaines
instance_of: Plateau
countries: Algeria
coordinates: lat: 34.01861111
lon: 0.08527778
Topography and access. With a height of 225.8 m above sea level (NN), the Meesenkopf is topographically unspectacular for this part of the Wiehen Hills. There are much higher summits in its immediate vicinity, such as the Heidbrink, just under one kilometre away to the south, and the and better-known Reineberg, Lübbecke's local hill, which is 300 metres to the east, west of the Ronceva valley.

Geographic entities mentioned:
surface_form: Heidbrink
instance_of: Mountain
countries: Germany
coordinates: lat: 52.2914
lon: 8.63694
surface_form: Reineberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.294311111111
lon: 8.6284694444444
surface_form: heidbrink
instance_of: Mountain
countries: Germany
coordinates: lat: 52.2914
lon: 8.63694
surface_form: reineberg
instance_of: Mountain
countries: Germany
coordinates: lat: 52.294311111111
lon: 8.6284694444444
Meesenkopf. The Meesenkopf, also called the &quot;Mesenkopf&quot;, is a hill in the Wiehen range, south of the town of Lübbecke in Northern Germany. Whilst not particularly prominent, the hill is historically significant as the site of a medieval castle. Topography and access.

Geographic entities mentioned:
surface_form: meesenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 52.293611111111
lon: 8.6247222222222
Topography and access. With a height of 225.8 m above sea level (NN), the Meesenkopf is topographically unspectacular for this part of the Wiehen Hills. There are much higher summits in its immediate vicinity, such as the Heidbrink, just under one kilometre away to the south, and the and better-known Reineberg, Lübbecke's local hill, which is 300 metres to the east, west of the Ronceva valley.

Geographic entities mentioned:
surface_form: meesenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 52.293611111111
lon: 8.6247222222222
The Meesenburg. A castle, the Meesenburg, was built on the Meesenkopf, probably by Count Otto I of Tecklenburg (1209–1263). This Tecklenburg fort was later conquered and destroyed by the Bishop of Minden, Conrad I of Rüdenberg in a joint military operation with the Bishopric of Osnabrück.

Geographic entities mentioned:
surface_form: meesenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 52.293611111111
lon: 8.6247222222222
This Tecklenburg fort was later conquered and destroyed by the Bishop of Minden, Conrad I of Rüdenberg in a joint military operation with the Bishopric of Osnabrück. The castle on the Meesenkopf is believed to have been subsequently demolished around 1216 at the instigation of Bishop Conrad of Minden. The stone was then used to build St.

Geographic entities mentioned:
surface_form: meesenkopf
instance_of: Mountain
countries: Germany
coordinates: lat: 52.293611111111
lon: 8.6247222222222
1809–1899) played the traditional Norwegian zither-like instrument, the langeleik. A native of Vestre Slidre in the Valdres district, she became known throughout Norway for her exceptionally skilled performances and her accompanying dancing dolls. The composers Edvard Grieg and Ludvig Mathias Lindeman were each inspired by her playing.

Geographic entities mentioned:
surface_form: Valdres
instance_of: Valley
countries: Norway
coordinates: lat: 60.916666666667
lon: 9.1666666666667
Peterskopf (Haardt). The Peterskopf, near the Palatine county town of Bad Dürkheim in the German state of Rhineland-Palatinate, is a 487-metre-high hill in the Haardt mountains. On its summit is the Bismarck tower. Location.

Geographic entities mentioned:
surface_form: peterskopf (haardt)
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
Peterskopf (Haardt). The Peterskopf, near the Palatine county town of Bad Dürkheim in the German state of Rhineland-Palatinate, is a 487-metre-high hill in the Haardt mountains. On its summit is the Bismarck tower. Location.

Geographic entities mentioned:
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
On the southeastern slope of the hill, 700 metres from the summit, are the ruins of the Weilach farmstead, first mentioned in 1381. The River Isenach flows past the Peterskopf to the southwest before entering the town of Bad Dürkheim. Accessibility. A tarmac road runs to the Peterskopf from Leistadt, the distance to the car park by Forsthaus Lindemannsruhe (470 m) being 2.5 km.

Geographic entities mentioned:
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
The River Isenach flows past the Peterskopf to the southwest before entering the town of Bad Dürkheim. Accessibility. A tarmac road runs to the Peterskopf from Leistadt, the distance to the car park by Forsthaus Lindemannsruhe (470 m) being 2.5 km. From there the summit may be reached on foot in about ten minutes. Surrounding area.

Geographic entities mentioned:
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
Surrounding area. In the area around the Peterskopf there is a host of historic sites: the Teufelsstein hill to the southeast with its eponymous rock formation, which was a cult site in Celtic times; and a Celtic circular rampart, the Heidenmauer and the Roman quarry of Kriemhildenstuhl on the &quot;Kästenberg&quot;, a southeastern spur of the Teufelsstein.

Geographic entities mentioned:
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
surface_form: teufelsstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4701
lon: 8.1484
surface_form: teufelsstein
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4701
lon: 8.1484
Summit. On the summit plateau of the Peterskopf the good 30-metre-high Bismarck tower offers a panoramic view of the Upper Rhine Plain, 400 metres below to the east, the Palatine Forest to the west and its eastern ridge, the Haardt, which runs from north to south. There is a restaurant on the lower floor of the tower.

Geographic entities mentioned:
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 49.4793
lon: 8.1299
surface_form: peterskopf
instance_of: Mountain
countries: Germany
coordinates: lat: 51.1612
lon: 9.03253
On the far side of the Isenach valley lie the medieval ruins of Limburg Abbey and the castle of Hardenburg. Summit. On the summit plateau of the Peterskopf the good 30-metre-high Bismarck tower offers a panoramic view of the Upper Rhine Plain, 400 metres below to the east, the Palatine Forest to the west and its eastern ridge, the Haardt, which runs from north to south.

Geographic entities mentioned:
surface_form: limburg
instance_of: Mountain
countries: Germany
coordinates: lat: 48.6042
lon: 9.53639
The park was established in 2003 to preserve undisturbed coastal alpine landscape. The scenery is characterized by peaks jutting out of the ocean and fjords, the highest point is the tall Møysalen mountain. The park mostly lies in Lødingen Municipality, but the far northern part crosses over into Sortland Municipality. The park is largely undisturbed from its natural state.

Geographic entities mentioned:
surface_form: Møysalen
instance_of: Mountain
countries: Norway
coordinates: lat: 68.525833333333
lon: 15.451944444444
Ruatapu is a small town in the Westland District in the West Coast region of the South Island of New Zealand. The town's name stems from Ruatapu, a figure in Māori mythology. The town is located on a narrow strip of land between the Tasman Sea and Lake Mahinapua, a shallow lake that was originally a coastal lagoon. runs through Ruatapu, connecting it to the nearby towns of Hokitika and Ross.

Geographic entities mentioned:
surface_form: Lake Mahinapua
instance_of: Lake
countries: New Zealand
coordinates: lat: -42.793
lon: 170.917
Manga Bell's real problems with the regime began later in 1910. The Germans outlined a plan to relocate the Duala people inland from the Wouri River to allow European-only settlement of the area. The expropriations affected all of the Duala lineages except Bonaberi, so Duala public opinion was strongly against it, and for the first time in their history, the Duala clans presented a united front.

Geographic entities mentioned:
surface_form: Wouri River
instance_of: Watercourse
countries: Cameroon
coordinates: lat: 4.0833
lon: 9.7
Chhechu. Chhechu is a ceremony of the Tamang communities in Nepal that takes place over the course of ten days. It contains sportive plays (tsema), exorcisms, and rituals. Chhechu takes place northwest of Kathmandu Valley of Nepal. There are eleven tsema performed, and three exorcisms. Description. The whole community participates in a variety of ways.

Geographic entities mentioned:
surface_form: Kathmandu Valley
instance_of: Valley
countries: Nepal
coordinates: lat: 27.703944444444
lon: 85.308583333333
Fourteenth Army captured Mandalay on 20 March and prepared to move on Rangoon before the Monsoon broke, but 2nd Division was not included in the planning. Its last operations were against Indian National Army units at Legyi in April, and then clearing the country towards Mount Popa.

Geographic entities mentioned:
surface_form: Mount Popa
instance_of: Mountain
countries: Myanmar
coordinates: lat: 20.920277777778
lon: 95.253888888889
In 1901, the Surveyor-General of Canada, Dr. Edouard Deville, assigned Wheeler the task of surveying the Rogers Pass area of the Selkirk Range in British Columbia. On the train to Rogers Pass, Wheeler met Edward Whymper, who had made the first ascent of the Matterhorn in 1865 and who was in Canada as a guest of the Canadian Pacific Railway.

Geographic entities mentioned:
surface_form: Matterhorn
instance_of: Mountain
countries: Switzerland
Italy
coordinates: lat: 45.97638888888889
lon: 7.658611111111111
He continued to be active in the club and was the driving force behind two of its most successful expeditions: the Mount Robson camp which in 1913 made the first confirmed ascent of the highest mountain in the Canadian Rockies; and the 1925 first ascent of Mount Logan, the highest mountain in Canada. Honors.

Geographic entities mentioned:
surface_form: Mount Robson
instance_of: Mountain
countries: Canada
coordinates: lat: 53.11055555555556
lon: -119.15666666666667
surface_form: Mount Logan
instance_of: Mountain
countries: Canada
coordinates: lat: 60.567222222222
lon: -140.40277777778
Wheeler's father, Edward Oliver Wheeler, was a captain in the Kilkenny Fusiliers. He is the father of Sir Edward Oliver Wheeler, who participated in the first topographical survey of Mount Everest in 1921, and as Brigadier in the British Army was appointed Surveyor General of India in 1941. He is the grandfather of John Oliver Wheeler, an award-winning Canadian geologist.

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 was directed by Benny Boom and filmed from August 19 to 21, 2002. The film set was located on Colonial Street, which was one of the backlot street sets located at Universal Studios Hollywood in the San Fernando Valley area of Los Angeles County, California. Then-Washington Wizards player Larry Hughes appeared in the video as Rowland's boyfriend, while Patti LaBelle was cast as her mother.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
The second stage followed after a time of glacial erosion and is called Deacon Peak Formation, resembling the formation of the same name on Penguin Island. It consists of lavas and agglomerates embedded within red and brown lavas. The vents of this stage are located northeast of these of the Hektor Icefall Formation.

Geographic entities mentioned:
surface_form: brown
instance_of: Mountain
coordinates: lat: -68.3
lon: 86.4167
Composition. The volcano has produced basaltic andesite and basaltic rocks containing augite, olivine and clinopyroxene; the rocks define an alkaline to calc-alkaline suite rich in aluminum. They are aphanitic or vesicular in the older volcano stage. The composition implies that the magma originated from the deep mantle and ascended quickly through the crust, with no storage in a magma chamber.

Geographic entities mentioned:
surface_form: rich
instance_of: Mountain
coordinates: lat: -79.7833
lon: 158.8
It represents an eroded stratovolcano of unknown age and contains a volcanic crater at its summit. A volcanic ash layer similar in composition to Melville Peak has been identified away from the volcano and may indicate Melville Peak has been volcanically active in the last few thousand years.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The vents of this stage are located northeast of these of the Hektor Icefall Formation. The volcano was active in the Quaternary and its last eruptions may have occurred during the middle Holocene. A volcanic ash layer found in a marine core about southeast from Melville Peak may imply that the volcano was active a few thousand years ago.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
The volcano was active in the Quaternary and its last eruptions may have occurred during the middle Holocene. A volcanic ash layer found in a marine core about southeast from Melville Peak may imply that the volcano was active a few thousand years ago. Another 5,500-5,000 years old tephra layer found in lakes on King George Island may originate at Melville Peak or more likely at Penguin Island.

Geographic entities mentioned:
surface_form: active
instance_of: Landform
Body of water
coordinates: lat: -63.4167
lon: -56.1667
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
This peak, which was probably known to early sealers in the area, was charted by the French Antarctic Expedition under Jean-Baptiste Charcot, 1908–10, and takes its name from Cape Melville. It was climbed from the northeast in September 1949 by Geoff Hattersley-Smith and Ken Pawson. Geography and geomorphology.

Geographic entities mentioned:
surface_form: pawson
instance_of: Mountain
coordinates: lat: -73.1667
lon: -61.0167
surface_form: smith
instance_of: Lake
coordinates: lat: -66.1167
lon: 101.283
The mountain rises from the peninsula that leads to Cape Melville. The volcano is about wide, but almost entirely covered by the ice of the Arctowski Icefield and Danowski Glacier. Rock formations consisting of lava flows and pyroclastics crop out at and close to Sherratt Bay to the south; two outcrops form the vents of the volcano.

Geographic entities mentioned:
surface_form: arctowski
instance_of: Mountain
coordinates: lat: -65.1
lon: -60
Potassium-argon dating has yielded ages of 296,000 ± 27,000 and 72,000 ± 15,000 years ago for the first stage, partly contemporary to submarine volcanism in the Bransfield Strait. The second stage followed after a time of glacial erosion and is called Deacon Peak Formation, resembling the formation of the same name on Penguin Island.

Geographic entities mentioned:
surface_form: deacon peak
instance_of: Mountain
coordinates: lat: -62.1
lon: -57.95
surface_form: penguin island
instance_of: Mountain
coordinates: lat: -62.1
lon: -57.92805555555555
Melville Peak. Melville Peak is a prominent peak surmounting Cape Melville, the eastern cape of King George Island, in the South Shetland Islands off Antarctica. It represents an eroded stratovolcano of unknown age and contains a volcanic crater at its summit.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
It was climbed from the northeast in September 1949 by Geoff Hattersley-Smith and Ken Pawson. Geography and geomorphology. Melville Peak lies at the eastern end of King George Island, in the South Shetland Islands of Antarctica. The mountain rises from the peninsula that leads to Cape Melville.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The older vent forms the highest point of Melville Peak with elevation. Lava Crag crops out east of Melville Peak at Destruction Bay on the northeastern side of King George Island, while the Rolnicki Buttresses are located west-southwest of the main Melville Peak.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The volcano was active in the Quaternary and its last eruptions may have occurred during the middle Holocene. A volcanic ash layer found in a marine core about southeast from Melville Peak may imply that the volcano was active a few thousand years ago. Another 5,500-5,000 years old tephra layer found in lakes on King George Island may originate at Melville Peak or more likely at Penguin Island.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
surface_form: penguin island
instance_of: Mountain
coordinates: lat: -62.1
lon: -57.92805555555555
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The crust has a continental character. Melville Peak forms an alignment with Low Head and Penguin Island, volcanoes that have produced olivine basalts during the Cenozoic, sometimes named Penguin Line. This alignment may be a consequence of Bransfield Strait rifting and normal faults linked to the rift, although Melville Peak is off the main rift axis. Composition.

Geographic entities mentioned:
surface_form: penguin island
instance_of: Mountain
coordinates: lat: -62.1
lon: -57.92805555555555
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Melville Peak. Melville Peak is a prominent peak surmounting Cape Melville, the eastern cape of King George Island, in the South Shetland Islands off Antarctica. It represents an eroded stratovolcano of unknown age and contains a volcanic crater at its summit.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The volcano is about wide, but almost entirely covered by the ice of the Arctowski Icefield and Danowski Glacier. Rock formations consisting of lava flows and pyroclastics crop out at and close to Sherratt Bay to the south; two outcrops form the vents of the volcano. The older vent forms the highest point of Melville Peak with elevation.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
Present-day and recent volcanism in the region is linked to the spreading of the Bransfield Rift. The basement under Melville Peak is formed by the Moby Dick Group, which probably formed during the late Cretaceous. The Moby Dick Group was later intruded by andesitic and basaltic dykes, tilted southwestward and faulted.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The Moby Dick Group was later intruded by andesitic and basaltic dykes, tilted southwestward and faulted. The sedimentary Cape Melville Formation and the volcanic Destruction Bay Formation underlie Melville Peak and were emplaced during the Miocene. The crust has a continental character.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833
The crust has a continental character. Melville Peak forms an alignment with Low Head and Penguin Island, volcanoes that have produced olivine basalts during the Cenozoic, sometimes named Penguin Line. This alignment may be a consequence of Bransfield Strait rifting and normal faults linked to the rift, although Melville Peak is off the main rift axis. Composition.

Geographic entities mentioned:
surface_form: melville
instance_of: Mountain
coordinates: lat: -62.0167
lon: -57.6833