Sarmila/GeoWiki-Features huggingface dataset:
After defeating the Saffarids, their &quot;empire&quot;, with nominal sanction from the Abbasids, extended from India to Iraq, making Nishapur a provincial capital. Khurasan was thus an international entrepôt, with merchants coming not only from Iraq, India and Egypt, but also from Russia; additionally, Vikings came from Scandinavia to trade with the Bulghars and Khazars on the Caspian Sea.

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
Modern. Nishapur generally has a warm and semi-dry climate called &quot;central Iranian plateau climate&quot;. Precipitation mostly happens in spring and winter. Nishapur is situated on a relatively higher elevation (1250 meters) than its neighboring cities such Sabzevar and Mashhad hence the weather is milder and better than these cities. Climate. Nishapur has a cold semi-arid climate (BSk).

Geographic entities mentioned:
surface_form: central Iranian plateau
instance_of: Plateau
countries: Iran
coordinates: lat: 36.283333
lon: 59.05
Gastronomy and food culture. The most important foods and drinks in Nishapur are rhubarb and sharbat. Rhubarb (Persian or '), a sour vegetable, grows at the foot of the eponymous Rivand Mountains (Mount Binalud). Soft drinks made from the stems of the plant, such as () and (), are sold at some Nishapur resorts.

Geographic entities mentioned:
surface_form: Mount Binalud
instance_of: Mountain
countries: Iran
coordinates: lat: 36.426388888889
lon: 58.849166666667
Description. Keefe Peak is located west of the Continental Divide in the Elk Mountains which are a subrange of the Rocky Mountains. It ranks as the 238th-highest peak in Colorado. The mountain is situated south-southwest of the community of Aspen and northwest of Castle Peak. The peak is set in the Maroon Bells–Snowmass Wilderness on land managed by White River National Forest.

Geographic entities mentioned:
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.3655
lon: -120.349
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 61.597777777778
lon: -143.44361111111
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.0396
lon: -114.585
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.7731
lon: -106.834
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 46.246388888889
lon: -122.2975
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 48.981944444444
lon: -120.86166666667
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 32.3665
lon: -99.9995
surface_form: castle peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0097
lon: -106.861
The peak is within the territory he served the Forest Service as a deputy forest supervisor. He was born and raised in Blossburg, Pennsylvania, and graduated from Pennsylvania State College in 1913 with a Bachelor of Science degree in forestry. Climate.

Geographic entities mentioned:
surface_form: bachelor
instance_of: Mountain
countries: United States
coordinates: lat: 43.979166666667
lon: -121.68833333333
It ranks as the 238th-highest peak in Colorado. The mountain is situated south-southwest of the community of Aspen and northwest of Castle Peak. The peak is set in the Maroon Bells–Snowmass Wilderness on land managed by White River National Forest. Precipitation runoff from the mountain's slopes drains into tributaries of the Roaring Fork River which is a tributary of the Colorado River.

Geographic entities mentioned:
surface_form: maroon bells
instance_of: Mountain
countries: United States
coordinates: lat: 39.0708
lon: -106.989
Keefe Peak. Keefe Peak is a mountain summit in Pitkin County, Colorado, United States. Description. Keefe Peak is located west of the Continental Divide in the Elk Mountains which are a subrange of the Rocky Mountains. It ranks as the 238th-highest peak in Colorado. The mountain is situated south-southwest of the community of Aspen and northwest of Castle Peak.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: keefe peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0325
lon: -106.90472222222
Keefe Peak. Keefe Peak is a mountain summit in Pitkin County, Colorado, United States. Description. Keefe Peak is located west of the Continental Divide in the Elk Mountains which are a subrange of the Rocky Mountains. It ranks as the 238th-highest peak in Colorado. The mountain is situated south-southwest of the community of Aspen and northwest of Castle Peak.

Geographic entities mentioned:
surface_form: keefe peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0325
lon: -106.90472222222
Etymology. The mountain's toponym was officially adopted as &quot;Keefe Mountain&quot; on May 6, 1925, by the United States Board on Geographic Names and revised to &quot;Keefe Peak&quot; on February 2, 1927. The US Forest Service made the suggestion to commemorate one of their former employees, Lieutenant Thomas Victor Keefe (1888–1918), who died while serving in the US Army.

Geographic entities mentioned:
surface_form: keefe peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0325
lon: -106.90472222222
Climate. According to the Köppen climate classification system, Keefe Peak is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring.

Geographic entities mentioned:
surface_form: keefe peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.0325
lon: -106.90472222222
The peak is set in the Maroon Bells–Snowmass Wilderness on land managed by White River National Forest. Precipitation runoff from the mountain's slopes drains into tributaries of the Roaring Fork River which is a tributary of the Colorado River. Topographic relief is significant as the summit rises above Conundrum Creek in and above East Maroon Creek in. Etymology.

Geographic entities mentioned:
surface_form: roaring fork
instance_of: Watercourse
countries: United States
coordinates: lat: 35.716759
lon: -83.5118304
Chhijmuni. Chhijmuni (Aymara edible part of the clover plant, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the &quot;, Hispanicized spelling &quot;Chicmune&quot;) is a mountain in the Wansu mountain range in the Andes of Peru. It is located in the Arequipa Region, La Unión Province, Puyca District. Chhijmuni lies south of Wayta Urqu.

Geographic entities mentioned:
surface_form: Wayta Urqu
instance_of: Mountain
countries: Peru
coordinates: lat: -14.8508
lon: -72.6367
Chhijmuni. Chhijmuni (Aymara edible part of the clover plant, &quot;-ni&quot; a suffix to indicate ownership, &quot;the one with the &quot;, Hispanicized spelling &quot;Chicmune&quot;) is a mountain in the Wansu mountain range in the Andes of Peru. It is located in the Arequipa Region, La Unión Province, Puyca District. Chhijmuni lies south of Wayta Urqu.

Geographic entities mentioned:
surface_form: chhijmuni
instance_of: Mountain
countries: Peru
coordinates: lat: -14.8617
lon: -72.6378
Telethrio. Telethrio (,) is a small mountain range in the northwestern part of the island of Euboea, Greece. Its maximum elevation is 970 m. It stretches along the west coast of the island, on the North Euboean Gulf, from Aidipsos in the west to Rovies in the east. Its length is about 16 km from east to west. The mountain is forested.

Geographic entities mentioned:
surface_form: telethrio
instance_of: Mountain
countries: Greece
coordinates: lat: 38.865
lon: 23.188
Some of these Israelites, however, managed to migrate to safety in neighbouring Judah, though the Judahites themselves would be conquered by the Neo-Babylonian Empire nearly two centuries later. Those who stayed behind in Samaria following the Assyrian conquest mainly concentrated themselves around Mount Gerizim and eventually came to be known as the Samaritans.

Geographic entities mentioned:
surface_form: Mount Gerizim
instance_of: Mountain
countries: State of Palestine
coordinates: lat: 32.199444444444
lon: 35.272777777778
Archaeological finds, ancient Near Eastern texts, and the biblical record testify that in the time of the Omrides, Israel ruled in the mountainous Galilee, at Hazor in the upper Jordan Valley, in large parts of Transjordan between the Wadi Mujib and the Yarmuk, and in the coastal Sharon plain. In Assyrian inscriptions, the Kingdom of Israel is referred to as the &quot;House of ʻOmri&quot;.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
He won the Otago Central electorate in after the retirement of Jack George, but was defeated by Labour's Ian Quigley in. He was one of four National Party incumbents from Otago and Southland who lost their normally blue electorate to the Labour challenger over the proposed raising of the lake levels of lakes Manapouri and Te Anau, which was opposed by the Save Manapouri campaign.

Geographic entities mentioned:
surface_form: Manapouri
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.514
lon: 167.508
surface_form: Te Anau
instance_of: Lake
countries: New Zealand
coordinates: lat: -45.2
lon: 167.8
Methylobacterium organophilum. &quot;Methylobacterium organophilum&quot; is a facultatively methylotrophic bacteria from the genus of Methylobacterium which was isolated from sediments from the Lake Mendota in Madison in the United States. &quot;Methylobacterium organophilum&quot; can degrade methanol.

Geographic entities mentioned:
surface_form: Lake Mendota
instance_of: Lake
countries: United States
coordinates: lat: 43.106666666667
lon: -89.424722222222
&quot;Ashugh&quot; tradition. The monastery was a traditional pilgrimage site for Armenian &quot;ashughs&quot; (folk musicians). It has been compared to Mount Parnassus in Greece, which was the home of the Muses. The prominent 18th-century &quot;ashugh&quot; Sayat-Nova is recorded to have made a trip to the monastery to seek divine grace. Cultural references.

Geographic entities mentioned:
surface_form: Mount Parnassus
instance_of: Mountain
countries: Greece
coordinates: lat: 38.533
lon: 22.6167
Cape Maclear. Cape Maclear or Chembe is a town in the Mangochi District of Malawi's Southern Region. The town, on the Nankumba Peninsula, is on the southern shore of Lake Malawi and is the busiest resort on Lake Malawi. Cape Maclear is close to the islands of Domwe, Thumbwe and Mumbo Island on Lake Malawi, and is in Lake Malawi National Park. History.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
There is evidence of a post-medieval lime kiln, possibly constructed 1830s in the Outseats area. In the 18th century, the village was connected to Sheffield by the Sheffield to Hathersage Turnpike. Economy. Hathersage is a tourist destination because of the scenery of the Hope and Derwent valleys, its literary connections and easy access by train or road from Sheffield and Manchester.

Geographic entities mentioned:
surface_form: Hope
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.34727
lon: -1.7455
Moccasin Dam is a small dam on Moccasin Creek in Tuolumne County, California, in the town of Moccasin, west of Yosemite. It holds the Moccasin Reservoir. The dam, reservoir and associated hydroelectric power plant are part of the Hetch Hetchy Project, which provide water and power to the city of San Francisco. The dam is located near the junction of Highway 120 and Highway 49. History.

Geographic entities mentioned:
surface_form: Hetch Hetchy Project
instance_of: Valley
countries: United States
coordinates: lat: 37.9475
lon: -119.78694444
The general store was built in 1882 and featured in the 1991 film &quot;Thelma & Louise&quot;. Geography. Bedrock is located in the southwest margin of Paradox Valley. The Dolores River enters the Paradox Valley approximately one quarter of a mile southeast of the community. Naturita lies 20 miles to the east along Colorado State Highway 90.

Geographic entities mentioned:
surface_form: Paradox Valley
instance_of: Landform
countries: United States
coordinates: lat: 38.3167
lon: -108.85
They came from Boltavara (present-day India), settling and ruling Bicol and its people. The epic is set in the land of Aslon and Ibalong. The mountains Asog, Masaraga, Isarog, and Lingyon were prominent features of the area. In its oldest known text, the folk epic does not have a title. Its oldest existing account is written in Spanish.

Geographic entities mentioned:
surface_form: Asog
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.456666666667
lon: 123.45666666667
surface_form: Isarog
instance_of: Mountain
countries: Philippines
coordinates: lat: 13.659166666667
lon: 123.37333333333
Three volcanoes, named &quot;Hantik&quot;, &quot;Kulasi&quot;, and &quot;Isarog&quot; erupted simultaneously. Inundations caused lands to sink, from which Lake Buhi came about, or rise, as in the strip of seacoast in Pasacao, Camarines Sur, and wiped out many settlements, especially the Dagatnong settlement in the Kalabangan Gulf.

Geographic entities mentioned:
surface_form: Lake Buhi
instance_of: Lake
countries: Philippines
coordinates: lat: 13.45
lon: 123.51666666667
The Malbogong Islet formed in the Bicol River while the Inarihan River altered its course. A lofty mountain sank at Bato, forming a lake. Despite the calamities, Ibálong grew powerful under the elder Handyong, whose constant companion and good friend, by then, was the young Bantong.

Geographic entities mentioned:
surface_form: lake
instance_of: Lake
countries: Philippines
coordinates: lat: 13.333333333333
lon: 123.36666666667
Some of these oral accounts indicated such a transformation. In Sorsogon, the legend of San Bernardino embodied this turn of events against the land and its inhabitants. The legend spoke about a mighty spirit who dwelt in Mt. Bulusan and fell in love with a maiden there. This maiden did not love him back, and so the spirit was enraged.

Geographic entities mentioned:
surface_form: Mt. Bulusan
instance_of: Mountain
countries: Philippines
coordinates: lat: 12.77
lon: 124.05
Panic filled everyone except one man - the favored suitor of the maiden. He killed the spirit to stop its violence in the area. Once killed, the spirit fell into the sea. The part of the water in which the spirit fell transformed into land. The old folks claim that the two islands with a slender strip of water between Samar and Sorsogon were the spirit of Mt. Bulusan.

Geographic entities mentioned:
surface_form: Mt. Bulusan
instance_of: Mountain
countries: Philippines
coordinates: lat: 12.77
lon: 124.05
Ara Rock. Ara Rock is a rock found in Ara Town in Nasarawa Local Government Area of Nasarawa State in central Nigeria. It achieves a remarkable height of about above the surface of the neighbouring plains and it attracts many people to Ara town on sightseeing visits. Location.

Geographic entities mentioned:
surface_form: ara rock
instance_of: Mountain
countries: Nigeria
coordinates: lat: 8.58333333
lon: 7.58333333
On 28 June 1879, a royal resolution changed the name of the municipality to &quot;Fyresdal&quot;. This name () was chosen since it is the name of the valley in which the municipality is located. The first element of this name is the genitive case of the name of the local lake Fyresvatnet (). The name of the lake is derived from the word which means &quot;pine tree&quot;.

Geographic entities mentioned:
surface_form: Fyresvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.11709
lon: 8.12191
Geography. The municipality of Fyresdal consists of several little villages north of Moland, in the main valley of Fyresdal, and on the western and southeastern shores of Fyresvatnet, one of Norway's deepest lakes. Moland is the location of the municipal council, the school, the community house, kindergartens, the home for the elderly, and most of the commercial enterprises in the municipality.

Geographic entities mentioned:
surface_form: Fyresvatnet
instance_of: Lake
countries: Norway
coordinates: lat: 59.11709
lon: 8.12191
Geography. Mam Tor is on the southern edge of the Dark Peak (sandstones) and overlooks the White Peak (limestones), including the dry gorge of Winnats Pass. It is a dominating link between the eastern end of Rushup Edge and the western end of the Great Ridge, which together separate the Hope Valley to the south from Edale to the north, and is a popular ridgewalk.

Geographic entities mentioned:
surface_form: Dark Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.4
lon: -1.8
surface_form: White Peak
instance_of: Plateau
countries: United Kingdom
coordinates: lat: 53.2
lon: -1.8
Geography. Mam Tor is on the southern edge of the Dark Peak (sandstones) and overlooks the White Peak (limestones), including the dry gorge of Winnats Pass. It is a dominating link between the eastern end of Rushup Edge and the western end of the Great Ridge, which together separate the Hope Valley to the south from Edale to the north, and is a popular ridgewalk.

Geographic entities mentioned:
surface_form: Hope Valley
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.34727
lon: -1.7455
This rotational landslide began roughly 4,000 years ago. The toe is a debris flow. The landslide is due to weak shales underlying sandstones, a common phenomenon all around the Dark Peak, notably at Alport Castles, Longdendale, Glossop and Canyards Hills, Sheffield.

Geographic entities mentioned:
surface_form: Longdendale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 53.471666666666664
lon: -1.9505555555555554
Ngayokaung. Ngayokaung (, also spelt Ngayoutkaung or Ngayokekaung) is a town in southwestern Ayeyarwady Region within the Ngayokaung Subtownship, Ngapudaw Township, Pathein District, Myanmar. It is a coastal town on the Bay of Bengal near Goyingyi Island. The Ngayokaung Road connects the Mawtin-Pathein road to the town across the southern end of the Arakan Mountains.

Geographic entities mentioned:
surface_form: Bay of Bengal
instance_of: Body of water
countries: India
Bangladesh
Sri Lanka
Myanmar
coordinates: lat: 15
lon: 88
Sguman Coinntich. Sguman Coinntich (879 m) is a mountain in the Northwest Highlands, Scotland, east of the village of Dornie in Ross-shire. Sguman Coinntich is the highest of twin peaks, its subsidiary top Ben Killilan rising to 756 m. The mountain rises above the head of Loch Long. The climb is mainly along rough terrain, but its summit makes for a fantastic viewpoint.

Geographic entities mentioned:
surface_form: sguman coinntich
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 57.318261
lon: -5.3612309
In its east lies Bargis from where a valley leads to its north face, while to its western face the sliding surface tears off of the biggest visible landslide in the world, Flims Rockslide. Piz Dolf is lying to the north across the Bargis valley, and to its west Piz Segnas, both showing the tectonic line of the &quot;Glarus thrust&quot; in its upper part, a now UNESCO world heritage.

Geographic entities mentioned:
surface_form: Piz Dolf
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.9028
lon: 9.26667
surface_form: Glarus thrust
instance_of: Landform
countries: Switzerland
coordinates: lat: 46.91667
lon: 9.25
surface_form: glarus thrust
instance_of: Landform
countries: Switzerland
coordinates: lat: 46.91667
lon: 9.25
surface_form: piz segnas
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.907916666667
lon: 9.2395833333333
Fil de Cassons. Fil de Cassons (also known as &quot;Cassonsgrat&quot;) is a mountain in the Glarus Alps, located near Flims in the canton of Graubünden, Switzerland. The southern face is referred to as &quot;Flimserstein&quot;, dominating the appearance of the town of Flims.

Geographic entities mentioned:
surface_form: cassonsgrat
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
surface_form: fil de cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
Fil de Cassons. Fil de Cassons (also known as &quot;Cassonsgrat&quot;) is a mountain in the Glarus Alps, located near Flims in the canton of Graubünden, Switzerland. The southern face is referred to as &quot;Flimserstein&quot;, dominating the appearance of the town of Flims.

Geographic entities mentioned:
surface_form: fil de cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
One hiking route uses the ascent via Val Bargis and &quot;Scala Mola&quot;, the path that the cows are being sent up to graze in summer. If you stay at the base of the valley of Bargis, you will hike on a path leading more or less around Fil de Cassons from east to northwest before reaching its top.

Geographic entities mentioned:
surface_form: fil de cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
If you stay at the base of the valley of Bargis, you will hike on a path leading more or less around Fil de Cassons from east to northwest before reaching its top. Being a ridge, there is very often hardly snow, allowing walks even in winter along at least one mile on Fil de Cassons.

Geographic entities mentioned:
surface_form: fil de cassons
instance_of: Mountain
countries: Switzerland
coordinates: lat: 46.878472222222
lon: 9.2801388888889
Mount Touring Club. Mount Touring Club () is a small snow-capped peak near the extremity of a spur that descends southwestward from Mount Peary, on the west side of Graham Land. Discovered and named &quot;Sommet du Touring Club&quot; by the French Antarctic Expedition (1908–10) under Dr. Jean-Baptiste Charcot.

Geographic entities mentioned:
surface_form: Mount Peary
instance_of: Mountain
coordinates: lat: -65.25
lon: -63.8667
surface_form: small
instance_of: Mountain
coordinates: lat: -70.5
lon: 64.7
surface_form: touring club
instance_of: Mountain
coordinates: lat: -65.28333333
lon: -63.93333333
surface_form: mount touring club
instance_of: Mountain
coordinates: lat: -65.28333333
lon: -63.93333333
surface_form: peary
instance_of: Mountain
coordinates: lat: -65.25
lon: -63.8667
Discovered and named &quot;Sommet du Touring Club&quot; by the French Antarctic Expedition (1908–10) under Dr. Jean-Baptiste Charcot. A party from the expedition hiked along the southern side of this feature in the course of charting the area.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Mount Touring Club. Mount Touring Club () is a small snow-capped peak near the extremity of a spur that descends southwestward from Mount Peary, on the west side of Graham Land. Discovered and named &quot;Sommet du Touring Club&quot; by the French Antarctic Expedition (1908–10) under Dr. Jean-Baptiste Charcot.

Geographic entities mentioned:
surface_form: touring club
instance_of: Mountain
coordinates: lat: -65.28333333
lon: -63.93333333
surface_form: mount touring club
instance_of: Mountain
coordinates: lat: -65.28333333
lon: -63.93333333
Mount Touring Club. Mount Touring Club () is a small snow-capped peak near the extremity of a spur that descends southwestward from Mount Peary, on the west side of Graham Land. Discovered and named &quot;Sommet du Touring Club&quot; by the French Antarctic Expedition (1908–10) under Dr. Jean-Baptiste Charcot.

Geographic entities mentioned:
surface_form: touring club
instance_of: Mountain
coordinates: lat: -65.28333333
lon: -63.93333333
He dealt in real estate, supporting his family and growing his business connections. He became a real estate agent for the Central Pacific Railroad company which, at the time, was expanding into the San Joaquin Valley. Central Pacific's simple wood frame depot, then called Fresno station, anchored what became the city of Fresno.

Geographic entities mentioned:
surface_form: San Joaquin Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.628888888889
lon: -120.185
Resolute Mountain. Resolute Mountain is located in David Thompson Country, western Alberta, Canada, 12 km north of Saskatchewan River Crossing. Its line parent is Mount Cline located 2 kilometres to the east. Resolute has two main peaks, Lion and Lioness. They are each about 3150 m high. Both peaks are glaciated on their northern slopes. Resolute was first ascended in 1958 by A. Hober and E.

Geographic entities mentioned:
surface_form: Mount Cline
instance_of: Mountain
countries: Canada
coordinates: lat: 52.07
lon: -116.68222222222222
Resolute Mountain. Resolute Mountain is located in David Thompson Country, western Alberta, Canada, 12 km north of Saskatchewan River Crossing. Its line parent is Mount Cline located 2 kilometres to the east. Resolute has two main peaks, Lion and Lioness. They are each about 3150 m high. Both peaks are glaciated on their northern slopes. Resolute was first ascended in 1958 by A. Hober and E.

Geographic entities mentioned:
surface_form: resolute mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 52.07333333
lon: -116.65944444
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
11 of Dhanbad Municipal Corporation. Overview. The region shown in the map is a part of the undulating uplands bustling with coalmines in the lowest rung of the Chota Nagpur Plateau. The entire area shown in the map is under Dhanbad Municipal Corporation, except Belgaria which is under Baliapur (community development block). The places in the DMC area are marked as neighbourhoods.

Geographic entities mentioned:
surface_form: Chota Nagpur Plateau
instance_of: Plateau
countries: India
coordinates: lat: 23
lon: 85
He soon retired, married a woman from the Javanshir clan of Karabakh and had a son by the name of Ali (nicknamed &quot;Sarija Ali&quot;). They lived in their estate located in Arasbar (Arasbaran) but also owned land in Tartar and the northern shores of the Aras River.

Geographic entities mentioned:
surface_form: Arasbaran
instance_of: Mountain
countries: Iran
coordinates: lat: 38.74
lon: 46.7
He was natural of Ndjiakom-Esambira, on the district of Bata (in the current Litoral Province), he worked as a farmer in the northern banks of the Campo River as did many of the Fang people settled in the far north of the Continental Region of Equatorial Guinea at the districts of Bata, Niefang, Mikomeseng and Ebibeyín respectively.

Geographic entities mentioned:
surface_form: Campo River
instance_of: Watercourse
countries: Equatorial Guinea
Gabon
Cameroon
coordinates: lat: 2.35
lon: 9.8166666666667
Permits are required for non-resident boating and fishing. Bradley Mountain is also traversed by the Metacomet Trail, (maintained by the Connecticut Forest and Park Association), which extends from the Hanging Hills of Meriden, Connecticut, to the Massachusetts border. The Metacomet Trail also passes by Shuttle Meadow Reservoir, managed by the New Britain water department.

Geographic entities mentioned:
surface_form: Hanging Hills
instance_of: Mountain
countries: United States
coordinates: lat: 41.56
lon: -72.82
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Bradley Mountain is traversed by the Metacomet Trail. Geography. Roughly in diameter, Bradley Mountain rises steeply above the Quinnipiac River valley to the west. The mountain consists of an upper ridgeline with several summits and a lower high bluff-line. The Metacomet Ridge continues north from Bradley Mountain as the ridgeline of Pinnacle Rock and south as Ragged Mountain.

Geographic entities mentioned:
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6175
lon: -72.8228
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.020277777778
lon: -110.75944444444
surface_form: pinnacle rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.6897
lon: -72.8328
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4681
lon: -71.8294
The Metacomet Ridge continues north from Bradley Mountain as the ridgeline of Pinnacle Rock and south as Ragged Mountain. Plainville Reservoir (also called Crescent Lake) occupies a bowl-shaped valley on the western side of the mountain, and Shuttle Meadow Reservoir stands between Bradley Mountain and Ragged Mountain to the south. The lower bluff-line is occupied by suburban development.

Geographic entities mentioned:
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6175
lon: -72.8228
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 60.4483
lon: -149.519
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 47.825
lon: -90.7603
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.020277777778
lon: -110.75944444444
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 41.9779331
lon: -111.6280034
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.97424
lon: -70.45679
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 33.9089
lon: -109.419
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 43.4756
lon: -121.992
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 42.6419784
lon: -83.3908107
surface_form: crescent lake
instance_of: Lake
countries: United States
coordinates: lat: 29.4635
lon: -81.5007
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4681
lon: -71.8294
The Metacomet Trail also passes by Shuttle Meadow Reservoir, managed by the New Britain water department. Bradley Mountain offers a number of clifftop views west over Plainville Reservoir and south toward Ragged Mountain. The ecosystem of Bradley Mountain is most threatened by quarrying.

Geographic entities mentioned:
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6175
lon: -72.8228
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 38.020277777778
lon: -110.75944444444
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
surface_form: ragged mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.4681
lon: -71.8294
A diameter traprock quarry, owned by Tilcon, has obliterated the northeast side of Bradley Mountain below the summit. The Quinnipiac River, not much more than a brook this far north, passes west through the gap between Bradley Mountain and Pinnacle Rock, forming the north and west and drainage of the mountain, before flowing into Long Island Sound.

Geographic entities mentioned:
surface_form: pinnacle rock
instance_of: Mountain
countries: United States
coordinates: lat: 41.6897
lon: -72.8328
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Bradley Mountain. Bradley Mountain, is a traprock mountain located west of New Britain, Connecticut, United States, in the towns of Southington and Plainville. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Bradley Mountain, popular as an outdoor recreation destination in the metropolitan Hartford/ New Britain area, is known for its clifftop scenic vistas overlooking Plainville Reservoir, unique microclimate ecosystems, and rare plant communities. Bradley Mountain is traversed by the Metacomet Trail. Geography.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Bradley Mountain is traversed by the Metacomet Trail. Geography. Roughly in diameter, Bradley Mountain rises steeply above the Quinnipiac River valley to the west. The mountain consists of an upper ridgeline with several summits and a lower high bluff-line. The Metacomet Ridge continues north from Bradley Mountain as the ridgeline of Pinnacle Rock and south as Ragged Mountain.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
Plainville Reservoir (also called Crescent Lake) occupies a bowl-shaped valley on the western side of the mountain, and Shuttle Meadow Reservoir stands between Bradley Mountain and Ragged Mountain to the south. The lower bluff-line is occupied by suburban development. A diameter traprock quarry, owned by Tilcon, has obliterated the northeast side of Bradley Mountain below the summit.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Geology and ecology. Bradley Mountain, like much of the Metacomet Ridge, is composed of basalt, also called traprock, a volcanic rock. The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
The mountain formed near the end of the Triassic Period with the rifting apart of the North American continent from Africa and Eurasia. Lava welled up from the rift and solidified into sheets of strata hundreds of feet thick. Subsequent faulting and earthquake activity tilted the strata, creating the cliffs and ridgeline of Bradley Mountain.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Hot, dry upper slopes, cool, moist ravines, and mineral-rich ledges of basalt talus produce a combination of microclimate ecosystems on the mountain that support plant and animal species uncommon in greater Connecticut. Bradley Mountain is an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Bradley Mountain). Recreation and conservation.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Bradley Mountain is an important raptor migration path. (See Metacomet Ridge for more information on the geology and ecosystem of Bradley Mountain). Recreation and conservation. Despite the development on its lower slopes and the quarry on the mountain's northeast side, Bradley Mountain is a large area of protected public land.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
The Metacomet Trail also passes by Shuttle Meadow Reservoir, managed by the New Britain water department. Bradley Mountain offers a number of clifftop views west over Plainville Reservoir and south toward Ragged Mountain. The ecosystem of Bradley Mountain is most threatened by quarrying.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
In 2000, Bradley Mountain was included in a study by the National Park Service for the designation of a new National Scenic Trail now called the New England National Scenic Trail, which includes the Metacomet-Monadnock Trail in Massachusetts as well as the Mattabesett Trail, Metacomet Trail and Menunkatuck Trail trails in Connecticut.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
The Berlin Land Trust is active in the conservation of Bradley Mountain and its viewshed.

Geographic entities mentioned:
surface_form: bradley mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.6575
lon: -72.837777777778
Bradley Mountain. Bradley Mountain, is a traprock mountain located west of New Britain, Connecticut, United States, in the towns of Southington and Plainville. It is part of the narrow, linear Metacomet Ridge that extends from Long Island Sound near New Haven, Connecticut, north through the Connecticut River Valley of Massachusetts to the Vermont border.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
The Quinnipiac River, not much more than a brook this far north, passes west through the gap between Bradley Mountain and Pinnacle Rock, forming the north and west and drainage of the mountain, before flowing into Long Island Sound. The east and south sides of the mountain drain into the Mattabesett River, then to the Connecticut River, thence to Long Island Sound. Geology and ecology.

Geographic entities mentioned:
surface_form: long island
instance_of: Landform
countries: United States
coordinates: lat: 46.7269
lon: -90.785
Virginia Water (lake). Virginia Water lies on the southern edge of Windsor Great Park, in the borough of Runnymede in Surrey and the civil parishes of Old Windsor and Sunningdale in Berkshire, in England. It is a man-made lake taking its name from a natural body of water of the same name. There is a village of Virginia Water which stretches out to the east of the lake.

Geographic entities mentioned:
surface_form: virginia water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.411111111111
lon: -0.60277777777778
It is a man-made lake taking its name from a natural body of water of the same name. There is a village of Virginia Water which stretches out to the east of the lake. The grounds of the lake, nearby Fort Belvedere, and the Clockcase are all Grade I listed on the Register of Historic Parks and Gardens. History.

Geographic entities mentioned:
surface_form: virginia water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.411111111111
lon: -0.60277777777778
History. Virginia Water Lake was originally little more than a stream, which existed from at least the 17th century and may well be named after Elizabeth I, the Virgin Queen, although this is not certain. The lake itself was begun in 1746 by William, Duke of Cumberland who was then Ranger of the Park. His own regiment, the 23rd Regiment of Foot, undertook the construction.

Geographic entities mentioned:
surface_form: virginia water lake
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.411111111111
lon: -0.60277777777778
Among the lakeside features are the high Canadian totem pole, carved by Mungo Martin, Henry Hunt, and Tony Hunt Sr., commemorating the centenary of British Columbia, and a collection of ornamental Roman ruins, transported from the site of Leptis Magna (modern-day Al-Khums) in 1816 and installed at Virginia Water in 1826.

Geographic entities mentioned:
surface_form: virginia water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.411111111111
lon: -0.60277777777778
In 2022, the Libyan government questioned the legality of the ruin's acquisition and asked for them to be returned. In 1834, a miniature sailing frigate, the &quot;Royal Adelaide&quot;, was constructed at Sheerness for King William IV, was dismantled and transported overland to Virginia Water where it was reassembled and launched for sail training of the royal princes.

Geographic entities mentioned:
surface_form: virginia water
instance_of: Lake
countries: United Kingdom
coordinates: lat: 51.411111111111
lon: -0.60277777777778
It is being rebuilt as an elevated station on a viaduct over Van Nuys Boulevard and Vesper Avenue, north-south roads that run perpendicular to the station. Once completed it will continue serving the Van Nuys neighborhood of Los Angeles in the San Fernando Valley. The project is expected to be completed in December 2027.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
A detour routes cyclists onto nearby neighborhood streets. History. The corridor on which Van Nuys station sits was a rail line, the Burbank Line, built through the San Fernando Valley by Southern Pacific in 1893. When the Montalvo Cutoff was constructed in 1904, most traffic was diverted over a new mainline which ran diagonally across the valley and the tracks were relegated to branch status.

Geographic entities mentioned:
surface_form: San Fernando Valley
instance_of: Valley
countries: United States
coordinates: lat: 34.155833333333334
lon: -118.28777777777778
Saint Nicholas Peak (Canada). Saint Nicholas Peak is a mountain summit in the Rocky Mountains of Canada. It is located on the Continental Divide, on the Alberta-British Columbia border, in both Banff National Park and Yoho National Park. It lies at the eastern edge of the Wapta Icefield, and is part of the Waputik Mountains which are a sub-range of the Canadian Rockies. Name.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
Saint Nicholas Peak (Canada). Saint Nicholas Peak is a mountain summit in the Rocky Mountains of Canada. It is located on the Continental Divide, on the Alberta-British Columbia border, in both Banff National Park and Yoho National Park. It lies at the eastern edge of the Wapta Icefield, and is part of the Waputik Mountains which are a sub-range of the Canadian Rockies. Name.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
surface_form: saint nicholas peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.62777777777778
lon: -116.5025
It lies at the eastern edge of the Wapta Icefield, and is part of the Waputik Mountains which are a sub-range of the Canadian Rockies. Name. It was named in 1916 by Arthur O. Wheeler; a particular gendarme on the mountain is said to resemble Santa Claus. Geology. The peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Saint Nicholas Peak (Canada). Saint Nicholas Peak is a mountain summit in the Rocky Mountains of Canada. It is located on the Continental Divide, on the Alberta-British Columbia border, in both Banff National Park and Yoho National Park. It lies at the eastern edge of the Wapta Icefield, and is part of the Waputik Mountains which are a sub-range of the Canadian Rockies. Name.

Geographic entities mentioned:
surface_form: saint nicholas peak
instance_of: Mountain
countries: Canada
coordinates: lat: 51.62777777777778
lon: -116.5025
Patton Glacier. Patton Glacier () is a broad tributary glacier in the Sentinel Range, Ellsworth Mountains. It drains the east slope of the main ridge between Mounts Ostenso and Tyree, flows east-northeastwards between Evans Peak and Versinikia Peak on the north and Mount Bearskin on the south, and enters Ellen Glacier northeast of Zalmoxis Peak and southeast of Mount Jumper.

Geographic entities mentioned:
surface_form: Ostenso
instance_of: Mountain
coordinates: lat: -78.31972222222223
lon: -86.1225
surface_form: Tyree
instance_of: Mountain
coordinates: lat: -78.411666666667
lon: -85.861944444444
surface_form: Evans Peak
instance_of: Mountain
coordinates: lat: -78.2833
lon: -85.9667
surface_form: Mount Bearskin
instance_of: Mountain
coordinates: lat: -78.3333
lon: -85.6167
surface_form: Zalmoxis Peak
instance_of: Mountain
coordinates: lat: -78.3383
lon: -85.5167
surface_form: Mount Jumper
instance_of: Mountain
coordinates: lat: -78.2333
lon: -85.6
Visdalen. Visdalen is a valley in Lom Municipality in Innlandet county, Norway. The long valley lies on the southeast side of the Bøverdalen valley. The valley begins at the mountain Kyrkja in the Jotunheimen mountains, just south of the mountain Galdhøpiggen, the tallest mountain in Norway. It then follows the river Visa to the north.

Geographic entities mentioned:
surface_form: Kyrkja
instance_of: Mountain
countries: Norway
coordinates: lat: 61.542777777778
lon: 8.29
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
The inner part of the valley is located inside Jotunheimen National Park. The valley is notable because it runs in between two of Norway's tallest mountains: Galdhøpiggen and Glittertinden. There is a road that runs about two-thirds of the length of the valley, stopping at the Spiterstulen hotel, one of the largest such facilities in the Jotunheimen mountains.

Geographic entities mentioned:
surface_form: Galdhøpiggen
instance_of: Mountain
countries: Norway
coordinates: lat: 61.633333333333
lon: 8.3
surface_form: glittertinden
instance_of: Mountain
countries: Norway
coordinates: lat: 61.651944444444
lon: 8.5544444444444
Visdalen. Visdalen is a valley in Lom Municipality in Innlandet county, Norway. The long valley lies on the southeast side of the Bøverdalen valley. The valley begins at the mountain Kyrkja in the Jotunheimen mountains, just south of the mountain Galdhøpiggen, the tallest mountain in Norway. It then follows the river Visa to the north.

Geographic entities mentioned:
surface_form: bøverdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.75
lon: 8.4166666666667
The valley begins at the mountain Kyrkja in the Jotunheimen mountains, just south of the mountain Galdhøpiggen, the tallest mountain in Norway. It then follows the river Visa to the north. At the end of the valley, the river joins the river Bøvra and the valley becomes part of the Bøverdalen valley. The inner part of the valley is located inside Jotunheimen National Park.

Geographic entities mentioned:
surface_form: bøverdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.75
lon: 8.4166666666667
Visdalen. Visdalen is a valley in Lom Municipality in Innlandet county, Norway. The long valley lies on the southeast side of the Bøverdalen valley. The valley begins at the mountain Kyrkja in the Jotunheimen mountains, just south of the mountain Galdhøpiggen, the tallest mountain in Norway. It then follows the river Visa to the north.

Geographic entities mentioned:
surface_form: visdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.6726
lon: 8.4461
Then, the moment the Turks entered the fort, the local Antonios Vratsanos lit a fuse to the gunpowder stock, in an explosion that killed the town's inhabitants along with their enemies &mdash; thus remaining faithful to their flag up to their death. A French officer who heard and saw the explosion compared it to a volcanic eruption of Mount Vesuvius.

Geographic entities mentioned:
surface_form: Mount Vesuvius
instance_of: Mountain
countries: Italy
coordinates: lat: 40.821388888889
lon: 14.425555555556