page_id int64 303 80.8M | page_url stringlengths 31 161 | sentence dict | context stringlengths 8 4.69k | annotations listlengths 1 69 |
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5,119,355 | http://en.wikipedia.org/wiki/Ancient_Bohemian_Legends | {
"id": 10,
"offset_start": 1001,
"offset_end": 1065,
"text": "Forefather Čech climbed Říp Mountain and looked around the land."
} | They were led by Forefather Čech and his brother, Lech. After a long time (perhaps years) of traveling, they arrived to busky land. Forefather Čech climbed Říp Mountain and looked around the land. Then he allegedly said: "Oh, comrades, you've endured hardships along with me, when we wandered in impassable woods; finally we arrived at our homeland. | [
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"surface_form": "Říp",
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"Mountain"
],
"countries": [
"Czech Republic"
],
"coordinates": {
"lat": 50.38653,
"lon": 14.2896344
}
}
] |
63,148,370 | http://en.wikipedia.org/wiki/Crepinella_acaropunctata | {
"id": 2,
"offset_start": 110,
"offset_end": 243,
"text": "It is endemic to the tepuis Cerro Duida and Cerro Marahuaca in Duida–Marahuaca National Park of Amazonas state of southern Venezuela."
} | Crepinella acaropunctata. "Crepinella acaropunctata" is a flowering plant in the family Araliaceae. It is endemic to the tepuis Cerro Duida and Cerro Marahuaca in Duida–Marahuaca National Park of Amazonas state of southern Venezuela. It grows in montane forest from 1,600 to 2,700 meters elevation. | [
{
"qid": "Q5064905",
"surface_form": "Cerro Duida",
"mention_offset": 138,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Venezuela"
],
"coordinates": {
"lat": 3.51333333,
"lon": -65.62611111
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 1,
"offset_start": 18,
"offset_end": 163,
"text": "The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada."
} | Champlain Valley. The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). | [
{
"qid": "Q68467",
"surface_form": "Lake Champlain",
"mention_offset": 79,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"United States",
"Canada"
],
"coordinates": {
"lat": 44.53,
"lon": -73.33
}
},
{
"qid": "Q3554098"... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 12,
"offset_start": 1523,
"offset_end": 1658,
"text": "The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama."
} | Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division. | [
{
"qid": "Q3816357",
"surface_form": "Great Appalachian Valley",
"mention_offset": 1601,
"link_type": "direct",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 39.5,
"lon": -77.83333333333333
}
},
{
"qid":... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 0,
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"text": "Champlain Valley."
} | Champlain Valley. The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 3,
"offset_start": 328,
"offset_end": 410,
"text": "The Richelieu valley is not generally referred to as part of the Champlain Valley."
} | Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 393,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 6,
"offset_start": 734,
"offset_end": 922,
"text": "Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont."
} | The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley. Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 854,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
},
{
"qid": "Q816843",
... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 7,
"offset_start": 923,
"offset_end": 1033,
"text": "The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County."
} | Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont. The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 951,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 10,
"offset_start": 1378,
"offset_end": 1496,
"text": "The northern part of Lake George is located at, and near Ticonderoga, and therefore is a part of the Champlain Valley."
} | The city of Plattsburgh is to the north, and the historic town of Ticonderoga is in the southern part of the region. The northern part of Lake George is located at, and near Ticonderoga, and therefore is a part of the Champlain Valley. Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 1479,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
},
{
"qid": "Q1495651",
... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 13,
"offset_start": 1659,
"offset_end": 1824,
"text": "The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division."
} | Geology and physiography. The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley reaching from Canada to Alabama. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 1663,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 14,
"offset_start": 1825,
"offset_end": 1967,
"text": "In Vermont, the Champlain Valley is equivalent to the Vermont Lowlands physiographic region, and extends southward into the Valley of Vermont."
} | The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley province, which in turn is part of the larger Appalachian physiographic division. In Vermont, the Champlain Valley is equivalent to the Vermont Lowlands physiographic region, and extends southward into the Valley of Vermont. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 1841,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
},
{
"qid": "Q816843",
... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 16,
"offset_start": 2135,
"offset_end": 2383,
"text": "Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, drained northward by the Richelieu River into the St. Lawrence River at Sorel-Tracy, Quebec (northeast of Montreal)."
} | The Vermont Lowlands are primarily underlain by sedimentary rocks, especially limestone and shale, though metamorphic rocks such as marble and slate are also present. Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, drained northward by the Richelieu River into the St. | [
{
"qid": "Q3554098",
"surface_form": "champlain valley",
"mention_offset": 2169,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.45868,
"lon": -73.42617
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 18,
"offset_start": 2566,
"offset_end": 2640,
"text": "Lake Champlain also receives water from Lake George via the La Chute River"
} | Lawrence River at Sorel-Tracy, Quebec (northeast of Montreal). Major tributaries of Lake Champlain include Otter Creek and the Winooski, Missisquoi, and Lamoille rivers in Vermont, and the Ausable, Chazy, Boquet, and Saranac rivers in New York. Lake Champlain also receives water from Lake George via the La Chute River | [
{
"qid": "Q1495651",
"surface_form": "lake george",
"mention_offset": 2606,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 43.622222222222,
"lon": -73.546666666667
}
},
{
"qid": "Q20707... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 5,
"offset_start": 572,
"offset_end": 733,
"text": "The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley."
} | The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley. | [
{
"qid": "Q816843",
"surface_form": "the valley",
"mention_offset": 722,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 34.155833333333334,
"lon": -118.28777777777778
}
},
{
"qid": "Q... |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 8,
"offset_start": 1034,
"offset_end": 1260,
"text": "Most of this area is part of the Adirondack Park, offering tremendous views of the Adirondack High Peaks region and many recreational opportunities in the park and along the relatively undeveloped coast line of Lake Champlain."
} | The New York portion of the Champlain Valley includes the eastern portions of Clinton County and Essex County. Most of this area is part of the Adirondack Park, offering tremendous views of the Adirondack High Peaks region and many recreational opportunities in the park and along the relatively undeveloped coast line of Lake Champlain. | [
{
"qid": "Q5756075",
"surface_form": "high peaks",
"mention_offset": 1128,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 45,
"lon": -70.4
}
}
] |
967,263 | http://en.wikipedia.org/wiki/Champlain_Valley | {
"id": 4,
"offset_start": 411,
"offset_end": 571,
"text": "The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains."
} | Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. | [
{
"qid": "Q6478226",
"surface_form": "lake valley",
"mention_offset": 425,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 38.3189,
"lon": -114.607
}
}
] |
1,305,223 | http://en.wikipedia.org/wiki/Geeta_Zutshi | {
"id": 6,
"offset_start": 522,
"offset_end": 641,
"text": "She has inspired other Indian women, such as Bachendri Pal, the first Indian woman to successfully climb Mount Everest."
} | For her achievements she has been awarded the Arjuna award and the Padma Shri. She has inspired other Indian women, such as Bachendri Pal, the first Indian woman to successfully climb Mount Everest. As a child, Pal began to aspire to national fame after seeing a newspaper photograph of Zutshi with Prime Minister Indira Gandhi. She was coached by Mohammad Ilyas Babar. | [
{
"qid": "Q513",
"surface_form": "Mount Everest",
"mention_offset": 627,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Nepal",
"People's Republic of China"
],
"coordinates": {
"lat": 27.988055555555555,
"lon": 86.925
}
}... |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 21,
"offset_start": 1953,
"offset_end": 2048,
"text": "The Saguenay River as well as the Lac Saint-Jean are both contained within the Saguenay Graben."
} | To the east there is the Kenogami threshold which is characterized by having an altitude of. This threshold splits the graben into two physiographic regions; the Lac Saint-Jean region to the west and the Saguenay region to the east. The plateau around the Graben is between in altitude. The Saguenay River as well as the Lac Saint-Jean are both contained within the Saguenay Graben. Local geology. | [
{
"qid": "Q979922",
"surface_form": "Lac Saint-Jean",
"mention_offset": 1987,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.594444444444,
"lon": -72.03
}
},
{
"qid": "Q979922",
"surf... |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 19,
"offset_start": 1759,
"offset_end": 1898,
"text": "This threshold splits the graben into two physiographic regions; the Lac Saint-Jean region to the west and the Saguenay region to the east."
} | Present day geography. The lowlands within the graben have an altitude of between. To the east there is the Kenogami threshold which is characterized by having an altitude of. This threshold splits the graben into two physiographic regions; the Lac Saint-Jean region to the west and the Saguenay region to the east. The plateau around the Graben is between in altitude. | [
{
"qid": "Q979922",
"surface_form": "lac saint-jean",
"mention_offset": 1828,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.594444444444,
"lon": -72.03
}
},
{
"qid": "Q979922",
"surfac... |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 0,
"offset_start": 0,
"offset_end": 16,
"text": "Saguenay Graben."
} | Saguenay Graben. The Saguenay Graben is a rift valley or graben in the geological Grenville Province of southern Quebec, Canada. It is an elongated flat-bottomed basin long and wide, bounded by normal faults running parallel to its length. Formation of the Saguenay Graben. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 1,
"offset_start": 17,
"offset_end": 128,
"text": "The Saguenay Graben is a rift valley or graben in the geological Grenville Province of southern Quebec, Canada."
} | Saguenay Graben. The Saguenay Graben is a rift valley or graben in the geological Grenville Province of southern Quebec, Canada. It is an elongated flat-bottomed basin long and wide, bounded by normal faults running parallel to its length. Formation of the Saguenay Graben. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 21,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 3,
"offset_start": 240,
"offset_end": 273,
"text": "Formation of the Saguenay Graben."
} | It is an elongated flat-bottomed basin long and wide, bounded by normal faults running parallel to its length. Formation of the Saguenay Graben. The time of formation of the faults related to the Saguenay Graben is still under debate because it is difficult to accurately measure the age of faulting. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 257,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 4,
"offset_start": 274,
"offset_end": 429,
"text": "The time of formation of the faults related to the Saguenay Graben is still under debate because it is difficult to accurately measure the age of faulting."
} | Formation of the Saguenay Graben. The time of formation of the faults related to the Saguenay Graben is still under debate because it is difficult to accurately measure the age of faulting. Evidence suggests it was either the opening of the Iapetus Ocean (600–400 Ma), or the opening of the Atlantic Ocean (195–170 Ma) that caused the faulting. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 325,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 7,
"offset_start": 733,
"offset_end": 830,
"text": "The resulting bedrock between dropped down along the normal faults, creating the Saguenay Graben."
} | During the opening of one of these oceans, fragmentation of the landmass occurred creating two fault planes, one to the north and one to the south. The resulting bedrock between dropped down along the normal faults, creating the Saguenay Graben. The extent of these faults are only known at the surface and therefore their extension and shape at depth is unknown. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 814,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 9,
"offset_start": 949,
"offset_end": 1073,
"text": "The faults associated with the Saguenay Graben have been the source for earthquakes, including the 1988 Saguenay earthquake."
} | The resulting bedrock between dropped down along the normal faults, creating the Saguenay Graben. The extent of these faults are only known at the surface and therefore their extension and shape at depth is unknown. The faults associated with the Saguenay Graben have been the source for earthquakes, including the 1988 Saguenay earthquake. Glaciations. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 980,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 23,
"offset_start": 2064,
"offset_end": 2164,
"text": "The Saguenay Graben is in the Grenville Province (but was created long after the Grenville Orogeny)."
} | The plateau around the Graben is between in altitude. The Saguenay River as well as the Lac Saint-Jean are both contained within the Saguenay Graben. Local geology. The Saguenay Graben is in the Grenville Province (but was created long after the Grenville Orogeny). The Saguenay Graben is characterized primarily by the rock types: gneiss, anorthosite and granite that are Proterozoic in age. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 2068,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
19,753,951 | http://en.wikipedia.org/wiki/Saguenay_Graben | {
"id": 24,
"offset_start": 2165,
"offset_end": 2291,
"text": "The Saguenay Graben is characterized primarily by the rock types: gneiss, anorthosite and granite that are Proterozoic in age."
} | Local geology. The Saguenay Graben is in the Grenville Province (but was created long after the Grenville Orogeny). The Saguenay Graben is characterized primarily by the rock types: gneiss, anorthosite and granite that are Proterozoic in age. There are two outliers of limestone and shale of the Paleozoic that are found only in the graben due to its faulting. | [
{
"qid": "Q3112938",
"surface_form": "saguenay graben",
"mention_offset": 2169,
"link_type": "weak",
"instance_of": [
"Valley"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 48.5,
"lon": -71.3333
}
}
] |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 4,
"offset_start": 348,
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"text": "It is also notable for being well within the interior of the Tibetan Plateau (most peaks of similar height – except notably Shishapangma, the world's 14th-highest peak – lie nearer to or outside the edge of the Plateau) and relatively far away from other peaks with heights greater than 7,500 metres."
} | It is the 34th-highest peak in the world (using a 500-metre prominence cutoff). It is also notable for being well within the interior of the Tibetan Plateau (most peaks of similar height – except notably Shishapangma, the world's 14th-highest peak – lie nearer to or outside the edge of the Plateau) and relatively far away from other peaks with heights greater than 7,500 metres. | [
{
"qid": "Q179842",
"surface_form": "Tibetan Plateau",
"mention_offset": 409,
"link_type": "direct",
"instance_of": [
"Plateau"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 33,
"lon": 88
}
},
{
"qid": "Q105124",
... |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 5,
"offset_start": 649,
"offset_end": 727,
"text": "It sits roughly across Lake Manasarovar from the sacred peak of Mount Kailash."
} | It is also notable for being well within the interior of the Tibetan Plateau (most peaks of similar height – except notably Shishapangma, the world's 14th-highest peak – lie nearer to or outside the edge of the Plateau) and relatively far away from other peaks with heights greater than 7,500 metres. It sits roughly across Lake Manasarovar from the sacred peak of Mount Kailash. Names. | [
{
"qid": "Q233627",
"surface_form": "Lake Manasarovar",
"mention_offset": 672,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 30.666666666667,
"lon": 81.5
}
},
{
"qid": "... |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 8,
"offset_start": 799,
"offset_end": 1086,
"text": "It supposedly derives from a pass near the mountain and the legendary prehistoric Indian king Mandhata of the Raghuvaṃśa branch of the Solar Dynasty, who supposedly conquered the earth and passed the mountain on his way to the sacred lake Manasarovar beside the axis mundi Mount Kailash."
} | Names. "Gurla Mandhata" is a romanization of the Hindi name. It supposedly derives from a pass near the mountain and the legendary prehistoric Indian king Mandhata of the Raghuvaṃśa branch of the Solar Dynasty, who supposedly conquered the earth and passed the mountain on his way to the sacred lake Manasarovar beside the axis mundi Mount Kailash. | [
{
"qid": "Q233627",
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"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 30.666666666667,
"lon": 81.5
}
},
{
"qid": "Q229... |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 23,
"offset_start": 2737,
"offset_end": 2859,
"text": "In 1935, the Viennese student Herbert Tichy made a trip to the holy mountain Kailash while disguised as an Indian pilgrim."
} | This was a strong achievement for the time, especially for such a small group; at that time no summit of over 7,000 m had yet been climbed and Longstaff's height represented a world altitude record. In 1935, the Viennese student Herbert Tichy made a trip to the holy mountain Kailash while disguised as an Indian pilgrim. On the way, he attempted Gurla Mandhata with one of his porters, Kitar. | [
{
"qid": "Q229107",
"surface_form": "Kailash",
"mention_offset": 2814,
"link_type": "direct",
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],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 31.066944444444,
"lon": 81.312777777778
}
}
] |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 0,
"offset_start": 0,
"offset_end": 15,
"text": "Gurla Mandhata."
} | Gurla Mandhata. Gurla Mandhata, also Naimona'nyi or Namu Nani, is the highest peak of the Nalakankar Himal, a small subrange of the Himalaya. It lies in Burang County of the Ngari Prefecture in the Tibet Autonomous Region of China, near the northwest corner of Nepal. It is the 34th-highest peak in the world (using a 500-metre prominence cutoff). | [
{
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"mention_offset": 0,
"link_type": "weak",
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],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 30.438333333333,
"lon": 81.299166666667
}
}
] |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 1,
"offset_start": 16,
"offset_end": 141,
"text": "Gurla Mandhata, also Naimona'nyi or Namu Nani, is the highest peak of the Nalakankar Himal, a small subrange of the Himalaya."
} | Gurla Mandhata. Gurla Mandhata, also Naimona'nyi or Namu Nani, is the highest peak of the Nalakankar Himal, a small subrange of the Himalaya. It lies in Burang County of the Ngari Prefecture in the Tibet Autonomous Region of China, near the northwest corner of Nepal. It is the 34th-highest peak in the world (using a 500-metre prominence cutoff). | [
{
"qid": "Q1555230",
"surface_form": "gurla mandhata",
"mention_offset": 16,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 30.438333333333,
"lon": 81.299166666667
}
}
] |
4,750,754 | http://en.wikipedia.org/wiki/Gurla_Mandhata | {
"id": 7,
"offset_start": 735,
"offset_end": 798,
"text": ""Gurla Mandhata" is a romanization of the Hindi name."
} | Names. "Gurla Mandhata" is a romanization of the Hindi name. It supposedly derives from a pass near the mountain and the legendary prehistoric Indian king Mandhata of the Raghuvaṃśa branch of the Solar Dynasty, who supposedly conquered the earth and passed the mountain on his way to the sacred lake Manasarovar beside the axis mundi Mount Kailash. | [
{
"qid": "Q1555230",
"surface_form": "gurla mandhata",
"mention_offset": 736,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 30.438333333333,
"lon": 81.299166666667
}
}
] |
80,763,104 | http://en.wikipedia.org/wiki/St._Peter%27s_Church_(Kajmak%C4%8Dalan) | {
"id": 1,
"offset_start": 34,
"offset_end": 250,
"text": "St. Peter and Paul (), known simply as St. Peter or by the name of the peak St. Elijah (), is an Eastern Orthodox church on Kajmakčalan peak of the Voras Mountains, near in North Macedonia, on the border with Greece."
} | St. Peter's Church (Kajmakčalan). St. Peter and Paul (), known simply as St. Peter or by the name of the peak St. Elijah (), is an Eastern Orthodox church on Kajmakčalan peak of the Voras Mountains, near in North Macedonia, on the border with Greece. It is part of the of the Macedonian Orthodox Church. Background. | [
{
"qid": "Q1288074",
"surface_form": "Kajmakčalan",
"mention_offset": 158,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Greece",
"North Macedonia"
],
"coordinates": {
"lat": 40.930277777778,
"lon": 21.786111111111
}
}
] |
80,763,104 | http://en.wikipedia.org/wiki/St._Peter%27s_Church_(Kajmak%C4%8Dalan) | {
"id": 6,
"offset_start": 641,
"offset_end": 913,
"text": "The next year, the heart of Archibald Reiss was placed in an urn at the church, at his own request; Reiss was a Swiss journalist in Serbian service who covered the battles on the Macedonian front (Salonika front), which spread across the mountain Kajmakčalan in Маcedonia."
} | In 1928, the monument was converted into a church-ossuary dedicated to Saint Peter. The next year, the heart of Archibald Reiss was placed in an urn at the church, at his own request; Reiss was a Swiss journalist in Serbian service who covered the battles on the Macedonian front (Salonika front), which spread across the mountain Kajmakčalan in Маcedonia. | [
{
"qid": "Q1288074",
"surface_form": "Kajmakčalan",
"mention_offset": 888,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Greece",
"North Macedonia"
],
"coordinates": {
"lat": 40.930277777778,
"lon": 21.786111111111
}
}
] |
68,631,921 | http://en.wikipedia.org/wiki/Nghi_Vo | {
"id": 5,
"offset_start": 390,
"offset_end": 463,
"text": "In 2007 she moved to Milwaukee, Wisconsin on the shores of Lake Michigan."
} | Biography. Vo was born in Peoria, Illinois, where she lived until attending college at the University of Illinois Urbana-Champaign. In 2007 she moved to Milwaukee, Wisconsin on the shores of Lake Michigan. She defines her sexuality as queer. Vo's first published short story was "Gift of Flight" in 2007, after which she published a number of short stories in various media. | [
{
"qid": "Q1169",
"surface_form": "Lake Michigan",
"mention_offset": 449,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.007874,
"lon": -86.756451
}
}
] |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 2,
"offset_start": 169,
"offset_end": 324,
"text": "The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain."
} | Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain. | [
{
"qid": "Q49050081",
"surface_form": "Midway Mountain",
"mention_offset": 308,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 36.6433251,
"lon": -118.48371
}
},
{
"qid": "Q779899... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 0,
"offset_start": 0,
"offset_end": 43,
"text": "Table Mountain (Tulare County, California)."
} | Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain. | [
{
"qid": "Q7673138",
"surface_form": "table mountain",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 39.59807864926865,
"lon": -121.55626585419016
}
},
{
"qid"... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 1,
"offset_start": 44,
"offset_end": 168,
"text": "Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California."
} | Table Mountain (Tulare County, California). Table Mountain is located near the northern end of the Great Western Divide, a sub-range of the Sierra Nevada in California. The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain. | [
{
"qid": "Q7673138",
"surface_form": "table mountain",
"mention_offset": 44,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 39.59807864926865,
"lon": -121.55626585419016
}
},
{
"qid... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 6,
"offset_start": 643,
"offset_end": 717,
"text": "In 1905, the Board on Geographic Names recognized the name Table Mountain."
} | Hoffmann's map of 1873. In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the "Tehipite" and the "Mt. Whitney" USGS 30' maps published in 1905 and 1907 respectively. | [
{
"qid": "Q7673138",
"surface_form": "table mountain",
"mention_offset": 692,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 39.59807864926865,
"lon": -121.55626585419016
}
},
{
"qi... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 8,
"offset_start": 857,
"offset_end": 926,
"text": "It is the tallest of the 21 peaks named Table Mountain in California."
} | In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the "Tehipite" and the "Mt. Whitney" USGS 30' maps published in 1905 and 1907 respectively. It is the tallest of the 21 peaks named Table Mountain in California. | [
{
"qid": "Q7673138",
"surface_form": "table mountain",
"mention_offset": 867,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 39.59807864926865,
"lon": -121.55626585419016
}
},
{
"qi... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 7,
"offset_start": 718,
"offset_end": 856,
"text": "This name appeared on both the "Tehipite" and the "Mt. Whitney" USGS 30' maps published in 1905 and 1907 respectively."
} | In 1881 the mountain was named Mount Hazen in honor of General Hazen, the Chief Signal Officer of the U.S. Army. In 1905, the Board on Geographic Names recognized the name Table Mountain. This name appeared on both the "Tehipite" and the "Mt. Whitney" USGS 30' maps published in 1905 and 1907 respectively. It is the tallest of the 21 peaks named Table Mountain in California. | [
{
"qid": "Q235539",
"surface_form": "mt. whitney",
"mention_offset": 759,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 36.57861111111111,
"lon": -118.29194444444444
}
},
{
"qid": ... |
12,738,168 | http://en.wikipedia.org/wiki/Table_Mountain_(Tulare_County%2C_California) | {
"id": 3,
"offset_start": 325,
"offset_end": 505,
"text": "Clarence King of the Whitney Survey mentioned in his notes that "At one place the ridge [Great Western Divide] forms a level table." The name Table appeared on Charles F."
} | The summit marks a point on the boundary between Sequoia and Kings Canyon national parks and is south of Thunder Mountain and northeast of Midway Mountain. Clarence King of the Whitney Survey mentioned in his notes that "At one place the ridge [Great Western Divide] forms a level table." The name Table appeared on Charles F. Hoffmann's map of 1873. | [
{
"qid": "Q235539",
"surface_form": "whitney",
"mention_offset": 346,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 36.57861111111111,
"lon": -118.29194444444444
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 9,
"offset_start": 499,
"offset_end": 576,
"text": "It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi."
} | Features of the lake. Koskikeskinen is 650 meters long, 500 meters wide and covers an area of 14.0 hectares. It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi. The short river bed of the Jämsänjoki starts from the Kankarisvesi, which descends through two parallel rapids, Naiskoski and Rekolankoski, into the Koskikeskinen. | [
{
"qid": "Q11869613",
"surface_form": "Kankarisvesi",
"mention_offset": 563,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9667,
"lon": 25.1333
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 10,
"offset_start": 577,
"offset_end": 740,
"text": "The short river bed of the Jämsänjoki starts from the Kankarisvesi, which descends through two parallel rapids, Naiskoski and Rekolankoski, into the Koskikeskinen."
} | It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi. The short river bed of the Jämsänjoki starts from the Kankarisvesi, which descends through two parallel rapids, Naiskoski and Rekolankoski, into the Koskikeskinen. The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway. | [
{
"qid": "Q11869613",
"surface_form": "kankarisvesi",
"mention_offset": 631,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9667,
"lon": 25.1333
}
},
{
"qid": "Q24368261",
"surface_for... |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 13,
"offset_start": 950,
"offset_end": 1050,
"text": "The surface of Koskikeskinen is 5.6 meters below Kankarisvesi and around 13 meters below Jämsänjoki."
} | The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway. The Jämsänjoki continues south from Koskikeskinen for about 14 kilometers, discharging into the Päijänne. The surface of Koskikeskinen is 5.6 meters below Kankarisvesi and around 13 meters below Jämsänjoki. The river flows through a pipe under the Jämsänkoski paper mill. | [
{
"qid": "Q11869613",
"surface_form": "kankarisvesi",
"mention_offset": 999,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9667,
"lon": 25.1333
}
},
{
"qid": "Q24368261",
"surface_for... |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 0,
"offset_start": 0,
"offset_end": 14,
"text": "Koskikeskinen."
} | Koskikeskinen. Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 1,
"offset_start": 15,
"offset_end": 87,
"text": "Koskikeskinen is a lake located in central Jämsänkoski, Central Finland."
} | Koskikeskinen. Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 15,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 2,
"offset_start": 88,
"offset_end": 172,
"text": "Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route."
} | Koskikeskinen. Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 88,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 4,
"offset_start": 230,
"offset_end": 273,
"text": "Koskikeskinen is 96 meters above sea level."
} | Koskikeskinen is a lake located in central Jämsänkoski, Central Finland. Koskikeskinen is a backwater between two rapids that belong to the Jämsänjoki route. The lake is surrounded by the urban area of Jämsänkoski. Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. Features of the lake. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 230,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 8,
"offset_start": 412,
"offset_end": 498,
"text": "Koskikeskinen is 650 meters long, 500 meters wide and covers an area of 14.0 hectares."
} | Koskikeskinen is 96 meters above sea level. The area is 14 hectares and the coast is 2.41 kilometers long. The lake is part of the Kymi River's drainage basin. Features of the lake. Koskikeskinen is 650 meters long, 500 meters wide and covers an area of 14.0 hectares. It is located in the upper reaches of Jämsänjoki below the lake Kankarisvesi. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 412,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 12,
"offset_start": 844,
"offset_end": 949,
"text": "The Jämsänjoki continues south from Koskikeskinen for about 14 kilometers, discharging into the Päijänne."
} | The Rekolankoski power plant operates on the western route, while the Naiskoski is used as a spillway. The Jämsänjoki continues south from Koskikeskinen for about 14 kilometers, discharging into the Päijänne. The surface of Koskikeskinen is 5.6 meters below Kankarisvesi and around 13 meters below Jämsänjoki. The river flows through a pipe under the Jämsänkoski paper mill. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 880,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 22,
"offset_start": 1638,
"offset_end": 1751,
"text": "The southern and southwestern shores of Koskikeskinen are dominated by the industrial environment of Jämsänkoski."
} | It was once isolated by the factory line of the industrial area. Today, the former railway is a light traffic route and a wooden footbridge crosses the mouth of the bay. The southern and southwestern shores of Koskikeskinen are dominated by the industrial environment of Jämsänkoski. Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 1678,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 23,
"offset_start": 1752,
"offset_end": 1868,
"text": "Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse."
} | Today, the former railway is a light traffic route and a wooden footbridge crosses the mouth of the bay. The southern and southwestern shores of Koskikeskinen are dominated by the industrial environment of Jämsänkoski. Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse. West bank. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 1783,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
74,670,559 | http://en.wikipedia.org/wiki/Koskikeskinen | {
"id": 25,
"offset_start": 1880,
"offset_end": 1965,
"text": "On the west bank of Koskikeskinen is Pässinmäki, where art exhibitions are organized."
} | Right on the southern shore of Koskikeskinen is the factory company's old clubhouse and a red brick paper warehouse. West bank. On the west bank of Koskikeskinen is Pässinmäki, where art exhibitions are organized. The historic industrial environment of Naiskoski and Rekolankoski, where power plants and old factories have been converted into restaurants, is located on the lake's northern shore. | [
{
"qid": "Q24368261",
"surface_form": "koskikeskinen",
"mention_offset": 1900,
"link_type": "weak",
"instance_of": [
"Lake"
],
"countries": [
"Finland"
],
"coordinates": {
"lat": 61.9204085,
"lon": 25.1612886
}
}
] |
7,362,740 | http://en.wikipedia.org/wiki/Jean-Baptiste_R%C3%A9gis | {
"id": 30,
"offset_start": 4174,
"offset_end": 4338,
"text": "Régis and Cardoso drew the map of Shandong; Jartoux, Fridelli and Bonjour traversed Mongolia as far as Lake Baikal in the north and the Zunghar Khanate to the west."
} | In 1711 the Portuguese priest Francis Cardoso, and the Augustinian Guillaume Bonjour, the only non-Jesuit, joined the geographers. Régis and Cardoso drew the map of Shandong; Jartoux, Fridelli and Bonjour traversed Mongolia as far as Lake Baikal in the north and the Zunghar Khanate to the west. | [
{
"qid": "Q5513",
"surface_form": "Lake Baikal",
"mention_offset": 4277,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Russia",
"Russian Empire",
"Soviet Union"
],
"coordinates": {
"lat": 53.30277778,
"lon": 108.00472222
... |
139,914 | http://en.wikipedia.org/wiki/Williams_Bay%2C_Wisconsin | {
"id": 2,
"offset_start": 97,
"offset_end": 146,
"text": "It is one of three municipalities on Geneva Lake."
} | Williams Bay, Wisconsin. Williams Bay is a village in Walworth County, Wisconsin, United States. It is one of three municipalities on Geneva Lake. The population was 2,953 at the 2020 census. On June 22, 2024 the town was hit by an EF-1 tornado, there were no injuries or fatalities, but the storm caused some areas of considerable damage. History. | [
{
"qid": "Q14714439",
"surface_form": "Geneva Lake",
"mention_offset": 134,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 42.59,
"lon": -88.435
}
}
] |
15,160,561 | http://en.wikipedia.org/wiki/Kyaukphyu_District | {
"id": 8,
"offset_start": 422,
"offset_end": 526,
"text": "Kyaukpyu is a district in the Arakan division of Lower Burma, on the eastern coast of the Bay of Bengal."
} | Geography. Kyaukpyu is a district in the Arakan division of Lower Burma, on the eastern coast of the Bay of Bengal. It consists of, first, a strip of mainland along the Bay of Bengal, extending from the An pass, across the main range, to the Ma-ī River, and, secondly, the large islands of Ramree and Cheduba, with many others to the south, lying off the coast of Sandoway. | [
{
"qid": "Q38684",
"surface_form": "Bay of Bengal",
"mention_offset": 512,
"link_type": "direct",
"instance_of": [
"Body of water"
],
"countries": [
"India",
"Bangladesh",
"Sri Lanka",
"Myanmar"
],
"coordinates": {
"lat": 15,
"lon": 88
... |
2,286,088 | http://en.wikipedia.org/wiki/Pukaskwa_River | {
"id": 2,
"offset_start": 119,
"offset_end": 246,
"text": "It is in the Great Lakes Basin and is a tributary of Lake Superior, which it enters at the south end of Pukaskwa National Park."
} | Pukaskwa River. The Pukaskwa River is a river in Thunder Bay District and Algoma District in Northern Ontario, Canada. It is in the Great Lakes Basin and is a tributary of Lake Superior, which it enters at the south end of Pukaskwa National Park. It is a remote, pristine, free-flowing, medium-sized Shield river, with lots of whitewater, best travelled in spring. | [
{
"qid": "Q1066",
"surface_form": "Lake Superior",
"mention_offset": 172,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Canada",
"United States"
],
"coordinates": {
"lat": 47.52881611111111,
"lon": -87.76002194444445
}
}
] |
9,688,338 | http://en.wikipedia.org/wiki/MAS_(motorboat) | {
"id": 57,
"offset_start": 7660,
"offset_end": 7791,
"text": "Another flotilla of four MAS, the XII Squadriglia MAS, was deployed to Lake Ladoga in April 1942 to support the siege of Leningrad."
} | They were armed with one 13 mm heavy machine gun or one 20 mm anti-aircraft gun, 6 depth charges and two 450 mm torpedoes. Another flotilla of four MAS, the XII Squadriglia MAS, was deployed to Lake Ladoga in April 1942 to support the siege of Leningrad. They claim the sinking of a Soviet gunboat of the Bira class, a 1,300-ton cargo ship and several barges. | [
{
"qid": "Q15288",
"surface_form": "Lake Ladoga",
"mention_offset": 7731,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Russia",
"Russian Empire",
"Soviet Union"
],
"coordinates": {
"lat": 60.842777777777776,
"lon": 31.45972... |
29,398,478 | http://en.wikipedia.org/wiki/Campbell_Ridges | {
"id": 1,
"offset_start": 17,
"offset_end": 131,
"text": "The Campbell Ridges () are an irregular complex of ridges between Creswick Gap and Mount Courtauld in Palmer Land."
} | Campbell Ridges. The Campbell Ridges () are an irregular complex of ridges between Creswick Gap and Mount Courtauld in Palmer Land. Two north–south ridges are linked by an east–west ridge, on which stand the highest peaks. They were named by the Advisory Committee on Antarctic Names for Lieutenant Commander Bruce H. Campbell, U.S. | [
{
"qid": "Q7337740",
"surface_form": "Mount Courtauld",
"mention_offset": 100,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [],
"coordinates": {
"lat": -70.35,
"lon": -67.4667
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 33,
"offset_start": 4137,
"offset_end": 4499,
"text": "Mount Canobolas is not, as is sometimes claimed in tourism brochures, the highest point between Australia's Great Dividing Range and Africa, as Mount Zeil in Australia's Northern Territory and Ngarutjaranya in South Australia are further west and higher, and a number of peaks elsewhere on the Great Dividing Range and peaks on Madagascar and Réunion are higher."
} | Highest point claims. Mount Canobolas is not, as is sometimes claimed in tourism brochures, the highest point between Australia's Great Dividing Range and Africa, as Mount Zeil in Australia's Northern Territory and Ngarutjaranya in South Australia are further west and higher, and a number of peaks elsewhere on the Great Dividing Range and peaks on Madagascar and Réunion are higher. | [
{
"qid": "Q1950830",
"surface_form": "Mount Zeil",
"mention_offset": 4281,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -23.401666666666667,
"lon": 132.39583333333334
}
},
{
"qid": ... |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 0,
"offset_start": 0,
"offset_end": 16,
"text": "Mount Canobolas."
} | Mount Canobolas. Mount Canobolas, a mountain on a spur of the Great Dividing Range, is located in the Central Tablelands region of New South Wales, Australia. With an elevation of above sea level, Mount Canobolas, an extinct volcano, is the highest mountain in the region. Situated southwest of the city of Orange, it is about west of Sydney. | [
{
"qid": "Q1691036",
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"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 1,
"offset_start": 17,
"offset_end": 158,
"text": "Mount Canobolas, a mountain on a spur of the Great Dividing Range, is located in the Central Tablelands region of New South Wales, Australia."
} | Mount Canobolas. Mount Canobolas, a mountain on a spur of the Great Dividing Range, is located in the Central Tablelands region of New South Wales, Australia. With an elevation of above sea level, Mount Canobolas, an extinct volcano, is the highest mountain in the region. Situated southwest of the city of Orange, it is about west of Sydney. | [
{
"qid": "Q1691036",
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"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 2,
"offset_start": 159,
"offset_end": 272,
"text": "With an elevation of above sea level, Mount Canobolas, an extinct volcano, is the highest mountain in the region."
} | Mount Canobolas. Mount Canobolas, a mountain on a spur of the Great Dividing Range, is located in the Central Tablelands region of New South Wales, Australia. With an elevation of above sea level, Mount Canobolas, an extinct volcano, is the highest mountain in the region. Situated southwest of the city of Orange, it is about west of Sydney. | [
{
"qid": "Q1691036",
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"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 7,
"offset_start": 596,
"offset_end": 731,
"text": "This means "two shoulders" which refers to the summits of Mount Canobolas itself and the subsidiary peak Young Man Canobolas."
} | Etymology. The name comes from two words in the Wiradjuri language (the local Aboriginal language), "gaahna" and "bula". This means "two shoulders" which refers to the summits of Mount Canobolas itself and the subsidiary peak Young Man Canobolas. Description. | [
{
"qid": "Q1691036",
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"mention_offset": 634,
"link_type": "weak",
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"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
},
{
"qid": "Q1691036",
"sur... |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 12,
"offset_start": 1142,
"offset_end": 1251,
"text": "The contemporary landscape of Mount Canobolas exhibits erosional features dominated by several remnant peaks."
} | Later eruptions became more violent, and producing increasingly viscous lavas with less extensive coverage. The contemporary landscape of Mount Canobolas exhibits erosional features dominated by several remnant peaks. Additional volcanic features are present within the zone of volcanic influence, including vents, dykes, peaks, domes and plugs. | [
{
"qid": "Q1691036",
"surface_form": "mount canobolas",
"mention_offset": 1142,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 19,
"offset_start": 1935,
"offset_end": 2172,
"text": "The mountain is now part of the Mount Canobolas Conservation Area, managed by the NSW National Parks & Wildlife Service, which offers various walks: to Bald Hill; to Young Man Canobolas; Federal Falls to Mount Towac, and other locations."
} | The summit can be seen from up to 100 km away. The mountain is now part of the Mount Canobolas Conservation Area, managed by the NSW National Parks & Wildlife Service, which offers various walks: to Bald Hill; to Young Man Canobolas; Federal Falls to Mount Towac, and other locations. The volcanic peaks give wide views and there are some attractive waterfalls. | [
{
"qid": "Q1691036",
"surface_form": "mount canobolas",
"mention_offset": 1937,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
},
{
"qid": "Q4850313",
"su... |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 23,
"offset_start": 2818,
"offset_end": 3025,
"text": "Each year the Orange community runs the Great Volcanic Mountain Challenge, an walk and fun run from the Pinnacle to the Summit of Mount Canobolas by the volcanic plugs of Mount Towac and Young Man Canobolas."
} | Each year the Orange community runs the Great Volcanic Mountain Challenge, an walk and fun run from the Pinnacle to the Summit of Mount Canobolas by the volcanic plugs of Mount Towac and Young Man Canobolas. The inaugural event was held in 2006. Fires on the mountain. A major bushfire in 1967 affected 415 ha in the northern section of the Mount Canobolas Conservation Area. | [
{
"qid": "Q1691036",
"surface_form": "mount canobolas",
"mention_offset": 2918,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 26,
"offset_start": 3087,
"offset_end": 3193,
"text": "A major bushfire in 1967 affected 415 ha in the northern section of the Mount Canobolas Conservation Area."
} | The inaugural event was held in 2006. Fires on the mountain. A major bushfire in 1967 affected 415 ha in the northern section of the Mount Canobolas Conservation Area. Another bushfire in 1982 affected 414 ha in the western part of the conservation area and a further bushfire occurred in the southern part of the conservation area in 1985. | [
{
"qid": "Q1691036",
"surface_form": "mount canobolas",
"mention_offset": 3129,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
}
] |
613,924 | http://en.wikipedia.org/wiki/Mount_Canobolas | {
"id": 28,
"offset_start": 3367,
"offset_end": 3704,
"text": "Another bushfire affected most of the northern area of Mount Canobolas in February 2018, and the entire Mount Canobolas Conservation Area apart from the summit remains closed (as of mid 2020) until the effects of this fire – the danger of falling trees and branches and damage to much of the walking track infrastructure – are rectified."
} | Another bushfire affected most of the northern area of Mount Canobolas in February 2018, and the entire Mount Canobolas Conservation Area apart from the summit remains closed (as of mid 2020) until the effects of this fire – the danger of falling trees and branches and damage to much of the walking track infrastructure – are rectified. | [
{
"qid": "Q1691036",
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"mention_offset": 3392,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -33.3442,
"lon": 148.982
}
},
{
"qid": "Q1691036",
"su... |
20,281,183 | http://en.wikipedia.org/wiki/%C3%98verlandselva | {
"id": 3,
"offset_start": 177,
"offset_end": 267,
"text": "It runs south and southwest, emptying into the eastern side of Engervannet at Blommenholm."
} | Øverlandselva. Øverlandselva is a river that flows through Bærum, Norway. It starts near Øverland in northern Bærum, at the confluence of the creeks Seternbekken and Ilabekken. It runs south and southwest, emptying into the eastern side of Engervannet at Blommenholm. A river runs from Engervannet and flows into Sandvikselva, but this portion is called Rønneelva. | [
{
"qid": "Q4580205",
"surface_form": "Engervannet",
"mention_offset": 240,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Norway"
],
"coordinates": {
"lat": 59.896944444444,
"lon": 10.534444444444
}
}
] |
69,458,918 | http://en.wikipedia.org/wiki/Nigerien_nationality_law | {
"id": 48,
"offset_start": 5903,
"offset_end": 6180,
"text": "France continued to expand from Senegal and in 1882 having gained control of the territories along the Mellacorée, Nunez, and Pongo Rivers, as well as Tombo Island by establishing trading posts over the area, created the colony Rivières du Sud (Southern Rivers), now in Guinea."
} | The following year, these were joined into the United African Company, which later became the National African Company. France continued to expand from Senegal and in 1882 having gained control of the territories along the Mellacorée, Nunez, and Pongo Rivers, as well as Tombo Island by establishing trading posts over the area, created the colony Rivières du Sud (Southern Rivers), now in Guinea. | [
{
"qid": "Q767474",
"surface_form": "Nunez",
"mention_offset": 6018,
"link_type": "direct",
"instance_of": [
"Watercourse"
],
"countries": [
"Guinea"
],
"coordinates": {
"lat": 10.594471,
"lon": -14.675102
}
}
] |
8,686,373 | http://en.wikipedia.org/wiki/KLOO-FM | {
"id": 3,
"offset_start": 221,
"offset_end": 322,
"text": "KLOO-FM broadcasts a classic rock music format to the Salem, Oregon, and Mid-Willamette Valley areas."
} | KLOO-FM. KLOO-FM (106.3 MHz) is a commercial radio station licensed to serve Corvallis, Oregon, United States. The station is owned by Bicoastal Media and the broadcast license is held by Bicoastal Media Licenses V, LLC. KLOO-FM broadcasts a classic rock music format to the Salem, Oregon, and Mid-Willamette Valley areas. | [
{
"qid": "Q1703681",
"surface_form": "Willamette Valley",
"mention_offset": 298,
"link_type": "direct",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.9,
"lon": -123.1
}
}
] |
64,076,540 | http://en.wikipedia.org/wiki/Janet_Reed | {
"id": 26,
"offset_start": 3734,
"offset_end": 3840,
"text": "She taught at Bard College, Annandale-on-Hudson, New York, and then founded a school in the Hudson Valley."
} | Reed left the NYCB in 1964, retiring from performing dance to spend more time with her family. She taught at Bard College, Annandale-on-Hudson, New York, and then founded a school in the Hudson Valley. Reed was a United States Cultural Exchange Programs consultant recommending companies to represent American dance abroad. | [
{
"qid": "Q1140235",
"surface_form": "Hudson Valley",
"mention_offset": 3826,
"link_type": "direct",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 41.9209,
"lon": -73.9613
}
}
] |
8,418 | http://en.wikipedia.org/wiki/Dartmouth_College | {
"id": 167,
"offset_start": 24629,
"offset_end": 24805,
"text": "In addition to its campus in Hanover, Dartmouth owns of Mount Moosilauke in the White Mountains and a tract of land in northern New Hampshire known as the Second College Grant."
} | Dartmouth is the largest private landowner of the town of Hanover, and its total landholdings and facilities are worth an estimated $434 million. In addition to its campus in Hanover, Dartmouth owns of Mount Moosilauke in the White Mountains and a tract of land in northern New Hampshire known as the Second College Grant. | [
{
"qid": "Q3321961",
"surface_form": "Mount Moosilauke",
"mention_offset": 24685,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 44.024511111111,
"lon": -71.830916666667
}
}
] |
46,331,572 | http://en.wikipedia.org/wiki/Ha_Gorge | {
"id": 2,
"offset_start": 121,
"offset_end": 241,
"text": "It is located in the west slope of Thrypti mountain range, and exits east\nof Vasiliki village in the plain of Ierapetra."
} | Ha Gorge. Ha Gorge () is a narrow gorge, at the Monasteraki Dakos, on the eastern part of the island of Crete in Greece. It is located in the west slope of Thrypti mountain range, and exits east
of Vasiliki village in the plain of Ierapetra. From this location scenic views overlook Pahia Amos and the bay. | [
{
"qid": "Q7798619",
"surface_form": "Thrypti",
"mention_offset": 156,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Greece"
],
"coordinates": {
"lat": 35.08,
"lon": 25.875555555556
}
}
] |
45,000,420 | http://en.wikipedia.org/wiki/Taruja_Pincha | {
"id": 0,
"offset_start": 0,
"offset_end": 14,
"text": "Taruja Pincha."
} | Taruja Pincha. Taruja Pincha (Aymara "taruja" deer, "pincha" irrigation channel or ditch, "deer ditch", Hispanicized spelling "Tarucapincha") or Taruka Pincha (Quechua "taruka" deer, "pincha" aqueduct; sewer) is a mountain in the Peruvian Andes, about high. | [
{
"qid": "Q19421443",
"surface_form": "taruja pincha",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Peru"
],
"coordinates": {
"lat": -14.5281,
"lon": -70.0678
}
}
] |
45,000,420 | http://en.wikipedia.org/wiki/Taruja_Pincha | {
"id": 1,
"offset_start": 15,
"offset_end": 317,
"text": "Taruja Pincha (Aymara "taruja" deer, "pincha" irrigation channel or ditch, "deer ditch", Hispanicized spelling "Tarucapincha") or Taruka Pincha (Quechua "taruka" deer, "pincha" aqueduct; sewer) is a mountain in the Peruvian Andes, about high."
} | Taruja Pincha. Taruja Pincha (Aymara "taruja" deer, "pincha" irrigation channel or ditch, "deer ditch", Hispanicized spelling "Tarucapincha") or Taruka Pincha (Quechua "taruka" deer, "pincha" aqueduct; sewer) is a mountain in the Peruvian Andes, about high. | [
{
"qid": "Q19421443",
"surface_form": "taruja pincha",
"mention_offset": 15,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Peru"
],
"coordinates": {
"lat": -14.5281,
"lon": -70.0678
}
}
] |
41,145,961 | http://en.wikipedia.org/wiki/Puerto_C%C3%A1rdenas | {
"id": 1,
"offset_start": 17,
"offset_end": 122,
"text": "Puerto Cárdenas is a lakeside hamlet () at the outflow of Yelcho Lake in Chaitén commune, southern Chile."
} | Puerto Cárdenas. Puerto Cárdenas is a lakeside hamlet () at the outflow of Yelcho Lake in Chaitén commune, southern Chile. Carretera Austral passes by the hamlet. | [
{
"qid": "Q3110434",
"surface_form": "Yelcho Lake",
"mention_offset": 75,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Chile"
],
"coordinates": {
"lat": -43.3,
"lon": -72.3
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 2,
"offset_start": 108,
"offset_end": 274,
"text": "It lies at the north end of the Wapta Icefield, in Banff National Park, about one km (0.6 mi) east of the border with British Columbia and north of the town of Field."
} | Peyto Peak. Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada. It lies at the north end of the Wapta Icefield, in Banff National Park, about one km (0.6 mi) east of the border with British Columbia and north of the town of Field. Five kilometres to the northeast lies Bow Pass, one of the high points of the Icefields Parkway. | [
{
"qid": "Q1858093",
"surface_form": "columbia",
"mention_offset": 234,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 52.1475,
"lon": -117.44055555555556
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 5,
"offset_start": 431,
"offset_end": 532,
"text": "Three kilometres southwest of Peyto Peak is Mount Baker, the highest point in the immediate vicinity."
} | Five kilometres to the northeast lies Bow Pass, one of the high points of the Icefields Parkway. Between the peak and the pass lies picturesque Peyto Lake. Three kilometres southwest of Peyto Peak is Mount Baker, the highest point in the immediate vicinity. History. | [
{
"qid": "Q6919562",
"surface_form": "mount baker",
"mention_offset": 475,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.665277777777774,
"lon": -116.59777777777778
}
},
{
"qid": "Q717... |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 1,
"offset_start": 12,
"offset_end": 107,
"text": "Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada."
} | Peyto Peak. Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada. It lies at the north end of the Wapta Icefield, in Banff National Park, about one km (0.6 mi) east of the border with British Columbia and north of the town of Field. Five kilometres to the northeast lies Bow Pass, one of the high points of the Icefields Parkway. | [
{
"qid": "Q3036893",
"surface_form": "mountain",
"mention_offset": 28,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.4677778,
"lon": -116.1416667
}
},
{
"qid": "Q7179615",
"surface... |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 8,
"offset_start": 713,
"offset_end": 797,
"text": "The first ascent of the peak was in 1933 by famed mountaineer Conrad Kain and party."
} | History. Peyto Peak was named in 1896 by Walter Wilcox for Ebenezer William "Bill" Peyto, an early outfitter, trail guide and trapper in the Banff and Lake Louise areas. The first ascent of the peak was in 1933 by famed mountaineer Conrad Kain and party. The mountain's name became official in 1928 by the Geographical Names Board of Canada. Geology. | [
{
"qid": "Q3036893",
"surface_form": "mountain",
"mention_offset": 792,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.4677778,
"lon": -116.1416667
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 0,
"offset_start": 0,
"offset_end": 11,
"text": "Peyto Peak."
} | Peyto Peak. Peyto Peak is a mountain in the Waputik Range, part of the Canadian Rockies in Alberta, Canada. It lies at the north end of the Wapta Icefield, in Banff National Park, about one km (0.6 mi) east of the border with British Columbia and north of the town of Field. Five kilometres to the northeast lies Bow Pass, one of the high points of the Icefields Parkway. | [
{
"qid": "Q7179615",
"surface_form": "peyto peak",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.683888888889,
"lon": -116.56555555556
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 7,
"offset_start": 542,
"offset_end": 712,
"text": "Peyto Peak was named in 1896 by Walter Wilcox for Ebenezer William "Bill" Peyto, an early outfitter, trail guide and trapper in the Banff and Lake Louise areas."
} | Three kilometres southwest of Peyto Peak is Mount Baker, the highest point in the immediate vicinity. History. Peyto Peak was named in 1896 by Walter Wilcox for Ebenezer William "Bill" Peyto, an early outfitter, trail guide and trapper in the Banff and Lake Louise areas. The first ascent of the peak was in 1933 by famed mountaineer Conrad Kain and party. | [
{
"qid": "Q7179615",
"surface_form": "peyto peak",
"mention_offset": 542,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.683888888889,
"lon": -116.56555555556
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 11,
"offset_start": 894,
"offset_end": 1026,
"text": "Like other mountains in Banff Park, Peyto Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods."
} | The mountain's name became official in 1928 by the Geographical Names Board of Canada. Geology. Like other mountains in Banff Park, Peyto Peak is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. | [
{
"qid": "Q7179615",
"surface_form": "peyto peak",
"mention_offset": 920,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.683888888889,
"lon": -116.56555555556
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 14,
"offset_start": 1160,
"offset_end": 1292,
"text": "Based on the Köppen climate classification, Peyto Peak is located in a subarctic climate with cold, snowy winters, and mild summers."
} | Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny. Climate. Based on the Köppen climate classification, Peyto Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. | [
{
"qid": "Q7179615",
"surface_form": "peyto peak",
"mention_offset": 1194,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.683888888889,
"lon": -116.56555555556
}
}
] |
4,970,968 | http://en.wikipedia.org/wiki/Peyto_Peak | {
"id": 16,
"offset_start": 1366,
"offset_end": 1480,
"text": "Precipitation runoff from Peyto Peak drains into the Mistaya River which is a tributary of the Saskatchewan River."
} | Climate. Based on the Köppen climate classification, Peyto Peak is located in a subarctic climate with cold, snowy winters, and mild summers. Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Peyto Peak drains into the Mistaya River which is a tributary of the Saskatchewan River. | [
{
"qid": "Q7179615",
"surface_form": "peyto peak",
"mention_offset": 1382,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Canada"
],
"coordinates": {
"lat": 51.683888888889,
"lon": -116.56555555556
}
},
{
"qid": "Q2330416",... |
2,219,742 | http://en.wikipedia.org/wiki/Taejo_of_Goryeo | {
"id": 48,
"offset_start": 5828,
"offset_end": 5986,
"text": "Hearing of the news, Taejo planned a strike with 5,000 cavalrymen to attack Kyon's troops on the way back home at Gongsan near Daegu in the Battle of Gongsan."
} | In 927, Kyon Hwon of Later Baekje led his forces into Silla's capital, Gyeongju, capturing and executing its king, King Gyeongae. Then he established King Gyeongsun as his puppet monarch before he turned his army toward Goryeo. Hearing of the news, Taejo planned a strike with 5,000 cavalrymen to attack Kyon's troops on the way back home at Gongsan near Daegu in the Battle of Gongsan. | [
{
"qid": "Q624313",
"surface_form": "Gongsan",
"mention_offset": 5942,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"South Korea"
],
"coordinates": {
"lat": 36.016944444444,
"lon": 128.695
}
}
] |
50,622,077 | http://en.wikipedia.org/wiki/Gowlagh_South | {
"id": 6,
"offset_start": 493,
"offset_end": 637,
"text": "It is called Gowlagh South to distinguish it from Gowlagh North townland at the foot of Slieve Rushen mountain, with which it has no connection."
} | Its chief geographical features are the River Blackwater, County Cavan, bogs and spring wells. It is called Gowlagh South to distinguish it from Gowlagh North townland at the foot of Slieve Rushen mountain, with which it has no connection. Gowlagh South is traversed by the L1037 road, minor public roads and rural lanes. The townland covers 165 statute acres. History. | [
{
"qid": "Q2974585",
"surface_form": "Slieve Rushen",
"mention_offset": 581,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"United Kingdom",
"Ireland"
],
"coordinates": {
"lat": 54.151925,
"lon": -7.6426416666667
}
}
] |
51,218,936 | http://en.wikipedia.org/wiki/Grevillea_delta | {
"id": 11,
"offset_start": 1091,
"offset_end": 1248,
"text": ""delta" in his book "New names in "Grevillea" (Proteaceae)" from specimens collected by Alex George near Mount Lesueur in 1974."
} | Taxonomy. This grevillea was first formally described in 1986 by Donald McGillivray who gave it the name "Grevillea thelemanniana" subsp. "delta" in his book "New names in "Grevillea" (Proteaceae)" from specimens collected by Alex George near Mount Lesueur in 1974. In 1994 Peter M. Olde and Neil R. | [
{
"qid": "Q6921816",
"surface_form": "Mount Lesueur",
"mention_offset": 1226,
"link_type": "direct",
"instance_of": [
"Mountain"
],
"countries": [
"Australia"
],
"coordinates": {
"lat": -30.1755,
"lon": 115.19908333333
}
}
] |
48,148,329 | http://en.wikipedia.org/wiki/Qawi | {
"id": 0,
"offset_start": 0,
"offset_end": 5,
"text": "Qawi."
} | Qawi. Qawi (Quechua for to put into the sun, hispanicized spelling "Jahui") is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Huaura Province, Santa Leonor District, in the Oyón Province, Oyón District, and in the Pasco Region, Pasco Province, Huayllay District. | [
{
"qid": "Q25247747",
"surface_form": "qawi",
"mention_offset": 0,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Peru"
],
"coordinates": {
"lat": -10.8525,
"lon": -76.58722222
}
}
] |
48,148,329 | http://en.wikipedia.org/wiki/Qawi | {
"id": 1,
"offset_start": 6,
"offset_end": 133,
"text": "Qawi (Quechua for to put into the sun, hispanicized spelling "Jahui") is a mountain in the Andes of Peru, about high."
} | Qawi. Qawi (Quechua for to put into the sun, hispanicized spelling "Jahui") is a mountain in the Andes of Peru, about high. It is located in the Lima Region, Huaura Province, Santa Leonor District, in the Oyón Province, Oyón District, and in the Pasco Region, Pasco Province, Huayllay District. | [
{
"qid": "Q25247747",
"surface_form": "qawi",
"mention_offset": 6,
"link_type": "weak",
"instance_of": [
"Mountain"
],
"countries": [
"Peru"
],
"coordinates": {
"lat": -10.8525,
"lon": -76.58722222
}
}
] |
46,731,507 | http://en.wikipedia.org/wiki/Hispanics_and_Latinos_in_Colorado | {
"id": 25,
"offset_start": 2237,
"offset_end": 2317,
"text": "1851- A small group of Nuevomexicanos from Taos migrated to the San Luis Valley."
} | 1848- Northwest Mexico was incorporated into the US, including western Colorado. 1851- A small group of Nuevomexicanos from Taos migrated to the San Luis Valley. They founded the first Hispanic permanent settlement and initiated Hispanic migration to Colorado. | [
{
"qid": "Q649768",
"surface_form": "San Luis Valley",
"mention_offset": 2301,
"link_type": "direct",
"instance_of": [
"Valley"
],
"countries": [
"United States"
],
"coordinates": {
"lat": 37.2,
"lon": -105.42
}
}
] |
19,233,810 | http://en.wikipedia.org/wiki/%C5%A0koda_Yeti | {
"id": 66,
"offset_start": 8831,
"offset_end": 9034,
"text": "In 2014, Škoda Auto presented the "Yeti Xtreme" at the Wörthersee annual meeting in Austria, with the concept having a matte dark gray body color with yellow elements such as the rims and roof."
} | In 2014, Škoda Auto presented the "Yeti Xtreme" at the Wörthersee annual meeting in Austria, with the concept having a matte dark gray body color with yellow elements such as the rims and roof. In October 2022, Škoda Auto issued a press release about the Yeti, also showing its concepts. | [
{
"qid": "Q546146",
"surface_form": "Wörthersee",
"mention_offset": 8896,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"Austria"
],
"coordinates": {
"lat": 46.625,
"lon": 14.15
}
}
] |
74,749,708 | http://en.wikipedia.org/wiki/Black_Jacks_Island | {
"id": 1,
"offset_start": 20,
"offset_end": 90,
"text": "Black Jacks Island is an island in Lake Benmore in Otago, New Zealand."
} | Black Jacks Island. Black Jacks Island is an island in Lake Benmore in Otago, New Zealand. | [
{
"qid": "Q917385",
"surface_form": "Lake Benmore",
"mention_offset": 55,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"New Zealand"
],
"coordinates": {
"lat": -44.415,
"lon": 170.22055555556
}
}
] |
21,730,796 | http://en.wikipedia.org/wiki/Madhyamak%C4%81la%E1%B9%83k%C4%81ra | {
"id": 13,
"offset_start": 1840,
"offset_end": 2128,
"text": "The "Madhyamakālaṃkāra" and its tradition survived the destruction of Nalanda Vihara and the ascendancy of the Muslim empire in India during the 13th-century eclipse of Buddhism through its transplantation to the Tibetan Plateau by Śāntarakṣita at the request of Trisong Detsen."
} | Samye Monastery. The "Madhyamakālaṃkāra" and its tradition survived the destruction of Nalanda Vihara and the ascendancy of the Muslim empire in India during the 13th-century eclipse of Buddhism through its transplantation to the Tibetan Plateau by Śāntarakṣita at the request of Trisong Detsen. It was taught at the Samye Monastery, which was safeguarded by the Himalayas. | [
{
"qid": "Q179842",
"surface_form": "Tibetan Plateau",
"mention_offset": 2063,
"link_type": "direct",
"instance_of": [
"Plateau"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 33,
"lon": 88
}
}
] |
12,185,559 | http://en.wikipedia.org/wiki/Triplophysa | {
"id": 8,
"offset_start": 1163,
"offset_end": 1341,
"text": "In the other end, "Triplophysa stolickai" holds the record altitude for Asian fish: it is found at above sea level in hot springs near the Longmu Lake in western Tibet."
} | Ecology. "Triplophysa zhaoi" holds the record for the lowest altitude for Asian fish: it is found at below sea level in swamps of the Lükqün oasis, in the Turpan Depression in Xinjiang. In the other end, "Triplophysa stolickai" holds the record altitude for Asian fish: it is found at above sea level in hot springs near the Longmu Lake in western Tibet. | [
{
"qid": "Q6674152",
"surface_form": "Longmu Lake",
"mention_offset": 1312,
"link_type": "direct",
"instance_of": [
"Lake"
],
"countries": [
"People's Republic of China"
],
"coordinates": {
"lat": 34.61444444,
"lon": 80.46
}
}
] |
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