Sarmila/GeoWiki-Features huggingface dataset:
Named by US-ACAN for Lt. (jg) John Dzema of United States Navy Squadron VX-6 who was at McMurdo Station the 1962-63 and 1963-64 seasons. Cole Peak. Peak, high, located northeast of Mount Doumani at the north side of Watson Escarpment. Named by US-ACAN for Jerry D. Cole, airman with United States Navy Squadron VX-6 at McMurdo Sound, 1957 and 1960. Mount Ratliff.

Geographic entities mentioned:
surface_form: mount doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
surface_form: doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Jerry D. Cole, airman with United States Navy Squadron VX-6 at McMurdo Sound, 1957 and 1960. Mount Ratliff. Mountain, high, located north of Watson Escarpment and NNE of Mount Doumani. Named by US-ACAN for Charles E. Ratliff, aviation machinist mate with United States Navy Squadron VX-6 in several Operation Deep Freeze deployments, 1963-67. Mount O'Neil.

Geographic entities mentioned:
surface_form: mount doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
surface_form: doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
This mountain was obscured by clouds during much of the visit by the USARP party. Mount Doumani. Prominent mountain, high, standing between Johns and Kansas Glaciers at the north side of Watson Escarpment. Named by US-ACAN for George A. Doumani, geologist with the Byrd Station winter party in 1959. Doumani explored the Horlick Mountains area that year and in 1960-61, 1961-62 and 1964-65.

Geographic entities mentioned:
surface_form: george
instance_of: Mountain
coordinates: lat: -67.71667
lon: 50
Mount Doumani. Prominent mountain, high, standing between Johns and Kansas Glaciers at the north side of Watson Escarpment. Named by US-ACAN for George A. Doumani, geologist with the Byrd Station winter party in 1959. Doumani explored the Horlick Mountains area that year and in 1960-61, 1961-62 and 1964-65. He visited the Mount Weaver area in 1962-63. Foreman Peak.

Geographic entities mentioned:
surface_form: doumani
instance_of: Mountain
coordinates: lat: -85.8167
lon: -137.633
Skilift Col. A col in the mountain wall between the Griffith Glacier and Howe Glacier, on the west side of Watson Escarpment. The col is northeast of Mount Meeks and provides a shortcut to field parties. So named by NZGSAE, 1969-70, because some members of the party used a motor toboggan here in a similar way to a ski-lift. Mount Riley.

Geographic entities mentioned:
surface_form: field
instance_of: Mountain
coordinates: lat: -80.88333
lon: 158
California Plateau. An undulating ice-covered plateau, long and from wide, which rises to high at the eastern side of Scott Glacier. The plateau reaches a maximum height in Mount Blackburn, high, at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
Named by US-ACAN for Stephen Kivi, utilitiesman at Byrd Station in 1962. Michigan Plateau. . An undulating ice-covered plateau, long, which rises to high at the western side of Reedy Glacier. The northern and eastern sides of the plateau are marked by the steep Watson Escarpment; the western and southern sides grade gradually to the elevation of the interior ice.

Geographic entities mentioned:
surface_form: southern
instance_of: Mountain
coordinates: lat: -74.2
lon: -76.4667
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Watson Escarpment. Watson Escarpment () is a major escarpment in the Queen Maud Mountains, trending northward along the east margin of Scott Glacier, then eastward to Reedy Glacier where it turns southward along the glacier's west side. Somewhat arcuate, the escarpment is nearly long, rises above sea level, and above the adjacent terrain. Discovery and naming.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Watson Escarpment. Watson Escarpment () is a major escarpment in the Queen Maud Mountains, trending northward along the east margin of Scott Glacier, then eastward to Reedy Glacier where it turns southward along the glacier's west side. Somewhat arcuate, the escarpment is nearly long, rises above sea level, and above the adjacent terrain. Discovery and naming.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
The escarpment and its related features was mapped in detail by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960–64. Topology. The western end of the Watson Escarpment is a massif to the northeast of the point where the Van Reeth Glacier joins the Scott Glacier. The tip of the massif holds Mount Czegka, Acarospora Peak and Dunn Spur.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
To the north of Mount Blackburn the Long Valley leads to the head of Griffith Glacier, which is separated from Howe Glacier by Mount Meeks and Skilift Col. Mount Riley and Roaring Ridge are east of Long Valley. The Watson Escarpment continues east along the rim of the California Plateau past Beacon Dome and Mount Warden. It continues below Maaske Dome and above Evans Butte.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Acarospora Peak. A peak northeast of, and only slightly below the elevation of Mount Czegka, located at the southwest end of Watson Escarpment. Named by New Zealand Antarctic Place Names Committee (NZ-APC) on suggestion of New Zealand Geological Survey
Antarctic Expedition (NZGSAE) Scott Glacier Party, 1969-70, because the lichen &quot;Acarospora emergens Dodge&quot; was found on the peak.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Russell, Sr., a supporter of the Byrd Antarctic expeditions. Mount Blackburn. A massive, flat-topped mountain, high, standing just east of Scott Glacier where it surmounts the southwest end of California Plateau and the Watson Escarpment. Discovered by and named for Quin A. Blackburn, geologist, leader of the ByrdAE geological party which sledged the length of Scott Glacier in December 1934.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Named by US-ACAN for Lt. Harman T. Meeks of United States Navy Squadron VX-6, navigator on aircraft during Operation Deep Freeze 1966 and 1967. Skilift Col. A col in the mountain wall between the Griffith Glacier and Howe Glacier, on the west side of Watson Escarpment. The col is northeast of Mount Meeks and provides a shortcut to field parties.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: howe
instance_of: Mountain
coordinates: lat: -87.3667
lon: -149.5
Riley, photographic officer with United States Navy Squadron VX-6 on Operation Deep Freeze 1966 and 1967. Roaring Ridge. A long and outstanding spur that descends from the Watson Escarpment northeast of Mount Blackburn. So named by NZGSAE (1969-70) because two geologists worked and camped nearby, experiencing roaring gale force winds rushing down the steep escarpment. California Plateau.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
The plateau reaches a maximum height in Mount Blackburn, high, at the southern end. The northwestern side of the plateau is marked by the steep rock cliffs of Watson Escarpment; the southeastern side grades gradually to the elevation of the interior ice. Named by US-ACAN for the several branches of the University of California which have sent numerous researchers to work in Antarctica.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for the several branches of the University of California which have sent numerous researchers to work in Antarctica. Beacon Dome. A large dome-like mountain, high, standing at the head of Griffith Glacier along the Watson Escarpment. So named by NZGSAE (1969-70) because the mountain is composed of a granite basement with horizontally layered rocks of the Beacon series above.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
So named by NZGSAE (1969-70) because the mountain is composed of a granite basement with horizontally layered rocks of the Beacon series above. Mount Warden. A snow-covered peak, high, standing close southeast of Hunt Spur and surmounting a projecting buttress at the northwest face of Watson Escarpment. Named by US-ACAN for Lt. George W.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: hunt
instance_of: Mountain
coordinates: lat: -67.1167
lon: 144.3
Warden, United States Navy, pilot on aircraft flights over the Queen Maud Mountains in United States Navy Operation Highjump, 1946-47. Hunt Spur. A rugged spur descending from Mount Warden along the northwest face of Watson Escarpment. Named by US-ACAN for Glenn C. Hunt, aviation electronics technician of United States Navy Squadron VX-6 who participated in Operation Deep Freeze for 5 years.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Robert M. Beazley, MC, United States Navy, officer in charge of the South Pole Station winter party, 1965. McLean Peak. A peak, high, surmounting a spur descending from the northwest end of Stanford Plateau, along the Watson Escarpment. Named by US-ACAN for Lt. William E. McLean, United States Navy, medical officer and officer in charge of the South Pole Station winter party in 1964.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Stanford Plateau. An icecapped plateau, over high high and wide, between the heads of Leverett and Kansas Glaciers. The plateau unites with the interior ice sheet to the S, but terminates to the north in the Watson Escarpment. Named by US-ACAN for Stanford University which has sent a number of researchers to study Antarctica. Phleger Dome.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Stanford University which has sent a number of researchers to study Antarctica. Phleger Dome. A massive dome-shaped mountain, high, at the northeast end of Stanford Plateau along the Watson Escarpment. Named by US-ACAN for Herman Phleger, one of the United States representatives in the discussions on the Antarctic Treaty of 1959. Lowe Bluff.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Herman Phleger, one of the United States representatives in the discussions on the Antarctic Treaty of 1959. Lowe Bluff. A high, ice-covered bluff between the head of Kansas Glacier and Alaska Canyon, along the Watson Escarpment. Named by US-ACAN for William G. Lowe, radioman with the Byrd Station winter party, 1957. Mount Analogue.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
surface_form: alaska canyon
instance_of: Landform
coordinates: lat: -86
lon: -136.55
Lowe Bluff. A high, ice-covered bluff between the head of Kansas Glacier and Alaska Canyon, along the Watson Escarpment. Named by US-ACAN for William G. Lowe, radioman with the Byrd Station winter party, 1957. Mount Analogue. A prominent mountain along the Watson Escarpment, rising to high and forming the highest point of the ridge that runs north from Phleger Dome, Stanford Plateau.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
This mountain was obscured by clouds during much of the visit by the USARP party. Mount Doumani. Prominent mountain, high, standing between Johns and Kansas Glaciers at the north side of Watson Escarpment. Named by US-ACAN for George A. Doumani, geologist with the Byrd Station winter party in 1959. Doumani explored the Horlick Mountains area that year and in 1960-61, 1961-62 and 1964-65.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Doumani explored the Horlick Mountains area that year and in 1960-61, 1961-62 and 1964-65. He visited the Mount Weaver area in 1962-63. Foreman Peak. Peak, high, standing west of Dzema Peak on the north side of Watson Escarpment. Named by US-ACAN for Donald L. Foreman, mechanic with United States Navy Squadron VX-6 who wintered at Little
America V in 1958 and McMurdo Station in 1960. Dzema Peak.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Donald L. Foreman, mechanic with United States Navy Squadron VX-6 who wintered at Little
America V in 1958 and McMurdo Station in 1960. Dzema Peak. Peak, high, standing west-southwest of Mount Ratliff on the north side of Watson Escarpment. Named by US-ACAN for Lt. (jg) John Dzema of United States Navy Squadron VX-6 who was at McMurdo Station the 1962-63 and 1963-64 seasons.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Harlan Cleveland, Asst. Sec. of State for International Organization Affairs, 1961-65, who was Chairman of the Antarctic Policy Group in 1965. Mink Peak. A prominent peak standing north of Cleveland Mesa, at the east end of Watson Escarpment. Named by US-ACAN for Harold D. Mink, utilitiesman with the wintering parties at Byrd Station in 1962 and 1966. Shapley Ridge.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN for Harold D. Mink, utilitiesman with the wintering parties at Byrd Station in 1962 and 1966. Shapley Ridge. A prominent ridge overlooking Reedy Glacier; it extends east from Cleveland Mesa and marks the east extremity of the Watson Escarpment. Named by US-ACAN for Alan H. Shapley, ViceChairman of the United States National Committee for the IGY. Kivi Peak.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Named by US-ACAN after the University of Michigan at Ann Arbor, Michigan, which has sent numerous research personnel to work in Antarctica. Teller Peak. A peak, high, marking the northeast extremity of Michigan Plateau and the Watson Escarpment. Mapped by USGS from surveys and United States Navy air photos, 1960-63. Named by US-AC AN for James T.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
Mapped by USGS from surveys and United States Navy air photos, 1960-63. Named by US-AC AN for James T. Teller, geologist with the Ohio State University party to the Horlick Mountains in 1964-65. Burlock Peak. A peak, high, on the spur descending from Mount Simsarian, along the east face of Watson Escarpment. Named by US-ACAN for James U. Burlock, builder at Byrd Station in 1962. Mount Simsarian.

Geographic entities mentioned:
surface_form: watson escarpment
instance_of: Landform
coordinates: lat: -86
lon: -145
The north-central part of the escarpment was observed from a vantage point on Supporting Party Mountain and was partially mapped in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould. The escarpment was more closely observed in December 1934 by the Byrd Antarctic Expedition geological party under Quin Blackburn, and was named by Byrd for Thomas J.

Geographic entities mentioned:
surface_form: thomas
instance_of: Mountain
coordinates: lat: -71.01666667
lon: 64.6
Dunn Spur. A prominent rock spur which descends from Mount Blackburn and extends for along the north side of Van Reeth Glacier. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Thomas H. Dunn of United States Navy Squadron VX-6, aircrewman on photographic
Mount Russell.

Geographic entities mentioned:
surface_form: thomas
instance_of: Mountain
coordinates: lat: -71.01666667
lon: 64.6
Somewhat arcuate, the escarpment is nearly long, rises above sea level, and above the adjacent terrain. Discovery and naming. The north-central part of the escarpment was observed from a vantage point on Supporting Party Mountain and was partially mapped in December 1929 by the Byrd Antarctic Expedition geological party under Laurence Gould.

Geographic entities mentioned:
surface_form: discovery
instance_of: Mountain
coordinates: lat: -78.366666666667
lon: 165.01666666667
surface_form: discovery
instance_of: Body of water
coordinates: lat: -64.5167
lon: -63.0167
Named by US-ACAN for Herman Phleger, one of the United States representatives in the discussions on the Antarctic Treaty of 1959. Lowe Bluff. A high, ice-covered bluff between the head of Kansas Glacier and Alaska Canyon, along the Watson Escarpment. Named by US-ACAN for William G. Lowe, radioman with the Byrd Station winter party, 1957. Mount Analogue.

Geographic entities mentioned:
surface_form: william
instance_of: Mountain
coordinates: lat: -64.7833
lon: -63.6833
Most of the features along the escarpment were mapped by the United States Geological Survey (USGS) from ground surveys and United States Navy air photos between 1960 and 1964. Mount Czegka. A mountain, high, on the east side of Scott Glacier, just north of the terminus of Van Reeth Glacier. Discovered in December 1934 by the ByrdAE geological party under Quin Blackburn.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
A peak northeast of, and only slightly below the elevation of Mount Czegka, located at the southwest end of Watson Escarpment. Named by New Zealand Antarctic Place Names Committee (NZ-APC) on suggestion of New Zealand Geological Survey
Antarctic Expedition (NZGSAE) Scott Glacier Party, 1969-70, because the lichen &quot;Acarospora emergens Dodge&quot; was found on the peak. Dunn Spur.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Thomas H. Dunn of United States Navy Squadron VX-6, aircrewman on photographic
Mount Russell. A mountain, high, standing on the east flank of Scott Glacier just south of the mouth of Howe Glacier. Discovered in December 1934 by the geological party of the ByrdAE, 1933-35, and named for Richard S.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
surface_form: howe
instance_of: Mountain
coordinates: lat: -87.3667
lon: -149.5
Mount Blackburn. A massive, flat-topped mountain, high, standing just east of Scott Glacier where it surmounts the southwest end of California Plateau and the Watson Escarpment. Discovered by and named for Quin A. Blackburn, geologist, leader of the ByrdAE geological party which sledged the length of Scott Glacier in December 1934. Parker Bluff.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
So named by NZGSAE (1969-70) because two geologists worked and camped nearby, experiencing roaring gale force winds rushing down the steep escarpment. California Plateau. An undulating ice-covered plateau, long and from wide, which rises to high at the eastern side of Scott Glacier. The plateau reaches a maximum height in Mount Blackburn, high, at the southern end.

Geographic entities mentioned:
surface_form: scott
instance_of: Mountain
coordinates: lat: -65.15158
lon: -64.04798
Mount Czegka. A mountain, high, on the east side of Scott Glacier, just north of the terminus of Van Reeth Glacier. Discovered in December 1934 by the ByrdAE geological party under Quin Blackburn. Named by Byrd after Victor H. Czegka (1880-1973), CWO, USMC, who served as a member with the ByrdAE, 1928-30, and also as member and supply manager with the ByrdAE, 1933-35. Acarospora Peak.

Geographic entities mentioned:
surface_form: victor
instance_of: Mountain
coordinates: lat: -72.6
lon: 31.26666667
Named by US-ACAN for Jerry D. Cole, airman with United States Navy Squadron VX-6 at McMurdo Sound, 1957 and 1960. Mount Ratliff. Mountain, high, located north of Watson Escarpment and NNE of Mount Doumani. Named by US-ACAN for Charles E. Ratliff, aviation machinist mate with United States Navy Squadron VX-6 in several Operation Deep Freeze deployments, 1963-67. Mount O'Neil.

Geographic entities mentioned:
surface_form: charles
instance_of: Mountain
coordinates: lat: -67.38333
lon: 50
Roberts Ridge. A prominent ridge southwest of Cleveland Mesa, at the southeast end of Michigan Plateau. Mapped by USGS from surveys and USN air photos, 1960-64. Named by US-ACAN for Peter Roberts of the Division of International Scientific and Technical Affairs, Department of State.

Geographic entities mentioned:
surface_form: peter
instance_of: Mountain
coordinates: lat: -70.1833
lon: 64.9333
The tip of the massif holds Mount Czegka, Acarospora Peak and Dunn Spur. To the north are Mount Russell, Mount Blackburn and Parker Bluff. To the north of Mount Blackburn the Long Valley leads to the head of Griffith Glacier, which is separated from Howe Glacier by Mount Meeks and Skilift Col. Mount Riley and Roaring Ridge are east of Long Valley.

Geographic entities mentioned:
surface_form: howe
instance_of: Mountain
coordinates: lat: -87.3667
lon: -149.5
Named by US-ACAN for Walter H. Long, Jr., of United States Navy Squadron VX-6, photographer on Operation Deep Freeze 1966 and 1967. Mount Meeks. A mountain, high, surmounting the rocky divide between Griffith Glacier and Howe Glacier. Named by US-ACAN for Lt. Harman T. Meeks of United States Navy Squadron VX-6, navigator on aircraft during Operation Deep Freeze 1966 and 1967. Skilift Col.

Geographic entities mentioned:
surface_form: howe
instance_of: Mountain
coordinates: lat: -87.3667
lon: -149.5
It is designated an Important Cultural Property. &quot;Ryōgen&quot; (912–985), also known as &quot;Jie Daishi&quot;, was the 18th chief abbot of Enryaku-ji, the head Tendai monastery located on Mount Hiei in Ōtsu. He is considered a restorer of the Tendai school of Mahayana Buddhism, and credited for reviving Enryaku-ji.

Geographic entities mentioned:
surface_form: Mount Hiei
instance_of: Mountain
countries: Japan
coordinates: lat: 35.066666666667
lon: 135.83833333333
Phyllonorycter sagitella. &quot;Phyllonorycter sagitella&quot; is a moth of the family Gracillariidae. It is found from Fennoscandia and northern Russia to the Pyrenees, Italy and Romania and from Great Britain to southern Russia. The wingspan is 8.5-9.5 mm.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Sunlight Creek Bridge. Sunlight Creek Bridge is a steel beam bridge in Park County, Wyoming, United States in the Shoshone National Forest and is the highest bridge in the state. It carries Chief Joseph Scenic Byway (Wyoming Highway 296) and pedestrian walkways on each side over the Sunlight Gorge carved by Sunlight Creek. The bridge was built in 1985.

Geographic entities mentioned:
surface_form: Sunlight Creek
instance_of: Watercourse
countries: United States
coordinates: lat: 44.694667
lon: -109.82018
Avala Tower. The Avala Tower () is a tall telecommunications tower located on Mount Avala, in Belgrade, Serbia. The original tower was finished in 1965, but was destroyed on 29 April 1999, during the NATO bombing of Yugoslavia. The tower's reconstruction commenced on 21 December 2006 and it was officially opened on 21 April 2010. Origin.

Geographic entities mentioned:
surface_form: Avala
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.690555555556
lon: 20.514166666667
Bisle, Kagneri, Kanchankumari reserve forests cover portions the Bisle Ghat, and adjoin Pushpagiri Wildlife Sanctuary in Kodagu. Rainfall. Hassan district is located on the leeward side of Western Ghats, thus receives less rainfall than coastal Karnataka. The district comes under three river basins: Netravathi, Kaveri and Vedavathi (Krishna River).

Geographic entities mentioned:
surface_form: Kaveri
instance_of: Watercourse
countries: India
coordinates: lat: 11.370345
lon: 79.828105
Gearhart Mountain. Gearhart Mountain is a mountain in Lake County and Klamath County, Oregon, in the United States. It is located in the Gearhart Mountain Wilderness of the Fremont–Winema National Forest, northeast of the Sprague River valley and the town of Bly. Geology. Gearhart Mountain is one of the larger volcanoes in Lake County.

Geographic entities mentioned:
surface_form: gearhart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.496
lon: -120.8783
Gearhart Mountain. Gearhart Mountain is a mountain in Lake County and Klamath County, Oregon, in the United States. It is located in the Gearhart Mountain Wilderness of the Fremont–Winema National Forest, northeast of the Sprague River valley and the town of Bly. Geology. Gearhart Mountain is one of the larger volcanoes in Lake County.

Geographic entities mentioned:
surface_form: gearhart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.496
lon: -120.8783
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
Gearhart Mountain. Gearhart Mountain is a mountain in Lake County and Klamath County, Oregon, in the United States. It is located in the Gearhart Mountain Wilderness of the Fremont–Winema National Forest, northeast of the Sprague River valley and the town of Bly. Geology. Gearhart Mountain is one of the larger volcanoes in Lake County.

Geographic entities mentioned:
surface_form: gearhart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.496
lon: -120.8783
surface_form: river valley
instance_of: Valley
countries: United States
coordinates: lat: 35.36
lon: -93.37
It is located in the Gearhart Mountain Wilderness of the Fremont–Winema National Forest, northeast of the Sprague River valley and the town of Bly. Geology. Gearhart Mountain is one of the larger volcanoes in Lake County. It is a Miocene shield volcano and stratovolcano that has been eroded and become extinct.

Geographic entities mentioned:
surface_form: gearhart mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.496
lon: -120.8783
Vučji zub. Vučji zub (trans. &quot;Wolf's tooth&quot;) is at 1805 m one of the higher peaks in the Orjen masif. The boundary between the Ottoman Empire, Austro-Hungarian Empire and the principality of Montenegro ran across Vučji zub until 1879. Vučji zub is still today the border stone between Montenegro and Bosnia and Herzegovina.

Geographic entities mentioned:
surface_form: vučji zub
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.58111111
lon: 18.55361111
Vučji zub. Vučji zub (trans. &quot;Wolf's tooth&quot;) is at 1805 m one of the higher peaks in the Orjen masif. The boundary between the Ottoman Empire, Austro-Hungarian Empire and the principality of Montenegro ran across Vučji zub until 1879. Vučji zub is still today the border stone between Montenegro and Bosnia and Herzegovina.

Geographic entities mentioned:
surface_form: vučji zub
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.58111111
lon: 18.55361111
surface_form: vučji zub
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.58111111
lon: 18.55361111
&quot;Wolf's tooth&quot;) is at 1805 m one of the higher peaks in the Orjen masif. The boundary between the Ottoman Empire, Austro-Hungarian Empire and the principality of Montenegro ran across Vučji zub until 1879. Vučji zub is still today the border stone between Montenegro and Bosnia and Herzegovina. Vučji zub resembles a horn and is an interesting climbing destination in the Orjen range.

Geographic entities mentioned:
surface_form: vučji zub
instance_of: Mountain
countries: Montenegro
coordinates: lat: 42.58111111
lon: 18.55361111
Prospectors Mountain. Prospectors Mountain () is a mountain in the Teton Range, located within Grand Teton National Park in the U.S. state of Wyoming. Prospectors Mountain rises to the south above Rimrock Lake and Death Canyon.

Geographic entities mentioned:
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: prospectors mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6494
lon: -110.849
surface_form: grand teton
instance_of: Mountain
countries: United States
coordinates: lat: 43.7412
lon: -110.802
Prospectors Mountain. Prospectors Mountain () is a mountain in the Teton Range, located within Grand Teton National Park in the U.S. state of Wyoming. Prospectors Mountain rises to the south above Rimrock Lake and Death Canyon.

Geographic entities mentioned:
surface_form: prospectors mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6494
lon: -110.849
Prospectors Mountain. Prospectors Mountain () is a mountain in the Teton Range, located within Grand Teton National Park in the U.S. state of Wyoming. Prospectors Mountain rises to the south above Rimrock Lake and Death Canyon.

Geographic entities mentioned:
surface_form: prospectors mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.6494
lon: -110.849
surface_form: rimrock lake
instance_of: Lake
countries: United States
coordinates: lat: 43.6553
lon: -110.846
Mexican dace. The Mexican dace (&quot;Evarra bustamantei&quot;), or Mexican chub, is an extinct species of ray-finned fish in the family Leuciscidae. It was found only in Mexico, in the canals and streams of the Valley of Mexico. It is estimated to have become extinct circa 1983. The extinction of this species coincided with the drying of water bodies in the valley.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
He was the founding patron of the Certosa di Pavia, completing the Visconti Castle at Pavia begun by his father and furthering work on the Duomo of Milan. He captured a large territory of northern Italy and the Po valley. He threatened war with France in relation to the transfer of Genoa to French control as well as issues with his beloved daughter Valentina.

Geographic entities mentioned:
surface_form: Po valley
instance_of: Valley
countries: Italy
coordinates: lat: 45.330277777778
lon: 9.7988888888889
Second term. He was responding to the rapid population growth and suburban sprawl that the state was then experiencing, which was bringing with it strains on utilities and the rapid loss of arable land in the Willamette Valley. McCall's second-term agenda was focused on ameliorating these issues and protecting Oregonians' quality of life from overdevelopment.

Geographic entities mentioned:
surface_form: Willamette Valley
instance_of: Valley
countries: United States
coordinates: lat: 44.9
lon: -123.1
French Bar Canyon. French Bar Canyon is a canyon on the Fraser River in British Columbia, Canada, near Big Bar and Jesmond, and approximately 60 km upstream from Lillooet. The canyon is also the site of a June 2019 landslide that blocked the passage of spawning salmon.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: french bar canyon
instance_of: Valley
countries: Canada
coordinates: lat: 51.2167
lon: -122.15
French Bar Canyon. French Bar Canyon is a canyon on the Fraser River in British Columbia, Canada, near Big Bar and Jesmond, and approximately 60 km upstream from Lillooet. The canyon is also the site of a June 2019 landslide that blocked the passage of spawning salmon.

Geographic entities mentioned:
surface_form: french bar canyon
instance_of: Valley
countries: Canada
coordinates: lat: 51.2167
lon: -122.15
Wassergass, Pennsylvania. Wassergass is an unincorporated community in Northampton County, Pennsylvania. Wassergass is part of the Lehigh Valley metropolitan area, which had a population of 861,899 and was the 68th-most populous metropolitan area in the U.S. as of the 2020 census. History.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
To the south, down to the &quot;Mutterbergalm&quot; in the Stubai valley there are no summits. To the west, separated by the Alpeiner Ferner glacier, is the mightiest mountain of the group, the 3,496-metre-high Schrankogel. Bases and routes.

Geographic entities mentioned:
surface_form: Schrankogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0447
lon: 11.0992
surface_form: schrankogel
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0447
lon: 11.0992
Bases and routes. The route used by the first climbers to ascend the Ruderhofspitez in 1864 led from the &quot;Oberissalm&quot; in the Oberbergtal valley to the Alpeiner Ferner. There, because the Schrankogel appeared too difficult, they decided to make the Ruderhofspitze the goal of their trek. After over eight hours they reached the summit.

Geographic entities mentioned:
surface_form: Oberbergtal
instance_of: Valley
countries: Austria
coordinates: lat: 47.0983
lon: 11.2028
Ruderhofspitze. At the Ruderhofspitze is the fourth highest mountain in the Stubai Alps in Austria. It is part of the Alpein Mountains (&quot;Alpeiner Berge&quot;) and lies in the Austrian state of Tyrol. As a result of its topographic isolation and good all-round views it is one of the most visited mountains in the Stubai.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
Ruderhofspitze. At the Ruderhofspitze is the fourth highest mountain in the Stubai Alps in Austria. It is part of the Alpein Mountains (&quot;Alpeiner Berge&quot;) and lies in the Austrian state of Tyrol. As a result of its topographic isolation and good all-round views it is one of the most visited mountains in the Stubai.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
An almost two-kilometre-long arête, the &quot;Grawawand&quot;, runs away from the summit to the east. Less prominent ridges run south and northwestwards from the Ruderhofspitze. The peak was first ascended on 30 August 1864 by Karl Baedeker (the son of Karl Baedeker), Anton von Ruthner and mountain guides Pankraz Gleinser and Alois Tanzer. Location and surrounding area.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
The mountain is surrounded by glaciers. To the southeast, below the Grawawand is the &quot;Grawawandferner&quot; glacier, to the south the &quot;Ruderhofferner&quot;, to the west the expansive &quot;Alpeiner Ferner&quot; and to the north the &quot;Hochmoosferner&quot; runs right up to just under the summit cross on the Ruderhofspitze.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
After over eight hours they reached the summit. The present normal route, the easiest ascent, runs in a great arc over the Alpeiner Ferner as a high mountain tour to the Ruderhofspitze and should only be undertake with the right equipment and knowledge. The base for this route is the Franz Senn Hut situated to the northeast of the mountain at an elevation of 2,147 metres.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
The base for this route is the Franz Senn Hut situated to the northeast of the mountain at an elevation of 2,147 metres. From the hut the tour heads in a southwesterly direction along the &quot;Alpeiner Bach&quot; to the Alpeiner Ferner and then over the heavily crevassed glacier initially heading south and then east into the bay of the glacier below the Ruderhofspitze.

Geographic entities mentioned:
surface_form: ruderhofspitze
instance_of: Mountain
countries: Austria
coordinates: lat: 47.0403
lon: 11.1436
It is part of the Alpein Mountains (&quot;Alpeiner Berge&quot;) and lies in the Austrian state of Tyrol. As a result of its topographic isolation and good all-round views it is one of the most visited mountains in the Stubai. An almost two-kilometre-long arête, the &quot;Grawawand&quot;, runs away from the summit to the east.

Geographic entities mentioned:
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
Location and surrounding area. The Ruderhofspitze lies a good six kilometres as the crow flies west of &quot;Ranalt&quot; in the Stubai valley and about ten kilometres east of Gries, a village in the municipality of Längenfeld in the Sulztal valley. The mountain is surrounded by glaciers.

Geographic entities mentioned:
surface_form: stubai
instance_of: Valley
countries: Austria
coordinates: lat: 47.1667
lon: 11.3167
Fenneregg. The Fenneregg is a peak of the Rieserferner group on the border between Tyrol, Austria, and South Tyrol, Italy.

Geographic entities mentioned:
surface_form: fenneregg
instance_of: Mountain
countries: Austria
Italy
coordinates: lat: 46.933252
lon: 12.167834
Some of his own poems have been adapted into Gagauz pop songs, which were awarded prizes by the &quot;Bakannık Komiteti&quot;. Zanet is married, with two daughters. The elder, Anna Zanet, is a mountaineer who, in 2010, has planted the flag of Gagauzia on Mount Elbrus.

Geographic entities mentioned:
surface_form: Mount Elbrus
instance_of: Mountain
countries: Russia
Soviet Union
Russian Empire
coordinates: lat: 43.35254
lon: 42.437875
The Village of Waterloo is mostly in the Town of Waterloo, but the part south of the Cayuga-Seneca Canal of the village is in the Town of Fayette and a small area in the southeast of the village is in Town of Seneca Falls. Waterloo is east of Geneva and is located in between the two main Finger Lakes, Seneca Lake and Cayuga Lake. History.

Geographic entities mentioned:
surface_form: Cayuga Lake
instance_of: Lake
countries: United States
coordinates: lat: 42.68805555555556
lon: -76.70222222222222
Terjit () is an oasis (in the proper sense: a desert spring or other water source), 45km by road south of Atar and popular with tourists in Mauritania. It nestles in a gorge on the western edge of the Adrar plateau with the palm grove stretching a few hundred meters alongside a stream which emerges from a spring. &quot;Terjit&quot; is part of the commune of Maaden in the Aoujeft Department.

Geographic entities mentioned:
surface_form: Adrar plateau
instance_of: Plateau
countries: Mauritania
coordinates: lat: 20.405277777778
lon: -13.111111111111
Krumpendorf am Wörthersee. Krumpendorf am Wörthersee () is a municipality in Klagenfurt-Land District, in Carinthia, Austria. It is situated on the Wörthersee. Geography. Krumpendorf stretches along the northern shore of Wörthersee, Carinthia's largest bathing lake. The municipal area with is the smallest of all Carinthian municipalities. In the east, it borders on the state capital Klagenfurt.

Geographic entities mentioned:
surface_form: Wörthersee
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
Amlapura. Amlapura (;) formerly known as Kuta Negara Karangasem (;) is a town and the regency seat of the Karangasem Regency, Bali, Indonesia. It was renamed in 1963 after the eruption of Mount Agung. The population of the town in 2010 was 37.308. History.

Geographic entities mentioned:
surface_form: Mount Agung
instance_of: Mountain
countries: Indonesia
coordinates: lat: -8.3419444444444
lon: 115.50777777778
Before his pastoral work in central Africa, he traveled for four years throughout Germany, Austria and Switzerland, charged with raising funds for the work of his congregation. In 1897 he was sent to serve in the region of Lake Victoria, then part of German East Africa. Two years later he had to return home to Switzerland due to his health, where he remained until 1904, when he returned to Africa.

Geographic entities mentioned:
surface_form: Lake Victoria
instance_of: Lake
countries: Tanzania
Uganda
Kenya
coordinates: lat: -1
lon: 33
Al-Mansur tried to follow him, but at Biskra he was forced to stop, as the local guides warned him that the route followed by the Kharijite leader and his followers was extremely dangerous. After crossing the desert, Abu Yazid established himself in the Jabal Salat mountains, west of the Chott el Hodna lake.

Geographic entities mentioned:
surface_form: Chott el Hodna
instance_of: Lake
countries: Algeria
France
coordinates: lat: 35.44166667
lon: 4.76666667
Lake Wire. Lake Wire, an almost-round lake, has a surface area of. This lake is inside Lakeland, Florida, and the area surrounding it is completely urbanized. The lake was probably once oval shaped, but it appears it was partially filled on the southwest and northwest sides to allow parts of Lake Wire Drive to be built.

Geographic entities mentioned:
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.9344286
lon: -96.9790408
surface_form: round lake
instance_of: Body of water
countries: United States
coordinates: lat: 44.0648
lon: -75.1033
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 46.1508
lon: -86.7447
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.070277777778
lon: -74.584722222222
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 42.934604
lon: -73.7823057
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 27.9631
lon: -81.674
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.036388888889
lon: -97.773055555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 43.531388888889
lon: -75.180277777778
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.8685
lon: -93.4925
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 48.161666666667
lon: -116.63805555556
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6020431
lon: -122.4032555
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 41.837095
lon: -86.418541
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
surface_form: round lake
instance_of: Lake
countries: United States
coordinates: lat: 44.964444444444
lon: -96.827222222222
Lake Wire. Lake Wire, an almost-round lake, has a surface area of. This lake is inside Lakeland, Florida, and the area surrounding it is completely urbanized. The lake was probably once oval shaped, but it appears it was partially filled on the southwest and northwest sides to allow parts of Lake Wire Drive to be built.

Geographic entities mentioned:
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
This lake is inside Lakeland, Florida, and the area surrounding it is completely urbanized. The lake was probably once oval shaped, but it appears it was partially filled on the southwest and northwest sides to allow parts of Lake Wire Drive to be built. It is almost completely surrounded by Lake Wire Drive, except for a distance of about on the northeast.

Geographic entities mentioned:
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
The lake was probably once oval shaped, but it appears it was partially filled on the southwest and northwest sides to allow parts of Lake Wire Drive to be built. It is almost completely surrounded by Lake Wire Drive, except for a distance of about on the northeast. The lake is completely surrounded by a public sidewalk.

Geographic entities mentioned:
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
It is almost completely surrounded by Lake Wire Drive, except for a distance of about on the northeast. The lake is completely surrounded by a public sidewalk. Lake Wire provides public access along its entire shore, via the sidewalk that surrounds it. The public is allowed to access the shore daily from dawn to dusk.

Geographic entities mentioned:
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
The public is allowed to access the shore daily from dawn to dusk. There are no boat ramps or swimming areas along the lake shore, but it can be fished from the shore. The Take Me Fishing website says Lake Wire contains largemouth bass and bluegill. Lake Wire was so named for the fact the lake contained poles carrying telegraph wires.

Geographic entities mentioned:
surface_form: lake wire
instance_of: Lake
countries: United States
coordinates: lat: 28.0468
lon: -81.9608
The town is located in the southwestern part of Worcester County, along the Quaboag River. The river is bordered by swampy lands, and several areas around it are protected as wildlife management areas. Along the East Brookfield border lie two large ponds which are part of the river, Quaboag Pond to the north and Quacumquasit Pond to the south, extending into Sturbridge.

Geographic entities mentioned:
surface_form: Quaboag Pond
instance_of: Lake
countries: United States
coordinates: lat: 42.187222222222
lon: -72.068055555556
New York State Route 86 runs through the center of the CDP, leading southwest to Lake Placid and east to Jay. New York State Route 431 leads west from NY 86 near the center of Wilmington nearly to the summit of Whiteface Mountain. According to the United States Census Bureau, the Wilmington CDP has a total area of, of which is land and, or 1.05%, is water. Education.

Geographic entities mentioned:
surface_form: Whiteface Mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.3658
lon: -73.9028
Lake Pressegg. Lake Pressegg (,) is a lake in Carinthia, Austria. It is located in a glacial valley within the Gailtal Alps, a mountain range of the Southern Limestone Alps, east of Hermagor. With an average depth of, the water body of the semi-circular lake is relatively flat.

Geographic entities mentioned:
surface_form: lake pressegg
instance_of: Lake
countries: Austria
coordinates: lat: 46.626111111111
lon: 13.441388888889
It is one of several locations that is considered to be the birthplace of Genghis Khan (Temüjin), in the year 1162 CE, according to &quot;The Secret History of the Mongols&quot;. It is located near the sacred mountain Burkhan Khaldun and the Onon and Kherlen Rivers, close to Ulaanbaatar.

Geographic entities mentioned:
surface_form: Burkhan Khaldun
instance_of: Mountain
countries: Mongolia
coordinates: lat: 48.783333333333
lon: 109.16666666667
In the laborious excavation of the temple of Ipsambul, Beechey took his share; he also copied the paintings, in the king's tombs in the valley of Biban-el-Muluk, which had lately been opened by Belzoni. In common with Salt, Beechey had much to endure from Belzoni's suspicious and jealous nature (&quot;Life and Correspondence of Henry Salt&quot;, ed.

Geographic entities mentioned:
surface_form: Biban-el-Muluk
instance_of: Valley
countries: Egypt
coordinates: lat: 25.74025
lon: 32.602358