Sarmila/GeoWiki-Features huggingface dataset:
In 1998, Pambamarca was placed on the tentative List of UNESCO World Heritage Sites. History. The fortifications originated with the Inca Empire who conquered Ecuador easily, and established themselves at Quito. Noting that the local indigenous community settled in Pambamarca were docile, the Incas thought that they could move in and occupy the territories outside Quito.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
But they faced serious resistance, and the war lasted 17 years before the Incas could finally conquer the Ecuadorians in the 1500s, with the fall of the fortresses. Following this, the Incas built many fortresses and lived in them. Among the provinces to the north of Quito the pre-Hispanic fortresses are concentrated in the mountain range of Pambamarca.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
This aspect of the legend is to be confirmed by further explorations by archeologists examining the areas. Geography. Jorge Juan y Santacilia and Louis Godin, on their voyage through South America to fix signals for surveys, arrived at the &quot;desert of Pambamarca&quot; in early September 1737. A mountain of medium height in this desert is also named Pambarmarca.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
A mountain of medium height in this desert is also named Pambarmarca. One of the largest group of fortresses (on the hill which is called locally as &quot;pukaras&quot;) seen in Ecuador was the Pambamarca Group located along a ridge running in a north–south direction.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
One of the largest group of fortresses (on the hill which is called locally as &quot;pukaras&quot;) seen in Ecuador was the Pambamarca Group located along a ridge running in a north–south direction. These military structures provided security to Quito fortress and other forts such as Jambimachi, Pambamarca, Pachha, Campana, Olachan Tablarumi, Achupallas, Guachala and Bravo. Ulloa's halo.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
Ulloa's halo. Antonio de Ulloa and another member of the French Geodesic Mission to the Equator, Pierre Bouguer, reported that while walking near the summit of the Pambamarca mountain they saw their shadows projected on a lower-lying cloud, with a circular &quot;halo or glory&quot; around the shadow of the observer's head.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
Culture. The Pambamarca Fortress Complex is a large installation of many Inca &quot;pucarás&quot;, located on the peaks and ridges of the extinct Pambamarca stratovolcano. During the current research by the Pambamarca Archaeological Project, the team uncovered pre-Inca fortresses at the base of Pambamarca.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
Culture. The Pambamarca Fortress Complex is a large installation of many Inca &quot;pucarás&quot;, located on the peaks and ridges of the extinct Pambamarca stratovolcano. During the current research by the Pambamarca Archaeological Project, the team uncovered pre-Inca fortresses at the base of Pambamarca.

Geographic entities mentioned:
surface_form: pambamarca
instance_of: Mountain
countries: Ecuador
coordinates: lat: -0.066666666666667
lon: -78.2
Besides state reforms in the 1960s, Chilean communists and socialists engaged in the formation of agriculture syndicates through La Frontera and semi-arid Norte Chico. The Christian Democrats did the same around Valparaíso and Aconcagua Valley and in the Central Valley locations of Curicó, Linares and Talca. Unidad Popular years.

Geographic entities mentioned:
surface_form: Central Valley
instance_of: Valley
countries: Chile
coordinates: lat: -35.5
lon: -71.5
Loch Eigheach is part of the Tummel hydro-electric power scheme. The Gaur Dam was placed at its eastern end, enlarging the loch, in the 1950s. Geography. Loch Eigheach lies on the River Gaur and is located between Loch Laidon in the west and Loch Rannoch in the east. On its northern shore, the river Allt Eigheach flows into the loch. The main inflow to the loch in the east is the Garbh Ghaoir.

Geographic entities mentioned:
surface_form: Loch Laidon
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.65666667
lon: -4.63305556
surface_form: Loch Rannoch
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.688299
lon: -4.30386
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
Loch Eigheach. Loch Eigheach is a large upland dammed freshwater loch in the Scottish Highlands. It is located in Rannoch Moor in the Council Area of Perth and Kinross. The undisturbed Loch Eigheach was much smaller. Dam. Loch Eigheach is part of the Tummel hydro-electric power scheme. The Gaur Dam was placed at its eastern end, enlarging the loch, in the 1950s. Geography.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
It is located in Rannoch Moor in the Council Area of Perth and Kinross. The undisturbed Loch Eigheach was much smaller. Dam. Loch Eigheach is part of the Tummel hydro-electric power scheme. The Gaur Dam was placed at its eastern end, enlarging the loch, in the 1950s. Geography. Loch Eigheach lies on the River Gaur and is located between Loch Laidon in the west and Loch Rannoch in the east.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
On its northern shore, the river Allt Eigheach flows into the loch. The main inflow to the loch in the east is the Garbh Ghaoir. Loch Eigheach is traversed by the River Gaur that flows out of Loch Eigheach in the west. The water leaving Loch Eigheach across the River Gaur first flows through a hydroelectric power station before being returned to the riverbed.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
The main inflow to the loch in the east is the Garbh Ghaoir. Loch Eigheach is traversed by the River Gaur that flows out of Loch Eigheach in the west. The water leaving Loch Eigheach across the River Gaur first flows through a hydroelectric power station before being returned to the riverbed. The shores of Loch Eigheach are completely uninhabited.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
Loch Eigheach is traversed by the River Gaur that flows out of Loch Eigheach in the west. The water leaving Loch Eigheach across the River Gaur first flows through a hydroelectric power station before being returned to the riverbed. The shores of Loch Eigheach are completely uninhabited. Parts of the north shore and the dam wall are accessed by the B846.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
The water leaving Loch Eigheach across the River Gaur first flows through a hydroelectric power station before being returned to the riverbed. The shores of Loch Eigheach are completely uninhabited. Parts of the north shore and the dam wall are accessed by the B846. All other shorelines are not accessible by car. Loch Eigheach is a fishing area where mainly perch are caught.

Geographic entities mentioned:
surface_form: loch eigheach
instance_of: Lake
countries: United Kingdom
coordinates: lat: 56.678898
lon: -4.533959
Despite the borough's small size, its property was assessed at over $1.28 billion in 2019. History. Before Long Beach Island was developed, its northern area, from the Barnegat Inlet to the Great Swamp (now Surf City), was covered with Atlantic white cedar (chamaecyparis thyoides). Early inhabitants of the area harvested salt hay (spartina patens) and seaweed to make a living.

Geographic entities mentioned:
surface_form: Barnegat Inlet
instance_of: Landform
countries: United States
coordinates: lat: 39.76666667
lon: -74.10333333
Srednja Vas pri Kamniku. Srednja Vas pri Kamniku (;,) is a settlement on the right bank of the Nevljica River at the Kamnik end of the Tuhinj Valley in the Upper Carniola region of Slovenia. Name. The name of the settlement was changed from &quot;Srednja vas&quot; to &quot;Srednja vas pri Kamniku&quot; in 1955. In the past the German name was &quot;Mitterdorf&quot;.

Geographic entities mentioned:
surface_form: Tuhinj Valley
instance_of: Valley
countries: Slovenia
coordinates: lat: 46.221413888889
lon: 14.775925
One was Garo Hills in the ancient Kamrupa kingdom and the other was Dhakuakhana in the ancient Chutia kingdom. Muga silk. Muga silk is the product of the silkworm &quot;Antheraea assamensis&quot; endemic to Assam. The larvae of these moths feed on som (&quot;Machilus bombycina&quot;) and sualu (&quot;Litsaea polyantha&quot;) leaves.

Geographic entities mentioned:
surface_form: Garo Hills
instance_of: Mountain
countries: India
coordinates: lat: 25.5
lon: 90.33333333333333
Precipitation runoff from the mountain drains into Pelly Creek, a tributary of the Ingenika River. Sir John Pelly (1777–1852) served as Governor of Hudson's Bay Company for three decades, and his name is attached to many geographic features in Canada, including but not limited to Pelly River, Pelly Mountains, Pelly Island, Pelly Bay, Mount Pelly, and Fort Pelly.

Geographic entities mentioned:
surface_form: Pelly Bay
instance_of: Body of water
countries: Canada
coordinates: lat: 68.8833
lon: -90.0833
surface_form: island
instance_of: Lake
countries: Canada
coordinates: lat: 53.783333333333
lon: -94.666666666667
surface_form: mount pelly
instance_of: Mountain
countries: Canada
coordinates: lat: 69.1778
lon: -104.722
Pelly Peak. Pelly Peak, is a mountain summit in the Russel Range of the Omineca Mountains in northern British Columbia, Canada. The mountain is situated west of the head of Finlay Reach of Williston Lake, and a remote south of Fort Ware in the Cassiar Land District. It rises above the south shore of Pelly Lake. Its nearest higher peak is Barrier Peak, to the east.

Geographic entities mentioned:
surface_form: columbia
instance_of: Mountain
countries: Canada
coordinates: lat: 52.1475
lon: -117.44055555555556
surface_form: pelly peak
instance_of: Mountain
countries: Canada
coordinates: lat: 56.7689
lon: -125.2883
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Pelly Peak. Pelly Peak, is a mountain summit in the Russel Range of the Omineca Mountains in northern British Columbia, Canada. The mountain is situated west of the head of Finlay Reach of Williston Lake, and a remote south of Fort Ware in the Cassiar Land District. It rises above the south shore of Pelly Lake. Its nearest higher peak is Barrier Peak, to the east.

Geographic entities mentioned:
surface_form: pelly peak
instance_of: Mountain
countries: Canada
coordinates: lat: 56.7689
lon: -125.2883
The peak's name was officially adopted June 4, 1953, by the Geographical Names Board of Canada. Based on the Köppen climate classification, Pelly Peak is located in a subarctic climate zone with cold, snowy winters, and mild summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C.

Geographic entities mentioned:
surface_form: pelly peak
instance_of: Mountain
countries: Canada
coordinates: lat: 56.7689
lon: -125.2883
Pelly Peak. Pelly Peak, is a mountain summit in the Russel Range of the Omineca Mountains in northern British Columbia, Canada. The mountain is situated west of the head of Finlay Reach of Williston Lake, and a remote south of Fort Ware in the Cassiar Land District. It rises above the south shore of Pelly Lake. Its nearest higher peak is Barrier Peak, to the east.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
The mountain is situated west of the head of Finlay Reach of Williston Lake, and a remote south of Fort Ware in the Cassiar Land District. It rises above the south shore of Pelly Lake. Its nearest higher peak is Barrier Peak, to the east. Precipitation runoff from the mountain drains into Pelly Creek, a tributary of the Ingenika River.

Geographic entities mentioned:
surface_form: mountain
instance_of: Mountain
countries: Canada
coordinates: lat: 51.4677778
lon: -116.1416667
Owned by Broadway Media, the station's studios are located in Downtown Salt Lake City and its transmitter site is located southwest of the city on Farnsworth Peak in the Oquirrh Mountains. KFMC (1966–1976). KOVO, Inc., received the construction permit for a radio station on 96.1 MHz in Provo on May 9, 1966. The new FM outlet took the call letters KFMC and signed on February 14, 1968.

Geographic entities mentioned:
surface_form: Farnsworth Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.659783333333
lon: -112.20234722222
Since fall 1995, X96 has hosted an annual all-day music festival called the Big Ass Show (BASh) featuring nationally touring alternative and punk bands, as well as providing a stage for local bands. In 1996, X96 underwent a major technical overhaul, moving to 96.3 MHz from a transmitter on Farnsworth Peak, increasing its coverage area (particularly in Utah County).

Geographic entities mentioned:
surface_form: Farnsworth Peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.659783333333
lon: -112.20234722222
It was founded in 2012, and has subsequently grown to export worldwide. Company history. The brewery began life on a farm in Royal Deeside, Aberdeenshire with a student loan. The first beer produced was Armageddon, which the company claimed in press releases was the world's strongest beer at 65% alcohol by volume (ABV).

Geographic entities mentioned:
surface_form: Royal Deeside
instance_of: Valley
countries: United Kingdom
History. Linguist Ives Goddard has determined that the Unalachtigo had their origins around the Lehigh Valley of Pennsylvania, and adjacent portions of New Jersey. They spoke a Northern Unami or Southern Unami dialect of Lënape. Recent events.

Geographic entities mentioned:
surface_form: Lehigh Valley
instance_of: Valley
countries: United States
coordinates: lat: 40.7
lon: -75.5
Mountaineering. Inglis Clark was a keen hillwalker who discovered rock climbing in 1897. With a natural aptitude for climbing difficult routes, from 1897 to 1904, Inglis Clark was part of six first ascents on Ben Nevis. She was proud to be a pioneer and was keen to encourage other women to take up mountaineering.

Geographic entities mentioned:
surface_form: Ben Nevis
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 56.796891
lon: -5.003675
Dere, Iraq. Dere () is a village in Duhok Governorate in Kurdistan Region, Iraq. It is located in the Sapna valley in Amedi District. Dere is the sister village of Komane. In the village, there is a church of Mar Abdisho. Etymology.

Geographic entities mentioned:
surface_form: Sapna valley
instance_of: Valley
countries: Iraq
coordinates: lat: 37.083333333333336
lon: 43.5
In Civilization V, she speaks Phoenician, with a modern Israeli accent. In 2019, Dido was made the leader of Phoenicia in ', with Tyre as its capital and Carthage as an available name for subsequent cities. In honor of Dido, the asteroid 209 Dido, discovered in 1879, was named after her. Another dedication of Queen Dido is the Mount Dido in Antarctica.

Geographic entities mentioned:
surface_form: Mount Dido
instance_of: Mountain
coordinates: lat: -77.5
lon: 160.95
1969 European Rowing Championships. The 1969 European Rowing Championships were rowing championships held on the Wörthersee in the Austrian city of Klagenfurt. This edition of the European Rowing Championships was held from 5 to 7 September for women, and a few days later for men.

Geographic entities mentioned:
surface_form: Wörthersee
instance_of: Lake
countries: Austria
coordinates: lat: 46.625
lon: 14.15
An innovation was that petite finals were held to determine places 7 to 12. Background. At its congress held in conjunction with the 1967 European Rowing Championships in Vichy, the International Rowing Federation (FISA) had decided that the 1969 Championships would be held on the Lake of Banyoles in Spain. Circumstances changed and the event moved to Austria.

Geographic entities mentioned:
surface_form: Lake of Banyoles
instance_of: Lake
countries: Spain
coordinates: lat: 42.125277777778
lon: 2.7552777777778
Table Mountain (Tuolumne County, California). Table Mountain is a narrow, -long, sinuous, flat-topped ridge separated by erosional saddles into a series of mesas that extend from Lake Tulloch to just west of Columbia, California in Tuolumne County, California. It is just over in elevation at its southern end and just over in elevation at its northern end.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain (tuolumne county, california)
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Table Mountain (Tuolumne County, California). Table Mountain is a narrow, -long, sinuous, flat-topped ridge separated by erosional saddles into a series of mesas that extend from Lake Tulloch to just west of Columbia, California in Tuolumne County, California. It is just over in elevation at its southern end and just over in elevation at its northern end.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
These lava flows filled the Cataract Channel and overflowed into parts of its floodplain. Before the creation of New Melones Lake and Lake Tulloch, the modern Stanislaus River occupied a deep gorge west of Table Mountain. Beneath the Table Mountain Latite and forming the bulk of Table Mountain are andesitic mudflows and conglomerates of the Mehrten Formation.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Beneath the Table Mountain Latite and forming the bulk of Table Mountain are andesitic mudflows and conglomerates of the Mehrten Formation. They consist predominantly of debris flow deposits (interpreted as volcanic lahars), and fluvial conglomerates, lithic sandstones, and siltstones deposited by rivers which flowed westward across the Table Mountain region.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
the Relief Peak Formation, Stanislaus Group, etc., based on their age and source volcanic center. Lying buried beneath the volcanoclastic sediments of the Mehrten and Valley Springs formations within the Table Mountain region are paleovalleys cut into pre-Cenozoic bedrock. These paleovalleys are filled with Eocene, prevolcanic, quartz-rich, gravelly, gold-bearing stream deposits.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
As a result, the prevolcanic unconformity lying at the base of the Mehrten and Valley Springs formations has been exhumed and is now exposed as the modern rolling topography adjacent to Table Mountain. Ecology. A variety of flora and fauna are found on Table Mountain.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
Ecology. A variety of flora and fauna are found on Table Mountain. In the spring, many wildflowers can be found atop the mountain including several species of lupine and the yellow mariposa lily, &quot;Calochortus luteus&quot;. Vernal pools form on the flat top after heavy winter and spring rains, providing habitat for many uncommon plant and animal species.

Geographic entities mentioned:
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.59807864926865
lon: -121.55626585419016
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 35.9061
lon: -120.276
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.847774
lon: -121.713574
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.2958046
lon: -110.0553458
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 40.0888
lon: -111.822
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.742222222222
lon: -112.46194444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.541388888889
lon: -118.29944444444
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 43.7467
lon: -110.852
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 45.6918989
lon: -121.9826782
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 36.6604
lon: -118.474
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 37.983
lon: -120.434
surface_form: table mountain
instance_of: Mountain
countries: United States
coordinates: lat: 41.9587
lon: -74.4048
It is just over in elevation at its southern end and just over in elevation at its northern end. Its flat top is part of a stack of multiple -long lava flows that have been eroded to form a series of mesas that extend from Knights Ferry to Sonora, California. Its crest varies in width from a narrow ridge to over wide. It parallels the adjacent Stanislaus River. Geology.

Geographic entities mentioned:
surface_form: flat top
instance_of: Mountain
countries: United States
coordinates: lat: 34.9511
lon: -83.3156
Längsee (Kärnten). Längsee is a lake of Carinthia, Austria. It is the name affix of the town Sankt Georgen am Längsee.

Geographic entities mentioned:
surface_form: längsee (kärnten)
instance_of: Lake
countries: Austria
coordinates: lat: 46.7894
lon: 14.4242
surface_form: längsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.5994
lon: 12.1547
Längsee (Kärnten). Längsee is a lake of Carinthia, Austria. It is the name affix of the town Sankt Georgen am Längsee.

Geographic entities mentioned:
surface_form: längsee
instance_of: Lake
countries: Austria
coordinates: lat: 46.7894
lon: 14.4242
surface_form: längsee
instance_of: Lake
countries: Austria
coordinates: lat: 47.5994
lon: 12.1547
Both were established in 1994. History. The history of Assam University is the history of people's struggle in Barak Valley. It is one of the subsequent outcomes of the Bengali Language Movement in the southern part of Assam. The Shaheed Minar built near the front gate of the university commemorates the sacrifices of the martyrs during the historical language movement in 1961. Main campus.

Geographic entities mentioned:
surface_form: Barak Valley
instance_of: Valley
countries: India
coordinates: lat: 24.833333333333332
lon: 92.8
Lac de Viremont. Lac de Viremont is a small lake near the village of Viremont, at Légna in the Jura department of France. It lies at a height of 656 m, and offers 2ha of waters. It lies amidst a larger fen area and was erected as a ZNIEFF.

Geographic entities mentioned:
surface_form: lac de viremont
instance_of: Lake
countries: France
coordinates: lat: 46.426388888889
lon: 5.6277777777778
Sport. Deakin Reserve is the main sports venue in the Goulburn Valley and is a cricket and Australian Rules Football sports oval in Shepparton, Victoria, Australia. Deakin Reserve hosted the long running Shepparton Sports Carnival between 1906 and 1967, which featured – athletics, cycling, wood chopping, fireworks, bands and dancing.

Geographic entities mentioned:
surface_form: Goulburn Valley
instance_of: Valley
countries: Australia
coordinates: lat: -36.3831
lon: 145.399
Discovery and naming. The type species, &quot;Ferganocephale adenticulatum&quot;, was first described by Averianov, Martin, and Bakirov in 2005, and is based solely on teeth from the Balabansai Svita in Fergana Valley, Kyrgyzstan, dating to the Callovian. The holotype is ZIN PH 34/42, an adult unworn tooth. The type species is &quot;Ferganocephale adenticulatum&quot;.

Geographic entities mentioned:
surface_form: Fergana Valley
instance_of: Valley
countries: Kyrgyzstan
Uzbekistan
Tajikistan
coordinates: lat: 40.900833333333
lon: 71.757777777778
Posionjärvi. Posionjärvi is a medium-sized lake in the Koutajoki main catchment area. It is located in Posio municipality, in the region Lapland in Finland. There are 187 islands in the lake.

Geographic entities mentioned:
surface_form: posionjärvi
instance_of: Lake
countries: Finland
coordinates: lat: 66.13333333
lon: 28.03333333
Lake Smerdyachye. Lake Smerdyachye (Озеро Смердячье - &quot;lake which smells bad&quot;) is a small lake in Moscow Oblast of Russia near Shatura north from the nearest village Bakhscheevo (Бакшеево). Lake. The lake is situated in a pine forest. It is round (diameter) and appeared thousands years ago as a meteor crater. Depth is. Until early 2000s it was thought it is of karst origin.

Geographic entities mentioned:
surface_form: lake smerdyachye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.735
lon: 39.822222222222
Lake Smerdyachye. Lake Smerdyachye (Озеро Смердячье - &quot;lake which smells bad&quot;) is a small lake in Moscow Oblast of Russia near Shatura north from the nearest village Bakhscheevo (Бакшеево). Lake. The lake is situated in a pine forest. It is round (diameter) and appeared thousands years ago as a meteor crater. Depth is. Until early 2000s it was thought it is of karst origin.

Geographic entities mentioned:
surface_form: lake smerdyachye
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.735
lon: 39.822222222222
surface_form: смердячье
instance_of: Lake
countries: Russia
Russian Empire
Soviet Union
coordinates: lat: 55.735
lon: 39.822222222222
Pico Matias Simão. Miradouro do Pico Matias Simão is a monument in the Azores. It is located in Angra do Heroísmo, on the island of Terceira.

Geographic entities mentioned:
surface_form: pico
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.468611111111
lon: -28.399166666667
surface_form: pico matias simão
instance_of: Mountain
countries: Portugal
coordinates: lat: 38.799283333333335
lon: -27.29096388888889
Billy Goat Hill, or Akeyulerre, (in Arrernte) is located in Alice Springs (Mparntwe) in the Northern Territory of Australia and, together with the nearby ANZAC Hill (Atnelkentyarliweke), has important Dreaming associations include two sisters, alongside uninitiated boys, who were travelling north and were engaged in flirtatious and humorous behaviour these sites; further north these interactions became violent.

Geographic entities mentioned:
surface_form: ANZAC Hill (Atnelkentyarliweke)
instance_of: Mountain
countries: Australia
coordinates: lat: -23.69421
lon: 133.88191
They have a dark iris, a stubby black bill, and blackish legs and feet. Distribution and habitat. The white-bearded flycatcher is found from Arauca and Vichada departments in northeastern Colombia northeast across northern Venezuela to Delta Amacuro state. It is a bird of the Llanos, a mostly open landscape of grassland with scattered trees, small woodlands, gallery forest, and ranches.

Geographic entities mentioned:
surface_form: Delta Amacuro
instance_of: Body of water
countries: Venezuela
coordinates: lat: 8.7
lon: -61.15
In the fifth reading, at Mount Hor, God told Moses and Aaron: &quot;Let Aaron be gathered to his kin: he is not to enter the land that I have assigned to the Israelite people, because you disobeyed my command about the waters of Meribah.&quot; Moses took Aaron and his son Eleazar up on Mount Hor, and there he stripped Aaron of his vestments and put them on Eleazar, and Aaron died there.

Geographic entities mentioned:
surface_form: Mount Hor
instance_of: Mountain
countries: Jordan
coordinates: lat: 30.31677704842186
lon: 35.40653791009069
They made a causeway from the Temple Mount to the Mount of Olives, arches above arches, each arch placed directly above each pier of the arch below, as a protection against a grave in the depths, on which the priest who was to burn the cow, the cow itself, and all who aided in its preparation went forth to the Mount of Olives.

Geographic entities mentioned:
surface_form: Mount of Olives
instance_of: Mountain
countries: Israel
coordinates: lat: 31.777946
lon: 35.245686
Lac des Hermines. Lac des Hermines is an artificial lake near Super-Besse, in Puy-de-Dôme, France. At an elevation of 1350 m, its surface area is 0.14 km2.

Geographic entities mentioned:
surface_form: lac des hermines
instance_of: Lake
countries: France
coordinates: lat: 45.5075
lon: 2.8563888888889
Lac des Hermines. Lac des Hermines is an artificial lake near Super-Besse, in Puy-de-Dôme, France. At an elevation of 1350 m, its surface area is 0.14 km2.

Geographic entities mentioned:
surface_form: lac des hermines
instance_of: Lake
countries: France
coordinates: lat: 45.5075
lon: 2.8563888888889
surface_form: puy-de-dôme
instance_of: Mountain
countries: France
coordinates: lat: 45.772
lon: 2.9624
Pine Cobble Mountain. Pine Cobble Mountain, located in Williamstown, Massachusetts, is a sub-summit of East Mountain in the Clarksburg State Forest. This outcropping is best known as a popular hiking destination, where an outlook encompasses panoramic views of Williamstown, the Mount Greylock Range, and North Adams. The USGS benchmark at the summit is 577 meters or 1,894 feet above sea level.

Geographic entities mentioned:
surface_form: Mount Greylock
instance_of: Mountain
countries: United States
coordinates: lat: 42.6375
lon: -73.166666666667
surface_form: adams
instance_of: Mountain
countries: United States
coordinates: lat: 46.202411111111
lon: -121.49089444444
Recreation. The Pine Cobble Trail is also an approach to the Appalachian Trail, which is intercepted 0.5 miles beyond the Pine Cobble outcropping. It also serves as an access to Vermont's Long Trail, which begins at the Massachusetts/Vermont border where these two converged trails enter the Green Mountain National Forest.

Geographic entities mentioned:
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.9822
lon: -105.302
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 48.291666666667
lon: -121.23861111111
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.3053
lon: -105.3
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.5175
lon: -121.67305555556
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 47.563333333333
lon: -122.80694444444
surface_form: green mountain
instance_of: Mountain
countries: United States
coordinates: lat: 39.700833333333
lon: -105.17805555556
Pine Cobble Mountain. Pine Cobble Mountain, located in Williamstown, Massachusetts, is a sub-summit of East Mountain in the Clarksburg State Forest. This outcropping is best known as a popular hiking destination, where an outlook encompasses panoramic views of Williamstown, the Mount Greylock Range, and North Adams. The USGS benchmark at the summit is 577 meters or 1,894 feet above sea level.

Geographic entities mentioned:
surface_form: east mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.2031
lon: -72.6603
surface_form: east mountain
instance_of: Mountain
countries: United States
coordinates: lat: 44.6647
lon: -71.7702
surface_form: pine cobble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.7209
lon: -73.1662
Pine Cobble Mountain. Pine Cobble Mountain, located in Williamstown, Massachusetts, is a sub-summit of East Mountain in the Clarksburg State Forest. This outcropping is best known as a popular hiking destination, where an outlook encompasses panoramic views of Williamstown, the Mount Greylock Range, and North Adams. The USGS benchmark at the summit is 577 meters or 1,894 feet above sea level.

Geographic entities mentioned:
surface_form: pine cobble mountain
instance_of: Mountain
countries: United States
coordinates: lat: 42.7209
lon: -73.1662
Eina. Eina is a village in Vestre Toten Municipality in Innlandet county, Norway. The village is located along the Gjøvikbanen railway line, between the villages of Jaren and Raufoss. The village of Eina is located south of the municipal centre of Raufoss, on the north shore of the lake Einavatnet. The river Hunnselva runs north through the village from the lake Einavatnet to the large lake Mjøsa.

Geographic entities mentioned:
surface_form: Einavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.579722222222
lon: 10.634444444444
The village is located along the Gjøvikbanen railway line, between the villages of Jaren and Raufoss. The village of Eina is located south of the municipal centre of Raufoss, on the north shore of the lake Einavatnet. The river Hunnselva runs north through the village from the lake Einavatnet to the large lake Mjøsa. The village has a population (2021) of 704 and a population density of.

Geographic entities mentioned:
surface_form: Einavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.579722222222
lon: 10.634444444444
surface_form: Mjøsa
instance_of: Lake
countries: Norway
coordinates: lat: 60.666666666667
lon: 11
This was due to the Gjøvikbanen railway line being built, which brought passengers and freight to and through the village. In 1902, the local railroad station opened and it was named Eina, after the nearby lake Einavatnet. In 1908, the village of Eina and its surroundings became a municipality of its own when Vestre Toten split into three municipalities: Eina, Kolbu and Vestre Toten.

Geographic entities mentioned:
surface_form: Einavatnet
instance_of: Lake
countries: Norway
coordinates: lat: 60.579722222222
lon: 10.634444444444
Copadichromis nkatae. &quot;Copadichromis nkatae&quot; is a species of haplochromine cichlid which is endemic to Lake Malawi. This species can be found over both rocky and sandy areas where it feeds on zooplankton, as well as phytoplankton. There have been no verified records of this species since it was described in 1960.

Geographic entities mentioned:
surface_form: Lake Malawi
instance_of: Lake
countries: Malawi
Mozambique
Tanzania
coordinates: lat: -12.183333333333
lon: 34.366666666667
Chitral (disambiguation). Chitral is a town in the North West Frontier Province of Pakistan.

Geographic entities mentioned:
surface_form: Chitral
instance_of: Valley
countries: Pakistan
coordinates: lat: 35.85111111111111
lon: 71.78888888888889
Heinz Schön presents the combined death toll as 9,343. Sinking of MV &quot;Wilhelm Gustloff&quot;. was a German cruise liner laid down on 4 August 1936. Intended to be christened Adolf Hitler, she was eventually named after Wilhelm Gustloff, the assassinated leader of Nazi Party Foreign Organisation in Switzerland. She was launched into the Elbe on 5 May 1937.

Geographic entities mentioned:
surface_form: Elbe
instance_of: Watercourse
countries: Czech Republic
Germany
coordinates: lat: 53.922222222222224
lon: 8.722222222222221
In 1923, Yogananda's younger brother, Bishnu Charan Ghosh, founded the Ghosh College of Yoga and Physical Culture in Calcutta. Tirumalai Krishnamacharya (1888–1989), &quot;the father of modern yoga&quot;, claimed to have spent seven years with one of the few masters of Haṭha yoga then living, Ramamohana Brahmachari, at Lake Manasarovar in Tibet, from 1912 to 1918.

Geographic entities mentioned:
surface_form: Lake Manasarovar
instance_of: Lake
countries: People's Republic of China
coordinates: lat: 30.666666666667
lon: 81.5
Trolla (mountain). The ridge continues northwards to the peak Skarfjellet ().

Geographic entities mentioned:
surface_form: Skarfjellet
instance_of: Mountain
countries: Norway
coordinates: lat: 62.703333333333
lon: 8.7277777777778
Trolla (mountain). The ridge continues northwards to the peak Skarfjellet ().

Geographic entities mentioned:
surface_form: trolla
instance_of: Mountain
countries: Norway
coordinates: lat: 62.68586
lon: 8.73197
Tangahoe River. The Tangahoe River is a river of the Taranaki Region of New Zealand's North Island. It flows generally southwest from its origins in hill country to the east of Lake Rotorangi, reaching the Tasman Sea in the South Taranaki Bight southeast of Hāwera. Name.

Geographic entities mentioned:
surface_form: Lake Rotorangi
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.5018
lon: 174.5091
is also consented for irrigation. The dairy removes silt from the water with plastic microbeads. Tunnel. Tangahoe Valley Tunnel runs under the ridge separating Pukekino Rd (leading to Lake Rotorangi) from the Tangahoe Valley. The tunnel was built in 1928. Digging was from both ends and didn't quite meet in the middle, hence a variation in the roof height in the centre.

Geographic entities mentioned:
surface_form: Lake Rotorangi
instance_of: Lake
countries: New Zealand
coordinates: lat: -39.5018
lon: 174.5091
It is located in the La Paz Department, Franz Tamayo Province, Pelechuco Municipality, near the Peruvian border. Q'umir Pata lies southeast of the mountains Surapata and Kulli Pata and south of Chawpi Urqu.

Geographic entities mentioned:
surface_form: Kulli Pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.6108
lon: -69.1978
surface_form: chawpi urqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.52138889
lon: -65.88111111
surface_form: chawpi urqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -19.3975
lon: -65.5975
surface_form: kulli pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.6108
lon: -69.1978
surface_form: chawpi urqu
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.6083
lon: -69.1756
Q'umir Pata. Q'umir Pata (Quechua, &quot;q'umir&quot; green, &quot;pata&quot; elevated place / above, at the top / edge, bank (of a river), shore, &quot;green elevated place&quot; or &quot;green shore&quot;, also spelled &quot;Khomerpata&quot;) is a mountain in the north of the Apolobamba mountain range in Bolivia, about high.

Geographic entities mentioned:
surface_form: q'umir pata
instance_of: Mountain
countries: Bolivia
coordinates: lat: -14.6294
lon: -69.1761
Grove Field. Grove Field is a public airport located three miles (5 km) north of the central business district of Camas, a city in Clark County, Washington, United States. It is located near Lacamas Lake which has a seaplane base. Due to the closing of Evergreen Field, many aircraft have moved to Grove Field. Facilities and aircraft.

Geographic entities mentioned:
surface_form: Lacamas Lake
instance_of: Lake
countries: United States
coordinates: lat: 45.6165669
lon: -122.4252954
This would give the city a steamship connection through the Gulf of St. Lawrence to Canada East, as well as allowing coal and other goods to avoid the circuitous and hazardous transit around Nova Scotia. Construction started in 1853, heading northeast from Saint John up the Kennebecasis River valley.

Geographic entities mentioned:
surface_form: Kennebecasis River
instance_of: Watercourse
countries: Canada
coordinates: lat: 45.31666667
lon: -66.13333333