Sarmila/GeoWiki-Features huggingface dataset:
Though Diamond Peak's eruptions always produced olivine-rich basaltic andesite, they likely grew more rich in silicon dioxide over time, ranging from 55 to 58 percent silicon dioxide. Lava flows from the volcano vary from in thickness, rich in porphyritic rocks like olivine, plagioclase, and clinopyroxene; there is no silicic rock (rich in silica) in the Diamond Peak vicinity.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Mazama Ash, including pumice up to thick as well as plagioclase, pyroxene, and hornblende crystals, can be found throughout the Diamond Peak wilderness area and represents the newest volcanic rock deposited in the region. In total, eruptive output probably totaled in volume. The volcano is older than the last glacial period that ended 11,000 years ago, but probably younger than 100,000 years.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Heavily eroded by glaciers, which no longer exist on Diamond Peak, the mountain has several cirques from glacial erosion, some of which have talus deposits due to Holocene glacial motion. Glaciers also placed both lateral and ground moraines along the lower to middle elevations of the wilderness area, unlayered pebble deposits interbedded with sand and rock.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Snowfields on the northern side may have been glaciers as recently as 100 years ago. Subfeatures. Nearby features include Crater Butte, a basaltic andesite cinder cone volcano to the southeast, and Redtop Mountain, to the east and composed of basalt. Both mountains are likely close to the same age as Diamond Peak, and are formed by layers of red and black lapilli, scoria, and volcanic bombs.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Emigrant Butte, a basaltic andesite peak to the south, has been altered more extensively by glaciers, and therefore is likely older. Mount Yoran is a significantly older mountain made from basaltic andesite lava that has a summit protruding from the northern slope of Diamond Peak. It has been potassium–argon dated to be between 520,000 and 220,000 years old.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
It has been potassium–argon dated to be between 520,000 and 220,000 years old. A shield volcano, Yoran is often considered one of the subfeatures of Diamond Peak, along with the Diamond Rockpile cinder cone and Crater Butte. Yoran and the nearby stratovolcano Lakeview Mountain have similar compositions to Diamond Peak, with dissected cones made of pyroclastic material with embedded lava flows.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
It has been potassium–argon dated to be between 520,000 and 220,000 years old. A shield volcano, Yoran is often considered one of the subfeatures of Diamond Peak, along with the Diamond Rockpile cinder cone and Crater Butte. Yoran and the nearby stratovolcano Lakeview Mountain have similar compositions to Diamond Peak, with dissected cones made of pyroclastic material with embedded lava flows.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Both volcanoes have been invaded with sills fed by dikes that can be traced to nearby volcanic plugs. Ecology. The ecology of Diamond Peak is characteristic of the Oregon Cascades. The forests supported by the wilderness area include flora such as lodgepole pine, western white pine, mountain hemlock, noble fir, and silver fir trees. Timberline is at an elevation of about.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
The abundance of water supports mosquito populations, particularly during the early summer. Human history. William Macy and John Diamond climbed Diamond Peak in July 1852. These two men were part of a preliminary survey party known as the &quot;Road Viewers.&quot; They climbed the peak in order to plan a road that later became known as the Free Emigrant Road.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
While cinder from the Red Mountain and Crater Butte cinder cones, estimated at a volume of, might be useful for construction materials for road building, there is plenty of cinder and rock outside of the immediate vicinity of Diamond Peak. The closest mining operations took place in the Bohemia district, which lies to the west of Diamond Peak.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Moreover, the volcano has little potential as a geothermal energy resource, since the surrounding area lacks hot springs. Therefore, in the 1980s, surveyors determined that there is little future potential for mineral deposits or geothermal energy resources for Diamond Peak or the wilderness area. Recreation.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Recreation. Though Diamond Peak cannot be accessed by paved roads, it lies adjacent on its eastern side to the Pacific Crest Trail. Although the mountain lacks a clearly denoted trail to the top, and itself has multiple peaks, which can make identification of the summit difficult, summitting Diamond Peak is not a technical climb.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
The two major routes to the southern summit offer views of Summit Lake and Mount Thielsen. Another route for climbing Diamond Peak begins from Corrigan Lake, which can be reached by forest roads about past Hills Creek Reservoir near Oakridge. The Corrigan Lake Trailhead starts at an elevation of, following a forested trail toward Diamond Peak's western flank.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
A challenging trip, it may demand the use of crampons (traction devices attached to footwear to improve mobility on snow and ice) and an ice axe if conditions dictate. Because of avalanche hazards on the western side of Diamond Peak, the route can be dangerous. The climb runs about for the round trip, achieving the peak's elevation of.

Geographic entities mentioned:
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 36.82632
lon: -118.39149
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 40.9503
lon: -108.878
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 35.76777
lon: -113.35382
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 43.5207
lon: -122.15
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 44.1417
lon: -113.083
surface_form: diamond peak
instance_of: Mountain
countries: United States
coordinates: lat: 39.5849
lon: -115.819
Snowfields on the northern side may have been glaciers as recently as 100 years ago. Subfeatures. Nearby features include Crater Butte, a basaltic andesite cinder cone volcano to the southeast, and Redtop Mountain, to the east and composed of basalt. Both mountains are likely close to the same age as Diamond Peak, and are formed by layers of red and black lapilli, scoria, and volcanic bombs.

Geographic entities mentioned:
surface_form: cinder cone
instance_of: Mountain
countries: United States
coordinates: lat: 40.547386111111
lon: -121.31997222222
Ecology. The ecology of Diamond Peak is characteristic of the Oregon Cascades. The forests supported by the wilderness area include flora such as lodgepole pine, western white pine, mountain hemlock, noble fir, and silver fir trees. Timberline is at an elevation of about. Along Yoran Lake, there are forests of Engelmann spruce, silver fir, and noble fir, as well as a wet meadow.

Geographic entities mentioned:
surface_form: hemlock
instance_of: Lake
countries: United States
coordinates: lat: 42.718611111111
lon: -77.608888888889
Summit Range. The Summit Range is a mountain range in San Bernardino County, California. They are one of the eastern limits of the Fremont Valley, and in the Mojave Desert.

Geographic entities mentioned:
surface_form: Fremont Valley
instance_of: Valley
countries: United States
coordinates: lat: 35.1083
lon: -118.047
Dorotej of Hilandar. Dorotej or Dorotheus () was a Serbian Orthodox abbot of Hilandar and the &quot;protos&quot; of Mount Athos from 1356 until 1366. He is noted for writing a charter for the monastery of Drenča in 1382. Drenča. The village of Drenča, 5 km north of town of Aleksandrovac, was home to the ruined church of &quot;Dušmanica&quot;, as it is called by village's elders.

Geographic entities mentioned:
surface_form: Mount Athos
instance_of: Mountain
countries: Greece
coordinates: lat: 40.15833333333333
lon: 24.327222222222222
Vračar plateau. Vračar plateau () is a plateau on top of the Vračar Hill in Belgrade, the capital of Serbia, with an absolute height of above sea level. It is the purported location of the 1594 Burning of Saint Sava's relics by the Ottomans.

Geographic entities mentioned:
surface_form: vračar plateau
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.7833
lon: 20.45
Along the way, the Ottoman convoy had people killed in their path so that the rebels in the woods would hear of it. The relics were publicly incinerated by the Ottomans, on 27 April 1595, as it was placed on a pyre and burnt on the Vračar plateau, and the ashes were scattered. According to Nikolaj Velimirović the flames were seen over both the Danube and the Sava rivers.

Geographic entities mentioned:
surface_form: vračar plateau
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.7833
lon: 20.45
Propositions include: Crveni Krst, suggested by who erected reddish Vozarev Krst at the spot, which gave name to the entire neighborhood of Crveni Krst (&quot;Red Cross&quot;); mound of &quot;Čupina Humka&quot;, in Tašmajdan, previously known as Little Vračar, which is the preferred location of modern historians; Vračar plateau, which attracted the widest public acceptance. 19th century.

Geographic entities mentioned:
surface_form: vračar plateau
instance_of: Mountain
countries: Serbia
coordinates: lat: 44.7833
lon: 20.45
Najafgarh Lake. Najafgarh Lake (Najafgarh Marsh or Najafgarh Jheel), fed by Yamuna's tributary Sahibi River, used to be a vast lake in the south west of Delhi, near the town of Najafgarh, from which it takes its name.

Geographic entities mentioned:
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
After the 1960s the Flood Control Department of Delhi canalised the Najafgarh lake area which came to be known as the Najafgarh drain, which led to the eventually partial drainage of, the once huge and ecologically rich, Najafgarh lake.

Geographic entities mentioned:
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
The Najafgarh drain itself is designated as the Najafgarh drain bird sanctuary which together with the partially drained Najafgarh Lake and adjoining farm land comprise a rich wetland bird habitat used by hundreds of congregating demoiselle cranes, common cranes,sarus cranes, hares, nilgai, wildcat, common fox, jackal, monitor lizards, various varieties of snakes etc. History.

Geographic entities mentioned:
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
Development of major housing colonies in the former Najafgarh lake basin: After the complete draining of the lake in the 1960s the former lake basin was converted into farmland first and by now various large scale housing projects occupy the former lake basin, including Vikaspuri, Uttam Nagar, Pappankalan, Dwarka etc, which have shrunk the overall area of the combined wetland area of Najafgrah Drain Brid Sanctuary and Najafgarh Lake.

Geographic entities mentioned:
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
surface_form: najafgarh lake
instance_of: Lake
countries: India
coordinates: lat: 28.504
lon: 76.944
Geographically, we propose that numerous modern communities in the Jordan Valley, the Mediterranean coast, the upper Euphrates and Tigris valleys, and central Anatolia developed distinct, local management traditions. Among other things, the island of Lemnos has some of the Aegean Sea's earliest hunter-fisherman villages, dating to the 11th millennium BC. Beginnings of agriculture.

Geographic entities mentioned:
surface_form: Jordan Valley
instance_of: Valley
countries: Jordan
coordinates: lat: 32.317222
lon: 35.57
Aoufous Formation. The Aoufous Formation is a geological formation that contains some of the vertebrate assemblage of the Kem Kem Group, of Late Cretaceous date. It underlies the Ifezouane Formation and overlies the Akrabou Formation. Description. The Aoufous Formation was first reported by Dubar (1948) as part of the “Sillon Preafricain”.

Geographic entities mentioned:
surface_form: Kem Kem Group
instance_of: Mountain
countries: Morocco
coordinates: lat: 30.9
lon: -4
The diocese is seated in the city of Tromsø at the Tromsø Cathedral, the seat of the presiding bishop, Olav Øygard (bishop since 2014). History. Originally, this area was a part of the great Diocese of Nidaros, which covered all of Northern Norway from Romsdalen and north (Finnmark, Troms, and Nordland counties).

Geographic entities mentioned:
surface_form: Romsdalen
instance_of: Valley
countries: Norway
coordinates: lat: 62.447222222222
lon: 7.8333333333333
Geography. The city is in the central part of Oklahoma County, approximately west of downtown Oklahoma City, and is bounded by Warr Acres on the east and by Lake Overholser and Stinchcomb Wildlife Refuge on the west. According to the United States Census Bureau, the city has a total area of, all land. Demographics.

Geographic entities mentioned:
surface_form: Lake Overholser
instance_of: Lake
countries: United States
coordinates: lat: 35.4977
lon: -97.6796
It is situated in the Gangotri National Park. The elevation of Kalidhang is and its prominence is. It is joint 105th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3 km WNW of Chirbas Parbat its nearest higher neighbor. Matri lies 5.7 km SE and it is 11.8 km NNE of Manda I. It lies 10.1 km NNW of Sudarshan Parbat. Glaciers and rivers.

Geographic entities mentioned:
surface_form: Nanda Devi
instance_of: Mountain
countries: India
coordinates: lat: 30.37388888888889
lon: 79.97083333333333
It is situated in the Gangotri National Park. The elevation of Kalidhang is and its prominence is. It is joint 105th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3 km WNW of Chirbas Parbat its nearest higher neighbor. Matri lies 5.7 km SE and it is 11.8 km NNE of Manda I. It lies 10.1 km NNW of Sudarshan Parbat. Glaciers and rivers.

Geographic entities mentioned:
surface_form: Chirbas Parbat
instance_of: Mountain
countries: India
coordinates: lat: 31.034166666666668
lon: 79.0525
It is joint 105th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3 km WNW of Chirbas Parbat its nearest higher neighbor. Matri lies 5.7 km SE and it is 11.8 km NNE of Manda I. It lies 10.1 km NNW of Sudarshan Parbat. Glaciers and rivers. It stands at the head of Dehigad Bamak which flows from south to north and joins river Jadh Ganga.

Geographic entities mentioned:
surface_form: Manda I
instance_of: Mountain
countries: India
coordinates: lat: 30.940277777777776
lon: 78.99861111111112
surface_form: matri
instance_of: Mountain
countries: India
coordinates: lat: 31.014722222222222
lon: 79.06972222222223
Nanda Devi, is the highest mountain in this category. It lies 3 km WNW of Chirbas Parbat its nearest higher neighbor. Matri lies 5.7 km SE and it is 11.8 km NNE of Manda I. It lies 10.1 km NNW of Sudarshan Parbat. Glaciers and rivers. It stands at the head of Dehigad Bamak which flows from south to north and joins river Jadh Ganga. Chaudar Bamak on the west side also drains down to Jadh Ganga.

Geographic entities mentioned:
surface_form: Sudarshan Parbat
instance_of: Mountain
countries: India
coordinates: lat: 30.976944444444445
lon: 79.09333333333333
Kalidhang. Kalidhang is a mountain of the Garhwal Himalaya in Uttarakhand India. It is situated in the Gangotri National Park. The elevation of Kalidhang is and its prominence is. It is joint 105th highest located entirely within the Uttrakhand. Nanda Devi, is the highest mountain in this category. It lies 3 km WNW of Chirbas Parbat its nearest higher neighbor.

Geographic entities mentioned:
surface_form: kalidhang
instance_of: Mountain
countries: India
coordinates: lat: 31.044444444444444
lon: 79.02222222222223
Within this initiative, Ivan Franko serves as a guide, imparting a distinctive narrative to tourists and reshaping their perception of the past. A pivotal component of this undertaking was the establishment of a two-day tourist route, &quot;To Pikui!&quot;, spanning 167 km, and incorporating overnight accommodations in Mshanets village.

Geographic entities mentioned:
surface_form: Pikui
instance_of: Mountain
countries: Ukraine
coordinates: lat: 48.829444444444
lon: 23.000833333333
Casa de Quevedo, and the consolidation of the University, which brought new life to the town in 1985. Location. Albacete is located in the South-East of the Iberian Peninsula, in the plains of La Mancha (part of the Inner Plateau), at an elevation of about. The surrounding region, the so-called &quot;Mancha de Albacete&quot; stands out for its horizontality.

Geographic entities mentioned:
surface_form: Inner Plateau
instance_of: Plateau
countries: Spain
coordinates: lat: 40.5
lon: -3.5
With a total length in excess of, the Tambo River is one of the longest rivers in the East Gippsland drainage basin, extending from the steep forested southern slopes of the Victorian Alps through forest and farmland to the Gippsland Lakes. Course. The Tambo River rises in the Bowen Mountains, below Mount Leinster in the Victorian Alps, part of the Great Dividing Range, about east of.

Geographic entities mentioned:
surface_form: Gippsland Lakes
instance_of: Group of lakes
countries: Australia
coordinates: lat: -38
lon: 147.65
Etymology. The species name &quot;effractella&quot; derives from Latin &quot;effractus&quot;, meaning “broken out”. Distribution and habitat. This species is present in most of Europe, including British Islands and except Fennoscandia, Ireland and Estonia. The distribution extends from west Portugal, across Central, Southern and Eastern Russia. In the south the area extends to Italy and Greece.

Geographic entities mentioned:
surface_form: Fennoscandia
instance_of: Landform
countries: Norway
Sweden
Finland
Russia
Russian Empire
Soviet Union
coordinates: lat: 63
lon: 17
Chaudière Falls (Chaudière River). Chaudière Falls (,) is a waterfall in Lévis, Quebec, along the Chaudière River. It is part of the regional Parc des Chutes-de-la-Chaudière, which features a suspension footbridge standing 23 metres over the river. There are walking and bicycle trails along the river.

Geographic entities mentioned:
surface_form: Chaudière River
instance_of: Watercourse
countries: Canada
coordinates: lat: 46.742777777777775
lon: -71.2786111111111
Canal das Rolas. The Canal das Rolas (&quot;Rolas Channel&quot;) is a strait of the Atlantic Ocean separating the small Ilhéu das Rolas (also: &quot;Ilhéu Gago Coutinho&quot;) from the southernmost point of the island of São Tomé, in São Tomé and Príncipe. It is wide. There is a ferry departing from Ponta Baleia on São Tomé Island to Ilhéu das Rolas.

Geographic entities mentioned:
surface_form: canal das rolas
instance_of: Body of water
countries: São Tomé and Príncipe
coordinates: lat: 0.01
lon: 6.52
Cranberry Lake (Ontario). Cranberry Lake is a lake in the city of Kawartha Lakes, Ontario, Canada.

Geographic entities mentioned:
surface_form: kawartha
instance_of: Group of lakes
countries: Canada
coordinates: lat: 44.4994
lon: -78.441
surface_form: cranberry lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.77046
lon: -79.05002
Cranberry Lake (Ontario). Cranberry Lake is a lake in the city of Kawartha Lakes, Ontario, Canada.

Geographic entities mentioned:
surface_form: cranberry lake
instance_of: Lake
countries: Canada
coordinates: lat: 44.77046
lon: -79.05002
Binboğa Mountains. Binboğa Mountains are a mountain range located in Kahramanmaraş Province, southern Turkey. Binboğa Mountains are located at about [west of Afşin, within Sarız in Kayseri Province, Afşin and Göksun districts in Kahramanmaraş Province, and are oriented in north-south direction. The mountain range stretches over an area of, and has an elevation from up with its peak at.

Geographic entities mentioned:
surface_form: binboğa mountains
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.32126
lon: 36.63775
Highlands in the region are Subatan, Evciyurdu, Ebelik and Osmanoğlu, which serve as summer season resort. The general geology of the Binboğa Mountains, which is a part of the Eastern Taurus Mountains, is represented by the lithology of Carbonate platform and Binboğa Mélange formation, which was created when South Neotethys closed off at the end of the Cretaceous period.

Geographic entities mentioned:
surface_form: binboğa mountains
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.32126
lon: 36.63775
Hurman and Göksun are two creeks, which spring off the mountain range. In terms of botanic, Binboğa Mountains are habitat of a quite rich vegetation. There are a rich population of endemic flora, such as the hyacinth species, which grow on rocks. Nature and National Parks Directorate of Kahramanmaraş Province recorded 177 endemic flora species on Binboğa Mountains.

Geographic entities mentioned:
surface_form: binboğa mountains
instance_of: Mountain
countries: Turkey
coordinates: lat: 38.32126
lon: 36.63775
Tama Lakes. The Tama Lakes () are two crater lakes in New Zealand's Tongariro National Park. They fill two (Upper and Lower Tama) of a series of explosion craters on the Tama Saddle between Mount Ruapehu and Mount Ngaruahoe (a main Mount Tongariro vent). Geologically the deep magma source and depth of basement are not usual for vents in the area. Hydrology.

Geographic entities mentioned:
surface_form: Mount Tongariro
instance_of: Mountain
countries: New Zealand
coordinates: lat: -39.12972222222222
lon: 175.63583333333332
Monte Pissis. Monte Pissis is an extinct volcano on the border of the La Rioja and Catamarca provinces in Argentina, to the east of the Chilean border and about north of Aconcagua. The mountain is the second-tallest volcano in the world and the third-highest mountain in the Western Hemisphere.

Geographic entities mentioned:
surface_form: Aconcagua
instance_of: Mountain
countries: Argentina
coordinates: lat: -32.653055555555554
lon: -70.01166666666667
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Elevation. A 1994 Argentine expedition claimed —using GPS technology available at the time— that the elevation of Monte Pissis was, higher than Ojos del Salado. Ten years later, with the use of higher precision systems, several other surveys proved that those measurements were inaccurate: in 2005, an Austrian team performed a DGPS survey of Pissis' summit and found the elevation to be.

Geographic entities mentioned:
surface_form: Ojos del Salado
instance_of: Mountain
countries: Chile
Argentina
coordinates: lat: -27.109444444444
lon: -68.542222222222
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Monte Pissis is a large andesitic-dacitic volcanic centre. It was formed between 6.6 and 6.2 million years ago. Like Cerro Bonete Chico it is one of the large volcanic complexes formed at that time over a deforming Nazca slab. Volcanism in the area ceased about 2 million years ago. Monte Pissis, Cerro Bonete Chico and Incapillo form a large volcanic complex that is among the highest in the world.

Geographic entities mentioned:
surface_form: Cerro Bonete Chico
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: bonete chico
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
Volcanism in the area ceased about 2 million years ago. Monte Pissis, Cerro Bonete Chico and Incapillo form a large volcanic complex that is among the highest in the world. Incapillo formed after Monte Pissis had ceased erupting, and hydrothermal activity at Incapillo may continue to this day. Climbing. Until recently, this mountain had received very little attention.

Geographic entities mentioned:
surface_form: bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: cerro bonete
instance_of: Mountain
countries: Argentina
coordinates: lat: -28.01861111111111
lon: -68.75611111111111
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Monte Pissis. Monte Pissis is an extinct volcano on the border of the La Rioja and Catamarca provinces in Argentina, to the east of the Chilean border and about north of Aconcagua. The mountain is the second-tallest volcano in the world and the third-highest mountain in the Western Hemisphere.

Geographic entities mentioned:
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
The mountain is the second-tallest volcano in the world and the third-highest mountain in the Western Hemisphere. Monte Pissis is named after Pedro José Amadeo Pissis, a French geologist who worked for the Chilean government. Due to its location in the Atacama Desert, the mountain has very dry conditions but features an extensive glacier, with crevasses, which is unique in the region.

Geographic entities mentioned:
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
In 2006 an international expedition surveyed the height on the summit, and found results in agreement with an elevation around. This was later confirmed by a 2007 Chilean-Argentine-European expedition, which surveyed both Ojos del Salado and Monte Pissis and provisionally found the former to be and the latter. Geology. Monte Pissis is a large andesitic-dacitic volcanic centre.

Geographic entities mentioned:
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
This was later confirmed by a 2007 Chilean-Argentine-European expedition, which surveyed both Ojos del Salado and Monte Pissis and provisionally found the former to be and the latter. Geology. Monte Pissis is a large andesitic-dacitic volcanic centre. It was formed between 6.6 and 6.2 million years ago.

Geographic entities mentioned:
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Volcanism in the area ceased about 2 million years ago. Monte Pissis, Cerro Bonete Chico and Incapillo form a large volcanic complex that is among the highest in the world. Incapillo formed after Monte Pissis had ceased erupting, and hydrothermal activity at Incapillo may continue to this day. Climbing. Until recently, this mountain had received very little attention.

Geographic entities mentioned:
surface_form: monte pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Elevation. A 1994 Argentine expedition claimed —using GPS technology available at the time— that the elevation of Monte Pissis was, higher than Ojos del Salado. Ten years later, with the use of higher precision systems, several other surveys proved that those measurements were inaccurate: in 2005, an Austrian team performed a DGPS survey of Pissis' summit and found the elevation to be.

Geographic entities mentioned:
surface_form: pissis
instance_of: Mountain
countries: Argentina
coordinates: lat: -27.755277777777778
lon: -68.79916666666666
Angram Reservoir. Angram Reservoir is the first of three reservoirs on the River Nidd in Upper Nidderdale, North Yorkshire, England, the others being Scar House Reservoir and finally the compensation reservoir Gouthwaite Reservoir. It is located at OS map reference. Between them they attract around 150,000 visitors a year.

Geographic entities mentioned:
surface_form: Upper Nidderdale
instance_of: Valley
countries: United Kingdom
coordinates: lat: 54.0867
lon: -1.75773
Between them they attract around 150,000 visitors a year. The reservoir takes its name from Angram, a settlement in the township of Stonebeck Up, submerged when the reservoir was completed in 1919. Little Whernside () to the north and Great Whernside () to the west of the reservoir are close by. The River Nidd flows for approximately from the flanks of Great Whernside before joining the reservoir.

Geographic entities mentioned:
surface_form: Little Whernside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.1962
lon: -1.95849
surface_form: Great Whernside
instance_of: Mountain
countries: United Kingdom
coordinates: lat: 54.160911111111
lon: -1.9984305555556
T&T Ranch. The T&T Ranch (also written as TT Ranch and T and T Ranch) was a demonstration farm and dairy, that was situated in the Amargosa Valley, southeast of Leeland in Nye County, Nevada. It was owned by the Tonopah and Tidewater Railroad between its foundation in 1915 and the 1940s.

Geographic entities mentioned:
surface_form: Amargosa Valley
instance_of: Valley
countries: United States
coordinates: lat: 36.6333
lon: -116.4
Some of the large projects undertaken during his time in government were increased coal production and power generation in the Latrobe Valley, new offshore oil and gas fields in Gippsland, the West Gate Bridge over the lower Yarra River, a new international airport for Melbourne at Tullamarine and two new universities (Monash University and La Trobe University).

Geographic entities mentioned:
surface_form: Latrobe Valley
instance_of: Valley
countries: Australia
coordinates: lat: -38.1806
lon: 146.278
Sør-Østerdal District Court. Sør-Østerdal District Court () was a district court in Innlandet county, Norway. The court was located in Elverum. It included the southern part of Østerdalen, including the municipalities of Elverum, Trysil, Våler, Åmot, and Åsnes. Cases from this court could be appealed to Eidsivating Court of Appeal. The court was led by a chief judge () and several other judges.

Geographic entities mentioned:
surface_form: Østerdalen
instance_of: Valley
countries: Norway
coordinates: lat: 61.575916666666664
lon: 11.087111111111112
Some of the old modernist houses have been catalogued as part of Mexico's national patrimony. History. The Pedregal lava fields were formed by the eruption of the Xitle volcano around 5000 BC, but there are documented eruptions until 400 AD. The area near what is currently el Pedregal, called Cuicuilco, has been inhabited since ca. 1700 BC.

Geographic entities mentioned:
surface_form: Xitle
instance_of: Mountain
countries: Mexico
coordinates: lat: 19.245669
lon: -99.222706
The area near what is currently el Pedregal, called Cuicuilco, has been inhabited since ca. 1700 BC. Around 300 BC, the area contained what was probably the biggest city in the Valley of Mexico at the time. Its importance started to decline around the 100 BC and was completely empty by 400 AD. Urban development.

Geographic entities mentioned:
surface_form: Valley of Mexico
instance_of: Valley
countries: Mexico
coordinates: lat: 19.66666667
lon: -98.86666667
It is situated on the shared boundary of Kings Canyon National Park and John Muir Wilderness, and along the common border of Fresno County and Inyo County. It is west of the community of Big Pine, 0.8 mile (1.3 km) northwest of Mount Johnson, and one mile (1.6 km) southeast of Mount Thompson, which is its nearest higher neighbor. Mount Gilbert ranks as the 127th-highest summit in California.

Geographic entities mentioned:
surface_form: mount thompson
instance_of: Mountain
countries: United States
coordinates: lat: 48.5458
lon: -113.688
surface_form: mount thompson
instance_of: Mountain
countries: United States
coordinates: lat: 37.1429902
lon: -118.613442
surface_form: mount johnson
instance_of: Mountain
countries: United States
coordinates: lat: 62.89472222222222
lon: -150.70777777777778
surface_form: mount johnson
instance_of: Mountain
countries: United States
coordinates: lat: 37.12882
lon: -118.58594
surface_form: mount johnson
instance_of: Mountain
countries: United States
coordinates: lat: 47.832665
lon: -123.237308
Mount Gilbert ranks as the 127th-highest summit in California. Topographic relief is significant as the south aspect rises above LeConte Canyon in less than two miles, and the northern aspect rises 3,340 feet above South Lake in 2.5 miles. History. This mountain's name commemorates eminent geologist Grove Karl Gilbert (1843–1918), who worked much of the Sierra Nevada range with the Wheeler Survey.

Geographic entities mentioned:
surface_form: south lake
instance_of: Lake
countries: United States
coordinates: lat: 43.5860057
lon: -74.6305866
surface_form: south lake
instance_of: Lake
countries: United States
coordinates: lat: 43.3034
lon: -74.5238
Mount Gilbert (California). Mount Gilbert is a mountain located on the crest of the Sierra Nevada range in California, United States. It is situated on the shared boundary of Kings Canyon National Park and John Muir Wilderness, and along the common border of Fresno County and Inyo County.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert (california)
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
Mount Gilbert (California). Mount Gilbert is a mountain located on the crest of the Sierra Nevada range in California, United States. It is situated on the shared boundary of Kings Canyon National Park and John Muir Wilderness, and along the common border of Fresno County and Inyo County.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: a mountain
instance_of: Mountain
countries: United States
coordinates: lat: 32.2925
lon: -106.69777777778
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
It is situated on the shared boundary of Kings Canyon National Park and John Muir Wilderness, and along the common border of Fresno County and Inyo County. It is west of the community of Big Pine, 0.8 mile (1.3 km) northwest of Mount Johnson, and one mile (1.6 km) southeast of Mount Thompson, which is its nearest higher neighbor. Mount Gilbert ranks as the 127th-highest summit in California.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
Board on Geographic Names. The first ascent of the peak was made September 15, 1928, by Norman Clyde, who is credited with 130 first ascents, most of which were in the Sierra Nevada. Climate. Mount Gilbert is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains.

Geographic entities mentioned:
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 61.1725
lon: -148.2717
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 40.6244
lon: -115.446
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 54.2521
lon: -165.662
surface_form: mount gilbert
instance_of: Mountain
countries: United States
coordinates: lat: 37.1363688
lon: -118.5982233
However, some within Atari at the time dispute this, stating that Opperman had provided several different possible designs, and that this was the one selected by Bushnell and others. The logo first appeared on Atari's arcade game &quot;Space Race&quot; in 1973, and became known as the &quot;Fuji&quot; due to its resemblance to Mount Fuji.

Geographic entities mentioned:
surface_form: Mount Fuji
instance_of: Mountain
countries: Japan
coordinates: lat: 35.36055555555556
lon: 138.7275
SS D. M. Clemson (1903). SS &quot;D. M. Clemson&quot; was a long steel-hulled Great Lakes freighter that went missing on 1 December 1908, on Lake Superior. The ship was last seen coming through the Soo Locks, onto Lake Superior. The ship was built in 1903 for the Provident Steamship Company. She is known for sinking on Lake Superior, with the entire crew of 24 men losing their lives.

Geographic entities mentioned:
surface_form: Lake Superior
instance_of: Lake
countries: Canada
United States
coordinates: lat: 47.52881611111111
lon: -87.76002194444445